Abderrahim Jardani – författare
Visar alla böcker från författaren Abderrahim Jardani. Handla med fri frakt och snabb leverans.
5 produkter
The Self-Potential Method
Theory and Applications in Environmental Geosciences
Av André Revil, Abderrahim Jardani
Inbunden, 2013
2053 kr
Lägg i varukorg
The self-potential method enables non-intrusive assessment and imaging of disturbances in electrical currents of conductive subsurface materials. It has an increasing number of applications, from mapping fluid flow in the subsurface of the Earth to detecting preferential flow paths in earth dams …
The Self-Potential Method
Theory and Applications in Environmental Geosciences
Av André Revil, Abderrahim Jardani
Häftad, 2018
944 kr
Lägg i varukorg
The self-potential method enables non-intrusive assessment and imaging of disturbances in electrical currents of conductive subsurface materials. It has an increasing number of applications, from mapping fluid flow in the subsurface of the Earth to detecting preferential flow paths in earth dams …
Seismoelectric Method
Theory and Applications
Av André Revil, Abderrahim Jardani m. fl.
Inbunden, 2015
1204 kr
Lägg i varukorg
The seismoelectric method consists of measuring electromagnetic signals associated with the propagation of seismic waves or seismic sources in porous media. This method is useful in an increasing number of applications, for example to characterize aquifers, contaminant plumes or the vadose zone. …
Seismoelectric Method
Theory and Applications
Av Allan Haas, Paul Sava m. fl.
E-bok, 2015
1371 kr
Lägg i varukorg
The seismoelectric method consists of measuring electromagnetic signals associated with the propagation of seismic waves or seismic sources in porous media. This method is useful in an increasing number of applications, for example to characterize aquifers, contaminant plumes or the vadose zone. …
Seismoelectric Method
Theory and Applications
Av Allan Haas, Paul Sava m. fl.
E-bok, 2015
1371 kr
Lägg i varukorg
The seismoelectric method consists of measuring electromagnetic signals associated with the propagation of seismic waves or seismic sources in porous media. This method is useful in an increasing number of applications, for example to characterize aquifers, contaminant plumes or the vadose zone. …
