Zobrazeno 1 - 10
of 87
pro vyhledávání: '"PROPRIETE HYDRIQUE"'
Publikováno v:
European Journal of Soil Science. 56:375-388
Summary This paper describes the characteristic shrinkage curve of a soil as it dries. It also introduces a new method to measure specific soil moisture states such as permanent wilting point and field capacity using the shrinkage curve. The model co
Autor:
Thierry Desjardins, Michel Grimaldi, Eleusa Barros, Patrick Lavelle, Danielle Mitja, Max Sarrazin, Armand Chauvel
Publikováno v:
Applied Soil Ecology. 26:157-168
In Brazilian Amazonia there are 26 million hectares of degraded pastures. One of the causes of degradation is assumed to be alterations in soil structure that is partly determined by a reduction in soil macrofauna diversity. The objective of this cas
Publikováno v:
Understanding mountain soils : a contribution from mountain areas to the International Year of Soils 2015
Understanding mountain soils : a contribution from mountain areas to the International Year of Soils 2015, pp 95-96, 2015
Understanding mountain soils : a contribution from mountain areas to the International Year of Soils 2015, pp 95-96, 2015
International audience; In the highlands of southern Colombia and northern Ecuador, soils developed on volcanic ash deposits have specific properties: high water retention, high hydraulic conductivity and high carbon (C) contents. The main role of th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::54b54f0870bd4d7f4ada17bfac1a21d8
https://hal.archives-ouvertes.fr/hal-01349101
https://hal.archives-ouvertes.fr/hal-01349101
Autor:
Deeb, M., Grimaldi, Michel, Lerch, T.Z., Podwojewski, Pascal, Dubs, Florence, Gigon, A., Blouin, M.
Les technosols construits sont une alternative au prélèvement de terre végétale en milieu naturel. La gestion durable de ces technosols suppose de comprendre l'évolution de leurs propriétés hydriques. Nous avons analysé les courbes de retrait
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______932::fef9527dd95e4dc5a2e6f13dcc3f1571
http://www.documentation.ird.fr/hor/fdi:010065091
http://www.documentation.ird.fr/hor/fdi:010065091
The pressure plate method is a standard method for measuring the pF curves, also called soil water retention curves, in a large soil moisture range from saturation to a dry state corresponding to an applied pressure of near 1500 kPa. However, the pre
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______932::35e70ce01f49524a5b63ad5f666fb10a
http://www.documentation.ird.fr/hor/fdi:010063539
http://www.documentation.ird.fr/hor/fdi:010063539
Des échantillons cylindriques reconstitués de mélanges du sable de Fontainebleau avec différentes proportions d'argile (kaolinite et bentonite) ont été préparés et humidifiés, afin de suivre le retrait pendant leur dessiccation par un rétra
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______932::a20a83143dfd8ea2caeeaa32d3c1d74d
http://www.documentation.ird.fr/hor/fdi:010063583
http://www.documentation.ird.fr/hor/fdi:010063583
Publikováno v:
Water Resources Research. 32:3025-3031
The relationship between water content and water potential for a soil is termed its water retention curve. This basic hydraulic property is closely related to the soil pore size distribution, for which it serves as a conventional method of measuremen
Publikováno v:
(15)2013; EGU, European Geosciences Union, General Assembly 2013, Vienne, AUT, 2013-04-07-2013-04-12, 1 p.
Geophysical Research Abstracts
EGU, European Geosciences Union, General Assembly 2013
EGU, European Geosciences Union, General Assembly 2013, Apr 2013, Vienne, Austria
European Geosciences Union General Assembly 2013
European Geosciences Union General Assembly 2013, Apr 2013, Vienna, Austria. pp.1
Geophysical Research Abstracts
EGU, European Geosciences Union, General Assembly 2013
EGU, European Geosciences Union, General Assembly 2013, Apr 2013, Vienne, Austria
European Geosciences Union General Assembly 2013
European Geosciences Union General Assembly 2013, Apr 2013, Vienna, Austria. pp.1
International audience; Due to its position at the interface between the atmosphere and the vadose zone, the soil significantly contributes to the partitioning of rainfall into infiltration and overland flow, and, as a consequence, to the water feedi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::9d62f8068058cc6290b31e5b430b63f4
http://prodinra.inra.fr/record/367587
http://prodinra.inra.fr/record/367587
Publikováno v:
Water Resources Research. 31:2927-2943
To study relationships between soil hydraulic properties and soil structural properties, a computer micro model of soil is constructed. We present first a general method of building a two-dimensional porous structure, including both pores and particl
Autor:
Tetegan, Marion
Publikováno v:
Modélisation des propriétés de rétention en eau des sols caillouteux. Application à l'estimation spatialisée de la réserve utile, Université d'Orléans(2011)
Sciences du Vivant [q-bio]. Université d'Orléans, 2011. Français
Sciences du Vivant [q-bio]. Université d'Orléans, 2011. Français
Les sols sont définis comme étant caillouteux à partir d’une proportion supérieure à 35 % d’éléments grossiers. Les sols caillouteux - dont certains supportent des zones de grandes cultures - couvrent environ 30% de la superficie de l’Eu
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::8e2530ee7084857553d458e751f7e2c8
http://prodinra.inra.fr/record/40103
http://prodinra.inra.fr/record/40103