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dc.contributor.authorHrkal, Zbynek
dc.date.accessioned2020-08-26T09:14:17Z
dc.date.available2020-08-26T09:14:17Z
dc.date.issued1992
dc.identifier.urihttps://hdl.handle.net/11250/2674297
dc.description.abstractAn investigation of regional groundwater acidification in the Krusne Hory mountains of northern Bohemia has been carried out. It is based on a comparison of two groundwater chemistry data sets, from the years 1955-1969 and 1980-1990 respectively. The survey uncovered a fivefold increase in the average concentration of NO,-from 0.06 meq\/l (4 mg\/l) to 0.31 meq\/l over the 25 year period, and a halving of the groundwater's average alkalinity. The most acidified groundwaters were found at the highest altitudes, but the most rapid rate of change in the groundwater's chemistry was found lower down, where for example, NO,- concentrations have increased by a factor of 10 over the study period.
dc.language.isonor
dc.relation.ispartofseriesNGU Bulletin (422)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectFORURENSNING
dc.subjectGRUNNVANN
dc.titleAcidification of groundwater in the Bohemian Massif.
dc.typeJournal article
dc.description.localcode35711
dc.source.pagenumber97-102


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