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首页> 外文期刊>Archives of Agronomy and Soil Science >Changes in recovery of native and applied phosphorus with time as affected by soil properties in some calcareous soils
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Changes in recovery of native and applied phosphorus with time as affected by soil properties in some calcareous soils

机译:一种随时间的土着和应用磷的恢复变化,其受到一些钙质土壤的土壤性质影响

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In an attempt to investigate variations in availability of native and applied phosphorus (P) with time, twenty five calcareous soil samples were treated with 0, 50 and 500 mg P kg(-1) soil and incubated at 80-90% of field capacity moisture content in an open door glasshouse for a period of one year. Soil samples were taken out at certain intervals for P extraction with Olsen extractant under moist condition. Results indicated that following wetting the mean value of native Olsen-P decreased initially and then increased gradually with time of incubation. Generally, the short term (24 h) recoveries were not correlated with long term ones. The recovery of added P with time was described properly by the following new proposed model: R = 100/(1 + kt(b)), where R is percent recovery at time t, and k and b are empirical parameters. The values of k constant at 50 and 500 mg P kg(-1) were in the ranges of 0.40 to 1.22 (0.84 +/- 0.25, on average) and 0.04 to 0.52 (0.23 +/- 0.14, on average), respectively. The corresponding respective values of b constant also ranged from 0.05 to 0.32 (0.15 +/- 0.06, on average) and 0.12 to 0.92 (0.46 +/- 0.23, on average).
机译:试图随时间调查天然和应用磷(P)的可用性的变化,用0,50和500mg p kg(-1)土壤处理二十五种钙质土壤样品,并以80-90%的现场容量孵育开放式玻璃室里的水分含量为一年。在潮湿条件下以某些间隔取出土壤样品,以便在湿条件下用Olsen萃取剂进行P.结果表明,在润湿后,原硝酮-P的平均值最初降低,然后随着孵育的时间逐渐增加。通常,短期(24小时)回收不与长期术语相关。通过以下新的提出模型适当地描述了随时间的添加P的恢复:r = 100 /(1 + kt(b)),其中R是在时间t的百分比,K和B是经验参数。在50和500mg p kg(-1)时的k常数值分别为0.40至1.22(0.84 +/- 0.25,平均值)和0.04至0.52(平均0.23 +/- 0.14)的范围。相应的B常数值也范围为0.05至0.32(平均0.15±0.06,平均为0.92(平均0.46 +/- 0.23)。

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