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Stream geochemistry as an indicator of increasing permafrost thaw depth in an arctic watershed

dc.contributor.authorKeller, Katy
dc.contributor.authorBlum, Joel D
dc.contributor.authorKling, George W.
dc.date.accessioned2020-06-25T18:48:48Z
dc.date.available2020-06-25T18:48:48Z
dc.date.issued2010
dc.identifier.citationKeller, K., Blum, J.D. and Kling, G.W. (2010) Stream geochemistry as an indicator of increasing permafrost thaw depth in an arctic watershed. Chemical Geology 273, 76-81.
dc.identifier.issn0009-2541
dc.identifier.urihttps://hdl.handle.net/2027.42/155688
dc.publisherElsevier BV
dc.titleStream geochemistry as an indicator of increasing permafrost thaw depth in an arctic watershed
dc.typeArticle
dc.subject.hlbsecondlevelEarth and Environmental Sciences
dc.subject.hlbtoplevelScience
dc.description.peerreviewedPeer Reviewed
dc.description.bitstreamurlhttps://deepblue.lib.umich.edu/bitstream/2027.42/155688/1/Keller_et_al_2010_Stream_geochemistry.pdf
dc.identifier.doi10.1016/j.chemgeo.2010.02.013
dc.identifier.sourceChemical Geology
dc.identifier.orcid0000-0001-5389-8633
dc.identifier.volume273
dc.identifier.issue2-Jan
dc.identifier.startpage76
dc.identifier.endpage81
dc.identifier.name-orcidBlum, Joel; 0000-0001-5389-8633en_US
dc.owningcollnameEarth and Environmental Sciences, Department of


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