首页> 外文会议>SPE International Hydraulic Fracturing Technology Conference and Exhibition >Early Insights from Various Load Fluid Recoveries after Hydraulic Fracturing Treatments: A Case History of a Developing Unconventional Oil Shale Play in Alberta
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Early Insights from Various Load Fluid Recoveries after Hydraulic Fracturing Treatments: A Case History of a Developing Unconventional Oil Shale Play in Alberta

机译:液压压裂处理后各种载荷液回收的早期见解:艾伯塔省在艾伯塔省发展非传统石油页岩的案​​例历史

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The Devonian Duvernay Formation in Alberta,characterized as a carbonate-siliceous source rock,is ramping up to be one of the largest and most prolific shale oil plays in Canada.In the southern part of the Duvernay Shale Basin(i.e.East Shale Basin),tight limestone beds are interbedded with laminated organicrich calcareous shales,which show an organic maturity ranging mostly from early oil-to condensatewindow.This new light oil shale play is still in the initial stages of development and the nature of these deposits requires hydraulic fracturing to increase stimulated rock volume.General completion programs involve ≥50 clustered plug’n’perf stages with slickwater treatments in excess of 40,000 m3 with ~4000 tonnes of proppant per well.The large water volume treatments will inevitably interact directly with the rock surface in the stimulated area and cause both oil-water and rock-water interactions.Post-hydraulic fracturing water retention is especially pronounced in light oil shale plays.The oil-wet nature of the Duvernay,along with calcareous and siliceous shale lithologies,adds to the complexity of water retention and perceived water-blockage.In addition,because of operational delays such as road bans and pipeline constraints,some wells may be shut-in after the fracturing treatment for weeks and even months,which will affect rock-oilwater behavior(i.e.production).The extent of water displacing into the matrix of the rocks of the Duvernay Formation in the East Shale Basin,as measured by load fluid recovery,varies significantly and appears to heavily rely on the choice of surfactant.Although the use of surfactants is generally accepted for this play,detailed understanding of the rock-fluid interaction mechanisms is still incomplete.This paper investigated the response of Duvernay Shale rocks from the East Shale Basin to various types of surfactants and analyzed production and fluid flowback data.Amott Cell analyses,which test for spontaneous oil displacement using various stimulation fluid types,demonstrated that in the East Shale Basin,nano-sized surfactants including multi-functional surfactants(MFS)and microemulsions significantly outperformed common surfactant chemistry when tested with mixed wettability shale core samples.The results provide an estimate as to extent of water migration into the matrix of the Duvernay as a result of the choice of surfactant.Our analysis is made possible from publicly available cores,laboratory analysis and high quality well production data from the Alberta Energy Regulator.
机译:艾伯塔省的德文翁杜夫杜弗省形成,被描述为碳酸盐岩 - 硅质源岩,是加拿大最大,最丰富的页岩油戏剧之一。在Duvernay页岩盆地(Ieeast Shale Basin)的南部,紧密石灰岩床与层压的有利化钙质石头互相堵塞,这表明有机成熟度大多来自早期的油印露出的露出。这一新的轻油页面播放仍处于开发的初始阶段,这些沉积物的性质需要液压压裂增加刺激的岩石体积。一般性完成程序涉及≥50个聚类插头的阶段,使用Slickwater治疗超过40,000 m3,每孔〜4000吨支撑剂。大的水量处理将不可避免地与刺激的岩石表面相互作用区域并导致油水和岩石水相互作用。液压压裂水保留在轻油页面剧中特别明显。Duvernay的油脂性质以及钙质和硅质页岩岩性,增加了水保留和感知水的复杂性。此外,由于道路禁令和管道限制等运行延误,一些井可能是在压裂处理后关闭周数甚至几个月,这将影响岩石油水行为(IEPRODUCTION)。通过载荷测量的uvernay盆地中杜弗云盆地岩石岩体的水分程度流体恢复,显着变化,似乎严重依赖于表面活性剂的选择。虽然通常接受表面活性剂的使用对于这种游戏,但对岩石流体相互作用机制的详细了解仍然不完整。本文调查了杜弗杜瓦莱岩石的反应从东页岩盆地到各种类型的表面活性剂,分析生产和流体流量数据。达特米特细胞分析,使用var测试自发的油位移刺激流体类型,证明,在东页岩盆地中,纳米大小的表面活性剂,包括多功能表面活性剂(MF)和微乳液,用混合润湿性页岩核心样品测试时显着优于常见的常见表面活性剂化学。结果提供了估计由于选择表面活性剂的选择,水迁移到Duvernay的基质。从Alberta能量调节器的公开可用核心,实验室分析和高质量的生产数据中,可以进行分析。

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