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Evaporation from aggregates of a podzolic, a light brown and a chernozem soil

100%

Witkowska-Walczak B.

International Agrophysics

|

1995

|

tom 09

|

nr 1

2

Anthropogenic transformation of soils in the Barycz valley - conclusions for soil classification

86%

Labaz B., Bogacz A., Kabala C.

Soil Science Annual

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2014

|

tom 65

|

nr 3

3

Characterising root density of peach trees in a semi-arid Chernozem to increase plant density

86%

Paltineanu C., Septar L., Gavat C., Chitu E., Oprita A., Moale C., Calciu I., Vizitiu O., Lamureanu G.

International Agrophysics

|

2016

|

tom 30

|

nr 1

4

The impact of soil types on bovine enterovirus migration introduced with slurry

86%

Olszewska H., Paluszak Z., Jarzabek Z., Gut W.

Electronic Journal of Polish Agricultural Universities. Series Agronomy

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1998

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tom 01

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nr 1

The penetration of bovine enterovirus, LCR - 4 strain deep into soil profiles in the field conditions was researched. Three soil types were selected: podzolic soil, black earth and browned black earth. The soils differed considerably in respect to their physical properties and chemical analysis. The best conditions for drainage were observed in podzolic soil, whereas the worst - in browned black earth. Experimental plots were being sprinkled with the 1:1 mixture of bovine enterovirus (at the concen-tration of 1x106.0 TCID50/1 ml) and slurry. The enterovirus researched, in any soil, migrated to the depth of 7.5 to 10 cm. The highest titres were observed in the surface layers of black earth and podzolic soil (0-2.5 cm). They differed from 102.72 - 104.27 TCID50/g of the soil. With depth the titres decreased, with slight fluctuations observed.

5

Soil solution chemistry in the profiles of forest and arable soils developed from loess

86%

Smal H., Misztal M., Bril J.

Polish Journal of Soil Science

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2000

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tom 33

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nr 1

6

Peculiarities of development of field crop root systems under different methods of basic soil tillage

86%

Medvedev V. V., Lyndina T. E.

Bibliotheca Fragmenta Agronomica

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1997

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tom 2B

7

Air-dry and water-stable soil aggregate distribution of Polish chernozems classified in various complexes of agricultural suitability

72%

Paluszek J.

Polish Journal of Environmental Studies

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2014

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tom 23

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nr 3

The objective of this study was quality estimation of air-dry and water-stable soil aggregate distribution in Polish Haplic Chernozems developed from loess. It was found that among the Chernozems classified in the particular complexes of agricultural suitability there were small differences in the content of air-dry aggregates with sizes of 0.25-10 mm. The distribution of air-dry aggregates in horizons Ap, A, and ABw was estimated as good or medium, while that in horizons Bw and Ck as medium or poor. In the Chernozems classified in the very good wheat complex and the good wheat complex the content of water-stable aggregates with sizes of 0.25-10 mm was significantly greater than in soils classified in the deficient wheat complex. The water-stable aggregate distribution in the Ap horizons of soils classified in the very good and good wheat complexes was estimated as good, and in the Ap horizons of soils of the deficient wheat complex as medium. In horizons A the distribution of water stable aggregates was assessed as medium, and in horizons ABw, Bw, and Ck as poor or very poor.

8

Properties of leached forest-meadow chernozem polluted with lead and cadmium

72%

Hrebelna N., Kosynets O., Sokolowska Z., Bowanko G., Warchulska P.

Acta Agrophysica

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2009

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tom 13

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nr 3[168]

9

Clay minerals of some European chernozems

72%

Ciolkosz E. J., Uziak S.

Polish Journal of Soil Science

|

2003

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tom 36

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nr 2

153-162

Five profiles of chernozems from several European countries were examined in the present study. The chernozems developed from various rocks and differed in their morphology and chemical properties. Mineralogical studies were carried out on the fraction <2 ľm by an X-ray method, using a diffractometer with a proportional recorder. It was found that all European chernozems examined in this study had a similar mineral complex of the clay fraction. Its major components were montmorillonite and illite usually forming mixed structures, whereas kaolinite, quartz, vermiculite and chlorite were present in smaller amounts, and feldspars occurred as trace minerals. Basically, differences in the mineral composition of various profiles and various soil horizons lie in different quantitative relations between the minerals listed above.

10

Porosity of leached forest-meadow chernozem polluted with lead and cadmium

72%

Sokolowska Z., Hrebelna N., Hajnos M.

Acta Agrophysica

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2007

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tom 10

|

nr 2[152]

p.455-463,fig.,ref.

11

Water and soil - the bases of our life

72%

Nestroy O.

International Journal of Ecohydrology and Hydrobiology

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2006

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tom 06

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nr 1-4

137-141

12

Impact of short- and long-term agricultural use of chernozem on its quality indicators

72%

Balashov E., Buchkina N., Buchkina N.

International Agrophysics

|

2011

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tom 25

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nr 1

13

Effect of surface conditions of runoff and soil loss for chernozem soil

72%

Rejman J., Helming K., Debicki R.

International Agrophysics

|

2001

|

tom 15

|

nr 1

14

The properties of humus in some profiles of the black earth-gleyic phaeozems - from the Malopolska Upland

72%

Mazurek R., Niemyska-Lukaszuk J.

Acta Agrophysica

|

2001

|

tom 50

The aim of the present research work was to evaluate the influence of lithogenic conditions on the physico-chemical properties, quantity and quality of humus components in the black earths from the Małopolska Upland. Soil samples were collected from 5 soil profiles which represented proper black earth (profiles No. 1-4) and degraded black earth (profile No. 5). All the investigated soils were under sward. The examined black earths were characterised by different physico-chemical properties strongly related to the parent rock type. Their pH level and sorption capability were decreasing with a decrease in the clay content of the soil texture. Humus resources were the lowest in sandy black earths (average 212 t ha-1) and the highest in the black earh derived from clay (454 t ha1). In the humus composition of the examined black earths, humic acids dominated over fulvic acids. In the A horizons, the Ch:Cf ratio was close to 1, and lower in the upper parts of these horizons which is typical of turf soils. Humus horizons in some of the investigated black earths were classified as epipedon anthropoid according to phosphorus content soluble in 1% citric acid (109 P kg-1 soil).

15

The importance of mineralogical and micromorphological investigations for the assessment of soil structure

72%

Rampazzo N., Blum W. E. H., Strauss P., Curlik J., Slowinska-Jurkiewicz A.

International Agrophysics

|

1993

|

tom 07

|

nr 2-3

16

Aeration properties and enzyme activity on the example of Arenic Chernozem [Tisice]

72%

Wlodarczyk T., Glinski J., Stepniewski W., Stepniewska Z., Brzezinska M., Kuraz V.

International Agrophysics

|

2001

|

tom 15

|

nr 2

17

Structure assessment of two agricultural soils of Lower Austria

72%

Rampazzo N., Blum W. E. H., Strauss P., Curlik J.

International Agrophysics

|

1993

|

tom 07

|

nr 1

18

Survival of bovine enterovirus strain LCR-4 in water, slurry, and soil

72%

Olszewska H., Paluszak Z., Jarzabek Z.

Bulletin of the Veterinary Institute in Puławy

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2008

|

tom 52

|

nr 2

The study of the bovine enterovirus survival in water, slurry, and two layers of black soil, was carried out at 4°C and 20°C under laboratory conditions. Samples of soil, water, and slurry were infected with a suspension of the enterovirus. The titre of the virus at 4°C was determined on the day of inoculation (day 0) and on 7, 21, 42, 70, and 135 d after inoculation. At 20°C, the titre was determined at day 0 and after 7, 21, 35, and 49 d. The study showed that bovine enterovirus, present particularly in the samples of water and slurry, retains its ability to cause cytopathic effects. The temperature of 20°C significantly shortened the survival of the virus in water, soil, and slurry. The process of virus inactivation in the soil proceeded faster than in slurry and water, which indicates that viruses in the soil are subjected to the action of different factors.

19

Influence of the microbiological activity on the soil aggregate stability

72%

Rampazzo N., Mentler A., Tscherko D., Pfeffer M., Blum W. E. H.

International Agrophysics

|

1995

|

tom 09

|

nr 2

20

Soil structure as an ecology forming factor

72%

Medvedev V. V.

International Agrophysics

|

1996

|

tom 10

|

nr 2

Ograniczanie wyników

Evaporation from aggregates of a podzolic, a light brown and a chernozem soil

Anthropogenic transformation of soils in the Barycz valley - conclusions for soil classification

Characterising root density of peach trees in a semi-arid Chernozem to increase plant density

The impact of soil types on bovine enterovirus migration introduced with slurry

Soil solution chemistry in the profiles of forest and arable soils developed from loess

Peculiarities of development of field crop root systems under different methods of basic soil tillage

Air-dry and water-stable soil aggregate distribution of Polish chernozems classified in various complexes of agricultural suitability

Properties of leached forest-meadow chernozem polluted with lead and cadmium