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Exploiting P in heavily P-dressed fields in Sweden

机译:在瑞典穿着大量P的领域开发P

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Phosphorus status of soils is regarded a component of soil fertility. This component can be influenced by cropping measures. In 1983 a number of Swedish fields with a high P status were identified. In all there were 17 fields chosen distributed overSweden. On these fields P fertilizer experiments were started with the treatments 0, 15 and 30 kg P ha~(-1) yr~(-1). In average of all experimental sites the starting P-AL value was 19.6 mg 100~(-1)g soil. Typically P-AL in Swedish arable soils are lessthan 10 mg, so the 19.6 average is a high value. pH varied from 5.1 to 7.3 with 46 percent of the sites having initial pH values less than 6.2. With no P applied the P-AL values decreased significantly with time. The slope of the regression line indicates that P-AL in the top soil decreased with 0.5 units year~(-1). The decline was statistically significant at the 5 percent level. When 30 kg P year~(-1) was applied the decline was insignificant. In the high pH range (>= 6.2) the decline in P-AL was 0.67 units year~(-1) compared with 0.18 in the low pH group. Measurement of the uptake and removal of P with harvest products was chosen as the best method to analyse the crop response with time. When the experiments were pH grouped and the effects in cereals were analysed a positive effect on the P uptake with time was found.
机译:土壤的磷状态被认为是土壤肥力的一个组成部分。该成分可能会受到裁剪措施的影响。 1983年,瑞典发现了许多P值高的田地。总共有17个字段被选中分布在瑞典各地。在这些领域,以0、15和30 kg P ha〜(-1)yr〜(-1)处理开始磷肥实验。平均所有实验点的起始P-AL值为土壤19.6 mg 100〜(-1)g。瑞典耕地土壤中的P-AL通常小于10 mg,因此平均值19.6是一个很高的值。 pH在5.1到7.3之间变化,其中46%的位点的初始pH值小于6.2。在没有施加P的情况下,P-AL值随时间显着下降。回归线的斜率表明,表层土壤中的P-AL下降了0.5个单位年(-1)。下降幅度为5%,具有统计学意义。当施用30 kg P year〜(-1)时,下降幅度不明显。在高pH范围(> = 6.2)中,P-AL的下降为0.67单位年(-1),而低pH组为0.18。选择收获产品对磷吸收和去除的测量方法作为分析作物随时间变化的最佳方法。当对实验进行pH分组并分析了对谷物的影响时,发现随时间对P吸收有积极影响。

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