Show simple item record

dc.contributor.authorGreenson, Phillip E.
dc.contributor.authorMeyers, George S.
dc.date.accessioned2021-09-07T20:44:45Z
dc.date.available2021-09-07T20:44:45Z
dc.date.issued1969-01-01
dc.identifier.urihttp://hdl.handle.net/20.500.12648/4070
dc.descriptionPrepared by the United States Department of the Interior Geological Survey. In cooperation with New York State Conservation Department Water Resources Commission
dc.description.abstractThis interim report discusses the general concepts of lake eutrophication and presents the findings of the first year of field investigations on the eutophication of Oneida Lake, New York. Routine biological and chemical data revealed that the lake has become eutrophic both through the natural processes of lake aging and from the inflow of nutrient-rich water from the fertile drainage basin. The four most important factors affecting the biological activities within the lake are: (1) the high fertility of the drainage basin, (2) the physical position and shallowness of the lake, (3) mixing of the water by wind action, and (4) the inclusion of bottom sediments in the recycling of nutrient materials.
dc.language.isoen_US
dc.subjectOneida Lake
dc.subjectLake Eutrophication
dc.titleThe Liminology of Oneida Lake - An Interim Report
dc.typearticle
refterms.dateFOA2021-09-07T20:44:45Z
dc.description.institutionSUNY Brockport
dc.source.statuspublished
dc.description.publicationtitleGovernment Documents (Water Resources)


Files in this item

Thumbnail
Name:
wr_misc/85/fulltext (1).pdf
Size:
1.842Mb
Format:
PDF

This item appears in the following Collection(s)

Show simple item record