In: Transport in Porous Media, 2015, vol. 110, no. 2, p. 225-250
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In: Geoscientific Instrumentation, Methods and Data Systems, 2020, vol. 9, no. 2020-2, p. 317–336
Climate-induced warming increasingly leads to degradation of high-alpine permafrost. In order to develop early warning systems for imminent slope destabilization, knowledge about hydrological flow processes in the subsurface is urgently needed. Due to the fast dynamics associated with slope failures, non- or minimally invasive methods are required for inexpensive and timely characterization...
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In: Frontiers in Earth Sc-ience, 2020, vol. 8, p. -
Quantification of ground ice is crucial for understanding permafrost systems and modeling their ongoing degradation. The volumetric ice content is however rarely estimated in permafrost studies, as it is particularly difficult to retrieve. Standard borehole temperature monitoring is unable to provide any ice content estimation, whereas non-invasive geophysical techniques, such as refraction ...
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In: Geophysical Journal International, 2019, vol. 219, no. 3, p. 1866–1875
Quantitative estimation of pore fractions filled with liquid water, ice and air is crucial for a process-based understanding of permafrost and its hazard potential upon climate- induced degradation. Geophysical methods offer opportunities to image distributions of permafrost constituents in a non-invasive manner. We present a method to jointly estimate the volumetric fractions of liquid water,...
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In: Transport in Porous Media, 2014, vol. 105, no. 2, p. 431-450
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In: Pure and Applied Geophysics, 2014, vol. 171, no. 9, p. 2111-2127
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In: Mathematical Geosciences, 2014, vol. 46, no. 5, p. 625-645
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In: Materials and Structures, 2006, vol. 39, no. 4, p. 433-443
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In: Pharmaceutical Research, 2002, vol. 19, no. 11, p. 1622-1629
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In: Granular Matter, 2010, vol. 12, no. 3, p. 303-316
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