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TDR technique for estimating the intensity of effective non rainfall

100%

Janik G., Skierucha W., Blas M., Sobik M., Albert M., Dubicki M., Zawada A.

International Agrophysics

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2014

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tom 28

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nr 1

The objective of this paper is to present a method for determining diurnal distribution of the intensity of effective non rainfall water flux. It was found that the application of TDR technique for the determination of diurnal dynamics of effective non rainfall water flux requires temperature correction of sensed volumetric moisture contents. Without temperature correction the error of estimated non rainfall water flux can be as much as 26%. In addition, the effect of temperature changes on the soil surface was determined in 0.5, 1, 2, 3, 4, and 5 hours periods. It was found that the intensity of effective non rainfall water flux was determined to the greatest extent by the rate of temperature drop during the period of 3 h preceding the non rainfall water flux determination. The agreement of non rainfall water flux calculated with the method proposed and that obtained by the collector was better for dew than for hoarfrost periods.

2

Concentration of soil CO2 as an indicator of the decalcification rate after liming treatment

100%

Chmiel S., Halas S., Glowacki S., Sposob J., Maciejewska E., Trembaczowski A.

International Agrophysics

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2016

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tom 30

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nr 2

3

Water infiltration into a glacial till soil following subsoiling and secondary tillage

84%

Pikul J. L., Aase J. K.

Bibliotheca Fragmenta Agronomica

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1997

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tom 2B

4

Recent advance in studies on physical properties of red soils in China

84%

Yao X. L.

International Agrophysics

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1993

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tom 07

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nr 1

5

Stability and sorptivity of soil aggregates in grassed and cultivated sloping vineyards

84%

Ferrero A., Lipiec J., Turski M., Nosalewicz A.

Polish Journal of Soil Science

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2007

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tom 40

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nr 1

The physical characteristics of soil aggregates influence soil tilth, surface sealing, water infiltration and root growth. Soil management and compaction significantly affect these characteristics. The aim of this work was to determine the effects of tractor traffic across the slope on bulk density, water stability, tensile strength and sorptivity of aggregates from grass covered and cultivated sloping (18%) vineyard soils. The grass covered (G) treatment included periodical mowing and cutting back of herbage and cultivation (C) treatment consisting of autumn ploughing (18 cm) and spring and summer rotary hoeing in the vineyard inter-row zones (2.7 m). A crawler tractor (2.82 Mg) was used in the inter-row zones, moving across the slope for all tillage and chemical operations. Soil aggregates were taken from the inter-rut and the upper and lower rut areas (0-10 and 20-30 cm) in the inter-row zones and then air-dried. Bulk density and tensile strength were lowest in the inter-rut areas and highest in the lower crawler rut. Aggregate water stability was greater under the lower rut and sorptivity in the inter-rut area in comparison to the remaining inter-row areas. In comparable inter-row areas, water stability and sorptivity of soil aggregates were greater and lower under G than C, respectively. The differences in bulk density and tensile strength between G and C were not consistent and varied depending on the inter-row zone and depth.

6

Runoff from soils on marls under semi-arid Mediterranean conditions

67%

Blum W. E. H., Gomer D.

International Agrophysics

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1996

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tom 10

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nr 1

7

Response of plantain to mulch on a tropical Ultisol: Part II. Effect of different mulching materials on soil hydrological properties

59%

Opara-Nadi O. A., Salau O. A., Swennen R.

International Agrophysics

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1992

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tom 06

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nr 3-4

Ograniczanie wyników

TDR technique for estimating the intensity of effective non rainfall

Concentration of soil CO2 as an indicator of the decalcification rate after liming treatment

Water infiltration into a glacial till soil following subsoiling and secondary tillage

Recent advance in studies on physical properties of red soils in China

Stability and sorptivity of soil aggregates in grassed and cultivated sloping vineyards

Runoff from soils on marls under semi-arid Mediterranean conditions

Response of plantain to mulch on a tropical Ultisol: Part II. Effect of different mulching materials on soil hydrological properties