Rapid isotopic changes in groundwater, upper Rio Guanajuato catchment, Mexico

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Autore principale: Stefanie Kralisch
Natura: Artículo científico
Lingua:en
Pubblicazione: Universidad Nacional Autónoma de México 2007
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author Stefanie Kralisch
author_facet Stefanie Kralisch
contents Rapid isotopic changes in groundwater, upper Rio Guanajuato catchment, Mexico Stefanie Kralisch Alejandra Cortés Jaime Durazo Ciencias de la Tierra Mexico Guanajuato rapid aquifer evolution Recent isotopic change in oxygen–18 and deuterium in groundwater Signifi cant changes in the isotopic composition of groundwater in the upper catchment of Rio Guanajuato, Mexico, weredetected in two independent sets of samples for 3 % of the 1600 high–production wells in the area. Sampling was done in December1998 (53 samples), and in July – August 2003 (41 samples). Average deuterium concentration did not change between 1998 and2003 but the average oxygen–18 concentration suggested a generalized dilution from deep water from infi ltrated local precipitation.This regional change occurred within 56 months, indicating a highly dynamic hydrogeologic system. Fast replenishment of aquiferstorage, or non sustainable over–pumping of old aquifer reserves, are possible explanations. 2007 artículo científico 0016-7169 https://www.redalyc.org/articulo.oa?id=56846105 en http://www.redalyc.org/revista.oa?id=568 Geofísica Internacional application/pdf Universidad Nacional Autónoma de México Geofísica Internacional (México) Num.1 Vol.46
format Artículo científico
id redalyc_56846105
institution Redalyc
language en
publishDate 2007
publisher Universidad Nacional Autónoma de México
spellingShingle Rapid isotopic changes in groundwater, upper Rio Guanajuato catchment, Mexico
Stefanie Kralisch
Ciencias de la Tierra
Mexico
Guanajuato
rapid aquifer evolution
Recent isotopic change in oxygen–18 and deuterium in groundwater
Rapid isotopic changes in groundwater, upper Rio Guanajuato catchment, Mexico Stefanie Kralisch Alejandra Cortés Jaime Durazo Ciencias de la Tierra Mexico Guanajuato rapid aquifer evolution Recent isotopic change in oxygen–18 and deuterium in groundwater Signifi cant changes in the isotopic composition of groundwater in the upper catchment of Rio Guanajuato, Mexico, weredetected in two independent sets of samples for 3 % of the 1600 high–production wells in the area. Sampling was done in December1998 (53 samples), and in July – August 2003 (41 samples). Average deuterium concentration did not change between 1998 and2003 but the average oxygen–18 concentration suggested a generalized dilution from deep water from infi ltrated local precipitation.This regional change occurred within 56 months, indicating a highly dynamic hydrogeologic system. Fast replenishment of aquiferstorage, or non sustainable over–pumping of old aquifer reserves, are possible explanations. 2007 artículo científico 0016-7169 https://www.redalyc.org/articulo.oa?id=56846105 en http://www.redalyc.org/revista.oa?id=568 Geofísica Internacional application/pdf Universidad Nacional Autónoma de México Geofísica Internacional (México) Num.1 Vol.46
title Rapid isotopic changes in groundwater, upper Rio Guanajuato catchment, Mexico
topic Ciencias de la Tierra
Mexico
Guanajuato
rapid aquifer evolution
Recent isotopic change in oxygen–18 and deuterium in groundwater
url https://www.redalyc.org/articulo.oa?id=56846105