岩土力学
巖土力學
암토역학
ROCK AND SOIL MECHANICS
2013年
4期
1025-1030
,共6页
姜德义%宋书一%任松%陈结%杨春和
薑德義%宋書一%任鬆%陳結%楊春和
강덕의%송서일%임송%진결%양춘화
岩盐%溶解速率%三轴应力%正交试验%层次分析法
巖鹽%溶解速率%三軸應力%正交試驗%層次分析法
암염%용해속솔%삼축응력%정교시험%층차분석법
rock salt%dissolution rate%triaxial stress%orthogonal%analytic hierarchy process
利用自行研制的三轴岩盐溶解试验机,实现在三轴应力条件下岩盐试样溶解试验.进行三轴应力条件下溶液浓度、温度、流量以及偏应力4个因素相互耦合状态的岩盐溶解速率正交试验,研究各个因素对岩盐溶解速率的影响规律.对任意两个影响因素分别进行二元线性回归,根据其标准回归系数对岩盐溶解速率相对重要性比值构建判断矩阵,运用层次分析法计算各个影响因素的权值.研究结果表明,岩盐溶解速率随着浓度增大迅速降低,随着温度升高而增大,随着流量增大缓慢增加,但变化并不明显;随着偏应力增大先减小,后缓慢增大.极差分析和权值计算结果表明,岩盐溶解速率影响因素主次关系依次为浓度、温度、流量和偏应力.4个因素对岩盐溶解速率影响权值大小依次为0.570、0.384、0.048、0.005,其中浓度和温度两个影响因素权重占到95%.
利用自行研製的三軸巖鹽溶解試驗機,實現在三軸應力條件下巖鹽試樣溶解試驗.進行三軸應力條件下溶液濃度、溫度、流量以及偏應力4箇因素相互耦閤狀態的巖鹽溶解速率正交試驗,研究各箇因素對巖鹽溶解速率的影響規律.對任意兩箇影響因素分彆進行二元線性迴歸,根據其標準迴歸繫數對巖鹽溶解速率相對重要性比值構建判斷矩陣,運用層次分析法計算各箇影響因素的權值.研究結果錶明,巖鹽溶解速率隨著濃度增大迅速降低,隨著溫度升高而增大,隨著流量增大緩慢增加,但變化併不明顯;隨著偏應力增大先減小,後緩慢增大.極差分析和權值計算結果錶明,巖鹽溶解速率影響因素主次關繫依次為濃度、溫度、流量和偏應力.4箇因素對巖鹽溶解速率影響權值大小依次為0.570、0.384、0.048、0.005,其中濃度和溫度兩箇影響因素權重佔到95%.
이용자행연제적삼축암염용해시험궤,실현재삼축응력조건하암염시양용해시험.진행삼축응력조건하용액농도、온도、류량이급편응력4개인소상호우합상태적암염용해속솔정교시험,연구각개인소대암염용해속솔적영향규률.대임의량개영향인소분별진행이원선성회귀,근거기표준회귀계수대암염용해속솔상대중요성비치구건판단구진,운용층차분석법계산각개영향인소적권치.연구결과표명,암염용해속솔수착농도증대신속강저,수착온도승고이증대,수착류량증대완만증가,단변화병불명현;수착편응력증대선감소,후완만증대.겁차분석화권치계산결과표명,암염용해속솔영향인소주차관계의차위농도、온도、류량화편응력.4개인소대암염용해속솔영향권치대소의차위0.570、0.384、0.048、0.005,기중농도화온도량개영향인소권중점도95%.
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, concentration and temperature, account for 95%.