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土地利用方式影响亚热带酸性土壤中 NO 的产生途径。

Land-use type affects NO production pathways in subtropical acidic soils.

机构信息

Institute of Soil and Fertilizer, Fujian Academy of Agricultural Sciences, Fuzhou, 350013, PR China; Sustainable Agricultural Sciences, Rothamsted Research, Devon, EX20 2SB, UK.

Institute of Soil and Fertilizer, Fujian Academy of Agricultural Sciences, Fuzhou, 350013, PR China.

出版信息

Environ Pollut. 2018 Jun;237:237-243. doi: 10.1016/j.envpol.2018.02.045. Epub 2018 Feb 24.

Abstract

The change in land-use from woodland to crop production leads to increased nitrous oxide (NO) emissions. An understanding of the main NO sources in soils under a particular land can be a useful tool in developing mitigation strategies. To better understand the effect of land-use on NO emissions, soils were collected from 5 different land-uses in southeast China: shrub land (SB), eucalyptus plantation (ET), sweet potato farmland (SP), citrus orchard (CO) and vegetable growing farmland (VE). A stable isotope experiment was conducted incubating soils from the different land use types at 60% water holding capacity (WHC), using NHNO and NHNO to determine the dominant NO production pathway for the different land-uses. The average NO emission rates for VE, CO and SP were 5.30, 4.23 and 3.36 μg N kg dry soil d, greater than for SB and ET at 0.98 and 1.10 μg N kg dry soil d, respectively. NO production was dominated by heterotrophic nitrification for SB and ET, accounting for 51 and 50% of NO emissions, respectively. However, heterotrophic nitrification was negligible (<8%) in SP, CO and VE, where autotrophic nitrification was a primary driver of NO production, accounting for 44, 45 and 66% for SP, CO and VE, respectively. Denitrification was also an important pathway of NO production across all land-uses, accounting for 35, 35, 49, 52 and 32% for SB, ET, SP, CO and VE respectively. Average NO emission rates via autotrophic nitrification, denitrification and heterotrophic nitrification increased significantly with gross nitrification rates, NO contents and C:N ratios respectively, indicating that these were important factors in the NO production pathways for these soils. These results contribute to our understanding and ability to predict NO emissions from different land-uses in subtropical acidic soils and in developing potential mitigation strategies.

摘要

土地利用从林地转变为作物种植会导致一氧化二氮(NO)排放量增加。了解特定土地下土壤中主要的 NO 来源可以成为制定减排策略的有用工具。为了更好地了解土地利用对 NO 排放的影响,从中国东南部的 5 种不同土地利用类型中采集了土壤:灌丛地(SB)、桉树种植园(ET)、红薯农田(SP)、柑橘果园(CO)和蔬菜种植农田(VE)。进行了一项稳定同位素实验,在 60%的水分保持能力(WHC)下,用 NHNO 和 NHNO 来确定不同土地利用类型的主要 NO 产生途径,对不同土地利用类型的土壤进行孵育。VE、CO 和 SP 的平均 NO 排放率分别为 5.30、4.23 和 3.36μgNkg干土d,大于 SB 和 ET 的 0.98 和 1.10μgNkg干土d。NO 的产生主要由异养硝化作用主导,分别占 SB 和 ET 中 NO 排放的 51%和 50%。然而,异养硝化作用在 SP、CO 和 VE 中可以忽略不计(<8%),在这些地方,自养硝化作用是 NO 产生的主要驱动力,分别占 SP、CO 和 VE 中 NO 产生的 44%、45%和 66%。反硝化作用也是所有土地利用类型中 NO 产生的重要途径,分别占 SB、ET、SP、CO 和 VE 的 35%、35%、49%、52%和 32%。通过自养硝化、反硝化和异养硝化产生的平均 NO 排放率与总硝化率、NO 含量和 C:N 比分别显著增加,表明这些是这些土壤中 NO 产生途径的重要因素。这些结果有助于我们了解和预测亚热带酸性土壤中不同土地利用类型的 NO 排放,并制定潜在的减排策略。

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