MP PFGun脉冲爆燃压裂技术在阿曼SSM-XX井的应用

简要叙述了MP PFGun技术工作原理、系统结构特点以及PropFrac脉冲压裂模拟器软件基本功能,并对SSM-XX井的模拟计算P-T曲线和井下压力仪实测曲线进行了对比。结果表明:SM-XX井采用MP PFGun电缆输送工艺安全,脉冲压裂持续时间长,且利用PropFrac模拟软件指导施工设计,取得了较好的应用效果。     

Description of the thermodynamic properties and fluid-phase behavior of aqueous solutions of linear,branched, and cyclic amines

The SAFT-γ Mie group-contribution equation of state is used to represent the fluid-phase behavior of aqueous solutions of a variety of linear, branched, and cyclic amines. New group interactions are developed in order to model the mixtures of interest, including the like and unlike interactions between alkyl primary, secondary, and tertiary amine groups (NH₂, NH, N), cyclic secondary and tertiary amine groups (cNH, cN), and cyclic methine-amine groups (cCHNH, cCHN) with water (H₂O). The group-interaction parameters are estimated from appropriate experimental thermodynamic data for pure amines and selected mixtures. By taking advantage of the group-contribution nature of the method, one can describe the fluid-phase behavior of mixtures of molecules comprising those groups over broad ranges of temperature, pressure, and composition. A number of aqueous solutions of amines are studied including linear, branched aliphatic, and cyclic amines. Liquid–liquid equilibria (LLE) bounded by lower critical solution temperatures (LCSTs) have been reported experimentally and are reproduced here with the SAFT-γ Mie approach. The main feature of the approach is the ability not only to represent accurately the experimental data employed in the parameter estimation, but also to predict the vapor–liquid, liquid–liquid, and vapor–liquid–liquid equilibria, and LCSTs with the same set of parameters. Pure compound and binary phase diagrams of diverse types of amines and their aqueous solutions are assessed in order to demonstrate the main features of the thermodynamic and fluid-phase behavior.     

Evidence of fluid evolution of Baoshan Cu−Pb−Zn polymetallic deposit: Constraints from in-situ sulfur isotope and trace element compositions of pyrite

In-situ LA-ICP-MS and S isotopes of pyrite from the Baoshan Cu polymetallic deposit were conducted to investigate the ore-forming process and the enrichment mechanism of elements. Three generations of pyrite (Py I, Py II, and Py III) in the skarn-type ores and pyrite in the carbonate-hosted sulfide ores from central, western, and northern (C_Py, W_Py, and N_Py) mining districts are selected for comparison. Compared with Py I and Py III, the contents of most elements in Py II are apparently higher. The As and Se contents are high within a wide range and are decoupled in the growth band of the C_Py. The highest As, Se, and Pb contents were found in W_Py and N_Py. These results indicate the drastic changes in the temperature and fluid mixing during the mineralization. The occurrence of fluctuation and change in temperature and f(O₂) was triggered by intermittent pulses of magmatic-hydrothermal fluids, mixing with meteoric water, and water−rock interactions. The sulfur isotopes of all species of pyrite indicated the magmatic source. The change in the f(O₂) conditions caused slight differences in the sulfur isotope compositions. Consequently, a metallogenic model was proposed to explain the ore-forming processes.     

Molding,patterning and driving liquids with light

When a laser beam induces surface tension gradient at the free surface of a liquid, a weak surface depression is expected and has been observed. Here we report giant depression and rupture in “optothermocapillary fluids” under the illumination of laser and sunlight. Computational fluid dynamics models were developed to understand the surface deformation and provided desirable physical parameters of the fluid for maximum deformation. New optothermocapillary fluids were created by mixing transparent lamp oil with different candle dyes. They can be cut open by sunlight and be patterned to different shapes and sizes using an ordinary laser show projector or a common laser pointer. Laser driving and elevation of optothermocapillary fluids, in addition to the manipulation of different droplets on their surface, were demonstrated as an efficient controlling method and platform for optofluidic operations. The fundamental understanding of light-induced giant depression and creation of new optothermocapillary fluids encourage the fundamental research and applications of optofluidics.     

双相不混溶流体饱和裂缝—孔隙岩石依赖频率的地震响应数值分析

裂缝—孔隙岩石中流体类型及其分布特征是影响弹性参数的重要因素，实际储层中流体大多不是单一流体，且在数值模拟过程中很少考虑流体间饱和状态的影响。为此，基于Chapman模型，针对饱含双相不混溶流体的裂缝—孔隙岩石，研讨了饱和度和毛细压力参数变化对砂岩储层频散衰减和地震响应的影响。数值分析结果表明：随着油气饱和度的增加，特征频率（不同于于单一流体介质情形）呈先减后增趋势，且在中间频段的变化最明显，地震响应存在时间延迟和波形畸变现象；当双相流体中存在气体时，频散衰减和地震响应对饱和度的变化更敏感；随着衡量流体间毛细压力的参数q值的增加，双相流体间由“斑块饱和”趋向“均匀饱和”状态，特征频率向着“高频低饱”方向移动。该数值模拟结果为储层流体识别提供了有效依据。     

不同脆性致密砂岩裂缝扩展规律实验

岩石的脆性与致密油气储集层压裂改造效果密切相关,但致密岩石的脆性对裂缝扩展规律的影响仍不明确。基于真三轴压裂模拟实验系统,对鄂尔多斯盆地东部3种不同脆性致密砂岩开展了压裂模拟实验,分析了脆性、压裂液类型和层理对裂缝扩展规律的影响。研究表明,山1段致密砂岩脆性最强,长7段致密砂岩次之,盒8段致密砂岩脆性最弱;在层理不发育的条件下,相比于中等脆性的盒8段致密砂岩,强脆性的山1段致密砂岩采用滑溜水压裂形成的单条裂缝扩展更充分,液态CO₂压裂形成的分支裂缝数量更多;在层理发育的条件下,长7段致密砂岩采用滑溜水压裂和液态CO₂压裂形成的裂缝的形态均较复杂;相比于滑溜水压裂,液态CO₂压裂形成的裂缝宽度更小;液态CO₂压裂更适用于脆性较强、层理发育的长7段致密砂岩储集层压裂改造。     

鄂尔多斯盆地东缘深部煤层气生产特征及开发对策——以大宁—吉县区块为例

我国埋深在1 000~2 000 m的深部煤层气地质资源量为22.5×1012m3,占总资源量的61.2%,如何提高深部煤层气单井产量,形成针对性的开发对策是研究和攻关的热点。通过统计分析大宁—吉县区块地质参数和试采井生产数据,表明深部煤储层具有渗透率低、微孔发育、可采系数低的特点,丛式井具有长期低产、上产缓慢和排采期长的生产特征,L型水平井具有上产期短,产气量高的生产特征。以此为基础建立了深部煤层气产能评价指标体系,影响深部煤层气产气效果的因素主要包括地质条件、工程技术及质量与管理三大类。因此,提高深部煤层气单井产量要做好以可采性为重点的高产区评价及预测,开展压裂施工参数优化和井型井网井距互相匹配的地质工程一体化设计,加强工程质量管理,降低储层伤害、实现长期持续排采。     

低渗透油藏中不同压裂注采井网非稳态产量计算分析

在井网压裂基础上进行注水，可以有效改善流场，增大泄油面积，是开发低渗透油藏的重要手段。快速准确预测低渗透油藏注水开发产量可以为开发优化设计奠定基础，但低渗透油藏注水开发呈现非稳态、非线性渗流特征，基于达西定律形成的油藏工程方法并不适用。本次研究通过流场分析，来划分等效流动单元，并在此基础上考虑了油水两相渗流启动压力梯度，采用流线积分法建立了不同压裂注采井网的水驱非稳态产量解析计算方法。与物理模拟及数值模拟相比，计算方法更简单，计算速度更快，可以为低渗透油藏压裂注采方式优选及注水开发对策制定提供手段。采用本方法计算并剖析了启动压力梯度、压裂注采方式及裂缝长度对油井生产动态的影响，结果表明：启动压力梯度增大了渗流阻力，与不考虑启动压力梯度相比，油井产量更低；受流动单元控制，不同压裂注采方式的增产效果及见水时间完全不同，同时压裂注采方式的增产效果最好，能够增产3.1倍，但见水时间仅为24个月；随着压裂缝长增加，油井产量越高，但当缝长超过最佳长度，增油效果不明显。     

地面微地震有源噪声自动识别与匹配压制方法

微地震监测技术通过对非常规储层压裂改造引发的震源点进行成像，实时提供压裂施工过程中产生的裂隙高度、长度、宽度和方位角等信息，为致密储层压裂提供指导，以提高油气采收率。在地面布设站点进行监测时，因微地震信号传播距离较远、近地表吸收衰减严重、地面有源噪声较多，微地震数据具有信号能量弱、噪声干扰强和信噪比低等特点，严重制约微地震事件的定位精度。噪声源多分布于地表，根据有源噪声与由储层向上传播的微地震事件在能量、频率、传播速度和源位置等方面的差异，本文提出微地震有源噪声自动识别与匹配方法。综合长短时窗能量比与微地震量板方法，自动识别有源噪声干扰，并进行噪声源位置和传播速度的三维最优并行搜索；利用同时确定的最优噪声源位置和传播速度对微地震数据进行动校正处理，得到噪声标准道，通过能量自适应匹配处理压制有源噪声。正演模拟数据和实际微地震数据去噪效果证明，本文方法能有效压制有源噪声，显著提高微地震数据品质，为后续微地震事件精确定位奠定了基础。