运用水文时间序列分析识别济南泉域岩溶发育特征

李严; 王家乐; 靳孟贵; 马河宽; 柳浩然; 彭涛

doi:10.3799/dqkx.2020.236

Volume 46 Issue 7

Jul. 2021

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Article Navigation > Earth Science > 2021 > 46(7): 2583-2593

Li Yan, Wang Jiale, Jin Menggui, Ma Hekuan, Liu Haoran, Peng Tao, 2021. Hydrodynamic Characteristics of Jinan Karst Spring System Identified by Hydrologic Time-Series Data. Earth Science, 46(7): 2583-2593. doi: 10.3799/dqkx.2020.236

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Li Yan, Wang Jiale, Jin Menggui, Ma Hekuan, Liu Haoran, Peng Tao, 2021. Hydrodynamic Characteristics of Jinan Karst Spring System Identified by Hydrologic Time-Series Data. Earth Science, 46(7): 2583-2593. doi: 10.3799/dqkx.2020.236

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Hydrodynamic Characteristics of Jinan Karst Spring System Identified by Hydrologic Time-Series Data

doi: 10.3799/dqkx.2020.236

Li Yan^{1, 2
,
,},
Wang Jiale^{2
,
,
,},
Jin Menggui¹,
Ma Hekuan³,
Liu Haoran³,
Peng Tao⁴

1.
School of Environmental Studies, China University of Geosciences, Wuhan 430074, China
2.
Department of Soil and Water Conservation, Changjiang River Scientific Research Institute, Wuhan 430010, China
3.
No. 801 Hydrogeology & Engineering Geology Brigade, Shandong Provincial Bureau of Geology and Mineral Resources, Jinan 250014, China
4.
Institute of Heavy Rain, China Meteorological Administration, Wuhan 430205, China

Received Date: 2020-08-12
Publish Date: 2021-07-15

Abstract

Abstract

Karst aquifers are characterized by highheterogeneity and spatial variability of their media. Time-series analysis of precipitation and waterlevel (as input and output functions), including correlation, spectrum analysis, were applied to the Jinan karst spring system in Shandong Province, in order to study the hydrodynamic behavior and hydraulic properties of the aquifer system. Autocorrelation and cross-correlation analysis showed that the sensitivity of the system to precipitation input signal decreased gradually from the recharge area to the discharge area, but the memory effect increased gradually. Phase analysis results show that the response of water level to precipitation signal in Jinan spring area lags behind. The lag time from recharge area to discharge area gradually prolongs, and the recharge area has better linear correlation. The results show that the quick flow accounts for about 20%-30% of the subsurface flow in the recharge zone, and the ratio is reduced to 2.5%-10.0% in the discharge zone. The fluctuation of water level in karst system is mainly affected by the internal structure of karstic medium. The karstification degree of the aquifer in Jinan is fairly low, and groundwater movement is dominated by matrix flow.
- Karst aquifer,
- Time-series analysis,
- Karstification degrees,
- Jinan,
- groundwater

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References(44)

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Hydrodynamic Characteristics of Jinan Karst Spring System Identified by Hydrologic Time-Series Data

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