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
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Czech description
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Classification
Type
J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database
CEP classification
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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
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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