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Phosphorus in runoff from two highly weathered soils of the tropics

机译:热带两种风化土壤中径流中的磷

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Ramirez-Avila, J. R., Sotomayor-Ramirez, D., Martinez-Rodriguez, G. A. and Perez-Alegria, L. R. 2011. Phosphorus in runoff from two highly weathered soils of the tropics. Can. J. Soil Sci. 91: 267-277. Agricultural fields with high soil phosphorus (P) content are important contributors to surface water degradation. Two consecutive simulated rainfall events were conducted on two Ultisols previously amended with inorganic P fertilizer or broiler litter. Soil test P (Bray 1 and Olsen) levels evaluated ranged from 1 to 350 mg kg(-1). Surface runoff concentrations of total P (TP) and dissolved P (DP) generated by a 30-min runoff event were quantified. Runoff DP concentrations ranged from 0.08 to 3.98 mg L-1 in fertilizer P-amended soils and from 0.08 to 4.93 mg L-1 in broiler litter-amended soils. A single exponential model adequately described the relationships between soil test P and DP concentrations in runoff. For each soil, the, soil test P-DP concentration relationships were positively influenced by soil organic matter and negatively influenced by antecedent soil moisture (P < 0.05). For both soils, the soil test P-DP concentration relationships were positively influenced by groundcover percentage and negatively influenced by slope. Environmental soil test P critical levels corresponding to a runoff threshold of 1 mg L-1 DP, ranged between 176 and 296 mg kg(-1) (Olsen) and 143 to 276 mg kg(-1) (Bray 1) in soils amended with fertilizer-P. In broiler litter-amended soils, threshold values were 88 and 111 mg kg(-1) using Olsen and Bray 1, respectively. Differences in surface runoff-P concentrations due to amendment sources, antecedent soil moisture content, soil organic matter, groundcover and slope suggest that these factors need to be considered in P management decisions at the farm level.
机译:拉米雷斯·阿维拉(Ramire-Avila,J. R.),索托马约尔·拉米雷斯(D. Sotomayor-Ramirez,D.),马丁内斯·罗德里格斯(Martinez-Rodriguez,G.A.)和佩雷斯·阿莱格里亚(Perez-Alegria,L.R。)。2011年。径流中的磷来自热带的两种高度风化土壤。能够。 J.土壤科学。 91:267-277。土壤磷(P)含量高的农田是造成地表水降解的重要因素。在先前用无机磷肥或肉鸡垫料改良过的两种Ultisol上进行了两次连续的模拟降雨事件。评估的土壤测试P(Bray 1和Olsen)水平为1至350 mg kg(-1)。量化了由30分钟径流事件产生的总P(TP)和溶解的P(DP)的地表径流浓度。在施用磷肥的土壤中,径流DP的浓度范围为0.08至3.98 mg L-1,而在用火鸡粪处理的土壤中,径流DP的浓度范围为0.08至4.93 mg L-1。一个单一的指数模型充分描述了径流中土壤测试P和DP浓度之间的关系。对于每种土壤,土壤测试P-DP浓度关系均受到土壤有机质的正向影响,而受前期土壤水分的不利影响(P <0.05)。对于两种土壤,土壤测试P-DP浓度关系都受到地被植物百分比的正影响,而受到坡度的负面影响。在修正的土壤中,环境土壤测试的P临界水平对应于1 mg L-1 DP的径流阈值,范围在176至296 mg kg(-1)(Olsen)和143至276 mg kg(-1)(草1)之间与肥料-P。在肉鸡垫料改良土壤中,使用Olsen和Bray 1的阈值分别为88和111 mg kg(-1)。由于修正源,前期土壤含水量,土壤有机质,地被植物和坡度造成的地表径流磷浓度差异表明,在农场一级的磷管理决策中需要考虑这些因素。

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