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- W3149772785 abstract "2008 年 5 月 12 日女士 8.0 Wenchuan 地震在三个峡区域在井的水层次引起了著名变化。这个工作在含水土层参数在水水平和变化检验在这些 coseismic 变化之间的关系。在有对地球潮的好回答的区域的三口井为分析被选择。到 2008 年 6 月的从 2 月的水级的数据被用来计算含水土层 transmissivity，渗透和岩石的特定的存储，并且分析在井和他们的含水土层参数的 coseismic 回答之间的关系。结果证明 Wenchuan 地震更加改变了这些参数，从而控制水的 co- 和 postseismic 变化水平。在地震以前的这些参数的价值线性地在水水平与 coseismic 变化的振幅被联系。越大含水土层 transmissivity，越多显著水里的 coseismic 变化水平。在地震期间，在参数被发现在水水平与 coseismic 变化被联系的含水土层变化，与当在水水平的 coseismic 变化更大时，发生的更大的变化。构造背景在水水平有对 co- 和 postseismic 变化的影响的某个度。差错地区的渗透结构看起来在水水平决定 coseismic 变化的方式。而且，看起来，在地下水更容易收敛的井的水水平能恢复更快的列在后面地震。从这研究的卓见帮助改进地震引起的水级的变化的特征的理解。" @default.
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- W3149772785 date "2013-01-01" @default.
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- W3149772785 title "Coseismic response of groundwater level in the Three Gorges well network and its relationship to aquifer parameters" @default.
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