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Volume 38 Issue 3
Jun.  2019
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Article Navigation >  CARSOLOGICA SINICA  > 2019  >  38(3): 361-369
WU Xia, PAN Moucheng, CAO Jianhua, ZHU Xiaoyan, ZHANG Meiliang, YANG Hui, TANG Wei, LAN Gaoyong. Characteristics of open cave environment and its influencing factors:A case study of Liangfeng cave, Guilin[J]. CARSOLOGICA SINICA, 2019, 38(3): 361-369. doi: 10.11932/karst2018y16
Citation: WU Xia, PAN Moucheng, CAO Jianhua, ZHU Xiaoyan, ZHANG Meiliang, YANG Hui, TANG Wei, LAN Gaoyong. Characteristics of open cave environment and its influencing factors:A case study of Liangfeng cave, Guilin[J]. CARSOLOGICA SINICA, 2019, 38(3): 361-369. doi: 10.11932/karst2018y16
shu

Characteristics of open cave environment and its influencing factors:A case study of Liangfeng cave, Guilin

doi: 10.11932/karst2018y16
  • 1.

    Institute of Karst Geology,CAGS/Key Laboratory of Karst Dynamics，MNR&GZAR, Guilin,Guangxi 541004,China/China University of Geosciences, Beijing 100083,China

  • 2.

    Institute of Karst Geology,CAGS/Key Laboratory of Karst Dynamics，MNR&GZAR, Guilin,Guangxi 541004,China

  • Publish Date: 2019-06-25
    Abstract
  • By continuous high-frequency monitoring of the internal and external temperature, humidity and pCO2 in the Liangfeng cave of Guilin, it is found that the temperature of the cave is seasonally changed under the influence of atmosphere temperature. However, due to "buffering effect" in the cave, the range of temperature change decreases with the cave depths from the outside to the inside, and its response time varies with season. The analysis of monitoring data indicated that the seasonal variation of temperature inside the cave is significantly lower than that outside the cave. By comparing the time series of temperature inside and outside of the cave, it is found that the temperature of the cave shows a longer lag time with the increase of atmospheric temperature and a shorter lag time with the decrease of atmospheric temperature at the seasonal timescale. This difference may be affected by the "buffering effect" of the internal structure of the cave in different seasons. The pCO2 in this cave has obvious seasonal variation characteristics of high in summer and low in winter. Moreover, seasonal changes in the external atmospheric environment and seasonal activities of the animals and plants on the caves have also caused seasonal variations in the main controlling factors of pCO2 in the caves.

     

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