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对盆栽的伴生有金雀花(Cytisus scoparius)、黑麦草(Lolium multiflorum)的辐射松(Pinus radiata)幼苗施用3种浓度(O,50,100 μg·g-1)的三过磷酸钙,14个月后测定缺磷Allophanic土壤中各磷形态变化,确定根际土壤中施加的磷肥的去向.结果表明,施加磷肥增加了根际土壤中NaOH-Pi、NaOH-P0和H2SO4-Pi的浓度,但是减少了土壤残留磷的含量,而树脂磷浓度维持不变,在这种土壤中树脂磷浓度仍然较低(1 to 3μg·g-1).施加到土壤里的磷肥,有机磷的回收率最高(40%-49%),这是因为这种土壤具有较高的磷固定能力(92%),其次是不稳定有机磷(7%-19%).在磷肥缺乏或不施加磷肥的情况下,辐射松根际土壤中有机磷浓度低于周边土壤以及金雀花、黑麦草根际土壤.这可能与磷肥缺乏条件下,根系和菌根产生较高的草酸盐而释放部分磷到根际土壤中有关.但此观点需要进一步的研究检验.“,”Changes in phosphorus (P) fractions in a P deficient allophanic soil under P. radiata seedlings grown with broom (Cytisus sco-parius L.) and ryegrass (Lolium multiflorum) in pots were studied 14 months after the application of triple superphosphate at the rates of 0, 50, and 100 μg·g-1, to determine the fate of fertiliser-derived P in the rhizosphere soils. Application of P fertiliser increased NaOH-Pi, NaOH-Po, and H2SO4-Pi concentrations in the soil, but decreased the residual-P concentration. The resin-Pi concentration, which is ex-tremely low in this soil (1 to 3 μg·g-1 ), remained the same. The majority of the added fertiliser P was however recovered in the NaOH-Pi fraction (40%-49%). This is due to the high P fixation in this soil (92%). The second highest P recovery was in NaOH-Po fraction (7%-19%). Under P deficient condition or addition at the rate of 0 μg·g-1, the NaOH-P1 concentration in the radiata rhizosphere soil was lower than that in the bulk soil end broom and grass rhizosphere soils. This may be due to higher oxalate production by the roots and my-corrhiza under P deficient conditions which released some of the P fixed to the soils in the rhizosphere, which needs to be tested in futurestudies.