延寿井水温资料的远场效应研究
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摘要
本文简单介绍了延寿台水温井的观测条件与环境,分析了该井观测到的多次同震水位变化以及伴随的深层水温变化,并且水温多是上升,震后一至数小时后又恢复。由于井水振荡使水受到扰动,导致不同深度不同温度水的混合,从而造成同震水温变化的弥散模型,而后由于水的热传导作用又恢复正常。
This paper briefly introduced the condition and environment of observation on the water temperature of Yanshou well.The coseismic water level oscillation and correlated deep water temperature changes have been observed in this well.And the water temperature usually rises and recovers after one to several hours.It suggested that the temperature drop is produced by dispersive transfer of heat as the water oscillates,and follow-up thermal conduction makes temperature recovery.
This paper briefly introduced the condition and environment of observation on the water temperature of Yanshou well.The coseismic water level oscillation and correlated deep water temperature changes have been observed in this well.And the water temperature usually rises and recovers after one to several hours.It suggested that the temperature drop is produced by dispersive transfer of heat as the water oscillates,and follow-up thermal conduction makes temperature recovery.
引文
[1]黑龙江省地质矿产局.黑龙江省区域地质志[M].北京:地质出版社.1993.
[2]杨竹转,邓志辉,陶京玲,等.北京塔院井数字化观测水温的同震效应研究[J].地震学报,2007,29(2):203-213.
[3]张昭栋,迟镇乐,陈会民,等.井水位的振荡与地震波[J].地震研究,2000,23(4):418-425.
[4]谷元珠,车用太,鱼金子,等.塔院井水温微动态研究[J].地震,2003,23(1):102-108.
[5]石耀霖,曹建玲,马丽,等.唐山井水温的同震变化及其物理解释[J].地震学报,2007,29(2):265-273.
[2]杨竹转,邓志辉,陶京玲,等.北京塔院井数字化观测水温的同震效应研究[J].地震学报,2007,29(2):203-213.
[3]张昭栋,迟镇乐,陈会民,等.井水位的振荡与地震波[J].地震研究,2000,23(4):418-425.
[4]谷元珠,车用太,鱼金子,等.塔院井水温微动态研究[J].地震,2003,23(1):102-108.
[5]石耀霖,曹建玲,马丽,等.唐山井水温的同震变化及其物理解释[J].地震学报,2007,29(2):265-273.
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