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峰丛洼地表层岩溶动力系统季节变化规律
引用本文:姜光辉,郭芳,曹建华,游省易,李恩香,邓艳.峰丛洼地表层岩溶动力系统季节变化规律[J].地球科学,2003,28(3):341-345.
作者姓名:姜光辉  郭芳  曹建华  游省易  李恩香  邓艳
作者单位:[1]国土资源部岩溶动力学开放研究实验室,广西桂林541004 [2]中国地质科学院岩溶地质研究所,广西桂林541004 [3]中国地质大学工程学院,湖北武汉430074 [4]广西师范大学生物系,广西桂林541004
基金项目:国土资源部重点科技项目 (No .2 0 0 0 2 0 8),科技部公益专项 (No .2 0 0 0 16 4) .
摘    要:峰丛洼地表层岩溶动力系统与土壤CO2密切相关.土壤C02体积分数变化受气温和降雨影响,其季节变化特征表现为:冬季的波谷、夏季的波峰交替出现,秋季出现次波谷和次波峰.受降雨影响,表层岩溶动力系统运行强度春、夏季较强,秋、冬季较弱.从冬至夏,在土壤CO2逐渐增多时,系统溶解、转移碳的能力也逐渐增强.在土壤CO2和温度双重支配下,系统由冬季的沉积趋势转为春、夏季的溶解趋势.

关 键 词:峰丛洼地  表层岩溶动力系统  季节变化  土壤CO2  气温  降雨  岩溶作用  表层地质作用  碳酸盐岩
文章编号:1000-2383(2003)03-0341-05

Seasonal Change of Epi-Karst Dynamic System in Peak-Depression Area
JIANG Guang-hui ,GUO Fang ,CAO Jian-hua ,YOU Sheng-yi,LI En-xiang,DENG Yan.Seasonal Change of Epi-Karst Dynamic System in Peak-Depression Area[J].Earth Science-Journal of China University of Geosciences,2003,28(3):341-345.
Authors:JIANG Guang-hui    GUO Fang    CAO Jian-hua    YOU Sheng-yi  LI En-xiang  DENG Yan
Institution:JIANG Guang-hui 1,2,GUO Fang 1,2,CAO Jian-hua 1,2,YOU Sheng-yi3,LI En-xiang4,DENG Yan4
Abstract:Epi-karst dynamic system is related closely with CO 2 content in soil. Temperature and rainfall dominate the seasonal change of CO 2 content in soil. The CO 2 content is low in winter when it is cold and dry while it is high in summer as it is hot and wet. There are a hypo-trough and a hypo-crest in autumn when there is a sudden increasing in rainfall. Epi-karst dynamic system is more active from spring to summer than from autumn to winter, because rainfall is focus in spring and summer. The system transfers more and more carbon with the increase of CO 2 content in soil from winter to summer. With the control of CO 2 content and temperature, the sedimentation-dissolution trend of the system changes from sedimentation trend to dissolution trend from winter to spring and summer.
Keywords:peak-cluster depression  epi-karst dynamic system  CO  2 in soi
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