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pro vyhledávání: '"B. J. M. Goes"'
Autor:
B. J. M. Goes
Publikováno v:
Hydrogeology Journal. 30:1035-1053
The current state of knowledge on groundwater in South Sudan (a data-scarce country) is presented, based on extensive field surveys in Lakes State in the central part of the country, limited published literature, and unpublished consultancy reports.
Publikováno v:
International Journal of Water Resources Development. 37:300-320
This article focuses on a major water use in the Ganges Basin, the Ganges Kobadak Irrigation Project in Bangladesh. The objectives of this article are to assess the present and projected irrigation...
Publikováno v:
Hydrogeology Journal. 25:269-286
A karez is a gently sloping tunnel into a hillside with a series of vertical shafts. At the upstream end, the karez depresses the water table such that groundwater enters the tunnel. Farmers all over Afghanistan have built and managed karezes for cen
Publikováno v:
International Journal of Water Resources Development. 32:3-25
The Helmand River Basin is a closed river basin in (semi)arid southern Afghanistan, Iran and Pakistan. Irrigation is by far the largest surface water use. Two of the three main rivers have large dams that regulate river flow for irrigation and hydrop
Autor:
B. J. M. Goes, J. A. C. Meekes
Publikováno v:
Journal of Environmental and Engineering Geophysics. 9:127-141
Locating Dense Non-Aqueous Phase Liquids (DNAPLs) is often a bottleneck for the successful remediation and∕or control of polluted sites. Electrical Resistivity Tomography (ERT) between boreholes can detect DNAPLs because of their high electrical re
Autor:
B. J. M. Goes
Publikováno v:
Hydrogeology Journal. 7:294-304
The Hadejia–Nguru Wetlands are annually inundated flood plains in semi-arid northeastern Nigeria. The area has a unique ecosystem that forms a natural barrier against the encroachment of the Sahara desert. Both the rich wetland vegetation and local
Autor:
B. J. M. Goes
Publikováno v:
SPIE Proceedings.
The Veluwe area is one of the main groundwater reservoirs in the Netherlands. The Veluwe consists of ice-pushed ridges. The ridges are reworked, mainly sandy, fluvial sediments with some dipping clay layers. Due to these dipping clay layers the sedim