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sup 15 N isotope biogeochemistry and natural denitrification process in groundwater: Application to the chalk aquifer of norther France

Journal Article · · Geochimica et Cosmochimica Acta; (USA)
;  [1];  [2]
  1. Universite Pierre et Marie Curie-INRA, Paris (France)
  2. BRGM Service Geologique National, Orleans (France)
The use of {sup 15}N natural isotope tracing in an aquifer contained within chalk rocks in northern France indicates that, under certain hydrogeological conditions, major denitrification occurs. At the boundary where the aquifer becomes confined, the nitrate concentrations decrease in the direction of groundwater flow accompanied by an exponential increase in {sup 15}N (expressed in {delta}{sup 15}N) of the residual nitrate. This is characteristic of kinetic isotope effects, which accompany the reduction of the nitrate ion during denitrification. Hydrogeochemical and bacteriological observations confirm this process. Natural isotope tracing also permits this process to be distinguished from local dilution with nitrate-free water, which would entail a major drop in nitrate values without {sup 15}N isotopic enrichment. A model is proposed to explain the relatively small observed magnitude of the isotopic fractionation effect.
OSTI ID:
5283508
Journal Information:
Geochimica et Cosmochimica Acta; (USA), Journal Name: Geochimica et Cosmochimica Acta; (USA) Vol. 52:7; ISSN GCACA; ISSN 0016-7037
Country of Publication:
United States
Language:
English