中国有色金属学报(英文版)
中國有色金屬學報(英文版)
중국유색금속학보(영문판)
TRANSACTIONS OF NONFERROUS METALS SOCIETY OF CHINA
2011年
12期
2711-2718
,共8页
曹平%万琳辉%汪亦显%黄永恒%张向阳
曹平%萬琳輝%汪亦顯%黃永恆%張嚮暘
조평%만림휘%왕역현%황영항%장향양
水%黏弹塑性%分级加卸载%广义开尔文模型
水%黏彈塑性%分級加卸載%廣義開爾文模型
수%점탄소성%분급가사재%엄의개이문모형
water%viscoelasto-plastic property%circular incremental step load and unload%generalized Kelvin model
采用分级增量循环加卸载方式,对金川有色金属公司二矿区深部斜长角闪岩进行干燥与水环境下的流变实验,分析流变实验数据,研究各级应力水平下斜长角闪岩两种试样的黏弹塑性.结果表明:水对岩石的瞬时弹模及黏塑特性的影响不大,对岩石黏弹性影响显著.分析水对岩石黏弹塑性影响的原因.根据试样的实验破坏前特点,选用广义开尔文模型描述斜长角闪岩流变特性,求得两种试样的岩石流变模型参数.模型参数分析发现:水对参数E1影响明显,而对参数E2影响不大:黏滞系数的离散性大,水对其影响不明确.
採用分級增量循環加卸載方式,對金川有色金屬公司二礦區深部斜長角閃巖進行榦燥與水環境下的流變實驗,分析流變實驗數據,研究各級應力水平下斜長角閃巖兩種試樣的黏彈塑性.結果錶明:水對巖石的瞬時彈模及黏塑特性的影響不大,對巖石黏彈性影響顯著.分析水對巖石黏彈塑性影響的原因.根據試樣的實驗破壞前特點,選用廣義開爾文模型描述斜長角閃巖流變特性,求得兩種試樣的巖石流變模型參數.模型參數分析髮現:水對參數E1影響明顯,而對參數E2影響不大:黏滯繫數的離散性大,水對其影響不明確.
채용분급증량순배가사재방식,대금천유색금속공사이광구심부사장각섬암진행간조여수배경하적류변실험,분석류변실험수거,연구각급응력수평하사장각섬암량충시양적점탄소성.결과표명:수대암석적순시탄모급점소특성적영향불대,대암석점탄성영향현저.분석수대암석점탄소성영향적원인.근거시양적실험파배전특점,선용엄의개이문모형묘술사장각섬암류변특성,구득량충시양적암석류변모형삼수.모형삼수분석발현:수대삼수E1영향명현,이대삼수E2영향불대:점체계수적리산성대,수대기영향불명학.
Using a circular incremental step load and unload method,a set of theological experiments were performed to study the viscoelasto-plastic properties of amphibolite in Jinchuan No.2 diggings under different environments.Based on the scientific analysis on rheological experimental data,the viscoelasto-plastic properties of amphibolite under different environments were studied.The results show that the instantaneous elastic modulus and viscoplastic properties of amphibolite are affected little,the viscoelastic properties of amphibolite are significantly affected.Based on the experimental results and characteristics of recovered rock specimen,a generalized Kelvin model was chosen to simulate theological properties of amphibolites and key parameters were obtained.It is found that the creep deformation modulus E1 is significantly influenced by the water,while the instant elastic modulus E2 is not significantly affected.The discreteness of the viscosity coefficient ηis large,the influence of water on η is not clear and needs to be further studied.