硫酸根对有机废水厌氧生物处理的影响

利用连续流上流式厌氧污泥床在控制和不控制H_2S浓度两种情况下,考察SO_4~(2-)对有机物厌氧生物处理的影响。试验表明,硫酸根本身对厌氧处理没有毒害作用,它对厌氧处理过程的破坏主要是其还原产物H_2S造成的。在用Fe~(2+)控制H_2S的情况下,硫酸根的存在和浓度大小对出水TOC、TOC去除率、产气量、气化率无不利影响,但会使气体中甲烷含量及甲烷产率逐渐减小而二氧化碳含量及二氧化碳产率逐渐增大,     

常温厌氧污泥消化的停留时间分析

通过对25℃下城市污泥常温厌氧消化过程的产气率、pH值、挥发酸、有机物分解率、消化速度常数等的测定,引入“微生物污泥（ActiveBiologicalSolids）”概念,进行了常温厌氧消化过程的动力学分析。结果表明,常温消化的反应速度、产气率、有机物分解率均明显低于高、中温消化。为获得同一程度的产气率和有机物分解率,常温消化需150天以上的停留时间,而中、高温则为12～30天。常温污泥消化的基质浓度与消化速度关系不同于合成基质,呈S型,可采用Moser模型模拟其动力学过程;n＝2时所得各项动力学常数及最小消化时间可用于常温厌氧消化过程的控制。     

反硝化型甲烷厌氧氧化(DAMO)系统pH值耦合模型研究

对3个具有不同优势菌种反应器中厌氧氧化(DAMO)过程与pH值进行动力学耦合,结果表明,在25℃,Anammox-DAMO混培系统最大脱氮速率、硝酸盐初始抑制浓度和铵盐初始抑制浓度分别为3.95mg/(L·d),182.63,196.40mg/L;Nitrate-DAMO系统最大脱氮速率、硝酸盐初始抑制浓度分别为4.3...     

不同渗滤液循环方式对填埋层甲烷产生的影响

通过填埋模拟柱 ,实验室研究了以我国大城市生活垃圾组成为依据的新鲜垃圾填埋层在不同渗滤液循环方式条件下甲烷产生的规律 .渗滤液循环方式包括 :原液循环、好氧预处理 (SBR)后循环、与陈垃圾出水混合后循环 .结果表明 :新鲜垃圾填埋层初期渗滤液COD、VFA浓度高 ,原液循环导致有机酸的积累 ,抑制了甲烷化进程 ;初期渗滤液经预处理控制一定COD、VFA浓度后循环 ,能够显著地缩短产甲烷滞后时间、加速甲烷化进程 ;当填埋层进入稳定的甲烷化阶段后 ,渗滤液循环才能有效地降解渗滤液中的有机污染 ,近 10 0 %地转化为填埋气体.     

矿化垃圾床反应器厌氧甲烷氧化协同生物脱氮的研究

垃圾卫生填埋过程中逸散的甲烷与渗滤液处理过程中反硝化段不够彻底产生的硝酸盐对周围环境具有严重的威胁,反硝化厌氧甲烷氧化技术可实现甲烷与硝酸盐的同步去除,极具应用前景.本研究通过模拟垃圾填埋过程,以矿化垃圾作为垃圾填埋的覆土层与反硝化厌氧甲烷氧化微生物的接种源,建立了矿化垃圾床系统.结果表明,反应系统在140d的运行期间...     

Preparation and catalytic properties of ZrO2-Al2O3 composite oxide supported nickel catalysts for methane reforming with carbon dioxide

ZrO2-Al2O3 composite oxides and supported Ni catalysts were prepared, and characterized by N2 adsorption/desorption, X-ray diffraction (XRD) and X-ray photoelectron spectroscopy (XPS) techniques. The catalytic performance and carbon deposition was also investigated. This mesoporous composite oxide is shown to be a promising catalyst support. An increase in the catalytic activity and stability of methane and carbon dioxide reforming reaction was resulted from the zirconia addition, especially at 5wt% ZrO2 content. The Ni catalyst supported ZrO2-Al2O3 has a strong resistance to sintering and the carbon deposition in a relatively long-term reaction.     

硝酸盐对矿化垃圾中兼/厌氧甲烷氧化的影响

设计全因子实验研究了NO-3-N对填埋10~12 a的矿化垃圾中兼/厌氧甲烷氧化作用的影响.结果表明,兼/厌氧条件下,NO-3-N能促进矿化垃圾中CH4的去除.初始CH4和NO-3-N对CH4去除和N2产生有明显影响,且两者具有交互作用(P<0.05).CH4去除量随着初始CH4体积分数的增加而增加,添加一定含量的NO-3-N能促进CH4去除,同时通入一定体积分数CH4可以明显促进反硝化作用,说明矿化垃圾中NO-3-N还原能与兼/厌氧甲烷氧化耦合.本实验条件下,初始CH4体积分数为30%,NO-3-N含量为110 mg·kg-1时耦合效应较好.     

多元可燃性气体爆炸压力与中间产物发射光谱特性的耦合研究

工业生产中爆炸事故往往是由多元可燃气体与空气混合后遇到明火而引起的，为研究乙烷（C₂H₆）、乙烯（C₂H₄）、一氧化碳（CO）、氢气（H₂）对甲烷爆炸特性的影响，选取多组分可燃气体甲烷爆炸压力特性和自由基发射光谱的影响进行研究，利用陕西省工业过程安全与应急救援工程技术研究中心重点实验室搭建的多功能球形气体/粉尘爆炸实验装置和单色仪进行爆炸实验测试，同步采集时间—压力曲线、中间产物（OH，CH₂O）的发射光谱信号，考察多组分可燃气体浓度对甲烷爆炸压力特性和中间产物的影响。结果表明:在富氧状态下，多组分可燃气体加剧了甲烷—空气混合体系的爆炸剧烈程度，随着体系中氧气含量的减少、由富氧状态变为贫氧状态、促进作用逐渐减弱转变为阻尼作用，爆炸压力特性与中间产物发射光谱参数的影响规律基本保持一致，均呈高度正相关；多元混合体系爆炸剧烈程度越大，自由基发射光谱达到峰值的速度越快，自由基更早、更快的积累是加剧爆炸程度的原因之一。     

Uncertainty in Agricultural CH<Subscript>4</Subscript> AND N<Subscript>2</Subscript>O Emissions from Finland – Possibilities to Increase Accuracy in Emission Estimates

According to the United Nations Framework Convention on Climate Change (UNFCCC) and Kyoto Protocol under it, industrial countries have to estimate their greenhouse gas emissions annually, and assess the uncertainties in these estimates. In Finland, agricultural methane (CH₄) and nitrous oxide (N_2O) emissions represent 7% of anthropogenic greenhouse gas emissions, and globally the share is much higher. Agriculture is one of the most uncertain emission categories (representing over 20% of greenhouse gas inventory uncertainty in Finland), due to both high natural variability of the emission sources and poor knowledge of the emission-generating processes. In this paper, we present an uncertainty estimate of agricultural CH₄ and N₂O emissions from Finland in 2002. Uncertainties were estimated based on measurement data, literature and expert judgement, and total uncertainty in agriculture was calculated using Monte Carlo simulation. According to the calculations, agricultural CH₄ and N₂O emissions from Finland were 3.7 to 7.8 Tg carbon dioxide (CO₂) equivalents, 5.4 Tg being the mean value.Estimates of CH₄ emissions are more reliable than those of N₂O. N₂O from agricultural soils was the most uncertain emission category, and the uncertainty was not reduced by using available national measurement data of N₂O fluxes. Sensitivity study revealed that the uncertainty in total agricultural inventory could be 7% points lower, if more accurate emission estimation methods were used, including 1) improved data collection in area estimates of organic soils, 2) climate-specific methods for N₂O from agricultural soils as already presented in literature, and 3) more detailed CH₄ estimation methods for enteric fermentation which can be achieved by investigating national circumstances and digestible systems of animals in more detail.     

覆草旱作稻田CH4和N2O的排放

通过田间试验比较水稻覆草旱作常规施氮肥、覆草旱作推荐施氮肥和常规水作水稻全生育期内稻田土壤微量气体的排放.结果表明,旱作稻田N2O排放总量比水作稻田高1.5~3.7倍,在旱作覆草处理中常规施肥N2O排放较推荐施肥高2.4倍.水作稻田CH4排放总量比旱作稻田多5~6倍,而两旱作处理间差异不显著.水作稻田CH4的排放与水稻生育期关系密切,以分蘖盛期的2.2mg/(m2h)为最大;旱作稻田CH4的排放与施氮关系不明显.施氮是影响旱作稻田N2O排放的关键因素,每次施氮后,旱作稻田均会出现剧烈的排放高峰.水稻不同栽培方式的增温潜势的高低顺序为:覆草旱作常规施氮肥>常规水作>覆草旱作推荐施氮肥.