<?xml version="1.0" encoding="UTF-8"?>
<mods xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns="http://www.loc.gov/mods/v3" version="3.1" xsi:schemaLocation="http://www.loc.gov/mods/v3 http://www.loc.gov/standards/mods/v3/mods-3-1.xsd">
  <titleInfo>
    <title>Studies on soils of toshka region</title>
    <subTitle>2- forms of inorganic phosphate in soils of Toshka region</subTitle>
  </titleInfo>
  <titleInfo type="alternative">
    <title>دراسات على أراضى إقليم توشكى</title>
    <subTitle>2-صور الفوسفور المعدنى فى أراضى من منطقة توشكى</subTitle>
  </titleInfo>
  <titleInfo type="uniform">
    <title>Zagazig journal of agricultural research, 2003 v. 30 (5)</title>
  </titleInfo>
  <name type="personal">
    <namePart>Behiry, E. M. K.</namePart>
    <role>
      <roleTerm authority="marcrelator" type="text">creator</roleTerm>
    </role>
  </name>
  <name type="personal">
    <namePart>Hassanein, A. E.</namePart>
  </name>
  <name type="personal">
    <namePart>Khider, M. H.</namePart>
  </name>
  <name type="personal">
    <namePart>Abdel Latif, E. A.</namePart>
  </name>
  <typeOfResource>text</typeOfResource>
  <genre authority="marc">bibliography</genre>
  <originInfo>
    <place>
      <placeTerm type="code" authority="marccountry">ua</placeTerm>
    </place>
    <dateIssued encoding="marc">2003</dateIssued>
    <issuance>continuing</issuance>
  </originInfo>
  <language>
    <languageTerm authority="iso639-2b" type="code">eng</languageTerm>
  </language>
  <language objectPart="summary or subtitle">
    <languageTerm authority="iso639-2b" type="code">ara</languageTerm>
  </language>
  <physicalDescription>
    <form authority="marcform">electronic</form>
    <form authority="gmd">electronic resource</form>
    <form authority="gmd">electronic resource</form>
    <extent>p.1901-1917.</extent>
  </physicalDescription>
  <abstract>Fifteen soil profiles were dug, during the 2001 year, at Toshka region and forty five soil samples were collected from layers 0-30, 30-60, and 60-90 cm. The inorganic P-fractions decreased with soil depth increases down the profile, and varied greatly along with the soil depth. The relative abundance of P-fractions in most soils is in the order: Ca-P&gt; saliod-P  Fe-P &gt; AI-P. The Ca-P was the most dominant fraction in these soil.</abstract>
  <note>Includes references.</note>
  <note>Summary in Arabic.</note>
  <subject>
    <geographicCode authority="marcgac">f-ua</geographicCode>
  </subject>
  <subject authority="lcsh">
    <topic>Soils</topic>
    <topic>Phosphorous content</topic>
    <geographic>Egypt</geographic>
  </subject>
  <subject authority="lcsh">
    <geographic>Tūshkah Sharq (Egypt)</geographic>
  </subject>
  <subject authority="nal">
    <topic>inorganic phosphorus</topic>
  </subject>
  <relatedItem type="host">
    <titleInfo>
      <title>Zagazig Journal of Agricultural Research</title>
    </titleInfo>
    <identifier type="issn">1110-0338</identifier>
    <identifier type="local">u158356</identifier>
    <part>
      <text>2003.v.30(5)</text>
    </part>
  </relatedItem>
  <identifier type="uri">http://nile.enal.sci.eg/EALE/2003/ZJAR/3003/5/1901.pdf</identifier>
  <location>
    <url>http://nile.enal.sci.eg/EALE/2003/ZJAR/3003/5/1901.pdf</url>
  </location>
  <recordInfo>
    <recordContentSource authority="marcorg">EAL</recordContentSource>
    <recordCreationDate encoding="marc">120426</recordCreationDate>
    <recordIdentifier source="SIRSI">u208452</recordIdentifier>
  </recordInfo>
</mods>
