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Impacts of soil fumigation on greenhouse gas emission.

机译:土壤熏蒸对温室气体排放的影响。

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摘要

Agricultural soils are a major source and/or sink for atmospheric greenhouse gases: nitrous oxide (N2O), carbon dioxide (CO 2), and methane (CH4). The production and consumption of these gases are directly linked to microbial activities. Soil fumigation, a common practice in agriculture to control soil-borne diseases and pests, affects a variety of soil organisms, including microbes. It was initially hypothesized that if soil fumigants were biocides there would be strictly negative impacts. However, the findings of this research indicated that there were stimulation effects as well, particularly for N2O production following chloropicrin (CP) fumigation. This was the first study that systematically quantified impacts of soil fumigation with CP and methyl isothiocyanate (MITC) on greenhouse gas exchange.; For N2O, increases in surface emissions from 7- to 12-fold were observed following fumigation with CP. The stimulation was confirmed in both laboratory and field experiments. Microbial activities contributed 82% to the CP-induced N2O production, with 18% from abiotic processes. Inhibitor studies suggested that fungal mediated denitrification reactions under aerobic conditions were the primary mechanisms for CP-induced N 2O production. There were no significant differences in N2O production following CP fumigation under various levels of acetylene (0 Pa, 10 Pa, and 10 kPa), suggesting that traditional nitrification and denitification reactions did not significantly contribute to N2O production after CP fumigation. 15N labeled studies indicated that 12% of N from CP was incorporated into N2O. No enrichment in N2 was observed, indicating that N2O was a terminal mineralization product of CP. Field measurements also illustrated a 4-fold increase in N 2O emissions following MITC fumigation. This stimulation effect was not observed in laboratory incubations under aerobic conditions.; There were slight reductions in CO2 emissions following both MITC and CP fumigation. The initial decreases were followed by an increase in CO2 emissions observed at 48 days resulting from the mineralization of the killed biomass from fumigation.; All fumigants tested significantly reduced CH4 oxidation rates in historically nonfumigated soils. However, fumigation with MITC increased CH4 oxidation rates in all historically MITC fumigated soils compared to controls. CP universally decreased oxidation capacity regardless of fumigation history.
机译:农业土壤是大气温室气体的主要来源和/或汇聚处:一氧化二氮(N2O),二氧化碳(CO 2)和甲烷(CH4)。这些气体的产生和消耗与微生物活动直接相关。土壤熏蒸是农业上控制土壤传播的病虫害的一种普遍做法,它影响着包括微生物在内的各种土壤生物。最初的假设是,如果土壤熏蒸剂是杀生物剂,将产生严格的负面影响。但是,这项研究的结果表明也有刺激作用,尤其是对氯仿(CP)熏蒸后的N2O产生。这是第一项系统地量化使用CP和异硫氰酸甲酯(MITC)熏蒸土壤对温室气体交换的影响的研究。对于N2O,用CP熏蒸后观察到的表面排放量从7倍增加到12倍。在实验室和现场实验中都证实了这种刺激。微生物活动占CP诱导的N2O产量的82%,其中18%来自非生物过程。抑制剂研究表明,有氧条件下真菌介导的反硝化反应是CP诱导N 2O产生的主要机制。在不同水平的乙炔(0 Pa,10 Pa和10 kPa)下,CP熏蒸后N2O的产生没有显着差异,表明传统的硝化和反硝化反应对CP熏蒸后的N2O产生没有显着贡献。 15N标记的研究表明,CP中有12%的N被掺入N2O中。未观察到N2富集,表明N2O是CP的最终矿化产物。现场测量还表明,MITC熏蒸后N 2O排放增加了4倍。在有氧条件下的实验室培养中未观察到这种刺激作用。 MITC和CP熏蒸后,CO2排放量略有减少。最初的减少是由于熏蒸杀死的生物量矿化导致在48天观察到的CO2排放增加。在历史上未熏蒸过的土壤中,所有测试的熏蒸剂均显着降低了CH4的氧化速率。但是,与对照相比,用MITC熏蒸可提高所有历史上用MITC熏蒸过的土壤中CH4的氧化率。无论熏蒸史如何,CP普遍降低了氧化能力。

著录项

  • 作者

    Spokas, Kurt Arnold.;

  • 作者单位

    University of Minnesota.;

  • 授予单位 University of Minnesota.;
  • 学科 Agriculture Soil Science.
  • 学位 Ph.D.
  • 年度 2005
  • 页码 179 p.
  • 总页数 179
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 土壤学;
  • 关键词

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