NOVÉ POZNATKY K PŮDÁM NA ÚZEMÍ NÁRODNÍHO PARKU PODYJÍ SE ZAMĚŘENÍM NA VÝSKYT HUMOLITŮ
Název anglicky
NEW FINDING OF THE SOILS IN THE NATIONAL PARK PODYJÍ FOCUSING ON THE DEPOSIT OF A HUMOLITES THERE (MORAVIA, CZECH REPUBLIC)
Autoři
ŠUŠOLOVÁ, Jana (203 Česká republika, garant), Nela DOLÁKOVÁ (203 Česká republika, domácí), Miroslava GREGEROVÁ (203 Česká republika, domácí), Peter DUNDEK (203 Česká republika) a Roman HADACZ (203 Česká republika)
Vydání
Acta Mus. Moraviae, Sci. geol. 2016, 1211-8796
Další údaje
Jazyk
čeština
Typ výsledku
Článek v odborném periodiku
Obor
40104 Soil science
Stát vydavatele
Česká republika
Utajení
není předmětem státního či obchodního tajemství
Kód RIV
RIV/00216224:14310/16:00093975
Organizační jednotka
Přírodovědecká fakulta
Klíčová slova anglicky
soils; recent; micromorphology; palynology; National park Podyjí; Moravia
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.
Anglicky
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.