2015
DOI: 10.1016/j.geodrs.2015.01.006
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Soil properties and organic carbon distribution under different land uses in reclaimed sodic soils of North-West India

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Cited by 80 publications
(41 citation statements)
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“…It was highly sodic with high pH (1:2.5) of 10.3 and exchangeable sodium of 97% at 0–5 cm depth in 1970. ICAR-Central Soil Salinity Research Institute was established in 1969 and developed reclamation technologies particularly addition of gypsum and adoption of best management practices for cereals, thereby the soils were reclaimed and cultivation of crops started (Datta et al 2015). The soil of the experimental field was loam in texture, low in organic carbon with slightly alkaline pH.…”
Section: Methodsmentioning
confidence: 99%
“…It was highly sodic with high pH (1:2.5) of 10.3 and exchangeable sodium of 97% at 0–5 cm depth in 1970. ICAR-Central Soil Salinity Research Institute was established in 1969 and developed reclamation technologies particularly addition of gypsum and adoption of best management practices for cereals, thereby the soils were reclaimed and cultivation of crops started (Datta et al 2015). The soil of the experimental field was loam in texture, low in organic carbon with slightly alkaline pH.…”
Section: Methodsmentioning
confidence: 99%
“…Its values differed when estimated in soilwater (6.3-6.8, mean 6.5) suspensions. Variations in acidity among the soils were due to production of organic acids by decomposition of leaf litter and their difference in biochemical composition (Datta et al, 2015). Soil under Jhau plantation recorded the highest value (6.8 g kg -1 ) of OC followed by Sagun and Sissoo (5.8 g kg -1 ), Lamboo (5.7 g kg -1…”
Section: Physico-chemical Properties Of Cultivated Soilsmentioning
confidence: 98%
“…This was possibly due to the fact that higher clay and organic matter contained different functional groups like carboxyl, phenolic and enolic contributing to the exchange capacity of the soils (Deb et al, 2016). Depth increment gradually increased the soil pH and decreased OC content and CEC in the soils irrespective of cultivated soils (Table 2) (Datta et al, 2015;Deb et al, 2016). Physical properties of soils under forest trees: Relative proportion of sand, silt and clay ranged from 12.5-17.1, 32.8-38.0 and 47.7-50.8% with the mean values of 14.4, 35.5 and 49.4%, respectively in soils under forest trees categorized as silty clay (Table 3).…”
Section: Physico-chemical Properties Of Cultivated Soilsmentioning
confidence: 99%
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“…However, micronutrient status in the soils was not targeted in this study. Higher BD in RW cropping system might be due to low organic matter input and compaction by the heavy vehicles like tractors (Datta et al, 2015;Chaudhari et al, 2015a).…”
Section: Physicochemical Properties Of the Soilmentioning
confidence: 99%