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土壤pH对硝酸根还原过程中N_2O产生的影响 被引量:24

EFFECT OF SOIL pH ON N_2O PRODUCTION IN NITRATE REDUCTION
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摘要 采用氢氧化钠和盐酸将中性和碱性土壤分别分步调节成具有不同pH的系列土壤 ,加入等量硝态氮后 ,在添加易有效碳源葡萄糖和不添加葡萄糖的厌气条件下进行培养 ,测定不同处理条件下的N2 O和N2 产生速率。结果表明 ,不加碳源培养 2 4h后 ,原中性土壤系列中N2 O的最大产生速率位于pH 5 2 5左右 ,碱性土壤系列的该值位于 5 90左右 ;加入葡萄糖后 ,中性土壤系列中最大N2 O产生速率的pH值不变 ,但产生N2 最大速率的pH已提高至 6 50。而碱性土壤系列中N2 O产生最大速率时的pH值已移至 6 90处 ,即碳源的加入对产生N2 O所需的最佳pH有所提高。试验还显示 ,酸性条件可提高总还原气体中N2 O所占的比例 ,但就N2 O产生速率的绝对值来说 。 By adding NaOH or HCl, one neutral soil and one w eakly alkaline soil was respectively adjusted to a series of samples with differ ent pH After addition of NO 3 - the soil samples were anaerobically incubate d with or without glucose for 24 h After that N 2O production rate was measur ed The results show that without glucose the optimum pH for the greatest N 2O production rate is about 5 25 for the neutral soil series, and 5 90 for the weakly alkaline soil series With glucose, however, the optimum pH for N 2O production is different, at about 6 50 and 6 90 for the neutral soil series a nd the weakly alkaline soil series, respectively, demonstrating that the addit ion of easily available carbon source has raised the optimum pH for N 2O produc tion The experiment results also show that acidic condition could increase the ratio of N 2O to total reduced gas, as for the absolute value of N 2O produc tion, however, the neutral condition is still more favorable
出处 《土壤学报》 CAS CSCD 北大核心 2004年第1期81-86,共6页 Acta Pedologica Sinica
基金 联邦德国教研部 (BMBF)项目 (CHN 0 0 /0 89)资助
关键词 土壤 PH值 硝酸根 还原过程 N2O 氧化亚氮 Nitrous oxide Soil pH Denitrification Soil
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  • 1[1]IPCC. Climate change 1992. The supplement reports to the IPPC scientific assessment. In:Houghon J T, Callander B A , Vaniey SK. eds. Greenhouse Sources and Sinks. Cambridge: Cambridge Uni. Press, 1992. 24~25
  • 2[2]Crutzen P J. Atmospheric chemical processes of the oxides of nitrogen, including nitrous oxide. In: Delwiche C C. ed. Denitrification, Nitrification and Atmospheric N2O. Chichester: John Wiley & Sons Ltd,1981. 17~44
  • 3[3]Mosier A R. Nitrous oxide emissions from agricultural soils. Fertil. Res., 1994,37:191~200
  • 4[4]Bouwman A F. Exchange of greenhouse gases between terrestrial ecosystems and the atmosphere. In: Bouwman A G.ed. Soils and the Greenhouse Effect. Chichester: John Wiley & Sons Ltd,1990.61~128
  • 5[5]Smith K A, Thomson P E, Clayton H, et al. Effects of temperature, water content and nitrogen fertilization on emissions of nitrous oxide by soils. Atoms Environ., 1998, 32: 3 301~3 309
  • 6[6]Weier K L, Gilliam W. Effect of acidity on denitrification and nitrous oxide evolution from Atlantic Coastal Plain soils. Soil Sci. Soc. Am. J., 1986, 50:1 202~1 205
  • 7[7]Stevens A F, Laughlin R J, Malone J P. Soil pH affects the processes reducing nitrate to nitrous oxide and di-nitrogen. Soil Biol. Biochem., l998, 30:1 119~1 126
  • 8[8]Wijler J, Delwiche C C. Investigations on the denitrifying process in soil. Plant and Soil,1954,5:155~169
  • 9[9]Feng K. Dynamik von Zwischenschicht-NH4+ in ueberfluteten Chinesischen Reisboeden. Germany: Shaker Press, 1996. 61~70
  • 10[10]Bremner J M , Shaw K. Denitrification in soil. II. Factors affecting denitrification. J. Agric. Sci., 1958, 51:40~52

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