Organic carbon spiraling in an Idaho river
Abstract. In running water ecosystems, the use of community attributes to infer biological integrity is widespread. In contrast, functional variables like energy flow and elemental cycling have received considerably less attention. In this study, we quantify organic carbon spiraling in four reaches...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Thomas, Steven A. [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2005 |
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| Anmerkung: |
© Eawag 2005 |
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| Übergeordnetes Werk: |
Enthalten in: Aquatic sciences - Basel : Springer, 1920, 67(2005), 4 vom: 30. Nov., Seite 424-433 |
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| Übergeordnetes Werk: |
volume:67 ; year:2005 ; number:4 ; day:30 ; month:11 ; pages:424-433 |
| Links: |
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| DOI / URN: |
10.1007/s00027-005-0790-5 |
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| Katalog-ID: |
SPR000288721 |
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| 100 | 1 | |a Thomas, Steven A. |e verfasserin |4 aut | |
| 245 | 1 | 0 | |a Organic carbon spiraling in an Idaho river |
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| 520 | |a Abstract. In running water ecosystems, the use of community attributes to infer biological integrity is widespread. In contrast, functional variables like energy flow and elemental cycling have received considerably less attention. In this study, we quantify organic carbon spiraling in four reaches of the Middle Snake River (MSR). We calculated organic carbon (OC) turnover rates ($ K_{OC} $), mean velocities ($ V_{OC} $), and turnover lengths ($ S_{OC} $) by quantifying suspended and benthic pools of organic carbon and measuring metabolic rates using both open-system and chamber approaches. Ultra-fine particulate organic carbon (UPOC) dominated both transported and benthic OC in all study reaches. $ K_{OC} $ was lowest where benthic standing stocks were greatest and $ K_{OC} $ was elevated in summer relative to spring and fall. $ V_{OC} $ was negatively correlated with benthic OC standing stock and greatest in spring and early summer when river discharge was highest. Turnover lengths ($ S_{OC} $) ranged from 11–108 km and were strongly related to temporal patterns in $ V_{OC} $. Comparison of the Snake River with other river systems suggests that MSR is more retentive and homogeneous than rivers of similar size in North America. | ||
| 700 | 1 | |a Royer, Todd V. |4 aut | |
| 700 | 1 | |a Snyder, Eric B. |4 aut | |
| 700 | 1 | |a Davis, Jeffrey C. |4 aut | |
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10.1007/s00027-005-0790-5 doi (DE-627)SPR000288721 (SPR)s00027-005-0790-5-e DE-627 ger DE-627 rakwb eng Thomas, Steven A. verfasserin aut Organic carbon spiraling in an Idaho river 2005 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Eawag 2005 Abstract. In running water ecosystems, the use of community attributes to infer biological integrity is widespread. In contrast, functional variables like energy flow and elemental cycling have received considerably less attention. In this study, we quantify organic carbon spiraling in four reaches of the Middle Snake River (MSR). We calculated organic carbon (OC) turnover rates ($ K_{OC} $), mean velocities ($ V_{OC} $), and turnover lengths ($ S_{OC} $) by quantifying suspended and benthic pools of organic carbon and measuring metabolic rates using both open-system and chamber approaches. Ultra-fine particulate organic carbon (UPOC) dominated both transported and benthic OC in all study reaches. $ K_{OC} $ was lowest where benthic standing stocks were greatest and $ K_{OC} $ was elevated in summer relative to spring and fall. $ V_{OC} $ was negatively correlated with benthic OC standing stock and greatest in spring and early summer when river discharge was highest. Turnover lengths ($ S_{OC} $) ranged from 11–108 km and were strongly related to temporal patterns in $ V_{OC} $. Comparison of the Snake River with other river systems suggests that MSR is more retentive and homogeneous than rivers of similar size in North America. Royer, Todd V. aut Snyder, Eric B. aut Davis, Jeffrey C. aut Enthalten in Aquatic sciences Basel : Springer, 1920 67(2005), 4 vom: 30. Nov., Seite 424-433 (DE-627)265506670 (DE-600)1464021-1 1420-9055 nnns volume:67 year:2005 number:4 day:30 month:11 pages:424-433 https://dx.doi.org/10.1007/s00027-005-0790-5 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 67 2005 4 30 11 424-433 |
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10.1007/s00027-005-0790-5 doi (DE-627)SPR000288721 (SPR)s00027-005-0790-5-e DE-627 ger DE-627 rakwb eng Thomas, Steven A. verfasserin aut Organic carbon spiraling in an Idaho river 2005 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Eawag 2005 Abstract. In running water ecosystems, the use of community attributes to infer biological integrity is widespread. In contrast, functional variables like energy flow and elemental cycling have received considerably less attention. In this study, we quantify organic carbon spiraling in four reaches of the Middle Snake River (MSR). We calculated organic carbon (OC) turnover rates ($ K_{OC} $), mean velocities ($ V_{OC} $), and turnover lengths ($ S_{OC} $) by quantifying suspended and benthic pools of organic carbon and measuring metabolic rates using both open-system and chamber approaches. Ultra-fine particulate organic carbon (UPOC) dominated both transported and benthic OC in all study reaches. $ K_{OC} $ was lowest where benthic standing stocks were greatest and $ K_{OC} $ was elevated in summer relative to spring and fall. $ V_{OC} $ was negatively correlated with benthic OC standing stock and greatest in spring and early summer when river discharge was highest. Turnover lengths ($ S_{OC} $) ranged from 11–108 km and were strongly related to temporal patterns in $ V_{OC} $. Comparison of the Snake River with other river systems suggests that MSR is more retentive and homogeneous than rivers of similar size in North America. Royer, Todd V. aut Snyder, Eric B. aut Davis, Jeffrey C. aut Enthalten in Aquatic sciences Basel : Springer, 1920 67(2005), 4 vom: 30. Nov., Seite 424-433 (DE-627)265506670 (DE-600)1464021-1 1420-9055 nnns volume:67 year:2005 number:4 day:30 month:11 pages:424-433 https://dx.doi.org/10.1007/s00027-005-0790-5 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 67 2005 4 30 11 424-433 |
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10.1007/s00027-005-0790-5 doi (DE-627)SPR000288721 (SPR)s00027-005-0790-5-e DE-627 ger DE-627 rakwb eng Thomas, Steven A. verfasserin aut Organic carbon spiraling in an Idaho river 2005 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Eawag 2005 Abstract. In running water ecosystems, the use of community attributes to infer biological integrity is widespread. In contrast, functional variables like energy flow and elemental cycling have received considerably less attention. In this study, we quantify organic carbon spiraling in four reaches of the Middle Snake River (MSR). We calculated organic carbon (OC) turnover rates ($ K_{OC} $), mean velocities ($ V_{OC} $), and turnover lengths ($ S_{OC} $) by quantifying suspended and benthic pools of organic carbon and measuring metabolic rates using both open-system and chamber approaches. Ultra-fine particulate organic carbon (UPOC) dominated both transported and benthic OC in all study reaches. $ K_{OC} $ was lowest where benthic standing stocks were greatest and $ K_{OC} $ was elevated in summer relative to spring and fall. $ V_{OC} $ was negatively correlated with benthic OC standing stock and greatest in spring and early summer when river discharge was highest. Turnover lengths ($ S_{OC} $) ranged from 11–108 km and were strongly related to temporal patterns in $ V_{OC} $. Comparison of the Snake River with other river systems suggests that MSR is more retentive and homogeneous than rivers of similar size in North America. Royer, Todd V. aut Snyder, Eric B. aut Davis, Jeffrey C. aut Enthalten in Aquatic sciences Basel : Springer, 1920 67(2005), 4 vom: 30. Nov., Seite 424-433 (DE-627)265506670 (DE-600)1464021-1 1420-9055 nnns volume:67 year:2005 number:4 day:30 month:11 pages:424-433 https://dx.doi.org/10.1007/s00027-005-0790-5 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 67 2005 4 30 11 424-433 |
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10.1007/s00027-005-0790-5 doi (DE-627)SPR000288721 (SPR)s00027-005-0790-5-e DE-627 ger DE-627 rakwb eng Thomas, Steven A. verfasserin aut Organic carbon spiraling in an Idaho river 2005 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Eawag 2005 Abstract. In running water ecosystems, the use of community attributes to infer biological integrity is widespread. In contrast, functional variables like energy flow and elemental cycling have received considerably less attention. In this study, we quantify organic carbon spiraling in four reaches of the Middle Snake River (MSR). We calculated organic carbon (OC) turnover rates ($ K_{OC} $), mean velocities ($ V_{OC} $), and turnover lengths ($ S_{OC} $) by quantifying suspended and benthic pools of organic carbon and measuring metabolic rates using both open-system and chamber approaches. Ultra-fine particulate organic carbon (UPOC) dominated both transported and benthic OC in all study reaches. $ K_{OC} $ was lowest where benthic standing stocks were greatest and $ K_{OC} $ was elevated in summer relative to spring and fall. $ V_{OC} $ was negatively correlated with benthic OC standing stock and greatest in spring and early summer when river discharge was highest. Turnover lengths ($ S_{OC} $) ranged from 11–108 km and were strongly related to temporal patterns in $ V_{OC} $. Comparison of the Snake River with other river systems suggests that MSR is more retentive and homogeneous than rivers of similar size in North America. Royer, Todd V. aut Snyder, Eric B. aut Davis, Jeffrey C. aut Enthalten in Aquatic sciences Basel : Springer, 1920 67(2005), 4 vom: 30. Nov., Seite 424-433 (DE-627)265506670 (DE-600)1464021-1 1420-9055 nnns volume:67 year:2005 number:4 day:30 month:11 pages:424-433 https://dx.doi.org/10.1007/s00027-005-0790-5 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 67 2005 4 30 11 424-433 |
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10.1007/s00027-005-0790-5 doi (DE-627)SPR000288721 (SPR)s00027-005-0790-5-e DE-627 ger DE-627 rakwb eng Thomas, Steven A. verfasserin aut Organic carbon spiraling in an Idaho river 2005 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Eawag 2005 Abstract. In running water ecosystems, the use of community attributes to infer biological integrity is widespread. In contrast, functional variables like energy flow and elemental cycling have received considerably less attention. In this study, we quantify organic carbon spiraling in four reaches of the Middle Snake River (MSR). We calculated organic carbon (OC) turnover rates ($ K_{OC} $), mean velocities ($ V_{OC} $), and turnover lengths ($ S_{OC} $) by quantifying suspended and benthic pools of organic carbon and measuring metabolic rates using both open-system and chamber approaches. Ultra-fine particulate organic carbon (UPOC) dominated both transported and benthic OC in all study reaches. $ K_{OC} $ was lowest where benthic standing stocks were greatest and $ K_{OC} $ was elevated in summer relative to spring and fall. $ V_{OC} $ was negatively correlated with benthic OC standing stock and greatest in spring and early summer when river discharge was highest. Turnover lengths ($ S_{OC} $) ranged from 11–108 km and were strongly related to temporal patterns in $ V_{OC} $. Comparison of the Snake River with other river systems suggests that MSR is more retentive and homogeneous than rivers of similar size in North America. Royer, Todd V. aut Snyder, Eric B. aut Davis, Jeffrey C. aut Enthalten in Aquatic sciences Basel : Springer, 1920 67(2005), 4 vom: 30. Nov., Seite 424-433 (DE-627)265506670 (DE-600)1464021-1 1420-9055 nnns volume:67 year:2005 number:4 day:30 month:11 pages:424-433 https://dx.doi.org/10.1007/s00027-005-0790-5 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 67 2005 4 30 11 424-433 |
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Thomas, Steven A. @@aut@@ Royer, Todd V. @@aut@@ Snyder, Eric B. @@aut@@ Davis, Jeffrey C. @@aut@@ |
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Thomas, Steven A. Organic carbon spiraling in an Idaho river |
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organic carbon spiraling in an idaho river |
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Organic carbon spiraling in an Idaho river |
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Abstract. In running water ecosystems, the use of community attributes to infer biological integrity is widespread. In contrast, functional variables like energy flow and elemental cycling have received considerably less attention. In this study, we quantify organic carbon spiraling in four reaches of the Middle Snake River (MSR). We calculated organic carbon (OC) turnover rates ($ K_{OC} $), mean velocities ($ V_{OC} $), and turnover lengths ($ S_{OC} $) by quantifying suspended and benthic pools of organic carbon and measuring metabolic rates using both open-system and chamber approaches. Ultra-fine particulate organic carbon (UPOC) dominated both transported and benthic OC in all study reaches. $ K_{OC} $ was lowest where benthic standing stocks were greatest and $ K_{OC} $ was elevated in summer relative to spring and fall. $ V_{OC} $ was negatively correlated with benthic OC standing stock and greatest in spring and early summer when river discharge was highest. Turnover lengths ($ S_{OC} $) ranged from 11–108 km and were strongly related to temporal patterns in $ V_{OC} $. Comparison of the Snake River with other river systems suggests that MSR is more retentive and homogeneous than rivers of similar size in North America. © Eawag 2005 |
| abstractGer |
Abstract. In running water ecosystems, the use of community attributes to infer biological integrity is widespread. In contrast, functional variables like energy flow and elemental cycling have received considerably less attention. In this study, we quantify organic carbon spiraling in four reaches of the Middle Snake River (MSR). We calculated organic carbon (OC) turnover rates ($ K_{OC} $), mean velocities ($ V_{OC} $), and turnover lengths ($ S_{OC} $) by quantifying suspended and benthic pools of organic carbon and measuring metabolic rates using both open-system and chamber approaches. Ultra-fine particulate organic carbon (UPOC) dominated both transported and benthic OC in all study reaches. $ K_{OC} $ was lowest where benthic standing stocks were greatest and $ K_{OC} $ was elevated in summer relative to spring and fall. $ V_{OC} $ was negatively correlated with benthic OC standing stock and greatest in spring and early summer when river discharge was highest. Turnover lengths ($ S_{OC} $) ranged from 11–108 km and were strongly related to temporal patterns in $ V_{OC} $. Comparison of the Snake River with other river systems suggests that MSR is more retentive and homogeneous than rivers of similar size in North America. © Eawag 2005 |
| abstract_unstemmed |
Abstract. In running water ecosystems, the use of community attributes to infer biological integrity is widespread. In contrast, functional variables like energy flow and elemental cycling have received considerably less attention. In this study, we quantify organic carbon spiraling in four reaches of the Middle Snake River (MSR). We calculated organic carbon (OC) turnover rates ($ K_{OC} $), mean velocities ($ V_{OC} $), and turnover lengths ($ S_{OC} $) by quantifying suspended and benthic pools of organic carbon and measuring metabolic rates using both open-system and chamber approaches. Ultra-fine particulate organic carbon (UPOC) dominated both transported and benthic OC in all study reaches. $ K_{OC} $ was lowest where benthic standing stocks were greatest and $ K_{OC} $ was elevated in summer relative to spring and fall. $ V_{OC} $ was negatively correlated with benthic OC standing stock and greatest in spring and early summer when river discharge was highest. Turnover lengths ($ S_{OC} $) ranged from 11–108 km and were strongly related to temporal patterns in $ V_{OC} $. Comparison of the Snake River with other river systems suggests that MSR is more retentive and homogeneous than rivers of similar size in North America. © Eawag 2005 |
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10.1007/s00027-005-0790-5 |
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2024-07-03T15:07:31.691Z |
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