含砷废水净化剂的制备及其应用研究

本文描述了用黄铁矿和还原铁粉或其代用品为原料制备含砷废水净化剂－硫化亚铁的新方法，获得了制备的最佳条件，探讨了其在含砷废水处理中的应用条件和影响因素，结果表明，该净化剂的生产及其处理含砷废水的工艺简单，经济高效，具有良好的开发应用前景。     

砷华生产废渣中硫的回收利用研究

高温下氧化焙烧细磨后的砷华生产废渣，利用软锰矿浆吸收产生的SO2气体，吸收液经净化除杂、浓缩结晶等工序可制备工业产品硫酸锰。适宜的焙烧条件如下：焙烧温度为650℃，焙烧时间为60min，废渣粒度为-97μm。选择合适的吸收工艺，Mn的浸出率可达96．20％，此时SO2脱除率为87．20％。     

Geochemical Characteristics of the Acid Mine Drainage in the Water System in the Vicinity of the Dogye Coal Mine in Korea

This study investigated geochemical characteristics of the acid mine drainage (AMD) discharged from the abandoned mine adits in the vicinity of the Dogye coal mine in Korea. Acid mine drainage discharged from Jeoncha pit adit of the Dogye coal mine, which is the main source of the AMD in the study area, had a pH value of 3.0 and concentrations of 2148mg SO₄ ^2– L^–1, 229mg Fe L^–1, 71mg A1 L^–1 and 11mg Mn L^–1. The reduction of some metal concentrations downstream from the discharge point could be explained on the basis of dilution and precipitation. The order of removal of metal ions downstream from the discharge point was Fe>A1, Cu>Zn, Mn. Acidity could be used as a good determining factor offering comprehensive and quantitative values for the polluting extent of acid mine drainage. The acidities existing in all acidic water samples in the Gunahan district originated primarily from mineral acidity, especially in the upper Nahan Creek from dissolved Fe and Al and in the middle and down Nahan Creek from dissolved Al. From the application of the WATEQ4F program, it was determined that predominant species of dissolved Fe in all water samples was Fe²⁺, and those of dissolved Al were AlSO₄ ⁺ and Al³⁺ except for IW2 sample which was associated with white precipitates. The species of dissolved Al in IW2 sample include also AlOH²⁺ and Al(OH)₂ ⁺. The saturation indices of goethite and haematite were positive in the water samples associated with ochrous precipitates (usually called Yellow Boy), therefore these solids might be precipitated. For the IW2 sample, the saturation indices of amorphous Al(OH)₃ and gibbsite were positive, so theoretically these solids might also be precipitated. By XRD analysis, it was found that goethite occurs in ochrous precipitates, and gibbsite in white precipitates.     

Phylogenetic analysis and arsenate reduction e ect of the arsenic-reducing bacteria enriched from contaminated soils at an abandoned smelter site

Microbial reduction of As(V) (i.e., arsenate) plays an important role in arsenic (As) mobilization in aqueous environment. In this study, we investigated As(Ⅴ) reduction characteristics of the bacteria enriched from the arsenic-contaminated soil at an abandoned smelter site. It was found that As(Ⅴ) was completely reduced to As(Ⅲ) (i.e., arsenite) in 21 h. After 3-d incubation, a yellow solid was precipitated and the concentration of As(Ⅲ) decreased sharply. After 150 h incubation, ca. 65% of soluble arsenic was removed from the solution. The analysis of the precipitate by scanning electron microscopy and energy dispersive spectrometer (SEM-EDS) and X-ray diffraction (XRD) revealed that the main component was crystalline arsenic sulfide (ASS). Microbial mediated reduction and mobilization of adsorbed As(Ⅴ) on ferric hydroxide was also examined. In the microcosm slurry experiment, ca. 53% of the adsorbed As(V) was reduced to As(Ⅲ) by the bacteria, which resulted in an appreciable release of arsenic into aqueous phase. The released arsenic was present predominantly as As(Ⅲ). The microbial diversity was analyzed by 16S rDNA-dependent molecular phylogeny. A near-full-length 16S rDNA gene clone library was constructed. The 197 clones were analyzed using RFLP (restriction fragment length polymorphism) and 72 OTUs were obtained, which contributed 51% of the content for total clone number in six OTUs. Six bacterial clones in these six OTUs were selected for sequencing and the sequenced clones were found to belong to the group Caloramator, Clostridium, and Bacillus.     

石煤开发利用重金属污染现状调查研究

报道了湖南、江西和浙江三省石煤开发利用过程中石煤、石煤渣、碳化砖、石煤烟尘灰、矿区周围土壤、水体和气溶胶部分重金属含量的调查方法和主要结果。调查结果表明：石煤的开采和利用对周围的土壤、水体和空气产生了一定污染,尤其是剧毒物质Cd和As的污染应引起高度重视。     

Arsenic and major cation hydrogeochemistry of the Central Victorian (Australia) surface waters

This paper reports on the major cations（Ca, Mg, Na and K） and arsenic（As） compositions of surface waters collected from major creeks, rivers and lakes in Central Victoria （Australia）. The surface waters were found to be neutral to alkaline （pH 6.7-9.4）, oxidised （average redox potential （Eh） about 130 mV） and showed variable concentrations of dissolved ions （EC, about 51-4386 /μS/cm）. The concen- trations of dissolved major cations in surface waters were found to be in the order of Na〉〉Mg〉Ca〉K and in soils the contents of metals followed an order of abundance as： Ca〉Mg〉〉K〉Na. While Na was the least abundant in soils, it registered the highest dissolved cation in surface waters. Of the four major cations, the average concentration ofNa（98.7 mg/L） was attributed to the weathering of feldspars and atmospheric input. Relatively highly dissolved concentrations of Na and Mg compared with the world average values of rivers reflected the weathering of rock and soil minerals within the catchments. The As soil level is naturally high（linked to lithology） as reflected by high background soil values and mining operations are also considered to be a contributory factor. Under relatively alkaline-oxidative conditions low mobility of dissolved As （average about 7.9 μg/L） was observed in most of the surface waters with a few higher values（〉15 μg/L） around a sewage disposal site and mine railings. Arsenic in soils is slowly released into water under alkaline and/or lower Eh conditions. The efficient sink of Fe, AI and Mn oxides acts as a barrier against the As release under near neutral-oxidising conditions. High As content （average about 28.3 mg/kg） in soils was found to be associated with Fe-hydroxides as revealed by XRD and SEM analysis. The dissolved As concentration was found to be below the recommended maximum levels for recreational water in all surface waters（lakes and rivers） in the study area. Catchment lithology exerted the fundamental control on surface water chemistry. Sites impacted by mining waste dumps showed a decline in water quality.     

深圳市郊区大气中PM2.5的特征分析

为了确定深圳市郊区大气中PM2.5的污染特征,本研究分析了2009年和2010年夏季和冬季PM2.5样品中的水溶性离子和多环芳烃成分.结果表明,深圳市郊区大气中PM2.5的质量浓度很高,夏季53.9%和冬季100%的样品超过了WHO的大气质量准则浓度.PM2.5中,冬季最主要的3种离子是SO24-、NO3-和NH4＋.在夏季,这3种离子在PM2.5中的含量都会减少,而Cl-、Na＋、K＋、Ca2＋和Mg2＋的含量会增多.另外,冬季是多环芳烃浓度较高的季节,其中萘、苊烯、苊和苯并荧蒽是冬季PM2.5中多环芳烃的主要成分.本研究还通过比值法和特征化合物法对深圳市郊区大气中的PM2.5进行了源解析,确定了PM2.5的可能来源.     

含砷废渣的资源化利用技术探讨

论述土法炼砷弃渣含砷固体废物处置方法,并对处置过程中的三废排放问题提出了相应的环境保护建议。     

柠檬酸对砷污染土壤的萃取优化条件实验研究

论文以新邱矿矸石山排土场土壤为研究对象,以去离子水做空白试验,选取尿素、十二烷基磺酸钠、碳酸氢钠、醋酸、柠檬酸等12种化学试剂做了萃取剂初选试验;并以柠檬酸为萃取剂进行了三因素三水平L9(33)正交实验。实验结果表明:柠檬酸和氢氧化钠可作为砷污染土壤的萃取剂,具有良好的萃取效果。柠檬酸作为砷污染土壤萃取剂的最优化条件是液土比为10mL/g,萃取时间为12h,萃取剂浓度为0.1mol/L。实验结果可为砷污染土壤的治理提供参考。     

水合物法海水淡化脱盐效率研究

采用水合物生成装置分别加入二氧化碳和甲烷气体通过水合物法进行2组海水淡化实验。每组实验分别提取3次不同反应时间的水合物晶体,检测水合物中Na+、Mg2+、K+、Ca2+、B3+的离子浓度。结果表明:CH4水合物形成过程中,盐离子的脱盐效率与离子半径和所带电荷量呈线性相关性。CO2水合物生成实验中,由于Ca2+与CO2-3反应生成Ca CO3颗粒,故Ca2+离子浓度变化与离子半径和电荷量呈非线性关系。同时提出更全面的水合物法海水淡化中盐离子的排斥机制。较于反渗透传统方法,水合物法具有脱硼效果好的优势。