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dc.date.accessioned 2022-07-04T15:01:51Z
dc.date.available 2022-07-04T15:01:51Z
dc.date.issued 1995
dc.identifier.uri http://sedici.unlp.edu.ar/handle/10915/138795
dc.description.abstract Water chemistry of the Chascomus Pond (Province of Buenos Aires, Argentina) was studied during a year characterized by low precipitation. Supersaturation of calcium carbonate up to a calcite saturation index of about 20 in spring and summer was observed, together with a diminution of the concentration of dissolved organic matter, in particular humic substances (HS). These results suggested an adsorption between organic matter and calcium carbonate which should influence the growth of calcium carbonate crystals. A preferential removal of higher molecular weight HS was observed by gel permeation chromatography experiments. en
dc.format.extent 55-59 es
dc.language en es
dc.subject dissolved organic matter es
dc.subject humic substances es
dc.subject calcium carbonate supersaturation es
dc.subject Chascomds Pond es
dc.title Dissolved organic matter in Chascomús Pond (Argentina) en
dc.type Articulo es
sedici.identifier.other doi:10.1007/bf00033501 es
sedici.identifier.issn 0018-8158 es
sedici.identifier.issn 1573-5117 es
sedici.title.subtitle Influence of calcium carbonate on humic acid concentration en
sedici.creator.person Conzonno, Víctor Hugo es
sedici.creator.person Fernández Cirelli, Alicia es
sedici.subject.materias Ciencias Naturales es
sedici.description.fulltext true es
mods.originInfo.place Instituto de Limnología "Dr. Raúl A. Ringuelet" es
mods.originInfo.place Universidad de Buenos Aires es
sedici.subtype Articulo es
sedici.rights.license Creative Commons Attribution 4.0 International (CC BY 4.0)
sedici.rights.uri http://creativecommons.org/licenses/by/4.0/
sedici.description.peerReview peer-review es
sedici.relation.journalTitle Hydrobiologia es
sedici.relation.journalVolumeAndIssue vol. 297, no. 1 es


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Creative Commons Attribution 4.0 International (CC BY 4.0) Excepto donde se diga explícitamente, este item se publica bajo la siguiente licencia Creative Commons Attribution 4.0 International (CC BY 4.0)