<mets:mets OBJID="eprint_3966" 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="2023-07-05T16:11:52Z"><mets:agent ROLE="CUSTODIAN" TYPE="ORGANIZATION"><mets:name>OAR@ICRISAT</mets:name></mets:agent></mets:metsHdr><mets:dmdSec ID="DMD_eprint_3966_mods"><mets:mdWrap MDTYPE="MODS"><mets:xmlData><mods:titleInfo><mods:title>Relationships between soil urease activity and other properties of some tropical wetland rice soils</mods:title></mods:titleInfo><mods:name type="personal"><mods:namePart type="given">K L</mods:namePart><mods:namePart type="family">Sahrawat</mods:namePart><mods:role><mods:roleTerm type="text">author</mods:roleTerm></mods:role></mods:name><mods:abstract>Simple correlation analyses of urease activity with properties of ten Philippine wetland rice soils differing widely in pH, texture and organic matter indicated that urease activity was correlated highly significantly with total N (r = 0.91)**, and organic C (r = 0.89**) but was not significantly correlated with CEC, clay, pH active Fe or active Mn content. Multiple regression anslyses showed that organic matter content of soils measured by oroganic C and total N accounted for most of the variation in urease activity</mods:abstract><mods:classification authority="lcc">Soil Science</mods:classification><mods:originInfo><mods:dateIssued encoding="iso8061">1983</mods:dateIssued></mods:originInfo><mods:originInfo><mods:publisher>Kluwer Academic Publishers</mods:publisher></mods:originInfo><mods:genre>Article</mods:genre></mets:xmlData></mets:mdWrap></mets:dmdSec><mets:amdSec ID="TMD_eprint_3966"><mets:rightsMD ID="rights_eprint_3966_mods"><mets:mdWrap MDTYPE="MODS"><mets:xmlData><mods:useAndReproduction>
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