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Soil formation on a calcic chronosequence of Ancient Lake Konya in Central Anatolia, Turkey

Ozaytekin, Hasan Huseyin; Mutlu, Hasan Huseyin; Dedeoglu, Mert

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  <identifier identifierType="URL"></identifier>
      <creatorName>Ozaytekin, Hasan Huseyin</creatorName>
      <givenName>Hasan Huseyin</givenName>
      <affiliation>Selcuk Univ, Fac Agr, Dept Soil Sci, TR-42031 Konya, Turkey</affiliation>
      <creatorName>Mutlu, Hasan Huseyin</creatorName>
      <givenName>Hasan Huseyin</givenName>
      <affiliation>Bet Fa Agr Co, TR-07350 Antalya, Turkey</affiliation>
      <creatorName>Dedeoglu, Mert</creatorName>
      <affiliation>Selcuk Univ, Fac Agr, Dept Soil Sci, TR-42031 Konya, Turkey</affiliation>
    <title>Soil Formation On A Calcic Chronosequence Of Ancient Lake Konya In Central Anatolia, Turkey</title>
    <date dateType="Issued">2012-01-01</date>
  <resourceType resourceTypeGeneral="Text">Journal article</resourceType>
    <alternateIdentifier alternateIdentifierType="url"></alternateIdentifier>
    <relatedIdentifier relatedIdentifierType="DOI" relationType="IsIdenticalTo">10.1016/j.jafrearsci.2012.09.002</relatedIdentifier>
    <rights rightsURI="">Creative Commons Attribution</rights>
    <rights rightsURI="info:eu-repo/semantics/openAccess">Open Access</rights>
    <description descriptionType="Abstract">With the passage of time, different soils show a wide range of variation in their formation. The passage of time in soil formation affects both soil features and the rates of weathering. The aim of this research is to study and compare the pedogenic evolution of soils developed on the terraces of Ancient Lake Konya using weathering indices such as Chemical Index of Alteration (CIA), Chemical Index of Weathering (CIW), and Eu and Ce anomalies. The study will also take into account other features, such as the physical and chemical properties, the analytical characteristics and how soil formation is determined according to the passage of time. For this purpose, four representative profiles were dug at different levels. After the macro-morphological identifications were completed in all the profiles, the samples were then collected from the horizons and were analysed for their physical, chemical, mineralogical and geochemical properties.</description>
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