磁性氧化铁/桑树杆生物炭的制备及其对砷污染土壤溶解性有机碳和砷形态的影响

以桑树杆为原料,制备了原始桑树杆生物炭（M-BC）及磁性氧化铁/桑树杆生物炭（Fe-BC）并对其进行表征.通过土壤培养实验,研究了3个温度下炭化制备的Fe-BC和M-BC在不同培养时间对土壤浸出液溶解性有机碳（DOC）和土壤砷（As）形态等的影响.结果表明：①Fe-BC负载的铁氧化物主要为Fe₃ O₄,且有磁性,主要官能团有C＝O双键、O—H键、C—O键和Fe—O键;Fe-BC-400、Fe-BC-500和Fe-BC-600的pH_zpc分别为8.92、8.74和9.19,比表面积分别为447.412、482.697和525.708 m² ·g^-1.②土壤浸出液中ρ（DOC）随着M-BC和Fe-BC炭化温度的升高而分别降低11.6~315.6 mg ·L^-1和78~365.6 mg ·L^-1,土壤浸出液中DOC浓度与土壤电导率（EC）值呈负相关;在培养第35 d,添加Fe-BC-600的土壤浸出液中As浓度比对照组土壤浸出液中的降低了55.96%.土壤浸出液中As浓度与DOC浓度相关性不显著.③添加Fe-BC的土壤有效态As占比均低于对照组的,在培养第35 d时,Fe-BC-600可使土壤有效态As占比降低39.21%.④在培养第35 d时,添加M-BC的土壤残渣态As含量减少了17.76%~49.11%,添加Fe-BC-600的土壤残渣态As占比增加了80%.Fe-BC-600最有利于降低土壤溶液DOC浓度,提高残渣态As含量,从而降低土壤As生物有效性.研究可为磁性氧化铁/生物炭在砷污染土壤修复提供理论依据.     

氮氧化物防治技术在台湾之应用及管制策略

主要探讨台湾过去二十年来,在治理氮氧化物(NOx)排放方面所作的努力,包括NOx防治技术的引进与开发,以及管制策略的制定.在防治技术的引进与开发方面,主要以在使用化石燃料的发电厂加装SCR(触媒除硝法)设备为主,此外,老的热电厂亦有加装SNCR(选择性非触媒还原法)以及采用再燃烧技术来抑制NOx的排放.进一步探讨了台湾使用的这些NOx防治技术的优缺点以及所获得的经验.在NOx管制策略的制定方面,可分为1995年以前所制定的《空气污染防制法》;1995年以后,基于污染者付费的原则,以及为了鼓励工业及发电厂加装高效率NOx污染防治设备,进一步制定《空气污染防制费收费办法》.此后,台湾固定污染源所排放的NOx已大为改善.     

背景溶液对纳米氧化铁吸附病毒的影响

以噬菌体X174为病毒替代,通过等温静态批量吸附实验,研究了4种纳米氧化铁(α-Fe2O3、γ-Fe2O3-B、γ-Fe2O3-N、Fe3O4)对病毒在不同背景溶液中的吸附行为及其影响因素.结果表明,在模拟地下水中,4种纳米氧化铁对病毒均具有较高的吸附比例,其中α-Fe2O3对病毒吸附比例最高,在病毒初始浓度比较低(约1E+03PFU.mL-1)时可达100%.经Langmuir和Freundlich吸附等温线方程对上述吸附结果进行拟合表示,纳米氧化铁对病毒的吸附均为有利吸附(favorable adsorption),并可能存在多层吸附,吸附比例均随着病毒初始浓度的增加而减少.纳米氧化铁对病毒的吸附比例随着背景溶液离子强度的增加而降低,表示其吸附行为以电性吸附为主.背景溶液中阴离子存在显著降低了病毒的吸附量,这可能与阴离子竞争病毒吸附位点有关,其中HPO24-比HCO3-表现得更为明显.结果同时显示背景溶液中多价阳离子的存在(比如Ca2+和Mg2+)比单价阳离子(比如Na+和K+)更有利于纳米氧化铁对病毒的吸附.综上可知,纳米氧化铁是一种潜在的病毒净化理想材料,应用时需考虑其环境因素的影响.     

Nitric oxide and nitrous oxide emission from Hungarian forest soils; linked with atmospheric N-deposition

Studies of forest nitrogen (N) budgets generally measure inputs from the atmosphere in wet and dry deposition and outputs via hydrologic export. Although denitrification has been shown to be important in many wetland ecosystems, emission of N oxides from forest soils is an important, and often overlooked, component of an ecosystem N budget. During 1 year (2002–03), emissions of nitric oxide (NO) and nitrous oxide (N₂O) were measured from Sessile oak and Norway spruce forest soils in northeast Hungary. Accumulation in small static chambers followed by gas chromatography-mass spectrometry detection was used for the estimation of N₂O emission flux. Because there are rapid chemical reactions of NO and ozone, small dynamic chambers were used for in situ NO flux measurements. Average soil emissions of NO were 1.2 and 2.1 μg N m⁻² h⁻¹, and for N₂O were 15 and 20 μg N m⁻² h⁻¹, for spruce and oak soils, respectively. Due to the relatively high soil water content, and low C/N ratio in soil, denitrification processes dominate, resulting in an order of magnitude greater N₂O emission rate compared to NO. The previously determined N balance between the atmosphere and the forest ecosystem was re-calculated using these soil emission figures. The total (dry+wet) atmospheric N-deposition to the soil was 1.42 and 1.59 g N m⁻² yr⁻¹ for spruce and oak, respectively, while the soil emissions are 0.14 and 0.20 g N m⁻² yr⁻¹. Thus, about 10–13% of N compounds deposited to the soil, mostly as and , were transformed in the soil and emitted back to the atmosphere, mostly as greenhouse gas (N₂O).     

Environmental sub models for a macroeconomic model: agricultural contribution to climate change and acidification in Denmark

Integrated modelling of the interaction between environmental pressure and economic development is a useful tool to evaluate environmental consequences of policy initiatives. However, the usefulness of such models is often restricted by the fact that these models only include a limited set of environmental impacts, which are often energy-related emissions. In order to evaluate the development in the overall environmental pressure correctly, these model systems must be extended. In this article an integrated macroeconomic model system of the Danish economy with environmental modules of energy related emissions is extended to include the agricultural contribution to climate change and acidification. Next to the energy sector, the agricultural sector is the most important contributor to these environmental themes and subsequently the extended model complex calculates more than 99% of the contribution to both climate change and acidification. Environmental sub-models are developed for agriculture-related emissions of CH(4), N(2)O and NH(3). Agricultural emission sources related to the production specific activity variables are mapped and emission dependent parameters are identified in order to calculate emission coefficients. The emission coefficients are linked to the economic activity variables of the Danish agricultural production. The model system is demonstrated by projections of agriculture-related emissions in Denmark under two alternative sets of assumptions: a baseline projection of the general economic development and a policy scenario for changes in the husbandry sector within the agricultural sector.     

Impact of soluble organic matter and particulate organic matter on anammox system: Performance,microbial community and N2O production

In this study,the effects of soluble readily biodegradable COD (sCOD) and particulate slowly biodegradable COD (pCOD) on anammox process were investigated.The results of the longterm experiment indicated that a low sCOD/N ratio of 0.5 could accelerate the anammox and denitrification activity,to reach as high as 84.9%±2.8% TN removal efficiency.Partial denitrification-anammox (PDN/anammox) and denitrification were proposed as the major pathways for nitrogen removal,accounting for 91.3% and 8.7% o...     

长江口潮间带湿地涨退潮期N2O的排放通量研究

随着河口区接收上游人为氮排放量的增加,为这一区域氧化亚氮（N2O）的排放增加了很大不确定性。选择长江河口潮间带湿地为研究对象,分别采用原位静态箱法和静态顶空法,从2011年1月至12月对长江口沉积物 大气界面以及涨潮水 大气界面的N2O排放通量进行了为期一年的现场观测和研究。研究结果表明,沉积物 大气界面N2O通量有着显著的时空差异。N2O排放通量在日变化以及季节变化上都表现出明显的源汇转变,就年平均排放通量,光滩带沉积物 大气界面达到了599 μgN2O/(m2〖DK〗·h),而海三棱藨草盐沼带与大气间N2O交换则十分微弱,为060 μgN2O/(m2〖DK〗·h)。对长江口涨退潮期光滩和草滩上覆水体 大气界面N2O排放通量的研究表明,长江口涨退潮期在夏季和秋季,无论是光滩还是草滩均表现为大气N2O的稳定排放源,其中夏季平均253 μgN2O/(m2〖DK〗·h),秋季平均排放通量为207 μgN2O/(m2〖DK〗·h)。作为河口区上游排放氮素的直接接收者,和沉积物 大气界面N2O排放相比,长江口涨潮水 大气界面N2O排放稳定而又显著,是长江口N2O排放的主要贡献者,应成为这一区域N2O排放的关注热点     

两种铁氧化物对土壤有效态汞的吸附作用研究

利用氧化物对土壤中汞的吸附特性,研究了汞污染土壤中添加铁锰和铁铝复合氧化物对土壤汞有效性的影响.结果表明,在土壤中添加氧化物后,土壤中有效态汞的含量明显降低,在相同添加量下铁铝复合氧化物比铁锰复合氧化物的吸附效果好.14 d时间内,添加铁铝氧化物后,两种土壤中有效态汞的含量分别降低了94.60%和93.11%;添加铁锰氧化物后,两种土样中有效态汞的含量分别降低了88.69%和87.85%,可见两种氧化物是土壤中有效态汞的有效吸附剂.通过方程拟合研究了氧化物对土壤中有效态汞吸附的规律,其中,铁铝氧化物对土壤中有效态汞的吸附规律以Elovich方程和权函数方程拟合度较好,铁锰氧化对土壤中有效态汞的吸附规律以Elovich方程拟合效果最好,零级速率方程及指数方程的拟合效果则相对较差.     

中国水泥工业节能减排效果分析及对策研究

根据水泥工业大气污染物排放的数学模型;测算2005年-2011年中国水泥工业二氧化碳(CO2)、氮氧化物(NO2)、二氧化硫(SO2)、颗粒物(PM)和氟化物(F)等污染物排放量,分析节能减排的效果并提出解决问题的对策。结果表明:水泥工业CO2排放量逐年增长,并且与水泥产量和单位产品综合能耗呈线性关系;原料煅烧和能源利用过程CO2排放量分别占56%和44%;单位水泥产品CO2排放强度由0.68 t·t-1下降到0.58 t·t-1,相当于每年节约标准煤682×104t、减少CO2排放共计1.03×108t。NO2排放量分别是SO2、PM、F的4、7、160倍。发展新型干法技术、建设烟气脱硝装置、协同处置固体废物是水泥工业未来节能减排的发展方向。     

硫素对水稻根系铁锰胶膜形成及吸收镉的影响

添加外源镉污染水稻土进行池栽试验,施入不同形态及数量的硫肥(单质硫、石膏),研究硫素对水稻根系铁锰胶膜的形成及对水稻吸收镉的影响.结果表明,整个水稻生育期内,土壤溶液Eh范围在-200~100 m V之间;p H在6.9~7.9之间;pe+p H在4~10之间.水稻根表胶膜以Fe膜为主,其质量分数达到5 000~13 000 mg·kg-1,Mn膜的质量分数相对较小,为170~580 mg·kg-1.在孕穗期高硫量处理与低硫量处理的铁胶膜质量分数分别为9 400 mg·kg-1和8 600 mg·kg-1,高硫量处理比低硫量处理可生成更多的铁胶膜;而根表锰胶膜的数量差异主要表现在分蘖期,单质硫和石膏硫处理的锰胶膜质量分数分别为600 mg·kg-1和400 mg·kg-1,达到显著差异水平,单质硫比石膏硫更易促进水稻根表锰胶膜的形成.胶膜对于Fe2+过量吸收有一定阻控作用,对Mn2+作用不显著.水稻根表胶膜吸附Cd的质量分数在分蘖期为78.8~131.1 mg·kg-1,孕穗期16.6~21.1mg·kg-1,成熟期3.0~9.2 mg·kg-1.在分蘖期与孕穗期,高硫量处理比低硫量处理的吸附量高,在成熟期反之.采用ACA方法浸提铁锰胶膜内的Cd测定值并不能真实地表明胶膜实际固定Cd的质量分数.水稻体内各部位Cd的质量分数表现为根茎叶籽粒.一定量的施硫能有效减少水稻各器官中Cd的质量分数.对于根和茎叶,单质硫在成熟期以前效果好于石膏硫;对于籽粒,石膏硫效果更佳.一定量的硫肥,能有效阻碍Cd从水稻根部向茎叶与籽粒的转移.对于茎叶,在孕穗期单质硫和石膏硫的Cd转移系数分别为0.13和0.25,差异显著,单质硫能更好地阻碍Cd的转移;对于籽粒,石膏硫的阻碍效果更好.