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Distinguishing sediments from the Yangtze and Yellow Rivers, China

A mineral magnetic approach

Dados Bibliográficos

ID12265083
AutoresWeiguo Zhang (0000-0002-2157-2177, State Key Laboratory of Estuarine and Coastal Research, East China Normal University, Shanghai 200062, China,, autor correspondente), Yu Xing (0009-0005-6138-5973, State Key Laboratory of Estuarine and Coastal Research, East China Normal University, Shanghai 200062, China), Lizhon Yu (State Key Laboratory of Estuarine and Coastal Research, East China Normal University, Shanghai 200062, China), Hua Feng (0000-0003-4748-6231, Montclair State University), Min Lu (0000-0003-3397-3637, East China Normal University)
Ano2008
Volume18
Fascículo7
Páginas1139-1145
Data de publicação2008-10-20
Peer ReviewedSim
Open AccessSim
TipoARTICLE
PeriódicoThe Holocene (JOURNAL)
Identificadores do periódicoISSN: 0959-6836 • E-ISSN: 1477-0911
EditoraSAGE Publishing (PUBLISHER • US)
DOI10.1177/0959683608095582
OpenAlexW2170070492
IdiomaEN
Citações recebidas1
Referências citadas31

The Yellow River and the Yangtze River contribute ~10% of the global fluvial sediment flux to the oceans. Proper characterization of the sediments of the two rivers is critical to the knowledge of their fate in the marginal seas of the west Pacific Ocean. Magnetic measurements have been made on bulk sediments as well as on separated particle size fractions of representative samples from the Yellow and Yangtze River estuaries, with the purpose of providing an efficient means of differentiating both groups of river sediments from each other. We found that on average the Yangtze River estuary sediments have relatively higher ferrimagnetic mineral contents and ferrimagnetic to antiferromagentic ratios compared with the Yellow River estuary sediments. A diagram of Saturated Isothermal Remanent Magnetization (SIRM) versus the demagnetization parameter S −100 can clearly distinguish sediments from the two rivers. Detailed magnetic measurements carried out on particle size fractions provide additional confirmation of magnetic contrasts between the two sets of river sediment samples. These contrasts reflect differences in lithology and weathering regimes in the catchments. To minimize possible biogenic and postdepositional diagenetic overprint in the marine environment, it is recommended that magnetic comparison on the coarser materials (eg, >4 μm) be carried out in addition to bulk measurements. This study shows that the magnetic approach can therefore provide a potentially efficient means of discriminating sediment sources in the Yellow Sea and East China Sea. In view of the rapid variations in sediment load carried by these two rivers in recent years, the present data set also provides a baseline against which possible future variations in sediment composition resulting from catchment changes can be assessed

Diagenesis · Environmental magnetism · Estuary · Fluvial · Geochemistry · Geomorphology · Hydrology (agriculture · Lithology · Sediment · Weathering · Geological formations and processes · Geology and Paleoclimatology Research · Geomagnetism and Paleomagnetism Studies · Geology · Oceanography

  • Holocene shifts in riverine fine-grained sediment supply to the East China Sea Distal Mud in response to climate change

    Open Access•Bangqi Hu, Zuosheng Yang et al.•The Holocene•2014

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    Open Access•Roy Thompson, Frank Oldfield•Environmental Magnetism•1986

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    Open Access•Barbara A Maher•Geophysical Journal International•1988

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    John D Milliman, James P M Syvitski•The Journal of Geology•1992

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    John D Milliman, Robert H Meade•The Journal of Geology•1983

  • Suspended sediment characterization and tracing using a magnetic fingerprinting technique

    Open Access•Robert G Hatfield, Barbara A Maher•The Holocene•2008

  • Sources of fine-grained magnetic minerals in sediments

    Open Access•Frank Oldfield•The Holocene•2007

Obras citantes distintas1
Citações por ano0,08
Intervalo de citações2014 - 2014 (1)
Velocidade de citaçãohistorical
Altamente citadoNão
Tipos de citaçãoNeutras: 1
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