首页> 外文期刊>European Journal of Agronomy >Effect of soil-N and urine-N on nitrate leaching under pure grass, pureclover and mixed grass/clover swards
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Effect of soil-N and urine-N on nitrate leaching under pure grass, pureclover and mixed grass/clover swards

机译:氮,尿素氮对纯草,纯三叶草和混草/三叶草覆盖下硝酸盐淋失的影响

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摘要

During six annual drainage periods (DPO to DP5). the drainage water, the NO3 concentration of the: drainage water and the total leached N were compared under bare soils and under ryegrass/white clover, pure ryegrass and pure white clover stands in 80 deep lysimeters with 3m(2) area. For each soil cover, the sensitivity of the variables to the soil N supplying capacity at sowing was measured, using a set up of 32 lysimeters. This initial capacity to supply mineral N (SoilN) varied from 90 to 230 kg N ha(-1) year(-1). The stands were managed in a simulated rotational grazing system, without addition of fertilizer N. During the first drainage period after sowing (DP0), N leaching increased significantly with the initial SoilN under the bare soils, the pure grass and the mixture, but wits not influenced under the pure clover. in the following drainage periods, N leaching increased according to the sequence pure grass (1-5 kg N ha(-1) year(-1)), mixed swards (1-19 kg N), pure white clover(28-140 kg N) and bare soils (84-149 kgN ha(-1) year(-1)). It was only slightly greater under the mixture than under the pure grass. despite the N harvest and the N animal returns were much higher. Under the mixed stands, N leaching became independent of the initial SoilN in DP1 and DP2 and decreased with increasing initial SoilN in DP3, DP4 and DP5. This inversion of the SoilN effect in time and the limited amounts of leached N demonstrated that adaptations in the ecosystem tend to counteract the SoilN effect on the N losses. In the mixed stands, the accumulated N leaching represented 12 and 21% of the accumulated N at harvest for the initially rich and poor soils. respectively and 32% of the accumulated N harvest in the mixed clover, whatever the initial SoilN. N leaching also represented 13%, of the urine-N above 80 kgN ha(-1) year(-1). The low values of N leaching under the mixed swards make them sustainable for environment quality. Mechanisms which regulate the N fluxes are discussed, using published data on the soil and some results concerning the harvests in the same experiment.
机译:在六个年度排水期间(DPO至DP5)。比较了裸露土壤和黑麦草/白三叶草,纯黑麦草和纯白三叶草在80 m深(3m(2))的土壤中的排水,NO3浓度和总浸出氮。对于每个土壤覆盖层,使用32个测力计,测量变量对播种时土壤氮素供应能力的敏感性。最初提供矿物质N(SoilN)的能力从90到230 kg N ha(-1)年(-1)不等。在模拟旋转放牧系统中对林分进行管理,不添加肥料氮。在播种后的第一个排水期(DP0),在裸土,纯草和混合肥下,初始土壤N的淋溶氮显着增加,但是机智不受纯三叶草的影响。在接下来的排水期中,N淋溶按以下顺序增加:纯草(1-5 kg N ha(-1)年(-1)),杂草(1-19 kg N),纯白三叶草(28-140) kg N)和裸土(84-149 kgN ha(-1)年(-1))。在混合物下,它仅比在纯草下略大。尽管收获了N种,而N种动物的回报却更高。在混合林下,氮的淋失与DP1和DP2中的初始土壤氮无关,并随着DP3,DP4和DP5中的初始土壤氮增加而减少。时间上的土壤氮效应的这种反转和有限量的淋溶氮的量表明,生态系统的适应趋向于抵消土壤氮对氮损失的影响。在混合林中,最初富土壤和贫土壤的累积氮淋失分别占收获时累积氮的12%和21%。不论最初的土壤氮量是多少,混合三叶草的氮素累积量分别为32%。 N浸出也占尿N的13%,高于80 kgN ha(-1)年(-1)。混合草皮下氮素淋溶的低值使其对环境质量具有可持续性。讨论了调节氮通量的机制,使用了已发表的土壤数据以及同一实验中有关收获的一些结果。

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