Refining the contribution of riverine particulate release to the global marine Nd budget
Abstract The release of neodymium (Nd) from particles along continental margins may contribute to losses in the global of Nd budget. The Changjiang River, which carries a heavy load of total suspended matter, empties into the East China Sea, and a strong particulate–seawater interaction process occu...
Ausführliche Beschreibung
Autor*in: |
Che, Hong [verfasserIn] |
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E-Artikel |
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Sprache: |
Englisch |
Erschienen: |
2022 |
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Schlagwörter: |
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Anmerkung: |
© The Author(s) 2022 |
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Übergeordnetes Werk: |
Enthalten in: Progress in Earth and Planetary Science - Berlin : SpringerOpen, 2014, 9(2022), 1 vom: 21. Apr. |
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Übergeordnetes Werk: |
volume:9 ; year:2022 ; number:1 ; day:21 ; month:04 |
Links: |
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DOI / URN: |
10.1186/s40645-022-00479-2 |
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Katalog-ID: |
SPR046813888 |
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520 | |a Abstract The release of neodymium (Nd) from particles along continental margins may contribute to losses in the global of Nd budget. The Changjiang River, which carries a heavy load of total suspended matter, empties into the East China Sea, and a strong particulate–seawater interaction process occurs along the salinity gradient. In the low-salinity region (S < 2.0), strong removal of dissolved rare earth elements (dREEs) occurs, but the Nd isotope values are uniform. At mid- and high-salinity (S = 2.0–28.0 and S > 28.0) areas, the dREE concentrations increase slightly. An Nd isotope mass balance indicates that the release of particulate matter is a source of dREEs in the Changjiang estuary. The release rate of particulate Nd ($ Nd_{SPM} $) to the dissolved Nd pool in Changjiang estuary is higher than other estuaries, such as Amazon estuary. Composite all river data available from the previous studies indicate that 5800–9200 Mg per year of Nd is released to global marine waters from riverine particles. This estimated quantity is on the same order of magnitude as the calculated global Nd release flux based on the case study in the Amazon estuary. Our study indicates that to better constrain the global Nd budget, it is required to consider the release rate of $ Nd_{SPM} $ in different rivers due to the significant difference among various rivers, but with very limited available data as of now. | ||
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700 | 1 | |a Zhang, Jing |0 (orcid)0000-0002-2926-0709 |4 aut | |
700 | 1 | |a Liu, Qian |4 aut | |
700 | 1 | |a He, Huijun |4 aut | |
700 | 1 | |a Zhao, Zhi-Qi |4 aut | |
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10.1186/s40645-022-00479-2 doi (DE-627)SPR046813888 (SPR)s40645-022-00479-2-e DE-627 ger DE-627 rakwb eng Che, Hong verfasserin aut Refining the contribution of riverine particulate release to the global marine Nd budget 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s) 2022 Abstract The release of neodymium (Nd) from particles along continental margins may contribute to losses in the global of Nd budget. The Changjiang River, which carries a heavy load of total suspended matter, empties into the East China Sea, and a strong particulate–seawater interaction process occurs along the salinity gradient. In the low-salinity region (S < 2.0), strong removal of dissolved rare earth elements (dREEs) occurs, but the Nd isotope values are uniform. At mid- and high-salinity (S = 2.0–28.0 and S > 28.0) areas, the dREE concentrations increase slightly. An Nd isotope mass balance indicates that the release of particulate matter is a source of dREEs in the Changjiang estuary. The release rate of particulate Nd ($ Nd_{SPM} $) to the dissolved Nd pool in Changjiang estuary is higher than other estuaries, such as Amazon estuary. Composite all river data available from the previous studies indicate that 5800–9200 Mg per year of Nd is released to global marine waters from riverine particles. This estimated quantity is on the same order of magnitude as the calculated global Nd release flux based on the case study in the Amazon estuary. Our study indicates that to better constrain the global Nd budget, it is required to consider the release rate of $ Nd_{SPM} $ in different rivers due to the significant difference among various rivers, but with very limited available data as of now. Particulate release (dpeaa)DE-He213 Nd budget (dpeaa)DE-He213 Rare earth elements (dpeaa)DE-He213 Changjiang estuary (dpeaa)DE-He213 Zhang, Jing (orcid)0000-0002-2926-0709 aut Liu, Qian aut He, Huijun aut Zhao, Zhi-Qi aut Enthalten in Progress in Earth and Planetary Science Berlin : SpringerOpen, 2014 9(2022), 1 vom: 21. Apr. (DE-627)785702520 (DE-600)2769526-8 2197-4284 nnns volume:9 year:2022 number:1 day:21 month:04 https://dx.doi.org/10.1186/s40645-022-00479-2 kostenfrei 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_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_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 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_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 9 2022 1 21 04 |
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10.1186/s40645-022-00479-2 doi (DE-627)SPR046813888 (SPR)s40645-022-00479-2-e DE-627 ger DE-627 rakwb eng Che, Hong verfasserin aut Refining the contribution of riverine particulate release to the global marine Nd budget 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s) 2022 Abstract The release of neodymium (Nd) from particles along continental margins may contribute to losses in the global of Nd budget. The Changjiang River, which carries a heavy load of total suspended matter, empties into the East China Sea, and a strong particulate–seawater interaction process occurs along the salinity gradient. In the low-salinity region (S < 2.0), strong removal of dissolved rare earth elements (dREEs) occurs, but the Nd isotope values are uniform. At mid- and high-salinity (S = 2.0–28.0 and S > 28.0) areas, the dREE concentrations increase slightly. An Nd isotope mass balance indicates that the release of particulate matter is a source of dREEs in the Changjiang estuary. The release rate of particulate Nd ($ Nd_{SPM} $) to the dissolved Nd pool in Changjiang estuary is higher than other estuaries, such as Amazon estuary. Composite all river data available from the previous studies indicate that 5800–9200 Mg per year of Nd is released to global marine waters from riverine particles. This estimated quantity is on the same order of magnitude as the calculated global Nd release flux based on the case study in the Amazon estuary. Our study indicates that to better constrain the global Nd budget, it is required to consider the release rate of $ Nd_{SPM} $ in different rivers due to the significant difference among various rivers, but with very limited available data as of now. Particulate release (dpeaa)DE-He213 Nd budget (dpeaa)DE-He213 Rare earth elements (dpeaa)DE-He213 Changjiang estuary (dpeaa)DE-He213 Zhang, Jing (orcid)0000-0002-2926-0709 aut Liu, Qian aut He, Huijun aut Zhao, Zhi-Qi aut Enthalten in Progress in Earth and Planetary Science Berlin : SpringerOpen, 2014 9(2022), 1 vom: 21. Apr. (DE-627)785702520 (DE-600)2769526-8 2197-4284 nnns volume:9 year:2022 number:1 day:21 month:04 https://dx.doi.org/10.1186/s40645-022-00479-2 kostenfrei 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_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_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 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_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 9 2022 1 21 04 |
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10.1186/s40645-022-00479-2 doi (DE-627)SPR046813888 (SPR)s40645-022-00479-2-e DE-627 ger DE-627 rakwb eng Che, Hong verfasserin aut Refining the contribution of riverine particulate release to the global marine Nd budget 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s) 2022 Abstract The release of neodymium (Nd) from particles along continental margins may contribute to losses in the global of Nd budget. The Changjiang River, which carries a heavy load of total suspended matter, empties into the East China Sea, and a strong particulate–seawater interaction process occurs along the salinity gradient. In the low-salinity region (S < 2.0), strong removal of dissolved rare earth elements (dREEs) occurs, but the Nd isotope values are uniform. At mid- and high-salinity (S = 2.0–28.0 and S > 28.0) areas, the dREE concentrations increase slightly. An Nd isotope mass balance indicates that the release of particulate matter is a source of dREEs in the Changjiang estuary. The release rate of particulate Nd ($ Nd_{SPM} $) to the dissolved Nd pool in Changjiang estuary is higher than other estuaries, such as Amazon estuary. Composite all river data available from the previous studies indicate that 5800–9200 Mg per year of Nd is released to global marine waters from riverine particles. This estimated quantity is on the same order of magnitude as the calculated global Nd release flux based on the case study in the Amazon estuary. Our study indicates that to better constrain the global Nd budget, it is required to consider the release rate of $ Nd_{SPM} $ in different rivers due to the significant difference among various rivers, but with very limited available data as of now. Particulate release (dpeaa)DE-He213 Nd budget (dpeaa)DE-He213 Rare earth elements (dpeaa)DE-He213 Changjiang estuary (dpeaa)DE-He213 Zhang, Jing (orcid)0000-0002-2926-0709 aut Liu, Qian aut He, Huijun aut Zhao, Zhi-Qi aut Enthalten in Progress in Earth and Planetary Science Berlin : SpringerOpen, 2014 9(2022), 1 vom: 21. Apr. (DE-627)785702520 (DE-600)2769526-8 2197-4284 nnns volume:9 year:2022 number:1 day:21 month:04 https://dx.doi.org/10.1186/s40645-022-00479-2 kostenfrei 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_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_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 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_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 9 2022 1 21 04 |
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10.1186/s40645-022-00479-2 doi (DE-627)SPR046813888 (SPR)s40645-022-00479-2-e DE-627 ger DE-627 rakwb eng Che, Hong verfasserin aut Refining the contribution of riverine particulate release to the global marine Nd budget 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s) 2022 Abstract The release of neodymium (Nd) from particles along continental margins may contribute to losses in the global of Nd budget. The Changjiang River, which carries a heavy load of total suspended matter, empties into the East China Sea, and a strong particulate–seawater interaction process occurs along the salinity gradient. In the low-salinity region (S < 2.0), strong removal of dissolved rare earth elements (dREEs) occurs, but the Nd isotope values are uniform. At mid- and high-salinity (S = 2.0–28.0 and S > 28.0) areas, the dREE concentrations increase slightly. An Nd isotope mass balance indicates that the release of particulate matter is a source of dREEs in the Changjiang estuary. The release rate of particulate Nd ($ Nd_{SPM} $) to the dissolved Nd pool in Changjiang estuary is higher than other estuaries, such as Amazon estuary. Composite all river data available from the previous studies indicate that 5800–9200 Mg per year of Nd is released to global marine waters from riverine particles. This estimated quantity is on the same order of magnitude as the calculated global Nd release flux based on the case study in the Amazon estuary. Our study indicates that to better constrain the global Nd budget, it is required to consider the release rate of $ Nd_{SPM} $ in different rivers due to the significant difference among various rivers, but with very limited available data as of now. Particulate release (dpeaa)DE-He213 Nd budget (dpeaa)DE-He213 Rare earth elements (dpeaa)DE-He213 Changjiang estuary (dpeaa)DE-He213 Zhang, Jing (orcid)0000-0002-2926-0709 aut Liu, Qian aut He, Huijun aut Zhao, Zhi-Qi aut Enthalten in Progress in Earth and Planetary Science Berlin : SpringerOpen, 2014 9(2022), 1 vom: 21. Apr. (DE-627)785702520 (DE-600)2769526-8 2197-4284 nnns volume:9 year:2022 number:1 day:21 month:04 https://dx.doi.org/10.1186/s40645-022-00479-2 kostenfrei 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_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_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 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_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 9 2022 1 21 04 |
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10.1186/s40645-022-00479-2 doi (DE-627)SPR046813888 (SPR)s40645-022-00479-2-e DE-627 ger DE-627 rakwb eng Che, Hong verfasserin aut Refining the contribution of riverine particulate release to the global marine Nd budget 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s) 2022 Abstract The release of neodymium (Nd) from particles along continental margins may contribute to losses in the global of Nd budget. The Changjiang River, which carries a heavy load of total suspended matter, empties into the East China Sea, and a strong particulate–seawater interaction process occurs along the salinity gradient. In the low-salinity region (S < 2.0), strong removal of dissolved rare earth elements (dREEs) occurs, but the Nd isotope values are uniform. At mid- and high-salinity (S = 2.0–28.0 and S > 28.0) areas, the dREE concentrations increase slightly. An Nd isotope mass balance indicates that the release of particulate matter is a source of dREEs in the Changjiang estuary. The release rate of particulate Nd ($ Nd_{SPM} $) to the dissolved Nd pool in Changjiang estuary is higher than other estuaries, such as Amazon estuary. Composite all river data available from the previous studies indicate that 5800–9200 Mg per year of Nd is released to global marine waters from riverine particles. This estimated quantity is on the same order of magnitude as the calculated global Nd release flux based on the case study in the Amazon estuary. Our study indicates that to better constrain the global Nd budget, it is required to consider the release rate of $ Nd_{SPM} $ in different rivers due to the significant difference among various rivers, but with very limited available data as of now. Particulate release (dpeaa)DE-He213 Nd budget (dpeaa)DE-He213 Rare earth elements (dpeaa)DE-He213 Changjiang estuary (dpeaa)DE-He213 Zhang, Jing (orcid)0000-0002-2926-0709 aut Liu, Qian aut He, Huijun aut Zhao, Zhi-Qi aut Enthalten in Progress in Earth and Planetary Science Berlin : SpringerOpen, 2014 9(2022), 1 vom: 21. Apr. (DE-627)785702520 (DE-600)2769526-8 2197-4284 nnns volume:9 year:2022 number:1 day:21 month:04 https://dx.doi.org/10.1186/s40645-022-00479-2 kostenfrei 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_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_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 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_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 9 2022 1 21 04 |
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Che, Hong misc Particulate release misc Nd budget misc Rare earth elements misc Changjiang estuary Refining the contribution of riverine particulate release to the global marine Nd budget |
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Refining the contribution of riverine particulate release to the global marine Nd budget Particulate release (dpeaa)DE-He213 Nd budget (dpeaa)DE-He213 Rare earth elements (dpeaa)DE-He213 Changjiang estuary (dpeaa)DE-He213 |
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refining the contribution of riverine particulate release to the global marine nd budget |
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Refining the contribution of riverine particulate release to the global marine Nd budget |
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Abstract The release of neodymium (Nd) from particles along continental margins may contribute to losses in the global of Nd budget. The Changjiang River, which carries a heavy load of total suspended matter, empties into the East China Sea, and a strong particulate–seawater interaction process occurs along the salinity gradient. In the low-salinity region (S < 2.0), strong removal of dissolved rare earth elements (dREEs) occurs, but the Nd isotope values are uniform. At mid- and high-salinity (S = 2.0–28.0 and S > 28.0) areas, the dREE concentrations increase slightly. An Nd isotope mass balance indicates that the release of particulate matter is a source of dREEs in the Changjiang estuary. The release rate of particulate Nd ($ Nd_{SPM} $) to the dissolved Nd pool in Changjiang estuary is higher than other estuaries, such as Amazon estuary. Composite all river data available from the previous studies indicate that 5800–9200 Mg per year of Nd is released to global marine waters from riverine particles. This estimated quantity is on the same order of magnitude as the calculated global Nd release flux based on the case study in the Amazon estuary. Our study indicates that to better constrain the global Nd budget, it is required to consider the release rate of $ Nd_{SPM} $ in different rivers due to the significant difference among various rivers, but with very limited available data as of now. © The Author(s) 2022 |
abstractGer |
Abstract The release of neodymium (Nd) from particles along continental margins may contribute to losses in the global of Nd budget. The Changjiang River, which carries a heavy load of total suspended matter, empties into the East China Sea, and a strong particulate–seawater interaction process occurs along the salinity gradient. In the low-salinity region (S < 2.0), strong removal of dissolved rare earth elements (dREEs) occurs, but the Nd isotope values are uniform. At mid- and high-salinity (S = 2.0–28.0 and S > 28.0) areas, the dREE concentrations increase slightly. An Nd isotope mass balance indicates that the release of particulate matter is a source of dREEs in the Changjiang estuary. The release rate of particulate Nd ($ Nd_{SPM} $) to the dissolved Nd pool in Changjiang estuary is higher than other estuaries, such as Amazon estuary. Composite all river data available from the previous studies indicate that 5800–9200 Mg per year of Nd is released to global marine waters from riverine particles. This estimated quantity is on the same order of magnitude as the calculated global Nd release flux based on the case study in the Amazon estuary. Our study indicates that to better constrain the global Nd budget, it is required to consider the release rate of $ Nd_{SPM} $ in different rivers due to the significant difference among various rivers, but with very limited available data as of now. © The Author(s) 2022 |
abstract_unstemmed |
Abstract The release of neodymium (Nd) from particles along continental margins may contribute to losses in the global of Nd budget. The Changjiang River, which carries a heavy load of total suspended matter, empties into the East China Sea, and a strong particulate–seawater interaction process occurs along the salinity gradient. In the low-salinity region (S < 2.0), strong removal of dissolved rare earth elements (dREEs) occurs, but the Nd isotope values are uniform. At mid- and high-salinity (S = 2.0–28.0 and S > 28.0) areas, the dREE concentrations increase slightly. An Nd isotope mass balance indicates that the release of particulate matter is a source of dREEs in the Changjiang estuary. The release rate of particulate Nd ($ Nd_{SPM} $) to the dissolved Nd pool in Changjiang estuary is higher than other estuaries, such as Amazon estuary. Composite all river data available from the previous studies indicate that 5800–9200 Mg per year of Nd is released to global marine waters from riverine particles. This estimated quantity is on the same order of magnitude as the calculated global Nd release flux based on the case study in the Amazon estuary. Our study indicates that to better constrain the global Nd budget, it is required to consider the release rate of $ Nd_{SPM} $ in different rivers due to the significant difference among various rivers, but with very limited available data as of now. © The Author(s) 2022 |
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Refining the contribution of riverine particulate release to the global marine Nd budget |
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