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onclusions 1) A set of period components corresponding well to those of Earth tides and barometric pressure can be separated from the
hydro-spectra of deep well. The well-aquifer system responds to these components in some degree, which shows that groundwater
regime is influenced by Earth tides and barometric pressure. However, in different frequency bands a well-aquifer system possesses
different transfer ability for various inputs.
2) The transfer function quantitatively describes the response ability of well-aquifer system to Earth tides and barometric
pressure. It is a characteristic parameter that the system itself possesses. According to the transfer function value of well-aquifer
system to a certain input factor, we can objectively understand the influence of the input on the groundwater regime in a
deep well. This is of important significance for revealing the formation of groundwater regime in a deep well and for evaluating
the seismic supervising well.
The work was supported by National Natural Science Foundation of China (No. 49372149). 相似文献
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