Dynamic monitoring of resuspension in the multiple eco-types of the littoral zone of a shallow wind-disturbed lake
Abstract Sedimentation and resuspension processes, are known to govern nutrient cycling and lake metabolic processes, but have not been well studied in littoral zones with multi-ecotypes of shallow wind-disturbed lakes. This time-series study used sediment traps to estimate the spatiotemporal change...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Qi, Chuang [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2019 |
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| Schlagwörter: |
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| Anmerkung: |
© Springer Nature Switzerland AG 2019 |
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| Übergeordnetes Werk: |
Enthalten in: Aquatic sciences - Basel : Springer, 1920, 81(2019), 2 vom: 18. Feb. |
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| Übergeordnetes Werk: |
volume:81 ; year:2019 ; number:2 ; day:18 ; month:02 |
| Links: |
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| DOI / URN: |
10.1007/s00027-019-0620-9 |
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| Katalog-ID: |
SPR000296368 |
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| 245 | 1 | 0 | |a Dynamic monitoring of resuspension in the multiple eco-types of the littoral zone of a shallow wind-disturbed lake |
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| 520 | |a Abstract Sedimentation and resuspension processes, are known to govern nutrient cycling and lake metabolic processes, but have not been well studied in littoral zones with multi-ecotypes of shallow wind-disturbed lakes. This time-series study used sediment traps to estimate the spatiotemporal changes in sedimentation and resuspension rates, during the four seasonal continuous deployment periods, in the littoral zone of Lake Taihu. The effect of sedimentation processes on nutrient accumulation was also investigated. Results showed that the sedimentation rates at six observation sites were highly variable, with gross sedimentation rates ranging from 184.83 to 2150.74 g $ m^{−2} $ $ day^{−1} $. Almost 88% of the total observed sedimentation originated from sediment resuspension. Cyanobacterial blooms coupled with the frequently changeable wind conditions in the littoral zone, were the key factors in lacustrine sediment redistribution and a large pool of organic material accumulated during cyanobacterial blooms. Moreover, the contribution of resuspended total phosphorous and total nitrogen to the water column, were 0.22 mg $ L^{−1} $ and 0.46 mg $ L^{−1} $, respectively. The high rate of rapid nutrient cycling observed at the sediment water interface due to resuspension, may be a key factor in maintaining eutrophication in large and shallow lakes, which is of high relevance to the future management of aquatic ecosystems. | ||
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| 650 | 4 | |a Sediment resuspension |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Sequential sediment trap |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Eutrophication lakes |7 (dpeaa)DE-He213 | |
| 700 | 1 | |a Zhou, Yang |4 aut | |
| 700 | 1 | |a Xu, Xiao-guang |4 aut | |
| 700 | 1 | |a Zhang, Li-min |4 aut | |
| 700 | 1 | |a Lin, Hui |4 aut | |
| 700 | 1 | |a Wu, Xin-ting |4 aut | |
| 700 | 1 | |a Shi, Kuan |4 aut | |
| 700 | 1 | |a Wang, Guo-xiang |4 aut | |
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10.1007/s00027-019-0620-9 doi (DE-627)SPR000296368 (SPR)s00027-019-0620-9-e DE-627 ger DE-627 rakwb eng Qi, Chuang verfasserin aut Dynamic monitoring of resuspension in the multiple eco-types of the littoral zone of a shallow wind-disturbed lake 2019 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer Nature Switzerland AG 2019 Abstract Sedimentation and resuspension processes, are known to govern nutrient cycling and lake metabolic processes, but have not been well studied in littoral zones with multi-ecotypes of shallow wind-disturbed lakes. This time-series study used sediment traps to estimate the spatiotemporal changes in sedimentation and resuspension rates, during the four seasonal continuous deployment periods, in the littoral zone of Lake Taihu. The effect of sedimentation processes on nutrient accumulation was also investigated. Results showed that the sedimentation rates at six observation sites were highly variable, with gross sedimentation rates ranging from 184.83 to 2150.74 g $ m^{−2} $ $ day^{−1} $. Almost 88% of the total observed sedimentation originated from sediment resuspension. Cyanobacterial blooms coupled with the frequently changeable wind conditions in the littoral zone, were the key factors in lacustrine sediment redistribution and a large pool of organic material accumulated during cyanobacterial blooms. Moreover, the contribution of resuspended total phosphorous and total nitrogen to the water column, were 0.22 mg $ L^{−1} $ and 0.46 mg $ L^{−1} $, respectively. The high rate of rapid nutrient cycling observed at the sediment water interface due to resuspension, may be a key factor in maintaining eutrophication in large and shallow lakes, which is of high relevance to the future management of aquatic ecosystems. Gross sedimentation (dpeaa)DE-He213 Sediment resuspension (dpeaa)DE-He213 Sequential sediment trap (dpeaa)DE-He213 Eutrophication lakes (dpeaa)DE-He213 Zhou, Yang aut Xu, Xiao-guang aut Zhang, Li-min aut Lin, Hui aut Wu, Xin-ting aut Shi, Kuan aut Wang, Guo-xiang aut Enthalten in Aquatic sciences Basel : Springer, 1920 81(2019), 2 vom: 18. Feb. (DE-627)265506670 (DE-600)1464021-1 1420-9055 nnns volume:81 year:2019 number:2 day:18 month:02 https://dx.doi.org/10.1007/s00027-019-0620-9 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_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 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 81 2019 2 18 02 |
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10.1007/s00027-019-0620-9 doi (DE-627)SPR000296368 (SPR)s00027-019-0620-9-e DE-627 ger DE-627 rakwb eng Qi, Chuang verfasserin aut Dynamic monitoring of resuspension in the multiple eco-types of the littoral zone of a shallow wind-disturbed lake 2019 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer Nature Switzerland AG 2019 Abstract Sedimentation and resuspension processes, are known to govern nutrient cycling and lake metabolic processes, but have not been well studied in littoral zones with multi-ecotypes of shallow wind-disturbed lakes. This time-series study used sediment traps to estimate the spatiotemporal changes in sedimentation and resuspension rates, during the four seasonal continuous deployment periods, in the littoral zone of Lake Taihu. The effect of sedimentation processes on nutrient accumulation was also investigated. Results showed that the sedimentation rates at six observation sites were highly variable, with gross sedimentation rates ranging from 184.83 to 2150.74 g $ m^{−2} $ $ day^{−1} $. Almost 88% of the total observed sedimentation originated from sediment resuspension. Cyanobacterial blooms coupled with the frequently changeable wind conditions in the littoral zone, were the key factors in lacustrine sediment redistribution and a large pool of organic material accumulated during cyanobacterial blooms. Moreover, the contribution of resuspended total phosphorous and total nitrogen to the water column, were 0.22 mg $ L^{−1} $ and 0.46 mg $ L^{−1} $, respectively. The high rate of rapid nutrient cycling observed at the sediment water interface due to resuspension, may be a key factor in maintaining eutrophication in large and shallow lakes, which is of high relevance to the future management of aquatic ecosystems. Gross sedimentation (dpeaa)DE-He213 Sediment resuspension (dpeaa)DE-He213 Sequential sediment trap (dpeaa)DE-He213 Eutrophication lakes (dpeaa)DE-He213 Zhou, Yang aut Xu, Xiao-guang aut Zhang, Li-min aut Lin, Hui aut Wu, Xin-ting aut Shi, Kuan aut Wang, Guo-xiang aut Enthalten in Aquatic sciences Basel : Springer, 1920 81(2019), 2 vom: 18. Feb. (DE-627)265506670 (DE-600)1464021-1 1420-9055 nnns volume:81 year:2019 number:2 day:18 month:02 https://dx.doi.org/10.1007/s00027-019-0620-9 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_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 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 81 2019 2 18 02 |
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10.1007/s00027-019-0620-9 doi (DE-627)SPR000296368 (SPR)s00027-019-0620-9-e DE-627 ger DE-627 rakwb eng Qi, Chuang verfasserin aut Dynamic monitoring of resuspension in the multiple eco-types of the littoral zone of a shallow wind-disturbed lake 2019 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer Nature Switzerland AG 2019 Abstract Sedimentation and resuspension processes, are known to govern nutrient cycling and lake metabolic processes, but have not been well studied in littoral zones with multi-ecotypes of shallow wind-disturbed lakes. This time-series study used sediment traps to estimate the spatiotemporal changes in sedimentation and resuspension rates, during the four seasonal continuous deployment periods, in the littoral zone of Lake Taihu. The effect of sedimentation processes on nutrient accumulation was also investigated. Results showed that the sedimentation rates at six observation sites were highly variable, with gross sedimentation rates ranging from 184.83 to 2150.74 g $ m^{−2} $ $ day^{−1} $. Almost 88% of the total observed sedimentation originated from sediment resuspension. Cyanobacterial blooms coupled with the frequently changeable wind conditions in the littoral zone, were the key factors in lacustrine sediment redistribution and a large pool of organic material accumulated during cyanobacterial blooms. Moreover, the contribution of resuspended total phosphorous and total nitrogen to the water column, were 0.22 mg $ L^{−1} $ and 0.46 mg $ L^{−1} $, respectively. The high rate of rapid nutrient cycling observed at the sediment water interface due to resuspension, may be a key factor in maintaining eutrophication in large and shallow lakes, which is of high relevance to the future management of aquatic ecosystems. Gross sedimentation (dpeaa)DE-He213 Sediment resuspension (dpeaa)DE-He213 Sequential sediment trap (dpeaa)DE-He213 Eutrophication lakes (dpeaa)DE-He213 Zhou, Yang aut Xu, Xiao-guang aut Zhang, Li-min aut Lin, Hui aut Wu, Xin-ting aut Shi, Kuan aut Wang, Guo-xiang aut Enthalten in Aquatic sciences Basel : Springer, 1920 81(2019), 2 vom: 18. Feb. (DE-627)265506670 (DE-600)1464021-1 1420-9055 nnns volume:81 year:2019 number:2 day:18 month:02 https://dx.doi.org/10.1007/s00027-019-0620-9 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_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 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 81 2019 2 18 02 |
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10.1007/s00027-019-0620-9 doi (DE-627)SPR000296368 (SPR)s00027-019-0620-9-e DE-627 ger DE-627 rakwb eng Qi, Chuang verfasserin aut Dynamic monitoring of resuspension in the multiple eco-types of the littoral zone of a shallow wind-disturbed lake 2019 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer Nature Switzerland AG 2019 Abstract Sedimentation and resuspension processes, are known to govern nutrient cycling and lake metabolic processes, but have not been well studied in littoral zones with multi-ecotypes of shallow wind-disturbed lakes. This time-series study used sediment traps to estimate the spatiotemporal changes in sedimentation and resuspension rates, during the four seasonal continuous deployment periods, in the littoral zone of Lake Taihu. The effect of sedimentation processes on nutrient accumulation was also investigated. Results showed that the sedimentation rates at six observation sites were highly variable, with gross sedimentation rates ranging from 184.83 to 2150.74 g $ m^{−2} $ $ day^{−1} $. Almost 88% of the total observed sedimentation originated from sediment resuspension. Cyanobacterial blooms coupled with the frequently changeable wind conditions in the littoral zone, were the key factors in lacustrine sediment redistribution and a large pool of organic material accumulated during cyanobacterial blooms. Moreover, the contribution of resuspended total phosphorous and total nitrogen to the water column, were 0.22 mg $ L^{−1} $ and 0.46 mg $ L^{−1} $, respectively. The high rate of rapid nutrient cycling observed at the sediment water interface due to resuspension, may be a key factor in maintaining eutrophication in large and shallow lakes, which is of high relevance to the future management of aquatic ecosystems. Gross sedimentation (dpeaa)DE-He213 Sediment resuspension (dpeaa)DE-He213 Sequential sediment trap (dpeaa)DE-He213 Eutrophication lakes (dpeaa)DE-He213 Zhou, Yang aut Xu, Xiao-guang aut Zhang, Li-min aut Lin, Hui aut Wu, Xin-ting aut Shi, Kuan aut Wang, Guo-xiang aut Enthalten in Aquatic sciences Basel : Springer, 1920 81(2019), 2 vom: 18. Feb. (DE-627)265506670 (DE-600)1464021-1 1420-9055 nnns volume:81 year:2019 number:2 day:18 month:02 https://dx.doi.org/10.1007/s00027-019-0620-9 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_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 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 81 2019 2 18 02 |
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10.1007/s00027-019-0620-9 doi (DE-627)SPR000296368 (SPR)s00027-019-0620-9-e DE-627 ger DE-627 rakwb eng Qi, Chuang verfasserin aut Dynamic monitoring of resuspension in the multiple eco-types of the littoral zone of a shallow wind-disturbed lake 2019 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer Nature Switzerland AG 2019 Abstract Sedimentation and resuspension processes, are known to govern nutrient cycling and lake metabolic processes, but have not been well studied in littoral zones with multi-ecotypes of shallow wind-disturbed lakes. This time-series study used sediment traps to estimate the spatiotemporal changes in sedimentation and resuspension rates, during the four seasonal continuous deployment periods, in the littoral zone of Lake Taihu. The effect of sedimentation processes on nutrient accumulation was also investigated. Results showed that the sedimentation rates at six observation sites were highly variable, with gross sedimentation rates ranging from 184.83 to 2150.74 g $ m^{−2} $ $ day^{−1} $. Almost 88% of the total observed sedimentation originated from sediment resuspension. Cyanobacterial blooms coupled with the frequently changeable wind conditions in the littoral zone, were the key factors in lacustrine sediment redistribution and a large pool of organic material accumulated during cyanobacterial blooms. Moreover, the contribution of resuspended total phosphorous and total nitrogen to the water column, were 0.22 mg $ L^{−1} $ and 0.46 mg $ L^{−1} $, respectively. The high rate of rapid nutrient cycling observed at the sediment water interface due to resuspension, may be a key factor in maintaining eutrophication in large and shallow lakes, which is of high relevance to the future management of aquatic ecosystems. Gross sedimentation (dpeaa)DE-He213 Sediment resuspension (dpeaa)DE-He213 Sequential sediment trap (dpeaa)DE-He213 Eutrophication lakes (dpeaa)DE-He213 Zhou, Yang aut Xu, Xiao-guang aut Zhang, Li-min aut Lin, Hui aut Wu, Xin-ting aut Shi, Kuan aut Wang, Guo-xiang aut Enthalten in Aquatic sciences Basel : Springer, 1920 81(2019), 2 vom: 18. Feb. (DE-627)265506670 (DE-600)1464021-1 1420-9055 nnns volume:81 year:2019 number:2 day:18 month:02 https://dx.doi.org/10.1007/s00027-019-0620-9 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_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 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 81 2019 2 18 02 |
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Qi, Chuang @@aut@@ Zhou, Yang @@aut@@ Xu, Xiao-guang @@aut@@ Zhang, Li-min @@aut@@ Lin, Hui @@aut@@ Wu, Xin-ting @@aut@@ Shi, Kuan @@aut@@ Wang, Guo-xiang @@aut@@ |
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<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">SPR000296368</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230327142615.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">201001s2019 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s00027-019-0620-9</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)SPR000296368</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(SPR)s00027-019-0620-9-e</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Qi, Chuang</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Dynamic monitoring of resuspension in the multiple eco-types of the littoral zone of a shallow wind-disturbed lake</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2019</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© Springer Nature Switzerland AG 2019</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract Sedimentation and resuspension processes, are known to govern nutrient cycling and lake metabolic processes, but have not been well studied in littoral zones with multi-ecotypes of shallow wind-disturbed lakes. This time-series study used sediment traps to estimate the spatiotemporal changes in sedimentation and resuspension rates, during the four seasonal continuous deployment periods, in the littoral zone of Lake Taihu. The effect of sedimentation processes on nutrient accumulation was also investigated. Results showed that the sedimentation rates at six observation sites were highly variable, with gross sedimentation rates ranging from 184.83 to 2150.74 g $ m^{−2} $ $ day^{−1} $. Almost 88% of the total observed sedimentation originated from sediment resuspension. Cyanobacterial blooms coupled with the frequently changeable wind conditions in the littoral zone, were the key factors in lacustrine sediment redistribution and a large pool of organic material accumulated during cyanobacterial blooms. Moreover, the contribution of resuspended total phosphorous and total nitrogen to the water column, were 0.22 mg $ L^{−1} $ and 0.46 mg $ L^{−1} $, respectively. 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Qi, Chuang |
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Dynamic monitoring of resuspension in the multiple eco-types of the littoral zone of a shallow wind-disturbed lake Gross sedimentation (dpeaa)DE-He213 Sediment resuspension (dpeaa)DE-He213 Sequential sediment trap (dpeaa)DE-He213 Eutrophication lakes (dpeaa)DE-He213 |
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dynamic monitoring of resuspension in the multiple eco-types of the littoral zone of a shallow wind-disturbed lake |
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Dynamic monitoring of resuspension in the multiple eco-types of the littoral zone of a shallow wind-disturbed lake |
| abstract |
Abstract Sedimentation and resuspension processes, are known to govern nutrient cycling and lake metabolic processes, but have not been well studied in littoral zones with multi-ecotypes of shallow wind-disturbed lakes. This time-series study used sediment traps to estimate the spatiotemporal changes in sedimentation and resuspension rates, during the four seasonal continuous deployment periods, in the littoral zone of Lake Taihu. The effect of sedimentation processes on nutrient accumulation was also investigated. Results showed that the sedimentation rates at six observation sites were highly variable, with gross sedimentation rates ranging from 184.83 to 2150.74 g $ m^{−2} $ $ day^{−1} $. Almost 88% of the total observed sedimentation originated from sediment resuspension. Cyanobacterial blooms coupled with the frequently changeable wind conditions in the littoral zone, were the key factors in lacustrine sediment redistribution and a large pool of organic material accumulated during cyanobacterial blooms. Moreover, the contribution of resuspended total phosphorous and total nitrogen to the water column, were 0.22 mg $ L^{−1} $ and 0.46 mg $ L^{−1} $, respectively. The high rate of rapid nutrient cycling observed at the sediment water interface due to resuspension, may be a key factor in maintaining eutrophication in large and shallow lakes, which is of high relevance to the future management of aquatic ecosystems. © Springer Nature Switzerland AG 2019 |
| abstractGer |
Abstract Sedimentation and resuspension processes, are known to govern nutrient cycling and lake metabolic processes, but have not been well studied in littoral zones with multi-ecotypes of shallow wind-disturbed lakes. This time-series study used sediment traps to estimate the spatiotemporal changes in sedimentation and resuspension rates, during the four seasonal continuous deployment periods, in the littoral zone of Lake Taihu. The effect of sedimentation processes on nutrient accumulation was also investigated. Results showed that the sedimentation rates at six observation sites were highly variable, with gross sedimentation rates ranging from 184.83 to 2150.74 g $ m^{−2} $ $ day^{−1} $. Almost 88% of the total observed sedimentation originated from sediment resuspension. Cyanobacterial blooms coupled with the frequently changeable wind conditions in the littoral zone, were the key factors in lacustrine sediment redistribution and a large pool of organic material accumulated during cyanobacterial blooms. Moreover, the contribution of resuspended total phosphorous and total nitrogen to the water column, were 0.22 mg $ L^{−1} $ and 0.46 mg $ L^{−1} $, respectively. The high rate of rapid nutrient cycling observed at the sediment water interface due to resuspension, may be a key factor in maintaining eutrophication in large and shallow lakes, which is of high relevance to the future management of aquatic ecosystems. © Springer Nature Switzerland AG 2019 |
| abstract_unstemmed |
Abstract Sedimentation and resuspension processes, are known to govern nutrient cycling and lake metabolic processes, but have not been well studied in littoral zones with multi-ecotypes of shallow wind-disturbed lakes. This time-series study used sediment traps to estimate the spatiotemporal changes in sedimentation and resuspension rates, during the four seasonal continuous deployment periods, in the littoral zone of Lake Taihu. The effect of sedimentation processes on nutrient accumulation was also investigated. Results showed that the sedimentation rates at six observation sites were highly variable, with gross sedimentation rates ranging from 184.83 to 2150.74 g $ m^{−2} $ $ day^{−1} $. Almost 88% of the total observed sedimentation originated from sediment resuspension. Cyanobacterial blooms coupled with the frequently changeable wind conditions in the littoral zone, were the key factors in lacustrine sediment redistribution and a large pool of organic material accumulated during cyanobacterial blooms. Moreover, the contribution of resuspended total phosphorous and total nitrogen to the water column, were 0.22 mg $ L^{−1} $ and 0.46 mg $ L^{−1} $, respectively. The high rate of rapid nutrient cycling observed at the sediment water interface due to resuspension, may be a key factor in maintaining eutrophication in large and shallow lakes, which is of high relevance to the future management of aquatic ecosystems. © Springer Nature Switzerland AG 2019 |
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Dynamic monitoring of resuspension in the multiple eco-types of the littoral zone of a shallow wind-disturbed lake |
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https://dx.doi.org/10.1007/s00027-019-0620-9 |
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Zhou, Yang Xu, Xiao-guang Zhang, Li-min Lin, Hui Wu, Xin-ting Shi, Kuan Wang, Guo-xiang |
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Zhou, Yang Xu, Xiao-guang Zhang, Li-min Lin, Hui Wu, Xin-ting Shi, Kuan Wang, Guo-xiang |
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| score |
7.399722 |