Diurnal and seasonal variations of $ pCO_{2} $ and fluorescent dissolved organic matter (FDOM) in different polluted lakes
Abstract This study aimed to assess pollution and daily-to-seasonal dynamics of the partial pressure of $ CO_{2} $ ($ pCO_{2} $) and $ CO_{2} $ degassing flux concerning the fluorescent dissolved organic matter (FDOM) from tropical lakes. A membrane-enclosed $ pCO_{2} $ sensor and water quality mult...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Miah, Osman [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2023 |
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| Anmerkung: |
© The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. |
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| Übergeordnetes Werk: |
Enthalten in: Environmental science and pollution research - Berlin : Springer, 1994, 30(2023), 40 vom: 26. Juli, Seite 92720-92735 |
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| Übergeordnetes Werk: |
volume:30 ; year:2023 ; number:40 ; day:26 ; month:07 ; pages:92720-92735 |
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| DOI / URN: |
10.1007/s11356-023-28878-y |
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| Katalog-ID: |
SPR052840263 |
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| 245 | 1 | 0 | |a Diurnal and seasonal variations of $ pCO_{2} $ and fluorescent dissolved organic matter (FDOM) in different polluted lakes |
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| 520 | |a Abstract This study aimed to assess pollution and daily-to-seasonal dynamics of the partial pressure of $ CO_{2} $ ($ pCO_{2} $) and $ CO_{2} $ degassing flux concerning the fluorescent dissolved organic matter (FDOM) from tropical lakes. A membrane-enclosed $ pCO_{2} $ sensor and water quality multimeter analyzer was deployed to continuously record daily and seasonal variations in $ pCO_{2} $ and $ CO_{2} $ degassing flux in three lakes in Savar, Dhaka. During both wet and dry seasons, all lake water was supersaturated with $ CO_{2} $ in contrast to the atmospheric equilibrium (~400 μatm). The $ pCO_{2} $ values in the lake water during the dry season were relatively low in comparison, and the $ pCO_{2} $ levels in the wet season were much higher due to external inputs of organic matter from watersheds and direct inputs of $ CO_{2} $ from soils or wetlands. The estimated water-to-air $ CO_{2} $ degassing flux in the different levels of polluted lakes varies with the pollution context. Study areas calculated the carbon flux and three lakes released respectively 86.75×$ 10^{7} $g $ CO_{2} $ $ year^{−1} $, 13.8×$ 10^{7} $g $ CO_{2} $ $ year^{−1} $, and 9.17×$ 10^{7} $g $ CO_{2} $ $ year^{−1} $. Three-dimensional excitation-emission matrix (3D-EEM) fluorescence spectroscopy combined with parallel factor (PARAFAC) analysis was used to investigate the distributions of fluorescent components in DOM. EEM-PARAFAC analysis identified humic-like, fulvic-like, protein-like, and more tyrosine-like FDOM components and their environmental dynamics. Terrestrial DOM may provide inputs to the terrestrial humic-like component in the lake water. In contrast, the biological activity of plankton-derived FDOM is the most likely source for the autochthonous humic-like component. FDOM and DO concentrations have negative correlations with $ pCO_{2} $, indicating that when the FDOM and DO level is decreased, the amount of $ pCO_{2} $ values increases. | ||
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| 700 | 1 | |a Tareq, Shafi M |4 aut | |
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10.1007/s11356-023-28878-y doi (DE-627)SPR052840263 (SPR)s11356-023-28878-y-e DE-627 ger DE-627 rakwb eng Miah, Osman verfasserin aut Diurnal and seasonal variations of $ pCO_{2} $ and fluorescent dissolved organic matter (FDOM) in different polluted lakes 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. Abstract This study aimed to assess pollution and daily-to-seasonal dynamics of the partial pressure of $ CO_{2} $ ($ pCO_{2} $) and $ CO_{2} $ degassing flux concerning the fluorescent dissolved organic matter (FDOM) from tropical lakes. A membrane-enclosed $ pCO_{2} $ sensor and water quality multimeter analyzer was deployed to continuously record daily and seasonal variations in $ pCO_{2} $ and $ CO_{2} $ degassing flux in three lakes in Savar, Dhaka. During both wet and dry seasons, all lake water was supersaturated with $ CO_{2} $ in contrast to the atmospheric equilibrium (~400 μatm). The $ pCO_{2} $ values in the lake water during the dry season were relatively low in comparison, and the $ pCO_{2} $ levels in the wet season were much higher due to external inputs of organic matter from watersheds and direct inputs of $ CO_{2} $ from soils or wetlands. The estimated water-to-air $ CO_{2} $ degassing flux in the different levels of polluted lakes varies with the pollution context. Study areas calculated the carbon flux and three lakes released respectively 86.75×$ 10^{7} $g $ CO_{2} $ $ year^{−1} $, 13.8×$ 10^{7} $g $ CO_{2} $ $ year^{−1} $, and 9.17×$ 10^{7} $g $ CO_{2} $ $ year^{−1} $. Three-dimensional excitation-emission matrix (3D-EEM) fluorescence spectroscopy combined with parallel factor (PARAFAC) analysis was used to investigate the distributions of fluorescent components in DOM. EEM-PARAFAC analysis identified humic-like, fulvic-like, protein-like, and more tyrosine-like FDOM components and their environmental dynamics. Terrestrial DOM may provide inputs to the terrestrial humic-like component in the lake water. In contrast, the biological activity of plankton-derived FDOM is the most likely source for the autochthonous humic-like component. FDOM and DO concentrations have negative correlations with $ pCO_{2} $, indicating that when the FDOM and DO level is decreased, the amount of $ pCO_{2} $ values increases. Carbon flux (dpeaa)DE-He213 pCO (dpeaa)DE-He213 Dissolved organic matter (DOM) (dpeaa)DE-He213 Water quality (dpeaa)DE-He213 Degassing flux (dpeaa)DE-He213 Pollution (dpeaa)DE-He213 PARAFAC (dpeaa)DE-He213 Roy, Avik aut Sakib, Abid Azad aut Niloy, Nahin Mostofa aut Haque, Md. Morshedul aut Shammi, Mashura (orcid)0000-0001-5449-4761 aut Tareq, Shafi M aut Enthalten in Environmental science and pollution research Berlin : Springer, 1994 30(2023), 40 vom: 26. Juli, Seite 92720-92735 (DE-627)320517926 (DE-600)2014192-0 1614-7499 nnns volume:30 year:2023 number:40 day:26 month:07 pages:92720-92735 https://dx.doi.org/10.1007/s11356-023-28878-y 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_381 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_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 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_2118 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_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_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 30 2023 40 26 07 92720-92735 |
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10.1007/s11356-023-28878-y doi (DE-627)SPR052840263 (SPR)s11356-023-28878-y-e DE-627 ger DE-627 rakwb eng Miah, Osman verfasserin aut Diurnal and seasonal variations of $ pCO_{2} $ and fluorescent dissolved organic matter (FDOM) in different polluted lakes 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. Abstract This study aimed to assess pollution and daily-to-seasonal dynamics of the partial pressure of $ CO_{2} $ ($ pCO_{2} $) and $ CO_{2} $ degassing flux concerning the fluorescent dissolved organic matter (FDOM) from tropical lakes. A membrane-enclosed $ pCO_{2} $ sensor and water quality multimeter analyzer was deployed to continuously record daily and seasonal variations in $ pCO_{2} $ and $ CO_{2} $ degassing flux in three lakes in Savar, Dhaka. During both wet and dry seasons, all lake water was supersaturated with $ CO_{2} $ in contrast to the atmospheric equilibrium (~400 μatm). The $ pCO_{2} $ values in the lake water during the dry season were relatively low in comparison, and the $ pCO_{2} $ levels in the wet season were much higher due to external inputs of organic matter from watersheds and direct inputs of $ CO_{2} $ from soils or wetlands. The estimated water-to-air $ CO_{2} $ degassing flux in the different levels of polluted lakes varies with the pollution context. Study areas calculated the carbon flux and three lakes released respectively 86.75×$ 10^{7} $g $ CO_{2} $ $ year^{−1} $, 13.8×$ 10^{7} $g $ CO_{2} $ $ year^{−1} $, and 9.17×$ 10^{7} $g $ CO_{2} $ $ year^{−1} $. Three-dimensional excitation-emission matrix (3D-EEM) fluorescence spectroscopy combined with parallel factor (PARAFAC) analysis was used to investigate the distributions of fluorescent components in DOM. EEM-PARAFAC analysis identified humic-like, fulvic-like, protein-like, and more tyrosine-like FDOM components and their environmental dynamics. Terrestrial DOM may provide inputs to the terrestrial humic-like component in the lake water. In contrast, the biological activity of plankton-derived FDOM is the most likely source for the autochthonous humic-like component. FDOM and DO concentrations have negative correlations with $ pCO_{2} $, indicating that when the FDOM and DO level is decreased, the amount of $ pCO_{2} $ values increases. Carbon flux (dpeaa)DE-He213 pCO (dpeaa)DE-He213 Dissolved organic matter (DOM) (dpeaa)DE-He213 Water quality (dpeaa)DE-He213 Degassing flux (dpeaa)DE-He213 Pollution (dpeaa)DE-He213 PARAFAC (dpeaa)DE-He213 Roy, Avik aut Sakib, Abid Azad aut Niloy, Nahin Mostofa aut Haque, Md. Morshedul aut Shammi, Mashura (orcid)0000-0001-5449-4761 aut Tareq, Shafi M aut Enthalten in Environmental science and pollution research Berlin : Springer, 1994 30(2023), 40 vom: 26. Juli, Seite 92720-92735 (DE-627)320517926 (DE-600)2014192-0 1614-7499 nnns volume:30 year:2023 number:40 day:26 month:07 pages:92720-92735 https://dx.doi.org/10.1007/s11356-023-28878-y 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_381 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_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 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_2118 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_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_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 30 2023 40 26 07 92720-92735 |
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10.1007/s11356-023-28878-y doi (DE-627)SPR052840263 (SPR)s11356-023-28878-y-e DE-627 ger DE-627 rakwb eng Miah, Osman verfasserin aut Diurnal and seasonal variations of $ pCO_{2} $ and fluorescent dissolved organic matter (FDOM) in different polluted lakes 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. Abstract This study aimed to assess pollution and daily-to-seasonal dynamics of the partial pressure of $ CO_{2} $ ($ pCO_{2} $) and $ CO_{2} $ degassing flux concerning the fluorescent dissolved organic matter (FDOM) from tropical lakes. A membrane-enclosed $ pCO_{2} $ sensor and water quality multimeter analyzer was deployed to continuously record daily and seasonal variations in $ pCO_{2} $ and $ CO_{2} $ degassing flux in three lakes in Savar, Dhaka. During both wet and dry seasons, all lake water was supersaturated with $ CO_{2} $ in contrast to the atmospheric equilibrium (~400 μatm). The $ pCO_{2} $ values in the lake water during the dry season were relatively low in comparison, and the $ pCO_{2} $ levels in the wet season were much higher due to external inputs of organic matter from watersheds and direct inputs of $ CO_{2} $ from soils or wetlands. The estimated water-to-air $ CO_{2} $ degassing flux in the different levels of polluted lakes varies with the pollution context. Study areas calculated the carbon flux and three lakes released respectively 86.75×$ 10^{7} $g $ CO_{2} $ $ year^{−1} $, 13.8×$ 10^{7} $g $ CO_{2} $ $ year^{−1} $, and 9.17×$ 10^{7} $g $ CO_{2} $ $ year^{−1} $. Three-dimensional excitation-emission matrix (3D-EEM) fluorescence spectroscopy combined with parallel factor (PARAFAC) analysis was used to investigate the distributions of fluorescent components in DOM. EEM-PARAFAC analysis identified humic-like, fulvic-like, protein-like, and more tyrosine-like FDOM components and their environmental dynamics. Terrestrial DOM may provide inputs to the terrestrial humic-like component in the lake water. In contrast, the biological activity of plankton-derived FDOM is the most likely source for the autochthonous humic-like component. FDOM and DO concentrations have negative correlations with $ pCO_{2} $, indicating that when the FDOM and DO level is decreased, the amount of $ pCO_{2} $ values increases. Carbon flux (dpeaa)DE-He213 pCO (dpeaa)DE-He213 Dissolved organic matter (DOM) (dpeaa)DE-He213 Water quality (dpeaa)DE-He213 Degassing flux (dpeaa)DE-He213 Pollution (dpeaa)DE-He213 PARAFAC (dpeaa)DE-He213 Roy, Avik aut Sakib, Abid Azad aut Niloy, Nahin Mostofa aut Haque, Md. Morshedul aut Shammi, Mashura (orcid)0000-0001-5449-4761 aut Tareq, Shafi M aut Enthalten in Environmental science and pollution research Berlin : Springer, 1994 30(2023), 40 vom: 26. Juli, Seite 92720-92735 (DE-627)320517926 (DE-600)2014192-0 1614-7499 nnns volume:30 year:2023 number:40 day:26 month:07 pages:92720-92735 https://dx.doi.org/10.1007/s11356-023-28878-y 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_381 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_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 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_2118 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_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_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 30 2023 40 26 07 92720-92735 |
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10.1007/s11356-023-28878-y doi (DE-627)SPR052840263 (SPR)s11356-023-28878-y-e DE-627 ger DE-627 rakwb eng Miah, Osman verfasserin aut Diurnal and seasonal variations of $ pCO_{2} $ and fluorescent dissolved organic matter (FDOM) in different polluted lakes 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. Abstract This study aimed to assess pollution and daily-to-seasonal dynamics of the partial pressure of $ CO_{2} $ ($ pCO_{2} $) and $ CO_{2} $ degassing flux concerning the fluorescent dissolved organic matter (FDOM) from tropical lakes. A membrane-enclosed $ pCO_{2} $ sensor and water quality multimeter analyzer was deployed to continuously record daily and seasonal variations in $ pCO_{2} $ and $ CO_{2} $ degassing flux in three lakes in Savar, Dhaka. During both wet and dry seasons, all lake water was supersaturated with $ CO_{2} $ in contrast to the atmospheric equilibrium (~400 μatm). The $ pCO_{2} $ values in the lake water during the dry season were relatively low in comparison, and the $ pCO_{2} $ levels in the wet season were much higher due to external inputs of organic matter from watersheds and direct inputs of $ CO_{2} $ from soils or wetlands. The estimated water-to-air $ CO_{2} $ degassing flux in the different levels of polluted lakes varies with the pollution context. Study areas calculated the carbon flux and three lakes released respectively 86.75×$ 10^{7} $g $ CO_{2} $ $ year^{−1} $, 13.8×$ 10^{7} $g $ CO_{2} $ $ year^{−1} $, and 9.17×$ 10^{7} $g $ CO_{2} $ $ year^{−1} $. Three-dimensional excitation-emission matrix (3D-EEM) fluorescence spectroscopy combined with parallel factor (PARAFAC) analysis was used to investigate the distributions of fluorescent components in DOM. EEM-PARAFAC analysis identified humic-like, fulvic-like, protein-like, and more tyrosine-like FDOM components and their environmental dynamics. Terrestrial DOM may provide inputs to the terrestrial humic-like component in the lake water. In contrast, the biological activity of plankton-derived FDOM is the most likely source for the autochthonous humic-like component. FDOM and DO concentrations have negative correlations with $ pCO_{2} $, indicating that when the FDOM and DO level is decreased, the amount of $ pCO_{2} $ values increases. Carbon flux (dpeaa)DE-He213 pCO (dpeaa)DE-He213 Dissolved organic matter (DOM) (dpeaa)DE-He213 Water quality (dpeaa)DE-He213 Degassing flux (dpeaa)DE-He213 Pollution (dpeaa)DE-He213 PARAFAC (dpeaa)DE-He213 Roy, Avik aut Sakib, Abid Azad aut Niloy, Nahin Mostofa aut Haque, Md. Morshedul aut Shammi, Mashura (orcid)0000-0001-5449-4761 aut Tareq, Shafi M aut Enthalten in Environmental science and pollution research Berlin : Springer, 1994 30(2023), 40 vom: 26. Juli, Seite 92720-92735 (DE-627)320517926 (DE-600)2014192-0 1614-7499 nnns volume:30 year:2023 number:40 day:26 month:07 pages:92720-92735 https://dx.doi.org/10.1007/s11356-023-28878-y 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_381 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_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 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_2118 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_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_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 30 2023 40 26 07 92720-92735 |
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10.1007/s11356-023-28878-y doi (DE-627)SPR052840263 (SPR)s11356-023-28878-y-e DE-627 ger DE-627 rakwb eng Miah, Osman verfasserin aut Diurnal and seasonal variations of $ pCO_{2} $ and fluorescent dissolved organic matter (FDOM) in different polluted lakes 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. Abstract This study aimed to assess pollution and daily-to-seasonal dynamics of the partial pressure of $ CO_{2} $ ($ pCO_{2} $) and $ CO_{2} $ degassing flux concerning the fluorescent dissolved organic matter (FDOM) from tropical lakes. A membrane-enclosed $ pCO_{2} $ sensor and water quality multimeter analyzer was deployed to continuously record daily and seasonal variations in $ pCO_{2} $ and $ CO_{2} $ degassing flux in three lakes in Savar, Dhaka. During both wet and dry seasons, all lake water was supersaturated with $ CO_{2} $ in contrast to the atmospheric equilibrium (~400 μatm). The $ pCO_{2} $ values in the lake water during the dry season were relatively low in comparison, and the $ pCO_{2} $ levels in the wet season were much higher due to external inputs of organic matter from watersheds and direct inputs of $ CO_{2} $ from soils or wetlands. The estimated water-to-air $ CO_{2} $ degassing flux in the different levels of polluted lakes varies with the pollution context. Study areas calculated the carbon flux and three lakes released respectively 86.75×$ 10^{7} $g $ CO_{2} $ $ year^{−1} $, 13.8×$ 10^{7} $g $ CO_{2} $ $ year^{−1} $, and 9.17×$ 10^{7} $g $ CO_{2} $ $ year^{−1} $. Three-dimensional excitation-emission matrix (3D-EEM) fluorescence spectroscopy combined with parallel factor (PARAFAC) analysis was used to investigate the distributions of fluorescent components in DOM. EEM-PARAFAC analysis identified humic-like, fulvic-like, protein-like, and more tyrosine-like FDOM components and their environmental dynamics. Terrestrial DOM may provide inputs to the terrestrial humic-like component in the lake water. In contrast, the biological activity of plankton-derived FDOM is the most likely source for the autochthonous humic-like component. FDOM and DO concentrations have negative correlations with $ pCO_{2} $, indicating that when the FDOM and DO level is decreased, the amount of $ pCO_{2} $ values increases. Carbon flux (dpeaa)DE-He213 pCO (dpeaa)DE-He213 Dissolved organic matter (DOM) (dpeaa)DE-He213 Water quality (dpeaa)DE-He213 Degassing flux (dpeaa)DE-He213 Pollution (dpeaa)DE-He213 PARAFAC (dpeaa)DE-He213 Roy, Avik aut Sakib, Abid Azad aut Niloy, Nahin Mostofa aut Haque, Md. Morshedul aut Shammi, Mashura (orcid)0000-0001-5449-4761 aut Tareq, Shafi M aut Enthalten in Environmental science and pollution research Berlin : Springer, 1994 30(2023), 40 vom: 26. Juli, Seite 92720-92735 (DE-627)320517926 (DE-600)2014192-0 1614-7499 nnns volume:30 year:2023 number:40 day:26 month:07 pages:92720-92735 https://dx.doi.org/10.1007/s11356-023-28878-y 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_381 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_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 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_2118 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_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_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 30 2023 40 26 07 92720-92735 |
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Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law.</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract This study aimed to assess pollution and daily-to-seasonal dynamics of the partial pressure of $ CO_{2} $ ($ pCO_{2} $) and $ CO_{2} $ degassing flux concerning the fluorescent dissolved organic matter (FDOM) from tropical lakes. A membrane-enclosed $ pCO_{2} $ sensor and water quality multimeter analyzer was deployed to continuously record daily and seasonal variations in $ pCO_{2} $ and $ CO_{2} $ degassing flux in three lakes in Savar, Dhaka. During both wet and dry seasons, all lake water was supersaturated with $ CO_{2} $ in contrast to the atmospheric equilibrium (~400 μatm). The $ pCO_{2} $ values in the lake water during the dry season were relatively low in comparison, and the $ pCO_{2} $ levels in the wet season were much higher due to external inputs of organic matter from watersheds and direct inputs of $ CO_{2} $ from soils or wetlands. The estimated water-to-air $ CO_{2} $ degassing flux in the different levels of polluted lakes varies with the pollution context. Study areas calculated the carbon flux and three lakes released respectively 86.75×$ 10^{7} $g $ CO_{2} $ $ year^{−1} $, 13.8×$ 10^{7} $g $ CO_{2} $ $ year^{−1} $, and 9.17×$ 10^{7} $g $ CO_{2} $ $ year^{−1} $. Three-dimensional excitation-emission matrix (3D-EEM) fluorescence spectroscopy combined with parallel factor (PARAFAC) analysis was used to investigate the distributions of fluorescent components in DOM. EEM-PARAFAC analysis identified humic-like, fulvic-like, protein-like, and more tyrosine-like FDOM components and their environmental dynamics. Terrestrial DOM may provide inputs to the terrestrial humic-like component in the lake water. In contrast, the biological activity of plankton-derived FDOM is the most likely source for the autochthonous humic-like component. 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Miah, Osman |
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Miah, Osman misc Carbon flux misc pCO misc Dissolved organic matter (DOM) misc Water quality misc Degassing flux misc Pollution misc PARAFAC Diurnal and seasonal variations of $ pCO_{2} $ and fluorescent dissolved organic matter (FDOM) in different polluted lakes |
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Diurnal and seasonal variations of $ pCO_{2} $ and fluorescent dissolved organic matter (FDOM) in different polluted lakes Carbon flux (dpeaa)DE-He213 pCO (dpeaa)DE-He213 Dissolved organic matter (DOM) (dpeaa)DE-He213 Water quality (dpeaa)DE-He213 Degassing flux (dpeaa)DE-He213 Pollution (dpeaa)DE-He213 PARAFAC (dpeaa)DE-He213 |
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Miah, Osman Roy, Avik Sakib, Abid Azad Niloy, Nahin Mostofa Haque, Md. Morshedul Shammi, Mashura Tareq, Shafi M |
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Miah, Osman |
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10.1007/s11356-023-28878-y |
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diurnal and seasonal variations of $ pco_{2} $ and fluorescent dissolved organic matter (fdom) in different polluted lakes |
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Diurnal and seasonal variations of $ pCO_{2} $ and fluorescent dissolved organic matter (FDOM) in different polluted lakes |
| abstract |
Abstract This study aimed to assess pollution and daily-to-seasonal dynamics of the partial pressure of $ CO_{2} $ ($ pCO_{2} $) and $ CO_{2} $ degassing flux concerning the fluorescent dissolved organic matter (FDOM) from tropical lakes. A membrane-enclosed $ pCO_{2} $ sensor and water quality multimeter analyzer was deployed to continuously record daily and seasonal variations in $ pCO_{2} $ and $ CO_{2} $ degassing flux in three lakes in Savar, Dhaka. During both wet and dry seasons, all lake water was supersaturated with $ CO_{2} $ in contrast to the atmospheric equilibrium (~400 μatm). The $ pCO_{2} $ values in the lake water during the dry season were relatively low in comparison, and the $ pCO_{2} $ levels in the wet season were much higher due to external inputs of organic matter from watersheds and direct inputs of $ CO_{2} $ from soils or wetlands. The estimated water-to-air $ CO_{2} $ degassing flux in the different levels of polluted lakes varies with the pollution context. Study areas calculated the carbon flux and three lakes released respectively 86.75×$ 10^{7} $g $ CO_{2} $ $ year^{−1} $, 13.8×$ 10^{7} $g $ CO_{2} $ $ year^{−1} $, and 9.17×$ 10^{7} $g $ CO_{2} $ $ year^{−1} $. Three-dimensional excitation-emission matrix (3D-EEM) fluorescence spectroscopy combined with parallel factor (PARAFAC) analysis was used to investigate the distributions of fluorescent components in DOM. EEM-PARAFAC analysis identified humic-like, fulvic-like, protein-like, and more tyrosine-like FDOM components and their environmental dynamics. Terrestrial DOM may provide inputs to the terrestrial humic-like component in the lake water. In contrast, the biological activity of plankton-derived FDOM is the most likely source for the autochthonous humic-like component. FDOM and DO concentrations have negative correlations with $ pCO_{2} $, indicating that when the FDOM and DO level is decreased, the amount of $ pCO_{2} $ values increases. © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. |
| abstractGer |
Abstract This study aimed to assess pollution and daily-to-seasonal dynamics of the partial pressure of $ CO_{2} $ ($ pCO_{2} $) and $ CO_{2} $ degassing flux concerning the fluorescent dissolved organic matter (FDOM) from tropical lakes. A membrane-enclosed $ pCO_{2} $ sensor and water quality multimeter analyzer was deployed to continuously record daily and seasonal variations in $ pCO_{2} $ and $ CO_{2} $ degassing flux in three lakes in Savar, Dhaka. During both wet and dry seasons, all lake water was supersaturated with $ CO_{2} $ in contrast to the atmospheric equilibrium (~400 μatm). The $ pCO_{2} $ values in the lake water during the dry season were relatively low in comparison, and the $ pCO_{2} $ levels in the wet season were much higher due to external inputs of organic matter from watersheds and direct inputs of $ CO_{2} $ from soils or wetlands. The estimated water-to-air $ CO_{2} $ degassing flux in the different levels of polluted lakes varies with the pollution context. Study areas calculated the carbon flux and three lakes released respectively 86.75×$ 10^{7} $g $ CO_{2} $ $ year^{−1} $, 13.8×$ 10^{7} $g $ CO_{2} $ $ year^{−1} $, and 9.17×$ 10^{7} $g $ CO_{2} $ $ year^{−1} $. Three-dimensional excitation-emission matrix (3D-EEM) fluorescence spectroscopy combined with parallel factor (PARAFAC) analysis was used to investigate the distributions of fluorescent components in DOM. EEM-PARAFAC analysis identified humic-like, fulvic-like, protein-like, and more tyrosine-like FDOM components and their environmental dynamics. Terrestrial DOM may provide inputs to the terrestrial humic-like component in the lake water. In contrast, the biological activity of plankton-derived FDOM is the most likely source for the autochthonous humic-like component. FDOM and DO concentrations have negative correlations with $ pCO_{2} $, indicating that when the FDOM and DO level is decreased, the amount of $ pCO_{2} $ values increases. © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. |
| abstract_unstemmed |
Abstract This study aimed to assess pollution and daily-to-seasonal dynamics of the partial pressure of $ CO_{2} $ ($ pCO_{2} $) and $ CO_{2} $ degassing flux concerning the fluorescent dissolved organic matter (FDOM) from tropical lakes. A membrane-enclosed $ pCO_{2} $ sensor and water quality multimeter analyzer was deployed to continuously record daily and seasonal variations in $ pCO_{2} $ and $ CO_{2} $ degassing flux in three lakes in Savar, Dhaka. During both wet and dry seasons, all lake water was supersaturated with $ CO_{2} $ in contrast to the atmospheric equilibrium (~400 μatm). The $ pCO_{2} $ values in the lake water during the dry season were relatively low in comparison, and the $ pCO_{2} $ levels in the wet season were much higher due to external inputs of organic matter from watersheds and direct inputs of $ CO_{2} $ from soils or wetlands. The estimated water-to-air $ CO_{2} $ degassing flux in the different levels of polluted lakes varies with the pollution context. Study areas calculated the carbon flux and three lakes released respectively 86.75×$ 10^{7} $g $ CO_{2} $ $ year^{−1} $, 13.8×$ 10^{7} $g $ CO_{2} $ $ year^{−1} $, and 9.17×$ 10^{7} $g $ CO_{2} $ $ year^{−1} $. Three-dimensional excitation-emission matrix (3D-EEM) fluorescence spectroscopy combined with parallel factor (PARAFAC) analysis was used to investigate the distributions of fluorescent components in DOM. EEM-PARAFAC analysis identified humic-like, fulvic-like, protein-like, and more tyrosine-like FDOM components and their environmental dynamics. Terrestrial DOM may provide inputs to the terrestrial humic-like component in the lake water. In contrast, the biological activity of plankton-derived FDOM is the most likely source for the autochthonous humic-like component. FDOM and DO concentrations have negative correlations with $ pCO_{2} $, indicating that when the FDOM and DO level is decreased, the amount of $ pCO_{2} $ values increases. © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. |
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Diurnal and seasonal variations of $ pCO_{2} $ and fluorescent dissolved organic matter (FDOM) in different polluted lakes |
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| score |
7.400177 |