
<ns0:uwmetadata xmlns:ns0="http://phaidra.univie.ac.at/XML/metadata/V1.0" xmlns:ns1="http://phaidra.univie.ac.at/XML/metadata/lom/V1.0" xmlns:ns10="http://phaidra.univie.ac.at/XML/metadata/provenience/V1.0" xmlns:ns11="http://phaidra.univie.ac.at/XML/metadata/provenience/V1.0/entity" xmlns:ns12="http://phaidra.univie.ac.at/XML/metadata/digitalbook/V1.0" xmlns:ns13="http://phaidra.univie.ac.at/XML/metadata/etheses/V1.0" xmlns:ns2="http://phaidra.univie.ac.at/XML/metadata/extended/V1.0" xmlns:ns3="http://phaidra.univie.ac.at/XML/metadata/lom/V1.0/entity" xmlns:ns4="http://phaidra.univie.ac.at/XML/metadata/lom/V1.0/requirement" xmlns:ns5="http://phaidra.univie.ac.at/XML/metadata/lom/V1.0/educational" xmlns:ns6="http://phaidra.univie.ac.at/XML/metadata/lom/V1.0/annotation" xmlns:ns7="http://phaidra.univie.ac.at/XML/metadata/lom/V1.0/classification" xmlns:ns8="http://phaidra.univie.ac.at/XML/metadata/lom/V1.0/organization" xmlns:ns9="http://phaidra.univie.ac.at/XML/metadata/histkult/V1.0">
  <ns1:general>
    <ns1:identifier>o:7114</ns1:identifier>
    <ns1:title language="sr">HIDROLOŠKE KARAKTERISTIKE SERPENTINITSKIH ZEMLJIŠTA I NJIHOVA ERODIBILNOST</ns1:title>
    <ns1:title language="en">HYDROLOGICAL CHARACTERISTICS OF SERPENTINITE SOILS AND THEIR ERODIBILITY</ns1:title>
    <ns1:language>sr</ns1:language>
    <ns1:description language="sr">Ispitivana su hidrološka svojstva zemljišta i vodni bilans po modelu
Tornthweite-a na šest lokaliteta na serpentinitima. Za dve hidrološke godine od
kojih je jedna znatno suvlja, a druga znatno vlažnija od prosečne. Za iste lokalitete
ustanovljen je faktor erodibilnosti zemljišta po metodu R. Lala. Izvršeno je
poređenje različitih evoluciono genetskih stadijuma zemljišta na serpentinitima u
količini otekle vode i njihovoj erodiblinosti.</ns1:description>
    <ns1:description language="en">Hydrological characteristics of the soil and water balance were researched
after Tornthweite&apos;s model at six localities on serpentinites in two
hydrological years of which one was considerably drier, and the other was considerably
moister than the average. Factor of soil erodibility was determined for
the same localities using R. Lat&apos;s method. Different evolution-genetic stages of
the soil on serpentinites were compared regarding the quantity of runoff water and erodibility.</ns1:description>
    <ns1:keyword language="en">serpentinites, soil type-, water infiltration and retention, runoff, erosion</ns1:keyword>
    <ns1:keyword language="sr">serpentiniti, tip zemljista, primanje i zadrzavanje vode, oticanje, erozija</ns1:keyword>
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    <ns1:contribute seq="0">
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        <ns3:firstname>Zoran</ns3:firstname>
        <ns3:lastname>Miletić</ns3:lastname>
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        <ns3:firstname>Milun</ns3:firstname>
        <ns3:lastname>Topalović</ns3:lastname>
      </ns1:entity>
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    <ns1:contribute seq="2">
      <ns1:role>46</ns1:role>
      <ns1:entity seq="0">
        <ns3:firstname>Čedomir</ns3:firstname>
        <ns3:lastname>Burlica</ns3:lastname>
      </ns1:entity>
    </ns1:contribute>
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  <ns1:technical>
    <ns1:format>application/pdf</ns1:format>
    <ns1:size>4460895</ns1:size>
    <ns1:location>https://unilib.phaidrabg.rs/o:7114</ns1:location>
  </ns1:technical>
  <ns1:rights>
    <ns1:cost>no</ns1:cost>
    <ns1:copyright>yes</ns1:copyright>
    <ns1:license>1</ns1:license>
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    <ns1:purpose>70</ns1:purpose>
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  <ns1:organization>
    <ns8:hoschtyp>92000001</ns8:hoschtyp>
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      <ns8:faculty>71A07</ns8:faculty>
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  <ns12:digitalbook>
    <ns12:name_magazine language="sr">Zbornik radova Instituta za šumarstvo</ns12:name_magazine>
    <ns12:booklet>44-45</ns12:booklet>
    <ns12:from_page>21</ns12:from_page>
    <ns12:to_page>36</ns12:to_page>
    <ns12:publisher>Institut za šumarstvo</ns12:publisher>
    <ns12:releaseyear>2001</ns12:releaseyear>
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