Humus balance and nutrient regime of irrigated soil under different systems of primary soil tillage and fertilization

M. Maliarchuk, A. Maliarchuk, A. V. Tomnitskiy
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Abstract

The article presents an analysis of the results of experimental research in a stationary field experiment to determine the peculiarities of the formation of humus reserves and the nutrient regime in the arable layer of the dark chestnut soil (Haplic Kastanozem) under the influence of different fertilization and main cultivation systems. The purpose of the research: to establish the patterns of transformation of by-products of agricultural crops of crop rotation into humus and the main elements of mineral nutrition of plants under organic and two organo-mineral fertilization systems against the background of five systems of main cultivation in a 4-field row crop rotation on irrigated lands in the area of operation of the Ingulets irrigation plant systems. The research was conducted in the stationary experiment of the Institute of Irrigated Agriculture of the National Academy of Sciences in the Kherson region of Ukraine during 2016-2020. The following indicators were used to analyze the effectiveness of the combined application of fertilization systems and the main tillage: mass of post-harvest residues for each of the crop rotations; stocks of humus in the arable layer; humus balance; the mass of nitrogen, phosphorus and potassium that reached the soil with plant residues; ecological and economic effect (UAH/ha); energy gain (GJ/ha). As a result of experimental studies, it was found that the formation of humus reserves in the soil depends on the mass of post-harvest residues of crop rotation and the methods and depth of their wrapping. The most favorable conditions for the accumulation of leaf-stem mass of crop rotation crops and the formation of a positive balance of humus with an average annual increase of 2.02 t/ha were provided by the organo-mineral fertilization system using the by-products of crop rotation crops and a dose of mineral fertilizers N120P60 against the background of differentiated main cultivation with one slotting to a depth of 38-40 cm per rotation.
不同土壤初耕与施肥制度下灌溉土壤腐殖质平衡与养分状况
本文对固定大田试验结果进行了分析,以确定不同施肥和主要耕作制度对黑栗子土可耕层腐殖质储量形成和养分状况的影响。研究目的:在英格莱灌溉植物系统作业区,以四田轮作五种主要栽培制度为背景,建立有机肥和两种有机矿肥制度下轮作作物副产物向腐殖质和植物矿质营养主要元素转化的规律。该研究是在2016-2020年期间在乌克兰赫尔松地区的国家科学院灌溉农业研究所的固定实验中进行的。采用以下指标分析施肥系统与主要耕作方式组合施用的有效性:每轮作物的收获后残茬质量;耕地层腐殖质储量;腐殖质平衡;随植物残茬进入土壤的氮、磷、钾的质量;生态和经济效应(UAH/ha);能量增益(GJ/ha)。试验研究发现,土壤中腐殖质储量的形成取决于作物轮作收获后残留物的数量及其包裹的方法和深度。轮作作物副产物有机肥配氮肥N120P60在主作分化、每轮垄深38 ~ 40 cm的条件下,为轮作作物叶茎质量积累和腐殖质正平衡的形成提供了最有利的条件,平均每年增加2.02 t/ha。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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