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The fate of nitrogen and phosphorus in soil receiving 30 annual cattle manure applications

机译:每年接受30次牛粪的土壤中的氮和磷的命运

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Improving nutrient management of livestock manure will benefit both agricultural production and the environment. This paper examines the fate of nitrogen and phosphorus nutrients in soil receiving 30 annual cattle manure applications under both rainfed and irrigated conditions in a semiarid climate. Solid cattle feedlot manure has been applied since 1973 in a split-plot experiment to rain-fed and irrigated well-drained Dark Brown Chemozemic clay loam at 0, 30, 60 and 90 Mg ha~(-1) yr~(-1) (wet wt) on rain-fed and 0, 60, 120 and 180 Mg ha~(-1) yr~(-1) on irrigated land under semi-arid climate conditions in Lethbridge, Alberta, Canada. The cumulative amount of manure TC, TN and TP applied between 1973 and 2003 increased with rate of manure application and the amount applied was much higher than that removed by crop uptake. Crop production used only about 12 to 33% manure N and 4% to 12% manure P applied over 30 years. Even at the recommended agronomic rate, crops only used 29% N and 10% P under rainfed and 33% N and 12% P under irrigated conditions. As a result, significant amounts of C, N and P accumulated in the soil. In addition, NO_3 accumulates in the soil profile with greater soil NO_3 content under rainfed conditions. Although soil NO_3 content was not as high, greater amounts of NO_3 have leached to the groundwater under irrigation. The residual effect of 14 years of manure application, even at the recommended agronomical rate, was long lasting. The C, N and P content in soil was still elevated even after 16 years of no manure applications. The high level of N and P content in soil could pose pollution risks as the nutrient rich soil erodes and is deposited onto nearby surface water.
机译:改善牲畜粪便的营养管理将有益于农业生产和环境。本文研究了半干旱气候下,在雨养和灌溉条件下,每年接受30种牛粪肥的土壤中氮和磷的养分归宿。自1973年以来,已在分块试验中应用了固态牛粪肥,对0、30、60和90 Mg ha〜(-1)yr〜(-1)的雨养和灌溉良好的排水型深棕色化肥壤土进行了施用。在加拿大阿尔伯塔省莱斯布里奇市的半干旱气候条件下,在雨水喂养的土地上(湿重)和在灌溉土地上的0、60、120和180 Mg ha〜(-1)yr〜(-1)。 1973年至2003年间施肥的TC,TN和TP的累积量随施肥率的增加而增加,施肥量远高于作物吸收的量。在30年中,作物生产仅使用了约12%至33%的氮肥和4%至12%的磷肥。即使以推荐的农艺率,在雨育条件下农作物仅使用了29%的氮和10%的磷,在灌溉条件下仅使用了33%的氮和12%的磷。结果,大量的C,N和P累积在土壤中。另外,在雨育条件下,NO_3累积在土壤剖面中,NO_3含量更高。尽管土壤NO_3含量不高,但灌溉条件下有更多的NO_3渗入地下水。即使以推荐的农艺速率施用,施用14年肥料的残留效果也持久。即使不施肥16年,土壤中的C,N和P含量仍然升高。土壤中高含量的N和P可能会造成污染风险,因为营养丰富的土壤会侵蚀并沉积在附近的地表水中。

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