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Split phosphorus fertiliser applications as a strategy to reduce incidental phosphorus losses in surface runoff

机译:分裂磷肥应用作为降低表面径流偶然磷损失的策略

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Organic soils have low sorption capacities for phosphorus (P), and may pose a risk of P loss to water if P applications to these soils coincide with runoff events. Little is known about the magnitude of exports of P in overland flow following application of P fertiliser onto these soils, or on the influence of the frequency on P losses and persistence. The number of P fertiliser applications was surveyed across 39 commercial farms to assess current practice and inform the design of a rainfall runoff experiment to evaluate the effect of frequency of P applications on losses and persistence across time. Superphosphate (16% P) was applied in single (equivalent to 30 and 55 kg P ha(-1) applied at day 0) and split (equivalent to 15 and 27.5 kg P ha(-1) applied in two doses at days 0 and 55) applications to an organic soil inclined at a slope of 6% in a rainfall simulator experiment. The surface runoff of dissolved reactive phosphorus (DRP) was measured in controlled 30-min rainfall simulations conducted intermittently over an 85-day period. The DRP losses in surface runoff after the first rainfall event were 44.6 and 97.8 mg L-1 for single applications of 30 and 55 kg ha(-1), respectively, and 13.3 and 21.8 mg L-1 for the same rates split in two doses, indicating that single P applications had disproportionately bigger impacts on losses than split applications. This supports the idea that frequent, but smaller, P applications can minimise the impact of fertilisation on waters. Dissolved reactive P concentrations remained significantly higher than those from the control samples until the end the experiment for almost all the P treatments, highlighting the long-lasting effects of added P and the elevated risk of P losses on organic soils. For climates with frequent rainfall events, which are likely to coincide with fertiliser applications, smaller but more frequent P applications can reduce the risk of P transfer as opposed to one single application.
机译:有机土壤对磷(P)吸附能力低,如果P应用与径流事件相一致,可能会对水进行P损失的风险。在将P肥料施加到这些土壤中或对P损失和持久性频率的影响下,陆上流动出口幅度少众所周知。在39个商业农场调查了P肥料应用的数量,以评估目前的实践,并告知降雨径流试验,以评估P应用频率对跨时损失和持久性的影响。施用过磷酸(16%P)以在第0天施加的单一(相当于30和55kg p Ha(-1))中,并分裂(相当于15和27.5kg p ha(-1)在0天0剂量中施用55)在降雨模拟器实验中以6%的斜率倾斜的有机土壤的应用。溶解的反应性磷(DRP)的表面径差在85天的时间间歇性地进行的30分钟的降雨模拟中测量。第一个降雨事件后表面径流的DRP损失为44.6和97.8mg L-1,分别为30和55千克(-1),以及21.3和21.8mg L-1,其相同的速率分为两个剂量,表明单个P应用的损失对损耗的影响比分流应用更大。这支持频繁但更小,P应用的想法可以最大限度地减少施肥对水域的影响。溶解的活性P浓度仍然显着高于对照样品的浓度,直到终止几乎所有P治疗的实验,突出了添加的P的持久效果以及有机土壤上的P损失的升高效果。对于具有频繁的降雨事件的气候,可能与肥料应用重合,更小但更频繁的P应用可以降低P转移的风险,而不是一个应用。

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