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Volume 34 Issue 3
Jun.  2015
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Article Navigation >  CARSOLOGICA SINICA  > 2015  >  34(3): 238-246
HUANG Chun-xia, LI Ting-yong, HAN Li-yin, LI Jun-yun, YUAN Na, WANG Hai-bo, ZHANG Tao-tao, ZHAO Xin. Deposition rates and element features of active sediments under drip water in Furong cave of Chongqing[J]. CARSOLOGICA SINICA, 2015, 34(3): 238-246. doi: 10.11932/karst20150306
Citation: HUANG Chun-xia, LI Ting-yong, HAN Li-yin, LI Jun-yun, YUAN Na, WANG Hai-bo, ZHANG Tao-tao, ZHAO Xin. Deposition rates and element features of active sediments under drip water in Furong cave of Chongqing[J]. CARSOLOGICA SINICA, 2015, 34(3): 238-246. doi: 10.11932/karst20150306
shu

Deposition rates and element features of active sediments under drip water in Furong cave of Chongqing

doi: 10.11932/karst20150306
  • 1.

    School of Geographical Sciences, Southwest University/Field Scientific Observation & Research Base of Karst Eco-environments at Nanchuan in Chongqing, Ministry of Land and Resources of China/Institute of Karst Geology, CAGS/Karst Dynamics Laboratory, MLR and GZAR

  • 2.

    School of Geographical Sciences, Southwest University

  • Publish Date: 2015-06-25
    Abstract
  • To explore the variation, control mechanism and environmental significance of deposition rates and elements in the recent sediments under drip water in the Furong cave, Chongqing, five drip sites were monitored continuously from November 2010 to November 2013, and recent sediments were collected for the deposition rate calculation and determination of trace elements. The results show distinct correlations among the deposition rates and the discharges of drip water, pH, Ca2+ concentration, PCO2 of the five drip sites. The deposition rates of MP4 and MP5 are both positively correlated with their discharges of drip water (r=0.75, n=11, p<0.01; r=0.63, n=11, p<0.05, respectively), and the deposition rates of the two drip sites exhibit obvious variations, high in rainy seasons while low in dry seasons. The deposition of MP4 and MP5 occur mainly in rainy seasons. The changes of their deposition rates can indicate the dry and humid changes of the outside environment. The annual precipitation increased during 2012-2013. Under the influence of dilution effect, water-rock interaction and different absorptions of plants for elements, the concentration of Mg decreased while the Sr concentration increased. At the same time, the Mg/Ca is negatively correlated with the Sr/Ca. They can respond to the increasing of the precipitation on the interannual time scale.

     

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