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首页> 外文期刊>Polish Journal of Natural Sciences >The effect of sulfate and elemental sulfur application on modification of concentrations of manganese and lead in soil.
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The effect of sulfate and elemental sulfur application on modification of concentrations of manganese and lead in soil.

机译:施用硫酸盐和元素硫对土壤中锰和铅浓度变化的影响。

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Soil acidification due to sulfur fertilization can produce an indirect result such as increased solubility and mobility of heavy metals in soil, thus affecting availability to plants of these elements derived from both natural and man-made resources. The purpose of this paper has been to explore the effect of incremental doses of sulfate and elemental sulfur on changes in the natural content of easily soluble forms of manganese and lead in two soil horizons: 0-40 and 40-80 cm. A three-year field experiment was set up on brown, acid soil with the texture of heavy loamy sand. Soil for chemical analyses was sampled in spring and autumn. Soluble forms were extracted from soil with 1 mol HC1 dm-3 solution and their concentrations were determined with the atomic absorption spectrophometric method. Throughout the whole experiment, the dose of 40 kg ha-1 S-SO2-4 induced higher concentrations of manganese in soil in the 0-40 cm layer compared to the other fertilization treatments. During the three years of the field trials, the application of sulfate sulfur and elemental sulfur to soil tended to cause a small increase in the soil content of lead soluble in 1 mol HCl dm-1 in the 0-40 cm soil depth compared to the soil before the experiment. The concentrations of manganese and lead in soil in the 40-80 cm layer did not depend much on the form and dose of sulfur introduced to soil.
机译:硫磺施肥引起的土壤酸化可产生间接结果,例如增加重金属在土壤中的溶解度和迁移率,从而影响这些天然和人工来源的元素对植物的利用率。本文的目的是探究增加剂量的硫酸盐和元素硫对两种土壤层(0-40和40-80 cm)中易溶形式的锰和铅的自然含量变化的影响。在带有重质壤土沙质的棕色酸性土壤上进行了为期三年的田间试验。在春季和秋季对用于化学分析的土壤进行了采样。用1 mol HCl dm -3 溶液从土壤中提取可溶形式,并采用原子吸收光谱法测定其浓度。在整个实验中,剂量为40 kg ha -1 S-SO 2- 4 的剂量在0诱导土壤中的锰含量更高。与其他施肥处理相比,厚度为-40厘米。在三年的田间试验中,向土壤中施用硫酸盐硫和元素硫往往会导致0-mol浓度为1 mol HCl dm -1 的可溶性铅的土壤含量小幅增加。与实验前的土壤相比,土壤深度为40厘米。 40-80厘米厚的土壤层中锰和铅的浓度与引入土壤的硫的形式和剂量关系不大。

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