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Soil development on Proterozoic and Paleozoic rocks of central Bohemia

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985831%3A_____%2F21%3A00546552" target="_blank" >RIV/67985831:_____/21:00546552 - isvavai.cz</a>

  • Result on the web

    <a href="https://www.irsm.cas.cz/materialy/acta_content/2021_doi/Zigova_AGG_2021_0031.pdf" target="_blank" >https://www.irsm.cas.cz/materialy/acta_content/2021_doi/Zigova_AGG_2021_0031.pdf</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.13168/AGG.2021.0031" target="_blank" >10.13168/AGG.2021.0031</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Soil development on Proterozoic and Paleozoic rocks of central Bohemia

  • Original language description

    The character of modern pedogenesis in the territory of the Brdská and Křivoklátská vrchovina Highlands was studied on silicate rocks such as Paleozoic granite and Proterozoic mudstone and greywacke. The parent materials were evaluated on the basis of petrography, X-ray diffractometry of powder samples of rock forming and heavy minerals. The soils were described as for their macromorphological characterics and the results of a variety of analyses of organic and anorganic components. Pedogenesis proceeded in acid conditions. The values of base saturation are mostly below 50 % for the Ah horizons. The intensity of soil development on individual parent material decreases in the order: mudstone (Ah-AhBw-Bw-C)>granite (Oi-Oe-Oa-Ah-Bw-C)>greywacke 1 (Oi-Oe-Oa-Ah-AhC-C)>greywacke 2 (Oi-Oe-Oa-Ah-C). The process of humification was documented at all study sites. Evidence of pedogenetic alteration is present in soils developed on granite and mudstone. High amounts of chlorite and elevated contents of illite are characteristic for Cambic Leptosols (Dystric, Skeletic) on mudstone. Weddellite and whewellite were found in relatively large amounts in O horizons of soils except for the Červený kríž site. The predominant from of calcium oxalate minerals at these sites is whewellite. Weddellite occurs in small amount, which is probably due to its lower stability.

  • 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

  • Continuities

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Others

  • Publication year

    2021

  • 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

    2336-4351

  • Volume of the periodical

    18

  • Issue of the periodical within the volume

    4

  • Country of publishing house

    CZ - CZECH REPUBLIC

  • Number of pages

    14

  • Pages from-to

    437-450

  • UT code for WoS article

    000755156300003

  • EID of the result in the Scopus database

    2-s2.0-85125483521