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Soil Phosphorus Release to the Water Bodies in the Upland Fields of Yellow Soil Areas and Impacting Factor

机译:黄壤旱地土壤磷素向水体的释放及其影响因素。

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摘要

Soil phosphorus release to the water bodies in the upland fields of yellow soil areas and impacting factor was studied in Guizhou province. The results showed that the content of dissolved active P of surface runoff from various upland fields of yellow-soil were significantly different, which the concentrations of dissolved active P of runoff correlated with the contents of available-P, amorphous oxides of Al, and organic matter in the soils. The amount of soil phosphorus release to the water bodies affected by the level of applying P fertilizer and the process of corn growth, which with fertilizing from 150 to 900 kg P_2O_5 ha~(-1) in the soil with high P level, the average contents of dissolved active P in the permeability-water of the soil increased from 0.020 mg L~(-1) to 0.137 mg L~(-1). The amount of soil phosphorus release to the water bodies also affected by environmental factor, which the amount of soil phosphorus release significantly increased under the conditions that temperature is 30℃-35℃, water/soil ratios is 15:1-25:1, submergence-time by water is 12-18 h and pH value of acid rains is 3.82-3.73.
机译:研究了贵州省黄壤旱地水体中磷的释放及其影响因素。结果表明,黄壤不同旱田地表径流的溶解态活性P含量存在显着差异,径流中的溶解态活性P含量与有效磷,铝的无定形氧化物和有机质含量相关。在土壤中的物质。施磷水平和玉米生长过程对水体的磷释放量影响较大。在高磷水平下,施肥量为150〜900 kg P_2O_5 ha〜(-1),平均土壤渗透性水中溶解态活性P的含量从0.020 mg L〜(-1)增加到0.137 mg L〜(-1)。土壤磷释放量也受环境因素的影响,温度为30℃-35℃,水土比为15:1-25:1时,土壤磷释放量显着增加,水中浸泡时间为12-18 h,酸雨的pH值为3.82-3.73。

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