Geochemical modelling of processes controlling baseline compositions of groundwater

D. Postma; C. Kjøller; M. Søgaard Andersen; M.T. Condesso  de Melo; I. Gaus

doi:10.1002/9781444300345.ch4

Geochemical modelling of processes controlling baseline compositions of groundwater

D. Postma, C. Kjøller, M. Søgaard Andersen, M.T. Condesso de Melo, I. Gaus

Afdeling for Geokemi

Publikation: Bidrag til bog/rapport/konferenceproceedings › Bogkapitel › Forskning › peer review

4 Citationer (Scopus)

Resumé

Reactive transport models were developed to explore the evolution in groundwater chemistry along the flow path in three aquifers; the Triassic East Midlands aquifer (UK), the Miocene aquifer at Valréas (France) and the Cretaceous aquifer near Aveiro (Portugal). All three aquifers contain very old groundwaters and variations in water chemistry that are caused by large-scale geochemical processes taking place at the timescale of
thousands of years.

Originalsprog	Engelsk
Titel	Natural groundwater quality
Redaktører	W. Mike Edmunds, Paul Shand
Forlag	Blackwell
Kapitel	4
Sider	71-90
Antal sider	20
ISBN (Elektronisk)	978-14443-0034-5
ISBN (Trykt)	978-14051-5675-2
DOI	https://doi.org/10.1002/9781444300345.ch4
Status	Udgivet - 22 jan. 2009

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Programområde 2: Vandressourcer

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10.1002/9781444300345.ch4

Citationsformater

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AU - Kjøller, C.

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AU - de Melo, M.T. Condesso

AU - Gaus, I.

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AB - Reactive transport models were developed to explore the evolution in groundwater chemistry along the flow path in three aquifers; the Triassic East Midlands aquifer (UK), the Miocene aquifer at Valréas (France) and the Cretaceous aquifer near Aveiro (Portugal). All three aquifers contain very old groundwaters and variations in water chemistry that are caused by large-scale geochemical processes taking place at the timescale of thousands of years.

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Geochemical modelling of processes controlling baseline compositions of groundwater

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