Informacja

Drogi użytkowniku, aplikacja do prawidłowego działania wymaga obsługi JavaScript. Proszę włącz obsługę JavaScript w Twojej przeglądarce.

Wyszukujesz frazę "Oswit, J" wg kryterium: Wszystkie pola


Wyświetlanie 1-2 z 2
Tytuł:
Potrzeby i mozliwosci ochrony doliny sandrowej uzytkowanej rolniczo na przykladzie Doliny Omulwi
Autorzy:
Oswit, J
Dembek, W
Powiązania:
https://bibliotekanauki.pl/articles/804240.pdf
Data publikacji:
1997
Wydawca:
Szkoła Główna Gospodarstwa Wiejskiego w Warszawie. Wydawnictwo Szkoły Głównej Gospodarstwa Wiejskiego w Warszawie
Tematy:
gleby
ochrona krajobrazu
warunki glebowe
ochrona przyrody
zbiorowiska roslinne
stratygrafia
sandr kurpiowski
geomorfologia
walory krajobrazowe
fitosocjologia
strefowosc ekologiczna
walory przyrodnicze
dolina Omulwi
Opis:
Among reclaimed valleys and canalised rivers of the Kurpiowski Sandr, the valley of Omulwia river is distinguished by relatively unchanged landscape and natural, strongly meandering river-bed of 15-20 m width. Its run is accompanied by zone of branched, picturesque, partly filled-with-water old-river beds. On the grounds of identification of the existing soils, plant communities and peat beds in the lines of 8 levelled transverse valley sections (fig. 2), the appearance of distinct, transverse ecological zonality related to the existing hydrological conditions, has been found. The distinguished zones differ in character of soils and vegetation as well as in the intensity of flood and ground feeding. In the area, directly adjacent to the river, being intensively flooded, the dominating type of habitat is silt-covered ground, generating alluvial heavy and medium, usually medium-deep (50-100 cm) formations. They occupy about 1/2 of valleys width. The zone of specific mads is situated at the nearest distance from the river. On both sides of this zone, the parallel bands of mineral-muck mads were found, being identified on the grounds of the presence of silt-originated moorsh in the upper layer up to 30 cm. In the marginal, usually higher situated parts of the valley, there are peatlands, supplied with ground water; they create a separate ecological zone, running like a band alongside both edges of the valley and fill the pockets, eroded in its mineral substratum, with peats. Shallow beds form alder and osier peats. In deeper cuttings of mineral substratum, there are beds of more complex structure with the share of sedge and rush peats and, in deeper initial levels, also of mossy peats. Between the zones of alluvial soils and the zone of peat soils, a zone of mineral-moorsh soils, built by peat-originated moorsh, has been additionally found. In alluvial zones, characterized by a rich microrelief, the communities of Magnocaricion, usually sedge (Caricetum gracilis) and reed canary grass and sedge-reed canary grass (Phalaridetum arundinaceae) are mainly found. They create a mosaic with the communities of Molinietalia order (Alopecuretum pratensis Valeriano-Filipenduletum), appearing on flat elevations. In peat zones, we find mainly communities of sedge (Ranunculo-Caricetum fuscae) and reed grass (Calamagrostietum neglectae), belonging to Caricion fuscae (nigrae). The areas of certain reclaimed and managed peatlands are overgrown with communities of cultivated meadows. Nature values of the valley were assessed, classifying it into 3 parts and identifying 4 most valuable fragments for closer protection (fig. 5). Zone of the river and near-river old beds, which is most valuable part of the valley from ecological viewpoint and is strongly differentiated from a viewpoint of hipsome- try, the habitat and phytosociology, should be a place of extensive economy; its protection should be a leading motive in case of planning any economic investments. On the other hand, intensive meadow management should be focused on the edge parts of the valley, especially in marginal, east zone of the valley on the areas of higher elevated peat soils, being drained by a large ditch, running parallelly to the valley edges.
Źródło:
Zeszyty Problemowe Postępów Nauk Rolniczych; 1997, 435; 127-153
0084-5477
Pojawia się w:
Zeszyty Problemowe Postępów Nauk Rolniczych
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Walory przyrodnicze przeobrazonego eksploatacja Torfowiska Wysokiego Karaska
Autorzy:
Dembek, W
Oswit, J
Rycharski, M
Powiązania:
https://bibliotekanauki.pl/articles/805942.pdf
Data publikacji:
1997
Wydawca:
Szkoła Główna Gospodarstwa Wiejskiego w Warszawie. Wydawnictwo Szkoły Głównej Gospodarstwa Wiejskiego w Warszawie
Tematy:
eksploatacja
zbiorowiska roslinne
Torfowisko Karaska
sklad gatunkowy
warunki wodne
torfowiska wysokie
sandr kurpiowski
waloryzacja przyrodnicza
torf
zmiany antropogeniczne
walory przyrodnicze
Opis:
Paper presents the results of the 1992 studies of Karaska Bog, one of the largest continental raised bogs in Poland. The object of research was to determine the impact of four decades of peat extraction on natural environment of the bog, to identify in particular: - impact of extraction on various elements of the bog ecosystem, - potential of extensive raised bog subjected to industrial-scale exploitation to preserve its nature values, - natural regeneration capacity of the peatbog. Investigation results helped to establish the origin and evolution of the peatbog as well as its interrelations with the surrounding area. The following four stages of development were distinguished: I - silting up of the water reservoir by lake sediment. II - final colonization of the lake by sedge-moss and raised bog-sedge communities responsible for accumulation of fen and transitional peat. III - accretion of highly decomposed raised bog Eriophorum-Sphagnum peat generated by oligotrophic peat-forming communities associated with water regime based on precipitation. IV - development of raised bog Sphagnum communities accompanied by accumulation of poorly decomposed raised bog tussock peat. Condition of vegetation and soils in Karaska Bog was found to be as follows: - condition of vegetation: - areas with natural or near-natural vegetation - jointly 55 %, - visibly dehydrated areas featuring secondary plant cover - 28 %, - heavily dehydrated areas destroyed by exploitation largely devoid of vegetation - 17 % total bog area - soils: - peat-swamp soils - 39 %, - peat-moorsh - 50 %, - post-extraction sites -11%. It was concluded that extensive raised bogs are relatively invulnerable to diverse impact of peat extraction. They retain much of their nature value and demonstrate high capacity for self-regeneration. As such they should be seen as sites not wholly lost to the natural environment. Consequently, it is advisable for each site of this type to assess its eligibility for nature-reserve type of protection.
Źródło:
Zeszyty Problemowe Postępów Nauk Rolniczych; 1997, 435; 99-125
0084-5477
Pojawia się w:
Zeszyty Problemowe Postępów Nauk Rolniczych
Dostawca treści:
Biblioteka Nauki
Artykuł
    Wyświetlanie 1-2 z 2

    Ta witryna wykorzystuje pliki cookies do przechowywania informacji na Twoim komputerze. Pliki cookies stosujemy w celu świadczenia usług na najwyższym poziomie, w tym w sposób dostosowany do indywidualnych potrzeb. Korzystanie z witryny bez zmiany ustawień dotyczących cookies oznacza, że będą one zamieszczane w Twoim komputerze. W każdym momencie możesz dokonać zmiany ustawień dotyczących cookies