2006
DOI: 10.1016/j.geoderma.2006.04.021
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Formation and persistence of Mollisols on zeolitic Deccan basalt of humid tropical India

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Cited by 50 publications
(46 citation statements)
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“…These zeolitized soils, rich in Ca 2+ ions, are often calcareous 8,19 . These Ca-rich zeolites have been termed as natural soil modifiers 21,22 . Besides zeolites, SAT soils also contain another soil modifier like gypsum 13 .…”
Section: Natural Process Of Resilience In Sat Soilsmentioning
confidence: 99%
“…These zeolitized soils, rich in Ca 2+ ions, are often calcareous 8,19 . These Ca-rich zeolites have been termed as natural soil modifiers 21,22 . Besides zeolites, SAT soils also contain another soil modifier like gypsum 13 .…”
Section: Natural Process Of Resilience In Sat Soilsmentioning
confidence: 99%
“…In general, these calcareous Vertisols and their intergrades in India cover 229 million ha area (Pal et al, 2000a). However, many of these soils do not have CaCO 3 > 40% in their control section (Bhattacharyya et al, 2006, 2009b; Srivastava et al, 2002; Pal, 2003) (Fig. 2, Table 4).…”
Section: Vertisols and Their Classificationmentioning
confidence: 99%
“…Mollisols have also been reported from hilly regions of the southern peninsular and north‐eastern India (Krishnan et al, 1996; Das et al, 1996; Shiva Prasad et al, 1998). However, Mollisols of the humid tropical climatic conditions of the Western Ghats and Satpura Range developed on Deccan basalt are acidic and fairly weathered (Bhattacharyya et al, 2006; Table 3). This is in contrast to the commonly reported calcareous Mollisols (Fanning and Fanning, 1989).…”
Section: Organic Carbon Sequestration In Soils Of Tropical Climatementioning
confidence: 99%
“…This is in contrast to the commonly reported calcareous Mollisols (Fanning and Fanning, 1989). The Indian Mollisols of humid tropical climate contain Ca‐zeolites, which act as a source of base‐rich heulandites that helps them persist even in adverse humid tropical climate with mean annual rainfall ranging from 1,400 to 3,300 mm (Bhattacharyya et al, 2006). The loss of bases during the leaching of soils has thus been continuously replenished by the steady supply of bases from heulandites (Ca‐zeolites).…”
Section: Organic Carbon Sequestration In Soils Of Tropical Climatementioning
confidence: 99%
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