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Wyszukujesz frazę "forest humus" wg kryterium: Temat


Wyświetlanie 1-3 z 3
Tytuł:
Chemistry of raw humus vs. chemistry of atmospheric precipitation on the example of pine forests of the Pomeranian Lakeland
Autorzy:
Wicik, Bogumił
Mikulska, Małgorzata
Powiązania:
https://bibliotekanauki.pl/articles/2028863.pdf
Data publikacji:
2004-06-01
Wydawca:
Uniwersytet Warszawski. Wydział Geografii i Studiów Regionalnych
Tematy:
forest litter
humus
atmospheric precipitation
Opis:
This research, conducted for the purposes of the protection of the National Park Bory Tucholskie, contains the results of the investigation of the chemical composition of humus (forest litter) and of atmospheric precipitation. The gathered material allowed determining the fate (accumulation or removal) of chemical elements contained in the pine forest humus as well as to compare the abundance of nutrients in humus and in atmospheric precipitation.
Źródło:
Miscellanea Geographica. Regional Studies on Development; 2004, 11; 51-55
0867-6046
2084-6118
Pojawia się w:
Miscellanea Geographica. Regional Studies on Development
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Energia powierzchniowa i wielkosci jej skladowych jako parametry okreslajace zwilzalnosc i stan agregacyjny wybranych mineralow ilastych i gleb
Surface energy and its components as parameters determining wettability and aggregation state of selected clay minerals and soils.
Autorzy:
Hajnos, M
Powiązania:
https://bibliotekanauki.pl/articles/1630383.pdf
Data publikacji:
1999
Wydawca:
Polska Akademia Nauk. Instytut Agrofizyki PAN
Tematy:
agrofizyka
gleby
gleby organiczne
gleby mineralne
mineraly ilaste
prochnica
prochnica lesna
kwasy huminowe
struktura gleb
zwilzalnosc
zwilzalnosc gleb
powierzchnia gleb
agregaty glebowe
energia powierzchniowa
soil
organic soil
mineral soil
clay mineral
humus
forest humus
humic acid
soil structure
wettability
soil wettability
soil surface
soil aggregate
surface free energy
Opis:
In the present work problems related to surface free energy of different agricultural materials such as clay minerals, mineral soils, organic soils and forest litter were considered. Methodical investigations of surface free energy determination as well as fundamental investigations connected with the influence of the surface cations and organic substance on the wettability, free energy and interaction forces between clay minerals and soil particles were undertaken. The interaction forces between clay minerals and soil particles perform a fundamental role in aggregation, flocculation and forming of solids structure. In case of solids the surface free energy can be determined indirectly for example from the measured contact angles or from the adsorption values (by determination of film pressure jt) with appropriate theoretical assumptions. Such methods were applied in this paper to determine surface free energy components for clay minerals and soils. Because of difficulties in contact angle measurements by sessile drop method (especially for organic soils and humus) thin layer wicking or thin column wicking technique were applied. The investigations of penetration rates of water and organic liquids carried out for clay minerals and their mono ionic forms showed the close dependence between the kind of mineral and surface cation. The linear dependence of penetration rates was obtained at the lowest penetration times for bentonite and the highest for kaolin. The kind and properties (e.g. radius of hydrated ions) play in this case an important role. The empiric series of wettability, depending on clay mineral and surface cation were determined experimentally. Similar measurements were performed for clay minerals with increasing additions of humic acid and for different soils. On the basis of the measurements the surface free energy components apolar and polar (electron-acceptor and electron-donor) were calculated and correlated with the kind of clay mineral, surface cation and humic acid content. The investigations for soils show that the penetration times depend on the soil samples. Contact angle values for investigated samples were also calculated. From the water vapour adsorption measurements on the surfaces of modified clay minerals and soils the water film pressure values were calculated for one or three monolayers and compared with the work of adhesion and immersion. For soil materials surface free energy had real influence on structure formation or its changes. The organic matter and surface cations had an important role in creation of soil structure.
Źródło:
Acta Agrophysica; 1999, 17; 1-112
1234-4125
Pojawia się w:
Acta Agrophysica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Właściwości gleby pod okapem czterech gatunków drzew leśnych po 30 latach od ich posadzenia na dwóch różnych siedliskach
Soil properties under the canopy of four forest tree species 30 years after planting on two different forest sites
Autorzy:
Mroziński, P.
Modrzyński, J.
Powiązania:
https://bibliotekanauki.pl/articles/1018330.pdf
Data publikacji:
2006
Wydawca:
Polskie Towarzystwo Leśne
Tematy:
siedliska lesne
Larix decidua
Quercus robur
wlasciwosci fizyczne
daglezja zielona
lesnictwo
Picea abies
dab szypulkowy
bor mieszany swiezy
modrzew europejski
wlasciwosci chemiczne
gleby lesne
Pseudotsuga menziesii
las mieszany swiezy
drzewa lesne
swierk pospolity
forest trees
humus type
soil properties
site fertility
central europe
Opis:
The main objective of this study was to demonstrate a relationship between the direction and effectiveness of impact of particular tree species on soil properties and the initial site fertility. The studies were conducted on two neighbouring experimental plots with different forest site types (fresh mixed coniferous forest – BMśw and fresh mixed deciduous forest – LMśw). The analysed species Norway spruce (Picea abies L. Karst.), European larch (Larix deciduas Mill.), Douglas fir (Pseudotsuga menziesii Franco) and penduculate oak (Quercus robur L.) were planted in three replications on 400 m2 plots. It was stated that: 1) the humification processes ongoing under the canopy of the analysed tree species are, to a large degree, determined by the type of forest site; 2) under the same tree species the content of calcium and nitrogen in the nitrate form was found to by markedly lower in the BMśw forest site; 3) in the BMśw forest site, the pH and electrolytic conductivity of the soil under the majority of the analysed tree species were lower; 4) the degrading impact of coniferous species on soil was noticeably stronger on the poorer BMśw forest site.
Źródło:
Sylwan; 2006, 150, 08; 26-37
0039-7660
Pojawia się w:
Sylwan
Dostawca treści:
Biblioteka Nauki
Artykuł
    Wyświetlanie 1-3 z 3

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