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首页> 外文期刊>Soil & Tillage Research >Nitrogen fertilization and tillage reversal affected water-extractable organic carbon and nitrogen differentially in a Black Chernozem and a Luvisol Gray Luvisol
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Nitrogen fertilization and tillage reversal affected water-extractable organic carbon and nitrogen differentially in a Black Chernozem and a Luvisol Gray Luvisol

机译:氮肥和耕作逆转对黑切诺西姆和卢维索尔灰色卢维索尔中水可提取的有机碳和氮的影响不同。

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摘要

Reversing land management from no tillage to conventional tillage (tillage reversal) to deal with weed infestation and accumulation of crop residue in long-term no tillage systems may dramatically alter soil carbon (C) dynamics. We studied the impact of nitrogen (N) fertilization and tillage reversal on the quantity and quality of water-extractable organic C (WEOC) and N (WEON) in the 0-10 cm soil layer in two contrasting soil types located at Ellerslie (high organic matter content) and Breton (low organic matter content) in central Alberta, Canada. We used a split-plot design with N assigned to the main plot and tillage to the subplot. Each treatment had two levels which included addition of 0 (NO) vs. 100 kg N ha(-1) yr(-1) (N100) N fertilizer and long-term no tillage (NT) vs. tillage reversal (TR); straw was retained on site in all treatments as part of the management regime. Our results showed that soil organic C and N storage were not affected by long-term N fertilization or tillage reversal at Ellerslie but were increased at Breton. Soil VVEOC was significantly higher under N100 than under NO at both sites. Soil WEOC was TR NT at Breton but was not affected by tillage at Ellerslie. Soil WEON was influenced by the interaction effects of N fertilization and tillage reversal at both sites. The highest WEON concentration was in the N100-TR treatment combination (17.8 +/- 1.5 and 10.5 +/- 0.7 mu gg(-1) at Ellerslie and Breton, respectively). Nitrogen fertilization decreased the aromaticity of WEOC at both sites but had different effects on WEOC condensation between Ellerslie and Breton. Nitrogen fertilization increased nonaromatic compounds in WEOC and the stability of WEOC at Breton but not at Ellerslie. Neither tillage nor tillage x fertilizer interaction affected the quality of WEOC in either soil. Therefore, N fertilization was the main factor controlling the quality and quantity of WEOC in the studied soils. (C) 2014 Elsevier B.V. All rights reserved.
机译:将土地管理从免耕转向传统耕作(翻耕),以应对长期无耕种系统中杂草的侵染和农作物残渣的积累,可能会大大改变土壤碳(C)的动态。我们研究了位于Ellerslie的两种对比土壤类型(高)中0-10 cm土层中氮(N)的施肥和耕作逆向对水可萃取有机碳(WEOC)和N(WEON)的数量和质量的影响有机物含量)和加拿大亚伯达省中部的不列塔尼(低有机物含量)。我们使用分割图设计,将N分配给主图,将耕作分配给子图。每种处理都有两个水平,包括添加0(NO)与100 kg N ha(-1)yr(-1)(N100)N肥料以及长期不耕作(NT)vs.耕作反转(TR);作为管理制度的一部分,所有处理中均将稻草保留在现场。我们的结果表明,土壤的有机碳和氮存储量不受Ellerslie的长期氮肥或耕作逆转的影响,但在不列塔尼州有所增加。在两个地点,N100下的土壤VEVEC均显着高于NO下。布列塔尼的土壤WEOC为TR

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