Temat: agregaty - Katalog OPAC zbiorów

Skocz do pozycji: 1.

Tytuł:: Sily oddzialywan miedzy czastkami gleb przez interfaze wodna
Interaction forces between soil particles across the water interface
Autorzy:: Hajnos, M
Powiązania:: https://bibliotekanauki.pl/articles/1630399.pdf
Data publikacji:: 1999
Wydawca:: Polska Akademia Nauk. Instytut Agrofizyki PAN
Tematy:: gleby
agregaty glebowe
czastki gleby
faza wodna
kat zwilzania
adhezja
sily oddzialywujace
energia powierzchniowa swobodna
rownanie Laplace'a
soil
soil aggregate
soil particle
water-phase
wetting angle
adhesion
interaction force
surface free energy
Laplace's equation
Opis:: Na podstawie równania Laplace'a wyprowadzono zależność między siłą działającą pomiędzy dwoma ziarnami materiału glebowego przez fazę wodną, a składowymi swobodnej energii powierzchniowej. Stwierdzono zależność wartości sił oddziaływań od zawartości Corg w badanych glebach. Dla gleb o zawartości Corg powyżej 40% wartości tych sił są ujemne. Słowa kluczowe: siły adhezji, kąt zwilżania, składowe swobodnej energii powierzchniowej.
On the basic of Laplace equation the dependence of the force interacting between two soil material particles across the water phase and surface free energy components was concluded.The dependence between interaction force values and organic carbon content C org higher then 40% the values of these forces are negative.
Źródło:: Acta Agrophysica; 1999, 22; 53-58
1234-4125
Pojawia się w:: Acta Agrophysica
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 2.

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

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