在裂变流体热压力动力学下页岩的孔隙结构-声学属性合
Yun Ling1,2, Peng Xia1,3,2, Yi Lou4
1College of Resources and Environmental Engineering, Guizhou University, Guiyang 550025, China.
Langmuir : the ACS journal of surfaces and colloids
|November 4, 2025
概括
裂变流体改变了页岩孔隙结构和声学特性. 温度和压力变化显著影响孔积,碎形尺寸和声速,这对水库管理至关重要.
科学领域:
- 地质科学 地质科学
- 石油工程是石油工程中的一个.
- 材料科学 材料科学 材料科学
背景情况:
- 预测水库稳定性和声学监测依赖于了解裂变流体冲击.
- 页岩的复杂孔隙结构和声学行为对环境条件敏感.
研究的目的:
- 为了研究页岩矿物成分,孔隙结构和声学特性的多层次演变.
- 在变化温度和限制压力下阐明"毛孔-声学"合机制.
主要方法:
- 在破裂液中静态浸泡Dawuba页岩样本72小时.
- 控制的封闭压力 (5-15 MPa) 和温度 (20-50 °C) 的应用.
- 分析矿物成分,孔隙结构 (孔隙体积,碎形维度) 和声学特性 (速度,衰减).
主要成果:
- 在20°C时,粘土膨胀减少了孔腔体积,增加了声速.
- 增加的压力导致了宏孔进化,微骨折,孔径增加,声速降低.
- 高温加速了碳酸盐的溶解,改变了孔隙结构,增加了波散射.
- 结合的温度和压力增加了孔隙连接,削弱了页岩骨架,降低了声速,增加了衰减.
结论:
- 揭示了一种取决于温度和压力的"毛孔声学"合机制.
- 低压水化会导致孔隙压缩,而高压/高温条件会诱导孔隙转变和裂纹发展.
- 页岩的孔隙结构演变直接影响声响应,孔隙体积和碎形尺寸之间存在很强的相关性.
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