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

机译:分割施用磷肥作为减少地表径流中偶然磷损失的策略

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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)的吸附能力低,如果向土壤中施用磷与径流事件同时发生,则可能造成磷向水中损失的风险。在这些土壤上施用磷肥后,对陆上磷流失的出口量或频率对磷流失和持久性的影响知之甚少。在39个商业农场中对磷肥的施用量进行了调查,以评估当前的做法,并为降雨径流试验的设计提供依据,以评估磷肥施用频率对时间损失和持久性的影响。过磷酸钙(16%P)以单剂量(相当于在第0天施加30和55 kg P ha(-1)的形式)施用,并分开服用(等效于15和27.5 kg P ha(-1)在第0天以两剂的形式施加) 55)在降雨模拟器实验中,将有机土壤倾斜到6%的坡度。在受控的30分钟降雨模拟中,在85天的时间间隔内进行了间歇性测量,测量了溶解性活性磷(DRP)的表面径流。第一次降雨后,一次径流的DRP损失对于30和55 kg ha(-1)的单次施用分别为44.6和97.8 mg L-1,对于相同的比例分成两份,分别为13.3和21.8 mg L-1剂量,表明单一的P施用对损失的影响比分开的施用更大。这支持这样的想法,即频繁但较小的磷肥施用可以最大程度地减少施肥对水的影响。直到几乎所有磷处理的实验结束,溶解的反应性P浓度仍显着高于对照样品,这突显了添加的P的持久作用以及有机土壤上P损失的风险增加。对于降雨频繁的气候(可能与肥料施用同时发生),与单一施用相比,较小但更频繁的磷施用可以降低磷转移的风险。

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