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Volume 37 Issue 2
Apr.  2018
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Article Navigation >  CARSOLOGICA SINICA  > 2018  >  37(2): 265-271
MAO Qingya, WANG Jianli, WANG Jialu, LI Wen. Characteristics and environmental significance of isotopes record from cave drip water and recent deposit in Naduo cave, Guizhou[J]. CARSOLOGICA SINICA, 2018, 37(2): 265-271. doi: 10.11932/karst20180213
Citation: MAO Qingya, WANG Jianli, WANG Jialu, LI Wen. Characteristics and environmental significance of isotopes record from cave drip water and recent deposit in Naduo cave, Guizhou[J]. CARSOLOGICA SINICA, 2018, 37(2): 265-271. doi: 10.11932/karst20180213
shu

Characteristics and environmental significance of isotopes record from cave drip water and recent deposit in Naduo cave, Guizhou

doi: 10.11932/karst20180213
  • 1.

    School of Geographical Sciences, Southwest University

  • 2.

    School of Geographical Sciences, Southwest University/Key Laboratory of the Three Gorges Reservoir Region’s Eco-Environment, MOE

  • 3.

    School of Geographical Sciences, Southwest University/School of Resources and Environmental Engineering, Anshun University

  • 4.

    Anshun Meteorological Bureau

  • Publish Date: 2018-04-25
    Abstract
  • To explore the cave drip water and the variation characteristics of its corresponding oxygen isotopes in modern deposits and their significance to the climatic environment, the atmospheric precipitation outside the Naduo cave in Guizhou, cave pool water, six drip points and their corresponding modern deposits oxygen stable isotopes have been monitored for the past 2 years. The results show that theδ18O in atmospheric precipitation, drip water, and deposits of Naduo cave are generally lower than those in most other southern regions. However, the seasonal variation ofδ18O from all three sources is significant. For example, theδ18O in atmospheric precipitation outside Naduo cave and in cave pool water both have seasonal characteristics that are higher in the dry season and lower in the wet season, and can basically reflect the climate change in the area where the cave is located. Though theδ18O in deposits and drip water have similar seasonal variation, they show a very different pattern from theδ18O in the atmospheric precipitation. This may be the result of the combination of regional topography, karst surface zone regulation, and atmospheric circulation.

     

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