Zobrazeno 1 - 10
of 32
pro vyhledávání: '"Martin Lanzendörfer"'
Publikováno v:
Nature Communications, Vol 15, Iss 1, Pp 1-10 (2024)
Abstract After discovering a jet activity near the south pole of Saturn’s moon Enceladus, the Cassini mission demonstrated the existence of a subsurface water ocean with a unique sampling opportunity through flybys. Diurnal variations in the observ
Externí odkaz:
https://doaj.org/article/cbb0138db06544f5adf3ee9af737f7c3
Autor:
Martin Slavík, Martin Lanzendörfer
Publikováno v:
Hydrology, Vol 11, Iss 9, p 133 (2024)
The study is concerned with the rate of evaporation from porous rock, including the second stage of evaporation characterised by the existence of a dry surface layer separated from the wet capillary zone by a sharp evaporation front. The main objecti
Externí odkaz:
https://doaj.org/article/063dae72f9c544cba3dd1e4f9e219ea3
Autor:
Heiko Woith, Josef Vlček, Tomáš Vylita, Torsten Dahm, Tomáš Fischer, Kyriaki Daskalopoulou, Martin Zimmer, Samuel Niedermann, Jessica A. Stammeier, Veronika Turjaková, Martin Lanzendörfer
Publikováno v:
Geosciences, Vol 13, Iss 1, p 2 (2022)
Mofettes are gas emission sites where high concentrations of CO2 ascend through conduits from as deep as the mantle to the Earth’s surface and as such provide direct windows to processes at depth. The Hartoušov mofette, located at the western marg
Externí odkaz:
https://doaj.org/article/1918a08550ca4bf691f673f605cff1ae
Akademický článek
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Since there is no doubt that soil compaction can induce substantial changes in the soil properties, affecting all kinds of physical, chemical, and biological processes in soils, it is worth some effort to attempt to characterize these changes quantit
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ef88ffe0c6c7afd551fe3eaeee00ed75
https://doi.org/10.5194/egusphere-egu23-8501
https://doi.org/10.5194/egusphere-egu23-8501
While there are many methods available for the characterization of pore space of soils, most of them are not suitable for observing the gradual changes of the pore sizes of a given sample during the process of its compaction. Non-Newtonian fluids hav
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::11e28b0918c187c38226067b4d44a1f6
https://doi.org/10.5194/egusphere-egu23-7426
https://doi.org/10.5194/egusphere-egu23-7426
Autor:
Martin Slavík, Martin Lanzendörfer
The characteristics of the pore space are considered a key factor in susceptibility of the stone to various weathering processes. The pore size distribution can be determined by a number of methods such as mercury intrusion porosimetry or computed to
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::65d5955736c001cd9c8f1771ac9b08a8
https://doi.org/10.5194/egusphere-egu23-5956
https://doi.org/10.5194/egusphere-egu23-5956
Publikováno v:
PAMM. 22
Autor:
Heiko Woith, Josef Vlček, Tomáš Vylita, Torsten Dahm, Tomáš Fischer, Kyriaki Daskalopoulou, Martin Zimmer, Samuel Niedermann, Jessica A. Stammeier, Veronika Turjaková, Martin Lanzendörfer
Publikováno v:
Geosciences
Geosciences; Volume 13; Issue 1; Pages: 2
Geosciences; Volume 13; Issue 1; Pages: 2
Mofettes are gas emission sites where high concentrations of CO2 ascend through conduits from as deep as the mantle to the Earth’s surface and as such provide direct windows to processes at depth. The Hartoušov mofette, located at the western marg
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::5ececa4ee11915616dcbf14e9a0886d9
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5014593
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5014593
Zbraslav sand has been used as a testing material in many former soil mechanics studies. It is a poorly graded sand with almost no fines and with grains of subangular shape. We will be interested in predicting the variation of its pore structure, in
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::51e657a2665e08c56279f9145a14f507
https://doi.org/10.5194/egusphere-egu22-11649
https://doi.org/10.5194/egusphere-egu22-11649