饱和岩石的时温等效关系  

TIME-TEMPERATURE EQUIVALENCE OF SATURATED ROCKS

作　　者：席道瑛[1] 张程远[1] 刘小燕[1] 白石羽 

机构地区：[1]中国科学技术大学地球和空间科学系

出　　处：《物探化探计算技术》2000年第2期127-131,共5页Computing Techniques For Geophysical and Geochemical Exploration

基　　金：国家自然基金资助项目!(49774250)

摘　　要：通过饱和岩石的低频共振实验 ,探讨了饱和岩石热激活的驰豫过程 ,获得饱和岩石的驰豫个性和驰豫共性 。Though low frequency resonance vibration experiments on saturated rocks, relaxation of thermal activation of saturated rocks is discussed in this article, and individual and general characters of relaxation are obtained. These two characters are valuable both in theory and in applications for large geotechnical engineering and mineral resources exploration.

关 键 词：饱和岩石 驰豫个性 驰豫共性 时温等效关系 

分 类 号：TU45[建筑科学—岩土工程] TU458.2[建筑科学—土工工程]