In: Mathematical Geosciences, 2015, vol. 47, no. 7, p. 771-789
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In: Environmental Earth Sciences, 2015, vol. 73, no. 7, p. 3275-3284
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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: Transport in Porous Media, 2014, vol. 104, no. 3, p. 607-620
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In: Rock Mechanics and Rock Engineering, 2014, vol. 47, no. 3, p. 869-884
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In: Mathematical Geosciences, 2014, vol. 46, no. 5, p. 625-645
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In: Mathematical Geosciences, 2014, vol. 46, no. 2, p. 187-204
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In: Molecular Imaging and Biology, 2014, vol. 16, no. 2, p. 199-209
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In: Mathematical Geosciences, 2014, vol. 46, no. 2, p. 129-131
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In: Swiss Journal of Geosciences, 2018, vol. 111, no. 3, p. 383–398
Located in NW Switzerland, the Mont Terri rock laboratory is a research facility primarily investigating the Opalinus Clay as potential host rock for deep geological disposal of radioactive waste. In the Mont Terri area, this Jurassic shale formation is characterized by three distinctive lithofacies: a shaly facies, a carbonate-rich sandy facies and a sandy facies. However, the lithological...
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