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Nitrogen mineralization of manure-amended soil: Effects of salinity and moisture content

机译:肥料改良土壤的氮矿化:盐分和水分含量的影响

摘要

Application of manure has been used to increase the nitrogen status of many arid and semi-arid agricultural soils, however, organic nitrogen contained in animal manures must be mineralized prior to utilization by crops. Nitrogen mineralization is, like other biological processes, affected by soil water status. This can be due to the direct influence of soil moisture and/or salt interactions on the nitrogen dynamics. It is critical to understand the interactive effects of salt and water on nitrogen in soils amended with organic fertilizer. Such knowledge may be used for improving and quantifying nitrogen use efficiency. Objectives of this study were (i) to examine the relative and interactive influences of soil osmotic and matric water potentials on nitrogen transformations in manure-amended and non-manured soils, (ii) to determine the extent of nitrogen mineralization over a range of soil water potentials, and (iii) to study the effect of manure addition on nitrogen dynamics in an agricultural desert soil. Gila fine sandy loam soil was treated by addition of varying amounts of distilled water, NaCl, and dairy manure and incubated at depth of 20 cm in 0.025 mm thickness Ziploc® bags. Ammonium nitrogen, nitrate nitrogen, gravimetric soil moisture content, and total soil water potential were measured weekly for 16 weeks. Our study showed a decrease in the amount of inorganic N released from both the non-manured and manure-amended soils at total soil water potentials of approximately -55 bars or less. Maximal amounts of inorganic-N were released at potentials of -23 to -3.5 bars. There was an accumulation in the amounts of NH₄-N released at potentials of -55 bars or less, presumably because of a reduction in net nitrification. The manure caused nitrogen immobilization especially during the early part of our study. Immobilization also occurred in non-manured soil, but this generally lasted only a few weeks. Immobilization was prolonged in soils with lower water potentials. Net N mineralization in the manure-amended soils was higher than in the non-manured soils when soil moisture content was at field capacity.
机译:施用肥料已用于提高许多干旱和半干旱农业土壤的氮素状况,但是,动物肥料中所含的有机氮必须先矿化,然后才能被农作物利用。与其他生物过程一样,氮矿化也受到土壤水分状况的影响。这可能是由于土壤水分和/或盐分相互作用对氮动力学的直接影响。了解盐和水对有机肥改良土壤中氮的交互作用至关重要。这样的知识可以用于改善和量化氮的使用效率。这项研究的目的是(i)研究土壤渗透和基质水势对肥料改良和非肥料土壤中氮转化的相对和相互作用的影响;(ii)确定一定范围土壤中氮矿化的程度(iii)研究添加肥料对农业沙漠土壤中氮动态的影响。通过添加不同量的蒸馏水,NaCl和乳牛粪处理吉拉细砂壤土,并在20厘米深度的0.025毫米厚的Ziploc®袋中孵育。连续16周每周测量一次铵态氮,硝态氮,重量土壤水分含量和总土壤水势。我们的研究表明,在总土壤水势约为-55 bar或更低的情况下,从非肥料和肥料改良土壤中释放的无机氮量均减少。在-23至-3.5 bar的电势下释放出最大量的无机N。在-55 bar或更低的电位下,NH 3-N的释放量不断增加,这可能是由于净硝化作用的降低。粪肥特别是在我们的研究初期引起了氮的固定。固定化也发生在未处理的土壤中,但这通常只持续了几周。在水势较低的土壤中固定化时间延长。当土壤含水量处于田间持水量时,肥料改良土壤的净氮矿化度高于非肥料土壤。

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    Al-Ismaily Said Salim;

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  • 年度 2004
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