Compressibility, Internal Pressure and Atomic Magnitudes - download pdf or read online

By Richards Th. W.

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2001, Beylich et al. 2003, Bucki et al. 2004, Maurer and Hauck 2007), but have been increasing in recent years. Electromagnetic techniques include frequency-domain EM systems (FEM), time-domain electromagnetic systems (TDEM), systems using very low frequencies (VLF) and the so-called radiomagnetotelluric method (RMT). Similar to the electrical methods (see Chapter 1) the physical parameter allowing a differentiation between ice and water or frozen and unfrozen substratum is the electrical resistivity (in ohm metres, X m) or more commonly its reciprocal, the electrical conductivity (in siemens/metre or usually millisiemens/ metre, mS/m).

And Hunter, J. (1990). Geophysics in the study of permafrost. In Geotechnical and Environmental Geophysics, ed. , Society of Exploration Geophysics, Tulsa, pp. 355–384. Slater, L. and Lesmes, D. (2002). IP interpretation in environmental investigations. Geophysics, 67(1), 77–88. Telford, W. , Geldart, L. P. and Sheriff, R. E. (1990). Applied Geophysics. Cambridge University Press. Tong, L. and Yang, C. (1990). Incorporation of topography into two-dimensional resistivity inversion. Geophysics, 55, 354–361.

Kneisel, C. (1999). Permafrost in Gletschervorfeldern – Eine vergleichende Untersuchung in den Ostschweizer Alpen und Nordschweden. Trierer Geographische Studien, 22, 156pp. 26 C. Kneisel and C. Hauck Kneisel, C. (2003). Electrical resistivity tomography as a tool for geomorphological investigations – some case studies. Zeitschrift fu¨r Geomorphologie, Supplement, 132, 37–49. Kneisel, C. (2004). New insights into mountain permafrost occurrence and characteristics in glacier forefields at high altitude through the application of 2D resistivity imaging.

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Compressibility, Internal Pressure and Atomic Magnitudes by Richards Th. W.


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