异化Mn(IV)还原菌激活及其对有机药物去除

以嘉陵江沉积物为菌源,利用荧光绝对定量（qPCR）技术探究了不同碳源（葡萄糖和乙酸钠）和不同形态的锰氧化物（δ-MnO₂和锰矿粉）对异化Mn（IV）还原菌激活效果的影响.在此基础上,研究了激活效果最佳的异化Mn（IV）还原菌对卡马西平、布洛芬、萘普生、雌激素和双氯芬酸5种有机药物的去除效果.结果表明,葡萄糖作为碳源,δ-MnO₂作为电子受体时激活效果最佳,Mn²⁺10d累计生成浓度达416.03mg/L,TOC消耗率达88.24%.激活后的异化金属还原菌在有无外加碳源时对卡马西平和布洛芬均无明显去除,对萘普生在外加碳源时能实现11.88%的去除.雌二醇和双氯芬酸可以作为异化Mn（IV）还原菌唯一碳源,其去除率可达75.70%和58.25%.     

多因素对ANAMMOX菌利用零价铁还原硝酸盐过程影响

以厌氧氨氧化（ANAMMOX）菌利用零价铁还原硝酸盐体系为研究对象,采用单因素调控法结合中心复合法（CCD）系统研究铁形态、进水pH值、温度、Fe/N等对该体系中硝酸盐去除率的影响.结果表明,在相同的反应条件下,投加纳米铁时ANAMMOX体系中硝酸盐的去除效果最优;反应温度和Fe/N对体系中硝酸盐去除率影响十分显著,而进水pH值影响较弱.利用CCD法得出模型预测的最佳反应条件为：进水pH值为4.00,反应温度为35.00℃,Fe/N为38.23,预测的硝酸盐去除率为94.70%,实际实验得出的硝酸盐去除率为88.99%.     

白果壳遗态Fe/C复合材料对水中磷的吸附特征

为研究PBGC-Fe/C-G（白果壳遗态Fe/C复合材料）对水中磷的吸附特征,以PBGC-Fe/C-G为吸附剂,对吸附剂投加量、溶液体系pH、初始磷质量浓度、温度和吸附剂粒径为影响因素进行静态吸附试验分析,并结合SEM、EDS、XRD和FT-IR等手段对吸附前、后材料进行表征,以揭示PBGC-Fe/C-G的吸附除磷机制.结果表明:①当初始磷质量浓度 < 10 mg/L、吸附剂投加量为0.2 g/（50 mL）、溶液为酸性（pH=3）、反应温度为45℃、吸附剂粒径 < 0.149 mm时,吸附效果最佳,吸附量达1.62 mg/g.②准二级动力学模型和Freundlich吸附等温模型能较好地模拟PBGC-Fe/C-G对磷的吸附过程.③热力学结果显示,ΔG < 0、ΔS>0和ΔH>0,说明PBGC-Fe/C-G对磷的吸附过程是自发、熵增的吸热过程.研究显示,PBGC-Fe/C-G吸附除磷主要通过配位作用、静电引力、等电荷离子交换和物理作用4种协同完成,其中Fe活性位与磷酸根离子的配位反应为主要的反应过程.      

An Environmental Application of Regional Geochemical Mapping in Understanding Enzootic Geophagia of Calves in the Reivilo Area, South Africa

A specific enzootic form of geophagia (the deliberate ingestion of soil) occurs in young cattle and sheep in restricted areas of the Barkley-West, Postmasburg and Vryburg Districts of the Northern Cape- and North West Provinces of the Republic of South Africa. It results in severe, subacute to chronic hepatitis and jaundice, with a high mortality rate in untreated cases. An association between the disease and high concentrations of manganese in soils was shown since all the affected farms are situated on outcrops of the Reivilo Formation of the Campbell Rand Subgroup, which consists mainly of manganiferous dolomite. Furthermore high concentrations of manganese were found in the analysis of liver specimens from affected calves and the characteristic microscopic pathological changes in the liver could be induced experimentally in a calf and lamb by oral administration of manganese sulphate. The highest incidence of geophagia occurs at 7 to 14 days, whereas calves older than about 2 months are rarely affected. The symptoms usually start with intermittent, progressive geophagia, followed by constipation, dehydration and death within ca. 7–10 days in untreated cases. Young calves and lambs display an insatiable appetite for soil and sometimes lick iron poles. The treatment of calves by the parenteral injection of commercial iron-dextran- and vitamin B₁₂ preparations at 1 to 2 days after birth, and at 14 days of age, at the registered therapeutic doses, appeared to have a marked preventative effect on the occurrence of geophagia and its complications. Regional geochemical maps show a northeast–southwest trending anomaly in MnO, Zn and Pb, visually correlating with the distribution of the affected farms. Anomalously high distributions of Pb and Zn are also spatially related to the Pering (Pb,Zn) Mine. In this study, two farms were selected for comparative purposes. Gam, a farm situated on the Reivilo Formation of the Campbellrand Subgroup was chosen where a high incidence of geophagia occurred, as well as the farm Holpan on the Lyttelton Formation of the Malmani Subgroup where the problem was not known to be present. The farm Holpan was chosen as a control area, and is situated close to an old manganese mine on dolomite with a high MnO content. Geographically, Holpan is situated in an area with a high rainfall, with leaching and the formation of deep red soils on the dolomite, together with a hilly relief and low soil pH_{H 2 O}. Gam is situated in an area with lower rainfall, where precipitation would be less than evapotranspiration. The dolomite of the Malmani Subgroup and the Reivilo Formation are significantly different in their soil geochemistry. The MnO, Fe₂O₃ ^T and Co contents are significantly higher in the soils of the Malmani Subgroup than in the Reivilo Formation. The MnO, Zn and Pb contents on Gam are higher than on Holpan, whereas the Fe₂O₃ ^T and Co contents are lower. Soil on Holpan contains iron-minerals such as haematite, while no iron minerals were detected in the soils of Gam. The concretions, found in the soils on both farms, differs remarkably in iron-contents. Concretions on both farms have similar high concentrations of MnO, whereas the FeO content are low for the concretions on Gam and high for Holpan. Preliminary comparative analytical results of the colostrum, sampled from cows with new born calves within three days of birth, do not entirely reflect the soil geochemistry of the different farms. Whereas the soils on Gam have higher MnO, Zn and Pb, and lower Fe₂O₃ ^T and Co than Holpan, the colostrum produced on Gam has lower Mn, Fe and Co than on Holpan. The Pb and Zn concentrations in the colostrum on both farms do not differ significantly. The comparative regional geochemical soil data, together with the colostrum data, suggest that young calves on the farm Gam probably suffer from Fe and Co deficiency. Conversely, it was illustrated that the Fe and Co content in the soils are high and the Fe is abundant in the concretions on the farm Holpan. These findings, together with the apparent absence of geophagia at Holpan, as well as the observed effect of iron and cobalt supplementation in the prevention of geophagia on the farm Gam, suggests an association of geophagia with iron and cobalt deficiencies on the farm Gam.     

Potential Remobilization of Toxic Anions during Reduction of Arsenated and Chromated Schwertmannite by the Dissimilatory Fe(III)-Reducing Bacterium Acidiphilium cryptum JF-5

Schwertmannite, an iron(III)-oxyhydroxysulfate formed in acidic mining-impacted stream or lake waters often contaminated with toxic elements like arsenate or chromate, is able to incorporate high amounts of these oxyanions. Detoxification of the water might be achieved if precipitated arsenated or chromated schwertmannite is fixed in the sediment. However, under reduced conditions, reductive dissolution of iron oxides mediated by the activity of Fe(III)-reducing bacteria might mobilize arsenate and chromate again. In this study, the reduction of synthesized arsenated or chromated schwertmannite by the acidophilic Fe(III)-reducer Acidiphilium cryptum JF-5, isolated from an acidic mining-impacted sediment, was investigated. In TSB medium at pH 2.7 with glucose as electron donor, A. cryptum JF-5 reduced about 10% of the total Fe(III) present in pure synthetic schwertmannite but only 5% of Fe(III) present in arsenated schwertmannite. In contrast to sulfate that was released during the reductive dissolution of pure schwertmannite, arsenate was not released during the reduction of arsenated schwertmannite probably due to the high surface complexation constant of arsenate and Fe(III). In medium containing chromated schwertmannite, no Fe(II) was formed, and no glucose was consumed indicating that chromate might have been toxic to cells of A. cryptum JF-5. Both As(V) or Cr(VI) could not be utilized as electron acceptor by A. cryptum JF-5. A comparison between autoclaved (121 °C for 20 min) and non-autoclaved schwertmannite samples demonstrated that nearly 100%of the bound sulfate was released during heating, and FTIR spectra indicated a transformation of schwertmannite to goethite. This structural change was not observed with autoclaved arsenated or chromated schwertmannite. These results suggest that the mobility of arsenate and chromate is not enhanced by the activity of acidophilic Fe(III)-reducing bacteria in mining-impacted sediments. In contrast, the presence of bound arsenate and chromate seemed to stabilize schwertmannite against reductive dissolution and its further transformation to goethite that is an ongoing process in those sediments.     

用含锰废水生产高纯碳酸锰

介绍了用含锰废水生产高纯碳酸锰的原理和工艺条件,生产出的高纯碳酸锰产品质量可以达到了ＧＢ１０５０３－８９Ⅱ型一等品标准,此法具有较好的经济效益和环境效益。     

铁-草酸配合物光分解降解活性染料的研究

研究了铁（Ⅲ)-草酸配合物在可见光及太阳光照射下，对活性染料的光解降解作用。结果表明，在pH=4．0、Fe(Ⅲ)／H2E2O4=0．060mmol／L／2．88mmol／L(草酸分2次加入)、光照3h的条件下，20mg／L的活性红的降解率为97．5％。溶液pH值、铁与草酸浓度比和活性染料浓度均对降解效果产生影响。     

从废旧锌锰电池中回收锌和锰的工艺研究

废旧锌锰干电池经过剖开、焙烧处理，去除汞和碳粉，再用硫酸浸取，滤液采用沉淀法分离锌和锰。锌和锰的回收率分别为94．5％和93．6％。     

低有机碳含量表层土中Fe2O3对γ-666光解的催化作用

考察5种低有机碳含量天然土中Fe2O3光催化降解γ-666的光解动力学,γ-666的光解符合准一级动力学方程.从所得的γ-666光解动力学常数可知,随Fe2O3质量分数从0.40%增加到5.40%,γ-666的一级光解动力学常数也增大,且两者的线性相关系数为0.952,其在5种天然土中的半衰期随Fe2O3含量的增加依次为133.3h,82.5h,44.1h,28.5h,20.4h.由此可见,低有机碳含量天然土中Fe2O3对γ-666的光解具有明显的催化作用.     

聚甲基丙烯酸-Fe3O4纳米吸附剂的吸附性能

以共沉淀法制备纳米Fe3O4,通过在颗粒表面接枝聚甲基丙烯酸(PMAA),制备了一种新型磁性纳米吸附剂.用透射电镜(TEM)、X-衍射分析(XRD)等对其进行了表征,并考察了它对酸性玫瑰红B(RB)的吸附性能.结果表明,制备的磁性微球平均粒径18nm.该吸附剂能有效去除RB,吸附速率很快,在5min内基本达到平衡.等温吸附数据符合Langmuir模型,饱和吸附容量为0.2mg/mg,吸附常数为7.2mL/mg.吸附为吸热过程,288～318K时,焓变为18kJ/mol.