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Volume 42 Issue 1
Feb.  2023
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Article Navigation >  CARSOLOGICA SINICA  > 2023  >  42(1): 161-170
ZHAO Youmei, LIU Xiaoping, QI Huan. Experimental study on source compensation of Xiaoling key seepage zone in Jinan karst area[J]. CARSOLOGICA SINICA, 2023, 42(1): 161-170. doi: 10.11932/karst20230112
Citation: ZHAO Youmei, LIU Xiaoping, QI Huan. Experimental study on source compensation of Xiaoling key seepage zone in Jinan karst area[J]. CARSOLOGICA SINICA, 2023, 42(1): 161-170. doi: 10.11932/karst20230112
shu

Experimental study on source compensation of Xiaoling key seepage zone in Jinan karst area

doi: 10.11932/karst20230112
  • 1.

    801 Institute of Hydrogeology and Engineering Geology, Shandong Provincial Bureau of Geology & Mineral Resources, Jinan, Shandong 250014, China

  • 2.

    Key Laboratory of Groundwater Resources and Environment, Shandong Provincial Bureau of Geology & Mineral Resources, Jinan, Shandong 250014, China

  • 3.

    Shandong Engineering Research Center for Environmental Protection and Remediation on Groundwater, Jinan, Shandong 250014, China

  • Received Date: 2022-01-10
    Abstract
  • Located in Baotu Spring area, the study area is a key leakage zone in Xiaoling, a valley with east-west trend surrounded by the foothills of Jiunu Mountain, Xinglong Mountain, Changgeng Mountain and Hujia Mountain. The total area of this leakage zone is 4.03 km2. This study is aimed at understanding the characteristics and influencing factors of the leakage of source supplement of the soluble rock under the key seepage zone of Baotu Spring area in Jinan. Besides, this study may provide a basis for the selection of accurate location of source supplement and for the restoration measures of key leakage zone.In this paper, the thickness of Quaternary system, the buried depth and thickness of underlying soluble rock layer, the development degree of karst fissures, the distribution characteristics of fault structures, and the leakage amount and its effect on spring water in Xiaoling key leakage zone are studied by using the methods of field geological investigation, geophysics exploration, drilling, water injection and recharge experiment, and model simulation and prediction evaluation. The thickness of the Quaternary in the Xiaoling key leakage zone is 2.7-6.0 m, and the underlying strata of the Quaternary are the Chaomidian Formation with the lithology mainly composed of medium-thick micro-crystalline limestone, thin-bedded limestone and argillaceous-banded limestone. Controlled by the sedimentary environment, the formation development of Chaomidian Formation gradually thickens from east to west with its thickness from 7.6 m in the east to 56.3 m in the west. Fault structures are mainly developed with the north-north-west Qianfo Mountain Fault and the near-east-west fault in the key leakage zone. The development of karst is mainly controlled by stratum lithology and fault structure. The karstification of Chaomidian Formation is weak in the study area, affected by the Qianfo Mountain fault. On both sides of the large-scale fault zone, the more developed the karst is, the stronger the leakage of source supplement becomes. Under the condition of drilling and source supplement test, the amount of source-replenishing leakage of the Chaomidian Formation is 20,023 m3·d−1 on both sides of the fault in the Xiaoling key leakage zone. Given other recharge measures, the recharge amount is 15,000 m3·d−1 in the dry season, and the influence value of one-month recharge time on spring water is 2 cm. The research findings show that the influencing factors of recharge amount of the Guaternary underlying soluble rocks are listed as follows: the lithology of the underlying soluble rock, the degree of karst development, the degree of controlling over karst development by the fault structure, the width of the fracture zone of the fault structure, etc.. Besides, the fractured shatter zone in the key leakage zone is a precise source supplement section.

     

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