Red ferruginous soils of tropical Indian environments: A review of the pedogenic processes and its implications for edaphology

cg.contactpaldilip2001@yahoo.comen_US
cg.contributor.centerIndian Council of Agricultural Research, National Bureau of Soil Survey and Land Use Planning - ICAR- NBSS&LUPen_US
cg.contributor.centerInternational Crops Research Institute for the Semi-Arid Tropics - ICRISATen_US
cg.contributor.centerUniversity of Delhien_US
cg.contributor.crpCRP on Dryland Systems - DSen_US
cg.contributor.funderNot Applicableen_US
cg.coverage.countryINen_US
cg.coverage.regionSouthern Asiaen_US
cg.date.embargo-end-date2018-06-17en_US
cg.identifier.doihttps://dx.doi.org/10.1016/j.catena.2014.05.023en_US
cg.isijournalISI journalen_US
cg.issn0341-8162en_US
cg.journalCatenaen_US
cg.subject.agrovocsoilen_US
cg.subject.agrovocalfisolsen_US
cg.subject.agrovocpedologyen_US
cg.subject.agrovoctropical soilsen_US
cg.subject.agrovocmollisolsen_US
cg.subject.agrovocultisolsen_US
cg.volume121en_US
dc.contributorWani, Suhasen_US
dc.contributorSahrawat, Kanwar Lalen_US
dc.contributorSrivastava, Pankajen_US
dc.creatorPal, Dilip Kumaren_US
dc.date.accessioned2017-01-09T21:19:08Z
dc.date.available2017-01-09T21:19:08Z
dc.description.abstractRed ferruginous (RF) soils of tropical Indian environments belong to Entisols, Inceptisols, Alfisols, Mollisols and Ultisols soil orders. The occurrence of Ultisols alongside acidic Alfisols and Mollisols in both zeolitic and nonzeolitic parent materials in humid tropical (HT) climatic environments, indicates that the soil diversity in India is large. These soils are not confined to a single production systemand generally maintain a positive organic carbon (OC) balance without adding significantly to greenhouse gas emissions. This review presents a synthesis of literature on the recent developments on the pedology of RF soils, including their physical, chemical, biological, mineralogical and micro-morphological properties, and their degradation status. It also addresses the changes in soil properties in semi-arid tropical (SAT) areas, created by climate shift during the Holocene. This knowledge contributed to our understanding as to howthe parentmaterial composition influences the formation of Alfisols, Mollisols and Ultisols inweathering environments of HT climate; and also as to howthe relict Alfisols of SAT areas are polygenetic. The state-of-the-art information developed through the extensivework on such soils has helped establish an organic link between pedogenetic processes and bulk soil properties, and has provided an insight of many pedological and edaphological issues related to Alfisols, Mollisols and Ultisols mainly of HT climate. The synthesis has helped us to understand as to why the formation of Oxisols from Ultisols is an improbable genetic pathway in tropical environment of India and elsewhere in the world. There is a strong need to modify the mineralogy class of highlyweathered RF soils.We hope this review will help to dispel some of the myths on the formation of tropical soils and their low fertility by putting in context their characteristics and capacity to be productiveen_US
dc.formatPDFen_US
dc.identifierhttp://oar.icrisat.org/id/eprint/8129en_US
dc.identifierhttps://mel.cgiar.org/reporting/downloadmelspace/hash/mpjm3DeQ/v/f5c958a4f6772afe1e90b19e712c125een_US
dc.identifier.citationDilip Kumar Pal, Suhas Wani, Kanwar Lal Sahrawat, Pankaj Srivastava. (17/6/2014). Red ferruginous soils of tropical Indian environments: A review of the pedogenic processes and its implications for edaphology. Catena, 121, pp. 260-278.en_US
dc.identifier.statusLimited accessen_US
dc.identifier.urihttps://hdl.handle.net/20.500.11766/5390
dc.languageenen_US
dc.publisherElsevieren_US
dc.rightsCC-BY-NC-4.0en_US
dc.sourceCatena;121,(2014) Pagination 260,278en_US
dc.subjectedaphologyen_US
dc.titleRed ferruginous soils of tropical Indian environments: A review of the pedogenic processes and its implications for edaphologyen_US
dc.typeJournal Articleen_US
dcterms.available2014-06-17en_US
dcterms.extent260-278en_US
mel.impact-factor2.612en_US

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