Detailed Information on Publication Record
2016
NOVÉ POZNATKY K PŮDÁM NA ÚZEMÍ NÁRODNÍHO PARKU PODYJÍ SE ZAMĚŘENÍM NA VÝSKYT HUMOLITŮ
ŠUŠOLOVÁ, Jana, Nela DOLÁKOVÁ, Miroslava GREGEROVÁ, Peter DUNDEK, Roman HADACZ et. al.Basic information
Original name
NOVÉ POZNATKY K PŮDÁM NA ÚZEMÍ NÁRODNÍHO PARKU PODYJÍ SE ZAMĚŘENÍM NA VÝSKYT HUMOLITŮ
Name (in English)
NEW FINDING OF THE SOILS IN THE NATIONAL PARK PODYJÍ FOCUSING ON THE DEPOSIT OF A HUMOLITES THERE (MORAVIA, CZECH REPUBLIC)
Authors
ŠUŠOLOVÁ, Jana (203 Czech Republic, guarantor), Nela DOLÁKOVÁ (203 Czech Republic, belonging to the institution), Miroslava GREGEROVÁ (203 Czech Republic, belonging to the institution), Peter DUNDEK (203 Czech Republic) and Roman HADACZ (203 Czech Republic)
Edition
Acta Mus. Moraviae, Sci. geol. 2016, 1211-8796
Other information
Language
Czech
Type of outcome
Článek v odborném periodiku
Field of Study
40104 Soil science
Country of publisher
Czech Republic
Confidentiality degree
není předmětem státního či obchodního tajemství
RIV identification code
RIV/00216224:14310/16:00093975
Organization unit
Faculty of Science
Keywords in English
soils; recent; micromorphology; palynology; National park Podyjí; Moravia
Změněno: 24/3/2017 10:01, doc. RNDr. Nela Doláková, CSc.
V originále
Between 2014–2015 soil researches in the National Park Podyjí were performed. The primary interest in the researches was to verify the deposit of humolites (peat, fen) in the National Park Podyjí and to get detailed knowledges about the development of the soil and the landscape in the Holocene. The Holocene past time was researched on the site at Jejkala, where we found the Gleysols stagnic. The second site was not far from the Ice caves, where the Fluvisols gleyic was found out. Both the soil types are fallen into the Holocene whose climatic fluctuations are reflected partially. All of the soil profiles were recorded the warmer climatic phase of the Holocene according to the palynology.
In English
Between 2014–2015 soil researches in the National Park Podyjí were performed. The primary interest in the researches was to verify the deposit of humolites (peat, fen) in the National Park Podyjí and to get detailed knowledges about the development of the soil and the landscape in the Holocene. The Holocene past time was researched on the site at Jejkala, where we found the Gleysols stagnic. The second site was not far from the Ice caves, where the Fluvisols gleyic was found out. Both the soil types are fallen into the Holocene whose climatic fluctuations are reflected partially. All of the soil profiles were recorded the warmer climatic phase of the Holocene according to the palynology.