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The Changes of P-fractions and Solubility of Phosphate Rock in Ultisol Treated by Organic Matter and Phosphate Rock

机译:有机物和磷矿石处理的Ultisol磷矿石中P馏分和溶解度的变化

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摘要

Phosphorus (P) is one of the essential elements for plant, however, its availability is mostly very low in acid soils. It is well documented that application of phosphate rock and organic matter are able to change the level of availability of P-form in acid soils.  The objective of the research were to evaluate the changes of P-fractions ( resin-P, NaHCO3-Pi, and NaHCO3-Po) and phosphate rock dissolution which were induced by application of organic matter (Imperata cylindrica, Pueraria javanica, dan Colopogonium mucunoides) and phosphate rock in Utisol Lampung.  The experiment was designed in a completely randomized design with three factors and three replications.  The first factor was the types of organic matter (I. cylindrica, P. javanica, and C. mucunoides), the second factor was the rate of organic matter (0, 2.5, and 5%), and the third factor was the rate of phosphate rock (0, 40, and 80 mg P kg-1).  The results showed that in the  rate of 0 and 1% organic matter, the type of organic matter did not affect P-fraction of NaHCO3-Pi, but in the rate of 2.5 and 5%,  NaHCO3-Pi due to application of  P. javanica, and C. mucunoides higher than due to application of  I. cylindrica.  However, the increasing rate of organic matter increased NaHCO3-Pi. Then, P-fraction of Resin-Pi was affected by the type of organic matter, the rate of  organic matter, and the rate of phosphate rock, respectively. P-fraction of resin-Pi due to application of P.  javanica, and C. mucunoides was higher than due to application of  I. cylindrica, but the effect of  P. javanica, and C. mucunoides was not different.  Increasing the rate of organic matter and phosphate rock increased P-fraction of resin-Pi and NaHCO3-Pi, but P-fraction of NaHCO3-Po was not affected by all treatments.  Meanwhile, dissolution of phosphate rock was affected by the kind of organic matter and soil reaction.  In the rate of 5% organic matter, dissolution of  phosphate rock by application of                                     I. cylindrica (70%) was higher than P. javanica (26.6%), and C.  mucunoides (33.5%), but in the rate of 1%, the effect of I. cylindrica , P. javanica, and C. mucunoides were not different.Keywords: C. mucunoides; I. cylindrica; P. javanica; phosphate rock; P-fractions[How to Cite: Djuniwati S, B Nugroho, and HB Pulunggono. 2012. The Changes of P-fractions and Solubility of Phosphate Rock in Ultisol Treated by Organic Matter and Phosphate Rock. J Trop Soils, 17: 203-210. doi: 10.5400/jts.2012.17.3.203][Permalink/DOI: www.dx.doi.org/10.5400/jts.2012.17.3.203]
机译:磷(P)是植物必需的元素之一,但是,在酸性土壤中磷的利用率通常非常低。大量文献证明,磷矿石和有机物的使用能够改变酸性土壤中P形态的有效性。该研究的目的是评估有机物(菊苣,葛根,丹皮草)的有机物引起的P组分(树脂-P,NaHCO3-Pi和NaHCO3-Po)的变化和磷酸盐岩的溶解。 )和Utisol Lampung中的磷酸盐岩。实验是在具有三个因素和三个重复的完全随机设计中进行的。第一个因素是有机物质的类型(I. cylindrica,P。javanica和C. mucunoides),第二个因素是有机物质的比率(0、2.5和5%),第三个因素是比率磷酸盐岩(0、40和80 mg P kg-1)。结果表明,在有机物含量为0和1%的情况下,有机物的类型不影响NaHCO3-Pi的P分数,但在2.5和5%的情况下,由于施用P而导致的NaHCO3-Pi的比率。 javanica和C. mucunoides高于应用I.cylindrica。但是,有机物的增加速率增加了NaHCO3-Pi。然后,树脂-Pi的P分数分别受有机物类型,有机物速率和磷矿石速率的影响。由于施用爪哇假单胞菌和粘液梭状芽胞杆菌而导致的树脂-Pi的P分数高于由于施用cylindrica造成的树脂-Pi的P分数,但爪哇假单胞菌和粘液梭状芽孢杆菌的作用没有差异。增加有机物和磷矿的比率会增加树脂-Pi和NaHCO3-Pi的P分数,但NaHCO3-Po的P分数并不受所有处理的影响。同时,磷矿的溶解受有机质的种类和土壤反应的影响。以5%的有机物比率计算,通过施用cylindrica(70%)高于I.cynicdrica(26.6%)和C.mucunoides(33.5%)溶解了磷酸盐岩,但比例为1。 ,I。cylindrica,P。javanica和C. mucunoides的作用没有差异。圆柱体P. javanica;磷矿P分数[如何引用:Djuniwati S,B Nugroho和HB Pulunggono。 2012。有机质和磷矿石处理的Ultisol磷矿石中P组分和溶解度的变化。 J Trop Soils,17:203-210。 doi:10.5400 / jts.2012.17.3.203] [Permalink / DOI:www.dx.doi.org/10.5400/jts.2012.17.3.203]

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