原文服务方: 地球化学学报(英文)       
摘要:
Speleothem carbonates are precipitated continuously from inorganic carbon dissolved in seepage water infiltrating from the land surface, that reflects a mixture of atmospheric CO2, respired soil carbon, and epikarst sources, each with distinct δ13C values. To aid in deconvolving these signatures, soil samples were collected above the Blue Spring cave system in Sparta, Tennessee, USA and subjected to a series of incubation experiments, in order to constrain the correlation between CO2 respiration rates and soil moisture. This relationship is used to parameterize a simple mixing model which predicts the relationship between δ13C and soil moisture in fluids infiltrating into the underlying cave system.
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篇名 The hydrologic record of karst systems: linking soil moisture to the carbon isotope signatures of so
来源期刊 学科 地球科学
关键词 Speleothem δ13C CO2 respiration Soil moisture
年,卷(期) 2022,(3) 所属期刊栏目
研究方向 页码范围 392-395
页数 3页 分类号
字数 语种 英文
DOI 10.1007/s11631-017-0171-5
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研究主题发展历程
节点文献
Speleothem
δ13C
CO2 respiration
Soil moisture
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地球化学学报(英文)
双月刊
2096-0956
52-1161/p
16开
贵阳市林城西路99号
1982-01-01
英语
出版文献量(篇)
230
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0
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