蒽醌染料中间体溴氨酸降解酶的特性

从污染地分离筛选出的菌株BX26对蒽醌染料中间体溴氨酸有显著的降解脱色作用,降解过程受降解酶的控制,试验结果表明,降解酶为溴氨酸诱导的胞外酶,该酶在温度高于50℃处理后失活,盐度对该酶失活有影响,盐度高于1%会显著降低该酶活力,酶对溴氨酸的催化脱色要有氧参加,氮气气氛中酶活受抑制。     

Enhanced degradation of azo dye alizarin yellow R in a combined process of iron–carbon microelectrolysis and aerobic bio-contact oxidation

Purpose

With the aim of enhanced degradation of azo dye alizarin yellow R (AY) and further removal of the low-strength recalcitrant matter (LsRM) of the secondary effluent as much as possible, our research focused on the combination of aerobic bio-contact oxidation (ABO) with iron/carbon microelectrolysis (ICME) process.

Materials and methods

The combined ABO (with effective volume of 2.4?l) and ICME (with effectively volume of 0.4?l) process were studied with relatively short hydraulic retention time (HRT) of 4 or 6?h.

Results

At the HRT of 6?h with the reflux ratio of 1 and 2, the AY degradation efficiency in the final effluent was >96.5%, and the total organic carbon (TOC) removal efficiency were 69.86% and 79.44%, respectively. At the HRT of 4?h and the reflux ratio of 2, TOC removal efficiency and AY degradation efficiency were 73.94% and 94.89%, respectively. The ICME process obviously enhanced the total AY removal and the generated micromolecule acids and aldehydes then that wastewater backflow to the ABO where they were further biodegraded.

Conclusion

The present research might provide the potential options for the advanced treatment azo dyes wastewater with short HRT and acceptable running costs.     

纳米零价铁对铀尾矿库土壤中铀形态分布及固定效果的影响

针对纳米零价铁(nZVI)对铀尾矿库土壤中铀形态分布和U(Ⅵ)固定效果影响问题,采用逐级化学提取、毒性浸出(TCLP)和磁性分离实验,利用SEM-EDS和XRD对nZVI固定前后的铀尾矿土壤进行表征;研究了nZVI在不同投加量和pH条件下,对尾矿库土壤固定前后铀的形态分布和固定效果的影响,并对nZVI的固定机理进行了探讨。结果表明：当nZVI的投加量为8%、pH为5时,土壤中U(Ⅵ)的固定效果最好,固定后土壤中铀的毒性浸出值仅为13.98%;对经过nZVI处理后的铀尾矿土壤进行磁性分离发现,磁性和非磁性土壤重量占比分别为32.87%和67.13%,其铀含量分别达到55.05%和44.95%,说明nZVI对土壤中的U(Ⅵ)有较好的富集作用。nZVI对铀尾矿库土壤中的U(Ⅵ)有较好的原位固定和富集效果,并能减少土壤中铀的析出。     

安徽沿江地区的区域发展特点与开发对策

安徽沿江地区虽然交通网络初具规模,城市专业化分工明显经济发展水平较低,属长江干流地区的低谷地带。另外,整个沿江地区应发挥水运与矿产资源的双重优势,促使建材,钢铁,石经等临江工业进一步开并予以合理布局。     

Identification of close relationship between atmospheric oxidation and ozone formation regimes in a photochemically active region

Understanding ozone (O₃) formation regime is a prerequisite in formulating an effective O₃ pollution control strategy. Photochemical indicator is a simple and direct method in identifying O₃ formation regimes. Most used indicators are derived from observations, whereas the role of atmospheric oxidation is not in consideration, which is the core driver of O₃ formation. Thus, it may impact accuracy in signaling O₃ formation regimes. In this study, an advanced three-dimensional numerical modeling system was used to investigate the relationship between atmospheric oxidation and O₃ formation regimes during a long-lasting O₃ exceedance event in September 2017 over the Pearl River Delta (PRD) of China. We discovered a clear relationship between atmospheric oxidative capacity and O₃ formation regime. Over eastern PRD, O₃ formation was mainly in a NO_x-limited regime when HO₂/OH ratio was higher than 11, while in a VOC-limited regime when the ratio was lower than 9.5. Over central and western PRD, an HO₂/OH ratio higher than 5 and lower than 2 was indicative of NO_x-limited and VOC-limited regime, respectively. Physical contribution, including horizontal transport and vertical transport, may pose uncertainties on the indication of O₃ formation regime by HO₂/OH ratio. In comparison with other commonly used photochemical indicators, HO₂/OH ratio had the best performance in differentiating O₃ formation regimes. This study highlighted the necessities in using an atmospheric oxidative capacity-based indicator to infer O₃ formation regime, and underscored the importance of characterizing behaviors of radicals to gain insight in atmospheric processes leading to O₃ pollution over a photochemically active region.     

新疆开都—孔雀河流域天然植被生态需水量研究

本研究以新疆开都—孔雀河流域为研究区,针对流域不同保护目标,采用定额法、阿克苏水平衡站公式和阿维里扬诺夫公式三种方法,分别估算了生态红线区和生态敏感区的生态需水量。研究结果表明开都—孔雀河流域生态红线区平均需水量为13.82×10~8m~3,生态敏感区平均生态需水量为2.06×10~8m~3,且潜水蒸发法中的阿克苏水平衡站公式的计算值与平均值最为接近。由于干旱区降水量稀少,天然植被生长完全依赖地下水,一般采用潜水蒸发法间接计算植被的生态需水量,在植被需水定额不好确定的情况下,更是首选潜水蒸发法进行生态需水量的估算。研究成果可以为孔雀河生态输水工程和塔里木河下游生态输水工程的实施提供科学依据。     

聚乙烯醇包埋奥奈达希瓦氏菌MR-1还原U(Ⅵ)

实验用聚乙烯醇包埋奥奈达希瓦氏菌MR-1制备了包埋微球,并用其对U（Ⅵ）进行还原实验。实验结果表明,当pH=7.0,不同聚乙烯醇浓度对包埋微球的成球性、稳定性和传质性均有影响,制备包埋微球的聚乙烯醇的最优浓度为10%;当U（Ⅵ）浓度为15 mg·L-1,奥奈达希瓦氏菌投加量为6 mL,且奥奈达希瓦氏菌与聚乙烯醇按1∶2的比例进行包埋后,包埋微球对U（Ⅵ）的去除率最高达96.22%。Cu2+、Mn2+、Ca2+等共存离子对包埋微球还原U（Ⅵ）产生影响,2.0 mmol·L-1的Ca2+对包埋微球还原U（Ⅵ）存在微弱的促进作用;2.0 mmol·L-1 Cu2+、Mn2+对包埋微球还原U（Ⅵ）存在不同程度的抑制作用,去除率分别仅为8.14%和65.99%。扫描电镜和电子能谱分析结果表明,铀被微球还原沉积在包埋微球中。     

粉末活性污泥处理含铀废水的特性

以生活污水处理厂剩余活性污泥为原料,制备粉末活性污泥(PAS)作为生物吸附剂,考察pH值,PAS投加量,U(Ⅵ)初始浓度和吸附时间对PAS吸附U(Ⅵ)的影响,探讨了PAS吸附U(Ⅵ)的作用机理。实验结果表明,在U(Ⅵ)初始浓度为10 mg/L时,其最佳吸附pH值为3,去除率97.77%,吸附平衡时间120 min;吸附过程较好地拟合了准二级动力学模型(R2≈1)和Freundlich等温模型(R2≈1);X射线能谱和离子交换实验分析表明,离子交换为其主要吸附方式,参与交换的主要离子为Ca2+;红外光谱分析表明,PAS吸附U(Ⅵ)后自身结构未发生改变。以0.1 mol/L的HCl溶液作为解吸液,初次解吸率达92.83%,循环利用3次仍具有较好的吸附效果。