Titlebook: Applied Hydrogeophysics; Harry Vereecken,Andrew Binley,Konstantin Titov Conference proceedings 20061st edition Springer Science+Business M

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A SUCCESSIVE LINEAR ESTIMATOR FOR ELECTRICAL RESISTIVITY TOMOGRAPHY,pular for the investigation of subsurface pollution problems (NRC, 2000). In principle, it measures the electric potential field generated by a transmission of dc electric current between electrodes implanted at the ground surface. Then, an apparent (bulk or effective) electrical resistivity for a p

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UNSATURATED ZONE PROCESSES,tween the subsurface and the atmosphere. Vadose zone hydrology provides boundary conditions for both atmospheric processes, including micro-meteorology and climatic changes, and subsurface water migration, with strong implications in water resources management. The rates, timing, and patterns of aqu

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SOLUTE TRANSPORT PROCESSES, important for water resources and also as repository for municipal, industrial, and government waste. Aquifers are typically recharged by natural rainfall entering the soil profile and leaching into deeper soil layers. Due to intensive agricultural or industrial activities the leachate leaving the

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COLD REGIONS HYDROGEOPHYSICS: PHYSICAL CHARACTERISATION AND MONITORING,98; Sullivan et al., 2000; Hauck et al., 2001; Hinkel et al., 2001; Moorman et al., 2003) including ground penetrating radar (GPR), electrical resistivity (ER) and electromagnetic (EM) sounding. Different methods have been employed to study water movement in frozen soils: time domain reflectrometry

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HYDROGEOPHYSICAL APPLICATIONS IN COASTAL AQUIFERS,s for both economical development and quality of life. On the other hand, coastal zones more than other regions suffer from natural disasters such as flooding and tsunami as well as from scarcity of fresh groundwater due to seawater intrusion. The latter problem is usually caused by a violation of a

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