裂缝性油藏:勘探和开发的具体情况

作者:尤里·林伯格(Yuri Limberger)——录井专家

裂缝性储层广泛存在于地下地层、不同深度以及大范围的压力和温度下。颗粒型储层(粒间储层、多孔储层)的分布仅与陆源岩和碳酸盐岩有关,即与特定但有限岩性的岩石有关,而裂缝型储层的发现和开发不仅与上述岩石有关但在页岩、花岗岩、粘土岩等不常见的储层岩石中

此类油藏的特点是累计产油量破纪录,有时单井突破百万吨。

本文谨供读者查阅,是作者多年研究的成果,试图解决油气田勘探勘探和油气开采过程中裂缝性油气藏识别和勘探的一些实践和理论问题。

这些研究包括:

  • 井柱地下勘探地球物理技术理论相关单项任务的陈述、设置和解决;
  • 根据获得的理论解计算地质和地球物理情况;
  • 开发裂缝性油藏研究新方法;
  • 处理和解释与在井内使用这些技术相关的结果;
  • 裂缝性油藏油田试井和开发数据的处理、解释和概括;
  • 特殊实验研究结果的处理和解释;
  • 对其他研究人员发表的出版物进行批判性的重新评估。

总体而言,针对所考虑的主题,对 180 个地区和油田的 1200 多口井的材料进行了研究。

从第一口探井的钻探开始到完全含水为止,对某些矿区的勘探和开发历史进行了跟踪。这些油田位于不同的地理、地质和气候条件下。裂缝性储层的年龄范围从渐新世到里菲世。储层岩石由砂岩、粉砂岩、石灰岩、白云岩、粘土岩、花岗岩、凝灰岩等组成,地层压力由异常低到极高,温度范围为25°小至185°。也就是说,已经在现代实践中遇到的整个地质和技术条件范围内研究了裂缝性油藏。

裂缝性储层结构

迄今为止,国内外大部分地质学家、地球科学家、油田开发人员都有裂缝性储层模型的概念,裂缝性储层模型是由不同方向、不同角度的裂缝分割而成的岩石体积。梯度和裂缝张开(图1)。这样的概念是对地质露头和岩心进行一些视觉观察的结果,传递到地表,它没有考虑到实际条件下发生的岩石的应力状态。因此,首先有必要解释油气藏的结构,因为对一个研究对象没有清晰的认识,就不可能制定其研究方法并分析油气生产过程中所发生的变化。

图1裂缝性油藏结构的普遍概念

通过对影响岩石元素的应力的最简单的考虑来判断,首先提出了一个工作假设:在自然条件下,出现垂直裂缝的概率高于出现开放水平裂缝的概率。使用三种独立的方法对该假设进行了检验:1)通过将完井结果与钻井过程中流失的冲洗液量进行比较。2) 通过比较流体流入的形成与钻孔壁上存在的切向应力;3) 通过研究 Yaregskoye 油田石油矿中岩石露头的描述。

基于第一种方法,认为钻井过程中吸收的冲洗液会沿着垂直裂缝系统下降到产状的含水部分,不会干扰清洁油的开采。如果那里存在水平裂缝,所吸收的流体将不可避免地与储层流体一起被回收。对裂缝性油藏钻探的 150 口井完井后获得的数据进行了分析,这些井的钻探表明,吸收的冲洗液体积从数百立方米到数十万立方米不等(许多井是用泵送的冲洗液钻的,根本没有出现在地表上)。所有这些井完井后的结果是油中不含任何吸收冲洗液的迹象。

因此,第一种方法证实了垂直张开裂缝在原位流体流动中起主导作用的假设。

第二种方法考虑了在钻孔壁及其附近产生和活跃的切向应力蟽θ的影响。在增产过程中可能产生的某些条件下,切向应力可能超过地层压力袪锌谢..这将导致垂直裂缝的壁闭合,井与储层之间的水力连接丧失,以及此类测试的结果是缺乏液体流入。水平裂缝在切向应力的影响下不可能闭合;储层和钻孔之间的液压连接仍然存在,并且流体将被回收。数据选取是在对以裂缝性油藏为代表的100多个目标进行测试后进行的,其改造过程中蟽>锌谢被保留下来。所有的目标首先碰巧都是“里”。刺激完成后,它们都产生地层流体。

使用第二种方法和第一种方法获得的结果证实了开放垂直裂缝在原位流体流动中起主导作用的假设。

使用第三种方法,研究了泥盆纪砂岩的详细描述,该砂岩发生在 180-250 m 深处,其石油是在 Yareganskoye 油田采用竖井法生产的。不同作者的研究著作中仅提到了近垂直的开放性骨折[2;12]。

我们应该注意到,这些数据反驳了关于在相对较浅的深度可能存在开放水平裂缝的可能性的广泛观点。

因此,事实证明,在天然岩石条件下,只有垂直裂缝才能打开(图2)。这些裂缝在产状中形成单一网络,为产状不同部分之间的水平和垂直方向提供水力连接。裂缝性油气藏探明结构的依据是岩体内部裂缝分布不均匀、不同开度裂缝在油气生产过程中的不均等性以及近垂直方向开放裂缝的主导作用。

图2裂缝性油藏真实结构

勘查勘探阶段要达到的目标

在开始新领域的勘探和勘探工作时,应始终牢记钻入和钻探裂缝性油藏的可能性。在这种情况下,人们必须解决一些特定于此类储层的任务,这些任务通常不包括在使用地球物理和水动力研究技术研究横截面的计划中。下面列出了裂缝性油藏研究中需要解决的一些核心任务,并给出了解决方法:

  • 识别井柱中的开放裂缝;
  • 评估水库类型;
  • 估计开放裂缝的垂直延伸范围;
  • 描绘裂缝和井之间的交点;
  • 提供下降压力以刺激流体从裂缝流入;
  • 估计骨折能力。

井柱中开放裂缝的识别方法

可以采用多种方法从根本上解决特定井柱是否存在开放裂缝的问题:

  1. 记录钻井过程中的滤失量和气、水、油的显示。钻井过程中记录的流体损失和/或气体、水和油显示通常是由与井相交的开放裂缝的存在引起的。在正常钻井进度过程中记录此类并发症可以指出井柱中是否存在裂缝,并且可以估计地层压力并识别节理区域。
  2. 寻找流动潜力。裂缝中流动电势(或自电势(SP))电动势问题的理论解表明[9],这种电动势比毛细管渗流电势电动势高4倍(亥姆霍兹方程)并可能带来极高的自身潜力。通过将实际 SP 异常幅度与标称静态电势进行比较,可以检测由于开放裂缝密度而导致的流动电势的存在 [8]。该方法最适合用于主要由陆源岩石组成的井柱。
  3. 比较不同长度波的传播速度如果岩石基质结构均匀,则短波和长波的传播速度相等。如果岩石基质结构受到开放裂缝的显着扰动,则短波的传播速度将超过长波的传播速度。在声波和地震频率范围内获得的值(声波测井和剖面拍摄数据)被用作不同长度的波速。该方法适合在岩性不变、深度较大的岩石深处使用。
  4. 比较水平应力与地层压力开放性垂直裂缝存在的条件是地层压力超过水平应力蟽谐芯褉(袪锌谢>蟽谐芯褉)。否则一定会丢失开放性骨折[6, 13]。流入测试过程中使用压力表测量地层压力。

水平应力可以使用两种方法确定:计算和使用地层水力压裂的结果。在第一种情况下:

谐芯褉= 未褋褉鈥� g � h � 谓/(1-谓) (1),

式中,未褋褉”为地下岩石从地表到深度h的平均密度;

谓“是泊松常数;g”为重力加速度。

泊松常数是根据已知公式根据纵波和横波传播速度的测量来计算的,如今它已成为常规程序。

如果在记录压裂过程期间考虑应力集中因子,则根据地层水力压裂结果确定水平应力可以为我们提供更准确的值。

否则,最小水平应力将被显着高估。文献[10]详细考虑了基于地层水力压裂材料的最小蟽谐芯褉值的确定。

值得注意的是,根据地层水力压裂材料确定的水平应力与地下压力计测量的地层压力进行比较的方法,为确定井柱中是否存在开放性垂直裂缝提供了绝对保证。在考虑中。

确定储层类型

储层类型的确定实际上仅限于岩石基质滤失特性的评价。为什么它是必要且重要的?如果岩石基质是可渗透的,那么我们就得到了具有可渗透基质的裂缝性储层,但是如果岩石基质是不可渗透的,那么我们就处理了纯裂缝性储层。

在第一种变体中,在估算储量时可以忽略裂缝系统的容量,因为它相对于基质孔隙体积的容量来说是非常低的,并且如果我们使用地球物理方法确定孔隙度,则它在绝对误差范围内。在第二种变体中,裂缝网络的容量决定了矿点的商业矿藏量。

通常用于判断是否存在粒间储层的岩石渗透率定性指标在这种情况下也是可以接受的。如果建立了这样的渗透率指标,我们就可以处理具有渗透基质的裂缝性储层。但如果我们没有明确的迹象表明岩石基质是可渗透的,我们就会得到一个纯粹的裂缝性储层。当我们具有钻井冲洗液的某些特性时,可能会丢失岩石基质渗透性的清晰迹象。对于这种情况,两种概念上新的任务解决方法已经被合理化和测试。

第一个是基于检测近井筒区域的拉裂,这些拉裂是在钻井过程中大量形成的,并且沿径向延伸。当冲入孔内的冲洗流体压力超过切向应力和岩石拉(断裂)应力之和时,就会出现这种裂缝。根据已知的近井预应力岩石任务理论解计算表明,狂野压裂区半径(R)不会超过井半径(R)的1.2~1.5,即R/R≤ �1,5。如果检测到这样的裂缝区域,则表明岩石基质是不渗透的。超出该区域,切向应力会产生收缩。

自发形成的裂缝区域是使用密度增加的冲洗液钻探的井柱的典型特征。在由不同岩性岩石组成的井柱中,使用密度不小于1.6 g/cm 3的冲洗液钻井时,有连续延伸超过1 km的记录

第二种方法基于上述关于确定直井附近应力的任务的理论解决方案,并且通过改变井底压力来考虑井面积限制内的切向应力来实现。

垂直裂缝延伸度的测定

为了确定裂缝性储层的垂直下边界并估算油气储量,需要了解垂直裂缝在垂直方向上的延伸范围。这可以使用上述裂缝识别方法通过比较水平应力与地层压力来定义。只要满足袪锌谢>蟽谐芯褉的条件,一定深度下就可能存在开放的垂直裂缝。当应用这种方法时,有必要估计水平压力和地层压力沿所考虑的井柱深度的变化。

有限厚度地层中的裂缝长度通常限制在地层厚度内。在地层压力异常高的区域,该规则被违反,其中开放垂直裂缝的连续长度(无论其离散层数如何)可能超过 1.5 公里。

识别裂缝井交叉点

正在解决的这一任务为选择从裂缝中生产地层流体的正确间隔提供了可靠的基础。井和开放裂缝之间的交点实际上是储层-钻孔水力通道到达井壁的点。因此,我们可以得出结论,记录这些通道上的流体运动的方法应该比其他方法具有明显的优先级。最简单的方法是记录钻井过程中的流体损失和/或气-油-水显示:记录事件的深度必须是第一近似值,即裂缝到达钻孔壁的位置。其他可能的变体是高电导率异常和存在流动潜力。为了准确地解决此任务,建议使用新方法,其具体使用取决于钻孔中泵送的冲洗液的特性。

如果井中充满了具有导电性的冲洗液,来自侧向测井装置中心电极的电流强度相当大,这将表明那里存在开放性裂缝。

电流强度记录为单独的曲线(图 3)。工作 [5] 中提出了该方法的理论论证。

图 3.使用横向 Log-3 (LL3) 中的电流强度异常来描绘断裂带 

如果井内充满了不导电的冲洗液,则采用感应测井。在这种情况下,感应测井的使用基于针对存在井和垂直裂缝的环境 3D 模型解决感应测井理论直接问题的结果 [3,7]。存在断裂的指标是电导率曲线出现特定形式的异常(图4)。

图 4利用感应测井电导率异常圈定断裂带

根据这些方法的应用结果,对井柱中开放裂缝的检测频率进行了检查。获得的数据显示,沿井筒两个连续裂缝(裂缝带)之间的距离在3米至84米之间。

使用地球物理调查方法对通过穿孔柱从裸眼井生产石油的井进行了额外的研究。

研究结果表明,石油是通过1至3条裂缝进入长度为150-200 m的裸眼井中,裂缝之间的距离不少于35 m。射孔柱中的活动裂缝之间的距离较小,但至少有一个射孔柱的产量不少于占总产量的70%至90%。考虑到裂缝的渗透率理论上与其开度的三次方成正比,所获得的数据意味着大开度裂缝在总产量中提供了主导份额的石油。

减少资金流入以刺激资金流入的理由

目前,我们没有地球物理方法来定义裂缝中流体填充的类型。作为解决这一任务的一种方法,流入井柱测试一直很流行。压降的基本原理是从裂缝中获取流体的保证。由于裂缝压缩系数不小于岩石孔隙压缩系数一个数量级,裂缝开度随着岩石应力的变化而发生显着变化,从而预先决定了裂缝的渗流能力。虽然地层压力大于井底压力(袪锌谢>袪蟹邪斜)是粒间油藏孔隙中石油增产的充分必要条件,但对于裂缝而言,这一条件的满足也是十分必要的。而满足第二个条件即“袪锌谢>蟽胃”就足够了。

较高的裂缝压缩系数预先决定了压降与油井产能之间的强相关性(图5)。正如我们从图中看到的,裂缝仅在一定的压降范围内屈服,这是为了刺激流入而产生的。超过压降的某个临界值会导致地层流体被阻止进入井中的情况。为了防止这种情况发生,应遵守根据各种目标测试结果制定的一个简单规则:在特定的地下条件和为此使用的测试设备下,裂缝流入刺激的压降必须尽可能低。

图 5. 裂缝性油藏的主曲线“压降”“生产率”,选项“最佳压降”。

实践中已经知道了多种情况,在钻井过程中井柱中记录到了明显的裂缝迹象,而在相应地层段的测试过程中实际上没有收到流体流入。各采油区统计数据显示,在钻井过程中使用钻杆测试仪对裂缝性油藏进行测试时,不少于70%的下入孔作业没有出现流体流入,测试目标为“瑞”。之后,当井完井后,所有这些目标都产生了地层流体的流入。它在主要测试期间的缺失是由于为了达到其最大规模而错误选择回撤造成的。

储量估算体积法

主要任务是裂缝网络容量的估计(裂缝孔隙度因子袣锌褌褉) ,其解决方案大部分预先确定碳氢化合物储量建议确定该因素的第一种方法包括找出岩石总孔隙度与基质孔隙度之间的差异。人们认为,中子测井和密度测井定义了总孔隙度,而声波测井或电测井可以定义基质孔隙度。但后者的结果受压裂影响,不能作为袣褌褉的估算标准。此外,地球物理方法估算孔隙度的绝对误差超过裂缝形成因子,因此地球物理方法原则上不适合解决此任务。

建议应用包围技术来估计袣褌褉值。该方法的实施需要在不同时间进行两次视电阻率测量,具有两个不同的冲洗流体电阻值。然后,使用在一定假设下推导的公式,我们计算裂纹形成因子。该方法的物理数学建模以及将获得的结果与袣褌褉模型进行比较表明了用于估计裂纹形成因子的包围技术的主要不可接受性。

一些著作包含基于岩石骨架压缩性、基质和裂缝的定义估计袣褌褉的描述。建议使用岩心分析、地球物理和横截面水动力测量的材料来评估压缩系数,即通过研究彼此之间几乎没有可比性的岩石体积。

不应同时应用核心和薄片中估计的裂纹形成因子的数据。这是因为我们观察到的压裂是岩石在钻探和提升到地面过程中变形的结果。

因此,目前还缺少任何已建立的估计裂纹形成因素的方法。解决这个问题的可能方法如下。利用从开发中移除的裂缝性储层的产状,可以使用体积法公式袣褌褉进行回溯计算,接受所生产的碳氢化合物的总累积体积。计算结果表明,裂缝网络的实际容量远低于个别出版物中遇到的袣褌褉值。

上述描述和勘测裂缝性储层的方法不仅适合在勘探和勘探阶段使用,而且适合在分析和重新解释先前钻井的材料期间使用。这些方法的特点是实施简单且每个公司都可以使用。通过在不同地区和油田的测试,证明了它们在解决既定任务方面的有效性,并证实了裂缝性油藏结构的确定性。对其中一个地区使用所描述的方法的结果可以作为说明性的例子,利用多年累积材料的分析结果,原则上可以强调大面积地区含油能力的前景。一种新的方式。[11]。

裂缝性油藏流体运动理论

裂缝性储层中的流体运动通过裂缝网络发生。在这样的储层中,不可渗透的基质块被认为是基质固体材料的结节,而裂缝则充当颗粒间空间。

利用裂缝性油藏与粒间油藏地层之间的类比,假设两个系统中的流体运动过程可以使用相同的方程来描述;例如,如果我们有层流条件,则根据达西定律导出运动方程。其起点是绝缘裂缝中的流动方程,其最简单的模型是两个平行板之间狭窄空间中的流。

在基质岩石具有渗透性的情况下,关于裂缝性储层中流体运动的理论假设基于一种介质插入另一种介质的思想(“双孔隙度”、“双海绵体”),首先工作[1]中提出。假设流动区域的条件实际上是一定量的流体从基质永久过渡到裂缝网络中以及等效流体质量同时向井移动的结果。所建立的流穿过双孔隙系统,与流经无孔裂隙岩石的流相同。

国内外双孔隙度概念的发展是在各种裂缝介质模型的理论求解层面上进行的,具有不同的假设和求解方法。已发表的解决方法纯粹基于作者对他们选择的介质模型中流体流动过程的思考概念,并且没有人证明他的观点是正确的[4]。在这方面,对一些具有裂缝性油藏异常性质的油田的研究结果具有特殊的实践和学术意义。

其中一区在厚度为55-70 m的石灰岩中发现了石油矿床,孔隙度为25-30%,基质渗透率为20-40 mD。根据测井资料处理结果,这些沉积物的含水饱和系数始终等于1袣(袣=1),即孔隙体积完全被地层水充满。这一结论与流入量测试指标的结果一目了然:在钻井过程中用钻柱测试仪进行RIH作业时,该井总是在开始时就产生地层水。但盐酸处理后,多口油井出现井喷、断油、断水。节流器越小,流入的总液体中的含油量就越高(表1)。

出色地 间隔 测试方法 结果 集约化 强化后的结果
1 随钻管道地层测试 水 — 54 m 3 /天  

 

1 柱穿孔 水 — 53 m 3 /天 盐酸处理 水+油,d=5 mm 流量 88 m 3 /天(水 74%,油 26%),d=3 mm 流量 30 m 3 /天(水 54%,油 46%)
2 随钻管道地层测试 水 �139 m 3 /天
2 柱穿孔 水量—125m 3 /天 盐酸处理 水+油,d=8 mm 流量 160 m 3 /天(水 67%,油 33%),d=5 mm 流量 108 m 3 /天(水 48%,油 52%)
1 随钻管道地层测试 水量—177m 3 /天
1 柱穿孔 盐酸处理 水+油,d=10 mm 流量 320 m 3 /天(水 25%,油 75%),d=8 mm 流量 240 m 3 /天(水 19%,油 81%) d=5 mm 流量流量 170 m 3 /天(水 18%,油 82%),d=3 mm 流量 76 m 3 /天(水 14%,油 86%)

表1「钻井过程中和完井后实物测试结果」

所考虑的储层实际上是具有渗透性岩石基质的裂缝性储层,后者充满了水,而石油占据了近垂直裂缝。

结果发现,为刺激流入而建立的过高压力导致剪切应力超过地层压力。换句话说,裂缝流入的第二个不可或缺的先决条件没有得到满足。

在钻井过程中以及在一些射孔操作之后使用钻杆测试仪刺激流入时,流体从基质岩石进入井中。并且由于基质是水饱和的,因此每次都能获得地层水的流入量。盐酸处理使得恢复裂缝和钻孔之间的连接成为可能,这反过来又确保了流体(即石油)渗透到裂缝网络中。在此类事件的开发过程中,没有一口井从一开始就生产含水油,并且水与油的相关性取决于总流量对操作节流器直径的影响。

所描述的结果本身很有趣,但它们对于理解具有渗透基质的裂缝性储层中的流体流动过程以及理解碳氢化合物的聚集具有特别重要的意义。

尽管如此,它还是来了。表 1 的数据表明,即使在裂缝闭合后,流体也会利用空隙过滤到井中。因此,由基质岩石供给裂缝网络的概念没有适当的基础。此外,双孔隙储层中裂缝的渗透率不低于孔隙渗透率一个数量级,流体通过基质孔隙的速度无法支持稳定地流入裂缝。裂缝中的压降快于基质中的压降,这提供了流体从基质流入裂缝的可能性,这纯粹是对此类事件中压力脉动过程的理论假设。

上述说明了以下事实:对于具有可渗透基质的裂缝性储层,每种介质,即基质岩石和裂缝网络,单独地提供分别包含在这些介质中的流体流入井中。当某个矿点持续发育一段时间后,由于基质岩石在经历一定的最终变形后发生破裂,可能会发生一定量的基质岩石裂隙网络的补给(仅是理论上的假设)。

许多研究人员针对他们选择的模型提出了裂缝性油藏结构的第一变体和第二变体的流体流动任务的解决方案。但无论哪种变体,图示流体流向井的模型都表明地层中从排水区域的外边界到井眼的径向流。相应的模型在文献中以其作者和作者的名字而闻名,并且在工作中进行了详细考虑[4]。

值得注意的是,所有裂缝性油藏的分析模型都表明存在水平裂缝,与其真实结构不相符。此外,排除了流体仅沿水平方向的裂缝运动,因为垂直方向的压差明显高于径向流内的压差。

油气聚集

碳氢化合物聚集假说表明,碳氢化合物以分散的形式从其形成地通过岩体迁移并以矿点形式聚集。矿点内部的流动意味着通过水向上漂浮,将水从孔隙中驱出并被碳氢化合物取代。上述具有可渗透基质的裂缝性油藏中的石油产状本身与其形成的初始阶段有关。岩石基质的整个宽度都充满了水,石油也填充了整个宽度上已经张开的裂缝。如果我们考虑到裂缝的渗透率远高于基质岩石的渗透率,那么以下结论不言而喻:正是地下裂缝才是碳氢化合物侵入矿区的运移方式。

液压连接恶化

根据对测试测量结果的分析,确定了裂缝与井眼之间的水力连接发生恶化的建井阶段。为此,选择具有相同岩性成分、岩石地球物理特征和测试条件的目标。对部分井,在钻井过程中使用经过盐酸初步处理和不经过盐酸初步处理的钻杆测试仪进行测试。经盐酸初步处理的目标地层流体流入量不小于数量级(13)。 40 倍)超过未进行盐酸处理的目标的流入量。考虑到钻杆测试是在用钻头穿透目标后立即在裸眼中进行的事实,唯一的结论不言而喻:裂缝和井之间的水力连接从在裂缝性储层中钻探的那一刻起就恶化了,并且它与冲洗液接触。随着钻井使用过程中冲洗液密度的增加,这种连接快速损坏的可能性越来越高。仅通过盐酸处理操作即可确定流体流入量的显着差异。

井底结构

根据上述结果,井底结构的选择非常重要。为此,研究了完井方法如何影响裂缝性油藏目标开发效率和产能。分析了与三种结构相关的数据:裸眼、带筛管的尾管、固井生产套管以及随后的射孔。油藏开发计划中未规定裸眼完井。这种井底结构通常用于钻井过程中由于冲洗液流失而无法下套管的情况,有时会造成灾难性的后果。尽管如此,裸眼目标的完成仍然没有任何问题。

即使为了控制井漏,使用了特殊填料(橡胶碎屑、木屑等),并且在随后的钻孔中对钻孔进行了胶结,也注入了膨润土塞子。此外,在完井过程中,在产生所需的压力下降后,立即获得了石油流入。裸眼井采油具有压降小、产能系数高、生产周期长的特点。后者说明了这样一个事实:所考虑的井柱中岩石的持续应力确保了井眼在其发生条件下的稳定性。

对于使用带筛管的衬管完成的井,观察到以下情况。在那些没有在筛管上方的衬管部分进行固井的情况下,目标开发没有任何问题。这种目标的特征在于具有与上述井底结构所描述的相同的优点。在这些情况下,当对筛网上方的衬管部分进行固井时,目标开发通常需要额外的时间投入和材料。这种情况是由于固井作业中使用的技术装置并不能保证水泥浆不会进入筛管区域。这导致了裂缝的排列和筛管开口的堵塞。任何后续操作都无法清除屏幕和裂缝。结果导致裂缝与油井之间的水力联系恶化:在高压降、低效率的情况下进行采油。

作为一个例子,我们可以带来同一区域的两口井的完井结果。开发的目标由石灰石组成。该井需要三倍盐酸处理才能完成,在筛管上方的衬管部分进行固井作业。尽管目标如此强化,但设定的压降仍等于 35Mpa,生产率为 0.8 吨/天*MP。而另一口井,未进行上述固井作业,用水置换较重的钻井液后即实现冲油。压降不超过2MPa,生产率为130吨/天*MPa。

通常,采用生产套管下入井中的完井、其固井和随后的射孔与采用下入孔准备好的筛管的完井以及在筛管上方进行的衬管固井是相同的。此类井需要额外的时间和材料投入(有时要进行多达 5 次盐酸处理,以可靠地恢复裂缝与井眼之间的水力连接)。盐酸处理可以有效地恢复主要由石灰石组成的横截面中的裂缝和钻孔之间的连接。

因此,在裸眼完井或准备筛管期间无需固井,即可实现裂缝性油藏石油生产的最大生产率。

压力下降

开发目标的压降被确定为对于特定节流直径,测量的地层压力与井底压力之间的差值。研究发现,当裂缝性储层发育时,压降值变化很大,从接近零到几十兆帕。对多口井数据的详细分析可以得出以下结论。大多数靶材的压降值不超过 2-2.5 MPa。压降超过 5 MPa 是未经过强化处理或效率非常低的目标的特征。

随时间推移进行压降动态分析。研究发现,尽管地层压力有时相对于初始压力下降 4 至 35 MPa,但在石油生产初期建立的压降在持续时间内保持不变。随着产品含水率的增加,节流器直径减小,这自动导致较低的压降。

酸处理的影响

While a target is developed its rocks are often treated with hydrochloric acid. In quality terms, the impact of hydrochloric acid on carbonate rocks is as follows: hydraulic connection between fractures and borehole (where such connection significantly deteriorated or completely ceased in the process of drilling and cementing a string); hydrodynamic characteristics of reservoirs improve relative their characteristics prior to hydrochloric acid treatment. In terms of quantity, hydrochloric acid treatment results in increased bottom hole pressure (drawdown decrease) and flow rate. As a consequence, the productivity index, as well as hydroconductivity and permeability, are noted to be increasing.

Examples from the practice of the development of certain targets:

  1. During the development of a target in the interval 5612-5674m no inflow was achieved at first; intake of water was registered under pressure equal to 34 MPa; oil free flow was achieved after hydrochloric acid treatment was carried out.
  2. With the target developed in the interval 3640-3672 m no inflow was registered at first; water intake was registered with pressure of 20MPa. The first hydrochloric acid treatment resulted in water spill out with flow rate of 4m3/day; oil flow with water cut followed the second hydrochloric acid treatment under bottom hole pressure of 袪蟹邪斜 = 25MPa; the third acid treatment resulted in a gush of oil with flow rate of 100 ton/day under 袪蟹邪斜 = 30 MPa.
  3. Target in the interval 2660-2681 m. After hydrochloric acid treatment operation was done, hydroconductivity and permeability increased 3.7 times relative their values prior to the hydraulic acid treatment operation.

From the examples above and other multiple examples it is obvious that hydrochloric acid treatment of fractured carbonate reservoirs is highly efficient.

         To evaluate the impact of lithological composition of rocks on the efficiency of acid treatment jobs a comparative analysis was carried out with regard to terrigenous and carbonate sediments. Deposits of lithologic and stratigraphic rock assemblages were selected where targets had been developed without any fundamental differences in technology of drilling and stimulation.

For all the areas where simultaneous development of deposits with fractured reservoirs had place, which were composed of carbonate and terrigenous rocks, it was found that pressure drops in the wells producing oil from sandy and clay rocks were 4 to 5 times higher than those in the wells producing oil from carbonate rocks. This difference in the pressure drop values is determined by extremely low effect of hydrochloric acid treatment on sandy and clay rocks. Other acid treatment blends were used, with the view to improve the hydraulic connection between well and fractures, the impact of which on the terrigenous deposits had no positive results.

         Hydraulic fracturing treatment has been the most resultative way to restore and improve the hydraulic connection between fractures and well in terrigenous rocks. One should only take into account that hydraulic fracturing of rocks in a fractured reservoir with impermeable matrix is in the end a way to connect fractures of hydrofrac with the network of natural open fractures of a deposit, while in case of a fractured reservoir with permeable matrix the fracture of hydraulic frac serves as a way to increase the area of the surface where screening of formation fluid takes place.

Rock Matrix Deformations and their influence on the development of deposits

Prior to bringing the occurence into development and oil production commencement, initial fracture opening was established in the fractured reservoir which has been determined by excess formation pressure over horizontal stress (袪锌谢>蟽谐芯褉). The difference between 袪锌谢 懈 蟽谐芯褉 shall also decrease from the moment of production commencement which would result in rock matrix deformation i.e. change in their linear size, volume or shape. The character and level of deformations depend on the type and size of applied stresses, as well as on elastic and plastic properties of rock (Fig. 6). Stress increase causes increased deformations and in the end destruction takes place 鈥� rock loses its continuity and splits into parts. Generally, three zones of deformation can be seen due to increased stress (Fig.6) 鈥� elastic (袨袙, 袨袙1), plastic (袙1小,袨小1), and breaking deformations (to the right of 袙,小,小1).

Fig. 6. Typical Diagrams of Deformation in Fragile Elastic (1) , Fragile Plastic (2), Plas-tic (3) rocks where 袙,袙1 are limits of elasticity; 小,小1 are limits of plasticity.

Matrix rock deformation takes place from the moment when formation pressure starts decreasing, that being said, the maximum deformation would be towards the least resistance i.e. inward fractures. This would result in reducing the initial openness of fractures. Elastic deformation of the matrix would last till a flexibility limit is achieved. Depending on the rock properties, either fragile breaking would take place or rock would pass into the area of plastic deformation with its consequent breaking. Both in the first and in the second variant, the rock breaking would be accompanied by formation of new cracks in the rock mass. The maximum underbalance falls on the near well-bore area, therefore rock deformation starts near walls of a well with gradual expansion from the well-bore inward the rock mass. Increasing number of production wells and further formation pressure decline in the process of oil production would stimulate deformations and take ever-growing volume of rocks. The deformation processes taking place during oil development and production in rocks of a deposits having fractured reservoirs impact on wells performance and their survey results.

The openness of fractures decreases at the stages of the elastic and plastic deformations, which results in reduction of their permeability and well productivity. Any following breaking of rocks and formation of new fractures determines productivity growth. Such processes repeat themselves in cycles, and if corresponding well surveys take place in wells on a regular basis, they can be registered and presented in the form of an IPR curve and its temporal changes, reflecting changes in well productivity, changes in bottom hole pressure, in the results of pressure interference test.

Below are the examples of the impact deformation processes provide for the results of wells surveyed in various areas:

  1. The well has a developed target of fractured limestones, its productivity index reduced from 1.7 ton/day*atm to 0.9 ton/day*atm during the period of 16 months from the moment of its bringing into development (Fig.7). After a hydraulic acid treatment, it increased up to 23 ton/day*atm and fluctuated for consequent 8 years in the range of 5.6 鈥� 49.4 ton/day*atm. During this period, formation pressure gradually decreased by 170 atm and nothing was undertaken to increase it. Pressure drop remained steady at the level of 3 to 4 atm for the whole period of observations after hydraulic acid treatment with the choke of 8mm was done. Decreased productivity reflects the areas of elastic and plastic deformation of rocks, while productivity growth is characteristic of matrix destruction and formation of new fractures.
  2. A rare case was registered in a well having a developed target in the thickness composed of fractured sandstones and siltstones. Well productivity index increased 5.3 times with a choke of 7mm in diameter in the process of a 10 day flowing test.

The increased productivity is determined by elastic and plastic deformations reaching their limits directly in the process of well flow tests. This resulted in destruction of the near well-bore zone, in formation of new cracks and, consequently, in increased productivity. For this well, change in productivity index across time, with choke of 5 mm in diameter, was similar to change in productivity index presented in Fig. 7.

Fig. 7. Dynamics of Formation Pressure and Productivity Index for a Well Operating a Fractured Reservoir

  1. Fig. 8 illustrates IPR curves and the dynamics of their change across time, over the target composed of fractured terrigenous rocks and metamorphised shales. The well was drilled and completed in 1967. Small drawdowns with high flow rates and straight-line IPR curve indicate well-purged fractures and steady productivity index with chokes of different diameters. Due to green field status of the field the well was in conservation before 1994. The following full-scale flow tests were carried out in 1999. Stages of elastic-and-plastic deformation and matrix rock breaking repeatedly cycled in the occurrence during the period of 1994-1999. In January 1999, the IRP curve shifted toward the left of the initial position and curves toward the axis of flow rates. Reduction of bottom-hole pressure with greater choke diameters increases rock contraction under growing tangential force and the IPR curve would have been more logical to observe toward the drawdown axis. In this case, the stage of rock breaking takes place in the well feed area, with formation of new fractures, which is intensified by the tangential stress and creation of additional fractures directly in the process of well survey. Flow tests in 2 months showed the IPR curve shift toward the right and upward which indicates the process of new cracks formation (i.e. the process of rock breaking) having effect on well performance, was prevailing in the rock mass since then. As the surveys were carried out, switching over to choke of d=6mm caused the IPR curving toward the axis of drawdowns and decreased productivity, which was determined by the impact of growing tangential stress as the process of elastic rock deformation was taking place. A single measurement with a choke of d=4mm carried out next month showed some growth in productivity and the dominant impact of the new crack formation process. The IPR of late 1999 indicates the reduction of productivity. Following April 1999, the process of rock breaking and formation of new cracks came to its end and a new stage of elastic-and-plastic deformation began, which resulted in reduced fracture opening and their permeability. Straight-line form of the ID reflects temporary equilibrium between reduced fracture opening and their increased concentration in the volume unit of rocks. Formation pressure of the occurrence was gradually decreasing and no measure were undertaken to increase it.

Fig. 8. Dynamics of IPR Curves Changing Across Time. Number of points-Choke Diameter (mm), near the IPR ends.
鈥� date (month/year)

  1. If no regular well flow tests are carried out, it is possible to judge about deformation processes taking place in an occurrence using measurements of bottom-hole pressure values with chokes of permanent diameter. Changed fractures openness and, correspondingly, their permeability are reflected in changed values of bottom-hole pressure.
  2. Example from practice. 7 measurements were made during the period of 03.04.2000-22.12.2000 谐. in a well where fractured sandstones were oil production target which registered the increase of bottom-hole pressure (choke = 8mm) from 10.2 MPa to 16.4 MPa. Bottom-hole pressure (7 measurements were taken) decreased from 16.4MPa to 10.8 MPa during the period of 23.12.2000-14.06.2001 and increased up to 12.4 MPa during the next measurement taken on 13.08.2001. The presented data can be interpreted in the following way: during the period of 03.04.2000-22.12.2000 the processes of matrix rock breaking and greater concentration of fractures are prevailing in the mass of rocks having effect on well performance; the period of 23.12.2000 鈥� 14.06.2001 鈥� processes of elastic-and-plastic deformations are prevailing in the rock volume having effect on well performance, resulting in reduced fractures opening and their permeability; following 14.06.2001 processes of rock breaking start dominating and concentration of fractures grows. Similar results were registered across multiple occurrences with fractured reservoirs.
  3. Processes of rock deformation are reflected in the results of well interference testing in the following way. If an occurrence is composed of fragile rocks, the growing concentration of fractures contributes to formation of new hydrodynamic ties. They can be detected by periodic interference well testing between the same pairs of wells. For example, a series of interference well tests was carried out on an occurrence composed of this type of rocks where one and the same pair of wells served as active well and observation well. . In this pair of wells, with the distance of 1800 m between them, no well interaction was detected; a repeated interference testing in 26 months registered a distinct interaction. The other pair of wells of the same occurrence, the distance between them being 750 m, showed no interaction during primary interference testing; the second interference testing, 7 months later, registered well interaction, which was additionally confirmed by the third interference testing 6 more months later.

If an occurrence is composed of elastic-and-plastic rocks and plastic deformations are not vividly expressed, an interference well testing most often would not show direct interaction between surveyed wells, although the objects under study refer to a single flow net. This is determined by the fact that due to plastic flow of rocks closing of fractures takes place in a shut-in well and pressure impulse does not reach a detecting instrument. The deformation type of rock can be defined by the IPR pattern. The IPRs of fragile rocks coincide in the drawdown and buildup modes (i.e. consequent increment and decrement in choke diameter) while the IPRs of the drawdown and build up modes are quite different from each other when we deal with elastic and plastic rocks.

Deformation processes related to the matrix rocks of a fractured reservoir can be managed by swapping the operating chokes: incrementing choke diameter accelerates the processes of deformation while decrementing reduces them. Water injection with the view to increase or maintain formation pressure is in its way a method to stabilize deformation processes. In other words, managing deformation processes in an occurrence with fractured reservoirs can be a simple and efficient way of management, field development and oil production.

Conclusion

         A fractured reservoir is a subsurface rock divided by subvertical open fractures making up a single flow network. The network itself is very sensitive to external and internal stresses on the rock and can immediately react to those changes by changing in well productivity. The variations of stresses can in certain way be controlled and modified making it possible to manage the process of field development and oil production using simple and available methods.

Sources

  1. G.I.. Barenblatt, Y.P. Zheltov and I.-N. Kochina Basic Concepts in the Theory of Seepage of Homogeneous Liquids in Fissured Rocks. Applied mathematics and mechanics. Academy of Sciences USSR, issue 5, 1960 p.852-864.
  2. K.G.Boltenko, A.I.Echeistov, S.F.Zdorov. Basic results of the study of fractured rocks at Yaregankskoye oil field. Works of the 2nd All-Union Meeting on Fractured reservoirs of oil and gas. Moscow 鈥淣edra鈥漰ublishing house, 1965, p.233-240.
  3. B.I. Vilge, K.G.Waxman, Y.A. Limberger, V.M.Il铆nsky 鈥淚nduction Logging in Subsurface Rocks with Vertical Open Fracturing. Applied geophysics., 1989, Issue 121, p.201-207.
  4. T.D. Golf-Racht 鈥淔undamentals of Oil Field Geology and Fractured Reservoir Engineering鈥�. Moscow, 鈥淣edra鈥漰ublishing house, 1986, p.608.
  5. V.N. Dakhnov 鈥淓lectrical and Magnetic Methods of Well Survey鈥� Moscow 鈥淣edra鈥�, 1967, p.390.
  6. Y.A Limberger, V.M.Il鈥檌nsky. 鈥淣ew Approach to Delineation of Fractured Rocks by the Results of Well Logging鈥�. Geology of oil and gas, 1978, Issue 11, p.58-63.
  7. Y.A.Limberger, B.I.Vilge, V.M.Il鈥檌nsky, K.G.Waxman. 鈥淒elineation of Open Fractures in Well Column Using the Results of Induction Logging鈥�. Geology of Oil and Gas, 1986, Issue 5, p.14-18.
  8. YALimberger、VMIl'nsky、TGRadchenko“关于克拉斯诺达尔边疆区库马地平线裂缝性储层流体流动的潜力”。石油和天然气地质,1986 年,第 8 期,第 17-22 页。
  9. YALimberger,BIVilge。”关于油井中流体流动的潜力。提高野外地球物理调查效率的问题(CGE学术论文集)。莫斯科,VNIIOENG,1989 年,第 19-28 页。
  10. YA Limberger“液压压裂模拟器:潜力和局限性”。罗格泰克。第 60 期,第 54-67 页。
  11. 你是林伯格。“巴热诺夫套件中真的有石油吗?”ROGTEC。第 66 期,第 68-81 页。
  12. IV Tatarinov“压裂对亚列格斯科耶油田流体流动和储层容量的作用。”第二次全联盟石油和天然气压裂储层会议的作品。莫斯科,“edra”出版社,1965 年,第 167-171 页。
  13. YALimberger,VM Il'nskiy。“基于钻孔地球物理研究结果的连体岩石识别新方法。”国际地质学评论,1980年,第22卷,“7”。第 831-835 页。
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Fractured Reservoirs: Specifics of Exploration and Development

Author: Yuri Limberger – Mud Logging Expert

Fractured reservoirs occur in a wide range of stratigraphy of subsurface, at various depths, and in a large range of pressures and temperatures. While the spread of granular type reservoirs (intergranular reservoirs, porous reservoirs) is associated with terrigenous and carbonate rocks only, i.e. with the rocks of specific but limited lithology, the fractured-type reservoirs were detected and have been developed not only the above mentioned rocks but in the rocks so unusual for reservoirs as shales, granites, claystones, etc.

Record-breaking cumulative oil production can be characteristic of such type reservoirs, exceeding the level of one million ton per well sometimes.

The article presented here for reader’s review is a result of author’s multiyear study in attempt to resolve some practical and theoretical issues of identifying and exploring fractured reservoirs in the process of prospecting and exploration of fields and recovering hydrocarbons from them.

These studies include:

  • Statement, setting and solution of individual tasks related to the theory of geophysical techniques of subsurface exploration of well columns;
  • Computation of geologic and geophysical situation based on obtained theoretic solutions;
  • Development of new research methods of studying fractured reservoirs;
  • Processing and Interpretation of the results related to using these techniques inside wells;
  • Processing, interpretation and generalisation of the data obtained after well testing and development of the fields with oil accumulated in fractured reservoirs;
  • Processing and interpretation of the results of special experimental researches;
  • Critical re-evaluation of publications issued by other research workers.

Overall, materials of more than 1200 wells over 180 areas and oil fields have been studied with regard to the subject matter under consideration.

The history of exploration and development of certain occurrences was tracked starting from drilling of the first prospecting well and ending with their complete water cut. The fields were located in various geographic, geologic and climatic conditions. The age of the fissured reservoirs ranges from Oligocene through Riphean. The rocks of the reservoirs are composed of sandstones, siltstones, limestones, dolomites, claystones, granites, tuffites, etc. Formation pressure was changing from the abnormally low to extremely high, the temperature range from 25 °С to 185°С. That is, fractured reservoirs have been studied in the whole range of their geologic and technical conditions that are encountered in modern practice.

Fractured Reservoir Structure

Up till now, the greater part of geologists, geoscientists, field developers, both in our country and abroad, have had a concept of a model of a fractured reservoir as a kind of volume of rock, dissected by fractures of different direction, angle of gradient and crack opening (Fig.1).Such a concept has been the result of some visual observations of geologic outcrops and core, delivered to the surface, which does not take any account of the stressed state of the rocks occurring in real conditions. Therefore, first of all, it is necessary to explain the structure of a reservoir, as not having a clear understanding of a research subject, it is impossible to develop methods of its study and analyze those changes taking place in the course of hydrocarbon production.

Fig. 1. Widespread Concept of Fractured Reservoir Structure

Judging by a simplest consideration of stresses affecting an element of rock, a working hypothesis was formulated first: for natural conditions of occurrence the probability of vertical fissures is higher than the probability of open horizontal cracks. The hypothesis was tested using three independent approaches: 1) By comparing the results of well completions with the volumes of flush fluid lost in the process of drilling. 2) by comparing the formation of fluid influx with tangential stress present at the walls of a borehole; 3) by studying the  depiction of rock outcropping in an oil mine at Yaregskoye field.

Based on the first approach, it was believed that the flush fluid absorbed during drilling would go down along the system of vertical fractures into the water cut part of the occurrence and would not interfere with the recovery of clean oil. And if horizontal fractures are present there, the absorbed fluid would be inevitably recovered together with the reservoir fluid. Analysis of the data was carried out that had been obtained after the completion of 150 wells drilled for fractured reservoirs the drilling of which showed the facts of absorbed flush fluid in the volumes ranging from several hundred cubic meters up to hundreds of thousands of cubic meters (a number of wells were drilled with pumped flush fluid not showing up on the surface at all). The result of the completion of all of those wells was oil not containing any signs of absorbed flush fluid.

Therefore, the first approach has confirmed the hypothesis about dominating role of vertical open fractures in fluid flow in situ.

The second approach took into account the impact of tangential stress σθ arising and active on the walls of a borehole and near it. Under certain conditions which can be created in the process of well stimulation, the tangential stress may exceed the formation pressure Рпл..which would result in closing the walls of vertical fractures, the loss of hydraulic connection between the well and the reservoir, and the lack of fluid influx as an outcome of such test. The closure of horizontal fractures under the influence of tangential stress is impossible; the hydraulic connection between reservoir and borehole would be still there and the fluid would be recovered. Selection of data was carried out after testing more than 100 targets represented by fractured reservoirs, during the stimulation treatment of which the condition σθ>Рпл. was preserved. All of the targets first happened to be “dry”. All of them produced formation fluid after stimulation was done.

The results, obtained using the second, as well as the first, approach, confirmed the hypothesis of a dominating role of open vertical fractures in fluid flow in situ.

Using the third approach, detailed depictions of the Devonian sandstone were studied, which occurs in the depths of 180-250 m, whose oil is produced using shaft method at the Yareganskoye field. Only subvertical open fractures were mentioned in research works of various authors [2; 12].

We should note that these data rebut the already widespread point of view about the possibility for open horizontal fractures to exist at relatively shallow depths.

Therefore, it was proved that only vertical fractures can be open in natural rock conditions (Fig. 2) These fractures form a single network in an occurrence, providing for hydraulic connection between different parts of the occurrence horizontally and vertically. The proven structure of fractured reservoir has the following factors as its basis: unevenness of fracture distribution inside rock massive, inequivalence of fractures of different degree of openness in the process of hydrocarbon production and dominating role of open fractures of subvertical direction.

Fig. 2. Real Structure of Fractured Reservoir

Objectives to be achieved at the stage of prospecting and exploration

Embarking on the prospecting and exploration jobs at a new field, one should always keep in mind the probability of drilling-in and drilling over a fractured reservoir. In such case, one shall have to solve a number of tasks which are specific for such kind of reservoir and which are normally not included into the program of studying a cross-section using geophysical and hydrodynamic research techniques. Listed below are some central tasks requiring their solution while studying fractured reservoirs, and the ways of solving them are presented next:

  • Identifying open fractures in a well column;
  • Assessing the type of reservoir;
  • Estimating the extension of open fractures vertically;
  • Delineating points of intersection between fractures and well;
  • Providing for drawdown pressure to stimulate fluid influx from fractures;
  • Estimating fracture capacity.

Methods of identifying open fractures in well columns

A number of methods can be used to fundamentally solve the issue of the presence (or absence) of open fractures in a column of a specific well:

  1. Recording of fluid loss and gas, water and oil shows in the process of drilling. Fluid loss and/or gas, water and oil shows, recorded in the process of drilling are usually caused by the presence of open fractures intersected with a well. Recording of such complications in the course of normal drilling progress points at presence of fractures in a well column, and it makes it possible to estimate formation pressure and identify the zone of jointing.
  2. Finding flow potential. A theoretic solution of a problem of electromotive force of flow potential (or potential of self-potential (SP)) in a fracture showed that [9] such electromotive force is 4π times higher than the electromotive force of the potential of capillary percolation (Helmholtz equation)and may bring about extremely high self-potential. By comparing the actual SP anomaly amplitude with nominal static potential one can detect the presence of flow potential which is due to open fracture density [8]. This method is optimal for the use at well columns predominantly composed of terrigenous rocks.
  3. Comparing propagation velocities of different length waves. If rock matrix structure is homogenous, propagation velocities of short length waves and long length ones are equal between themselves. If rock matrix structure is significantly disturbed with open fractures, the propagation velocity of short length waves would exceed the one of long length waves. Values obtained in the acoustic and seismic range of frequencies (acoustic logging and profile shooting data) were used as velocities of waves of different length. This method is advisable for the use in the depths of rocks with unvarying lithology and considerable depth.
  4. Comparing horizontal stress with formation pressure. Condition for existence of open vertical fractures shall be formation pressure exceeding horizontal stress σгорплгор). Otherwise open fractures must be missing [6, 13]. Formation pressure is measured using pressure gauge in the process of inflow tests.

Horizontal stress can be determined using two methods: – computation and using the results of hydraulic fracturing of formation. In the first case:

σгор = δср • g • h • ν/(1-ν)                       (1),

where δср – is average density of subsurface rock from surface to depth h;

ν – is Poisson’s constant; g – is gravity acceleration.

Poisson’s constant is computed based on the measurement of velocities with which longitudinal and transversal waves are propagated according to the known formula, and nowadays it is a routine procedure.

Determination of horizontal stress based on the results of hydraulic fracturing of formation gives us a more accurate value, provided stress concentration factor is taken into account during the recording of the fracturing process.

Otherwise, the minimal horizontal stress would be significantly overestimated. Determination of the minimal σгор value based on the materials of hydraulic fracturing of formation is in details considered in the work [10].

We should note that the method of comparing horizontal stress, determined on the basis of materials of hydraulic fracturing of formation, and formation pressure measured using a subsurface pressure gauge, provides an absolute guarantee for determining presence or absence of open vertical fractures in a well column under consideration.

Determining reservoir type

Determining reservoir type actually confines to evaluation of fluid loss properties of rock matrix. Why is it necessary and important? If rock matrix is permeable, then we have a fractured reservoir with permeable matrix, but in case rock matrix is impermeable, we deal with a purely fractured reservoir.

In the first variant, one can ignore the capacity of the fracture system while estimating reserves since it is incomparably low against the capacity of matrix pore volume and it is within an absolute error if we determine porosity using geophysical methods. In the second variant, it is the capacity of the fracture network that determines the volume of commercial deposit of an occurrence.

Qualitative indicators of rock permeability which are normally used to judge about presence of an intergranular reservoir, are acceptable in this case too. If such permeability indicators are established we deal with a fractured reservoir with permeable matrix. But if we have no clear indication that the rock matrix is permeable, we have a purely fractured reservoir. Clear signs of the rock matrix permeability may be missing when we have certain properties of drilling flush fluid. For such cases, two conceptually new methods of task solving have been rationalized and tested.

The first one is based on detecting tension cracks in the near-wellbore zone, which wildly formed in the process of drilling, and which are extended in radial directions. Such fractures emerge under conditions when flush fluid pressure down the hole is exceeding the combined tangential stress and the rock’s tensile (fracturing) stress. Calculations based on the known theoretic solution of the task about prestressed rock near a well bore, indicate that the radius of wild fracturing zone ( R ) would not exceed 1.2-1.5 of a well radius (Rс),i.e. R/Rс≤ 1,5. If such fractured area is detected, it is an indication that rock matrix is impermeable. Beyond such area the tangential stress works for contraction.

Zones of spontaneously formed cracks are typical of well columns drilled using flush fluid of increased density. There is a record of a continuous extension of such fracturing exceeding 1 km in well columns composed of rocks with different lithology and drilled using flush fluid with density of not less than 1.6 g/cm3.

The second method is based on the mentioned theoretic solution of the task about determining stresses near a vertical well and it is implemented by taking into account the tangential stresses within the areal limits of a well by changing the bottom-hole pressure.

Determination of vertical fractures extension

It is necessary to know the extension of vertical fractures through the section vertically to determine the lower boundary of a fractured reservoir vertically and to estimate hydrocarbon reserves. This can be defined using the above mentioned method of fracture identification by comparing horizontal stress with formation pressure. As long as condition Рплгор is fulfilled, open vertical fractures may exist down to certain depth. When applying this approach it is necessary to estimate the change of horizontal pressure and formation pressure along the depth of a well column under consideration.

The length of fractures in formations of limited thickness is usually confined within formation thickness. This rule is violated in zones of abnormally high formation pressure, where continuous length of open vertical fractures (regardless of their discrete layers) may exceed 1.5 km.

Identifying the fracture-well intersections

This task being resolved is a reliable basis for selecting the right interval for producing formation fluid out of cracks. Points of intersection between a well and open fractures are in fact the spots of the reservoir-borehole hydraulic channel reaching the walls of a well. Hence, we may conclude that the methods of registering the fluid movement over such channels should have vivid priority over other methods. The simplest way is registering fluid losses and/or gas-oil-water shows in the process of drilling: the depth, at which the event is registered, must be as a first approximation, the place where fractures reach the walls of a borehole. Other possible variants are anomaly of high electric conductivity and present streaming potential. To accurately solve this task it is advisable to use new methods, the specific use of which depends on the properties of a flush fluid pumped in a borehole.

If the well is filled with flush fluid capable of electric conductivity, considerable surges in strength of current, coming from the central electrode of the lateral logging device, would be an indicator of open fractures present there.

The strength of current is registered as a separate curve (Fig.3). Theoretical justification of the method is presented in the work [5].

Fig. 3. Delineation of Fractured Zone Using Current Strength Anomaly in Lateral Log-3 (LL3) 

If the well is filled with flush fluid incapable of electric conductivity, the induction logging is applied then. The use of the induction logging is in such cases based on the results of solving the direct problem of the induction logging theory for a 3D model of environment with a well and vertical fractures present [3,7]. An indicator of fractures present there would be the anomaly of specific form of the electric conductivity curve (Fig.4).

Fig. 4. Delineation of Fractured Zone Using Electrical Conductivity Anomaly of Induction Log

Based on the results of the application of these methods, an examination of the frequency of detection of open fractures in a well column was carried out. The data obtained showed that the distance between two consecutive fractures (fracture zones) ranges between 3 to 84 meters along the well bore.

Additional research was carried out using geophysical survey methods in operating wells producing oil from an open hole through perforated column.

The results of such research showed that oil was coming into an open hole of 150-200 m in length from 1 to 3 cracks distant from each other in not less than 35 m. Distance between active fractures in perforated columns was smaller but at least one of them produced not less than 70% to 90% of oil making up the total production. Taking into account that permeability of a fracture is theoretically proportional to the cube of its openness, the obtained data imply that a wide open fracture provides for a dominant share of oil in the total production rate.

Rationale for drawdown to stimulate inflow

Presently we have no geophysical methods of defining the type of fluid filling in a fracture. Well column testing for inflow has been prevailing as a way to solve this task. Rationale for drawdown serves as a guarantee for obtaining fluid from fractures. Due to the fact that fracture compressibility factor is not less than an order greater than rock pore compressibility, the fracture openness considerably changes along with changing stress on the rock and this predetermines fracture flow capacity. While the condition that formation pressure is greater than bottom hole pressure (Рплзаб) is necessary and sufficient for stimulation of oil from the pores of intergranular reservoir, the fulfillment of such condition for fractures is quite necessary. While the fulfillment of the second condition i.e – Рплθ will be just sufficient.

Higher fracture compressibility predetermines strong correlation between drawdown and well productivity (Fig. 5). As we can see from the picture, fractures yield only within a definite range of drawdowns, created to stimulate inflow. Exceeding some critical value of drawdown leads to a situation when formation fluid is prevented from coming into a well. To prevent this one should abide by a simple rule formulated on the basis of the results of testing various targets: drawdown for stimulation of inflow from fractures must be as low as practicable under specific subsurface conditions and the testing equipment used for that.

Fig. 5. Master Curve “Drawdown – Productivity“for Fractured Reservoirs, Opt – Optimal Drawdown.

Multiple cases have been known from practice when vivid signs of present fractures were registered in a well column in the course of drilling while no fluid inflow was actually received during the testing of corresponding formation segments. Statistical data from various areas of oil production showed that when the fractured reservoirs were tested using drill stem tester in the process of drilling, not less than 70% of run-in-hole operations resulted in no fluid inflow and the tested targets were indicated as “dry”. Afterwards, when the wells were completed, all of such targets yielded an inflow of formation fluid. Its absence during the primary testing was caused by wrong choice of drawdown, in the effort to achieve its maximum size.

Reserves Estimation Volumetric Method

The major task, the solution of which most of all predetermines hydrocarbon reserves, is the estimation of fracture network capacity (fracture porosity factor Кптр). The first method suggested for determining this factor included finding the difference between total porosity of rock and the matrix porosity. It was believed that neutron logging and density logging define total porosity while the acoustic logging or electric logging can do this for matrix porosity. However, the results of the latter are influenced by fracturing and such approach cannot be a criterion for estimating Кптр.Besides, the absolute error of estimating porosity using geophysical methods exceeds the crack formation factor due to which the geophysical methods are in principle inappropriate for resolving this task.

It was suggested to apply the bracketing technique to estimate the Кптр value. The implementation of this method requires two measurements of apparent resistivity to be done at different times, having two different values of flush fluid resistance. Then, using the formula derived under certain assumptions, we calculate the crack formation factor. The physio-mathematical modeling of the method and comparing the obtained results with the Кптр models has shown the principal unacceptability of the bracketing technique for estimating the crack formation factor.

Some works contain the description of estimating Кптр based on the definition of rock skeleton compressibility, the matrix and fractures. It was recommended to evaluate the compressibility factors using the materials of core analysis, geophysical and hydrodynamic surveys of a cross-section, i.e. by studying rock volumes that are hardly comparable between each other.

One should not also apply the data of estimated crack formation factor in the core and thin sections. This is due to the fact that the fracturing we observe there is a result of rock deformation during its drilling and lifting to the surface.

Thus, any founded methods of estimating the crack formation factor are missing for today. A possible way out of this could be as follows. Using the occurrences with fractured reservoirs that were removed from development, it is possible to carry out a retrace calculation using the Кптр, volumetric method formula, accepting the total cumulative volume of produced hydrocarbons. The results of such calculations have shown that the real capacity of fracture network is considerably lower than the values of Кптр, that are encountered in individual publications.

The above described methods of delineating and surveying fractured reservoirs are advisable for the use during not only prospecting and exploration stages but during the analysis and reinterpretation of materials of previously drilled wells. These methods are characterized with simplicity of their implementation and their accessibility for each company. Tested at different areas and fields, they proved efficiency in resolving set tasks and confirmed the certainty of the fractured reservoirs structure. The results of using the described methods for one of the areas serve as an illustrative example which made it possible, using the results of the analysis of cumulative multi-year materials, to in principle highlight the prospects of oil bearing capacity of a vast area in a new way. [11].

About the theory of fluid movement in fractured reservoirs

Fluid movement in a fractured reservoir takes place via fracture network. Impermeable blocks of matrix are considered in such a reservoir as noddles of matrix solid material, while fractures serve as intergranular space.

Using the analogy drawn between such fractured reservoir and formation with intergranular reservoir, it is assumed that the process of fluid movement in both systems can be described using the same equations; for instance, if we have conditions of laminar flow, the motion equation is derived on the basis of the Darcy law. The starting point of this would be the equation of flow in an insulated crack, the simplest model of which would be a stream in narrow space between two parallel plates.

In case when the matrix rocks are permeable, the theoretic assumptions about the movement of fluids in such fractured reservoir are based on the idea of one medium inserted into another one (“double porosity”, “double cavernosity”), first formulated in the work [1]. It is assumed that the conditions of the flow area are actually a result of permanent transition of certain amount of fluid from the matrix into the fracture network and simultaneous movement of equivalent fluid mass towards the well. The established stream, moving across the double porosity system, is identical to the stream via nonporous fissured rock.

The development of the double porosity concept took place in our country and abroad at a level of theoretic solutions for various models of fractured medium, with different assumptions and solution methods. The published methods of solution have been purely based on the authors’ contemplative notions about the process of fluid flow in a model of medium selected by them and no one of them has presented a proof that his point of view was true [4]. In this regard, the results of the studies of a number of fields whose properties were unusual for fractured reservoirs are of special practical and academic interest.

Oil deposits in limestones of 55-70 m in thickness were discovered in one of the areas, having porosity of 25-30% and matrix permeability of 20-40 mD. According to the results of processing well logging materials, the water saturation factor of these deposits is always equal to 1 Квв=1).That is, the pore volume is completely filled with formation water. This conclusion is at first sight confirmed with the results of testing targets for inflow: when RIH operations with drill-stem tester were performed in the process of drilling a well, the well would always produce formation water right at the start. However, after hydrochloric acid treatment was carried out, many wells started blowing out with oil and water cut. And the smaller a choke was, the higher oil content was present in the total liquid influx (Table 1).

WellIntervalTest MethodResultsIntensificationResults after intensification
А1Formation testing on pipes while drillingWater – 54 m3 / dayNo 

 

А1Column perforationWater – 53 m3 / dayHydrochloric acid treatmentWater + oil, d=5 mm flow rate 88 m3/day (water 74%, oil 26%), d=3 mm flow rate 30 m3/day (water 54%, oil 46%)
А2Formation testing on pipes while drillingWater –139 m3/dayNo
А2Column perforationWater –125m3/dayHydrochloric acid treatmentWater + oil, d=8 mm flow rate 160 m3/day (water 67%, oil 33%), d=5 mm flow rate 108 m3/day (water 48%, oil 52%)
B1Formation testing on pipes while drillingWater –177m3/dayNo
B1Column perforationWaterHydrochloric acid treatmentWater + oil, d=10 mm flow rate 320 m3/day (water 25%, oil 75%), d=8 mm flow rate 240 m3/day (water 19%, oil 81%) d=5 mm flow rate 170 m3/day (water 18%, oil 82%), d=3 mm flow rate 76 m3/day (water 14%, oil 86%)

Table 1 — Results of object testing during well drilling and after well completion

The reservoirs of the occurences under consideration are actually fractured reservoirs with permeable rock matrix, the latter being filled with water, while oil occupies subvertical fractures.

It was found that excessive pressure established to stimulate inflow was causing shearing stress exceeding formation pressure. In other words, the second indispensable prerequisite of inflow from fractures was not met.

When inflow was stimulated using a drill stem tester in the course of drilling procedures, as well as after some perforation operations, fluid was coming into a well from the matrix rocks. And since matrix was water-saturated the inflow of formation water was obtained each time. Hydrochloric acid treatment made it possible to restore the connection between fractures and the borehole which, in its turn, ensured penetration of the fluid i.e. oil into fractured network. During development of such occurrences none of the wells was producing water cut oil from the very start, and the correlation of water to oil depended in the total flow rate on the operating choke diameter.

The depicted results are interesting by themselves, but they are of special importance for understanding the processes of fluid flow in a fractured reservoir with permeable matrix, as well as for understanding of hydrocarbon accumulation.

Nevertheless it is coming. The data of Table 1 suggest that even after fractures are closed, the filtration of fluid towards a well takes place using voids. Therefore, the concept of the fracture network being fed by the matrix rocks has no proper foundation. Besides, permeability of fractures in reservoirs with double porosity is not less than by an order higher than the permeability of pores and the velocity of fluid moving through the pores of matrix would not support a steady flow into fractures. The suggestion that pressure drop in fractures is faster than the pressure drop in the matrix, which provides the possibility of fluid flow from the matrix into fractures, is a purely theoretic assumption of the process of pressure fluctuation in this kind of occurrences.

The above said is illustrative of the fact that regarding fractured reservoirs with permeable matrix, each medium, i.e. matrix rocks and fracture network, individually provide for the influx into the well of the fluids separately contained in those mediums. When an occurrence is developed for a durative time, the recharge of fractured network due to the matrix rocks is possibly taking place (merely theoretic assumption) in some amount due to breaking of matrix rocks after it undergoes some ultimate deformation.

Many researchers suggest the solution of the task of fluid flow, both for the first and the second variant of the structure of fractured reservoir for a model selected by them. But regardless of a variant, the model schematizing fluid flow towards a well suggests radial flow in a formation from the outer boundary of drainage area to a well borehole. Corresponding models are known in the literature by the names of their and authors and are in detail considered in the work [4].

We should note that all of the analyzed models of fractured reservoir suggest the existence of horizontal fractures which does not correspond to its real structure. Besides, fluid movement along fractures in merely horizontal direction is ruled out, since the differential pressure vertically is significantly higher than the differential pressure within the radial flow.

Hydrocarbon accumulation

The hypothesis of hydrocarbon accumulation suggests that hydrocarbons, in dispersed form migrate from the places of their formation through rock masses and accumulate in the form of occurrences. Flow inside occurrences means floating up through water, driving water from pores and its displacement by hydrocarbons. The above described oil occurrences in fractured reservoirs with permeable matrix are as such related to the initial stage of their formation. The rock matrix is filled with water across the whole of its width, and oil fills in the already open fractures across the width as well. If we take into account that permeability of fractures is considerably higher than permeability of the matrix rocks the following conclusion suggests itself: it is just subvertical fractures that are the ways of migration for hydrocarbons providing their invasion into an occurrence.

Hydraulic connection deterioration

Based on the analysis of the results of test surveys it was determined at which stage of well construction the deterioration of the hydraulic connection between fractures and borehole takes place. For this purpose, the targets were selected that had identical lithological composition, geophysical characteristics of rocks and test conditions. For some wells, testing was done in the process of drilling using drill stem tester both with preliminary hydrochloric acid treatment and without it.The volumes of the formation fluid inflow from the targets with preliminary hydrochloric acid treatment were not less than in an order (13 to 40 times) exceeding the inflow volumes from the targets not exposed to hydrochloric treatment. Taking into account the fact that drill stem testing was carried out in the open hole immediately after penetrating targets with a drill bit the only conclusion suggests itself: the hydraulic connection between fractures and a well deteriorates right from the moment of drilling in a fractured reservoir and its contact with flush fluid. The probability of rapid deterioration of this connection is higher and higher as the density of flush fluid grows in the process of its use while drilling. Significant difference in the volumes of fluid inflow is determined with hydrochloric acid treatment operation only..

Well Bottom Structure

Based on the above presented results, the selection of well bottom structure is of high importance. Due to this, the issue was studied how well completion method may make an impact on the efficiency of target development in fractured reservoirs and on productivity. The data related to three structures were analyzed: open hole, liner with screen, production casing with cementing and consequent perforation. Open hole completion of wells was not given provision in reservoir development plans. This well bottom structure was usually used when it was impossible to run casing in-hole due to loss of flush fluid in the process of drilling, sometimes having catastrophic consequences. Nevertheless, the completion of targets with open hole was carried out without any problems.

Even there where for the purposes of lost circulation control special filler (rubber crumb, wood scrap etc) was used and borehole was cemented with consequent drilling, bentonite stoppers were injected. Further on, oil inflow was obtained in the course of well completion right away after creating a required pressure drawdown. Oil production from open hole wells is characterized with low pressure drops, high productivity factors, long production periods. The latter speaks for the fact that sustained stress of the rocks in the well columns under consideration ensures the stability of borehole in the conditions of its occurrences.

For wells completed using liner with screen the following was observed. In those cases when cementing was not carried out on the section of the liner above the screen, target development did not have any problems. Such targets are characterized with the same advantages that have been described for the above mentioned structure of well bottom. In those cases when cementing was done on the part of the liner above screen target development often required additional time investment and materials. The situation is determined by the fact that technical devices used during cementing operation did not guarantee that cement slurries would not get into the zone of a screen. This resulted in colmatation of fractures and clogging of screen pipe openings. Any following manipulations were useless in attempts to purge the screen and fractures. As a result, the hydraulic connection between fractures and well deteriorated: oil production was carried out with high pressure drop and low efficiency.

As an example, we can bring the results of completing two wells of one and the same area. The developed target was composed of limestones. Threefold hydrochloric acid treatment was required to complete the well where cementing operation was carried out on the section of liner above the screen. In spite of such intensification of the target, the established pressure drop was equal to 35Mpa, productivity was 0.8 ton/day*MP. As for the other well, without cementing operation above, flush flow of oil was achieved right after the replacement of weighty drilling fluid with water. Pressure drop did not exceed 2 MPa, productivity was 130 ton/day*MPa.

Completion of wells with production casing run in hole, its cementing and the following perforation was identical, as a rule, to completion of wells with run-in-hole ready screen and cementing  of the liner done above the screen. Such wells required additional investment of time and materials (up to 5 hydrochloric acid treatments were carried out sometimes for reliable restoration of hydraulic connection between fractures and borehole). Hydrochloric acid treatments have been efficient to restore the connection between fractures and borehole in cross-sections predominantly composed of lime stones.

Hence, the maximum productivity of oil production from fractured reservoirs can be achieved during their open hole completion or ready screen without cementing.

Pressure drops

Pressure drops of developed targets were determined as difference between measured formation pressure and bottom hole pressure for certain choke diameter. It was found that pressure drops vary in a wide range of values when occurrences with fractured reservoirs are developed – from values close to zero up to several dozens of MPa’s . Detailed analysis of data from multiple wells made it possible to make the following conclusion. The bulk of the targets have been developed with drawdown values not exceeding 2-2.5 MPa. Drawdowns over 5 MPa were characteristic of the targets that had not been exposed to intensifying treatment or when it was very low in efficiency.

Dynamics of pressure drops was carried out across time. It was found that drawdowns established at the initial period of oil production for durative time remained the same although the formation pressure was decreasing in occurrences by 4 to 35 MPa relative their initial pressure. As product water cut was increasing, the choke diameter was reduced, which automatically resulted in lower drawdown.

Impact of acid treatments

While a target is developed its rocks are often treated with hydrochloric acid. In quality terms, the impact of hydrochloric acid on carbonate rocks is as follows: hydraulic connection between fractures and borehole (where such connection significantly deteriorated or completely ceased in the process of drilling and cementing a string); hydrodynamic characteristics of reservoirs improve relative their characteristics prior to hydrochloric acid treatment. In terms of quantity, hydrochloric acid treatment results in increased bottom hole pressure (drawdown decrease) and flow rate. As a consequence, the productivity index, as well as hydroconductivity and permeability, are noted to be increasing.

Examples from the practice of the development of certain targets:

  1. During the development of a target in the interval 5612-5674m no inflow was achieved at first; intake of water was registered under pressure equal to 34 MPa; oil free flow was achieved after hydrochloric acid treatment was carried out.
  2. With the target developed in the interval 3640-3672 m no inflow was registered at first; water intake was registered with pressure of 20MPa. The first hydrochloric acid treatment resulted in water spill out with flow rate of 4m3/day; oil flow with water cut followed the second hydrochloric acid treatment under bottom hole pressure of Рзаб = 25MPa; the third acid treatment resulted in a gush of oil with flow rate of 100 ton/day under Рзаб = 30 MPa.
  3. Target in the interval 2660-2681 m. After hydrochloric acid treatment operation was done, hydroconductivity and permeability increased 3.7 times relative their values prior to the hydraulic acid treatment operation.

From the examples above and other multiple examples it is obvious that hydrochloric acid treatment of fractured carbonate reservoirs is highly efficient.

         To evaluate the impact of lithological composition of rocks on the efficiency of acid treatment jobs a comparative analysis was carried out with regard to terrigenous and carbonate sediments. Deposits of lithologic and stratigraphic rock assemblages were selected where targets had been developed without any fundamental differences in technology of drilling and stimulation.

For all the areas where simultaneous development of deposits with fractured reservoirs had place, which were composed of carbonate and terrigenous rocks, it was found that pressure drops in the wells producing oil from sandy and clay rocks were 4 to 5 times higher than those in the wells producing oil from carbonate rocks. This difference in the pressure drop values is determined by extremely low effect of hydrochloric acid treatment on sandy and clay rocks. Other acid treatment blends were used, with the view to improve the hydraulic connection between well and fractures, the impact of which on the terrigenous deposits had no positive results.

         Hydraulic fracturing treatment has been the most resultative way to restore and improve the hydraulic connection between fractures and well in terrigenous rocks. One should only take into account that hydraulic fracturing of rocks in a fractured reservoir with impermeable matrix is in the end a way to connect fractures of hydrofrac with the network of natural open fractures of a deposit, while in case of a fractured reservoir with permeable matrix the fracture of hydraulic frac serves as a way to increase the area of the surface where screening of formation fluid takes place.

Rock Matrix Deformations and their influence on the development of deposits

Prior to bringing the occurence into development and oil production commencement, initial fracture opening was established in the fractured reservoir which has been determined by excess formation pressure over horizontal stress (Рплгор). The difference between Рпл и σгор shall also decrease from the moment of production commencement which would result in rock matrix deformation i.e. change in their linear size, volume or shape. The character and level of deformations depend on the type and size of applied stresses, as well as on elastic and plastic properties of rock (Fig. 6). Stress increase causes increased deformations and in the end destruction takes place – rock loses its continuity and splits into parts. Generally, three zones of deformation can be seen due to increased stress (Fig.6) – elastic (ОВ, ОВ1), plastic (В1С,ОС1), and breaking deformations (to the right of В,С,С1).

Fig. 6. Typical Diagrams of Deformation in Fragile Elastic (1) , Fragile Plastic (2), Plas-tic (3) rocks where В,В1 are limits of elasticity; С,С1 are limits of plasticity.

Matrix rock deformation takes place from the moment when formation pressure starts decreasing, that being said, the maximum deformation would be towards the least resistance i.e. inward fractures. This would result in reducing the initial openness of fractures. Elastic deformation of the matrix would last till a flexibility limit is achieved. Depending on the rock properties, either fragile breaking would take place or rock would pass into the area of plastic deformation with its consequent breaking. Both in the first and in the second variant, the rock breaking would be accompanied by formation of new cracks in the rock mass. The maximum underbalance falls on the near well-bore area, therefore rock deformation starts near walls of a well with gradual expansion from the well-bore inward the rock mass. Increasing number of production wells and further formation pressure decline in the process of oil production would stimulate deformations and take ever-growing volume of rocks. The deformation processes taking place during oil development and production in rocks of a deposits having fractured reservoirs impact on wells performance and their survey results.

The openness of fractures decreases at the stages of the elastic and plastic deformations, which results in reduction of their permeability and well productivity. Any following breaking of rocks and formation of new fractures determines productivity growth. Such processes repeat themselves in cycles, and if corresponding well surveys take place in wells on a regular basis, they can be registered and presented in the form of an IPR curve and its temporal changes, reflecting changes in well productivity, changes in bottom hole pressure, in the results of pressure interference test.

Below are the examples of the impact deformation processes provide for the results of wells surveyed in various areas:

  1. The well has a developed target of fractured limestones, its productivity index reduced from 1.7 ton/day*atm to 0.9 ton/day*atm during the period of 16 months from the moment of its bringing into development (Fig.7). After a hydraulic acid treatment, it increased up to 23 ton/day*atm and fluctuated for consequent 8 years in the range of 5.6 – 49.4 ton/day*atm. During this period, formation pressure gradually decreased by 170 atm and nothing was undertaken to increase it. Pressure drop remained steady at the level of 3 to 4 atm for the whole period of observations after hydraulic acid treatment with the choke of 8mm was done. Decreased productivity reflects the areas of elastic and plastic deformation of rocks, while productivity growth is characteristic of matrix destruction and formation of new fractures.
  2. A rare case was registered in a well having a developed target in the thickness composed of fractured sandstones and siltstones. Well productivity index increased 5.3 times with a choke of 7mm in diameter in the process of a 10 day flowing test.

The increased productivity is determined by elastic and plastic deformations reaching their limits directly in the process of well flow tests. This resulted in destruction of the near well-bore zone, in formation of new cracks and, consequently, in increased productivity. For this well, change in productivity index across time, with choke of 5 mm in diameter, was similar to change in productivity index presented in Fig. 7.

Fig. 7. Dynamics of Formation Pressure and Productivity Index for a Well Operating a Fractured Reservoir

  1. Fig. 8 illustrates IPR curves and the dynamics of their change across time, over the target composed of fractured terrigenous rocks and metamorphised shales. The well was drilled and completed in 1967. Small drawdowns with high flow rates and straight-line IPR curve indicate well-purged fractures and steady productivity index with chokes of different diameters. Due to green field status of the field the well was in conservation before 1994. The following full-scale flow tests were carried out in 1999. Stages of elastic-and-plastic deformation and matrix rock breaking repeatedly cycled in the occurrence during the period of 1994-1999. In January 1999, the IRP curve shifted toward the left of the initial position and curves toward the axis of flow rates. Reduction of bottom-hole pressure with greater choke diameters increases rock contraction under growing tangential force and the IPR curve would have been more logical to observe toward the drawdown axis. In this case, the stage of rock breaking takes place in the well feed area, with formation of new fractures, which is intensified by the tangential stress and creation of additional fractures directly in the process of well survey. Flow tests in 2 months showed the IPR curve shift toward the right and upward which indicates the process of new cracks formation (i.e. the process of rock breaking) having effect on well performance, was prevailing in the rock mass since then. As the surveys were carried out, switching over to choke of d=6mm caused the IPR curving toward the axis of drawdowns and decreased productivity, which was determined by the impact of growing tangential stress as the process of elastic rock deformation was taking place. A single measurement with a choke of d=4mm carried out next month showed some growth in productivity and the dominant impact of the new crack formation process. The IPR of late 1999 indicates the reduction of productivity. Following April 1999, the process of rock breaking and formation of new cracks came to its end and a new stage of elastic-and-plastic deformation began, which resulted in reduced fracture opening and their permeability. Straight-line form of the ID reflects temporary equilibrium between reduced fracture opening and their increased concentration in the volume unit of rocks. Formation pressure of the occurrence was gradually decreasing and no measure were undertaken to increase it.

Fig. 8. Dynamics of IPR Curves Changing Across Time. Number of points-Choke Diameter (mm), near the IPR ends.
– date (month/year)

  1. If no regular well flow tests are carried out, it is possible to judge about deformation processes taking place in an occurrence using measurements of bottom-hole pressure values with chokes of permanent diameter. Changed fractures openness and, correspondingly, their permeability are reflected in changed values of bottom-hole pressure.
  2. Example from practice. 7 measurements were made during the period of 03.04.2000-22.12.2000 г. in a well where fractured sandstones were oil production target which registered the increase of bottom-hole pressure (choke = 8mm) from 10.2 MPa to 16.4 MPa. Bottom-hole pressure (7 measurements were taken) decreased from 16.4MPa to 10.8 MPa during the period of 23.12.2000-14.06.2001 and increased up to 12.4 MPa during the next measurement taken on 13.08.2001. The presented data can be interpreted in the following way: during the period of 03.04.2000-22.12.2000 the processes of matrix rock breaking and greater concentration of fractures are prevailing in the mass of rocks having effect on well performance; the period of 23.12.2000 – 14.06.2001 – processes of elastic-and-plastic deformations are prevailing in the rock volume having effect on well performance, resulting in reduced fractures opening and their permeability; following 14.06.2001 processes of rock breaking start dominating and concentration of fractures grows. Similar results were registered across multiple occurrences with fractured reservoirs.
  3. Processes of rock deformation are reflected in the results of well interference testing in the following way. If an occurrence is composed of fragile rocks, the growing concentration of fractures contributes to formation of new hydrodynamic ties. They can be detected by periodic interference well testing between the same pairs of wells. For example, a series of interference well tests was carried out on an occurrence composed of this type of rocks where one and the same pair of wells served as active well and observation well. . In this pair of wells, with the distance of 1800 m between them, no well interaction was detected; a repeated interference testing in 26 months registered a distinct interaction. The other pair of wells of the same occurrence, the distance between them being 750 m, showed no interaction during primary interference testing; the second interference testing, 7 months later, registered well interaction, which was additionally confirmed by the third interference testing 6 more months later.

If an occurrence is composed of elastic-and-plastic rocks and plastic deformations are not vividly expressed, an interference well testing most often would not show direct interaction between surveyed wells, although the objects under study refer to a single flow net. This is determined by the fact that due to plastic flow of rocks closing of fractures takes place in a shut-in well and pressure impulse does not reach a detecting instrument. The deformation type of rock can be defined by the IPR pattern. The IPRs of fragile rocks coincide in the drawdown and buildup modes (i.e. consequent increment and decrement in choke diameter) while the IPRs of the drawdown and build up modes are quite different from each other when we deal with elastic and plastic rocks.

Deformation processes related to the matrix rocks of a fractured reservoir can be managed by swapping the operating chokes: incrementing choke diameter accelerates the processes of deformation while decrementing reduces them. Water injection with the view to increase or maintain formation pressure is in its way a method to stabilize deformation processes. In other words, managing deformation processes in an occurrence with fractured reservoirs can be a simple and efficient way of management, field development and oil production.

Conclusion

         A fractured reservoir is a subsurface rock divided by subvertical open fractures making up a single flow network. The network itself is very sensitive to external and internal stresses on the rock and can immediately react to those changes by changing in well productivity. The variations of stresses can in certain way be controlled and modified making it possible to manage the process of field development and oil production using simple and available methods.

Sources

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  2. K.G.Boltenko, A.I.Echeistov, S.F.Zdorov. Basic results of the study of fractured rocks at Yaregankskoye oil field. Works of the 2nd All-Union Meeting on Fractured reservoirs of oil and gas. Moscow “Nedra”publishing house, 1965, p.233-240.
  3. B.I. Vilge, K.G.Waxman, Y.A. Limberger, V.M.Ilínsky “Induction Logging in Subsurface Rocks with Vertical Open Fracturing. Applied geophysics., 1989, Issue 121, p.201-207.
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  8. Y.A.Limberger, V.M.Il’insky, T.G.Radchenko “About the Potential of Fluid Flow in Fractured Reservoirs of the Kuma Horizon of Krasnodar Territory”. Geology of Oil and Gas, 1986, Issue 8, p.17-22.
  9. Y.A.Limberger, B.I.Vilge. “About the Potential of Fluid Flow in Oil Wells. Issues of Enhancing the Efficiency of Field Geophysical Survey (Collected Academic Papers of CGE). Moscow, VNIIOENG, 1989, p.19-28.
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