Interaction Features of Some Acid Ameliorants in the Process of Chemical Reclamation of Sodic Solonetz-Solonchaks

IF 1.9 Q3 SOIL SCIENCE EGYPTIAN JOURNAL OF SOIL SCIENCE Pub Date : 2022-09-01 DOI:10.21608/ejss.2022.150226.1517
S. Sahakyan, T. Yedoyan, A. Eloyan, S.H. Daveyan
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Abstract

T he purpose of the study is to reveal the mechanisms of interaction of some acid ameliorants in the process of chemical reclamation of Sodic Solonetzes-Solonchaks (SSS). The experiments have been carried out within 2018-2020 under laboratory conditions using soil column techniques.13 soil samples have been collected from Ararat valley, Republic of Armenia. These soils have a high alkaline reaction (pH 9.5-10.5), a sodium exchangeable percentage (ESP 44.5-74.0%) and electrical conductivity (EC 12.4-42.2 dS cm-1).It has been shown, that in thecase of iron sulphate application the products of its hydrolysis promote soil dealkalization and improvement of soil physical properties due to creation of iron-clay complexes accumulated in the soil primarily in crystalline form (66-67 %). It has been revealed, that the penetration depth of 1% of sulphuric acid and iron sulphate solutions during the chemical reclamation is 8-12 cm, and the accumulation of gypsum in topsoil (0-12 cm) is observed. Due to thehigher solubility of magnesium sulphate in the process of acidification, soil dealkalization and the increase of filtration rate of soil solutions (10-12 cm day -1 ) are watched. During the soil leaching process, the newly-formed gypsum plays a major role in further dealkalization process of soils and regulation of exchangeable Ca and Mg relation in optimal range. It is shown, that in the process of acidification, the pressure of the formed carbon dioxide gas (CDG) in the soil may reach up to 2.2 atm, in which the solubility of calcium and magnesium carbonate are increased, and the share of CDG in soil dealkalization process is in average 50%. The results obtained allow for the opportunity to recommend improvements of SSS chemical reclamation technology.
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Sodic Solonetz Solonchaks化学回收过程中几种酸性改进剂的相互作用特征
本研究的目的是揭示一些酸性改良剂在Sodic Solonetzes Solonchaks(SSS)化学回收过程中的相互作用机制。实验于2018-2020年在实验室条件下使用土柱技术进行。13从亚美尼亚共和国阿拉拉特山谷采集了土壤样本。这些土壤具有较高的碱性反应(pH 9.5-10.5)、钠交换率(ESP 44.5-74.0%)和电导率(EC 12.4-42.2 dS cm-1),在施用硫酸铁的过程中,其水解产物促进了土壤脱碱和土壤物理性质的改善,因为在土壤中形成了主要以结晶形式积累的铁-粘土复合物(66-67%)。研究表明,在化学回收过程中,1%的硫酸和硫酸铁溶液的渗透深度为8-12cm,并观察到石膏在表层土中的积聚(0-12cm)。由于硫酸镁在酸化过程中具有较高的溶解性,因此观察了土壤脱碱和土壤溶液过滤速率的增加(10-12cm天-1)。在土壤浸出过程中,新形成的石膏在土壤进一步脱碱过程中发挥着重要作用,并在最佳范围内调节了交换性Ca和Mg的关系。结果表明,在酸化过程中,土壤中形成的二氧化碳气体(CDG)的压力可达2.2atm,其中碳酸钙和碳酸镁的溶解度增加,CDG在土壤脱碱过程中的份额平均为50%。所获得的结果为SSS化学回收技术的改进提供了建议。
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