通过抹灰防止矿化水灌溉土壤的退化过程

D. Onopriienko, T. Makarova, A. Tkachuk, H. Hapich, H. Roubík
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摘要

长期使用低质量和矿化水灌溉乌克兰大草原地区的广大地区造成了与土壤盐碱化有关的退化过程。为了减轻或减轻这些过程,研究人员通过应用磷石膏研究了化学回收的潜力。该研究在乌克兰北部大草原,第聂伯罗彼得罗夫斯克州第聂伯罗地区的Oleksandrivka村附近进行。多年来,进行了实地试验,引进磷石膏作为化学改良剂。试验设计包括磷石膏在一年中不同时期的施用量,分别为1.4、3.0和6.0 t/ha。采用标准化的研究方法进行取样、实验室分析和结果处理。研究发现,研究区耕层含盐量高(0.35 ~ 0.48%),有盐渍化迹象(交换性钠含量3.64%),土壤物理条件不理想。磷石膏的施用导致土壤中硫酸盐阴离子的增加,这在土壤的硫酸盐化学中观察到,而对照区呈现出硫酸钠类型的盐度。在整个研究过程中,水提取物的pH值一直保持在中性。土壤盐渍化程度呈正向变化。具体来说,在灌溉区以3和6吨/公顷的速度施用磷石膏,导致了从中度到轻度盐的盐度水平的变化。研究还证明了磷石膏对钠吸附比的积极影响,特别是在第三年灌溉时施用磷石膏。与对照相比,磷石膏的钠吸附比降低了69%,说明磷石膏在灌溉过程中的改善效果更好。在ⅱ类水质灌溉条件下,春栽磷石膏用量为3 t/ha,秋栽磷石膏用量为6 t/ha。这些施用量有效地降低了土壤盐渍化程度,改善了灌区的生态条件和改良条件
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Prevention of degradation processes of soils irrigated with mineralized water through plastering
The long-term irrigation of extensive areas in the steppe zone of Ukraine using low-quality and mineralized water has caused degradation processes associated with soil salinization. To mitigate or alleviate these processes, researchers investigated the potential of chemical reclamation through the application of phosphogypsum. The study took place in the northern Steppe of Ukraine near the village of Oleksandrivka, Dnipro district, Dnipropetrovsk region. Over many years, field experiments were conducted, introducing phosphogypsum as a chemical meliorant. The experimental design included the application of phosphogypsum at rates of 1.4, 3.0, and 6.0 t/ha during different periods of the year. Standardized research methods were used for sampling, laboratory analysis, and processing of the results. The research identified a high salt content (0.35-0.48%) in the arable soil layer, signs of salinization (exchangeable sodium content of 3.64%), and unsatisfactory physical condition of the soil in the research areas. The application of phosphogypsum led to an increase in sulfate anions, as observed in the soil's sulfate chemistry, while the control areas exhibited a soda-sulfate type of salinity. The pH level of the water extract remained within neutral values throughout the years of the study. Positive changes were observed regarding the degree of soil salinity. Specifically, the application of phosphogypsum at rates of 3 and 6 t/ha in irrigated areas resulted in a change from moderate to slightly saline salinity levels. The research also demonstrated a positive effect on the sodium-adsorption ratio, particularly when phosphogypsum was applied during irrigation in the third year. The sodium-adsorption ratio decreased by 69% compared to the control options, indicating a better ameliorative effect of phosphogypsum during irrigation. Under the conditions of using water of class II quality for irrigation, the optimal application of phosphogypsum was found to be at doses of 3 t/ha for spring cultivation and 6 t/ha for the main cultivation in autumn. These application rates effectively reduced the degree of soil salinity and improved the ecological and meliorational conditions of the irrigated area
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