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Volume 38 Issue 5
Oct.  2019
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Article Navigation >  CARSOLOGICA SINICA  > 2019  >  38(5): 643-652
LI Chuansheng, QI Xiaofan, WANG Yushan, AN Yonghui, XING Liting. Response characteristics of typical karst groundwater levels of central Shandong Province to precipitation and climatic index[J]. CARSOLOGICA SINICA, 2019, 38(5): 643-652. doi: 10.11932/karst2019y12
Citation: LI Chuansheng, QI Xiaofan, WANG Yushan, AN Yonghui, XING Liting. Response characteristics of typical karst groundwater levels of central Shandong Province to precipitation and climatic index[J]. CARSOLOGICA SINICA, 2019, 38(5): 643-652. doi: 10.11932/karst2019y12
shu

Response characteristics of typical karst groundwater levels of central Shandong Province to precipitation and climatic index

doi: 10.11932/karst2019y12
  • 1.

    Shandong Institute of Surveying and Mapping of Geology, Jinan, Shandong 250002, China

  • 2.

    Center for Hydrogeology and Environmental Geology Survey, CGS, Baoding, Hebei 071051, China

  • 3.

    School of Water Conservancy and Environment, University of Jinan, Jinan,Shandong 250022, China；/Shandong Provincial Engineering Technology Research Center for Groundwater Numerical Simulation and Contamination Control, Jinan, Shandong 250022, China

  • Publish Date: 2019-10-25
    Abstract
  • Karst water resources in northern China is an important resource basis for economic and social development of its distribution area. The analysis of the dynamics of karst groundwater levels and its influencing factors can provide important supports for the management and rational development and utilization of the karst water resources, which is of practical significance. In this paper, 3 typical hydrogeological units in central Shandong Province are selected as the study area, and based on monthly data of precipitation, groundwater levels and NPI climatic index from 2010 to 2017, the periodicities, response characteristics and teleconnections of the above indices are analyzed by wavelet analysis methods. The results show that: ①The main fluctuation periods of the karst groundwater level dynamics, precipitation and NPI are all 1a, and the similarities and differences of the significant periods and the distribution time are the results of the combination of natural conditions and human activities. ②The response time lags of karst water levels to precipitation in the hydrogeological units are 95.81~146.64 d, and the differences mainly originate from the different monitoring positions of the groundwater flow systems. ③There are teleconnections between NPI and Zibo precipitation, and there are also teleconnections between NPI and the karst groundwater dynamics, which are mainly affected by precipitation. The time delays of karst groundwater levels to NPI are 111.75~169.77d, which are a bit longer than the time delays of precipitation and the groundwater levels. Recognizing the regular response characteristics of the karst groundwater levels to precipitation and NPI can provide assistance for the early warning and prediction of karst groundwater levels in northern China.

     

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