火化过程中二噁英类污染物减排技术研究

为减少火化过程中二噁英类污染物的排放,研究了"热交换器 布袋除尘器 活性炭纤维毡"三级组合对火化遗体烟气中二噁英类污染物的去除效果.利用急冷技术将二次燃烧室排出的火化烟气温度降到90～130℃.实验表明,布袋除尘器去除火化烟气中二噁英类污染物的效率为57.4%;布袋除尘器分别与厚度为5、15 mm的活性炭纤维毡组合去除火化烟气中二噁英类污染物的效率分别为64.0%和89.2%.     

Heterogeneity of chlorinated hydrocarbon sorption properties in a sandy aquifer

Hydraulic conductivity and sorption coefficients for chlorinated hydrocarbons (chloroform, carbon tetrachloride and tetrachloroethylene) were evaluated for 216 sediment samples collected across a 15 m transect and a 21 m depth interval in a contaminated aquifer near Schoolcraft, Michigan. Relationships between hydraulic conductivity, linear sorption partition coefficients, grain size classes, and spatial location were investigated using linear regression analysis and geostatistical techniques. Clear evidence of layering was found in sorption properties, hydraulic conductivity and grain sizes. Conductivity correlated well with grain size, as expected, but sorption varied inversely with grain size, contrary to some previous reports. No significant correlation was found between sorption properties and hydraulic conductivity. This is likely due to the unexpected presence of small amounts of highly sorptive coal-like solids, which dominate the sorption behavior but have little effect on conductivity. The results demonstrate that recent findings regarding the high sorption capacity of coal materials found in soils can exert a controlling influence on contaminant transport. Designers of in situ remediation systems should be cautioned that 1) it is not reasonable to assume that sorption capacity and hydraulic conductivity are related, 2) sorption capacity and hydraulic conductivity are critical measurements for contaminant site characterization and subsequent transport modeling, 3) estimating sorption capacity from organic carbon measurement may lead to greater errors than performing sorption isotherms, and 4) it is more important to characterize vertical heterogeneity rather than horizontal heterogeneity because both sorption and hydraulic conductivity are correlated across longer distances in the horizontal plane.     

基于生态足迹模型的浙江省可持续发展研究

基于废弃物处理技术与土地面积之间的关系,对Wackernagel等提出的生态足迹模型中废弃物账户的核算方法作了补充,并以浙江省为实例,分析了2003年浙江省可持续发展状况.结果表明,2003年浙江省人均生态足迹为1.70 hm2,人均生态承载力为0.42 hm2,人均生态赤字为1.28 hm2,生态需求与供给之间存在一定差距.     

Monitoring trichloroethene remediation at an iron permeable reactive barrier using stable carbon isotopic analysis

Stable carbon isotopic analysis, in combination with compositional analysis, was used to evaluate the performance of an iron permeable reactive barrier (PRB) for the remediation of ground water contaminated with trichloroethene (TCE) at Spill Site 7 (SS7), F.E. Warren Air Force Base, Wyoming. Compositional data indicated that although the PRB appeared to be reducing TCE to concentrations below treatment goals within and immediately downgradient of the PRB, concentrations remained higher than expected at wells further downgradient (i.e. >9 m) of the PRB. At two wells downgradient of the PRB, TCE concentrations were comparable to upgradient values, and delta13C values of TCE at these wells were not significantly different than upgradient values. Since the process of sorption/desorption does not significantly fractionate carbon isotope values, this suggests that the TCE observed at these wells is desorbing from local aquifer materials and was present before the PRB was installed. In contrast, three other downgradient wells show significantly more enriched delta13C values compared to the upgradient mean. In addition, delta13C values for the degradation products of TCE, cis-dichloroethene and vinyl chloride, show fractionation patterns expected for the products of the reductive dechlorination of TCE. Since concentrations of both TCE and degradation products drop to below detection limit in wells within the PRB and directly below it, these downgradient chlorinated hydrocarbon concentrations are attributed to desorption from local aquifer material. The carbon isotope values indicate that this dissolved contaminant is subject to local degradation, likely due to in situ microbial activity.     

S–O–C isotopic picture of sulphate–methane–carbonate system in freshwater lakes from Poland. A review

Microbial oxidation of organic compounds (including methane), in freshwater sediments, may result in precipitation of carbonates, which may become an important geochemical archive of paleoenvironmental variations. Most probably low δ¹³C value in calcite in eutrophic systems results from an advanced oxidation of organic compounds in turbulent or/and sulphate-rich conditions. Likewise, high δ¹³C value in calcite from organic-rich sediments may evidence low redox potential of the freshwater system. Oxidation of methane and organic matter results in significant isotope effects in sulphates dissolved in water. Therefore, to better understand the origin of carbon isotope signal in carbonates, concentration and stable isotope measurements in dissolved sulphate (water column), bubble methane and calcite (freshwater sediments) have been carried out in 24 lakes, 2 ponds and 4 rivers in Poland. The highest concentration of sulphate has been detected in rivers (85.47 SO₄ ²⁻ mg/l) and an artificial lake (70.30 SO₄ ²⁻ mg/l) located in the extremely SO₄ ²⁻-polluted region called the “Black Triangle”. The lowest concentration of sulphate is found in dystrophic and mountain lakes (from 0.5 SO₄ ²⁻ to about 3 mg/l). The lowest δ³⁴S(SO₄ ²⁻) and δ¹⁸O(SO₄ ²⁻) values occur in unpolluted lakes in eastern Poland (−0.94 and 1.38‰, respectively). The highest S and O isotopic ratios are found in a polluted lake in western Poland (δ¹⁴S(SO₄ ²)=12.95‰) and in a dystrophic lake in eastern Poland (δ¹⁸O(SO₄ ²) = 16.15‰) respectively. It is proposed that δ³⁴SO₄ ²⁻ and (¹⁸O(SO₄ ²⁻) values in lakes represent a good tool to assess and quantify anthropogenic impact by acid precipitation and to monitor variations in the trophic state and redox processes controlled by biodegradation of organic compounds in sediments and water column. In general, increasing depth (up to 12 m) of the water column is associated with decreasing trend the δ¹³C(CH₄) value from about –35 to about –78‰. However, δ¹³C value in sedimentary calcite (δ¹³C vary from –10 to 0.5‰) shows opposite trends as compared to the corresponding methane. This is probably due to redox processes and distribution of heavy isotopes between methane and calcite. Likewise, turbulent water (river) show high δ¹³C value in methane and low δ¹³C value in calcite—this is probably due to an enhanced oxidation of methane producing ¹³C-depleted CO₂. In contrast to clean lakes, it is observed that an increase of the δ¹³C(CH₄) value occurs with increasing depth of the water column in a strongly SO₄ ²⁻-contaminated lake. This is probably due to a loss of biological buffering potential of the lake accompanied by an active oxidation of methane precursors.     

青岛市生态足迹动态研究

利用生态足迹和生态承载力度量和评价1995—2004年间的青岛市可持续发展程度。结果发现,随着经济的发展和社会的进步青岛市的生态足迹显著上升,各类用地都呈现增加趋势,耕地增加程度最大,而水域则表现出不稳定;承载力明显下降,其中主要是耕地承载力下降,林地、水域等其他用地则有相对的提高。生态足迹和承载力的变化造成生态赤字进一步加大。将单位生态足迹内产生的GDP作为生态效率,可以发现青岛市的生态效率呈现增加趋势,表明青岛市的资源利用效率明显增加。按照1995到2004年的发展趋势,青岛在未来十年的生态赤字将进一步加大,通过科学技术提高生态效率是青岛降低生态赤字的主要途径。文章首次分析了青岛市的生态足迹动态,提出了降低生态赤字的途径,为青岛市的可持续发展提供了理论参考。     

Analysis of leakage in carbon sequestration projects in forestry: a case study of upper magat watershed,Philippines

The role of forestry projects in carbon conservation and sequestration is receiving much attention because of their role in the mitigation of climate change. The main objective of the study is to analyze the potential of the Upper Magat Watershed for a carbon sequestration project. The three main development components of the project are forest conservation: tree plantations, and agroforestry farm development. At Year 30, the watershed can attain a net carbon benefit of 19.5 M tC at a cost of US$ 34.5 M. The potential leakage of the project is estimated using historical experience in technology adoption in watershed areas in the Philippines and a high adoption rate. Two leakage scenarios were used: baseline and project leakage scenarios. Most of the leakage occurs in the first 10 years of the project as displacement of livelihood occurs during this time. The carbon lost via leakage is estimated to be 3.7 M tC in the historical adoption scenario, and 8.1 M tC under the enhanced adoption scenario.     

混凝氧化法处理精研精抛清洗废液

采用混凝、氧化的方法对精研精抛清洗废液进行处理，对絮凝过程中所用的６种混凝剂的投加量ｐＨ值和氧化过程中的氧化试剂Ｈ２Ｏ２的投加量分别进行了筛选，同时简单地分析了反应机理．经混凝氧化处理后，ＣＯＤ值由１２００ｍｇ／ｍＬ降至５００ｍｇ／ｍＬ左右，ＣＯＤ去除率达９５％；最后进行活性炭吸附，ＣＯＤ值达到国家排放标准．     

理论等温方程式在CS2—ACF静态吸附体系的应用

测定了CS_2蒸气在4种ACF(活性炭纤维)和GAC(粒状活性炭)上的若干吸附等温线。用BET方程、H-J方程和D-A方程对CS_2-ACF静态吸附体系进行了处理。结果表明,除H-J方程外,其它两个方程适用良好。通过理论等温方程式,求出了吸附剂的比表面积和微孔体积。     

大学校园的生态足迹探究

生态足迹分析法是评价绿色校园建设水平较好的指标之一,能定量揭示学校的生态状况,本文结合黑龙江科技学院的校园状况,简要介绍生态足迹成分法的原理和计算分析方法.研究结果表明,黑龙江科技学院2005年总生态足迹为18410.53 hm2,即需要18410.53 hm2生态生产性土地来支持学校的各类消费以及吸纳废弃物;人均生态足迹为0.94 hm2/人,与全国人均生态足迹1.5 hm2相比较,学校的生态状况比较乐观.