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考虑孔隙微观结构特征红砂岩自渗吸特性的研究

毕锋 周(重庆市江津区规划和自然资源局,中国)
颖 周(重庆市江津区规划和自然资源局,中国)
瑞川 田(重庆蜀通岩土工程有限公司,中国)
飞 干(贵州大学土木工程学院,中国)

摘要

为微观孔隙结构对红砂岩毛细水迁移特征的影响,论文采用低场核磁共振设备测试红砂岩的T2谱,进而获得红砂岩孔径分布和分形特征以及孔隙数量,并测试红砂岩吸14 d内吸水质量,同时比较了考虑孔隙分布的毛细吸水质量与实验值差距。结果表明:红砂岩孔隙数量分布差距巨大,数量比达到4406∶69∶1(小孔∶中孔∶大孔),且大孔分形维数大于中孔,大孔分布较为复杂,微孔不具有分形特征。同时,红砂岩毛细吸水质量变化前24h与时间呈 M(t)=1.1078t 0.6577 的幂函数变化,24h之后变化微小。另外,毛细吸水质量采用累加法计算与实验值基本吻合,故在计算毛细吸水质量时应充分考虑孔径分布特征,不能简单假设为一种孔径进行计算。

关键词

自渗吸;吸水质量;孔隙微观结构特征;NMR;红砂岩

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DOI: http://dx.doi.org/10.12345/smg.v6i1.15762

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