Analysis of factors influencing rock salt dissolution rate under triaxial stress effect
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Analysis of factors influencing rock salt dissolution rate under triaxial stress effect
Vol. 34, Issue 4, (2013)
作者机构:
1. 重庆大学 煤矿灾害动力学与控制国家重点实验室,重庆,400044
2. 中国科学院武汉岩土力学研究所,武汉,430071
作者简介:
基金信息:
DOI:
CLC:TU452
Online First:16 April 2013,
Published:2013
稿件说明:
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JIANG De-yi, SONG Shu-yi, REN Song, et al. Analysis of factors influencing rock salt dissolution rate under triaxial stress effect[J]. 2013, 34(4).
DOI:
JIANG De-yi, SONG Shu-yi, REN Song, et al. Analysis of factors influencing rock salt dissolution rate under triaxial stress effect[J]. 2013, 34(4).DOI:
Analysis of factors influencing rock salt dissolution rate under triaxial stress effect
Rock salt sample dissolution tests under on the condition of triaxial stress with self-designed triaxial testing machine
rock salt dissolution rate orthogonal experiment under the mutual coupling of concentration
temperature
flow and deviatoric stress under the condition of triaxial stress
are carried out. Various factors influencing rock salt dissolution rate are studied. Any two factors are the binary linear regression
the relative importance ratio according to the standardized regression coefficients for rock salt dissolution rate to build judgment matrix; analytic hierarchy process is used to calculate weights of various factors. The results show that: Rock salt dissolution rate decreased rapidly with the concentration increasing. Dissolution rate increases with the temperature rising. Dissolution rate increases slowly with the flow increasing and did not change significantly. Dissolution rate decreases first and then slowly increases with increasing deviatoric stress. Range analysis and weights calculation show that primary and secondary factors affecting the rock salt dissolution rate are concentration
temperature
flow and the deviatoric stress. The weights of concentration
temperature
flow and the equivalent stress affecting the dissolution rate are 0.570
0.384
0.048
0.005 respectively; the weights of the two factors