DEPENDENCE OF PHOSPHATE CONTENT IN WATER ON MOBILE AND TOTAL FORMS OF PHOSPHORUS IN SOIL IN AGRICULTURAL TERRITORY OF TERNOPIL REGION (UKRAINE)

O. Skyba, L. Fedonyuk, O. Yarema, K. Lesnyak-Mochuk
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Abstract

The indicators of phosphates in water, the content of mobile and total forms of phosphorus in bottom sediments and soils in the hydroecosystem of the agrarian territory, which is characterized by active agriculture and animal husbandry, have been determined and analyzed. It was found that the presence of the total form of phosphorus in soil, water and bottom sediments differs significantly in different months, and the mobile form, on the contrary, is the same. It indicates a significant mobility of mobile forms of phosphorus in the “soil-water-bottom” sediments system. It was found that in spring most of the total phosphorus is in the soil, and in summer and until the beginning of autumn, its share in bottom sediments increases. It was revealed that the content of phosphates in the studied hydroecosystem is determined by their migration in the “soil-water-bottom” sediments system and has a seasonal character.
捷尔诺波尔农业区土壤中磷的流动形态和全形态对水中磷含量的依赖性(乌克兰)
测定并分析了以农牧业为主的农区水生态系统中水中磷、底泥和土壤中磷的流动形态和总形态的含量。结果发现,不同月份土壤、水体和底泥中磷的总形态存在显著差异,而流动形态存在相同。这表明在“土壤-水-底”沉积物系统中,磷的流动形式具有显著的流动性。结果表明,春季全磷主要集中在土壤中,夏季至秋初,全磷在底泥中所占比例增加。结果表明,所研究的水文生态系统中磷酸盐的含量是由其在“土壤-水-底”沉积物系统中的迁移决定的,具有季节性特征。
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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