Matrix, fracture and channel components of storage and flow in a Paleozoic limestone aquifer
- Author
- WORTHINGTON, S. R. H1 ; FORD, D. C1 ; DAVIES, G. J2
[1] School of Geography and Geology, McMaster University, Hamilton, Ontario, Canada
[2] Cambrian Ground Water, Tennessee, United States - Book title
- Groundwater flow and contaminant transport in carbonate aquifers
- Author (monograph)
- SASOWSKY, Ira D (Editor)1 ; WICKS, Carol M (Editor)2
[1] Department of Geology, University of Akron, Ohio, United States
[2] Department of Geological Sciences, University of Missouri, Columbia, United States - Source
Groundwater flow and contaminant transport in carbonate aquifers. 2000, pp 113-128 ; Illustration , Table ; ref : 46 ref
- ISBN
- 90-5410-498-8
- Publisher
- A.A. Balkema, Rotterdam
- Publication country
- Netherlands
- Document type
- Book Chapter
- Language
- English
- Keyword (fr)
- Chenal Fracture Hydrologie karst Matrice roche Mississippien Perméabilité Porosité Temps résidence Bassin Turnhole Spring Kentucky Amérique du Nord Carbonifère Paléozoïque sup Paléozoïque Etats Unis
- Keyword (en)
- channels fractures karst hydrology rock matrix Mississippian permeability porosity residence time Kentucky North America Carboniferous upper Paleozoic Paleozoic United States
- Keyword (es)
- Canal Fractura Matriz roca Mississippiense Permeabilidad Porosidad Kentucky America del norte Carbonífero Estados Unidos
- Classification
- Pascal
- 001 Exact sciences and technology / 001E Earth, ocean, space / 001E01 Earth sciences / 001E01N Hydrology. Hydrogeology / 001E01N02 Hydrogeology
- Discipline
- Earth sciences
- Origin
- BRGM
- Database
- PASCAL
- INIST identifier
- 6190929
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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