By Richards Th. W.
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Additional info for Compressibility, Internal Pressure and Atomic Magnitudes
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.
Compressibility, Internal Pressure and Atomic Magnitudes by Richards Th. W.