Water-harvesting designs for fruit tree production in dry environments

cg.contacta.tubeileh@cgiar.orgen_US
cg.contributor.centerInternational Center for Agricultural Research in the Dry Areas - ICARDAen_US
cg.contributor.funderGerman Federal Ministry for Economic Cooperation and Development - BMZen_US
cg.contributor.projectCommunication and Documentation Information Services (CODIS)en_US
cg.contributor.project-lead-instituteInternational Center for Agricultural Research in the Dry Areas - ICARDAen_US
cg.date.embargo-end-dateTimelessen_US
cg.identifier.doihttps://dx.doi.org/10.1016/j.agwat.2015.11.006en_US
cg.isijournalISI Journalen_US
cg.issn0378-3774en_US
cg.journalAgricultural Water Managementen_US
cg.subject.agrovocwater managementen_US
cg.subject.agrovocfruit treesen_US
cg.subject.agrovocOliveen_US
cg.volume165en_US
dc.contributorBruggeman, Adrianaen_US
dc.contributorTurkelboom, Francisen_US
dc.creatorTubeileh, Ashrafen_US
dc.date.accessioned2021-01-21T21:57:19Z
dc.date.available2021-01-21T21:57:19Z
dc.description.abstractWater scarcity and increasing demand coupled with climate change require maximizing the use of available resources. Water harvesting (WH) systems are currently being used in many areas to sustain crops and increase water productivity. This study investigated the effect of three treatments (S15: 50-m(2) catchment area with 15% slope, S8: 50-m(2) catchment area with 8% slope, and L8: 70-m(2) catchment area with 8% slope) on the amount of water harvested in tree basin for young olive (Olea europaea L.) trees from November 2002 to July 2003. Soil moisture was monitored weekly during the rainy season and bi-weekly afterwards. To determine moisture changes in the catchment and target areas and amount of water harvested (in liters) for each tree, volumetric soil moisture content was measured at three or four points along the slope using a neutron probe down to a maximum depth of 120 cm, as soil depth allowed. WH structures increased soil moisture content in the rootzone compared to the catchment area. The rainfall threshold for runoff generation was less than 15 mm. Land slope was more important than micro catchment size for increasing the amount of water harvested. Compared to the 8% slope, the 15% slope resulted in larger harvested amounts for small storms, but the two were comparable when storms were large. The large micro-catchment size resulted in higher amounts of harvested water only in the presence of storms greater than 26 mm. After adding the amounts lost by evapotranspiration, the net amount of water harvested in the tree basin of each tree for the 2002-2003 rainy season reached 722 and 6881 (or 361 and 344mm) for treatments S15 and S8, respectively. Deeper soil profiles (i.e., >90 cm) were important to ensure longer storage periods. By early July, soil moisture content in the tree basin for treatments S15, L8 and S8 was still higher by 38, 13, and 5% respectively, than the levels recorded at the onset of the experiment. WH increased soil moisture content during the spring and early summer, a critical period for olive production. 2015 Elsevier B.V. All rights reserved.en_US
dc.identifierhttps://mel.cgiar.org/dspace/limiteden_US
dc.identifier.citationAshraf Tubeileh, Adriana Bruggeman, Francis Turkelboom. (24/11/2015). Water-harvesting designs for fruit tree production in dry environments. Agricultural Water Management, 165, pp. 190-197.en_US
dc.identifier.statusTimeless limited accessen_US
dc.identifier.urihttps://hdl.handle.net/20.500.11766/12380
dc.languageenen_US
dc.publisherElsevier (12 months)en_US
dc.sourceAgricultural Water Management;165,(2015) Pagination 190-197en_US
dc.subjectdry areasen_US
dc.subjecthillslopes olive treesen_US
dc.subjectsoil moisture contenten_US
dc.titleWater-harvesting designs for fruit tree production in dry environmentsen_US
dc.typeJournal Articleen_US
dcterms.available2015-11-24en_US
dcterms.extent190-197en_US
mel.impact-factor4.021en_US

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