氧化锰共生矿烟气脱硫的机理及影响因素

利用南非的氧化锰共生矿进行烟气脱硫,研究了共生锰矿烟气脱硫性能及其机理,并考察了锰矿粒径、反应温度、液固比、进气流量、进口SO2浓度等因素对脱硫率的影响。结果表明,氧化锰共生矿中主要的锰化合物是MnO2、Mn2O3和MnCO3,烟气脱硫过程主要存在4种方式：MnO2与SO2发生氧化还原反应生成硫酸锰;液相中Mn2+催化氧化SO2产生硫酸;MnCO3与硫酸反应生成硫酸锰;Mn2O3与硫酸反应后生成的MnO2可以继续与SO2进行脱硫反应,但是Mn2O3与SO2直接反应的活性较差。氧化锰共生矿烟气脱硫的最佳工艺参数为：锰矿粒径200目、反应温度80 ℃、液固比10:1以及进气流量600 mL?min-1     

碱激发电解锰渣制备水泥掺合料

电解锰渣是湿法冶炼金属锰的残渣,为降低其对环境的浸出毒性影响并提高其在水泥产品中的掺入量,利用碱激发技术处理电解锰渣制备水泥掺合料是一种可行的方法。主要研究了碱激发剂种类、掺量对电解锰渣的激发效果,并将碱激发电解锰渣用作水泥掺合料与水泥按不同比例混合研究对水泥抗压强度和浸出毒性的影响。结果表明：碱激发电解锰渣活性显著提高,NaOH中Na2O当量为10%时试件M-SH10的3、7、28 d抗压强度最高,分别为7.15、9.46、10.03 MPa;将此条件下激发的电解锰渣按质量比取15%与85%的水泥混合制得的掺合料其抗压强度较净水泥试件有一定程度的提高;浸出毒性结果显示Cd、Cr、Pb、Ni、Mn和Zn浓度均下降,且低于GB 8978-1996限值。     

高锰酸钾修复PAHs污染土壤过程中Mn迁移转化规律

为探究高锰酸钾氧化修复技术应用过程中Mn元素迁移转化规律及其潜在的环境风险,通过室内模拟实验,采用某焦化厂PAHs污染土壤作为研究材料,探究了高锰酸钾修复技术中不同药剂投加量对PAHs去除、高锰酸钾消耗量、土壤中Mn质量分数、Mn赋存形态分布及有效态Mn质量分数等的影响。结果表明,高锰酸钾氧化处理可有效去除土壤中PAHs;当高锰酸钾投加量为0.20 mmol·g⁻¹、反应时间为1 d时,PAHs去除率最高,可达89.61%。氧化处理过程中,高锰酸钾消耗量和土壤Mn质量分数均与高锰酸钾的投加量有关,随投加量增加而升高。其中,土壤Mn的质量分数与高锰酸钾消耗量呈显著正相关关系。高锰酸钾氧化处理后土壤中Mn主要以铁锰氧化物结合态存在,所占比例为77.04%~92.17%。土壤经0.05 mmol·g⁻¹高锰酸钾氧化处理后,土壤有效态Mn的质量分数比对照组增加了0.94倍;而在高锰酸钾投加量为0.10~0.40 mmol·g⁻¹的处理条件下,土壤有效态Mn的质量分数下降了77.65%~99.09%。药剂投加量是影响高锰酸钾氧化修复PAHs污染土壤过程中Mn环境行为的关键因子。本研究结果可为高锰酸钾氧化修复技术应用工艺优化提供参考。     

助剂作用下超声浸取电解锰渣

用8-羟基喹啉、黄原酸钾、十六烷基三甲基溴化铵、磷酸三丁酯、柠檬酸5种物质作浸取助剂,考察了助剂作用下超声辅助浸取法从电解锰渣中提取锰的工艺条件。实验结果表明：用1%（质量分数）柠檬酸作浸取助剂,在固液比（g/mL）为1∶4、酸矿比（mL/g）为0.3∶1、浸取温度为70℃的条件下,超声浸取15min,锰浸出率平均可达57.28%,是加热酸浸法锰浸出率的2.72倍,是无助剂超声辅助浸取法锰浸出率的1.52倍。     

THE IMPACT OF URBANIZATION ON THE DISTRIBUTION OF HEAVY METALS IN BOTTOM SEDIMENTS OF THE SADDLE RIVER1

ABSTRACT: A three-year study has been conducted on a 4.6 mile stretch of the Saddle River near Lodi, New Jersey. The primary objectives of this investigation were (1) to provide baseline information on the concentration and distribution of heavy metals in bottom sediments of the Saddle River; (2) to qualitatively evaluate which parameters affect this distribution; and (3) to determine the effect of urbanization on the concentration and distribution of these materials. Significant enrichments of several heavy metals were observed in bottom sediments of the lower Saddle River near Lodi, New Jersey, as compared to the upper Saddle River. Attempts to correlate metal concentrations in bottom sediments with chemical-oxygen demand were not successful in demonstrating a relationship between these two factors. Metal concentrations were found to be strongly dependent upon particle size. In general, metal concentrations in bottom sediments increased with decreasing partical diameter. However, metals enrichment was observed to be considerably greater in the larger sediment fractions studied (>420μ) than the smaller sediment fractions as one proceeded downstream through the urban area. Since the larger sediment fractions are least effected by scour and transport they may best reflect the effect of urbanization on the distribution of heavy metals over an extended period of time at a given location.     

龙口褐煤对Ni^2＋,Mn^2＋,Hg^2＋等重金属离子的吸附特性

本文以龙口褐煤作吸附剂,对重金属离子Ｎｉ＾２,Ｍｎ＾２＋,Ｈｇ＾２＋的单组分水溶液进行吸附研究,探讨了吸附剂的吸附性能,影响吸附的因素和吸附机理。结果表明：褐煤对Ｎｉ＾２＋,Ｍｎ＾２＋,Ｈｇ＾２＋的吸附均表现出Ｌａｎｇｍｕｉｒ特征,ＰＨ值是影响吸附的一个重要因素。     

用喷射鼓泡反应器进行烟气脱硫

介绍了采用喷射鼓泡反应器处理烟气量为7 000~10 000 m3/h的软锰矿浆烟气脱硫中试试验。试验中,对喷射鼓泡反应器及系统的阻力进行了测定,考察了不同品位、不同液固比的软锰矿条件及系统连续运行时的脱硫率和锰浸出率。中试表明,在液固比为(2~3)∶1、矿粉粒度约为100目的连续运行条件下,无论是选用品位高的钦锰矿还是品位低的软锰矿,系统运行稳定,且脱硫率保持在90%以上,锰浸出率在70%以上。吸收液经净化处理后得到的MnSO4.H2O产品可达到国家GB1622—86标准。     

海底铁锰氧化还原过程的模拟研究

本文用室内海水-沉积物平衡箱研究了沉积物间隙水中铁、锰的垂直变化分布和随时间变化的分布,Fe~(2+)随深度、时间的变化幅度大,在六个月的实验期内均是如此,而Mn~(2+)在放置三个月后即趋于稳定;Fe~(2+),Mn~(2+)产生的宏观经验动力学表明:Fe~(2+)受pH影响远比Mn~(2+)大,且随着深度的增加更为明显,Fe~(2+)在较下层产生速率大,而Mn~(2+)反之;Fe~(2+)的扩散转移是上覆海水向沉积物中转移,扩散量为-60.7ug/m~2d,Nn~(2+)转移方向相反,扩散量为1746.2ug/m~2.d。     

Arsenic contamination in the Kanker district of central-east India: geology and health effects

This paper identifies newer areas of arsenic contamination in the District Kanker, which adjoins the District Rajnandgaon where high contamination has been reported earlier. A correlation with the mobile phase episodes of arsenic contamination has been identified, which further hinges on the complex geology of the area. Arsenic concentrations in both surface and groundwater, aquatic organisms (snail and water weeds) soil and vegetation of Kanker district and its adjoining area have been reported here. The region has been found to contain an elevated level of arsenic. All segments of the ecoysystem are contaminated with arsenic at varying degrees. The levels of arsenic vary constantly depending on the season and location. An analysis of groundwater from 89 locations in the Kanker district has shown high values of arsenic, iron and manganese (mean: 144, 914 and 371 μg L⁻¹, respectively). The surface water of the region shows elevated levels of arsenic, which is influenced by the geological mineralised zonation. The most prevalent species in the groundwater is As(III), whereas the surface water of the rivers shows a significant contamination with the As(V) species. The analysis shows a bio-concentration of the toxic metals arsenic, nickel, copper and chromium. Higher arsenic concentrations (groundwater concentrations greater than 50 μg L⁻¹) are associated with sedimentary deposits derived from volcanic rocks, hence mineral leaching appears to be the source of arsenic contamination. Higher levels of arsenic and manganese in the Kanker district have been found to cause impacts on the flora and fauna. A case study of episodic arsenical diarrhoea is presented.     

溶解氧和温度对地下水除铁、锰效果的影响

研究锰砂滤层去除铁、锰过程中温度、溶解氧两个因素对去除效果的影响,为生物法除铁、锰的实际运行提供了参考依据。从经济性和微生物角度考虑,原水DO维持在3mg／L左右即可满足运行要求,采用跌水曝气的方式去除效果优于管道混合器。当铁锰共存时最适宜的处理环境温度为20℃。