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首页> 外文期刊>Soil & Tillage Research >Seasonal and inter-annual variation of leaching of dissolved organic carbon and nitrogen under long-term manure application in an acidic clay soil in subtropical China
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Seasonal and inter-annual variation of leaching of dissolved organic carbon and nitrogen under long-term manure application in an acidic clay soil in subtropical China

机译:亚热带酸性黏土长期施肥对有机碳和氮溶失的季节变化和年际变化

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摘要

Dissolved organic matter (DOM) plays an important role in soil biological activity and transport of pollutants and nutrients in soils, but very little information is available with regard to the long-term impact of agricultural management practices on the dynamics and fate of DOM in acidic soils. The seasonal and inter-annual variation of dissolved organic carbon (DOC) and nitrogen (DON) contents and leaching were investigated in an acidic clay soil (Ferric Acrisol) by a long-term field lysimeter experiment in subtropical China. The experiment was conducted from 2002 to 2010 with 4 fertilization treatments under maize monoculture: no manure (CK), low-rate manure with 150 kg N ha(-1) y(-1) (LM), high-rate manure with 600 kg N ha(-1) y(-1) (HM), and high-rate manure with 600 kg N ha(-1) y(-1) and lime at 3000 kg Ca(OH)(2) ha(-1)3 y(-1) (HML). Manure application resulted in a seasonal variation of soil DOC and DON, and significant effects were observed by manure DOC, microbial biomass and soil water content. Soil DOC, which was mainly determined by soil organic matter and soil water content, increased yearly until the seventh year when it was stabilized. Manure application on acidic clay soil did not alter DOC leaching, whereas DON leaching clearly increased after three years of high manure application of 600 kg N ha(-1) y(-1). The average annual DON leaching losses under long-term manure application had a range of 3.8-5.4 kg ha(-1), accounting for 6-11% of total nitrogen leached. The addition of lime, combined with manure application, produced no impact on soil dynamics and leaching of DOC and DON, with the exception of increasing emission of CO2. (C) 2014 Elsevier B.V. All rights reserved.
机译:溶解性有机物(DOM)在土壤生物活性以及污染物和养分在土壤中的运输中起着重要作用,但是关于农业管理实践对酸性环境中DOM的动态和结局的长期影响的信息很少土壤。在亚热带地区,通过长期的溶渗仪试验,研究了酸性黏土(Ferric Acrisol)中溶解性有机碳(DOC)和氮(DON)含量的季节性和年际变化以及淋溶。该实验于2002年至2010年进行,玉米单培养下有4种施肥处理:无肥(CK),150 kg N ha(-1)y(-1)(LM)低速肥料,600高氮肥kg N ha(-1)y(-1)(HM),以及以3000 kg Ca(OH)(2)ha(-)施用600 kg N ha(-1)y(-1)和石灰的高速率肥料1)3 y(-1)(HML)。施肥导致土壤DOC和DON的季节变化,并且粪肥DOC,微生物生物量和土壤含水量观察到显着影响。土壤DOC主要由土壤有机质和土壤水分决定,逐年增加直至稳定的第七年。在酸性粘土土壤上施用肥料不会改变DOC的淋溶,而在600 kg N ha(-1)y(-1)施用了三年的高肥料后,DON淋溶明显增加。长期施用粪肥后,DON的年平均浸出损失范围为3.8-5.4 kg ha(-1),占浸出总氮的6-11%。除了增加二氧化碳的排放外,添加石灰和施肥对土壤动力学和DOC和DON的浸出均无影响。 (C)2014 Elsevier B.V.保留所有权利。

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