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Spatial patterns of partial pressure of carbon dioxide and its exchange flux in karst lakes and reservoirs in a metropolis |
LI Yuan-yuan1, WANG Zhi-kang1, Irumva Olivier1, MA Yong-mei2, NI Mao-fei1,2, WU Yun-jie1,3 |
1. College of Eco-Environmental Engineering, Guizhou Minzu University, Guiyang 550025, China; 2. Chongqing Institute of Green and Intelligent Technology, Chinese Academy of Sciences, Chongqing 400714, China; 3. Guizhou Provincial Engineering Geological Disaster Prevention and Control Engineering Research Center, Guizhou Minzu University, Guiyang 550025, China |
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Abstract The typical karst lakes and reservoirs including AHa Reservoir (AHa), Songbaishan Reservoir (SBS), Baihua Lake (BHH) and Hongfeng Lake were investigated regarding spatial patterns of partial pressure of CO2 (pCO2) and CO2 exchange flux (F) in this study. We examined in-situ hydrometeorologic parameters, carbonate equilibria and environmental factors, as well as their potential constraints on water-air CO2 exchange. The higher pCO2 levels were observed in the AHa (861.6±462.8) μatm in comparison to the SBS (223.6±213.1) μatm, BHH (139.3±63.6) μatm and HFH (126.2±50.9) μatm (P<0.05). Gas transfer velocity of CO2 (k values) varied between 2.05~3.82cm/h. The F values were respectively (6.23±9.59) mmol/(m2·d), (-5.86±5.25) mmol/(m2·d), (-8.63±1.03) mmol/(m2·d) and (-7.58±1.10) mmol/(m2·d) in the AHa, SBS, BHH and HFH, indicating that karst lakes and reservoirs served as both CO2 sink and source with respect to the overlying atmosphere. Aquatic pCO2 was tightly linked to chlorophyll a (Chla) and ammonia nitrogen (NH4+-N), suggesting that surface water CO2 levels responded to coupled carbonate dissolution with photosynthesis and regional human inputs in the karst waters.
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Received: 13 May 2022
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