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垃圾填埋场渗滤液灌溉及覆土土质对填埋场氧化亚氮释放的影响
引用本文:何品晶,陈淼,张后虎,邵立明.垃圾填埋场渗滤液灌溉及覆土土质对填埋场氧化亚氮释放的影响[J].应用生态学报,2008,19(7):1591-1596.
作者姓名:何品晶  陈淼  张后虎  邵立明
作者单位:污染控制与资源化研究国家重点实验室,长江水环境教育部重点实验室,同济大学环境科学与工程学院,上海,200092
基金项目:国家科技支撑计划 , 国家自然科学基金 , 国家高技术研究发展计划(863计划)
摘    要:采用静态箱法,现场监测黏土和砂土覆盖层生活垃圾填埋场N2O释放通量的春夏季节及昼夜变化,研究渗滤液灌溉、覆土土质对填埋场N2O释放的影响.结果表明:砂土和黏土覆盖层填埋场N2O夏季的释放通量均值分别为(242±576)和(591±767) μg N2ON·m-2·h-1,是春季[分别为(74.4±314)和(269±335) μg N2ON·m-2·h-1]的3.2(P>0.05)和2.2倍(P<0.05).渗滤液灌溉促进了砂土填埋场覆土N2O的释放,填埋场中灌溉区N2O的释放通量为无灌溉区的2倍(P>0.05).渗滤液灌溉的砂土覆盖层填埋场N2O春夏两季释放通量均值[(211±460) μg N2ON·m-2·h-1]仅为无渗滤液灌溉的黏土覆盖层填埋场[(430±605) μg N2ON·m-2·h-1]的1/2(P>0.05).无论渗滤液灌溉与否,选择贫瘠的砂性覆盖土均有助于减少生活垃圾填埋场N2O释放.

关 键 词:生活垃圾填埋场  N2O释放通量  渗滤液灌溉  覆土土质  垃圾填埋场渗滤液  灌溉区  覆土  土质  氧化亚氮释放  影响  municipal  solid  waste  landfill  emission  soil  type  cover  irrigation  leachate  覆盖土  砂性  选择  春季  均值  结果  研究  变化
收稿时间:2007-11-13

Effects of leachate irrigation and cover soil type on N2O emission from municipal solid waste landfill.
HE Pin-jing,CHEN Miao,ZHANG Hou-hu,SHAO Li-ming.Effects of leachate irrigation and cover soil type on N2O emission from municipal solid waste landfill.[J].Chinese Journal of Applied Ecology,2008,19(7):1591-1596.
Authors:HE Pin-jing  CHEN Miao  ZHANG Hou-hu  SHAO Li-ming
Institution:State Key Laboratory of Pollution Control and Resources Reuse, College of Environmental Science and Engineering, Tongji University, Shanghai 200092, China.
Abstract:By the method of static chamber, the seasonal and diurnal variations of N2O fluxes in two full-scale municipal solid waste (MSW) landfills covered with sandy and clay soils were measured to study the effects of leachate irrigation and cover soil type on the landfill N2O emission. The results showed that the N2O flux in the MSW landfill covered with sandy soil was (242 +/- 576) microg N2O-N x m(-2) x h(-1) in summer, being 3.2 times (P > 0.05) as high as that in spring (74.4 +/- 314) microg N2O-N x m(-2) x h(-1), while the N2O flux in the MSW landfill covered with clay soil was (591 +/- 767) microg N2O-N x m(-2) x h(-1) in summer, being 2.2 times (P < 0.05) as high as that in spring (269 +/- 335) microg N2O-N x m(-2) x h(-1)]. Leachate irrigation promoted the N2O emission from the soil cover of the landfill covered with sandy soil, and the N2O flux in the landfill was 1 time higher than that of the control (P > 0.05). Under leachate irrigation, the average N2O flux in spring and summer in the landfill covered with sand soil was (211 +/- 460) microg N2O-N x m(-2) x h(-1), being only 1/2 of that (430 +/- 605) microg N2O-N x m(-2) x h(-1)] in the landfill covered with clay soil without leachate irrigation (P > 0.05 ). Therefore, no matter leachate irrigation was conducted or not, the N2O emission from MSW landfill could be minimized by covering with infertile sandy soil.
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