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首页> 外文期刊>Moscow University Soil Science Bulletin >Physical properties of soddy-podzolic soils in a long-term field experiment
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Physical properties of soddy-podzolic soils in a long-term field experiment

机译:长期田间试验的土壤水滑土的物理性质

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摘要

The main physical properties of soddy-podzolic soils in a long-term field experiment have been studied. It is shown that their changes under the impact of a century-long application of lime, fertilizers, and manure have been relatively small. Reliable differences in the parameters of approximation of the dependence of penetration resistance on the soil water content in the variant with regular application of organic fertilizers have been revealed. This attests to stronger interparticle bonds (within the studied moisture range) in this variant. Interparticle bonds in the control variant and in the variant with lime application tend to increase with a decrease in the soil water content more significantly than those in other experimental variants. This may be due to the coarser texture of the soil in the control variant and to the aggregation of soil particles under the impact of lime in the variant with lime application.
机译:在长期的田间试验中,研究了土壤水滑土的主要物理性质。结果表明,在长达一个世纪的石灰,肥料和肥料应用下,它们的变化相对较小。在常规施用有机肥料的情况下,该变量的渗透阻力对土壤水分的依赖性的近似参数已显示出可靠的差异。这证明了该变体中更强的颗粒间键(在研究的湿度范围内)。与其他试验变体相比,对照变体和施用石灰的变体中的颗粒间键往往随着土壤含水量的减少而增加。这可能是由于对照变体中的土壤质地较粗,并且是由于在施用石灰的变体中,在石灰的影响下土壤颗粒的聚集。

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