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Wyszukujesz frazę "macroporosity" wg kryterium: Temat


Wyświetlanie 1-6 z 6
Tytuł:
Application of image analysis for soil macropore characterization according to pore diameter
Autorzy:
Glab, T.
Powiązania:
https://bibliotekanauki.pl/articles/26286.pdf
Data publikacji:
2007
Wydawca:
Polska Akademia Nauk. Instytut Agrofizyki PAN
Tematy:
soil macropore
soil structure
soil macroporosity
application
pore diameter
image analysis
macroporosity
Źródło:
International Agrophysics; 2007, 21, 1
0236-8722
Pojawia się w:
International Agrophysics
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Evaluation of soil physical quality in dominant series of calcareous soils in south-west of Iran
Autorzy:
Meskini-Vishkaee, Fatemeh
Jafarnejadi, Ali Reza
Mousavi-Fazl, Mohammad Hadi
Powiązania:
https://bibliotekanauki.pl/articles/2088190.pdf
Data publikacji:
2020
Wydawca:
Uniwersytet Marii Curie-Skłodowskiej. Wydawnictwo Uniwersytetu Marii Curie-Skłodowskiej
Tematy:
aeration
macroporosity
soil available water
S index
Opis:
Calcareous soils are widely spread in arid and semiarid regions. Carbonates can affect soil quality by influencing soil pH, structure and soil available water. There are lots of calcareous soils in Iran and especially Khuzestan province, so, providing sustainable agriculture evaluating the soil quality is essential. This study was done to evaluate the soil physical quality in dominant calcareous soil series in Khuzestan province, Iran. Soil physical quality indicators, including Dexter's S index, air capacity, soil available water capacity, relative water capacity and macroporosity were calculated. The results showed that, based on Dexter's S index, only one calcareous soil series had a poor physical quality (S < 0.035). However, the simultaneous evaluation of different soil quality indicators showed that 56 % and 22 % of studied calcareous soil series had limited aeration and soil available water, respectively. While the weakest soil physical quality was related to the southeastern soil of Ahvaz, with both aeration and soil available water limitations. The results showed that the proper assessment of soil physical quality in calcareous soils requires considering more physical indicators than just Dexter's S index related to soil aeration condition including air capacity and macroporosity.
Źródło:
Polish Journal of Soil Science; 2020, 53, 2; 225-243
0079-2985
Pojawia się w:
Polish Journal of Soil Science
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Effects of two tillage techniques on soil macroporosity in sub-humid environment
Autorzy:
Josa, R.
Ginovart, M.
Sole, A.
Powiązania:
https://bibliotekanauki.pl/articles/26619.pdf
Data publikacji:
2010
Wydawca:
Polska Akademia Nauk. Instytut Agrofizyki PAN
Tematy:
tillage system
soil macroporosity
leguminous-cereal rotation
macroporosity
macropore area
bulk density
Spain
conventional tillage
direct drilling
soil surface
water balance
micromorphology
ploughed horizon
Źródło:
International Agrophysics; 2010, 24, 2; 139-147
0236-8722
Pojawia się w:
International Agrophysics
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
An attempt to characterise soil macroporosity on the basis of structure standards
Autorzy:
Bryk, M
Domzal, H.
Pranagal, J.
Slowinska-Jurkiewicz, A.
Powiązania:
https://bibliotekanauki.pl/articles/1401857.pdf
Data publikacji:
2000
Wydawca:
Polska Akademia Nauk. Instytut Agrofizyki PAN
Tematy:
soil macroporosity
rendzina soil
computer image analysis
structure standard
loess
soil porosity
water property
porosity
macroporosity
morphometric analysis
air property
soil preparation
black earth
Opis:
The aim of this work was to characterise macro porosity of soil preparations by means of image analysis. Preparations were made from the samples taken from 0-20 cm layer of four types of soil: typical soil lessive developed from loess, proper rendzina developed Irom cretaceous marl, chernozemic rendzina developed from chalk and mud-gley soil developed from clayey silt. The values of porosity by image analysis, Pk, (pores of the diameter greater than 200 (µm) were compared with the values of field air capacity, (Ppp, pores greater than 20 µm) and total porosity, determined by classical methods used in soil science. For most of the samples porosity obtained by computer image analysis, Pk, was lower than the values of field air capacity, Ppp„ as expected. For the rest of standards, the values obtained morphometrically, Pk, were higher than Ppp. It probably- resulted fram unequal pore sizes in the dried and moistened soil material and innate altributes of the method of soil water desorption. Statistical analyses revealed strong, statistically valid dependencies, with high values of the correlation coefficients (0.883 - 0.951) between porosity, Pk, total porosity, Po, and field air capacity, Ppp. Moreover, correlation indices calculated for Po and Ppp confirmed the already known relation.
Źródło:
Acta Agrophysica; 2000, 35; 23-30
1234-4125
Pojawia się w:
Acta Agrophysica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Czy anizotropia elektryczna może być wywołana zmianami nasycenia wodą i gazem w mikro- i makroporach skał miocenu?
Can electric anisotropy be caused by variations of water and gas saturation in micro- and macropores of Miocene rocks?
Autorzy:
Bała, M.
Powiązania:
https://bibliotekanauki.pl/articles/2075089.pdf
Data publikacji:
2013
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
electrical anisotropy
horizontal resistivity
vertical resistivity
water saturation
hydrocarbon saturation
microporosity
macroporosity
Miocene
anizotropia elektryczna
oporność wzdłużna
oporność poprzeczna
nasycenie wodą
nasycenia węglowodorów
mikroporowatość
makroporowatość
miocen
Opis:
The paper presents the problem of evaluation of variation in the electrical anisotropy coefficient for sandstone-shaly Miocene deposits depending on water and gas saturation of the pore space. A rock model built of alternating layers with varying micro- and macroporosity is discussed. This may correspond to a rock formation composed ofparallel thin layers of sandstones or mudstones and claystones, which are dominated by macro- and micropores, and are characterized by different grain size or grain sorting. The anisotropy coefficient is then affected by changes in electrical resistivity in individual layers that are a result of changes in saturation.
Źródło:
Przegląd Geologiczny; 2013, 61, 9; 523--531
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
    Wyświetlanie 1-6 z 6

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