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Volumn 329, Issue 4, 1999, Pages 257-263

Demonstration of strong temporary vertical circulation between wetlands and alluvial and regional aquifers;Mise en evidence de fortes circulations verticales temporaires entre zones humides et aquiferes alluviaux et regionaux

Author keywords

Alluvial wetlands; France; Hydraulic conductivity; Hydraulic head; Hydrology; Piezometry; Seine river; Tensiometry

Indexed keywords

AQUIFER; HYDROLOGY; VERTICAL MIXING; WETLAND;

EID: 0033618833     PISSN: 12518050     EISSN: None     Source Type: Journal    
DOI: 10.1016/S1251-8050(99)80244-4     Document Type: Article
Times cited : (5)

References (12)
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  • 3
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  • 5
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    • Hayashi, M.1    Kamp, G.2    Rudolph, D.L.3
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    • Groundwater inflow measurements in wetland systems
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    • Quantification des écoulements nappe-gravières, en zone alluviale, par optimisation du bilan hydrologique
    • série lla
    • Schanen O., Bendjoudi H., Levassor A. et Fustec E. 1998. Quantification des écoulements nappe-gravières, en zone alluviale, par optimisation du bilan hydrologique, C. R. Acad. Sci. Paris, 326, série lla, 107-112
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    • Hydrological modelling and the sustainable development of the Hadejia-Nguru Wetlands, Nigeria
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  • 12
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    • Groundwater circulations between alluvial aquifer and underlying Senonian chalk in the Seine valley
    • Weng P., Coudrain-Ribstein A., Talbi A. et Bendjoudi H. 1999. Groundwater circulations between alluvial aquifer and underlying Senonian chalk in the Seine valley, Phys. Chem. Earth, 24 (1-2), 151-154
    • (1999) Phys. Chem. Earth , vol.24 , Issue.1-2 , pp. 151-154
    • Weng, P.1    Coudrain-Ribstein, A.2    Talbi, A.3    Bendjoudi, H.4


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.