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Wyszukujesz frazę "meadow plant" wg kryterium: Temat


Wyświetlanie 1-4 z 4
Tytuł:
The content of selenium in some species of meadow plants
Zawartość selenu w niektórych gatunkach roślin łąkowych
Autorzy:
Patorczyk-Pytlik, B.
Powiązania:
https://bibliotekanauki.pl/articles/14397.pdf
Data publikacji:
2009
Wydawca:
Uniwersytet Warmińsko-Mazurski w Olsztynie / Polskie Towarzystwo Magnezologiczne im. Prof. Juliana Aleksandrowicza
Tematy:
meadow plant
plant species
grass
selenium content
herb
selenium accumulation
soil
Opis:
The aim of the investigation carried out in 2006-2007 was to assess differences between 5 grass species and 5 species of plants belonging to meadow herbs in their ability to accumulate selenium. According to the results, among the grass species, the samples of Arrhenatherum elatuis L. had the highest average Se content (46 μg Se⋅kg-1 d.m.), and the lowest average Se amount was found in Holcus lanatus L. (24 μg Se⋅kg-1 d.m.). The content of Se in meadow weeds (70 μg Se⋅kg-1 d.m.) was approximately twice as high as in grasses (32 μg Se⋅kg-1 dm.). Among this group of plants, the highest Se accumulation occurred in Equisetum arvense L. (103 μg Se⋅kg-1 dm.) and the lowest – in Taraxacum officinale (59 μg Se⋅kg-1 dm.). Both in grasses and in meadow weeds, the Se content significantly depended on the amount of this element in soils. In the following species: Dactylis glomerata L., Arrhenatherum elatius L., Poa pratensis L. and Taraxacum officinale, the amount of accumulated Se was also conditioned by the soil’s abundance in organic and total C.
Celem badań prowadzonych w latach 2006-2007 było określenie zróżnicowania w zdolności nagromadzania selenu przez 5 gatunków traw oraz 5 gatunków roślin zaliczanych do ziół łąkowych. Wykazano, że wśród analizowanych gatunków traw najwięcej selenu zawierały próby Arrhenatherum elatuis L. (46 μg Se⋅kg-1 sm.), a najmniej Holcus lanatus L. (24 μg Se⋅kg-1 sm.), średnio dla badanych gatunków roślin. Zawartość Se w chwastach łąkowych (70 μg Se⋅kg-1 sm.) była ok. 2-krotnie większa niż określona dla traw (32 μg Se⋅kg-1 sm.). W tej grupie roślin największą kumulację Se wykazywał Equisetum arvense L. (103 μg Se⋅kg-1 sm.), najmniejszą Taraxacum officinale (59 μg Se⋅kg-1 sm.). Zarówno w trawach, jak i chwastach zawartość selenu była istotnie zależna od ilości tego pierwiastka w glebach. Dla gatunków: Dactylis glomerata L., Arrhenatherum elatius L., Poa pratensis L. oraz Taraxacum officinale o ilości nagromadzonego Se decydowała również zasobność gleb w C-org. i S-og.
Źródło:
Journal of Elementology; 2009, 14, 4
1644-2296
Pojawia się w:
Journal of Elementology
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Mutual relations between soil cover and plants in mountainous humid climatic conditions
Autorzy:
Wozniak, L
Powiązania:
https://bibliotekanauki.pl/articles/1450543.pdf
Data publikacji:
2001
Wydawca:
Polska Akademia Nauk. Instytut Agrofizyki PAN
Tematy:
mountain area
meadow
vegetation
ecosystem
chemical composition
soil cover
soil-plant relation
Bieszczady Mountains
mountain meadow
soil
climate condition
terrestrial ecosystem
plant
Opis:
Specific, humid climate of mountain areas has a great influence on the properties of soils and vegetation, as well as on the mutual relations between these inseparable elements of ecosystems. Research on the interdependence between soils and natural vegetation was carried out on ' the mountain meadows of the Bieszczady National Park. In conditions of the cooler and more humid mountain climate the peculiar character of the soils lies in the presence of organic surface horizon of properties varying considerably from the properties of deeper mineral horizons. This horizon is of great importance in the protection of scarce elements. It prevents pollutants from reaching the ecosystem. It influences the soil water economy. It prevents erosion. This buffer element of the mountain soils requires special protection - in the Bieszczady Mountains the erosion of the mountain meadow soils is only noticeable where the covering vegetation and the organic surface soil horizon were destroyed, e.g. on tourist tracks. The plants of the Bieszczady mountain meadows, together with their direct product - the organic surface soil horizon, prevents the chemical erosion of the mountain meadows, reducing the leaching of many biogenous elements, e.g. calcium.
Źródło:
Acta Agrophysica; 2001, 50; 253-261
1234-4125
Pojawia się w:
Acta Agrophysica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Statistical assessment of certain properties of soil under permanent grasslands
Autorzy:
Wylupek, T.
Gawryluk, A.
Powiązania:
https://bibliotekanauki.pl/articles/961385.pdf
Data publikacji:
2016
Wydawca:
Uniwersytet Warmińsko-Mazurski w Olsztynie / Polskie Towarzystwo Magnezologiczne im. Prof. Juliana Aleksandrowicza
Tematy:
statistical assessment
certain property
soil
permanent grassland
grassland
meadow soil
plant community
organic matter
pH
macroelement
Opis:
Geobotanical studies comprised soil and permanent grasslands in the valley of the Por River. The paper describes an assessment of the content of organic matter, reaction (pH) and availability of P, K and Mg in meadow soils overgrown with plant communities classified within the following syntaxonomic units: associations Phragmition and Magnocaricion, orders Molinietalia and Arrhenatheretalia, classes Scheuchzerio-Caricetea nigrae and the order Trifolio fragiferae-Agrostietalia stoloniferae. The results of chemical analyses were confronted with the limit ordinals after IUNG in Puławy (1990) and submitted to statistical analysis using the system of SAS 9.2 from Enterprise Guide 4.2. The analyzed habitats of permanent grasslands had neutral reaction and were dominated by organic soils. Mineral soils occurred in a small area. Generally, a very high or high availability of assimilable P, a low or very low availability of K and a differentiated content of Mg were found in organic soils. In mineral soils, on the other hand, a very high content of P and Mg and a very low content of K were observed. Comparative analyses of selected properties of the habitats showed very significant diversity. Variability coefficients were generally characterized by high values, which points to considerable differentiation of the analyzed properties of the soils within the distinguished syntaxonomic units. Based on our analysis of the Pearson’s correlation coefficients, a number of relations, both positive and negative ones, can be noticed between the properties studied.
Źródło:
Journal of Elementology; 2016, 21, 2
1644-2296
Pojawia się w:
Journal of Elementology
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Characteristics of the meadow hydrogenic soils in Przedmoscie against the background of forming plant communities
Autorzy:
Bogacz, A
Grosdzinska, D.
Chachula, K.
Kasowska, D.
Powiązania:
https://bibliotekanauki.pl/articles/1450407.pdf
Data publikacji:
2001
Wydawca:
Polska Akademia Nauk. Instytut Agrofizyki PAN
Tematy:
organic matter
physicochemical property
physical property
hydrogenic soil
chemical property
plant community
soil
meadow soil
soil property
melioration
terrestrial ecosystem
Opis:
The aim of this work was to compile characteristics of some selected physical, physico-chemical and chemical properties of the reclaimed hydrogenic soils in the meadow part of the Przedmoście bog in the context of new forming plant communities. Melioration work conducted in this area before the Second World War ended peat accumulation processes. Consequently, drying peat began to disintegrate and mineralise. Analyses of floral lists proved that the existing vegetation replaced the original bog plant communities, which flourished in this area in the past. Descriptions of profiles point to the existence of mixed formations (gyttja, peat) often containing high quantities of CaCO3. Peat formations present in the profiles are usually at the advanced degree of decomposition (H>7) and contain substantial quantities of ash. This high degree of ash content and bulk density results in strong compaction and muddy soil horizons. A low coefficient of C/N showed intense mineralization of organic matter in the upper soil horizons.
Źródło:
Acta Agrophysica; 2001, 50; 17-28
1234-4125
Pojawia się w:
Acta Agrophysica
Dostawca treści:
Biblioteka Nauki
Artykuł
    Wyświetlanie 1-4 z 4

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