Fire retardant and post-fire nutrient mobility in a mountain surface water—karst groundwater system: the Hidden Fire, Sequoia National Park, California, USA
Abstract Nutrient mobility in strongly coupled surface water–groundwater systems is not well studied in fire dominated ecosystems. In 2008, the Hidden Fire in the Kaweah River basin in the Sierra Nevada, CA, USA provided an unexpected opportunity to document how nutrient concentrations change post-f...
Ausführliche Beschreibung
Autor*in: |
Tobin, Benjamin W. [verfasserIn] |
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Format: |
E-Artikel |
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Sprache: |
Englisch |
Erschienen: |
2014 |
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Schlagwörter: |
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Anmerkung: |
© Springer-Verlag Berlin Heidelberg 2014 |
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Übergeordnetes Werk: |
Enthalten in: Environmental earth sciences - Berlin : Springer, 2009, 73(2014), 3 vom: 03. Juli, Seite 951-960 |
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Übergeordnetes Werk: |
volume:73 ; year:2014 ; number:3 ; day:03 ; month:07 ; pages:951-960 |
Links: |
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DOI / URN: |
10.1007/s12665-014-3444-x |
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Katalog-ID: |
SPR026703904 |
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520 | |a Abstract Nutrient mobility in strongly coupled surface water–groundwater systems is not well studied in fire dominated ecosystems. In 2008, the Hidden Fire in the Kaweah River basin in the Sierra Nevada, CA, USA provided an unexpected opportunity to document how nutrient concentrations change post-fire in a karstic groundwater—surface water system. The results from 4 years of sampling and water quality data (2009–2012) suggest that nutrient byproducts from 94 Phos-Check D75 R fire retardant that was dropped to combat the fire were mobilized into the aquatic system. Dissolved nitrate concentrations sharply increased at most monitoring sites with the onset of winter precipitation and seasonal snowmelt in the spring of 2009, remained elevated during seasonal sampling at some sites in 2010, and were significantly lower in 2011 and 2012. Average nitrate concentrations in sub-basins during the 2009 high-discharge period are strongly correlated with the amount of retardant applied in each sub-basin, but not correlated with the sub-basin area. Dissolved phosphate concentrations were highest upstream of sink points where streams directly recharge marble karst aquifers, and decreased between recharge sites and springs; indicating organic and/or inorganic uptake of P in the subterranean system. Although measured nutrient concentrations were within the range documented post-fire in other aquatic systems that did not receive fire retardant, evidence from the Hidden Fire strongly suggests that fire retardant derived nutrients entered and flushed through the Yucca Creek system, and that managers should consider the potential impacts of retardant application on aquatic ecosystems even when retardant is not applied directly on waterways . | ||
650 | 4 | |a Fire effects |7 (dpeaa)DE-He213 | |
650 | 4 | |a Mountain hydrogeology |7 (dpeaa)DE-He213 | |
650 | 4 | |a Nutrient mobility |7 (dpeaa)DE-He213 | |
650 | 4 | |a Karst |7 (dpeaa)DE-He213 | |
650 | 4 | |a Fire retardant |7 (dpeaa)DE-He213 | |
700 | 1 | |a Schwartz, Benjamin F. |4 aut | |
700 | 1 | |a Kelly, Marissa |4 aut | |
700 | 1 | |a Despain, Joel D. |4 aut | |
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10.1007/s12665-014-3444-x doi (DE-627)SPR026703904 (SPR)s12665-014-3444-x-e DE-627 ger DE-627 rakwb eng Tobin, Benjamin W. verfasserin aut Fire retardant and post-fire nutrient mobility in a mountain surface water—karst groundwater system: the Hidden Fire, Sequoia National Park, California, USA 2014 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag Berlin Heidelberg 2014 Abstract Nutrient mobility in strongly coupled surface water–groundwater systems is not well studied in fire dominated ecosystems. In 2008, the Hidden Fire in the Kaweah River basin in the Sierra Nevada, CA, USA provided an unexpected opportunity to document how nutrient concentrations change post-fire in a karstic groundwater—surface water system. The results from 4 years of sampling and water quality data (2009–2012) suggest that nutrient byproducts from 94 Phos-Check D75 R fire retardant that was dropped to combat the fire were mobilized into the aquatic system. Dissolved nitrate concentrations sharply increased at most monitoring sites with the onset of winter precipitation and seasonal snowmelt in the spring of 2009, remained elevated during seasonal sampling at some sites in 2010, and were significantly lower in 2011 and 2012. Average nitrate concentrations in sub-basins during the 2009 high-discharge period are strongly correlated with the amount of retardant applied in each sub-basin, but not correlated with the sub-basin area. Dissolved phosphate concentrations were highest upstream of sink points where streams directly recharge marble karst aquifers, and decreased between recharge sites and springs; indicating organic and/or inorganic uptake of P in the subterranean system. Although measured nutrient concentrations were within the range documented post-fire in other aquatic systems that did not receive fire retardant, evidence from the Hidden Fire strongly suggests that fire retardant derived nutrients entered and flushed through the Yucca Creek system, and that managers should consider the potential impacts of retardant application on aquatic ecosystems even when retardant is not applied directly on waterways . Fire effects (dpeaa)DE-He213 Mountain hydrogeology (dpeaa)DE-He213 Nutrient mobility (dpeaa)DE-He213 Karst (dpeaa)DE-He213 Fire retardant (dpeaa)DE-He213 Schwartz, Benjamin F. aut Kelly, Marissa aut Despain, Joel D. aut Enthalten in Environmental earth sciences Berlin : Springer, 2009 73(2014), 3 vom: 03. Juli, Seite 951-960 (DE-627)599673451 (DE-600)2493699-6 1866-6299 nnns volume:73 year:2014 number:3 day:03 month:07 pages:951-960 https://dx.doi.org/10.1007/s12665-014-3444-x 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_65 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_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_2008 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_2360 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 73 2014 3 03 07 951-960 |
spelling |
10.1007/s12665-014-3444-x doi (DE-627)SPR026703904 (SPR)s12665-014-3444-x-e DE-627 ger DE-627 rakwb eng Tobin, Benjamin W. verfasserin aut Fire retardant and post-fire nutrient mobility in a mountain surface water—karst groundwater system: the Hidden Fire, Sequoia National Park, California, USA 2014 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag Berlin Heidelberg 2014 Abstract Nutrient mobility in strongly coupled surface water–groundwater systems is not well studied in fire dominated ecosystems. In 2008, the Hidden Fire in the Kaweah River basin in the Sierra Nevada, CA, USA provided an unexpected opportunity to document how nutrient concentrations change post-fire in a karstic groundwater—surface water system. The results from 4 years of sampling and water quality data (2009–2012) suggest that nutrient byproducts from 94 Phos-Check D75 R fire retardant that was dropped to combat the fire were mobilized into the aquatic system. Dissolved nitrate concentrations sharply increased at most monitoring sites with the onset of winter precipitation and seasonal snowmelt in the spring of 2009, remained elevated during seasonal sampling at some sites in 2010, and were significantly lower in 2011 and 2012. Average nitrate concentrations in sub-basins during the 2009 high-discharge period are strongly correlated with the amount of retardant applied in each sub-basin, but not correlated with the sub-basin area. Dissolved phosphate concentrations were highest upstream of sink points where streams directly recharge marble karst aquifers, and decreased between recharge sites and springs; indicating organic and/or inorganic uptake of P in the subterranean system. Although measured nutrient concentrations were within the range documented post-fire in other aquatic systems that did not receive fire retardant, evidence from the Hidden Fire strongly suggests that fire retardant derived nutrients entered and flushed through the Yucca Creek system, and that managers should consider the potential impacts of retardant application on aquatic ecosystems even when retardant is not applied directly on waterways . Fire effects (dpeaa)DE-He213 Mountain hydrogeology (dpeaa)DE-He213 Nutrient mobility (dpeaa)DE-He213 Karst (dpeaa)DE-He213 Fire retardant (dpeaa)DE-He213 Schwartz, Benjamin F. aut Kelly, Marissa aut Despain, Joel D. aut Enthalten in Environmental earth sciences Berlin : Springer, 2009 73(2014), 3 vom: 03. Juli, Seite 951-960 (DE-627)599673451 (DE-600)2493699-6 1866-6299 nnns volume:73 year:2014 number:3 day:03 month:07 pages:951-960 https://dx.doi.org/10.1007/s12665-014-3444-x 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_65 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_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_2008 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_2360 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 73 2014 3 03 07 951-960 |
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10.1007/s12665-014-3444-x doi (DE-627)SPR026703904 (SPR)s12665-014-3444-x-e DE-627 ger DE-627 rakwb eng Tobin, Benjamin W. verfasserin aut Fire retardant and post-fire nutrient mobility in a mountain surface water—karst groundwater system: the Hidden Fire, Sequoia National Park, California, USA 2014 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag Berlin Heidelberg 2014 Abstract Nutrient mobility in strongly coupled surface water–groundwater systems is not well studied in fire dominated ecosystems. In 2008, the Hidden Fire in the Kaweah River basin in the Sierra Nevada, CA, USA provided an unexpected opportunity to document how nutrient concentrations change post-fire in a karstic groundwater—surface water system. The results from 4 years of sampling and water quality data (2009–2012) suggest that nutrient byproducts from 94 Phos-Check D75 R fire retardant that was dropped to combat the fire were mobilized into the aquatic system. Dissolved nitrate concentrations sharply increased at most monitoring sites with the onset of winter precipitation and seasonal snowmelt in the spring of 2009, remained elevated during seasonal sampling at some sites in 2010, and were significantly lower in 2011 and 2012. Average nitrate concentrations in sub-basins during the 2009 high-discharge period are strongly correlated with the amount of retardant applied in each sub-basin, but not correlated with the sub-basin area. Dissolved phosphate concentrations were highest upstream of sink points where streams directly recharge marble karst aquifers, and decreased between recharge sites and springs; indicating organic and/or inorganic uptake of P in the subterranean system. Although measured nutrient concentrations were within the range documented post-fire in other aquatic systems that did not receive fire retardant, evidence from the Hidden Fire strongly suggests that fire retardant derived nutrients entered and flushed through the Yucca Creek system, and that managers should consider the potential impacts of retardant application on aquatic ecosystems even when retardant is not applied directly on waterways . Fire effects (dpeaa)DE-He213 Mountain hydrogeology (dpeaa)DE-He213 Nutrient mobility (dpeaa)DE-He213 Karst (dpeaa)DE-He213 Fire retardant (dpeaa)DE-He213 Schwartz, Benjamin F. aut Kelly, Marissa aut Despain, Joel D. aut Enthalten in Environmental earth sciences Berlin : Springer, 2009 73(2014), 3 vom: 03. Juli, Seite 951-960 (DE-627)599673451 (DE-600)2493699-6 1866-6299 nnns volume:73 year:2014 number:3 day:03 month:07 pages:951-960 https://dx.doi.org/10.1007/s12665-014-3444-x 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_65 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_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_2008 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_2360 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 73 2014 3 03 07 951-960 |
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10.1007/s12665-014-3444-x doi (DE-627)SPR026703904 (SPR)s12665-014-3444-x-e DE-627 ger DE-627 rakwb eng Tobin, Benjamin W. verfasserin aut Fire retardant and post-fire nutrient mobility in a mountain surface water—karst groundwater system: the Hidden Fire, Sequoia National Park, California, USA 2014 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag Berlin Heidelberg 2014 Abstract Nutrient mobility in strongly coupled surface water–groundwater systems is not well studied in fire dominated ecosystems. In 2008, the Hidden Fire in the Kaweah River basin in the Sierra Nevada, CA, USA provided an unexpected opportunity to document how nutrient concentrations change post-fire in a karstic groundwater—surface water system. The results from 4 years of sampling and water quality data (2009–2012) suggest that nutrient byproducts from 94 Phos-Check D75 R fire retardant that was dropped to combat the fire were mobilized into the aquatic system. Dissolved nitrate concentrations sharply increased at most monitoring sites with the onset of winter precipitation and seasonal snowmelt in the spring of 2009, remained elevated during seasonal sampling at some sites in 2010, and were significantly lower in 2011 and 2012. Average nitrate concentrations in sub-basins during the 2009 high-discharge period are strongly correlated with the amount of retardant applied in each sub-basin, but not correlated with the sub-basin area. Dissolved phosphate concentrations were highest upstream of sink points where streams directly recharge marble karst aquifers, and decreased between recharge sites and springs; indicating organic and/or inorganic uptake of P in the subterranean system. Although measured nutrient concentrations were within the range documented post-fire in other aquatic systems that did not receive fire retardant, evidence from the Hidden Fire strongly suggests that fire retardant derived nutrients entered and flushed through the Yucca Creek system, and that managers should consider the potential impacts of retardant application on aquatic ecosystems even when retardant is not applied directly on waterways . Fire effects (dpeaa)DE-He213 Mountain hydrogeology (dpeaa)DE-He213 Nutrient mobility (dpeaa)DE-He213 Karst (dpeaa)DE-He213 Fire retardant (dpeaa)DE-He213 Schwartz, Benjamin F. aut Kelly, Marissa aut Despain, Joel D. aut Enthalten in Environmental earth sciences Berlin : Springer, 2009 73(2014), 3 vom: 03. Juli, Seite 951-960 (DE-627)599673451 (DE-600)2493699-6 1866-6299 nnns volume:73 year:2014 number:3 day:03 month:07 pages:951-960 https://dx.doi.org/10.1007/s12665-014-3444-x 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_65 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_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_2008 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_2360 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 73 2014 3 03 07 951-960 |
allfieldsSound |
10.1007/s12665-014-3444-x doi (DE-627)SPR026703904 (SPR)s12665-014-3444-x-e DE-627 ger DE-627 rakwb eng Tobin, Benjamin W. verfasserin aut Fire retardant and post-fire nutrient mobility in a mountain surface water—karst groundwater system: the Hidden Fire, Sequoia National Park, California, USA 2014 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag Berlin Heidelberg 2014 Abstract Nutrient mobility in strongly coupled surface water–groundwater systems is not well studied in fire dominated ecosystems. In 2008, the Hidden Fire in the Kaweah River basin in the Sierra Nevada, CA, USA provided an unexpected opportunity to document how nutrient concentrations change post-fire in a karstic groundwater—surface water system. The results from 4 years of sampling and water quality data (2009–2012) suggest that nutrient byproducts from 94 Phos-Check D75 R fire retardant that was dropped to combat the fire were mobilized into the aquatic system. Dissolved nitrate concentrations sharply increased at most monitoring sites with the onset of winter precipitation and seasonal snowmelt in the spring of 2009, remained elevated during seasonal sampling at some sites in 2010, and were significantly lower in 2011 and 2012. Average nitrate concentrations in sub-basins during the 2009 high-discharge period are strongly correlated with the amount of retardant applied in each sub-basin, but not correlated with the sub-basin area. Dissolved phosphate concentrations were highest upstream of sink points where streams directly recharge marble karst aquifers, and decreased between recharge sites and springs; indicating organic and/or inorganic uptake of P in the subterranean system. Although measured nutrient concentrations were within the range documented post-fire in other aquatic systems that did not receive fire retardant, evidence from the Hidden Fire strongly suggests that fire retardant derived nutrients entered and flushed through the Yucca Creek system, and that managers should consider the potential impacts of retardant application on aquatic ecosystems even when retardant is not applied directly on waterways . Fire effects (dpeaa)DE-He213 Mountain hydrogeology (dpeaa)DE-He213 Nutrient mobility (dpeaa)DE-He213 Karst (dpeaa)DE-He213 Fire retardant (dpeaa)DE-He213 Schwartz, Benjamin F. aut Kelly, Marissa aut Despain, Joel D. aut Enthalten in Environmental earth sciences Berlin : Springer, 2009 73(2014), 3 vom: 03. Juli, Seite 951-960 (DE-627)599673451 (DE-600)2493699-6 1866-6299 nnns volume:73 year:2014 number:3 day:03 month:07 pages:951-960 https://dx.doi.org/10.1007/s12665-014-3444-x 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_65 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_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_2008 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_2360 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 73 2014 3 03 07 951-960 |
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Enthalten in Environmental earth sciences 73(2014), 3 vom: 03. Juli, Seite 951-960 volume:73 year:2014 number:3 day:03 month:07 pages:951-960 |
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Tobin, Benjamin W. @@aut@@ Schwartz, Benjamin F. @@aut@@ Kelly, Marissa @@aut@@ Despain, Joel D. @@aut@@ |
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In 2008, the Hidden Fire in the Kaweah River basin in the Sierra Nevada, CA, USA provided an unexpected opportunity to document how nutrient concentrations change post-fire in a karstic groundwater—surface water system. The results from 4 years of sampling and water quality data (2009–2012) suggest that nutrient byproducts from 94 Phos-Check D75 R fire retardant that was dropped to combat the fire were mobilized into the aquatic system. Dissolved nitrate concentrations sharply increased at most monitoring sites with the onset of winter precipitation and seasonal snowmelt in the spring of 2009, remained elevated during seasonal sampling at some sites in 2010, and were significantly lower in 2011 and 2012. Average nitrate concentrations in sub-basins during the 2009 high-discharge period are strongly correlated with the amount of retardant applied in each sub-basin, but not correlated with the sub-basin area. Dissolved phosphate concentrations were highest upstream of sink points where streams directly recharge marble karst aquifers, and decreased between recharge sites and springs; indicating organic and/or inorganic uptake of P in the subterranean system. 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Tobin, Benjamin W. |
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Tobin, Benjamin W. misc Fire effects misc Mountain hydrogeology misc Nutrient mobility misc Karst misc Fire retardant Fire retardant and post-fire nutrient mobility in a mountain surface water—karst groundwater system: the Hidden Fire, Sequoia National Park, California, USA |
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Fire retardant and post-fire nutrient mobility in a mountain surface water—karst groundwater system: the Hidden Fire, Sequoia National Park, California, USA Fire effects (dpeaa)DE-He213 Mountain hydrogeology (dpeaa)DE-He213 Nutrient mobility (dpeaa)DE-He213 Karst (dpeaa)DE-He213 Fire retardant (dpeaa)DE-He213 |
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Fire retardant and post-fire nutrient mobility in a mountain surface water—karst groundwater system: the Hidden Fire, Sequoia National Park, California, USA |
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Fire retardant and post-fire nutrient mobility in a mountain surface water—karst groundwater system: the Hidden Fire, Sequoia National Park, California, USA |
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fire retardant and post-fire nutrient mobility in a mountain surface water—karst groundwater system: the hidden fire, sequoia national park, california, usa |
title_auth |
Fire retardant and post-fire nutrient mobility in a mountain surface water—karst groundwater system: the Hidden Fire, Sequoia National Park, California, USA |
abstract |
Abstract Nutrient mobility in strongly coupled surface water–groundwater systems is not well studied in fire dominated ecosystems. In 2008, the Hidden Fire in the Kaweah River basin in the Sierra Nevada, CA, USA provided an unexpected opportunity to document how nutrient concentrations change post-fire in a karstic groundwater—surface water system. The results from 4 years of sampling and water quality data (2009–2012) suggest that nutrient byproducts from 94 Phos-Check D75 R fire retardant that was dropped to combat the fire were mobilized into the aquatic system. Dissolved nitrate concentrations sharply increased at most monitoring sites with the onset of winter precipitation and seasonal snowmelt in the spring of 2009, remained elevated during seasonal sampling at some sites in 2010, and were significantly lower in 2011 and 2012. Average nitrate concentrations in sub-basins during the 2009 high-discharge period are strongly correlated with the amount of retardant applied in each sub-basin, but not correlated with the sub-basin area. Dissolved phosphate concentrations were highest upstream of sink points where streams directly recharge marble karst aquifers, and decreased between recharge sites and springs; indicating organic and/or inorganic uptake of P in the subterranean system. Although measured nutrient concentrations were within the range documented post-fire in other aquatic systems that did not receive fire retardant, evidence from the Hidden Fire strongly suggests that fire retardant derived nutrients entered and flushed through the Yucca Creek system, and that managers should consider the potential impacts of retardant application on aquatic ecosystems even when retardant is not applied directly on waterways . © Springer-Verlag Berlin Heidelberg 2014 |
abstractGer |
Abstract Nutrient mobility in strongly coupled surface water–groundwater systems is not well studied in fire dominated ecosystems. In 2008, the Hidden Fire in the Kaweah River basin in the Sierra Nevada, CA, USA provided an unexpected opportunity to document how nutrient concentrations change post-fire in a karstic groundwater—surface water system. The results from 4 years of sampling and water quality data (2009–2012) suggest that nutrient byproducts from 94 Phos-Check D75 R fire retardant that was dropped to combat the fire were mobilized into the aquatic system. Dissolved nitrate concentrations sharply increased at most monitoring sites with the onset of winter precipitation and seasonal snowmelt in the spring of 2009, remained elevated during seasonal sampling at some sites in 2010, and were significantly lower in 2011 and 2012. Average nitrate concentrations in sub-basins during the 2009 high-discharge period are strongly correlated with the amount of retardant applied in each sub-basin, but not correlated with the sub-basin area. Dissolved phosphate concentrations were highest upstream of sink points where streams directly recharge marble karst aquifers, and decreased between recharge sites and springs; indicating organic and/or inorganic uptake of P in the subterranean system. Although measured nutrient concentrations were within the range documented post-fire in other aquatic systems that did not receive fire retardant, evidence from the Hidden Fire strongly suggests that fire retardant derived nutrients entered and flushed through the Yucca Creek system, and that managers should consider the potential impacts of retardant application on aquatic ecosystems even when retardant is not applied directly on waterways . © Springer-Verlag Berlin Heidelberg 2014 |
abstract_unstemmed |
Abstract Nutrient mobility in strongly coupled surface water–groundwater systems is not well studied in fire dominated ecosystems. In 2008, the Hidden Fire in the Kaweah River basin in the Sierra Nevada, CA, USA provided an unexpected opportunity to document how nutrient concentrations change post-fire in a karstic groundwater—surface water system. The results from 4 years of sampling and water quality data (2009–2012) suggest that nutrient byproducts from 94 Phos-Check D75 R fire retardant that was dropped to combat the fire were mobilized into the aquatic system. Dissolved nitrate concentrations sharply increased at most monitoring sites with the onset of winter precipitation and seasonal snowmelt in the spring of 2009, remained elevated during seasonal sampling at some sites in 2010, and were significantly lower in 2011 and 2012. Average nitrate concentrations in sub-basins during the 2009 high-discharge period are strongly correlated with the amount of retardant applied in each sub-basin, but not correlated with the sub-basin area. Dissolved phosphate concentrations were highest upstream of sink points where streams directly recharge marble karst aquifers, and decreased between recharge sites and springs; indicating organic and/or inorganic uptake of P in the subterranean system. Although measured nutrient concentrations were within the range documented post-fire in other aquatic systems that did not receive fire retardant, evidence from the Hidden Fire strongly suggests that fire retardant derived nutrients entered and flushed through the Yucca Creek system, and that managers should consider the potential impacts of retardant application on aquatic ecosystems even when retardant is not applied directly on waterways . © Springer-Verlag Berlin Heidelberg 2014 |
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title_short |
Fire retardant and post-fire nutrient mobility in a mountain surface water—karst groundwater system: the Hidden Fire, Sequoia National Park, California, USA |
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https://dx.doi.org/10.1007/s12665-014-3444-x |
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Schwartz, Benjamin F. Kelly, Marissa Despain, Joel D. |
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up_date |
2024-07-03T22:16:01.580Z |
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score |
7.4008617 |