首页> 外文期刊>Australian Journal of Soil Research >Fate of applied biosolids nitrogen in a cut and remove forage system on an alluvial clay loam soil.
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Fate of applied biosolids nitrogen in a cut and remove forage system on an alluvial clay loam soil.

机译:在冲积壤土上切割并去除草料系统后,施加的生物固氮的命运。

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The fate of nitrogen (N) applied in biosolids was investigated in a forage production system on an alluvial clay loam soil in south-eastern Queensland, Australia. Biosolids were applied in October 2002 at the rates of 6, 12, 36, and 54 dry t/ha for aerobically digested biosolids (AE) and 8, 16, 48, and 72 dry t/ha for anaerobically digested biosolids (AN). Rates were based on multiples of the nitrogen limited biosolids application rate (0.5, 1.0, 3.0, and 4.5NLBAR) for each type of biosolid. The experiment included an unfertilized control and a fertilized control that received multiple applications of synthetic fertilizer. Forage sorghum was planted 1 week after biosolids application and harvested 4 times between December 2002 and May 2003. Dry matter production was significantly greater from the biosolids-treated plots (21-27 t/ha) than from the unfertilized (16 t/ha) and fertilized (18 t/ha) controls. The harvested plant material removed an extra 148-488 kg N from the biosolids-treated plots. Partial N budgets were calculated for the 1NLBAR and 4.5NLBAR treatments for each biosolids type at the end of the crop season. Crop removal only accounted for 25-33% of the applied N in the 1NLBAR treatments and as low as 8-15% with 4.5NLBAR. Residual biosolids N was predominantly in the form of organic N (38-51% of applied biosolids N), although there was also a significant proportion (10-23%) as NO3-N, predominantly in the top 0.90 m of the soil profile. From 12 to 29% of applied N was unaccounted for, and presumed to be lost as gaseous nitrogen and/or ammonia, as a consequence of volatilization or denitrification, respectively. In-season mineralization of organic N in biosolids was 43-59% of the applied organic N, which was much greater than the 15% (AN)-25% (AE) expected, based on current NLBAR calculation methods. Excessive biosolids application produced little additional biomass but led to high soil mineral N concentrations that were vulnerable to multiple loss pathways. Queensland Guidelines need to account for higher rates of mineralization and losses via denitrification and volatilization and should therefore encourage lower application rates to achieve optimal plant growth and minimize the potential for detrimental impacts on the environment.
机译:在澳大利亚昆士兰州东南部的一个冲积粘土壤土上,在草料生产系统中研究了生物固体中氮素的命运。 2002年10月,需氧消化的生物固体(AE)的施用量为6、12、36和54干吨/公顷,厌氧消化的生物固体(AN)的施用量为8、16、48和72干吨/公顷。比率基于每种类型的生物固体氮限制的生物固体施用率(0.5、1.0、3.0和4.5NLBAR)的倍数。该实验包括一个未施肥的对照和一个接受了多次施用化肥的施肥的对照。饲草高粱在施用生物固体后1周种植,在2002年12月至2003年5月之间收获了4次。高粱的生物物质处理量(21-27吨/公顷)比未施肥(16吨/公顷)的干物质产量高得多。和施肥的(18吨/公顷)对照。收获的植物材料从经过生物固体处理的地块中除去了额外的148-488 kg氮。在作物季节结束时,针对每种生物固体类型的1NLBAR和4.5NLBAR处理计算了部分N预算。在1NLBAR处理中,农作物的去除仅占施氮量的25-33%,而对于4.5NLBAR,其去除率仅为8-15%。残留的生物固体氮主要以有机氮的形式(占施用的生物固体氮的38-51%),尽管也有相当一部分(10-23%)的NO 3 N,主要是土壤剖面的顶部0.90 m。由于挥发或反硝化作用,未解释的施用N中有12%到29%的N被认为是气态氮和/或氨而损失掉。根据当前的NLBAR计算方法,生物固体中有机氮的季节性矿化作用为所施用有机氮的43-59%,远大于预期的15%(AN)-25%(AE)。过量施用生物固体几乎没有产生额外的生物量,但导致土壤矿物质氮含量高,容易受到多种损失途径的影响。昆士兰准则需要考虑到较高的矿化率和通过反硝化和挥发造成的损失,因此应鼓励降低施药量以实现最佳的植物生长,并最大程度地减少对环境造成不利影响的可能性。

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