High sensitivity of dissolved organic carbon transport during hydrological events in a small subtropical karst catchment
文献类型:期刊论文
作者 | Caiqing Qin; Si-Liang Li; Yiping Wu; Adrian M. Bass; Weijun Luo; Hu Ding; Fu-Jun Yue; Pan Zhang |
刊名 | Science of The Total Environment
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出版日期 | 2024 |
卷号 | 946页码:174090 |
DOI | 10.1016/j.scitotenv.2024.174090 |
英文摘要 | Dissolved organic carbon (DOC) and discharge are often tightly coupled, though these relationships in karst environments remain poorly constrained. In this study, DOC dynamics over 13 hydrological events, alongside monthly monitoring over an entire hydrological year were monitored in a small karst catchment, SW China. The concurrent analyses of power-law model and hysteresis patterns reveal that DOC behavior is generally transport-limited due to flushing effects of increased discharge but highly variable at both intra- and inter-event scales. The initial discharge at event onset and discharge-weighted mean concentration of DOC ([DOC]DW) of individual events can explain 37.7 % and 19.9 % of the variance of DOC behavior among events, respectively. The sustained dry-cold antecedent conditions make DOC hysteresis behavior during the earliest event complex and different from subsequent events. At event scale, the variability in DOC export is primarily controlled by [DOC]DW (explaining 64.3 %) and the yield of total dissolved solutes (YTDS, explaining 30.4 %), reflecting the impacts of variable hydrological connectivity and intense soil-water-rock interactions in this karst catchment. On an annual scale, DOC yield (YDOC, 222.86 kg C km−2) was mostly derived during the wet season (98.19 %) under the hydrological driving force. The difference in annual YDOC between this karst catchment and other regions can be well explained by annual water yield (Ywater, explaining 24.2 %) and [DOC] (explaining 35.4 %), whereas the variance in DOC export efficiency among catchments is almost exclusively controlled by [DOC] alone, independent of drainage area and annual Ywater. This study highlights the necessity of high-frequency sampling for modeling carbon biogeochemical processes and the particularity of the earliest hydrological events occurred after a long cold-dry period in karst catchments. Under the changing climate, whether DOC dynamics in karst catchments will present source-limited patterns during more extreme hydrological events merits further study.
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URL标识 | 查看原文 |
语种 | 英语 |
源URL | [http://ir.gyig.ac.cn/handle/42920512-1/15771] ![]() |
专题 | 地球化学研究所_环境地球化学国家重点实验室 |
作者单位 | 1.Department of Earth & Environmental Science, School of Human Settlements and Civil Engineering, Xi'an Jiaotong University, Xi'an, 710049, China 2.Institute of Surface-Earth System Science, School of Earth System Science, Tianjin University, Tianjin 300072, China 3.School of Geographical and Earth Sciences, University of Glasgow, Glasgow G12 8QQ, United Kingdom 4.State Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550081, China |
推荐引用方式 GB/T 7714 | Caiqing Qin,Si-Liang Li,Yiping Wu,et al. High sensitivity of dissolved organic carbon transport during hydrological events in a small subtropical karst catchment[J]. Science of The Total Environment,2024,946:174090. |
APA | Caiqing Qin.,Si-Liang Li.,Yiping Wu.,Adrian M. Bass.,Weijun Luo.,...&Pan Zhang.(2024).High sensitivity of dissolved organic carbon transport during hydrological events in a small subtropical karst catchment.Science of The Total Environment,946,174090. |
MLA | Caiqing Qin,et al."High sensitivity of dissolved organic carbon transport during hydrological events in a small subtropical karst catchment".Science of The Total Environment 946(2024):174090. |
入库方式: OAI收割
来源:地球化学研究所
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