Development of soils on paragneiss and granite in the southeastern part of Bohemia

Title:

Development of soils on paragneiss and granite in the southeastern part of Bohemia

Creator:

Žigová, Anna, Šťastný, Martin, and Radka Kodešová

Identifier:

https://cdk.lib.cas.cz/client/handle/uuid:5dc398bf-ea6e-4c1e-b847-95dd32b49812
uuid:5dc398bf-ea6e-4c1e-b847-95dd32b49812
doi:10.13168/AGG.2013.0008
issn:1214-9705

Subject:

Geologie. Meteorologie. Klimatologie, mineralogie, mineralogy, soil formation, reserves of soil organic matter, parent material, cambic horizon, micromorphology, 7, and 551

Type:

article, články, model:article, and TEXT

Format:

print, bez média, and svazek

Description:

This study presents data about the effect of parent material on the intensity of processes that lead to the formation of a cambic subsurface horizon. The study was performed in the Voděradské bučiny National Nature Reserve with granite bedrock and in Humpolec with paragneiss bedrock. Representative soil profiles in the southeastern part of Bohemia were characterised on a macroscale level based on macromorphological description, particle size distribution, chemical, physical and soil organic matter properties. On the basis of the values of organic carbon and bulk density, the stock of soil organic matter was calculated in the upper 25 cm of soils. A more detailed characteristic of soil cover employed micromorphological and X-ray diffraction analyses. The results revealed differences in the formation of the cambic horizon on different types of parent material. The main soil forming process responsible for the cambic horizon is more intensive at localities with paragneiss bedrock., Anna Žigová, Martin Šťastný and Radka Kodešová., and Obsahuje bibliografii

Language:

English

Rights:

http://creativecommons.org/licenses/by-nc-sa/4.0/
policy:public

Source:

Acta geodynamica et geomaterialia : | 2013 Volume:10 | Number:1 (169)

Harvested from:

CDK

Metadata only:

false