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Effect of Si-rich substances on phosphorous adsorption by sandy soils

机译:富含Si富含物质对砂土磷吸附的影响

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摘要

The poor adsorption capacity of sandy soils is one of the primary reasons of a high level of phosphorus (P) leaching. Silicon (Si)-rich soil amendments have the potential to improve the low absorption capacity of sandy soils for P. The objective of this study was to evaluate the ability of different Si-rich materials to regulate P adsorption and retention by sandy soils. Amorphous fine silica (FSS), calcium silicate (CaSiO3), chemically pure CaCO3, and two types of Casilicate slags from metal industry (Pro-Sil) and chemical industry (TS) were used in laboratory experiments being conducted with pure quartz sand and cultivated and virgin Entisols and Spodosols collected in the South Florida. The binding energy-related constants were evaluated for soils treated by Si-rich materials and then incubated during 2 months. The following row of tested materials on the increasing level of "affinity parameter" was determined: for virgin Spodosol, Pro-Sil < CaCO3 < FSS< CaSiO3 < TS; for cultivated Spodosol, FSS < Pro-Sil < CaCO3< CaSiO3 < TS; for virgin Entisol, Pro-Sil < CaSiO3 < CaCO3 < FSS < TS; and for cultivated Entisol, FSS < Pro-Sil < CaSiO3< CaCO3 < TS. Chemical, physical, and physical-chemical mechanisms of increasing soil adsorption capacity are hypothesized and discussed to explain the results obtained. The conducted experiments have demonstrated high prospective of Si-rich materials for reduction of P leaching from cultivated sandy soils.
机译:沙质土壤的吸附能力差是浸出高水平的磷(P)的主要原因之一。硅(Si)丰富的土壤改良剂必须提高沙质土壤对P的目标本研究的低吸收能力的潜力是评估不同富硅材料的沙质土壤,调节磷吸附和保留的能力。无定形精细二氧化硅(FSS),硅酸钙(CaSiO3),化学纯碳酸钙,和两种类型的从金属工业(临-SIL)和化学工业(TS)Casilicate炉渣在实验室实验中使用被用纯石英砂进行,并培养和处女新成土和灰土收集在南佛罗里达。结合能相关常数由富硅材料处理的土壤进行评价,然后在2个月孵育。被确定的“亲和力参数”的水平日益提高被测材料的下列行:处女灰土,临-SIL <碳酸钙

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