Magnetic properties of surface sediments from Liuxi River, southern China and their environmental significance
Purpose Magnetic minerals within fluvial sediments are affected by a variety of natural and anthropogenic factors, limiting the capability of sediment magnetism in tracing provenance, assessing pollution, and other environmental or geological fields. Methods Twenty-three samples were collected from...
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| Veröffentlicht in: | Journal of soils and sediments 2022-04, Vol.22 (4), p.1286-1301 |
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| creator | Zheng, Erqi Bai, Yang Li, Mingkun Ouyang, Tingping Zhang, Fangzhi Yu, Mingjie Lei, Gang Pan, Zhiyi Long, Gang |
| description | Purpose
Magnetic minerals within fluvial sediments are affected by a variety of natural and anthropogenic factors, limiting the capability of sediment magnetism in tracing provenance, assessing pollution, and other environmental or geological fields.
Methods
Twenty-three samples were collected from Liuxi River, a river influenced by complex natural and human processes, in southern China to conduct the analysis of magnetism, particle size, and geochemical elements. The micromorphology of magnetic particles was directly observed by scanning electron microscope and energy dispersive spectrometer.
Results
The following are the factors affecting the sediment magnetic properties: (1) There is a sampling site in the upper reach with over 100 times magnetic susceptibility than other sites. This sampling site is close to the areas having documented iron ore mining and smelting activities in the past few hundred years, and the sample contains the very high concentrations of metals (e.g., Fe, Mn, Ni, Pb, Sn, V, Cr, Cu, and Bi), implying the ancient mining activity could pose environmental risks in modern sediments. (2) In a downstream direction, magnetic concentration shows a decreasing tendency and magnetic grain size becomes finer. The contributions of superparamagnetic particles and high-coercivity minerals (e.g., hematite) to the total magnetism increase, and technogenic magnetic particles appear downstream of urban areas. In general, the upstream magnetic minerals are controlled by weakly weathered coarse-grained particles produced by granite denudation, while the downstream magnetic minerals are affected by the sedimentary rocks and the human activity. (3) Magnetic minerals become coarse after the river flows over barrages in response to the hydrodynamic changes.
Conclusions
The investigation reveals the natural and anthropogenic influences according to the analysis of the sediments in Liuxi River, and further research related to the sediment magnetism in complex river should be conducted. |
| doi_str_mv | 10.1007/s11368-022-03154-7 |
| format | Article |
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Magnetic minerals within fluvial sediments are affected by a variety of natural and anthropogenic factors, limiting the capability of sediment magnetism in tracing provenance, assessing pollution, and other environmental or geological fields.
Methods
Twenty-three samples were collected from Liuxi River, a river influenced by complex natural and human processes, in southern China to conduct the analysis of magnetism, particle size, and geochemical elements. The micromorphology of magnetic particles was directly observed by scanning electron microscope and energy dispersive spectrometer.
Results
The following are the factors affecting the sediment magnetic properties: (1) There is a sampling site in the upper reach with over 100 times magnetic susceptibility than other sites. This sampling site is close to the areas having documented iron ore mining and smelting activities in the past few hundred years, and the sample contains the very high concentrations of metals (e.g., Fe, Mn, Ni, Pb, Sn, V, Cr, Cu, and Bi), implying the ancient mining activity could pose environmental risks in modern sediments. (2) In a downstream direction, magnetic concentration shows a decreasing tendency and magnetic grain size becomes finer. The contributions of superparamagnetic particles and high-coercivity minerals (e.g., hematite) to the total magnetism increase, and technogenic magnetic particles appear downstream of urban areas. In general, the upstream magnetic minerals are controlled by weakly weathered coarse-grained particles produced by granite denudation, while the downstream magnetic minerals are affected by the sedimentary rocks and the human activity. (3) Magnetic minerals become coarse after the river flows over barrages in response to the hydrodynamic changes.
Conclusions
The investigation reveals the natural and anthropogenic influences according to the analysis of the sediments in Liuxi River, and further research related to the sediment magnetism in complex river should be conducted.</description><identifier>ISSN: 1439-0108</identifier><identifier>EISSN: 1614-7480</identifier><identifier>DOI: 10.1007/s11368-022-03154-7</identifier><language>eng</language><publisher>Berlin/Heidelberg: Springer Berlin Heidelberg</publisher><subject>Anthropogenic factors ; Barrages ; Chromium ; Coercivity ; Copper ; Denudation ; Downstream ; Earth and Environmental Science ; Environment ; Environmental assessment ; Environmental Physics ; Environmental risk ; Fluvial sedimentation ; Fluvial sediments ; Grain size ; Haematite ; Heavy metals ; Hematite ; Human influences ; Iron ores ; Lead ; Magnetic permeability ; Magnetic properties ; Magnetic susceptibility ; Magnetism ; Manganese ; Metal concentrations ; Metals ; Minerals ; Mining ; River flow ; Rivers ; Sampling ; Scanning electron microscopy ; Sec 2 • Physical and Biogeochemical Processes • Research Article ; Sediment ; Sedimentary rocks ; Sediments ; Soil Science & Conservation ; Tin ; Urban areas</subject><ispartof>Journal of soils and sediments, 2022-04, Vol.22 (4), p.1286-1301</ispartof><rights>The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2022</rights><rights>The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2022.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c319t-f641b8a8a1404070093352a8f0ce0b36f6ae55d96e7ebbbf4397836c616fd0903</citedby><cites>FETCH-LOGICAL-c319t-f641b8a8a1404070093352a8f0ce0b36f6ae55d96e7ebbbf4397836c616fd0903</cites><orcidid>0000-0001-5663-8677</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s11368-022-03154-7$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s11368-022-03154-7$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,776,780,27901,27902,41464,42533,51294</link.rule.ids></links><search><creatorcontrib>Zheng, Erqi</creatorcontrib><creatorcontrib>Bai, Yang</creatorcontrib><creatorcontrib>Li, Mingkun</creatorcontrib><creatorcontrib>Ouyang, Tingping</creatorcontrib><creatorcontrib>Zhang, Fangzhi</creatorcontrib><creatorcontrib>Yu, Mingjie</creatorcontrib><creatorcontrib>Lei, Gang</creatorcontrib><creatorcontrib>Pan, Zhiyi</creatorcontrib><creatorcontrib>Long, Gang</creatorcontrib><title>Magnetic properties of surface sediments from Liuxi River, southern China and their environmental significance</title><title>Journal of soils and sediments</title><addtitle>J Soils Sediments</addtitle><description>Purpose
Magnetic minerals within fluvial sediments are affected by a variety of natural and anthropogenic factors, limiting the capability of sediment magnetism in tracing provenance, assessing pollution, and other environmental or geological fields.
Methods
Twenty-three samples were collected from Liuxi River, a river influenced by complex natural and human processes, in southern China to conduct the analysis of magnetism, particle size, and geochemical elements. The micromorphology of magnetic particles was directly observed by scanning electron microscope and energy dispersive spectrometer.
Results
The following are the factors affecting the sediment magnetic properties: (1) There is a sampling site in the upper reach with over 100 times magnetic susceptibility than other sites. This sampling site is close to the areas having documented iron ore mining and smelting activities in the past few hundred years, and the sample contains the very high concentrations of metals (e.g., Fe, Mn, Ni, Pb, Sn, V, Cr, Cu, and Bi), implying the ancient mining activity could pose environmental risks in modern sediments. (2) In a downstream direction, magnetic concentration shows a decreasing tendency and magnetic grain size becomes finer. The contributions of superparamagnetic particles and high-coercivity minerals (e.g., hematite) to the total magnetism increase, and technogenic magnetic particles appear downstream of urban areas. In general, the upstream magnetic minerals are controlled by weakly weathered coarse-grained particles produced by granite denudation, while the downstream magnetic minerals are affected by the sedimentary rocks and the human activity. (3) Magnetic minerals become coarse after the river flows over barrages in response to the hydrodynamic changes.
Conclusions
The investigation reveals the natural and anthropogenic influences according to the analysis of the sediments in Liuxi River, and further research related to the sediment magnetism in complex river should be conducted.</description><subject>Anthropogenic factors</subject><subject>Barrages</subject><subject>Chromium</subject><subject>Coercivity</subject><subject>Copper</subject><subject>Denudation</subject><subject>Downstream</subject><subject>Earth and Environmental Science</subject><subject>Environment</subject><subject>Environmental assessment</subject><subject>Environmental Physics</subject><subject>Environmental risk</subject><subject>Fluvial sedimentation</subject><subject>Fluvial sediments</subject><subject>Grain size</subject><subject>Haematite</subject><subject>Heavy metals</subject><subject>Hematite</subject><subject>Human influences</subject><subject>Iron ores</subject><subject>Lead</subject><subject>Magnetic permeability</subject><subject>Magnetic properties</subject><subject>Magnetic susceptibility</subject><subject>Magnetism</subject><subject>Manganese</subject><subject>Metal concentrations</subject><subject>Metals</subject><subject>Minerals</subject><subject>Mining</subject><subject>River flow</subject><subject>Rivers</subject><subject>Sampling</subject><subject>Scanning electron microscopy</subject><subject>Sec 2 • Physical and Biogeochemical Processes • Research Article</subject><subject>Sediment</subject><subject>Sedimentary rocks</subject><subject>Sediments</subject><subject>Soil Science & Conservation</subject><subject>Tin</subject><subject>Urban 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significance</title><author>Zheng, Erqi ; Bai, Yang ; Li, Mingkun ; Ouyang, Tingping ; Zhang, Fangzhi ; Yu, Mingjie ; Lei, Gang ; Pan, Zhiyi ; Long, Gang</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c319t-f641b8a8a1404070093352a8f0ce0b36f6ae55d96e7ebbbf4397836c616fd0903</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2022</creationdate><topic>Anthropogenic factors</topic><topic>Barrages</topic><topic>Chromium</topic><topic>Coercivity</topic><topic>Copper</topic><topic>Denudation</topic><topic>Downstream</topic><topic>Earth and Environmental Science</topic><topic>Environment</topic><topic>Environmental assessment</topic><topic>Environmental Physics</topic><topic>Environmental risk</topic><topic>Fluvial sedimentation</topic><topic>Fluvial sediments</topic><topic>Grain size</topic><topic>Haematite</topic><topic>Heavy metals</topic><topic>Hematite</topic><topic>Human influences</topic><topic>Iron ores</topic><topic>Lead</topic><topic>Magnetic permeability</topic><topic>Magnetic properties</topic><topic>Magnetic susceptibility</topic><topic>Magnetism</topic><topic>Manganese</topic><topic>Metal concentrations</topic><topic>Metals</topic><topic>Minerals</topic><topic>Mining</topic><topic>River flow</topic><topic>Rivers</topic><topic>Sampling</topic><topic>Scanning electron microscopy</topic><topic>Sec 2 • Physical and Biogeochemical Processes • Research Article</topic><topic>Sediment</topic><topic>Sedimentary rocks</topic><topic>Sediments</topic><topic>Soil Science & Conservation</topic><topic>Tin</topic><topic>Urban areas</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Zheng, Erqi</creatorcontrib><creatorcontrib>Bai, Yang</creatorcontrib><creatorcontrib>Li, Mingkun</creatorcontrib><creatorcontrib>Ouyang, Tingping</creatorcontrib><creatorcontrib>Zhang, Fangzhi</creatorcontrib><creatorcontrib>Yu, 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sediments</jtitle><stitle>J Soils Sediments</stitle><date>2022-04-01</date><risdate>2022</risdate><volume>22</volume><issue>4</issue><spage>1286</spage><epage>1301</epage><pages>1286-1301</pages><issn>1439-0108</issn><eissn>1614-7480</eissn><abstract>Purpose
Magnetic minerals within fluvial sediments are affected by a variety of natural and anthropogenic factors, limiting the capability of sediment magnetism in tracing provenance, assessing pollution, and other environmental or geological fields.
Methods
Twenty-three samples were collected from Liuxi River, a river influenced by complex natural and human processes, in southern China to conduct the analysis of magnetism, particle size, and geochemical elements. The micromorphology of magnetic particles was directly observed by scanning electron microscope and energy dispersive spectrometer.
Results
The following are the factors affecting the sediment magnetic properties: (1) There is a sampling site in the upper reach with over 100 times magnetic susceptibility than other sites. This sampling site is close to the areas having documented iron ore mining and smelting activities in the past few hundred years, and the sample contains the very high concentrations of metals (e.g., Fe, Mn, Ni, Pb, Sn, V, Cr, Cu, and Bi), implying the ancient mining activity could pose environmental risks in modern sediments. (2) In a downstream direction, magnetic concentration shows a decreasing tendency and magnetic grain size becomes finer. The contributions of superparamagnetic particles and high-coercivity minerals (e.g., hematite) to the total magnetism increase, and technogenic magnetic particles appear downstream of urban areas. In general, the upstream magnetic minerals are controlled by weakly weathered coarse-grained particles produced by granite denudation, while the downstream magnetic minerals are affected by the sedimentary rocks and the human activity. (3) Magnetic minerals become coarse after the river flows over barrages in response to the hydrodynamic changes.
Conclusions
The investigation reveals the natural and anthropogenic influences according to the analysis of the sediments in Liuxi River, and further research related to the sediment magnetism in complex river should be conducted.</abstract><cop>Berlin/Heidelberg</cop><pub>Springer Berlin Heidelberg</pub><doi>10.1007/s11368-022-03154-7</doi><tpages>16</tpages><orcidid>https://orcid.org/0000-0001-5663-8677</orcidid></addata></record> |
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| subjects | Anthropogenic factors Barrages Chromium Coercivity Copper Denudation Downstream Earth and Environmental Science Environment Environmental assessment Environmental Physics Environmental risk Fluvial sedimentation Fluvial sediments Grain size Haematite Heavy metals Hematite Human influences Iron ores Lead Magnetic permeability Magnetic properties Magnetic susceptibility Magnetism Manganese Metal concentrations Metals Minerals Mining River flow Rivers Sampling Scanning electron microscopy Sec 2 • Physical and Biogeochemical Processes • Research Article Sediment Sedimentary rocks Sediments Soil Science & Conservation Tin Urban areas |
| title | Magnetic properties of surface sediments from Liuxi River, southern China and their environmental significance |
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