乌克兰草原北部天然森林土壤电物理特性及介电常数

V. Gorban'
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引用次数: 1

摘要

目前在土壤科学中,寻找新的土壤研究方法和技术是相关的,它可以在短时间内以最低的经济成本获得大量的土壤状况信息。测定土壤电物理参数和介电常数的方法符合这些要求。调查结果发现,位于乌克兰草原地带(乌克兰第聂伯罗彼得罗夫斯克地区,Novomoskovsk地区)的Glubokiy峡谷土壤的上层与下层相比,电阻和介电常数值较低。与下部地层相比,上部地层的电导率、矿化度和矿化度均有所增加。在沟谷北部露露区露露地表和塔尔维格区露露地表地表,所有研究参数的值都在积层和积层边界处发生了突然变化。在山沟森林北露的陆域风化层和山沟平坦地区的陆域风化层中,在淋积层和洪积层的边界处,所有研究参数的值都发生了急剧变化。在Luvic phaeozem的淋积层中,与淋积层相邻,观察到介电常数的急剧增加。北沟露钙钙质上部层位电阻、电导率和介电常数均高于南沟露钙钙质上部层位,矿化和矿化度均低于南沟露钙钙质上部层位。与峡谷南部森林区Luvic phaeozem的上层相比,峡谷北部森林区Luvic phaeozem的上层具有更高的电阻和介电常数值。在电导率、矿化度和矿化度方面,Luvic phaeozems实际上没有什么不同。与钙质黑钙矿相比,上层钙钙矿具有电阻和介电常数较低,电导率、矿化度和矿化度较高的特点。结果表明,森林黑钙土的有机质和水溶性化合物含量最高,结构团聚体组成最佳,且结构团聚体组成最佳。这是由于在峡谷的南部暴露处形成的,其特点是介电常数和电阻值最低,电导率、矿化和盐度值最高。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Electrophysical characteristics and dielectric constant of soils of northern natural forests of Ukrainian steppe zone
Currently in soil science the search for new methods and technologies for soil research is relevant, which in a short time allows to receive a large amount of information about its condition with the lowest financial cost. Methods for determining electrophysical parameters and dielectric constant of soils are conforming to these requirements. As a result of the investigations, it was found that the upper horizons of the soils of Glubokiy ravine, located in the Ukrainian steppe zone (Novomoskovsk district, Dnipropetrovsk region, Ukraine), differ to lower values of electrical resistance and dielectric constant compared to the lower horizons. The upper horizons are characterized by increased values of electrical conductivity, mineralization and salinity compared with the lower horizons. Sudden changes in the values of all investigated parameters at the boundary of the eluvial and illuvial horizons were found in Luvic phaeozem of northern exposition of ravine and in Luvic gleyic phaeozem of thalweg. In the Luvic phaeozem of the forest northern exposure of the ravine and in the Luvic gleyic phaeozem of the leveled area of the ravine, sharp changes were found in the values of all the investigated parameters at the boundary of the eluvial and illuvial horizons. In the eluvial horizons of Luvic phaeozem, which bordering on the illuvial horizons, a sharp increase in the dielectric constant is observed. The upper horizons of Calcic chernozem of the northern ravine exposition are characterized by increased values of electrical resistance, electrical conductivity and dielectric constant, as well as lower values of mineralization and salinity compared to the upper horizons of Calcic chernozem of the southern ravine exposition. The upper horizons of the Luvic phaeozem of the forest north exposition of the ravine are characterized by higher values of electrical resistance and dielectric constant compared to the upper horizons of the Luvic phaeozem of the forest south exposition of the ravine. In terms of electrical conductivity, mineralization and salinity, Luvic phaeozems practically don’t differ. The upper horizons of Luvic phaeozems are characterized by lower values of electrical resistance and dielectric constant, as well as higher values of electrical conductivity, mineralization and salinity compared to Calcic chernozems. The results obtained indicate that the highest content of organic matter and water-soluble compounds, as well as the best structurally-aggregate composition, and also the best structural-aggregate composition is characteristic of forest chernozem. This is due to the one that formed on the southern exposition of the ravine and which is characterized by the lowest values of dielectric constant and electrical resistance, as well as the highest values of electrical conductivity, mineralization and salinity.
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