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Aspects of pedogenesis on rocks of the central part of the Bohemian Cretaceous Basin

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985831%3A_____%2F19%3A00510709" target="_blank" >RIV/67985831:_____/19:00510709 - isvavai.cz</a>

  • Result on the web

    <a href="https://www.irsm.cas.cz/materialy/acta_content/2019_doi/Zigova_AGG_2019_0031.pdf" target="_blank" >https://www.irsm.cas.cz/materialy/acta_content/2019_doi/Zigova_AGG_2019_0031.pdf</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.13168/AGG.2019.0031" target="_blank" >10.13168/AGG.2019.0031</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Aspects of pedogenesis on rocks of the central part of the Bohemian Cretaceous Basin

  • Original language description

    Pedogenesis was studied on clayey sandstones, calcareous sandstones, sandy marlstones and silty marlstones in the Bohemian Cretaceous Basin. These rocks were evaluated by petrography and X-ray diffractometry. The soils were characterized on the basis of a variety of analyses of organic and anorganic components. Soil formation proceeded predominantly under neutral and basic conditions. Calcaric Leptosols are of smaller thickness and less prominent pedogenesis than Cambic Leptosols. The main pedogenetic process in all soils is humification. A rapid reduction of the amount of organic matter in soil profiles is typical for soils on clayey sandstone and sandy marlstone. The content of organic matter decreases gradually down the soil profiles on calcareous sandstone and silty marlstone. The intensity of modern pedogenesis is higher in Cambic Leptosols developed on calcareous sandstone and silty marlstone compared to Calcaric Leptosols on sandy marlstone and clayey sandstone. This is due to the more balanced quartz/calcite ratio in the parent material (1.06 for calcareous sandstone, 1.51 for silty marlstone). It appears that the most important factor in Leptosol development is the parent material and that the development towards Cambisols can be hardly expected on silicate–carbonate rocks with a high proportion of quartz

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database

  • CEP classification

  • OECD FORD branch

    40104 - Soil science

Result continuities

  • Project

    <a href="/en/project/GA16-15065S" target="_blank" >GA16-15065S: Factors affecting heavy metal accumulation in macrofungi</a><br>

  • Continuities

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Others

  • Publication year

    2019

  • Confidentiality

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Data specific for result type

  • Name of the periodical

    Acta geodynamica et geomaterialia

  • ISSN

    1214-9705

  • e-ISSN

  • Volume of the periodical

    16

  • Issue of the periodical within the volume

    4

  • Country of publishing house

    CZ - CZECH REPUBLIC

  • Number of pages

    13

  • Pages from-to

    365-377

  • UT code for WoS article

    000500942800004

  • EID of the result in the Scopus database

    2-s2.0-85077840936