Salt dynamics, leaching requirements, and leaching fractions during irrigation of a halophyte with different saline waters

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dc.citation.issue1
dc.citation.volume62
dc.contributor.authorAl-Tamimi M
dc.contributor.authorGreen S
dc.contributor.authorDahr WA
dc.contributor.authorAl-Muaini A
dc.contributor.authorLyra D
dc.contributor.authorAmmar K
dc.contributor.authorDawoud M
dc.contributor.authorKenyon P
dc.contributor.authorKemp P
dc.contributor.authorKennedy L
dc.contributor.authorClothier B
dc.contributor.editorMcGrath G
dc.date.accessioned2024-09-18T20:48:10Z
dc.date.available2024-09-18T20:48:10Z
dc.date.issued2023-12-18
dc.description.abstractContext More than 830 million ha of soils are salt affected, representing around 9% of the world’s land surface. Groundwater high in salt already covers some 16% of the land area. Saline water can be used effectively for irrigation by salt leaching to despatch the accumulated salts, but this can pose a risk of salinisation of groundwater. It is important that the efficacy of salt leaching is confirmed, and the impacts of salt loading below the rootzone can be assessed. Aims We examine the efficiency and impact of salt leaching to remove salt from the rootzone. Methods Our soil, a Typic Torripsamment, is the dominant soil across the Arabian Peninsula. We carried out detailed laboratory experiments of salt leaching dynamics via salt breakthrough curves, analytical modelling, and through the field monitoring of impacts. Key results Analytical solutions well predicted the salt breakthrough curves from repacked soil columns in the laboratory and we were able to confirm that all of the soil’s water was actively involved in transport, and that salt behaved as an inert tracer. The breakthrough curves were well predicted using a small solute dispersivity, so piston displacement was found to be a good assumption. Salt was easily flushed from the columns. To back this up in the field, soil sampling was carried out down to 1 m across 36 profiles after the harvest of a halophytic crop irrigated with saline water. Salt storage was only 1.8 kg m−2, even though 80 kg m−2 had been applied. This is a positive result for managing irrigation. Conclusions Salt leaching can maintain equable salinity in the rootzone. However, this leaching carried salt back to groundwater at 2–3 times the concentration of the applied water. We confirmed that the amount of salt leaching back to groundwater can be significant. Implications This salt dilemma will require careful management to achieve crop yields and protect the environment.
dc.description.confidentialfalse
dc.identifier.citationAl-Tamimi M, Green S, Dahr WA, Al-Muaini A, Lyra D, Ammar K, Dawoud M, Kenyon P, Kemp P, Kennedy L, Clothier B. (2023). Salt dynamics, leaching requirements, and leaching fractions during irrigation of a halophyte with different saline waters. Soil Research. 62. 1.
dc.identifier.doi10.1071/SR23173
dc.identifier.eissn1838-6768
dc.identifier.elements-typejournal-article
dc.identifier.issn1838-675X
dc.identifier.numberSR23173
dc.identifier.urihttps://mro.massey.ac.nz/handle/10179/71488
dc.languageEnglish
dc.publisherCSIRO Publishing
dc.publisher.urihttps://www.publish.csiro.au/SR/SR23173
dc.relation.isPartOfSoil Research
dc.rights(c) 2024 The Author/s
dc.rightsCC BY-NC-ND 4.0
dc.rights.urihttps://creativecommons.org/licenses/by-nc-nd/4.0/
dc.subjectconvection-dispersion
dc.subjectleaching fraction
dc.subjectmobile–immobile pore-water
dc.subjectpiston displacement
dc.subjectresidual salts
dc.subjectsaline irrigation
dc.subjectsalt breakthrough analysis
dc.subjectsalt-leaching requirements
dc.titleSalt dynamics, leaching requirements, and leaching fractions during irrigation of a halophyte with different saline waters
dc.typeJournal article
pubs.elements-id487686
pubs.organisational-groupCollege of Health
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