白垩系地层深井冻结壁温度场分布规律  

Wall Temperature Field of a Deep Frozen Shaft in Cretaceous Strata

作　　者：周盛全 陈海明[1,2] 

机构地区：[1]安徽理工大学土木建筑学院,安徽淮南232001 [2]安徽理工大学矿山地下工程教育部工程研究中心,安徽淮南232001

出　　处：《冰川冻土》2013年第5期1232-1236,共5页Journal of Glaciology and Geocryology

基　　金：国家自然科学基金项目(51271071)资助

摘　　要：西部地区主要为白垩系软岩地层，煤炭资源储量大，成为我国重要产煤区．白垩系软岩地层冻结壁温度场分布规律尚不清楚，给白垩系地层冻结法凿井设计与施工带了一定的困难．通过现场实测、室内试验和数值模拟等手段，获得了白垩系地层冻结软岩热物理参数分布规律、力学特性及深井冻结壁冻融规律．测点冻结温度场反演白垩系冻结软岩导热系数值一般介于3．328～3．465W·m。·K-1之间，现场实测表明：白垩系地层融冻时间比一般为1．0～1．2之间．研究白垩系地层冻融规律，对指导我国西部地区白垩系地层冻结法凿井设计与施工具有重要的理论参考价值．Abstract. Western China, where the strata of Cre- taceous have been widely distributed, has become China＇s important coal producing area because of the large amount of coal resources. The frozen wall temperature field in Cretaceous soft rock stra ta is not clear, which brings some difficulties to the design and construction of freezing shaft sink- ing. The thermal physical parameters distribution, mechanical properties of the frozen soft rock and freezing and thawing rule of deep frozen wall in Cretaceous strata are able to gain by means ofmodern technical means, such as field measure- ment, laboratory test, numerical simulation and so on. Derived from the monitored freezing point and freezing temperature field, it is revealed that con ductivity value of the frozen soft rock in Cretaceous strata is generally in 3. 328-3. 465 W m 1 - K 1. In-situ measurements show that the time ra- tios of thawing-freezing in Cretaceous strata are u- sually between 1.0 and 1.2. These results will be useful for design and construction of freezing shaft sinking in Cretaceous strata in western China.

关 键 词：现场实测 数值模拟 冻结法凿井 白垩系地层 冻融规律 

分 类 号：P642.14[天文地球—工程地质学]