Distinct phosphorus release from fresh and legacy biosolids-amended sandy soils

IF 3.6 4区 农林科学 Q1 AGRICULTURE, MULTIDISCIPLINARY
Yang Lin, Isabella D. Brush, JoAnn B. Donald, Me'Keila A. Lightfoot, Todd Z. Osborne, Rex Ellis, Andy Canion
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引用次数: 0

Abstract

Biosolids are commonly used as soil amendments; however, repeated application of biosolids results in phosphorus (P) accumulation, elevating environmental risks by increasing P loss through runoff and leaching. Predicting soil P loss after ceasing biosolids application remains challenging. In a laboratory experiment, 80 leaching events were applied to sandy soils with biosolids application histories from active use to 15 years post-application. Soils with recent applications showed an early peak in P release that later stabilized, while those with legacy applications exhibited lower but more consistent P release. These results suggest that fresh biosolids contained a highly mobile P fraction that depletes over time, leaving behind more fixed P that may persist for decades. These P release trajectories could be reasonably modeled by two-pool exponential decay models. Overall, these findings highlight the importance of biosolids aging in regulating P dynamics and identify the hot moments in P loss in biosolids-impacted systems.

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不同的磷释放从新鲜和遗留的生物固体修正沙质土壤
生物固体通常用作土壤改良剂;然而,反复施用生物固体会导致磷(P)积累,通过径流和淋滤增加P的损失,从而增加环境风险。停止施用生物固体后预测土壤磷流失仍然具有挑战性。在一项实验室实验中,80个浸出事件应用于沙质土壤,这些土壤具有生物固体应用历史,从积极使用到应用后15年。最近施用的土壤磷素释放在早期达到峰值,随后趋于稳定,而遗留施用的土壤磷素释放较低但较为稳定。这些结果表明,新鲜的生物固体含有高度流动的磷组分,随着时间的推移会耗尽,留下更多的固定磷,可能会持续数十年。这些P释放轨迹可以用双池指数衰减模型合理地模拟。总的来说,这些发现强调了生物固体老化在调节磷动力学中的重要性,并确定了生物固体影响系统中磷损失的热点时刻。
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来源期刊
CiteScore
3.70
自引率
3.80%
发文量
28
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