Zobrazeno 1 - 5
of 5
pro vyhledávání: '"stopový prvek"'
Autor:
Krátký, Ondřej
Carbonatites are unique and enigmatic magmatic rocks of unclear origin, with very specific mineralogy and geochemical properties. They are predominantly composed of magmatic calcite or other carbonate minerals (Le Bas 1987) and have low content of Si
Externí odkaz:
http://www.nusl.cz/ntk/nusl-356497
Autor:
Krátký, Ondřej
Carbonatites are unique and enigmatic magmatic rocks of unclear origin, with very specific mineralogy and geochemical properties. They are predominantly composed of magmatic calcite or other carbonate minerals (Le Bas 1987) and have low content of Si
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______2186::2ba05f26c834fbfaf605981daa350e60
http://www.nusl.cz/ntk/nusl-356497
http://www.nusl.cz/ntk/nusl-356497
Autor:
ŽIŽKOVÁ, Věra
The thesis focuses on an evaluation of own experience in determining trace elements in hair and on gathering literature data from this area. The thesis concurrently attempts to answer the question of whether the determination of trace elements in hai
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______2186::421f2b298561d7977bcba90cd2c0839e
http://www.nusl.cz/ntk/nusl-153802
http://www.nusl.cz/ntk/nusl-153802
Autor:
Kochergina, Yulia
Distributions of toxic trace elements were studied in soils before and after disturbation of their profiles.Two areas with different vegetation cover were selected: beech (Fagus sylvatica) and spruce (Picea abies) forests at the Načetín site in the
Externí odkaz:
http://www.nusl.cz/ntk/nusl-310809
Autor:
Kochergina, Yulia
Distributions of toxic trace elements were studied in soils before and after disturbation of their profiles.Two areas with different vegetation cover were selected: beech (Fagus sylvatica) and spruce (Picea abies) forests at the Načetín site in the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::1543306f40ba1b4d07991600eaf7f51a
http://www.nusl.cz/ntk/nusl-310809
http://www.nusl.cz/ntk/nusl-310809