Salt-Affected Soils and Marginal Waters 2021
DOI: 10.1007/978-3-030-78435-5_7
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Nutrient Management in Salt-affected Soils

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Cited by 13 publications
(16 citation statements)
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“…The color change from dark black to brown in soil after gypsum and farmyard manure application to salt-affected sodic soils can be attributed to several factors [ 110 ]. These include the displacement of sodium by calcium, oxidation of organic matter, chemical reactions with iron, and leaching of salts [ 111 , 112 ].…”
Section: Resultsmentioning
confidence: 99%
“…The color change from dark black to brown in soil after gypsum and farmyard manure application to salt-affected sodic soils can be attributed to several factors [ 110 ]. These include the displacement of sodium by calcium, oxidation of organic matter, chemical reactions with iron, and leaching of salts [ 111 , 112 ].…”
Section: Resultsmentioning
confidence: 99%
“…Irrigation methods with poor quality of water alongside inefficient drainage systems are recognized as the main cause of secondary salinity. Irrigation with inadequate quality and quantity of water increases leakage rising and sea water intrusion in the over-exploited groundwater [19,20]. Due to salt migration in the top and lower soil layers, deforestation, clearance of vegetation, and changes in land use are also regarded as key contributors to land salinization and alkalization [21].…”
Section: Soil Salinizationmentioning
confidence: 99%
“…The formation of very hard layers that are impermeable to water and crop roots, as well as phosphorus fixation fertilizer in calcareous soils, can result in areas with the highest CaCO 3 values [92]. The range of ESP values is 3.22% to 24.94%, with an average of 11.27 ± 6.06%, indicating sodicity hazards in the area [93]. The upper northwest of the research area has seen an increase in the spatial patterns of EC and ESP (Figure S1a,c).…”
Section: Soil Characteristics In the Study Areamentioning
confidence: 99%