长江科学院院报 ›› 2015, Vol. 32 ›› Issue (5): 95-99.DOI: 10.3969/j.issn.1001-5485.2015.05.018

• 岩土工程 • 上一篇    下一篇

岩石毛细吸水试验新方法

贾志刚1,2,齐平2,李科1,曾洪彪1   

  1. 1.中国地质大学 工程学院,武汉 430074;
    2.黄淮学院 建筑工程学院,河南 驻马店 463000
  • 收稿日期:2013-12-13 出版日期:2015-05-01 发布日期:2015-05-14
  • 作者简介:贾志刚(1977-),男,河南汤阴人,讲师,博士研究生,从事岩土工程方面的研究,(电话)13783350253
  • 基金资助:
    国家自然科学基金资助项目(41272377)

New Approach in Measuring Capillary Water Absorption of Rock

JIA Zhi-gang1,2,QI Ping2,LI Ke1,ZENG Hong-biao1   

  1. 1.Faculty of Engineering, China University of Geoscience, Wuhan 430074, China;
    2.Architecture Engineering College, Huanghuai University, Zhumadian 463000, China
  • Received:2013-12-13 Online:2015-05-01 Published:2015-05-14

摘要: 毛细作用下岩石吸水作为一种水分传输现象在诸多领域有极其重要的影响。推导了岩石毛细直管吸水模型,在详细讨论已有吸水试验方法的基础上提出了一种吸水量量测新方法。结论如下:① 新试验方法以称量剩余水量为基础,可以实现岩石吸水过程中吸水量连续、精确的量测,且可以满足一维或三维2种边界条件;② 采用试验新方法,在石膏质岩初始吸水阶段,其吸水量与时间的关系基本上满足毛管理论模型,新方法能较好地适用于岩石毛细吸水试验;③ 分析了吸水试验数据拟合时相关系数-频次的关系,证明了试验新方法具有较小的系统误差,试验数据更加稳定与可靠。

关键词: 石膏质岩, 毛细作用, 岩石吸水, 试验方法, 量测方法

Abstract: Capillary water absorption in porous rock, as a water transport phenomenon, is of extreme importance in many fields. The kinetics of capillary water absorption of rock was derived and discussed in detail, and then a new approach of measuring the capillary water absorption was proposed. We conclude that 1) the new approach is based on measuring residual water, thus is simple and accurate in continuously measuring the genuine water absorption rate of rocks, and meets two-dimensional or three-dimensional boundary conditions; 2) in the initial stage of water absorption of gypsum rocks, the relationship between water absorption value and time is consistent with capillary theoretical model; 3) the relationship between correlation coefficient and frequency during the fitting of test data proves that the new approach has small errors and the test data is stable and reliable.

Key words: gypsum rocks, capillary phenomenon, rock imbibitions, test method, measurement method

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