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Phosphorus in Finnish soils in the 1900s with particular reference to the acid ammonium acetate soil test

机译:1900年代芬兰土壤中的磷,特别参考酸性乙酸铵土壤试验

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Comprehensive research into phosphorus (P) in soils and crops began in Finland in the early 1900s. The average amount of total P in the ploughed topsoil layer of mineral soils was about two tonnes per hectare in the 1930s, before the abundant use of fertilisers. The main chemical fractions of P in mineral soils were organic matter, primary apatite and secondary complexes of the hydrous oxides of Al and Fe. Of the smaller amounts of P in light peat soils, as much as 80% was present in stable organic compounds. Field experiments showed that the native P reserves of Finnish soils are poorly available to plants, and that P fertilisers are inefficiently utilised because of the strong fixation of applied phosphate in soils. In evaluations before the late 1950s, all simple chemical tests appeared to be rather unreliable indicators of the supply of P from soils to plants, but later research has shown that the results were impaired by errors implicit in the research materials. Some soil test P values (STP)obtained from old samples stored for more than ten years evidently were too high, particularly for organic soils, and many of the soils studied were strongly acidic and therefore biologically less fertile than the chemical P tests indicated. The acid ammonium acetate method (pH 4.65) was introduced in the early 1950s and has since been used in routine soil testing in Finland, not only for P but for all macronutrients except N. In later evaluations of different methods used for estimating the requirement of P fertilisation, the acid ammonium acetate method has proven equal or superior to any other simple chemical method.;
机译:1900年代初,芬兰开始对土壤和农作物中的磷进行全面研究。在大量使用肥料之前,1930年代耕作的矿质土壤表土层中的平均P总量约为每公顷2吨。矿质土壤中磷的主要化学成分是有机质,磷灰石和铝和铁的水合氧化物的二级络合物。在轻质泥炭土壤中少量的P中,稳定的有机化合物中存在多达80%的P。田间试验表明,芬兰土壤的天然P储量几乎无法为植物所利用,而且由于磷肥在土壤中的牢固固定,磷肥的利用效率低下。在1950年代后期之前的评估中,所有简单的化学测试似乎都不是从土壤到植物的磷供应的可靠指标,但后来的研究表明,研究材料中隐含的误差会损害结果。从存储了十年以上的旧样品中获得的一些土壤测试P值(STP)显然过高,尤其是对于有机土壤,而且研究的许多土壤都是强酸性的,因此生物学上比化学P测试低。乙酸乙酸铵法(pH 4.65)于1950年代初期引入,此后已用于芬兰的常规土壤测试中,不仅用于磷,而且用于除氮以外的所有其他常量营养素。在随后的评估中,使用不同的方法来评估磷乙酸铵法已证明与其他简单化学方法相同或优于其他方法。

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