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Simultaneous determination of water retention curve and unsaturated hydraulic conductivity of substrates using a steady-state laboratory method

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dc.contributor.author Londra, PA en
dc.date.accessioned 2014-06-06T06:50:42Z
dc.date.available 2014-06-06T06:50:42Z
dc.date.issued 2010 en
dc.identifier.issn 00185345 en
dc.identifier.uri http://62.217.125.90/xmlui/handle/123456789/5127
dc.relation.uri http://www.scopus.com/inward/record.url?eid=2-s2.0-77954836891&partnerID=40&md5=4949d69c124df926ec3ab65d32656ad4 en
dc.subject Coir en
dc.subject Hydraulic properties en
dc.subject Peat en
dc.subject Perlite en
dc.subject Steady-state profiles en
dc.title Simultaneous determination of water retention curve and unsaturated hydraulic conductivity of substrates using a steady-state laboratory method en
heal.type journalArticle en
heal.publicationDate 2010 en
heal.abstract For effective irrigation and fertilization management, the knowledge of substrate hydraulic properties is essential. In this study, a steady-state laboratory method was used to determine simultaneously the water retention curve, θ(h), and unsaturated hydraulic conductivity as a function of volumetric water content, K(θ), and water pressure head, K(h), of five substrates used widely in horticulture. The substrates examined were pure peat, 75/25 peat/perlite, 50/50 peat/perlite, 50/50 coir/perlite, and pure perlite. The experimental retention curve results showed that in the case of peat and its mixtures with perlite, there is a hysteresis between drying and wetting branches of the retention curve. Whereas in the case of coir/perlite and perlite, the phenomenon of hysteresis was less pronounced. The increase of perlite proportion in the peat/perlite mixtures led to a decrease of total porosity and water-holding capacity and an increase of air space. Study of the K(θ) and K(h) experimental data showed that the hysteresis phenomenon of K(θ) was negligible compared with the K(h) data for all substrates examined. Within a narrow range of water pressure head (0 to -70 cm H2O) that occurs between two successive irrigations, a sharp decrease of the unsaturated hydraulic conductivity was observed. The comparison of the K(θ) experimental data between the peat-based substrate mixtures and the coir-based substrate mixture showed that for water contents lower than 0.40 m3·m-3, the hydraulic conductivity of the 50/50 coir/perlite mixture was greater. The comparison between experimental water retention curves and predictions using Brooks-Corey and van Genuchten models showed a high correlation (0.992 ≤ R2 ≤ 1) for both models for all substrates examined. On the other hand, in the case of unsaturated hydraulic conductivity, the comparison showed a relatively good correlation (0.951≤R2≤0.981) for the van Genuchten-Mualem model for all substrates used except perlite and a significant deviation (0.436≤R2≤0.872) for the Brooks-Corey model for all substrates used. en
heal.journalName HortScience en
dc.identifier.issue 7 en
dc.identifier.volume 45 en
dc.identifier.spage 1106 en
dc.identifier.epage 1112 en


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