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dc.contributor.author	R. Alfaro
dc.contributor.author	V. Martínez
dc.contributor.author	N. Segovia
dc.contributor.author	P. Peña
dc.contributor.author	M. B. E. López
dc.contributor.author	M. A. Armienta
dc.contributor.author	J. Rangel
dc.contributor.author	J. L. Seidel
dc.creator	R. Alfaro
dc.creator	V. Martínez
dc.creator	N. Segovia
dc.creator	P. Peña
dc.creator	M. B. E. López
dc.creator	M. A. Armienta
dc.creator	J. Rangel
dc.creator	J. L. Seidel
dc.date	2002
dc.date.accessioned	2016-03-16T17:17:33Z
dc.date.available	2016-03-16T17:17:33Z
dc.identifier	http://www.redalyc.org/articulo.oa?id=56841413
dc.identifier.uri	http://hdl.handle.net/20.500.11799/39351
dc.description	Radon was determined in springs and wells from urban and agricultural zones around Cuitzeo lake, in the Lerma river basin, Mexico. Major and trace elements were also studied in the water samples. The measurement techniques included the liquid scintillation method for 222Rn, conventional chemical analysis for major components and ICP-MS for metallic trace elements. The average radon concentration values were relatively low, ranging from 0.88 to 3.66 Bq L-1 indicating a rapid transit from recharge to the output of the springs. The major and trace elements are discussed considering the geological characteristics of the studied sites.
dc.format	application/pdf
dc.language	eng
dc.publisher	Universidad Nacional Autónoma de México
dc.relation	http://www.redalyc.org/revista.oa?id=568
dc.rights	openAcess
dc.rights	Geofísica Internacional
dc.source	Geofísica Internacional (México) Num.4 Vol.41
dc.subject	Ciencias de la Tierra
dc.subject	Volcanic zone
dc.subject	groundwater
dc.subject	radon
dc.subject	chemical composition
dc.subject	dissolved trace elements
dc.title	Radon behavior in springs and wells around Cuitzeo lake, Lerma river basin, Mexico
dc.type	Artículo
dc.provenance	Científica
dc.road	Dorada

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