2012—2013年重庆雪玉洞洞穴系统碳循环特征

任坤; 沈立成; 袁道先; 王晓晓; 徐尚全

doi:10.3799/dqkx.2016.113

Volume 41 Issue 8

Aug. 2016

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Ren Kun, Shen Licheng, Yuan Daoxian, Wang Xiaoxiao, Xu Shangquan, 2016. Carbon Cycle Characteristics in Karst Cave System of Xueyu Cave from 2012 to 2013. Earth Science, 41(8): 1424-1434. doi: 10.3799/dqkx.2016.113

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Ren Kun, Shen Licheng, Yuan Daoxian, Wang Xiaoxiao, Xu Shangquan, 2016. Carbon Cycle Characteristics in Karst Cave System of Xueyu Cave from 2012 to 2013. Earth Science, 41(8): 1424-1434. doi: 10.3799/dqkx.2016.113

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Carbon Cycle Characteristics in Karst Cave System of Xueyu Cave from 2012 to 2013

doi: 10.3799/dqkx.2016.113

1.
Institute of Karst Geology, Chinese Academy of Geological Sciences, Karst Dynamics Laboratory of Ministry of Land and Resources & Guangxi, Guilin 541004, China
2.
International Research Center on Karst under the Auspices of UNESCO, Guilin 541004, China
3.
School of Geographical Sciences, Southwest University, Chongqing 400715, China
4.
Institute of Mountain Hazards and Environment, CAS, Chengdu 610041, China

Received Date: 2016-01-29
Publish Date: 2016-08-15

Abstract

Abstract

The high CO₂ concentration in Xueyue cave, Chongqing, is rare at home and abroad. However, the circulation characteristics of carbon and its controlling factors in this cave system remain unknown. P_{CO_2^-soil}, P_{CO_2^-cave}, P_{CO_2^-eq}, SIc, and δ¹³C_DIC of subterranean stream were analyzed to investigate the laws of CO₂ concentration variations in Xueyu cave and its contolling factors, as well as the impact on carbon cycle in this cave by subterranean stream. It is found that soil P_CO₂ mainly controlled by precipitation in subtropical areas was higher in rainy season than that of dry season. Cave air P_CO₂ exhibited seasonal variations, high cave air P_CO₂ typically occurred during warm periods, and low cave air P_CO₂ were typical of cold periods. It was ventilation driven by the temperature difference between cave and outside air that resulted in a sharp transition of cave air P_CO₂. Meanwhile, cave air P_CO₂ could rise to high level in a short period of time because of CO₂ degassing from subterranean stream. Due to soil CO₂ effect, groundwater became more mineralized water with low SIc and high water P_{CO_2^-eq}, and dissolution in some months in rainy season. With the reduction of soil CO₂ and precipitation, groundwater had low degree of mineralization with high SIc and low water P_{CO_2^-eq} in dry season.
- karst cave system,
- carbon cycle,
- CO₂ partial pressure,
- calcite saturation index,
- Xueyu cave,
- climate change

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References(53)

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Carbon Cycle Characteristics in Karst Cave System of Xueyu Cave from 2012 to 2013

doi: 10.3799/dqkx.2016.113

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