氧化还原介体强化厌氧活性污泥发酵产氢特征

为提高厌氧污泥的发酵产氢能力,采用间歇培养方式考察了氧化还原介体（ROMs）对厌氧污泥发酵葡萄糖产氢效能的影响,并通过Illumina MiSeq测序揭示了ROMs对微生物群落的影响.结果表明,在发酵液体积为100mL及葡萄糖初始浓度500mg/L条件下,对照的累计产氢量和最大产氢速率（R_max）分别为11.0mL和0.28mL/h.当腐殖酸和蒽醌-2-磺酸钠（AQS）作为ROMs加入发酵体系后,厌氧污泥的产氢能力显著提高,其累计产氢量和R_max分别比对照高出56.4%、13.6%和53.6%、10.7%.相反,氧化石墨烯（GO）、指甲花醌和蒽醌-2,6-二磺酸钠（AQDS）导致厌氧污泥的产氢能力受到不同程度的抑制.Illumina MiSeq测序揭示了发酵系统的优势菌群存在显著差异.对照系统中的优势菌群主要来自5个属（Thermomarinilinea、Longilinea、Defluviimonas、Gimesia、Planctomicrobium）,腐殖酸、AQS和指甲花醌发酵系统的主要优势菌群为Thermomarinilinea、Longilinea、Ottowia,而Thermomarinilinea、Longilinea、Ottowia、Defluviimonas为AQDS和GO发酵系统的主要菌群.冗余分析的结果表明,产氢量与Longilinea、Macellibacteroides、Trichococcus、Thioflavicoccus和Ottowia呈正相关,而与Defluviimonas、Pirellula、Gimesia和Ignavibacterium呈负相关.     

氧化还原介体调控亚硝酸盐反硝化特性研究

采用实验室驯化的亚硝酸盐反硝化菌群作为菌种,优化亚硝酸盐降解条件,探究在氧化还原介体蒽醌-2-磺酸钠(AQS)存在条件下亚硝酸盐反硝化的特性.结果表明,反硝化菌群降解亚硝酸盐的最适条件为:温度35℃,pH为8,丁二酸钠为碳源,碳氮比4∶1,初始亚硝酸盐浓度100 mg.L-1;AQS的最佳投加量为0.16 mmol.L-1,介体调控的反硝化体系氧化还原电位略有降低,维持在-400～-500 mV之间,pH随亚硝酸盐降解速率增加而增大,最终稳定到9～10之间;通过分析反硝化中间代谢产物,推测AQS在亚硝酸盐反硝化过程中不仅起到辅酶CoQ的作用而且加速了细胞色素传递电子的全过程.本研究可为氧化还原介体调控亚硝酸盐反硝化实际应用提供理论基础和优化参数.     

Effect of Fe（Ⅲ） on the bromate reduction by humic substances in aqueous solution

Humic substances are ubiquitous redox-active organic compounds of environment. In this study, experiments were conducted to determine the reduction capacity of humic acid in the man-ix of bromate and Fe（Ⅲ） solutions and the role of Fe（Ⅲ） in this redox process. The results showed that the humic acid regenerated Fe（Ⅱ） and reduced bromate abiotically. The addition of Fe（Ⅲ） could accelerate the bromate reduction rate by forming humic acid-Fe（Ⅲ） complexes. Iron species acts as electron mediator and catalyst for the bromate reduction by humic acid, in which humic acid transfers electrons to the complexed Fe（Ⅲ） to form Fe（Ⅱ）, and the regenerated Fe（Ⅱ） donate the electrons to bromate. The kinetics study on bromate reduction further indicated that bromate reduction by humic acid-Fe（Ⅲ） complexes is pH dependent. The rate decreased by 2-fold with the increase in solution pH by one unit. The reduction capacity of Aldrich humic acid was observed to be lower than that of humic acid or natural organic matter of Suwanne River, indicating that such redox process is expected to occur in the environment.     

Effect of Fe(Ⅲ) on the bromate reduction by humic substances in aqueous solution

Humic substances are ubiquitous redox-active organic compounds of environment.In this study,experiments were conducted to determine the reduction capacity of humic acid in the matrix of bromate and Fe(Ⅲ) solutions and the role of Fe(Ⅲ) in this redox process.The results showed that the humic acid regenerated Fe(Ⅱ) and reduced bromate abiotically.The addition of Fe(Ⅲ) could accelerate the bromate reduction rate by forming humic acid-Fe(Ⅲ) complexes.Iron species acts as electron mediator and catalyst for the bromate reduction by humic acid,in which humic acid transfers electrons to the complexed Fe(Ⅲ) to form Fe(Ⅱ),and the regenerated Fe(Ⅱ) donate the electrons to bromate.The kinetics study on bromate reduction further indicated that bromate reduction by humic acid-Fe(Ⅲ) complexes is pH dependent.The rate decreased by 2-fold with the increase in solution pH by one unit.The reduction capacity of Aldrich humic acid was observed to be lower than that of humic acid or natural organic matter of Suwanne River,indicating that such redox process is expected to occur in the environment.     

漆酶介体系统对孔雀绿的脱色研究

研究了漆酶介体系统对代表性三苯甲烷类染料孔雀绿的脱色处理。漆酶介体系统对孔雀绿的脱色效率比单独使用漆酶要高出10倍。高浓度的孔雀绿对漆酶介体系统的脱色效率有抑制作用,最适的pH值和温度分别在4.2和32°C左右。介体浓度的提高可促进脱色率的增加,但高浓度的介体会抑制脱色效率。漆酶和漆酶介体系统对孔雀绿的脱色机制上存在不同,前者的作用机制为脱甲基反应,而后者的脱色机制为自由基介导的聚合反应。     

北天堂垃圾污染场地氧化还原分带及污染物自然衰减研究

通过对北京市北天堂垃圾填埋场周围实际监测数据资料的分析,研究了垃圾填埋污染场地的氧化还原分带和污染物的自然衰减作用.结果表明,北天堂垃圾填埋污染场地存在氧化还原分带现象,依据各氧化还原带标志性物质浓度的分布规律和特点划分了5个氧化还原带,即产甲烷带、硫酸盐还原带、铁还原带、硝酸盐还原带和氧还原带.不同有机污染物在不同的氧化还原带中的衰减不同;挥发酚和氰化物在硫酸盐还原带中的含量相对较高,分别为0.005和0.019 μg/L;Cr、Pb、Ni、As、Cu、Cd、Zn和Mn等重金属在产甲烷带中的含量相对较高,分别为25.11、 33.82、 29.93、 3.18、 2.3、 0.1、 283.1、 1 220　μg/L.因此,氧化还原带对污染物的衰减起重要作用.     

水溶性有机物的电子穿梭功能研究

以源于污泥的DOM(dissolved organic matter)为供试材料,以中国希瓦氏菌(Shewanella cinica)D14T为电子转移驱动力,研究了DOM的氧化还原性能与电子穿梭功能.结果表明,污泥DOM可作为末端电子受体接受醌还原菌D14T呼吸链上的电子,从而转变为还原态DOM,而还原态DOM可将电子再次转移给Fe(Ⅲ).经D14T还原后,DOM电子供给量(e-/C)由初始2.2~14μmol.g-1增加到253~347μmol.g-1.循环伏安法与多次还原-氧化循环实验表明,DOM呈现2对明显的氧化还原峰,经3次还原-氧化循环后电子供给量可稳定维持在150~250μmol.g-1之间,说明DOM具有重复利用、反复转移电子的特性.在菌株D14T还原水铁矿的体系中,加入DOM可提高水铁矿的还原溶解速率,其原因是DOM在D14T与水铁矿之间充当了电子穿梭体的角色.这些结果反映了DOM在电子转移反应中的重要性,为DOM的环境属性提出了一个新见解.     

垃圾渗滤液污染地下环境物质变化对污染缓冲的影响

通过砂柱模拟实验研究垃圾渗滤液污染地下环境中氧化还原环境和主要组成物质的变化对沉积物的pH缓冲能力和氧化还原能力的影响及其相互关系.结果表明,氧化还原环境的变化对地下环境沉积物的pH缓冲和氧化还原缓冲能力有重要影响,产甲烷带/硫酸盐还原带(MGZ/SRZ)、铁还原带(IRZ)、硝酸盐还原带(NRZ)和氧还原带(ORZ)沉积物的pH缓冲容量相对于本底值分别增加了12.4%、 10.8%、 19.8%和11.1%;pH缓冲和氧化还原缓冲之间相互影响、相互促进,它们直接影响着地下环境中污染物的自然衰减作用;沉积物中的铁氧化物、有机质、SO_4~(2-)和NH_4~+-N等的含量对pH缓冲能力和氧化还原缓冲能力均有不同的影响,整个体系的污染缓冲能力是各组分的综合作用结果.     

基于氧化还原分析的硫化矿尘爆炸压力预测*

为探究可应用于生产现场的硫化矿尘爆炸压力预测方法,基于硫化矿尘爆炸反应机理和粉尘引爆试验数据对硫化矿尘的氧化还原成分与其爆炸压力的相关关系进行分析。研究结果表明:硫化矿尘的还原成分指数与其爆炸压力的相关性极高,尤其是与其爆炸压力峰值的相关性系数高达0.993。整合研究结果形成的硫化矿尘爆炸压力和爆炸压力峰值计算和预测模型,可为金属矿山的硫化矿尘爆炸预防提供决策依据。     

Metal associations in anoxic sediments and changes following upland disposal†

The ecological effects of heavy metals in contaminated sediments are more determined by the chemical form and reactivity than by the level of accumulation. Dredging of anoxic sediments and disposal on land is attended by changes of redox conditions. Under oxidizing conditions some controlling solid compounds may change gradually thus changing the solubility of certain metals.

Chemical extraction experiments for estimating characteristic association forms of heavy metals in anoxic sediments were carried out, both under presence and absence of air during the analytical procedure. Drying of the sediment decreases the proportion of the sulfidic metal fractions to a stronger degree, and oxidized Cd and Zn are found in the most available, exchangeable fraction.

With respect to long‐term effects acidification of poorly buffered sludges after disposal on land is probably the most important factor affecting metal associations and mobility. For many metal examples a linear relationship has been found between decreasing pH values and increasing dissolved metal concentrations. To quantify these relationships and for better comparison of samples a simple test procedure is proposed which is based on pH differences before and after addition of acid.