English   español  
Please use this identifier to cite or link to this item: http://hdl.handle.net/10261/141241
Share/Impact:
Statistics
logo share SHARE   Add this article to your Mendeley library MendeleyBASE

Visualizar otros formatos: MARC | Dublin Core | RDF | ORE | MODS | METS | DIDL
Exportar a otros formatos:
Title

Influence of the wetting process on estimation of the water-retention curve of tilled soils

AuthorsMoret-Fernández, David ; Peña-Sancho, Carolina; López Sánchez, María Victoria
Keywordshydraulic properties
undisturbed soil samples
water holding capacity
Issue Date2016
PublisherCSIRO Publishing
CitationMoret-Fernández D, Peña-Sancho C, López MV. Influence of the wetting process on estimation of the water-retention curve of tilled soils. Soil Research 54 (7): 840-846 (2016)
AbstractCorrect estimation of the soil-water retention curve (WRC) is of paramount importance to characterise the hydraulic behaviour of soils. This paper studies the influence of two different soil-wetting processes (waterlogging soil, WP; capillary rise to saturation, CRP) on the estimate of the WRC. The two procedures were applied on undisturbed loam soil samples with three degrees of soil structure: (i) consolidated soils under conventional tillage (CT), reduced tillage (RT) and no tillage (NT); (ii) freshly tilled soil under CT and RT; and (iii) CT and RT after secondary tillage plus some intense rainfalls events. WRCs were estimated with time-domain reflectometry (TDR) pressure cells and volumetric water content was measured at saturation conditions (for the WP method) and at pressure heads of 0.5, 1.5, 3, 5, 10, 50, 100, 500 and 1500 kPa. The same cores were used to determine the soil bulk density (ρb), which was subsequently used to estimate the saturated water content under CRP. The ρb value of the consolidated soil under NT was significantly higher (P < 0.001) than under CT and RT. No effect of the wetting process on the WRC of consolidated soils was observed. Only the freshly tilled soil samples under RT were significantly affected by the wetting process. In these cases, the water draining after WP collapsed the more unstable soil macropores and increased the volume of the smaller ones. However, this effect was minimised by the CRP method, which prevented the collapse of the more unstable soil pores. This work demonstrates that the soil-wetting process may have an important effect on the characterisation of the water-holding capacity on freshly tilled soils.
Description18 Pags.- 1 Tabl.- 3 Figs. The definitive version is available at: http://www.publish.csiro.au/sr
Publisher version (URL)http://dx.doi.org/10.1071/SR15274
URIhttp://hdl.handle.net/10261/141241
DOI10.1071/SR15274
ISSN1838-675X
E-ISSN1838-6768
Appears in Collections:(EEAD) Artículos
Files in This Item:
File Description SizeFormat 
MoretD_SoilRes_2016.pdf410,73 kBAdobe PDFThumbnail
View/Open
Show full item record
Review this work
 


WARNING: Items in Digital.CSIC are protected by copyright, with all rights reserved, unless otherwise indicated.