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Radon in Chalk streams : Spatial and temporal variation of groundwater sources in the Pang and Lambourn catchments, UK

Author
MULLINGER, N. J1 ; BINLEY, A. M1 ; PATES, J. M1 ; CROOK, N. P1
[1] Department of Environmental Science, Lancaster University, Lancaster LA 1 4YQ, United Kingdom
Source

Journal of hydrology (Amsterdam). 2007, Vol 339, Num 3-4, pp 172-182, 11 p ; ref : 3/4 p

CODEN
JHYDA7
ISSN
0022-1694
Scientific domain
Geology
Publisher
Elsevier Science, Amsterdam
Publication country
Netherlands
Document type
Article
Language
English
Author keyword
Chalk rivers Groundwater hydrology Radon River-aquifer interactions
Keyword (fr)
Accrétion Aquifère Bassin versant Concentration Cours eau Craie Crétacé Débit Eau souterraine Modèle Radon Source ponctuelle Traceur Variation spatiale Variation temporelle Rivière Chalk Amérique du Nord Mésozoïque Phanérozoïque Roche carbonatée Roche sédimentaire Canada Est Canada Ontario
Keyword (en)
accretion aquifers drainage basins concentration streams chalk Cretaceous discharge ground water models radon point sources tracers spatial variations time variations Chalk River North America Mesozoic Phanerozoic carbonate rocks sedimentary rocks Eastern Canada Canada Ontario
Keyword (es)
Acreción Cuenca Concentración Curso agua Tiza Cretáceo Gasto Agua subterránea Modelo Radón Trazador Variación espacial Variación temporal America del norte Fanerozoico Roca carbonatada Roca sedimentaria Canadá Este Canada Ontario
Classification
Pascal
001 Exact sciences and technology / 001E Earth, ocean, space / 001E01 Earth sciences / 001E01N Hydrology. Hydrogeology

Discipline
Earth sciences
Origin
Inist-CNRS
Database
PASCAL
INIST identifier
18834603

Sauf mention contraire ci-dessus, le contenu de cette notice bibliographique peut être utilisé dans le cadre d’une licence CC BY 4.0 Inist-CNRS / Unless otherwise stated above, the content of this bibliographic record may be used under a CC BY 4.0 licence by Inist-CNRS / A menos que se haya señalado antes, el contenido de este registro bibliográfico puede ser utilizado al amparo de una licencia CC BY 4.0 Inist-CNRS

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