首页> 外文期刊>Journal of the Indian Society of Soil Science >Effect of Rice Husk Ash and Bagasse Ash on Inorganic Phosphorus Fractions and Available Phosphorus in an Alkaline Soil under Rice (Oryza sativa L.)-Wheat (Triticum aestivum L.) Cropping System
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Effect of Rice Husk Ash and Bagasse Ash on Inorganic Phosphorus Fractions and Available Phosphorus in an Alkaline Soil under Rice (Oryza sativa L.)-Wheat (Triticum aestivum L.) Cropping System

机译:稻麦-小麦种植系统下稻壳灰和甘蔗渣灰对碱性土壤无机磷组分和有效磷的影响

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The cost of production of phosphatic fertilizers has increased tremendously with the rise in prices of raw materials and energy. It has been suggested that organic wastes can help to bridge the gap between demand and supply of chemical fertilizers toa great extent by supplying plant nutrients. Agro-industrial wastes like rice husk ash (RHA) and bagasse ash (BA) are available in sufficient quantities and their disposal is posing a great threat to environment causing damage to the land and the surrounding area where these are dumped. It is estimated that 45 million tonnes (Mt) of bagasse is produced annually by the sugar factories in India (NAAS 2008). The corresponding value of rice husk, which is produced as a by-product of rice mills is about 25 Mt. The BA and RHA constitute about 4.6 and 25% of the total production of bagasse and rice husk, respectively. The reaction products formed in a soil could be entirely different with chemical fertilizers than with organic ashes like RHA and BA, because of their influence on chemical reactions in soil. Fractionation of P_i, such as Ca-P, Fe- and Al-P (non-occluded Fe- and Al-bound P) can provide an effective approach for investigating soil P_i; availability and P_i inter-conversion among soil P_i fractions from different P pools (Hedley et al. 1982; Solis and Torrent 1989; Shen et al. 2004). Since there is limited information about the effect of regular applications of RHA and BA on different P fractions in soils, 3-year field study was undertaken to assess the effects of application of P through RHA and BA on the transformations of P into different inorganic (P_i) fractions and Olsen P in an alkaline soil in a rice-wheat cropping system (2006-2009). The soil of the experimental field was a Typic Ustochrept, loamy sand (5% clay and 74% sand) with pH 7.2, cation exchange capacity of 8.54 cmol(p~+)kg~(-1), EC 0.26 dS m~(-1), 3.71 g kg~(-1) organic C, 3.0 mg kg~(-1) of 0.5 M NaHCO_3-extractable P, and 55 mg kg~(-1) of 1 M NH40Ac-extractable K.
机译:随着原材料和能源价格的上涨,磷肥的生产成本已大大增加。已经提出,有机废物可以通过供应植物养分来最大程度地帮助弥合化肥需求与供应之间的差距。稻壳灰(RHA)和甘蔗渣灰(BA)等农业工业废物数量充足,其处置对环境构成了巨大威胁,对这些废物倾倒的土地和周围地区造成了损害。据估计,印度食糖厂每年生产4500万吨蔗渣(NAAS 2008)。作为碾米厂的副产品生产的稻壳的相应价值约为25Mt。 BA和RHA分别占甘蔗渣和稻壳总产量的4.6%和25%。在土壤中形成的反应产物与有机灰烬(如RHA和BA)相比,在化学肥料中可能完全不同,因为它们对土壤中的化学反应有影响。 P_i的分级,例如Ca-P,Fe-和Al-P(未吸附的Fe-和Al-结合的P)可以为研究土壤P_i提供有效的方法。不同磷库中土壤P_i组分之间的有效性和P_i相互转化(Hedley等,1982; Solis和Torrent 1989; Shen等,2004)。由于关于常规施用RHA和BA对土壤中不同P含量的影响的信息有限,因此进行了3年的田间研究,以评估通过RHA和BA施用P对将P转化为不同无机盐的影响( P_i)馏分和水稻-小麦种植系统中碱性土壤中的Olsen P(2006-2009年)。实验场的土壤是典型的Ustochrept型土壤,pH值为7.2的壤土砂(5%粘土和74%砂),阳离子交换容量为8.54 cmol(p〜+)kg〜(-1),EC 0.26 dS m〜( -1),3.71 g kg〜(-1)有机C,3.0 mg kg〜(-1)的0.5 M NaHCO_3可萃取的P和55 mg kg〜(-1)的1 M NH40Ac可萃取的K.

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