Zobrazeno 1 - 7
of 7
pro vyhledávání: '"Barbora Vysloužilová"'
Publikováno v:
Acta Universitatis Carolinae Geographica, Vol 51, Iss 1, Pp 85-95 (2016)
In this paper, we put together the most important facts that lead to the research on chernozem. Thanks to the work of V. V. Dokuchaev (1846–1903), chernozem stands at the forefront of pedology. In 1883, Dokuchaev introduced the first concept of che
Externí odkaz:
https://doaj.org/article/780e5b3a37ae41a482c3e798eea7cdee
Publikováno v:
Acta Universitatis Carolinae Geographica, Vol 51, Iss 1, Pp 85-95 (2016)
In this paper, we put together the most important facts that lead to the research on chernozem. Thanks to the work of V. V. Dokuchaev (1846–1903), chernozem stands at the forefront of pedology. In 1883, Dokuchaev introduced the first concept of che
Autor:
Timothy I. Eglinton, Michael Zech, Verena Lanny, Imke Kathrin Schäfer, Barbora Vysloužilová, Roland Zech, Jörg Franke
Publikováno v:
SOIL, Vol 2, Iss 4, Pp 551-564 (2016)
Schäfer, Imke Kathrin; Lanny, Verena; Franke, Jörg; Eglinton, Timothy I.; Zech, Michael; Vysloužilová, Barbora; Zech, Roland (2016). Leaf waxes in litter and topsoils along a European transect. SOIL, 2(4), pp. 551-564. Copernicus 10.5194/soil-2-551-2016
Schäfer, Imke Kathrin; Lanny, Verena; Franke, Jörg; Eglinton, Timothy I.; Zech, Michael; Vysloužilová, Barbora; Zech, Roland (2016). Leaf waxes in litter and topsoils along a European transect. SOIL, 2(4), pp. 551-564. Copernicus 10.5194/soil-2-551-2016
Lipid biomarkers are increasingly used to reconstruct past environmental and climate conditions. Leaf-wax-derived long-chain n-alkanes and n-alkanoic acids may have great potential for reconstructing past changes in vegetation, but the factors that a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b032c3dd3b28ebc54da30e3717eb6c3a
https://www.soil-journal.net/2/551/2016/
https://www.soil-journal.net/2/551/2016/
Autor:
Dominique Schwartz, Luděk Šefrna, Damien Ertlen, Arnaud Campaner, Barbora Vysloužilová, Dagmar Dreslerová, Klára Virágh, Mathieu Rué, Tibor József Novák
Publikováno v:
Quaternary International
Quaternary International, Elsevier, 2015, 365, pp.203-211. ⟨10.1016/j.quaint.2014.07.035⟩
Quaternary International, Elsevier, 2015, 365, pp.203-211. ⟨10.1016/j.quaint.2014.07.035⟩
International audience; The environmental conditions of the evolution of chernozems in Central Europe have not been satisfactory explained. In this paper, seven buried chernozems were investigated using near-infrared spectroscopy (NIRS) in order to g
Autor:
Barbora Vysloužilová, Zdeněk Kliment
Publikováno v:
Geografie. 117:170-191
Water erosion is considered to be the most important factor behind the degradation of agricultural land. Many methods of measuring soil erosion processes, using mathematical models, have been developed in recent years. The most widespread of these, U
Autor:
Jean-François Berger, Claire Delhon, Dominique Schwartz, Lenka Danková, Barbora Vysloužilová, Luděk Šefrna, Jan Novák, Damien Ertlen
Publikováno v:
Vegetation History and Archaeobotany
Vegetation History and Archaeobotany, Springer Verlag, 2014, 23 (S1), pp.97-108. ⟨10.1007/s00334-014-0441-7⟩
Vegetation History and Archaeobotany, 2014, 23 (1), pp.97-108. ⟨10.1007/s00334-014-0441-7⟩
Vegetation History and Archaeobotany, Springer Verlag, 2014, 23 (1), pp.97-108. ⟨10.1007/s00334-014-0441-7⟩
Vegetation History and Archaeobotany, Springer Verlag, 2014, 23 (S1), pp.97-108. ⟨10.1007/s00334-014-0441-7⟩
Vegetation History and Archaeobotany, 2014, 23 (1), pp.97-108. ⟨10.1007/s00334-014-0441-7⟩
Vegetation History and Archaeobotany, Springer Verlag, 2014, 23 (1), pp.97-108. ⟨10.1007/s00334-014-0441-7⟩
International audience; Chernozem is a soil type which can be characterised by a thick dark surface horizon, which consists of organic matter and tends to change into a carbonate horizon or more often into a loess horizon. Chernozem is defined as a z
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::89b118b04097481ff24f59c20b2b79ae
https://hal.archives-ouvertes.fr/hal-02125287
https://hal.archives-ouvertes.fr/hal-02125287