...
首页> 外文期刊>Petroleum science >Experimental investigation of shale imbibition capacity and the factors influencing loss of hydraulic fracturing fluids
【24h】

Experimental investigation of shale imbibition capacity and the factors influencing loss of hydraulic fracturing fluids

机译:页岩吸水能力及水力压裂液流失影响因素的实验研究

获取原文
           

摘要

Spontaneous imbibition of water-based fracturing fluids into the shale matrix is considered to be the main mechanism responsible for the high volume of water loss during the flowback period. Understanding the matrix imbibition capacity and rate helps to determine the fracturing fluid volume, optimize the flowback design, and to analyze the influences on the production of shale gas. Imbibition experiments were conducted on shale samples from the Sichuan Basin, and some tight sandstone samples from the Ordos Basin. Tight volcanic samples from the Songliao Basin were also investigated for comparison. The effects of porosity, clay minerals, surfactants, and KCl solutions on the matrix imbibition capacity and rate were systematically investigated. The results show that the imbibition characteristic of tight rocks can be characterized by the imbibition curve shape, the imbibition capacity, the imbibition rate, and the diffusion rate. The driving forces of water imbibition are the capillary pressure and the clay absorption force. For the tight rocks with low clay contents, the imbibition capacity and rate are positively correlated with the porosity. For tight rocks with high clay content, the type and content of clay minerals are the most important factors affecting the imbibition capacity. The imbibed water volume normalized by the porosity increases with an increasing total clay content. Smectite and illite/smectite tend to greatly enhance the water imbibition capacity. Furthermore, clay-rich tight rocks can imbibe a volume of water greater than their measured pore volume. The average ratio of the imbibed water volume to the pore volume is approximately 1.1 in the Niutitang shale, 1.9 in the Lujiaping shale, 2.8 in the Longmaxi shale, and 4.0 in the Yingcheng volcanic rock, and this ratio can be regarded as a parameter that indicates the influence of clay. In addition, surfactants can change the imbibition capacity due to alteration of the capillary pressure and wettability. A 10 wt% KCl solution can inhibit clay absorption to reduce the imbibition capacity.
机译:水基压裂液自发吸收到页岩基质中被认为是造成返排期间大量失水的主要机理。了解基质的吸收能力和速率有助于确定压裂液的体积,优化返排设计并分析对页岩气生产的影响。对四川盆地的页岩样品和鄂尔多斯盆地的一些致密砂岩样品进行了吸水实验。还对松辽盆地的致密火山岩样品进行了比较。系统地研究了孔隙度,粘土矿物,表面活性剂和KCl溶液对基质吸收能力和吸收速率的影响。结果表明,致密岩的吸水特征可以用吸水曲线形状,吸水量,吸水率和扩散率来表征。吸水的驱动力是毛细压力和粘土吸收力。对于粘土含量低的致密岩石,吸水率和吸水率与孔隙率成正相关。对于高粘土含量的致密岩石,粘土矿物的类型和含量是影响吸水能力的最重要因素。通过孔隙率归一化的吸水量随总粘土含量的增加而增加。蒙脱石和伊利石/蒙脱石倾向于大大增强吸水能力。此外,富含粘土的致密岩石吸收的水量大于其测得的孔体积。牛头塘页岩的吸水体积与孔隙体积的平均比约为1.1,卢家坪页岩为1.9,龙马溪页岩为2.8,应城火山岩为4.0,该比例可以看作是一个参数,表示粘土的影响。另外,由于毛细管压力和润湿性的改变,表面活性剂可以改变吸收能力。 10 wt%的KCl溶液会抑制粘土的吸收,从而降低吸收能力。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号