首页> 外文期刊>Journal of plant nutrition and soil science >Vertical distribution of soluble organic nitrogen, nitrogen mineralization, nitrification, and amidohydrolase activities in a manure-treated soil
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Vertical distribution of soluble organic nitrogen, nitrogen mineralization, nitrification, and amidohydrolase activities in a manure-treated soil

机译:肥料处理后土壤中可溶性有机氮的垂直分布,氮矿化,硝化和酰胺水解酶的活性

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Recent studies indicate that soil soluble organic nitrogen (SON) plays an important regulatory role in the soil-plant N cycle. The aims of this study were to identify the vertical distribution of SON and its correlation with N mineralization, nitrification, and amidohydrolase activities, in a soil repeatedly amended with cow manure or chemical fertilizer. For this purpose, soil samples were collected from 0-20, 20-40, 40-60, 60-80, and 80-100cm depths of a calcareous soil, which has been annually amended for 5 y with cow manure (CM) at two rates of 50 (CM _(50)) and 100 (CM _(100)) Mg CM ha ~(-1) y ~(-1). Treatments with chemical fertilizer (CF) and a control (CT) were also included. Soluble organic N, N mineralization, nitrification rates, as well as L-glutaminase and L-asparaginase activities were determined. Both CM _(50) and CM _(100) enhanced SON content throughout the soil profile. Nitrogen-mineralization rate (N _m) was increased at the 0-20cm depth of the CM _(100) treatment and remained unaffected at the deeper depths. Nitrification rate (N _n) was significantly higher at the 0-60cm depth of CM _(100) compared to CF and CT. L-glutaminase and L-asparaginase activities were significantly increased at the 0-40cm depth in both CM _(50) and CM _(100) compared to CF and CT. The amidohydrolase activities could not be detected below 40cm, regardless of the fertilizer treatments. Our results suggest that SON makes a minor contribution to N mineralization in deep soil layers. It was also concluded that changes in the SON throughout the soil profile were not associated with changes in the N-transformation rates (N _m and N _n) and amidohydrolase activities. While we conclude that SON is a major N pool in the whole profile of the manure applied soil further investigation is required to characterize SON and to investigate the bioavailability of SON for microbial activity in different soil depths.
机译:最近的研究表明,土壤可溶性有机氮(SON)在土壤-植物N循环中起着重要的调节作用。这项研究的目的是确定在反复用牛粪肥或化肥改良的土壤中,SON的垂直分布及其与氮矿化,硝化和酰胺水解酶活性的关系。为此,从0-20、20-40、40-60、60-80和80-100cm深度的钙质土壤中收集土壤样品,该土壤每年用牛粪肥(CM)进行5年的修正两种比率分别为50(CM _(50))和100(CM _(100))Mg CM ha〜(-1)y〜(-1)。还包括使用化肥(CF)和对照(CT)的治疗。测定了可溶性有机氮,氮矿化,硝化速率以及L-谷氨酰胺酶和L-天冬酰胺酶的活性。 CM _(50)和CM _(100)在整个土壤剖面中均提高了SON含量。在CM _(100)处理的0-20cm深度处,氮矿化率(N _m)增加,而在更深的深度不受影响。与CF和CT相比,在CM _(100)的0-60cm深度处的硝化率(N _n)明显更高。与CF和CT相比,CM _(50)和CM _(100)的0-40cm深度的L-谷氨酰胺酶和L-天冬酰胺酶活性显着增加。无论使用何种肥料,在40cm以下都无法检测到酰胺水解酶的活性。我们的结果表明,SON对深层土壤中的氮矿化贡献很小。还得出结论,整个土壤剖面中SON的变化与N转化率(N _m和N _n)和酰胺水解酶活性的变化无关。虽然我们得出结论,SON是施肥土壤整个剖面中的主要氮库,但仍需要进一步研究以表征SON并调查SON在不同土壤深度下对微生物活性的生物利用度。

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