HIGHLIGHTS
SUMMARY
This results in a short-term decrease in suction or increase in pore water pressure and the eventual decrease in shear strength below a critical value for failure (Van Asch et_al, 1999; Godt et_al, 2009; Terzaghi, 1943). A. Wicki et_al: A case study from the Swiss Alpine Foreland based sensors), are then related to the dielectric permittivity of the bulk soil. Data quality depends on the measurement frequency, soil temperature, and clay content of the soil, and precision can be improved by applying site-specific calibration functions (Kelleners et_al, 2005; Robinson et_al, 2008). To . . .
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