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作 者:Liang Wang Dong-hui Wang Qiong Xiao
机构地区:[1]Natural Resources Integrated Survey Command Center,China Geological Survey,Ministry of Natural Resources,Beijing 100055,China [2]Chengdu Center,China Geological Survey,Ministry of Natural Resources,Chengdu 610200,China [3]Institute of Karst Geology,Chinese Academy of Geological Sciences,Guilin 541004,China
出 处:《China Geology》2023年第4期759-761,共3页中国地质(英文)
摘 要:Carbonate rocks, as soluble rocks, will dissolve and experience karstification driven by flowing water. This process consumes CO_(2)from the air and converts atmospheric CO_(2) and CO_(3)^(2-)of rocks into HCO_(3)^(-), resulting in the transfer of carbon from the atmosphere to the hydrosphere. Part of those dissolved HCO3-in the groundwater and surface water will degrade as CO_(2) and return to the atmosphere.
关 键 词:PROSPECTING EASTERN KARST
分 类 号:P53[天文地球—古生物学与地层学]
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