English   español  
Please use this identifier to cite or link to this item: http://hdl.handle.net/10261/125971
Share/Impact:
Statistics
logo share SHARE logo core CORE   Add this article to your Mendeley library MendeleyBASE

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

Effective run-off flow length over biological soil crusts on silty loam soils in drylands

AuthorsLázaro, Roberto ; Calvo-Cases, Adolfo; Lázaro, Amparo ; Molina, Isabel
KeywordsAntecedent soil moisture
Biocrusts
Rainfall intensity
Rainfall simulation
Run-off connectivity
Tabernas desert
Issue Date3-Dec-2014
PublisherJohn Wiley & Sons
CitationHydrological Processes 29(11): 2534-2544 (2015)
Abstract© 2014 John Wiley & Sons, Ltd. Surface hydrological behaviour is important in drylands because it affects the distribution of soil moisture and vegetation and the hydrological functioning of slopes and catchments. Microplot scale run-off can be relatively easily measured, i.e. by rainfall simulations. However, slope or catchment run-off cannot be deduced from microplots, requiring long-time monitoring, because run-off coefficients decrease with increasing drainage area. Therefore, to determine the slope length covered by run-off (run-off length) is crucial to connect scales. Biological soil crusts (BSCs) are good model systems, and their hydrology at slope scale is insufficiently known. This study provides run-off lengths from BSCs, by field factorial experiments using rainfall simulation, including two BSC types, three rain types, three antecedent soil moistures and four plot lengths. Data were analysed by generalized linear modelling, including vascular plant cover as covariates. Results were the following: (i) the real contributing area is almost always much smaller than the topographical contributing area; (ii) the BSC type is key to controlling run-off; run-off length reached 3m on cyanobacterial crust, but hardly over 1m on lichen crust; this pattern remained through rain type or soil moisture; (iii) run-off decreased with BSC development because soil sealing disappears; porosity, biomass and roughness increase and some changes occur in the uppermost soil layer; and (iv) run-off flow increased with both rain type and soil moisture but run-off coefficient only with soil moisture (as larger rains increased both run-off and infiltration); vascular plant cover had a slight effect on run-off because it was low and random.
Publisher version (URL)http://dx.doi.org/10.1002/hyp.10345
URIhttp://hdl.handle.net/10261/125971
DOI10.1002/hyp.10345
Identifiersdoi: 10.1002/hyp.10345
issn: 1099-1085
Appears in Collections:(IMEDEA) Artículos
(EEZA) Artículos
Files in This Item:
File Description SizeFormat 
accesoRestringido.pdf15,38 kBAdobe PDFThumbnail
View/Open
Show full item record
Review this work
 

Related articles:


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