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- > ZAVALA, L.M., (Editeur scientifique)[a1] (supprimer)
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Par Collection Par Auteur- DOERR, S.H., (Editeur scientifique) (4)
- JORDÁN, A., (Editeur scientifique) (4)
- MATAIX-SOLERA, J., (Editeur scientifique) (4)
- ZAVALA, L.M., (Editeur scientifique) (4)
- ABKENAR, K.T. (1)
- ARCENEGUI, V. (1)
- BODÍ, M.B. (1)
- CASELLES, P. (1)
- CERDÀ, A. (1)
- CZACHOR, H. (1)
- DOERR, S.H. (1)
- DRONGOVÁ, Z. (1)
- HALLETT, P.D. (1)
- HOMOLÁK, M. (1)
- JORDÁN, M.M. (1)
- KOVACIK, L. (1)
- MALKINSON, D. (1)
- MARTÍNEZ, C. (1)
- MATAIX-SOLERA, J. (1)
- MATAIX-SOLERA, J. (1)
- 2013 (4)
- Alga ; Duna ; Encostramiento ; Eslovaquia ; Experimentación ; Infiltración ; Propiedades del suelo ; Suelo ; Suelo arenoso (1)
- Algae ; Dune ; Duricrust ; Experimentation ; Infiltration ; Repellency ; Sandy soil ; Slovak Republic ; Soil ; Soil properties (1)
- Algue ; Dune ; Encroûtement ; Expérimentation ; Imperméabilité ; Infiltration ; Propriétés du sol ; Slovaquie ; Slovaquie du Sud-Ouest ; Sol ; Sol sableux (1)
- Alicante ; Arid area ; Comparative study ; Forest fire ; Impact ; Israel ; Mediterranean area ; Repellency ; Soil ; Soil properties ; Spain ; Terra rossa ; Valencian Community (1)
- Alicante ; Ash ; Forest fire ; Geochemistry ; Mediterranean area ; Repellency ; Soil ; Soil properties ; Spain ; Spectroscopy ; Valencia ; Valencian Community (1)
- Alicante ; Cendre ; Comunidad Valenciana ; Domaine méditerranéen ; Espagne ; Géochimie ; Imperméabilité ; Incendie de forêt ; Propriétés du sol ; Sol ; Spectroscopie ; Valencia (1)
- Alicante ; Comunidad Valenciana ; Domaine aride ; Domaine méditerranéen ; Espagne ; Etude comparée ; Impact ; Imperméabilité ; Incendie de forêt ; Israël ; Propriétés du sol ; Sol ; Terra rossa (1)
- Bosque ; Especie vegetal ; Gilán ; Humedad del suelo ; Irán ; Propiedades del suelo ; Suelo ; Variación estacional (1)
- Campo mediterráneo ; Campo árido ; España ; Estudio comparativo ; Impacto ; Incendio forestal ; Israel ; Propiedades del suelo ; Suelo ; Terra rossa (1)
- Campo mediterráneo ; España ; Geoquímica ; Incendio forestal ; Propiedades del suelo ; Suelo (1)
- Espèce végétale ; Forêt ; Gīlān ; Humidité du sol ; Imperméabilité ; Iran ; Propriétés du sol ; Sol ; Variation saisonnière (1)
- Forest ; Gilan ; Iran ; Plant species ; Repellency ; Seasonal variation ; Soil ; Soil moisture ; Soil properties (1)
- Soil water repellency (4)
- Algae influence the hydrophysical parameters of a sandy soil (1)
- FT-IR spectroscopy reveals that ash water repellency is highly dependent on ash chemical composition (1)
- Relationship between soil water repellency and some of soil properties in northern Iran (1)
- Soil properties as key factors controlling water repellency in fire-affected areas : evidences from burned sites in Spain and Israel (1)
FT-IR spectroscopy reveals that ash water repellency is highly dependent on ash chemical composition
- and number of water repellent samples within the four locations. In all FT-IR spectra obtained, the absorbance bands assigned to organic matter and carbonates were dominant. Organic matter content in all water repellent ash samples was more than twice
- the carbonate content. From the results obtained it is concluded that the water repellency or wettability of wildfire ash is driven by the ratio of remaining organic matter to emerging carbonates, which in turn, is related to fire severity.
- , organic matter contents and pH levels. In the field, the actual water repellency was determined using the Water Drop Penetration Time Test (WDPT) but the same test was used to determine the potential water repellency after drying process for several days
- when soil becomes so dry. The results show that soil organic matter content, texture and pH are important factors for developing SWR in soil.
- to a control soil (Pure sand) with limited impact of vegetation or organic matter, occurring at 50 cm depth beneath a glade area. The hydrophysical parameters were substantially different between the 2 surfaces. The growth of artificial algal crusts resulted
- . It is highlighted that organic matter, clay content and mineralogy of clay were the main key factors; Kaolinite seems to be one of the main responsible for the lower WR values found.