H. B. Humeniuk, V. O. Khomenchuk, N. G. Zinkovska, N. Moskalyuk
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摘要

乌克兰的土壤已经得到了很好的研究,但这并没有阻止它们的严重退化过程。约三分之一的耕地被侵蚀,约20%的有机质流失,底土中几乎所有的耕地都被压实,流动磷尤其是钙的养分形态明显减少,钙占据了土壤阳离子交换容量的大部分,起着调节作用。钙是土壤胶体的凝固剂,保护它们不被破坏和移到剖面的下层;促进腐殖质及其稳定化合物的形成和保存;创造适当的物理条件,在结构形成中起关键作用;结合移动形式的铝、铁、锰化合物,对栽培植被产生不利影响。钙也是植物和土壤微生物的直接养分,在土壤中起排他性的动员作用,增加植物可利用的基本养分含量,主要是磷。在这项工作中,我们对捷尔诺波尔地区的科佐娃、Zboriv Shumsk、Pidhaytsi和别列扎尼地区的土壤进行了化学评估。我们还研究了酸度、交换钙含量和决定农业自然资源利用特性的自然因素及其影响。建立了研究值之间的相关关系。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
ПОРІВНЯЛЬНА ХАРАКТЕРИСТИКА ВМІСТУ КАЛЬЦІЮ ТА СТУПЕНЯ КИСЛОТНОСТІ У ҐРУНТАХ ТЕРНОПІЛЬСЬКОЇ ОБЛАСТІ
The soils of Ukraine have been well studied, however this did not prevent them from the intensive degradation processes. About a third of the arable land is eroded, about 20% of organic matter is lost, almost all the arable land in the subsoil is compacted, the nutrient forms of mobile phosphorus and especially calcium are significantly reduced, calcium, occupying the bulk of the cation exchange capacity of the soil, serves as a regulator. Calcium is a coagulator of soil colloids, protects them from destruction and removal to the lower horizons of the profile; promotes the formation and preservation of humus and its stable compounds; creates proper physical conditions, plays a crucial role in structure formation; binds moving forms of compounds of aluminum, iron, manganese, which adversely affect the cultural vegetation. Calcium is also a direct nutrient of plants and soil microorganisms and plays an exclusive mobilizing role in soil, increasing the content of basic nutrients available to plants, primarily phosphorus. In the work we carried out chemical assessment of soils of Kozova, Zboriv Shumsk, Pidhaytsi and Berezhany districts of Ternopil region. We also studied the acidity, content of exchangeable calcium and natural factors that determine the peculiarities of agricultural natural resource use and influence. Correlation relationships between the studied values are established.
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