首页> 外文OA文献 >Sustaining productivity of a Vertosol at Warra, Queensland, with fertilisers, no-tillage or legumes. 8. Effect of duration of lucerne ley on soil nitrogen and water, wheat yield and protein.
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Sustaining productivity of a Vertosol at Warra, Queensland, with fertilisers, no-tillage or legumes. 8. Effect of duration of lucerne ley on soil nitrogen and water, wheat yield and protein.

机译:使用肥料,免耕或豆类维持昆士兰州Warra的Vertosol生产效率。 8.卢塞恩莱病的持续时间对土壤氮和水,小麦产量和蛋白质的影响。

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摘要

Soil nitrogen (N) supply in the Vertosols of southern Queensland, Australia has steadily declined as a result of long-term cereal cropping without N fertiliser application or rotations with legumes. Nitrogen-fixing legumes such as lucerne may enhance soil N supply and therefore could be used in lucerne-wheat rotations. However, lucerne leys in this subtropical environment can create a soil moisture deficit, which may persist for a number of seasons. Therefore, we evaluated the effect of varying the duration of a lucerne ley (for up to 4 years) on soil N increase, N supply to wheat, soil water changes, wheat yields and wheat protein on a fertility-depleted Vertosol in a field experiment between 1989 and 1996 at Warra (26degrees 47'S, 150degrees53'E), southern Queensland. ududThe experiment consisted of a wheat-wheat rotation, and 8 treatments of lucerne leys starting in 1989 (phase 1) or 1990 (phase 2) for 1,2,3 or 4 years duration, followed by wheat cropping. Lucerne DM yield and N yield increased with increasing duration of lucerne leys. Soil N increased over time following 2 years of lucerne but there was no further significant increase after 3 or 4 years of lucerne ley. Soil nitrate concentrations increased significantly with all lucerne leys and moved progressively downward in the soil profile from 1992 to 1995. Soil water, especially at 0.9-1.2 m depth, remained significantly lower for the next 3 years after the termination of the 4 year lucerne ley than under continuous wheat. No significant increase in wheat yields was observed from 1992 to 1995, irrespective of the lucerne ley. However, wheat grain protein concentrations were significantly higher under lucerne-wheat than under wheat wheat rotations for 3-5 years. The lucerne yield and soil water and nitrate-N concentrations were satisfactorily simulated with the APSIM model. Although significant N accretion occurred in the soil following lucerne leys, in drier seasons, recharge of the drier soil profile following long duration lucerne occurred after 3 years.ududConsequently, 3- and 4-year lucerne-wheat rotations resulted in more variable wheat yields than wheat-wheat rotations in this region. The remaining challenge in using lucerne-wheat rotations is balancing the N accretion benefits with plant-available water deficits, which are most likely to occur in the highly variable rainfall conditions of this region.
机译:由于不施用氮肥或豆科作物轮作的长期谷物作物的种植,澳大利亚昆士兰州南部凡尔托溶胶的土壤氮(N)供应量稳步下降。诸如卢塞恩这样的固氮豆类作物可以增加土壤氮的供应,因此可以用于苜蓿/小麦的轮作。但是,在这种亚热带环境中,卢塞恩麦芽会造成土壤水分不足,并可能持续多个季节。因此,我们在田间试验中评估了改变苜蓿持续时间(长达4年)对土壤N的增加,氮素对小麦的供应,土壤水分的变化,小麦的产量和小麦蛋白对贫瘠的Vertosol的影响。 1989年至1996年在昆士兰州南部的Warra(南纬26度47度,北纬150度53度)。这项实验由小麦小麦轮作组成,从1989年(第1阶段)或1990年(第2阶段)开始,共进行了1,2,3或4年的8种卢塞恩病处理,然后进行了小麦种植。卢塞恩DM产量和N产量随卢塞恩麦穗持续时间的增加而增加。卢塞恩2年后土壤N随时间增加,但在3或4年卢塞恩莱后土壤N不再进一步显着增加。从1992年到1995年,所有苜蓿的土壤硝酸盐浓度均显着增加,并且在土壤剖面中逐渐向下移动。在4年期苜蓿终止后的接下来的3年中,尤其是深度在0.9-1.2 m的土壤水仍然显着降低。比连续麦下。从1992年到1995年,无论卢塞恩利如何,小麦单产都没有显着增加。但是,在3-5年内,卢塞恩小麦的小麦籽粒蛋白质浓度显着高于小麦小麦轮作。使用APSIM模型可以令人满意地模拟了苜蓿产量,土壤水分和硝酸盐氮含量。尽管卢塞恩ley发生后土壤中明显增加了N的吸收,但在较干燥的季节中,3年后长期使用卢塞恩后,较干燥的土壤剖面发生了补给。 ud ud,因此3年和4年的卢塞恩小麦轮作导致更多的变化该地区的小麦单产高于小麦轮作。使用苜蓿/小麦轮作的另一个挑战是,在氮素增加带来的好处与植物可利用的水分亏缺之间取得平衡,这最有可能发生在该地区降雨多变的情况下。

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