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Investigation of karst hydrological processes by using grey auto-incidence analysis

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Abstract

The karst hydrological processes are the response of karst groundwater system to precipitation. The precipitation penetrates through the vadose zone, the subsequent groundwater pressure wave propagates to a spring outlet, and then, the spring discharge changes. This paper proposes a grey auto-incidence analysis for studying the karst hydrological processes. The method can detect the periodicity of a time series, for example, precipitation and spring discharge. Then the approach is applied to Liulin Springs Basin, China. The results show that the auto-incidence degree of precipitation reaches to the maximum (i.e., 0.816) when time delay equals to 8 years. The auto-incidence degree of spring discharge reaches to the maximum (i.e., 0.865) when time delay equals to 3 years. These results show that the periodicity of precipitation is 8 years, and of spring discharge is 3 years. The difference of periodicity between the precipitation and the spring discharge reveals that the processes of precipitation recharging groundwater and groundwater transport are regulated or controlled by karst aquifer. Because of heterogeneity of karst aquifer, the quick flow and base flow occur during the groundwater propagation, which causes the periodicity of spring discharge is not coincidence with of precipitation.

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Acknowledgments

This work is partially funded by the National Natural Science Foundation of China (41272245, 40972165, 40572150), the Opening Fund of Tianjin Key Laboratory of Water Resources and Environment 52XS1015, and 2012 National College Students’ Innovative Entrepreneurial Training Program 201210065025. We are also grateful to the two anonymous reviewers who have spent enormous efforts reviewing the manuscript and provided very encouraging, insightful, and constructive comments.

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Correspondence to Yonghong Hao.

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Hao, Y., Chen, X. & Wang, X. Investigation of karst hydrological processes by using grey auto-incidence analysis . Nat Hazards 71, 1017–1024 (2014). https://doi.org/10.1007/s11069-013-0695-x

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