不同树龄和施肥量的家禽粪便改良土壤中磷的分布:农艺学和环境视角

Debolina Chakraborty, Rishi Prasad, Hanxiao Feng, Dexter B. Watts, H. Allen Torbert
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引用次数: 0

摘要

家禽粪便(PL)可作为磷肥的可行替代品。然而,目前还缺乏有关磷(P)在无机磷(Pi)和有机磷(Po)形态中的分布及其在使用不同龄期(基于垃圾清理频率)和施用量的家禽粪便改良土壤中的转化的信息。本研究旨在确定聚乳酸龄期和施用率对土壤中磷的形态及其生物利用率的影响。使用 6 个月、18 个月和 30 个月的垃圾对土壤进行 5 毫克/公顷和 10 毫克/公顷 PL 的改良,并培养 6 个月。按照 Hedley 方案进行土壤钾分馏。使用 Mehlich 3(M3)萃取法测定了土壤钾的可用性和土壤钾的储存能力(SPSC)。结果表明,在 150 天的培养过程中,土壤中的钾从易变形式转化为稳定形式。粪肥龄对土壤中 P 形态的分布没有明显影响。然而,在第 0 天,施用 10 Mg ha-1 PL 的处理中,高活性钾(HRPi)的形式较高,表明存在钾流失的风险,这些处理的 SPSC 也显示为负值。在第 0 天,M3-P 与 HRPi 呈正相关。然而,从第 30 天到第 150 天,M3-P 与 HRPi 和中度活性 Pi(MRPi)形式都有很强的相关性,表明中度活性 Pi 对土壤钾的可用性有贡献。HRPi 与 SPSC 之间的负相关关系进一步证实,第 0 天的高 HRPi 可能是一个环境问题。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Distribution of phosphorus forms in soil amended with poultry litter of different ages and application rates: Agronomic and environmental perspectives

Distribution of phosphorus forms in soil amended with poultry litter of different ages and application rates: Agronomic and environmental perspectives

Poultry litter (PL) can be used as a viable alternative to phosphate fertilizers. However, there is a lack of information about phosphorus (P) distribution in inorganic (Pi) and organic (Po) forms and its transformation in soils amended with PL of varying age (based on litter clean-out frequency) and application rate. This study aimed to determine the effect of PL age and application rate on soil P forms and their bioavailability. Soils were amended with 5 and 10 Mg ha−1 PL using 6-, 18-, and 30-month-old litter and incubated for 6 months. Soil P fractionation was performed following the Hedley protocol. Soil P availability and soil P storage capacity (SPSC) were determined using Mehlich 3 (M3) extraction. Results indicated that P transformation from labile to stable P forms occurred over 150-day incubation. Litter age had no significant effect on the distribution of soil P forms. However, the highly reactive Pi (HRPi) form was higher for treatments with 10 Mg ha−1 PL on Day 0, indicating a risk for P loss, which was also revealed by negative SPSC for those treatments. At Day 0, M3-P was positively correlated to HRPi. However, from Day 30 to 150, M3-P was strongly correlated to both HRPi and moderately reactive Pi (MRPi) forms, indicating MRPi contribution to soil P availability. The negative relationship between HRPi and SPSC further confirms that high HRPi on Day 0 may be an environmental concern.

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