COSEISMIC RESPONSE ANALYSIS OF WATER LEVELAND TEMPERATURE AT WULIYING WELL FOR WENCHUAN AND JAPAN EARTHQUAKES
Wu Xiaodong 1) ; Wang Zhihui 1) ; Wang Chunyuan 2) ; Lu Yue 2) ; and Cao Kai 2)
1)Yanqing Seismostation of Earthquake Administration of Beijing Municipality, Beijing 102100;2)Earthquake Administration of Beijing Municipality, Beijing 100038
Abstract On the basis of observations of Wuliying Well， we studied the coseismic effects of water level and temperature and found both of the data raised by Wenchuan and Japan earthquakes independent with the focal mechanism or seismic location．Through the primary analysis, we found that the rock fracture shown the elasticplastic spread and shutting by the influence of the quakes on the well round area. The decreased rock porosity and the pressed waterbearing stratum made the water level rise, the up deep warmer water made the temperature go up.
Key words ：
Wuliying well
water level
water temperature
earthquake
coseismic change
Received: 01 January 1900
Corresponding Authors:
Wu Xiaodong
Cite this article:
Wu Xiaodong ,Wang Zhihui ,Wang Chunyuan et al. COSEISMIC RESPONSE ANALYSIS OF WATER LEVELAND TEMPERATURE AT WULIYING WELL FOR WENCHUAN AND JAPAN EARTHQUAKES[J]. , 2012, 32(Supp.): 22-24.
Wu Xiaodong ,Wang Zhihui ,Wang Chunyuan et al. COSEISMIC RESPONSE ANALYSIS OF WATER LEVELAND TEMPERATURE AT WULIYING WELL FOR WENCHUAN AND JAPAN EARTHQUAKES[J]. jgg, 2012, 32(Supp.): 22-24.
URL:
http://www.jgg09.com/EN/ OR http://www.jgg09.com/EN/Y2012/V32/ISupp./22
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