中央森林草原景观丘陵不同年龄耕地土壤酸碱条件研究

IF 0.2 Q4 AGRICULTURE, MULTIDISCIPLINARY
E. Kovalyova, I. Vagurin, A. Akinchin, O. Kuzmina
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引用次数: 0

摘要

土壤的肥力在很大程度上取决于它们的物理和化学性质。土壤环境的响应是土壤肥力的一个动态指标。几乎所有提供土壤氮、磷和钾制度的土壤过程的方向和强度,以及植物的宏量和微量元素的可用性,都取决于它。本文介绍了2019年别尔哥罗德地区草甸-草原段土壤土壤典型和浸出不同农业利用条件黑土剖面酸碱条件的野外研究结果。研究对象为农业发展年限分别为140年和240年的不同年龄的耕地。与森林草原草甸-草原地带性景观相对应的地表陡度不超过4 ~ 6°。根据野外调查结果,在草地-低草原剖面共研究了32个切口(背景切口6个,开阔切口12个)。每个切口均提供土层形态计量指标的分层值。对于背景草原土壤,与南坡相比,阴坡具有更多的碱性条件。对于140年的耕地,情况正好相反:与不溶性土壤相比,阴坡的介质酸性反应更强;对于240年历史的耕地,不同处理的坡面酸碱条件差异不显著。在耕种的前140年,土壤剖面发生酸化;北坡140年耕地pH值与背景pH值的差异表层达1.6,深层逐渐减小至0.2。进一步耕作导致土壤剖面碱化0.6-0.9 pH单位。研究结果可用于作物产业的农业系统开发。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Study of acid-alkaline conditions of different-age arable soils of landscape catens of Central Forest-Steppe
Fertility of soils is largely determined by their physical and chemical properties. Response of soil environment is a mobile indicator of soil fertility. Direction and intensity of almost all soil processes that provide nitrogen, phosphorus and potassi- um regimes of soils, as well as availability of macro- and microelements for plants, depend on it. The paper presents the result of a field study of acid-alkaline conditions of profiles of black soil of typical and leached different terms of agricultural use of soil cat- ens of the meadow-steppe section of the Belgorod region in 2019. The research object was different-age arable areas with an age of agricultural development of 140 and 240 years, respectively. The steepness of surface in areas corresponding to the meadow-steppe zonal landscape of the forest-steppe did not exceed 4-6 °. As a result of field studies, 32 incisions were studied in the mead- ow-steppe section (6 incisions on background catens and 12 incisions on open catens). Each incision was provided with layered values of morphometric indicators of soil horizons. For background steppe soils, shade slopes are characterized by more alkaline conditions, in comparison with southern slopes. For 140-year-old arable land, the situation is opposite: shadow slopes have a more acidic reaction of the medium, in comparison with insoluble ones; for 240-year-old arable land, alkaline-acid conditions on the slopes of opposite expositions did not differ significantly. In the first 140 years of plowing, acidification of the soil profile occurs; the difference in the pH value between the background and arable land values of 140 years of age on the slope of the northern ex- position reaches 1.6 on the surface, gradually decreasing to 0.2 at depth. Further plowing leads to alkalization of the soil profile by 0.6-0.9 pH units. The research results can be used in development of agricultural systems in crop industries.
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