Distribution and mass inventory of mercury in sediment from the Yangtze River estuarine-inner shelf of the East China Sea
Mercury (Hg) was measured in 70 sediment samples from the Yangtze River estuarine-inner shelf of the East China Sea (ECS) to evaluate its occurrence, distribution, and deposition flux. Its concentrations were 10–92ng/g with a mean of 46±17ng/g. A decrease of Hg concentration with increasing distance...
Ausführliche Beschreibung
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| Autor*in: |
Liu, Wenchuan [verfasserIn] |
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E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2017transfer abstract |
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| Umfang: |
9 |
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| Übergeordnetes Werk: |
Enthalten in: A Comparative Analysis of Performance of Several Wavelet Based ECG Data Compression Methodologies - Chandra', S. ELSEVIER, 2020, Amsterdam [u.a.] |
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| Übergeordnetes Werk: |
volume:132 ; year:2017 ; day:1 ; month:01 ; pages:29-37 ; extent:9 |
| Links: |
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| DOI / URN: |
10.1016/j.csr.2016.11.004 |
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| 520 | |a Mercury (Hg) was measured in 70 sediment samples from the Yangtze River estuarine-inner shelf of the East China Sea (ECS) to evaluate its occurrence, distribution, and deposition flux. Its concentrations were 10–92ng/g with a mean of 46±17ng/g. A decrease of Hg concentration with increasing distance offshore suggested a dominance of riverine input. The high levels of Hg observed at the southern inner shelf were partly due to the sorption affinity of fine-grained sediments. Hg concentration was significantly correlated with total organic carbon content and sediment grain size, implying that the nature of sedimentary organic matter and hydrodynamic forces could influence the Hg occurrence. A moderate correlation between Hg with high-molecular-weight polycyclic aromatic hydrocarbons in the YRE suggested that they shared a similar input pathway. The total deposition flux of Hg was estimated to be ~52t/y with a deposition rate of 6–120ng/cm2 y, which indicated that the estuarine-inner shelf of the ECS was a major sink of Hg in the margins off China, and this area could play a significant role in the Hg biogeochemical cycle on a global scale. | ||
| 520 | |a Mercury (Hg) was measured in 70 sediment samples from the Yangtze River estuarine-inner shelf of the East China Sea (ECS) to evaluate its occurrence, distribution, and deposition flux. Its concentrations were 10–92ng/g with a mean of 46±17ng/g. A decrease of Hg concentration with increasing distance offshore suggested a dominance of riverine input. The high levels of Hg observed at the southern inner shelf were partly due to the sorption affinity of fine-grained sediments. Hg concentration was significantly correlated with total organic carbon content and sediment grain size, implying that the nature of sedimentary organic matter and hydrodynamic forces could influence the Hg occurrence. A moderate correlation between Hg with high-molecular-weight polycyclic aromatic hydrocarbons in the YRE suggested that they shared a similar input pathway. The total deposition flux of Hg was estimated to be ~52t/y with a deposition rate of 6–120ng/cm2 y, which indicated that the estuarine-inner shelf of the ECS was a major sink of Hg in the margins off China, and this area could play a significant role in the Hg biogeochemical cycle on a global scale. | ||
| 650 | 7 | |a Large river input |2 Elsevier | |
| 650 | 7 | |a Mass inventory |2 Elsevier | |
| 650 | 7 | |a Distribution |2 Elsevier | |
| 650 | 7 | |a The coastal East China Sea |2 Elsevier | |
| 650 | 7 | |a Surface sediments |2 Elsevier | |
| 650 | 7 | |a Mercury |2 Elsevier | |
| 700 | 1 | |a Hu, Limin |4 oth | |
| 700 | 1 | |a Lin, Tian |4 oth | |
| 700 | 1 | |a Li, Yuanyuan |4 oth | |
| 700 | 1 | |a Guo, Zhigang |4 oth | |
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10.1016/j.csr.2016.11.004 doi GBVA2017009000023.pica (DE-627)ELV035849711 (ELSEVIER)S0278-4343(16)30593-3 DE-627 ger DE-627 rakwb eng 550 550 DE-600 570 610 VZ 44.09 bkl Liu, Wenchuan verfasserin aut Distribution and mass inventory of mercury in sediment from the Yangtze River estuarine-inner shelf of the East China Sea 2017transfer abstract 9 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Mercury (Hg) was measured in 70 sediment samples from the Yangtze River estuarine-inner shelf of the East China Sea (ECS) to evaluate its occurrence, distribution, and deposition flux. Its concentrations were 10–92ng/g with a mean of 46±17ng/g. A decrease of Hg concentration with increasing distance offshore suggested a dominance of riverine input. The high levels of Hg observed at the southern inner shelf were partly due to the sorption affinity of fine-grained sediments. Hg concentration was significantly correlated with total organic carbon content and sediment grain size, implying that the nature of sedimentary organic matter and hydrodynamic forces could influence the Hg occurrence. A moderate correlation between Hg with high-molecular-weight polycyclic aromatic hydrocarbons in the YRE suggested that they shared a similar input pathway. The total deposition flux of Hg was estimated to be ~52t/y with a deposition rate of 6–120ng/cm2 y, which indicated that the estuarine-inner shelf of the ECS was a major sink of Hg in the margins off China, and this area could play a significant role in the Hg biogeochemical cycle on a global scale. Mercury (Hg) was measured in 70 sediment samples from the Yangtze River estuarine-inner shelf of the East China Sea (ECS) to evaluate its occurrence, distribution, and deposition flux. Its concentrations were 10–92ng/g with a mean of 46±17ng/g. A decrease of Hg concentration with increasing distance offshore suggested a dominance of riverine input. The high levels of Hg observed at the southern inner shelf were partly due to the sorption affinity of fine-grained sediments. Hg concentration was significantly correlated with total organic carbon content and sediment grain size, implying that the nature of sedimentary organic matter and hydrodynamic forces could influence the Hg occurrence. A moderate correlation between Hg with high-molecular-weight polycyclic aromatic hydrocarbons in the YRE suggested that they shared a similar input pathway. The total deposition flux of Hg was estimated to be ~52t/y with a deposition rate of 6–120ng/cm2 y, which indicated that the estuarine-inner shelf of the ECS was a major sink of Hg in the margins off China, and this area could play a significant role in the Hg biogeochemical cycle on a global scale. Large river input Elsevier Mass inventory Elsevier Distribution Elsevier The coastal East China Sea Elsevier Surface sediments Elsevier Mercury Elsevier Hu, Limin oth Lin, Tian oth Li, Yuanyuan oth Guo, Zhigang oth Enthalten in Elsevier Science Chandra', S. ELSEVIER A Comparative Analysis of Performance of Several Wavelet Based ECG Data Compression Methodologies 2020 Amsterdam [u.a.] (DE-627)ELV006306659 volume:132 year:2017 day:1 month:01 pages:29-37 extent:9 https://doi.org/10.1016/j.csr.2016.11.004 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U 44.09 Medizintechnik VZ AR 132 2017 1 0101 29-37 9 045F 550 |
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10.1016/j.csr.2016.11.004 doi GBVA2017009000023.pica (DE-627)ELV035849711 (ELSEVIER)S0278-4343(16)30593-3 DE-627 ger DE-627 rakwb eng 550 550 DE-600 570 610 VZ 44.09 bkl Liu, Wenchuan verfasserin aut Distribution and mass inventory of mercury in sediment from the Yangtze River estuarine-inner shelf of the East China Sea 2017transfer abstract 9 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Mercury (Hg) was measured in 70 sediment samples from the Yangtze River estuarine-inner shelf of the East China Sea (ECS) to evaluate its occurrence, distribution, and deposition flux. Its concentrations were 10–92ng/g with a mean of 46±17ng/g. A decrease of Hg concentration with increasing distance offshore suggested a dominance of riverine input. The high levels of Hg observed at the southern inner shelf were partly due to the sorption affinity of fine-grained sediments. Hg concentration was significantly correlated with total organic carbon content and sediment grain size, implying that the nature of sedimentary organic matter and hydrodynamic forces could influence the Hg occurrence. A moderate correlation between Hg with high-molecular-weight polycyclic aromatic hydrocarbons in the YRE suggested that they shared a similar input pathway. The total deposition flux of Hg was estimated to be ~52t/y with a deposition rate of 6–120ng/cm2 y, which indicated that the estuarine-inner shelf of the ECS was a major sink of Hg in the margins off China, and this area could play a significant role in the Hg biogeochemical cycle on a global scale. Mercury (Hg) was measured in 70 sediment samples from the Yangtze River estuarine-inner shelf of the East China Sea (ECS) to evaluate its occurrence, distribution, and deposition flux. Its concentrations were 10–92ng/g with a mean of 46±17ng/g. A decrease of Hg concentration with increasing distance offshore suggested a dominance of riverine input. The high levels of Hg observed at the southern inner shelf were partly due to the sorption affinity of fine-grained sediments. Hg concentration was significantly correlated with total organic carbon content and sediment grain size, implying that the nature of sedimentary organic matter and hydrodynamic forces could influence the Hg occurrence. A moderate correlation between Hg with high-molecular-weight polycyclic aromatic hydrocarbons in the YRE suggested that they shared a similar input pathway. The total deposition flux of Hg was estimated to be ~52t/y with a deposition rate of 6–120ng/cm2 y, which indicated that the estuarine-inner shelf of the ECS was a major sink of Hg in the margins off China, and this area could play a significant role in the Hg biogeochemical cycle on a global scale. Large river input Elsevier Mass inventory Elsevier Distribution Elsevier The coastal East China Sea Elsevier Surface sediments Elsevier Mercury Elsevier Hu, Limin oth Lin, Tian oth Li, Yuanyuan oth Guo, Zhigang oth Enthalten in Elsevier Science Chandra', S. ELSEVIER A Comparative Analysis of Performance of Several Wavelet Based ECG Data Compression Methodologies 2020 Amsterdam [u.a.] (DE-627)ELV006306659 volume:132 year:2017 day:1 month:01 pages:29-37 extent:9 https://doi.org/10.1016/j.csr.2016.11.004 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U 44.09 Medizintechnik VZ AR 132 2017 1 0101 29-37 9 045F 550 |
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10.1016/j.csr.2016.11.004 doi GBVA2017009000023.pica (DE-627)ELV035849711 (ELSEVIER)S0278-4343(16)30593-3 DE-627 ger DE-627 rakwb eng 550 550 DE-600 570 610 VZ 44.09 bkl Liu, Wenchuan verfasserin aut Distribution and mass inventory of mercury in sediment from the Yangtze River estuarine-inner shelf of the East China Sea 2017transfer abstract 9 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Mercury (Hg) was measured in 70 sediment samples from the Yangtze River estuarine-inner shelf of the East China Sea (ECS) to evaluate its occurrence, distribution, and deposition flux. Its concentrations were 10–92ng/g with a mean of 46±17ng/g. A decrease of Hg concentration with increasing distance offshore suggested a dominance of riverine input. The high levels of Hg observed at the southern inner shelf were partly due to the sorption affinity of fine-grained sediments. Hg concentration was significantly correlated with total organic carbon content and sediment grain size, implying that the nature of sedimentary organic matter and hydrodynamic forces could influence the Hg occurrence. A moderate correlation between Hg with high-molecular-weight polycyclic aromatic hydrocarbons in the YRE suggested that they shared a similar input pathway. The total deposition flux of Hg was estimated to be ~52t/y with a deposition rate of 6–120ng/cm2 y, which indicated that the estuarine-inner shelf of the ECS was a major sink of Hg in the margins off China, and this area could play a significant role in the Hg biogeochemical cycle on a global scale. Mercury (Hg) was measured in 70 sediment samples from the Yangtze River estuarine-inner shelf of the East China Sea (ECS) to evaluate its occurrence, distribution, and deposition flux. Its concentrations were 10–92ng/g with a mean of 46±17ng/g. A decrease of Hg concentration with increasing distance offshore suggested a dominance of riverine input. The high levels of Hg observed at the southern inner shelf were partly due to the sorption affinity of fine-grained sediments. Hg concentration was significantly correlated with total organic carbon content and sediment grain size, implying that the nature of sedimentary organic matter and hydrodynamic forces could influence the Hg occurrence. A moderate correlation between Hg with high-molecular-weight polycyclic aromatic hydrocarbons in the YRE suggested that they shared a similar input pathway. The total deposition flux of Hg was estimated to be ~52t/y with a deposition rate of 6–120ng/cm2 y, which indicated that the estuarine-inner shelf of the ECS was a major sink of Hg in the margins off China, and this area could play a significant role in the Hg biogeochemical cycle on a global scale. Large river input Elsevier Mass inventory Elsevier Distribution Elsevier The coastal East China Sea Elsevier Surface sediments Elsevier Mercury Elsevier Hu, Limin oth Lin, Tian oth Li, Yuanyuan oth Guo, Zhigang oth Enthalten in Elsevier Science Chandra', S. ELSEVIER A Comparative Analysis of Performance of Several Wavelet Based ECG Data Compression Methodologies 2020 Amsterdam [u.a.] (DE-627)ELV006306659 volume:132 year:2017 day:1 month:01 pages:29-37 extent:9 https://doi.org/10.1016/j.csr.2016.11.004 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U 44.09 Medizintechnik VZ AR 132 2017 1 0101 29-37 9 045F 550 |
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10.1016/j.csr.2016.11.004 doi GBVA2017009000023.pica (DE-627)ELV035849711 (ELSEVIER)S0278-4343(16)30593-3 DE-627 ger DE-627 rakwb eng 550 550 DE-600 570 610 VZ 44.09 bkl Liu, Wenchuan verfasserin aut Distribution and mass inventory of mercury in sediment from the Yangtze River estuarine-inner shelf of the East China Sea 2017transfer abstract 9 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Mercury (Hg) was measured in 70 sediment samples from the Yangtze River estuarine-inner shelf of the East China Sea (ECS) to evaluate its occurrence, distribution, and deposition flux. Its concentrations were 10–92ng/g with a mean of 46±17ng/g. A decrease of Hg concentration with increasing distance offshore suggested a dominance of riverine input. The high levels of Hg observed at the southern inner shelf were partly due to the sorption affinity of fine-grained sediments. Hg concentration was significantly correlated with total organic carbon content and sediment grain size, implying that the nature of sedimentary organic matter and hydrodynamic forces could influence the Hg occurrence. A moderate correlation between Hg with high-molecular-weight polycyclic aromatic hydrocarbons in the YRE suggested that they shared a similar input pathway. The total deposition flux of Hg was estimated to be ~52t/y with a deposition rate of 6–120ng/cm2 y, which indicated that the estuarine-inner shelf of the ECS was a major sink of Hg in the margins off China, and this area could play a significant role in the Hg biogeochemical cycle on a global scale. Mercury (Hg) was measured in 70 sediment samples from the Yangtze River estuarine-inner shelf of the East China Sea (ECS) to evaluate its occurrence, distribution, and deposition flux. Its concentrations were 10–92ng/g with a mean of 46±17ng/g. A decrease of Hg concentration with increasing distance offshore suggested a dominance of riverine input. The high levels of Hg observed at the southern inner shelf were partly due to the sorption affinity of fine-grained sediments. Hg concentration was significantly correlated with total organic carbon content and sediment grain size, implying that the nature of sedimentary organic matter and hydrodynamic forces could influence the Hg occurrence. A moderate correlation between Hg with high-molecular-weight polycyclic aromatic hydrocarbons in the YRE suggested that they shared a similar input pathway. The total deposition flux of Hg was estimated to be ~52t/y with a deposition rate of 6–120ng/cm2 y, which indicated that the estuarine-inner shelf of the ECS was a major sink of Hg in the margins off China, and this area could play a significant role in the Hg biogeochemical cycle on a global scale. Large river input Elsevier Mass inventory Elsevier Distribution Elsevier The coastal East China Sea Elsevier Surface sediments Elsevier Mercury Elsevier Hu, Limin oth Lin, Tian oth Li, Yuanyuan oth Guo, Zhigang oth Enthalten in Elsevier Science Chandra', S. ELSEVIER A Comparative Analysis of Performance of Several Wavelet Based ECG Data Compression Methodologies 2020 Amsterdam [u.a.] (DE-627)ELV006306659 volume:132 year:2017 day:1 month:01 pages:29-37 extent:9 https://doi.org/10.1016/j.csr.2016.11.004 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U 44.09 Medizintechnik VZ AR 132 2017 1 0101 29-37 9 045F 550 |
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10.1016/j.csr.2016.11.004 doi GBVA2017009000023.pica (DE-627)ELV035849711 (ELSEVIER)S0278-4343(16)30593-3 DE-627 ger DE-627 rakwb eng 550 550 DE-600 570 610 VZ 44.09 bkl Liu, Wenchuan verfasserin aut Distribution and mass inventory of mercury in sediment from the Yangtze River estuarine-inner shelf of the East China Sea 2017transfer abstract 9 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Mercury (Hg) was measured in 70 sediment samples from the Yangtze River estuarine-inner shelf of the East China Sea (ECS) to evaluate its occurrence, distribution, and deposition flux. Its concentrations were 10–92ng/g with a mean of 46±17ng/g. A decrease of Hg concentration with increasing distance offshore suggested a dominance of riverine input. The high levels of Hg observed at the southern inner shelf were partly due to the sorption affinity of fine-grained sediments. Hg concentration was significantly correlated with total organic carbon content and sediment grain size, implying that the nature of sedimentary organic matter and hydrodynamic forces could influence the Hg occurrence. A moderate correlation between Hg with high-molecular-weight polycyclic aromatic hydrocarbons in the YRE suggested that they shared a similar input pathway. The total deposition flux of Hg was estimated to be ~52t/y with a deposition rate of 6–120ng/cm2 y, which indicated that the estuarine-inner shelf of the ECS was a major sink of Hg in the margins off China, and this area could play a significant role in the Hg biogeochemical cycle on a global scale. Mercury (Hg) was measured in 70 sediment samples from the Yangtze River estuarine-inner shelf of the East China Sea (ECS) to evaluate its occurrence, distribution, and deposition flux. Its concentrations were 10–92ng/g with a mean of 46±17ng/g. A decrease of Hg concentration with increasing distance offshore suggested a dominance of riverine input. The high levels of Hg observed at the southern inner shelf were partly due to the sorption affinity of fine-grained sediments. Hg concentration was significantly correlated with total organic carbon content and sediment grain size, implying that the nature of sedimentary organic matter and hydrodynamic forces could influence the Hg occurrence. A moderate correlation between Hg with high-molecular-weight polycyclic aromatic hydrocarbons in the YRE suggested that they shared a similar input pathway. The total deposition flux of Hg was estimated to be ~52t/y with a deposition rate of 6–120ng/cm2 y, which indicated that the estuarine-inner shelf of the ECS was a major sink of Hg in the margins off China, and this area could play a significant role in the Hg biogeochemical cycle on a global scale. Large river input Elsevier Mass inventory Elsevier Distribution Elsevier The coastal East China Sea Elsevier Surface sediments Elsevier Mercury Elsevier Hu, Limin oth Lin, Tian oth Li, Yuanyuan oth Guo, Zhigang oth Enthalten in Elsevier Science Chandra', S. ELSEVIER A Comparative Analysis of Performance of Several Wavelet Based ECG Data Compression Methodologies 2020 Amsterdam [u.a.] (DE-627)ELV006306659 volume:132 year:2017 day:1 month:01 pages:29-37 extent:9 https://doi.org/10.1016/j.csr.2016.11.004 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U 44.09 Medizintechnik VZ AR 132 2017 1 0101 29-37 9 045F 550 |
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Enthalten in A Comparative Analysis of Performance of Several Wavelet Based ECG Data Compression Methodologies Amsterdam [u.a.] volume:132 year:2017 day:1 month:01 pages:29-37 extent:9 |
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Distribution and mass inventory of mercury in sediment from the Yangtze River estuarine-inner shelf of the East China Sea |
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Mercury (Hg) was measured in 70 sediment samples from the Yangtze River estuarine-inner shelf of the East China Sea (ECS) to evaluate its occurrence, distribution, and deposition flux. Its concentrations were 10–92ng/g with a mean of 46±17ng/g. A decrease of Hg concentration with increasing distance offshore suggested a dominance of riverine input. The high levels of Hg observed at the southern inner shelf were partly due to the sorption affinity of fine-grained sediments. Hg concentration was significantly correlated with total organic carbon content and sediment grain size, implying that the nature of sedimentary organic matter and hydrodynamic forces could influence the Hg occurrence. A moderate correlation between Hg with high-molecular-weight polycyclic aromatic hydrocarbons in the YRE suggested that they shared a similar input pathway. The total deposition flux of Hg was estimated to be ~52t/y with a deposition rate of 6–120ng/cm2 y, which indicated that the estuarine-inner shelf of the ECS was a major sink of Hg in the margins off China, and this area could play a significant role in the Hg biogeochemical cycle on a global scale. |
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Mercury (Hg) was measured in 70 sediment samples from the Yangtze River estuarine-inner shelf of the East China Sea (ECS) to evaluate its occurrence, distribution, and deposition flux. Its concentrations were 10–92ng/g with a mean of 46±17ng/g. A decrease of Hg concentration with increasing distance offshore suggested a dominance of riverine input. The high levels of Hg observed at the southern inner shelf were partly due to the sorption affinity of fine-grained sediments. Hg concentration was significantly correlated with total organic carbon content and sediment grain size, implying that the nature of sedimentary organic matter and hydrodynamic forces could influence the Hg occurrence. A moderate correlation between Hg with high-molecular-weight polycyclic aromatic hydrocarbons in the YRE suggested that they shared a similar input pathway. The total deposition flux of Hg was estimated to be ~52t/y with a deposition rate of 6–120ng/cm2 y, which indicated that the estuarine-inner shelf of the ECS was a major sink of Hg in the margins off China, and this area could play a significant role in the Hg biogeochemical cycle on a global scale. |
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Mercury (Hg) was measured in 70 sediment samples from the Yangtze River estuarine-inner shelf of the East China Sea (ECS) to evaluate its occurrence, distribution, and deposition flux. Its concentrations were 10–92ng/g with a mean of 46±17ng/g. A decrease of Hg concentration with increasing distance offshore suggested a dominance of riverine input. The high levels of Hg observed at the southern inner shelf were partly due to the sorption affinity of fine-grained sediments. Hg concentration was significantly correlated with total organic carbon content and sediment grain size, implying that the nature of sedimentary organic matter and hydrodynamic forces could influence the Hg occurrence. A moderate correlation between Hg with high-molecular-weight polycyclic aromatic hydrocarbons in the YRE suggested that they shared a similar input pathway. The total deposition flux of Hg was estimated to be ~52t/y with a deposition rate of 6–120ng/cm2 y, which indicated that the estuarine-inner shelf of the ECS was a major sink of Hg in the margins off China, and this area could play a significant role in the Hg biogeochemical cycle on a global scale. |
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