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Phosphorus Fractionation in Biosolids-Amended Soils: Relationship to Soluble and Desorbable Phosphorus

机译:生物固体改良土壤中的磷分级分离:与可溶性和可解吸磷的关系

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Phosphorus has been identified as a major factor involved in decreasing water quality through its role in eutrophication, and there is now a focus on controlling nonpoint agricultural P sources. This work was conducted to identify how biosolids applications under current regulations have affected the forms and release potential of P in agricultural soils. We collected samples from eight farms with a history of biosolids amendments, selecting fields that had setback areas (where biosolids applications were not permitted) to allow comparison of amended and unamended soils. We analyzed these soils for P fractions (soluble P, Al-P, Fe-P, reductant soluble P, and Ca-P; their sum equals total P), sequentially desorbable P (Fe-strip), oxalate P, Al and Fe, Mehlich-1 P, and the degree of P saturation. Our results show that following a N-based biosolids nutrient management plan can significantly increase total P (from 403 to 738 mg kg-1) and initially desorbable P (from 32 to 61 mg kg-1). The main soil components associated with P retention (Alox and Feox) also tended to be increased by biosolids amendment and this may help mitigate P release. Biosolids amendment significantly increased Fe-P (from 137 to 311 mg kg-1), probably due to Fe added to biosolids during production, and there was also a strong trend for higher Al-P where biosolids had been applied. Desorbable P was initially greatest from biosolids sites, but with increasing extractions, the release converged towards that from the setback areas. Mehlich-1 P and Pox were good predictors of desorbable P release, as measured by one and five sequential extractions with Fe-strips. Desorbable P, by both one and five Fe-strip extractions, was more closely correlated with Al-P than Fe-P, especially in setback areas, indicating that Al-P is probably the most important source of desorbable P independent of biosolids amendment. This work indicates the importance of considering P availability at agricultural biosolids application sites and of maintaining setback areas near water bodies, where no biosolids may be applied, to reduce the risk of P losses.
机译:磷通过其在富营养化中的作用而被认为是导致 降低水质的主要因素, 现已成为控制非点源农业 的重点。 P源。开展这项工作的目的是确定当前法规下的生物固体 应用如何影响农业土壤中磷的形态和释放潜力。我们从八个具有生物固体修订历史的农场中收集了 样本, 选择了具有退缩区域(不允许使用生物固体应用程序 的区域)以允许修改过的土壤和未修改过的 土壤的比较。我们依次分析了这些土壤中的P组分(可溶性P,Al-P, Fe-P,还原剂可溶性P和Ca-P;它们的总和等于total P)。可解吸的P(铁带),草酸盐P,Al和 Fe,Mehlich-1 P和P的饱和度。我们的结果 表明,基于N的生物固体养分管理计划 可以显着增加总磷(从403到738 mg kg - 1 )和最初可解吸的P(32至61 mg kg -1 )。与固氮相关的 主要土壤成分(Al ox 和Fe ox 也倾向于被生物固体增加修订和this 可能有助于减轻P的释放。生物固形物修正物显着 使Fe-P增加(从137到311 mg kg -1 ),这可能是由于在生产过程中向生物固形物中添加了Fe 和对于使用了生物固体的更高的Al-P,也有很强的 趋势。可释放的 P最初在生物固体位点最大,但是随着 提取物的增加,释放趋向于挫折 区域。 Mehlich-1 P和P ox 是可解吸的 P释放的良好预测物,通过一次和五次连续的Fe-strip提取 进行测量。一到五次Fe-strip 提取物的可解吸P与Al-P的关系比Fe-P 更紧密,特别是在退缩地区,这表明Al-P可能是 与生物固体 修正无关的最重要的可解吸P来源。这项工作表明,必须考虑在农业生物固体施用场所使用 P的可用性,以及 维持水体附近受挫区域的可能性,在该区域不得使用生物固体 ,以减少P丢失的风险。

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