Agyin-Birikorang S, O'Connor G A, Brinton S R
Soil and Water Sci. Dep., Univ. of Florida, 106 Newell Hall, P.O. Box 110510, Gainesville, FL 32611-0510, USA.
J Environ Qual. 2008 May 2;37(3):1180-9. doi: 10.2134/jeq2007.0535. Print 2008 May-Jun.
Incorporating applied phosphorus (P) sources can reduce P runoff losses and is a recommended best management practice. However, in soils with low P retention capacities, leaching can be a major mechanism for off-site P loss, and the P-source application method (surface or incorporation) may not significantly affect the total amount of off-site P loss. We utilized simulated rainfall protocols to investigate effects of P-source characteristics and application methods on the forms and amounts of P losses from six P sources, including five biosolids materials produced and/or marketed in Florida, and one inorganic fertilizer (triple superphosphate). A typical Florida Spodosol (Immokalee fine sand; sandy, siliceous, hyperthermic Arenic Alaquods) was used for the study, to which the P sources were each applied at a rate of 224 kg P ha(-1) (approximately the P rate associated with N-based biosolids applications). The P sources were either surface-applied to the soil or incorporated into the soil to a depth of 5 cm. Amended soils were subjected to three simulated rainfall events, at 1-d intervals. Runoff and leachate were collected after each rainfall event and analyzed for P losses in the form of soluble reactive P (SRP), total dissolved P (TDP), total P (TP), and bioavailable P (BAP) (in runoff only). Cumulative masses (runoff + leachate for the three rainfall events) of P losses from all the P sources were similar, whether the amendments were surface-applied or incorporated into the soil. The solubility of the amendment, rather than application method, largely determines the P loss potential in poorly P-sorbing Florida Spodosols.
添加施用磷源可以减少磷的径流损失,这是一种推荐的最佳管理措施。然而,在磷保留能力较低的土壤中,淋溶可能是磷流失到其他地方的主要机制,并且磷源的施用方法(表面施用或混入土壤)可能不会显著影响磷流失到其他地方的总量。我们利用模拟降雨方案来研究磷源特性和施用方法对六种磷源磷流失的形态和数量的影响,这六种磷源包括在佛罗里达州生产和/或销售的五种生物固体材料,以及一种无机肥料(重过磷酸钙)。本研究使用了一种典型的佛罗里达灰化土(伊莫卡利细砂;砂质、硅质、高热性潮湿淋溶土),每种磷源以224 kg P ha(-1)的施用量施用到该土壤中(大约是与基于氮的生物固体施用相关的磷施用量)。磷源要么表面施用到土壤上,要么混入土壤至5厘米深度。对改良后的土壤每隔1天进行三次模拟降雨事件。每次降雨事件后收集径流和渗滤液,并分析其中以可溶性活性磷(SRP)、总溶解磷(TDP)、总磷(TP)和生物可利用磷(BAP,仅针对径流)形式存在的磷流失情况。无论磷源是表面施用还是混入土壤,所有磷源的磷流失累积质量(三次降雨事件的径流+渗滤液)都是相似的。在磷吸附能力较差的佛罗里达灰化土中,改良剂的溶解性而非施用方法在很大程度上决定了磷的流失潜力。