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Fertility Deterioration in a Remediated Petroleum-Contaminated Soil

机译:修复的石油污染土壤中的肥力恶化

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摘要

A soil that had been remediated by soil washing and chemical oxidation was evaluated, comparing it to an uncontaminated control soil ~30 m away. Profile descriptions were made of both soils over a 0–1 m depth, and samples were analyzed from each soil horizon. Samples were also analyzed from surface soil (0–30 cm). The control soil (a Fluvisol), had several unaltered A and C horizons, but the remediated soil presented only two poorly differentiated horizons, without structure and much lower in organic matter (<0.5%). In surface samples (0–30 cm), the bulk density, sand-silt-clay contents, field capacity, organic matter, and porosity were different with respect to the control ( > 0.05), and there was much greater compaction (3.04 vs. 1.10 MPa). However, the hydrocarbon concentration in the remediated soil was low (969.12 mg kg , average), and was not correlated to soil fertility parameters, such as porosity, organic matter, pH, moisture, field capacity or texture (R < 0.69), indicating that the impacts (such as compaction, lower field capacity and moisture content) were not due to residual hydrocarbons. Likewise, acute toxicity (Microtox) was not found, nor water repellency (penetration time < 5 s). It was concluded that the fertility deterioration in this soil was caused principally from the mixture of upper (loam) and lower (silty clay to silty clay loam) horizons during remediation treatment. Another important factor was the reduction in organic material, probably caused by the chemical oxidation treatment.
机译:对经过土壤洗涤和化学氧化修复的土壤进行了评估,并将其与约30 m外的未污染对照土壤进行了比较。对这两种土壤在0–1 m的深度进行了剖面描述,并对每个土壤层进行了样品分析。还从地表土壤(0–30 cm)分析了样品。对照土壤(氟维索尔)的A和C层数未变,但修复后的土壤仅表现出两个差的层位,没有结构且有机质含量低得多(<0.5%)。在表面样品(0–30 cm)中,相对于对照(> 0.05),其堆积密度,沙粉粘土含量,田间持水量,有机质和孔隙率均不同,并且压实度要大得多(3.04 vs. 1.10 MPa)。但是,修复土壤中的碳氢化合物浓度很低(平均969.12 mg kg),并且与土壤肥力参数(例如孔隙度,有机质,pH,水分,田间持水量或质地)无关(R <0.69),表明影响(例如压实,较低的田间持水量和水分含量)不是由于残留的碳氢化合物引起的。同样,也没有发现急性毒性(Microtox),也没有发现疏水性(穿透时间<5 s)。可以得出结论,该土壤的肥力恶化主要是由修复处理期间上层(壤土)和下层(粉质粘土到粉质粘土壤土)的混合引起的。另一个重要因素是有机材料的减少,可能是化学氧化处理引起的。

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