ON THE COMPARATIVE ANALYSIS OF THE COMPOSITION OF LYSIMETRIC WATER UNDER CONDITIONS OF DIFFERENT SOIL TREATMENT AND UNDER PHYTOCENOSES

L. G. BOGATYREV, V. A. KUZNETSOV, A. I. BENEDIKTOVA, M. M. KARPUKHIN, V. M. TELESNINA, S. A. BORISOVA, M. S. KADULIN, G. R. GLAZMAN, Z. S. EZHELEV, N. A. SHNYREV, S. A. BIBULATOV, V. V. DEMIN
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Abstract

A comparative analysis of the composition of lysimetric waters for 2021–2022 was carried out. for two groups of stationary soil lysimeters in the city. The first group of lysimeters is formed by the system: fallow — grass phytocenosis — overgrown fallow — spruce forest — mixed and broadleaved plantation, developing on the same type of mantle loam. The second group of lysimeters represents soils with different types of tillage: conventional plowing, extradeep planting according to Bushinsky, plowing according to Mosolov, deep plowing according to Kachinsky.For both groups, the same type of migration of components is shown, in which the most migrating elements are carbon, mono- and divalent cations, and chloride ion, with minimal migration of iron, manganese, and aluminum.In the group of lysimeters under various types of vegetation, as the tree canopy develops and, accordingly, the intensity of the biological cycle increases in migrating waters, the concentration of such important biophilic elements as magnesium, calcium, potassium, and carbon increases significantly, and among anions, chloride and sulfate ions. This determines, within the framework of the cluster analysis, two different subgroups in terms of the composition of natural waters: the first one is formed by the fallow-grass phytocenosis — overgrown fallow system, and the second one combines tree plantations.In the group of lysimeters with different tillage, a cluster characterizes the composition of water in lysimeters with reclamation plowing according to Mosolov and deep plowing according to Kachinsky. At the same time, individual aggregates form lysimeters with conventional plowing and ultradeep planting according to Bushinsky. This is explained by the fact that in this group of lysimeters, the initially created soil profile design is transformed, which is characterized by the placement of eluvial and illuvial soil horizons in various combinations and at different depths depending on the type of plowing.
不同土壤处理条件下和植物控制下溶沉水组成的比较分析
对2021-2022年溶沉水体组成进行了对比分析。用于两组固定式城市土壤溶渗仪。在同一类型的地幔壤土上发育的休耕-草植林-杂草丛生的休耕-云杉林-混交林阔叶林系统形成了第一类溶渗器。第二组溶渗仪代表不同耕作方式的土壤:常规耕作,Bushinsky认为的超深种植,Mosolov认为的耕,Kachinsky认为的深耕。对于这两组,显示了相同类型的组分迁移,其中迁移最多的元素是碳、一价和二价阳离子以及氯离子,迁移最少的是铁、锰和铝。在不同类型植被下的溶水器群中,随着树冠的发育,迁移水体中生物循环强度随之增加,镁、钙、钾、碳等重要亲生物元素的浓度显著增加,阴离子、氯离子、硫酸盐离子之间的浓度也显著增加。在聚类分析的框架内,这就确定了天然水域组成的两个不同的亚群:第一个是由杂草丛生的休耕系统形成的,第二个是由树木人工林组成的。在采用不同耕作方式的溶渗仪组中,根据Mosolov的复垦耕作和Kachinsky的深耕耕作,有一个集群描述了溶渗仪中水的组成。与此同时,根据Bushinsky的说法,通过传统的耕作和超深种植,单个聚集体形成溶渗仪。这可以通过以下事实来解释:在这组溶土仪中,最初创建的土壤剖面设计被改变了,其特点是根据耕作类型,以各种组合和不同深度放置淋积土和淤泥土层。
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