The basic phenomena of phosphorus dynamics in soil is important to define the rate and application manners of phosphates fertilizers. The forms'/> Factors affecting the phosphorus availability and the fertilization management in no-tillage system
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Factors affecting the phosphorus availability and the fertilization management in no-tillage system

机译:免耕体系中磷素利用率及施肥管理的影响因素

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> size="2" face="Verdana, Arial, Helvetica, sans-serif">The basic phenomena of phosphorus dynamics in soil is important to define the rate and application manners of phosphates fertilizers. The forms and availability of phosphorus vary with the soil characteristics and properties. In young soils, the calcium phosphates are the main source to organisms. On the other hand, in highly weathered soils the organic phosphorus cycling assumes great importance in the maintenance of the biological bioavailability, although it is insufficient to economical crop productivity. In tropical and subtropical cultivated soils, the soil phosphorus in solution is controlled by phosphorus adsorbed at functional groups of inorganic colloids. The phosphorus diagnosis is made by soils analysis at different methodologies, each one with their advantages and limitations. The decision on adding phosphate and to the rate define is more dependent on the calibration between the value extracted with the crop yield than the extraction method. The elevation of phosphorus availability can be made in corrective or gradual addition. The corrective fertilization is more efficient, and maybe the only alternative, for phosphorus deficiency correction in deeper soil layers. The correction of phosphorus deficiency in deeper layers after the no-tillage system adoption is difficult. The superficial phosphate application in no-tillage seems not to be a good economical alternative and can become an environmental problem. The research must be intensified focusing among others: (a) phosphorus fractions in soil and crop yield; (b) phosphates fertilizers application in no-tillage system; (c) relation of phosphorus availability with exchangeable aluminum and compacted soil layers in soil deep; (d) monitoring of transferred phosphate from soil to aquatic systems.
机译:> size =“ 2” face =“ Verdana,Arial,Helvetica,sans-serif”>土壤中磷动力学的基本现象对于确定磷肥的用量和施用方式很重要。磷的形式和有效性随土壤的特性和性质而变化。在年轻的土壤中,磷酸钙是生物的主要来源。另一方面,在高风化土壤中,有机磷循环在维持生物生物利用度方面起着极为重要的作用,尽管不足以实现经济的农作物生产力。在热带和亚热带的耕作土壤中,溶液中的磷受吸附在无机胶体官能团上的磷的控制。磷的诊断是通过土壤分析的不同方法进行的,每种方法都有其优势和局限性。添加磷酸盐和确定速率的决定,与提取方法相比,更取决于作物产量提取的值之间的校准。磷的利用率可以通过校正或逐步添加来提高。纠正性施肥对于更深层土壤中的磷缺乏症纠正更为有效,并且也许是唯一的选择。免耕系统采用后,很难纠正深层的磷缺乏症。免耕浅表施用磷酸盐似乎不是一个好的经济选择,并且可能成为环境问题。必须加强研究,重点包括:(a)土壤和作物产量中的磷含量; (b)在免耕系统中使用磷肥; (c)深层土壤中磷的有效性与可交换铝和压实土壤层的关系; (d)监测从土壤向水生系统转移的磷酸盐。

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