Zobrazeno 1 - 6
of 6
pro vyhledávání: '"Rachel Jorand"'
Autor:
Daniel Ferry, Eric Chaput, Yann Magnin, Rachel Jorand, Jérémie Berthonneau, Olivier Grauby, Nicolas Chanut, Roland J.-M. Pellenq, Franz J. Ulm
Publikováno v:
ACS Applied Nano Materials
ACS Applied Nano Materials, American Chemical Society, 2020, 3 (8), pp.7604-7610. ⟨10.1021/acsanm.0c01191⟩
ACS Applied Nano Materials, 2020, 3 (8), pp.7604-7610. ⟨10.1021/acsanm.0c01191⟩
ACS Applied Nano Materials, American Chemical Society, 2020, 3 (8), pp.7604-7610. ⟨10.1021/acsanm.0c01191⟩
ACS Applied Nano Materials, 2020, 3 (8), pp.7604-7610. ⟨10.1021/acsanm.0c01191⟩
International audience; Methane diffusion in micro- and mesopores of carbonaceous materials is dominated by molecular interactions with the pore walls. As a consequence, the fluid molecules are mainly in a diffusive regime and the laws of fluid mecha
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::98c3030f520044477353775f421cb880
https://hal.archives-ouvertes.fr/hal-02932903/document
https://hal.archives-ouvertes.fr/hal-02932903/document
Publikováno v:
Hydrology and Earth System Sciences, Vol 19, Iss 6, Pp 2763-2773 (2015)
Hydrology and earth system sciences 19(6), 2763-2773 (2015). doi:10.5194/hess-19-2763-2015
Hydrology and earth system sciences 19(6), 2763-2773 (2015). doi:10.5194/hess-19-2763-2015
Nuclear Magnetic Resonance (NMR) relaxometry measurements are commonly used to characterize the storage and transport properties of water-saturated rocks. These assessments are based on the proportionality of NMR signal amplitude and relaxation time
Publikováno v:
Geothermics. 53:413-428
We present a comprehensive statistical analysis of petrophysical properties of rocks of the northeastern Rhenish Massif and the Lower Rhine Embayment in Germany. Properties measured comprise thermal conductivity, specific heat capacity density, poros
Publikováno v:
Journal of Geophysical Research: Solid Earth. 118:5225-5235
[1] Studying heat transfer processes in sedimentary crustal rocks requires the correct thermal conductivity of the respective rock type. Often a single value is used for a given rock type, obtained from the measurements on homogenous samples. We demo
Autor:
Bruno Goutorbe, Rachel Jorand, Hélène Bouquerel, Francis Lucazeau, Jean-Claude Mareschal, Frederique Rolandone, Sylvie Leroy
Publikováno v:
Tectonophysics
Tectonophysics, Elsevier, 2013, 589, pp.77-89. ⟨10.1016/j.tecto.2012.12.034⟩
Tectonophysics, 2013, 589, pp.77-89. ⟨10.1016/j.tecto.2012.12.034⟩
Tectonophysics, Elsevier, 2013, 589, pp.77-89. ⟨10.1016/j.tecto.2012.12.034⟩
Tectonophysics, 2013, 589, pp.77-89. ⟨10.1016/j.tecto.2012.12.034⟩
International audience; The present-day thermal regime of the Arabian plate is affected by the dynamics of the Afar plume and the rifting of the Red Sea and the Gulf of Aden. The Arabian plate is a Precambrian Shield and its thermal regime, before th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::58ea642cbc2d23956b39e22bd678f842
https://hal.archives-ouvertes.fr/hal-01437595
https://hal.archives-ouvertes.fr/hal-01437595
Publikováno v:
Journal of Geophysical Research. 116
[1] In this paper, we present a method that allows one to correct thermal conductivity measurements for the effect of water loss when extrapolating laboratory data to in situ conditions. The water loss in shales and unconsolidated rocks is a serious