dc.contributor.author |
Cooray, Asitha |
|
dc.date.accessioned |
2021-03-22T05:28:21Z |
|
dc.date.available |
2021-03-22T05:28:21Z |
|
dc.date.issued |
2019-01 |
|
dc.identifier.uri |
http://ichemcdr.com:8080/xmlui/handle/123456789/25 |
|
dc.description |
page 13 - 16 |
en_US |
dc.description.abstract |
Iron is one of the most important redox active trace
metals present in aquatic systems. The redox cycling
of iron is closely associated with the biogeochemical
cycling of oxygen, dissolved organic carbon (DOC),
and other trace metals. |
en_US |
dc.language.iso |
en |
en_US |
dc.publisher |
Institute of Chemistry Ceylon |
en_US |
dc.relation.ispartofseries |
36;1 |
|
dc.subject |
Biogeochemical |
en_US |
dc.subject |
Natural Waters |
en_US |
dc.title |
Biogeochemical Cycling of iron in Natural Waters |
en_US |
dc.type |
Article |
en_US |