2018
DOI: 10.31545/aagr/100456
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Effect of long-term use of apple orchard on selected chemical properties of soils developed from silts

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(6 citation statements)
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“…soil texture-particle size distributions (PSD)-with Casagrande method modified by Prószy ński [53], -particle density (PD)-with the pycnometric method [54] (Mg × m −3 ), -bulk density (BD)-with the gravimetric method, from the ratio of the mass of soil dried at 105 • C to the initial soil volume of 100 cm 3 [55] (Mg × m −3 ), -total porosity (TP) was calculated from the results of particle density (PD) and bulk density (BD), TP = 1 − BD/PD [56] (m 3 × m −3 ), -air capacity at the potential of −15.5 kPa (FAC) was derived from the results of total porosity (TP) and field water capacity (FC) (−15.5 kPa), FAC = TP−FC [56] (m 3 × m −3 ), -air permeability at the potential of −15.5 kPa (FAP) was measured using an apparatus for the measurement of permeability of molding sand, LPiR-2e [7][8][9]. The measurements were conducted at vertical (upward) airflow through the soil sample.…”
Section: Analysesmentioning
confidence: 99%
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“…soil texture-particle size distributions (PSD)-with Casagrande method modified by Prószy ński [53], -particle density (PD)-with the pycnometric method [54] (Mg × m −3 ), -bulk density (BD)-with the gravimetric method, from the ratio of the mass of soil dried at 105 • C to the initial soil volume of 100 cm 3 [55] (Mg × m −3 ), -total porosity (TP) was calculated from the results of particle density (PD) and bulk density (BD), TP = 1 − BD/PD [56] (m 3 × m −3 ), -air capacity at the potential of −15.5 kPa (FAC) was derived from the results of total porosity (TP) and field water capacity (FC) (−15.5 kPa), FAC = TP−FC [56] (m 3 × m −3 ), -air permeability at the potential of −15.5 kPa (FAP) was measured using an apparatus for the measurement of permeability of molding sand, LPiR-2e [7][8][9]. The measurements were conducted at vertical (upward) airflow through the soil sample.…”
Section: Analysesmentioning
confidence: 99%
“…Such changes can only marginally affect, e.g., soil compaction or/and air-water properties. The authors of some papers [5,7,8] have stressed that high rates of different soil-applied materials, both mineral and organic ones, result in a significant change in particle size distribution. The soil texture is then restructured towards the one that is determined by the type of the material applied to the soil [15,24,42].…”
Section: Soil Texture (Psd) and Density (Pd And Bd)mentioning
confidence: 99%
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