Spatial patterns and environmental controls of particulate organic carbon in surface waters in the conterminous United States

Carbon cycling in inland waters has been identified as an important, but poorly constrained component of the global carbon cycle. In this study, we compile and analyze particulate organic carbon (POC) concentration data from 1145U.S. Geological Survey (USGS) gauge stations to investigate the spatial...

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Veröffentlicht in:The Science of the total environment 2016-06, Vol.554-555, p.266-275
Hauptverfasser: Yang, Qichun, Zhang, Xuesong, Xu, Xingya, Asrar, Ghassem R., Smith, Richard A., Shih, Jhih-Shyang, Duan, Shuiwang
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container_issue
container_start_page 266
container_title The Science of the total environment
container_volume 554-555
creator Yang, Qichun
Zhang, Xuesong
Xu, Xingya
Asrar, Ghassem R.
Smith, Richard A.
Shih, Jhih-Shyang
Duan, Shuiwang
description Carbon cycling in inland waters has been identified as an important, but poorly constrained component of the global carbon cycle. In this study, we compile and analyze particulate organic carbon (POC) concentration data from 1145U.S. Geological Survey (USGS) gauge stations to investigate the spatial variability and environmental controls of POC concentration. We observe substantial spatial variability in POC concentration (1.43±2.56mgC/L, mean±one standard deviation), with the Upper Mississippi River basin and the Piedmont region in the eastern U.S. having the highest POC concentration. Further, we employ generalized linear models (GLMs) to analyze the impacts of sediment transport and algae growth as well as twenty-one other environmental factors on the POC variability. Suspended sediment and chlorophyll-a explain 26% and 17% of the variability in POC concentration, respectively. At the national level, the twenty-one environmental factors combined can explain ca. 40% of the spatial variance in POC concentration. At the national scale, urban area and soil clay content show significant negative correlations with POC concentration, whereas soil water content and soil bulk density correlate positively with POC. In addition, total phosphorus concentration and dam density correlate positively with POC concentration. Furthermore, regional scale analyses reveal substantial variation in environmental controls of POC concentration across eighteen major water resource regions in the U.S. The POC concentration and associated environmental controls also vary non-monotonically from headwaters to large rivers. These findings indicate complex interactions among multiple factors in regulating POC concentration over different spatial scales and across various sections of the river networks. This complexity, together with the large unexplained uncertainty, highlights the need for considering non-linear interplays of multiple environmental factors and developing appropriate methodologies to track the transformation and transport of POC along the terrestrial-aquatic interfaces. The 1145 U.S. Geological Survey gauge stations and concentration of particulate organic carbon. [Display omitted] •POC concentration varies substantially across surface waters in the United States.•Suspended sediment and chlorophyll-a explain 26% and 17% of the POC variability.•Twenty one environmental factors explain ca. 40% of the spatial variance in POC.
doi_str_mv 10.1016/j.scitotenv.2016.02.164
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(PNNL), Richland, WA (United States)</creatorcontrib><description>Carbon cycling in inland waters has been identified as an important, but poorly constrained component of the global carbon cycle. In this study, we compile and analyze particulate organic carbon (POC) concentration data from 1145U.S. Geological Survey (USGS) gauge stations to investigate the spatial variability and environmental controls of POC concentration. We observe substantial spatial variability in POC concentration (1.43±2.56mgC/L, mean±one standard deviation), with the Upper Mississippi River basin and the Piedmont region in the eastern U.S. having the highest POC concentration. Further, we employ generalized linear models (GLMs) to analyze the impacts of sediment transport and algae growth as well as twenty-one other environmental factors on the POC variability. Suspended sediment and chlorophyll-a explain 26% and 17% of the variability in POC concentration, respectively. At the national level, the twenty-one environmental factors combined can explain ca. 40% of the spatial variance in POC concentration. At the national scale, urban area and soil clay content show significant negative correlations with POC concentration, whereas soil water content and soil bulk density correlate positively with POC. In addition, total phosphorus concentration and dam density correlate positively with POC concentration. Furthermore, regional scale analyses reveal substantial variation in environmental controls of POC concentration across eighteen major water resource regions in the U.S. The POC concentration and associated environmental controls also vary non-monotonically from headwaters to large rivers. These findings indicate complex interactions among multiple factors in regulating POC concentration over different spatial scales and across various sections of the river networks. This complexity, together with the large unexplained uncertainty, highlights the need for considering non-linear interplays of multiple environmental factors and developing appropriate methodologies to track the transformation and transport of POC along the terrestrial-aquatic interfaces. The 1145 U.S. Geological Survey gauge stations and concentration of particulate organic carbon. 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We observe substantial spatial variability in POC concentration (1.43±2.56mgC/L, mean±one standard deviation), with the Upper Mississippi River basin and the Piedmont region in the eastern U.S. having the highest POC concentration. Further, we employ generalized linear models (GLMs) to analyze the impacts of sediment transport and algae growth as well as twenty-one other environmental factors on the POC variability. Suspended sediment and chlorophyll-a explain 26% and 17% of the variability in POC concentration, respectively. At the national level, the twenty-one environmental factors combined can explain ca. 40% of the spatial variance in POC concentration. At the national scale, urban area and soil clay content show significant negative correlations with POC concentration, whereas soil water content and soil bulk density correlate positively with POC. In addition, total phosphorus concentration and dam density correlate positively with POC concentration. 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subjects Carbon - analysis
Carbon Cycle
Environmental control
environmental factors
Environmental Monitoring
Fresh Water - chemistry
Humic Substances - analysis
Particulate organic carbon
riverine carbon
Spatial variability
Uncertainty
United States
Water Pollutants - analysis
title Spatial patterns and environmental controls of particulate organic carbon in surface waters in the conterminous United States
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