論文

査読有り
2019年4月

Dilution characteristics of riverine input contaminants in the Seto Inland Sea

MARINE POLLUTION BULLETIN
  • Junying Zhu
  • ,
  • Xinyu Guo
  • ,
  • Jie Shi
  • ,
  • Huiwang Gao

141
開始ページ
91
終了ページ
103
記述言語
英語
掲載種別
研究論文(学術雑誌)
DOI
10.1016/j.marpolbul.2019.02.029
出版者・発行元
PERGAMON-ELSEVIER SCIENCE LTD

Riverine input is an important source of contaminants in the marine environments. Based on a hydrodynamic model, the dilution characteristics of riverine contaminants in the Seto Inland Sea and their controlling factors were studied. Results showed that contaminant concentration was high in summer and low in winter. Contaminant concentration decreased with the reduction of its half-life period, and the relationship between them followed power functions. Sensitivity experiments suggested that the horizontal current and vertical stratification associated with air-sea heat flux controlled the seasonal cycle of contaminant concentration in the water column; however, surface wind velocity was the dominant factor affecting the surface contaminant concentration. In addition, contaminant concentration in a sub-region was likely controlled by the variations in river discharges close to the sub-region. These results are helpful for predicting contaminant concentrations in the sea and are expected to contribute to assessing the potential ecological risks to aquatic organisms.

リンク情報
DOI
https://doi.org/10.1016/j.marpolbul.2019.02.029
PubMed
https://www.ncbi.nlm.nih.gov/pubmed/30955786
Web of Science
https://gateway.webofknowledge.com/gateway/Gateway.cgi?GWVersion=2&SrcAuth=JSTA_CEL&SrcApp=J_Gate_JST&DestLinkType=FullRecord&KeyUT=WOS:000465509700012&DestApp=WOS_CPL
Scopus
https://www.scopus.com/inward/record.uri?partnerID=HzOxMe3b&scp=85061650892&origin=inward
Scopus Citedby
https://www.scopus.com/inward/citedby.uri?partnerID=HzOxMe3b&scp=85061650892&origin=inward
ID情報
  • DOI : 10.1016/j.marpolbul.2019.02.029
  • ISSN : 0025-326X
  • eISSN : 1879-3363
  • PubMed ID : 30955786
  • SCOPUS ID : 85061650892
  • Web of Science ID : WOS:000465509700012

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