Improving Long-Term Hydraulic Fracture Conductivity in Carbonate Formations by Substitution of Harder Minerals

Y. Samarkin, M. Aljawad, A. Amao, T. Sølling, K. Al-Ramadan, M. AlTammar, K. Alruwaili
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引用次数: 4

Abstract

Hydraulic fracturing is applied in tight formations to create conductive paths within the reservoir. However, the conductivity of the created fractures declines with time due to the closure stresses. The decline is sharp in soft formations because of proppant embedment and fracture surface asperities failure. The improvement in fracture surface hardness can mitigate the abovementioned challenges and sustain the fracture conductivity. This research targeted enhancing carbonate rock's hardness by forming minerals harder than calcite. Carbonate rocks, namely dolomite, limestone, and chalk, were treated at ambient temperature conditions by immersion into the aqueous solutions of NaF and ZnSO4 with a concentration of 0.1M. During treatment, the solution was sampled to monitor the changes in ion concentration and estimate the reaction kinetics by ICP - OES and IC devices. The hardness of rock samples was measured by impulse hammering technique before and after the treatment. The changes in rock's mineralogy and elemental content were studied by XRD and SEM imaging. The permeability of rocks was estimated by the steady-state gas injection method. The formation of smithsonite (ZnCO3, Mohs scale hardness - 4.5) and fluorite (CaF2, Mohs scale hardness - 4) was achieved in the reaction of calcite (CaCO3, Mohs scale hardness – 3) with ZnSO4 and NaF, respectively. Chalk and limestone reacted efficiently with both solutions; however, the dolomite reaction with solutions was feeble. XRD detected the newly formed smithsonite minerals, and it was observed in SEM images that minerals formed an interconnected net in chalk and limestone specimens. In dolomite samples, the minerals formed isolated gatherings that were sparsely located on the grains. The treatments caused the improvement of the rock specimen's hardness. 0.1M solution of NaF was not effective in strengthening the rock samples (only chalk sample experienced 6.7% improvement in hardness) because of low concentration of the solutions used; however, treatment resulted in negligible changes in permeability of the samples. In contrast, Young's modulus of limestone and chalk treated by ZnSO4 increased by 17% and 21%. Permeability of rocks treated by ZnSO4 reduced drastically, most likely due to the formation of gypsum as a byproduct of the reaction. This research presents a method for carbonate rock hardening via the transformation of parent calcite into harder minerals. It explains its possible application in the petroleum industry to sustain the conductivity of propped/acid fractures. The proposed technique will help to mitigate fracture conductivity decline due to proppant embedment and asperities failure issues that are especially severe in soft formations.
替代较硬矿物提高碳酸盐地层水力裂缝长期导流能力
水力压裂应用于致密地层,在储层内形成导电通道。然而,由于闭合应力的作用,裂缝的导流能力随着时间的推移而下降。在软地层中,由于支撑剂的嵌入和裂缝表面的凹凸破坏,下降幅度较大。裂缝表面硬度的提高可以缓解上述挑战,并保持裂缝导流能力。本研究旨在通过形成比方解石更硬的矿物来提高碳酸盐岩的硬度。在常温条件下,将碳酸盐岩(白云岩、灰岩和白垩岩)浸入0.1M浓度的NaF和ZnSO4水溶液中进行处理。在处理过程中,通过ICP - OES和IC装置对溶液进行采样,监测离子浓度的变化并估计反应动力学。采用脉冲锤击法测定了处理前后岩石试样的硬度。采用x射线衍射(XRD)和扫描电镜(SEM)成像研究了岩石矿物学和元素含量的变化。采用稳态注气法估算岩石渗透率。方解石(CaCO3,莫氏硬度- 3)与ZnSO4和NaF反应分别生成了菱锌矿(ZnCO3,莫氏硬度- 4.5)和萤石(CaF2,莫氏硬度- 4)。白垩和石灰石在两种溶液中都能有效反应;然而,白云石与溶液的反应很弱。XRD检测到新形成的菱锌矿矿物,SEM图像观察到矿物在白垩和石灰岩样品中形成相互连接的网状结构。在白云岩样品中,矿物形成孤立的集合体,稀疏地分布在颗粒上。这些处理使岩石试样的硬度有所提高。0.1M NaF溶液由于浓度过低,对岩样的强化效果不明显(只有白垩样品的硬度提高了6.7%);然而,处理导致样品的渗透性变化可以忽略不计。相比之下,经过ZnSO4处理的石灰石和白垩的杨氏模量分别提高了17%和21%。经过ZnSO4处理的岩石的渗透率急剧降低,很可能是由于反应的副产品石膏的形成。本研究提出了一种通过母方解石向较硬矿物的转变使碳酸盐岩硬化的方法。它解释了它在石油工业中维持支撑/酸性裂缝导流能力的可能应用。所提出的技术将有助于缓解由于支撑剂嵌入和颗粒破坏问题而导致的裂缝导流能力下降,这些问题在软地层中尤其严重。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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