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美国德尔马瓦半岛农业土壤中的磷淋失

Phosphorus leaching from agricultural soils of the delmarva peninsula, USA.

作者信息

Kleinman Peter J A, Church Clinton, Saporito Lou S, McGrath Josh M, Reiter Mark S, Allen Arthur L, Tingle Shawn, Binford Greg D, Han Kun, Joern Brad C

出版信息

J Environ Qual. 2015 Mar;44(2):524-34. doi: 10.2134/jeq2014.07.0301.

DOI:10.2134/jeq2014.07.0301
PMID:26023971
Abstract

Leaching of phosphorus (P) mobilizes edaphic and applied sources of P and is a primary pathway of concern in agricultural soils of the Delmarva Peninsula, which defines the eastern boundary of the eutrophic Chesapeake Bay. We evaluated P leaching before and after poultry litter application from intact soil columns (30 cm diameter × 50 cm depth) obtained from low- and high-P members of four dominant Delmarva Peninsula soils. Surface soil textures ranged from fine sand to silt loam, and Mehlich-3 soil P ranged from 64 to 628 mg kg. Irrigation of soil columns before litter application pointed to surface soil P controls on dissolved P in leachate (with soil P sorption saturation providing a stronger relationship than Mehlich-3 P); however, strong relationships between P in the subsoil (45-50 cm) and leachate P concentrations were also observed ( = 0.61-0.73). After poultry litter application (4.5 Mg ha), leachate P concentrations and loads increased significantly for the finest-textured soils, consistent with observations that well-structured soils have the greatest propensity to transmit applied P. Phosphorus derived from poultry litter appeared to contribute 41 and 76% of total P loss in leachate from the two soils with the finest textures. Results point to soil P, including P sorption saturation, as a sound metric of P loss potential in leachate when manure is not an acute source of P but highlight the need to factor in macropore transport potential to predict leaching losses from applied P sources.

摘要

磷的淋失会使土壤中的磷源和施加的磷源活化,这是德尔马瓦半岛农业土壤中一个主要的关注途径,该半岛界定了富营养化的切萨皮克湾的东部边界。我们从德尔马瓦半岛四种主要土壤的低磷和高磷成员采集的原状土柱(直径30厘米×深度50厘米)中,评估了家禽粪便施用前后的磷淋失情况。表层土壤质地从细砂到粉质壤土不等,Mehlich-3土壤磷含量从64毫克/千克到628毫克/千克不等。在施用粪便之前对土柱进行灌溉表明,表层土壤磷控制着渗滤液中的溶解磷(土壤磷吸附饱和度比Mehlich-3磷提供了更强的相关性);然而,也观察到了亚表层土壤(45 - 50厘米)中的磷与渗滤液磷浓度之间的强相关性(r = 0.61 - 0.73)。在家禽粪便施用(4.5 公吨/公顷)后,质地最细的土壤的渗滤液磷浓度和负荷显著增加,这与结构良好的土壤最容易传输施用的磷的观察结果一致。来自家禽粪便的磷似乎占了两种质地最细的土壤渗滤液中总磷损失的41%和76%。结果表明,当粪便不是磷的急性来源时,土壤磷,包括磷吸附饱和度,是渗滤液中磷损失潜力的一个合理指标,但强调需要考虑大孔隙传输潜力来预测施用磷源的淋失损失。

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