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Volume 38 Issue 4
Aug.  2019
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MAO Jicheng, LIU Hong, ZUO Shuangying, HU Xuan. Formation mechanism of the karst spring in Dalongjing, Zhijin, Guizhou Province[J]. CARSOLOGICA SINICA, 2019, 38(4): 539-545. doi: 10.11932/karst20190410
Citation: MAO Jicheng, LIU Hong, ZUO Shuangying, HU Xuan. Formation mechanism of the karst spring in Dalongjing, Zhijin, Guizhou Province[J]. CARSOLOGICA SINICA, 2019, 38(4): 539-545. doi: 10.11932/karst20190410

Formation mechanism of the karst spring in Dalongjing, Zhijin, Guizhou Province

doi: 10.11932/karst20190410
  • Publish Date: 2019-08-25
  • The Dalongjing karst spring system lies in Chadian township, Zhijin, Guizhou Province. This work attempts to clarify its formation mechanism and the relevant relationship between groundwater recharge and drainage by investigations to the terrain, landform, and chemical analysis. Results show that this big karst spring system formed in a limestone area with low mountains and hills. It is formed during the Range-basin and the Wujiang periods when the area have experienced a persistent river incision and strong karstifiction. As a result, karst depressions and funnels extensively developed between surface peak clusters on the Shangzhai platform and the water holes in the middle area. In addition, atmospheric rainwater enters the underground along the sinkhole, producing southward runoffs at a natural gradient. During this process, the water flow is gradually concentrated in the karst cave voids, and in turn the karst space is gradually expanded by means of physical and chemical erosions. Finally, the water is collected in the Longdonggou and discharges to the ground surface in a concentrating manner, resulting in the Dalongjing karst springs and the Dalongjing water system

     

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