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      <ref-type name="Journal Article">17</ref-type>
      <contributors>
        <authors>
          <author>O. U. Rehman</author>
          <author>S. M. Mehdi</author>
          <author>M. Sarfraz M. A. Shakir</author>
          <author>G. Shabir Soil</author>
        </authors>
      </contributors>
      <titles>
        <title>PHOSPHORUS DYNAMICS IN RASULPUR SOIL SERIES ( T YPIC CAMBORTHID) UNDER RICE BASED CROPPING SYSTEM</title>
        <secondary-title>Journal of Animal and Plant Sciences</secondary-title>
        <alt-title>JAPS</alt-title>
      </titles>
      <dates><year>2013</year><pub-dates><date>2013/04/01</date></pub-dates></dates>
      <volume>23</volume>
      <number>2</number>
      <pages>480-486</pages>
      <isbn>1018-7081</isbn>
      <electronic-resource-num>NA</electronic-resource-num>
      <abstract>&lt;p&gt;Phosphorus (P) nutrition of the rice cropping system is very important due to alternate wetting and drying cycles. A field experiment was conducted on a sandy loam soil (Typic Camborthid) to observe residual effect of P on succeeding crops and rate of P depletion after one crop rotation (wheat- sorghum fodder-rice). Rice was raised as second crop on the residual P after sorghum fodder, grown after wheat. Analysis of variance (ANOVA) technique under RCBD was used and Duncan&amp;rsquo;s multiple range test (DMR) was applied to see the significance of difference among treatment means. Maximum residual P after sorghum fodder was 13.10 mg kg-1 , considered quite sufficient for rice crop. The significantly higher yield of paddy (2.83 Mg ha-1) and straw (2.96 Mg ha-1) was found where residual P was 10.65 mg kg-1 soil. Maximum P concentration (0.15 %) in paddy was found at highest residual P level while in straw it was maximum (0.10 %) where residual P was 10.65 mg kg-1 soil. Similar trend was found in case of P uptake i.e. it was significantly higher in paddy (4.22 Kg ha-1) at highest residual P level and straw (3.05 Kg ha-1) where residual P was 10.65 mg kg-1 while total P uptake was maximum (7.20 kg ha-1) at highest residual P level. Maximum Olsen- P (8.70 mg kg-1) was found after harvest of rice crop where maximum P was applied to wheat. Level of P depletion at the end of three crops was found to be 0.004 mg kg-1 annum-1 where P was applied at 13.76 mg kg-1 soil and this depletion was promoted where no NPK was applied and further deterioration was noticed where only NK was applied without P. However at the higher rates of P application, there was no net P depletion It may be concluded from this study that phosphatic fertilizers be recommended and applied to the crops by taking P adsorption capacities into the account and P application should be soil and crop specific as the solution P and Olsen P vary with varying soils and crops. The residual P upto 13.1 mg Kg-1 can support 2 to 3 succeeding crops in loose textured soils and soils are being mined annum-1 @ 0.138 mg P kg-1 if no fertilizers are applied @ 0.149 mg P kg-1 if only NK are applied in light textured soils under rice cropping system.&lt;/p&gt;</abstract>
      <keywords><keyword>P decline rate, phosphorus, residual effect, rice, Typic Camborthid</keyword></keywords>
      <publisher>Pakistan Agricultural Scientists Forum</publisher>
      <urls><related-urls><url>https://thejaps.org.pk/AbstractView.aspx?mid=2013-JAPS-225</url></related-urls></urls>
    </record>
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