Distribution of heavy metals and nutrients in rainwater in coastal regions between the southern Yellow Sea and East China Sea
Rainwater samples were collected in series in Qianliyan Island (southern Yellow Sea) and Shengsi Archipelago (East China Sea) between May 2000 and May 2002, chemical analysis for pH values,concentrations of heavy metals (Cu, Pb, Zn and Cd) and nutrients (NH4^-, NO3^-, PO43^-, SiO32^-) were performed...
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| Veröffentlicht in: | Chinese journal of oceanology and limnology 2005-06, Vol.23 (2), p.230-237 |
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| creator | 刘昌岭 张国森 任宏波 张经 |
| description | Rainwater samples were collected in series in Qianliyan Island (southern Yellow Sea) and Shengsi Archipelago (East China Sea) between May 2000 and May 2002, chemical analysis for pH values,concentrations of heavy metals (Cu, Pb, Zn and Cd) and nutrients (NH4^-, NO3^-, PO43^-, SiO32^-) were performed.Results indicate that concentrations of most of the heavy metals and nutrients in rainwater show clear seasonal variation, i.e. high level in winter and low level in summer. Regionally, concentrations are higher in the southern Yellow Sea than in the East China Sea, but the annual input of heavy metals into oceans by wet deposition is similar in both stations. However, the input of nutrients by wet deposition in the East China Sea is 2-3 times higher than that in the southern Yellow Sea. In individual, Pb and PO4^3- are input to the sea mainly by dry deposition; whereas Cu, Zn, Cd and N compounds are input dominantly by wet deposition, the N/P ratios in the rainwater from two stations are much higher than those in seawater, showing a significant impact of atmospheric wet deposition on marine production and biogeochemical circulation of nutrients in these sea regions. |
| doi_str_mv | 10.1007/BF02894244 |
| format | Article |
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Regionally, concentrations are higher in the southern Yellow Sea than in the East China Sea, but the annual input of heavy metals into oceans by wet deposition is similar in both stations. However, the input of nutrients by wet deposition in the East China Sea is 2-3 times higher than that in the southern Yellow Sea. In individual, Pb and PO4^3- are input to the sea mainly by dry deposition; whereas Cu, Zn, Cd and N compounds are input dominantly by wet deposition, the N/P ratios in the rainwater from two stations are much higher than those in seawater, showing a significant impact of atmospheric wet deposition on marine production and biogeochemical circulation of nutrients in these sea regions.</description><identifier>ISSN: 0254-4059</identifier><identifier>ISSN: 2096-5508</identifier><identifier>EISSN: 1993-5005</identifier><identifier>EISSN: 2523-3521</identifier><identifier>DOI: 10.1007/BF02894244</identifier><language>eng</language><publisher>Dordrecht: Springer Nature B.V</publisher><subject>Archipelagoes ; Atmospheric circulation ; Cadmium ; Chemical analysis ; Coastal zone ; Copper ; Deposition ; Dry deposition ; Heavy metals ; Lead ; Low level ; Marine ; Metal concentrations ; Metals ; Nutrients ; Oceans ; Rain ; Rain water ; Seasonal variation ; Seasonal variations ; Seawater ; Water analysis ; Wet deposition ; Zinc ; 中国海东部 ; 海洋化学 ; 营养元素 ; 重金属 ; 黄海南部</subject><ispartof>Chinese journal of oceanology and limnology, 2005-06, Vol.23 (2), p.230-237</ispartof><rights>Science Press 2005</rights><rights>Science Press 2005.</rights><rights>Copyright © Wanfang Data Co. 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Regionally, concentrations are higher in the southern Yellow Sea than in the East China Sea, but the annual input of heavy metals into oceans by wet deposition is similar in both stations. However, the input of nutrients by wet deposition in the East China Sea is 2-3 times higher than that in the southern Yellow Sea. In individual, Pb and PO4^3- are input to the sea mainly by dry deposition; whereas Cu, Zn, Cd and N compounds are input dominantly by wet deposition, the N/P ratios in the rainwater from two stations are much higher than those in seawater, showing a significant impact of atmospheric wet deposition on marine production and biogeochemical circulation of nutrients in these sea regions.</description><subject>Archipelagoes</subject><subject>Atmospheric circulation</subject><subject>Cadmium</subject><subject>Chemical analysis</subject><subject>Coastal zone</subject><subject>Copper</subject><subject>Deposition</subject><subject>Dry deposition</subject><subject>Heavy metals</subject><subject>Lead</subject><subject>Low level</subject><subject>Marine</subject><subject>Metal concentrations</subject><subject>Metals</subject><subject>Nutrients</subject><subject>Oceans</subject><subject>Rain</subject><subject>Rain water</subject><subject>Seasonal variation</subject><subject>Seasonal 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Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>刘昌岭 张国森 任宏波 张经</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Distribution of heavy metals and nutrients in rainwater in coastal regions between the southern Yellow Sea and East China Sea</atitle><jtitle>Chinese journal of oceanology and limnology</jtitle><addtitle>Chinese Journal of Oceanology and Limnology</addtitle><date>2005-06-01</date><risdate>2005</risdate><volume>23</volume><issue>2</issue><spage>230</spage><epage>237</epage><pages>230-237</pages><issn>0254-4059</issn><issn>2096-5508</issn><eissn>1993-5005</eissn><eissn>2523-3521</eissn><abstract>Rainwater samples were collected in series in Qianliyan Island (southern Yellow Sea) and Shengsi Archipelago (East China Sea) between May 2000 and May 2002, chemical analysis for pH values,concentrations of heavy metals (Cu, Pb, Zn and Cd) and nutrients (NH4^-, NO3^-, PO43^-, SiO32^-) were performed.Results indicate that concentrations of most of the heavy metals and nutrients in rainwater show clear seasonal variation, i.e. high level in winter and low level in summer. Regionally, concentrations are higher in the southern Yellow Sea than in the East China Sea, but the annual input of heavy metals into oceans by wet deposition is similar in both stations. However, the input of nutrients by wet deposition in the East China Sea is 2-3 times higher than that in the southern Yellow Sea. In individual, Pb and PO4^3- are input to the sea mainly by dry deposition; whereas Cu, Zn, Cd and N compounds are input dominantly by wet deposition, the N/P ratios in the rainwater from two stations are much higher than those in seawater, showing a significant impact of atmospheric wet deposition on marine production and biogeochemical circulation of nutrients in these sea regions.</abstract><cop>Dordrecht</cop><pub>Springer Nature B.V</pub><doi>10.1007/BF02894244</doi><tpages>8</tpages></addata></record> |
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| subjects | Archipelagoes Atmospheric circulation Cadmium Chemical analysis Coastal zone Copper Deposition Dry deposition Heavy metals Lead Low level Marine Metal concentrations Metals Nutrients Oceans Rain Rain water Seasonal variation Seasonal variations Seawater Water analysis Wet deposition Zinc 中国海东部 海洋化学 营养元素 重金属 黄海南部 |
| title | Distribution of heavy metals and nutrients in rainwater in coastal regions between the southern Yellow Sea and East China Sea |
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