<mets:mets OBJID="eprint_6579" LABEL="Eprints Item" xsi:schemaLocation="http://www.loc.gov/METS/ http://www.loc.gov/standards/mets/mets.xsd http://www.loc.gov/mods/v3 http://www.loc.gov/standards/mods/v3/mods-3-3.xsd" xmlns:mets="http://www.loc.gov/METS/" xmlns:mods="http://www.loc.gov/mods/v3" xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance"><mets:metsHdr CREATEDATE="2023-07-05T13:08:05Z"><mets:agent ROLE="CUSTODIAN" TYPE="ORGANIZATION"><mets:name>OAR@ICRISAT</mets:name></mets:agent></mets:metsHdr><mets:dmdSec ID="DMD_eprint_6579_mods"><mets:mdWrap MDTYPE="MODS"><mets:xmlData><mods:titleInfo><mods:title>Impact of Climate Change in Soils of Semi-Arid Tropics (SAT)</mods:title></mods:titleInfo><mods:name type="personal"><mods:namePart type="given">D K</mods:namePart><mods:namePart type="family">Pal</mods:namePart><mods:role><mods:roleTerm type="text">author</mods:roleTerm></mods:role></mods:name><mods:name type="personal"><mods:namePart type="given">D</mods:namePart><mods:namePart type="family">Sarkar</mods:namePart><mods:role><mods:roleTerm type="text">author</mods:roleTerm></mods:role></mods:name><mods:name type="personal"><mods:namePart type="given">T</mods:namePart><mods:namePart type="family">Bhattacharyya</mods:namePart><mods:role><mods:roleTerm type="text">author</mods:roleTerm></mods:role></mods:name><mods:name type="personal"><mods:namePart type="given">S C</mods:namePart><mods:namePart type="family">Datta</mods:namePart><mods:role><mods:roleTerm type="text">author</mods:roleTerm></mods:role></mods:name><mods:name type="personal"><mods:namePart type="given">P</mods:namePart><mods:namePart type="family">Chandran</mods:namePart><mods:role><mods:roleTerm type="text">author</mods:roleTerm></mods:role></mods:name><mods:name type="personal"><mods:namePart type="given">S K</mods:namePart><mods:namePart type="family">Ray</mods:namePart><mods:role><mods:roleTerm type="text">author</mods:roleTerm></mods:role></mods:name><mods:abstract>The review o f research results on Indian major soil types under semi-arid&#13;
tropics (SAT) indicates that climate change from humid to arid occurred in the&#13;
Peninsular regions o f India during the Holocene period. This change is being&#13;
realized in the rise in mean annual temperature (MAT) and decrease in mean&#13;
annual rainfall (MAR). The prevailing arid climatic adversities favoured the&#13;
sequestration o f inorganic carbon as CaC03 with concomitant development of&#13;
soil sodicity in major soil types o f India, representing regressive pedogenesis.&#13;
As a result, crop productivity in these soils often has reduced to less than 50%.&#13;
Thus the regressive pedogenetic processes under SAT environments pose a&#13;
threat to agriculture being an unfavourable natural endowment that will ever&#13;
demand for extra resources for raising crops (especially the winter crops) by&#13;
the resource poor farmers in the naturally degraded soils.</mods:abstract><mods:classification authority="lcc">Soil Science</mods:classification><mods:classification authority="lcc">Climate Change</mods:classification><mods:originInfo><mods:dateIssued encoding="iso8061">2013</mods:dateIssued></mods:originInfo><mods:originInfo><mods:publisher>Studium Press India Pvt Ltd</mods:publisher></mods:originInfo><mods:genre>Book Section</mods:genre></mets:xmlData></mets:mdWrap></mets:dmdSec><mets:amdSec ID="TMD_eprint_6579"><mets:rightsMD ID="rights_eprint_6579_mods"><mets:mdWrap MDTYPE="MODS"><mets:xmlData><mods:useAndReproduction>
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