砂土供磷特性及磷肥效应研究
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CHARACTERS OF PHOSPHORUS SUPPLY AND RESPONSE TO PHOSPHATIC FERTILIZER IN SANDY SOILS
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    摘要:

    砂土供磷特性及磷肥效应的研究结果表明,砂土磷素形态以无机磷为主,有机磷甚少,仅占全磷含量的8.84%.无机磷占91.15%,无机磷形态组成以磷酸钙为主,Ca-P平均为无机磷总量的86.1%,O-P占9.6%,Al-P占3%,Fe-P占1.3%.各种形态无机磷与速效磷的关系为:y(速效磷)=49.30x1(AL-P)+21.8547x4(Ca-P)-3.4209,表明Al-P、CX-P对砂土速效磷的贡献具有一定的意义,磷酸铁铝和磷酸钙盐均可以作为砂土磷素的给源。磷肥的作用主要在作物牛育前期,而在中、后期则更多的吸收利用土壤中的磷素。粗、细砂潮土小麦磷肥的肥效分别比轻砂潮土高41.1%和17.7%.

    Abstract:

    The study on characters of phosphorus supply and response to phosphatic fertilizer showed that inorganic p and organic P accounted for 91.12% and 8.87% respectively. In the former Ca-P,O-P, Al-P and Fe-P accounted for 86.1%,9.6%, 3.0% and 1.3% respectively. The relation between inorganic-P forms and rapidly available phosphorus (RAP) could be described by y(RAP)=49.30x1(AL-P)+21.8547x4(Ca-P)-3.4209, which indicated the significance of Al-P and Ca-P to RAP and the feasibility that iron and aluminum phosphates and calcium phosphates served as soures to soil P. The growth and decline of total P and available P deponded on P balance in soils. The changes of P forms in fertilizers aapplied relied on soil properties. The great effect of fertilizer P occurred at the early growth stage of plants. At the middle and late stages, plant took up more soil P. P-fertilizer efficiency in coarse and fine sand soils was 41.1% and 17.7% respectively, higher, than that in light sand soil.

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王秋杰,寇长林,王永歧,祝秀花,王恒玉.砂土供磷特性及磷肥效应研究[J].土壤学报,1996,33(4):366-372. DOI:10.11766/trxb199504260406 Wang Qiujie, Kou Changlin, Wang Yongqi, Zhu Xinhua, Wang Hengyu. CHARACTERS OF PHOSPHORUS SUPPLY AND RESPONSE TO PHOSPHATIC FERTILIZER IN SANDY SOILS[J]. Acta Pedologica Sinica,1996,33(4):366-372.

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  • 收稿日期:1995-04-26
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  • 在线发布日期: 2013-02-25
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