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Solonetzic process in postagrogenic and postameliorative conditions of the Kamennaya Steppe area

机译:Kamennaya草原地区在农耕后和改良后的条件下的整体构造过程

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The physicochemical conditions and morphological features of solonetzic process in soils of chernozemic solonetzic complexes were studied in the area of solonetzic experimental station no. 1 in the Kamennaya Steppe area in 55 years after a single application of ameliorative measures (earthening, gypsuming, and manuring) and cessation of the annual plowing. It was found that the modern soil-forming factors favor the development of soil processes inherent in native chernozems and solonetzes prior to their plowing and amelioration. They cause the restoration of the humus horizon in chernozems and the morphological differentiation of solonetzes after the cessation of plowing. Active postameliorative and postagrogenic restoration of solonetzic features is related to the preservation of the physicochemical conditions (the low concentration of salts and the presence of exchangeable sodium) in the soil profile. The humus horizon of chernozems applied over the surface of solonetzes is characterized by the appearance of solonetzic features under hydromorphic conditions.
机译:在1号松散试验台区研究了黑松质松散配合物在土壤中的松散过程的理化条件和形态特征。在单次应用改善措施(耕作,石膏和施肥)并停止每年耕作后的55年中,在Kamennaya草原地区为1。人们发现,现代的土壤形成因素在耕种和改良之前,有利于天然黑钙土和孤石的固有土壤过程的发展。它们会导致黑麦草腐殖质层的恢复以及犁耕停止后孤石的形态分化。茄子特征的积极的后改良和后农艺恢复与土壤剖面中物理化学条件(盐浓度低和可交换钠的存在)的保存有关。黑钙石的腐殖质层位在孤石表面上的特征是在水溶条件下出现了孤石特征。

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