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喀斯特槽谷区土壤CO2浓度的短时变化及影响因素研究
引用本文:游贤慧,杨琰,徐刚,邹晓岗,何志立,田宁,田洪明,曾朱周.喀斯特槽谷区土壤CO2浓度的短时变化及影响因素研究[J].地球与环境,2019,47(1):16-25.
作者姓名:游贤慧  杨琰  徐刚  邹晓岗  何志立  田宁  田洪明  曾朱周
作者单位:西南大学地理科学学院,岩溶环境重庆市重点实验室,重庆400715;国土资源部岩溶生态环境-重庆南川野外基地,重庆408435;重庆和信农业发展有限公司,重庆,409800
基金项目:国家重点研发计划(2016YFC050230205);国家自然科学基金项目(41672160)。
摘    要:龙潭喀斯特槽谷两侧顺、逆倾坡裸岩出露率、植被覆盖率存在较大差异,为探究龙潭槽谷两侧顺、逆倾坡土壤CO_2浓度的短时变化及其影响因素,于2017年6月~2018年5月用固态CO_2传感器法在槽谷两侧顺、逆倾坡土面上开展高分辨率土壤CO_2浓度动态监测,并同时对监测点进行土壤温度、土壤湿度连续自动化监测。结果表明:(1)强降雨事件中,除强降雨初期(1h内),土壤CO_2浓度出现短暂降低外,降雨事件整体上促进了土壤CO_2浓度的上升;(2)昼夜尺度上,白天土壤CO_2浓度大于夜晚,土壤CO_2浓度对气温的响应速度较土温快;一年四季中,土壤CO_2浓度波动幅度大小次序为夏季秋季春季冬季;(3)在短时天气变化下,裸岩出露率越高、植被覆盖率越低,土壤CO_2浓度与土温的相关性越强且在强降雨下的变化幅度越大。

关 键 词:喀斯特槽谷区  土壤CO2浓度  强降雨  土壤温度  土壤湿度
收稿时间:2018/6/24 0:00:00
修稿时间:2018/8/28 0:00:00

Short Term Concentration Change of CO2 in Soils of Karst Trough Valley Area and Its Influencing Factors
YOU Xianhui,YANG Yan,XU Gang,ZOU Xiaogang,HE Zhili,TIAN Ning,TIAN Hongming,ZENG Zhuzhou.Short Term Concentration Change of CO2 in Soils of Karst Trough Valley Area and Its Influencing Factors[J].Earth and Environment,2019,47(1):16-25.
Authors:YOU Xianhui  YANG Yan  XU Gang  ZOU Xiaogang  HE Zhili  TIAN Ning  TIAN Hongming  ZENG Zhuzhou
Institution:1. Chongqing Key Laboratory of Karst Environment, School of Geographical Sciences, Southwest University, Chongqing 400715, China;2. Field Scientific Observation & Research Base of Karst Eco-environments at Nanchuan in Chongqing, Ministry of Land and Resources of China, Chongqing 408435, China;3. Harmo Trust Agriculture Development Co., Ltd, Chongqing 409800, China
Abstract:It had been reported that the rock exposure ratio and the vegetation coverage rate in the sloping and reversed slopes on both sides of the Longtan karst trough valley were different remarkably. This study conducted the dynamic high-resolution monitoring of CO2 concentration in soils on both sides of the Longtan karst trough valley, and monitored temperature and moisture of soils simultaneously using solid CO2 sensors during the period of from June 2017 to May 2018. The results showed that:(1) During heavy rainfalls, the overall soil CO2 concentration was promoted by rainfall events, except a short decrease in the early stage of rainfalls (within 1 hour). (2) The concentration of CO2 in soil was higher in the day than in the night, the concentration of CO2 in soil was more sensitive to the air temperature than the soil temperature did, and the daily fluctuation of CO2 concentration in soil followed an order of summer > autumn > spring > winter. (3) In terms of short-term weather conditions, the rock exposure and vegetation coverage rate have important influences on CO2 concentration of soil, the higher is the rock exposure rate, the higher is the fluctuation of CO2 concentrations in soil under heavy rainfalls, and the higher is the correlation of the CO2 concentrations in soil and the soil temperature.
Keywords:karst trough valley area  soil CO2 concentration  heavy rainfall  soil temperature  soil moisture
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