Preferencje help
Polish version English version Język
Widoczny [Schowaj] Abstrakt
Liczba wyników

Znaleziono wyników: 4

Liczba wyników na stronie
Pierwsza strona wyników Pięć stron wyników wstecz Poprzednia strona wyników Strona / 1 Następna strona wyników Pięć stron wyników wprzód Ostatnia strona wyników

Wyniki wyszukiwania

Wyszukiwano:
w słowach kluczowych:  moorsh soil
help Sortuj według:

help Ogranicz wyniki do:
Pierwsza strona wyników Pięć stron wyników wstecz Poprzednia strona wyników Strona / 1 Następna strona wyników Pięć stron wyników wprzód Ostatnia strona wyników
1
Artykuł dostępny w postaci pełnego tekstu - kliknij by otworzyć plik
Content available

The analysis of some physical properties of drained peat-moorsh soil layers

100%
Oleszczuk R., Truba M.
Annals of Warsaw University of Life Sciences - SGGW. Land Reclamation
|
2013
|
tom 45
|
nr 1
The paper presents the results of measurements of some physical properties for 14 drained fen peat-moorsh layers (degree of decomposition, bulk density, particle density, porosity and saturated moisture content). The soil samples were taken from north- -east, central and east part of Poland. These areas were drained in order to use as a grassland and meadows. The article presents obtained data of selected physical properties from several drained peatlands in Poland and shows the comparison of established results with relevant data published in literature.
2
Artykuł dostępny w postaci pełnego tekstu - kliknij by otworzyć plik
Content available

An analysis of some basic chemical and physical properties of drained fen peat and moorsh soil layers

67%
Truba M., Oleszczuk R.
Annals of Warsaw University of Life Sciences - SGGW. Land Reclamation
|
2014
|
tom 46
|
nr 1
The paper presents the results of measurements of some chemical properties for 14 drained fen peat-moorsh layers taken from north-east, central and east part of Poland. These areas were drained in order to use as a grassland and most of them in former time were under subirrigation systems. The following basic chemical properties were analysed: organic C, total N, C:N ratio, pH and ash content. In the paper also the relationships between some basic chemical and physical properties were analysed (ash content with bulk density, particle density and porosity). Increasing of ash content caused the decreasing of some chemical properties (organic carbon and total nitrogen content) and increasing some physical properties (bulk density and particle density).
3
Artykuł dostępny w postaci pełnego tekstu - kliknij by otworzyć plik
Content available

Influence of the kind of moorsh and the state of its transformation on the germination and growth of Lolium perenne in the pot plant experiment during spring-summer cycle

67%
Gawlik J., Harkot W.
Acta Agrophysica
|
2000
|
tom 26
The influence of the kind of moorsh and the state of its transformation, as expressed in numerical values of the water absorption index W1, on the germination conditions of Lolium perenne seeds and further growth of young plants have been studied. It was found out that the main factor differentiating these conditions was grain structure of the moorsh mass that determined water conductive properties of the studies soils. The highestnumber of germinated seeds (40-85%) and the best plant growth was observed on peaty moorshes (Z1) of fine fibrous character with fresh humus admixture. Considerably worse conditions for darnel germination and growth (25-50% of germinated seeds) were found on proper fine-grained moorsh (Z3). It was confirmed by a relatively low dty mass yield of plants collected on these soils after completion of the experiment. The highest differentiation of seedlings, and at the same time the poorest germination were found on the proper degraded moorsh with crumble-grained structure with poor conductivity, and on peaty fibrous moorsh that formed a macro-porous layer on the soil surface in the conditions of intensive insolation and high air temperatures. This macro-porous layer efficiently limited capillary rise and evaporation. It was observed that the stale of transformation of moorsh formations expressed with numerical values of the W1 index did not exert any visible influence on the conditions of plant vegetation. The above observation proved that the W1 index is only vaguely connected with the soil conductive properties.
4
Artykuł dostępny w postaci pełnego tekstu - kliknij by otworzyć plik
Content available

Influence of differentiated irrigation on changes in the fraction composition of moorshy humus

67%
Wojcieszczuk T.
Acta Agrophysica
|
2000
|
tom 26
In order to determine the direction of moorshy soil organic substance transformation, especially its fraction composition under different humidity conditions laboratory experiments was carried out using a Column Device for investigation the soil with irrigation (PO no. 54427). Soil material was taken from accumulation horizon of mineral-moorshy soil from the 0-10 cm layer, placed in columns and irrigated afler appropriate preparation using following water doses: 0 - without irrigation, I - to fill the capillary water capacity, II-615 ml, III - 1042 ml, IV - 1657 ml. The fractions of humus, reaction, sorption properties and total content of carbon and nitrogen were determined in the soil material with methods commonly used in soil science. The results indicate that along with the increase of water dose increase the amount of eluted total carbon from the soil material. Quantity changes of total carbon are accompanied by qualitative and quantitative changes of particular determined humus.
Pierwsza strona wyników Pięć stron wyników wstecz Poprzednia strona wyników Strona / 1 Następna strona wyników Pięć stron wyników wprzód Ostatnia strona wyników
JavaScript jest wyłączony w Twojej przeglądarce internetowej. Włącz go, a następnie odśwież stronę, aby móc w pełni z niej korzystać.