内陆地震
內陸地震
내륙지진
INLAND EARTHQUAKE
2014年
4期
312-318
,共7页
田韬%杨军%郝永亮%王维
田韜%楊軍%郝永亮%王維
전도%양군%학영량%왕유
钻孔应变%耦合系数%厚壁筒%引潮力标定%应力场
鑽孔應變%耦閤繫數%厚壁筒%引潮力標定%應力場
찬공응변%우합계수%후벽통%인조력표정%응력장
Borehole strain%Coupling coefficient%Thick -walled cylinder%Tide generating force calibration%Stress field
利用多层厚壁筒组合的力学模型,分析介质力学性质变化对钻孔面应变耦合系数的影响。利用引潮力标定方法对观测资料的研究表明,“地层、水泥环和钢筒”模型不能完全反映观测条件,考虑原地应力卸载影响的四层介质耦合模型,与观测环境基本相符,可以对观测结果进行较合理解释,同时发现钻孔面应变耦合系数的大小与台站的背景应力场存在一定关系。
利用多層厚壁筒組閤的力學模型,分析介質力學性質變化對鑽孔麵應變耦閤繫數的影響。利用引潮力標定方法對觀測資料的研究錶明,“地層、水泥環和鋼筒”模型不能完全反映觀測條件,攷慮原地應力卸載影響的四層介質耦閤模型,與觀測環境基本相符,可以對觀測結果進行較閤理解釋,同時髮現鑽孔麵應變耦閤繫數的大小與檯站的揹景應力場存在一定關繫。
이용다층후벽통조합적역학모형,분석개질역학성질변화대찬공면응변우합계수적영향。이용인조력표정방법대관측자료적연구표명,“지층、수니배화강통”모형불능완전반영관측조건,고필원지응력사재영향적사층개질우합모형,여관측배경기본상부,가이대관측결과진행교합리해석,동시발현찬공면응변우합계수적대소여태참적배경응력장존재일정관계。
In this paper , using more thick-walled cylinder force models , we analyze the impact of media mechanics properties change on coupling coefficient of borehole plane strain .Studying on the observation data with tide generating force calibration method show that ,“the stratum , cement and steel tube” model cannot fully reflect the observation conditions , considering the four layers coupled model influenced by in situ stress unloading is basically consistent with the observation environment , and the measured result can be more reasonable explained .In addition, we also find that there is a certain relationship between the borehole plane strain coupling coefficient size and background stress field of the station .