Temporal-spatial variation of SO42- concentration of the drip water and its significance in the Shihua cave, Beijing

Ban Feng-mei; Pan Gen-xing; Cai Bing-gui; Zhu Jian; Tan Ming

doi:10.3969/j.issn.1001-4810.2009.03.003

Volume 28 Issue 3

Sep. 2009

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Ban Feng-mei, Pan Gen-xing, Cai Bing-gui, Zhu Jian, Tan Ming. Temporal-spatial variation of SO42- concentration of the drip water and its significance in the Shihua cave, Beijing[J]. CARSOLOGICA SINICA, 2009, 28(3): 243-248. doi: 10.3969/j.issn.1001-4810.2009.03.003

Citation:

Ban Feng-mei, Pan Gen-xing, Cai Bing-gui, Zhu Jian, Tan Ming. Temporal-spatial variation of SO42- concentration of the drip water and its significance in the Shihua cave, Beijing[J]. CARSOLOGICA SINICA, 2009, 28(3): 243-248. doi: 10.3969/j.issn.1001-4810.2009.03.003

Citation:

Ban Feng-mei, Pan Gen-xing, Cai Bing-gui, Zhu Jian, Tan Ming. Temporal-spatial variation of SO42- concentration of the drip water and its significance in the Shihua cave, Beijing[J]. CARSOLOGICA SINICA, 2009, 28(3): 243-248. doi: 10.3969/j.issn.1001-4810.2009.03.003

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Temporal-spatial variation of SO42- concentration of the drip water and its significance in the Shihua cave, Beijing

doi: 10.3969/j.issn.1001-4810.2009.03.003

1.
Faculty of Environment Economics, Shanxi University of Finance ＆ Economics,Institute of Geology and Geophysics, Chinese Academy of Science
2.
Institute of Resources, Ecosystem and Environment of Agriculture, Nanjing Agricultural University
3.
Institute of Geology and Geophysics, Chinese Academy of Science

Received Date: 2009-05-05
Publish Date: 2009-09-25

Abstract

Abstract

As a crucial element in environmental geochemistry cycle, sulfur reflects the environmental change on both regional and global scales. In this study, sulfate radical concentration form 4 drip water points (PL1, PL2, SH, JG) in the Shihua cave have been monitored for three years, and those form the drip water point(BL) was monitored for two years. Drip discharges show three types of response to surface precipitation variations: rapid response, response with associated time-lag and stable (no response). The results show that: (1) SO42- concentration in rapid response drip water increases sharply during rain period, and has a exponential relationship with drip rate.; (2) in the drip water of lag response, SO42- concentration has no significant increase during rainfall, but they show a increasing trend during a long-term monitoring; (3) SO42- concentration at the stable drip site is low and has no obvious change during wet season. This means that the sharp increase of SO42- concentration may influence to some extent the pH value at the rapid response sites, which results in the declined calcium saturation index (SIc) of the drip water in rainy season. So it may be a indispensable factor to restrain the deposition rate of the drip waters in the Shihua cave.
- drip water,
- concentration of sulfate radical,
- deposition by drip water,
- the Shihua cave

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References

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Temporal-spatial variation of SO42- concentration of the drip water and its significance in the Shihua cave, Beijing

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Temporal-spatial variation of SO42- concentration of the drip water and its significance in the Shihua cave, Beijing

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