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Distribution of particulate and reactive mercury in surface waters of Swedish forest lakes - an empirically based predictive model
Uppsala universitet, Teknisk-naturvetenskapliga vetenskapsområdet, Geovetenskapliga sektionen, Institutionen för geovetenskaper.
2001 (engelsk)Inngår i: ECOLOGICAL MODELLING, ISSN 0304-3800, Vol. 136, nr 1, 81-93 s.Artikkel i tidsskrift (Fagfellevurdert) Published
Abstract [en]

The partition coefficient (K-d) expresses the ratio between particulate bound and dissolved metals. In lake dynamic modelling, it is used to distribute the total load between the dissolved and particulate routes of lake transport. An empirically based mod

sted, utgiver, år, opplag, sider
ELSEVIER SCIENCE BV , 2001. Vol. 136, nr 1, 81-93 s.
Emneord [en]
lakes; mercury; partition coefficient; predictive model; critical tests; ELEMENTAL MERCURY; AQUATIC SYSTEMS; ONONDAGA LAKE; SEDIMENTS; METHYLMERCURY; METALS; FATE; DEPOSITION; TRANSPORT; PARTICLES
Identifikatorer
URN: urn:nbn:se:uu:diva-37857OAI: oai:DiVA.org:uu-37857DiVA: diva2:65756
Merknad
Addresses: Lindstrom M, Uppsala Univ, Dept Earth Sci, Villavagen 16, S-75236 Uppsala, Sweden. Uppsala Univ, Dept Earth Sci, S-75236 Uppsala, Sweden.Tilgjengelig fra: 2008-10-17 Laget: 2008-10-17 Sist oppdatert: 2011-01-14

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