Historical change of mercury pollution in remote Yongle archipelago, South China Sea

We collected three ornithogenic coral sand sedimentary profiles from Jinyin Island, Jinqing Island and Guangjin Island of Yongle archipelago, South China Sea and reconstructed the deposition flux of anthropogenic Hg over the past 700 years in the study area. On the whole, the anthropogenic Hg flux is relatively low; it remained at a low level before the Industrial Revolution with a small peak at about 1450-1550 AD, which may record the enhanced metallurgy activity in Ming Dynasty of China. During the 20th century, the deposition flux of anthropogenic Hg increased rapidly, but two troughs occurred during the periods around 1940s and 1970s, corresponding to the economic depression caused by World War II, Civil War in China (1945-1949), and the Culture Revolution (1966-1976) in China. Since the 1970s the deposition flux of anthropogenic Hg has been persistently increasing, apparently the result of fast economic development in East and Southeast Asia countries around South China Sea.     

Comparison of homologous and heterologous formats in nanocolloidal gold-based immunoassays for parathion residue determination

The effectiveness of homologous and heterologous formats in a nanocolloidal gold-based immunoassay for pesticide residue determination was investigated. Parathion, one of the most toxic organophosphorus pesticides, was used as the target analyte. One-step homologous and heterologous test strips based on a nanocolloidal gold-labeled monoclonal antibody were developed for the rapid detection of parathion residues. The results showed that the heterologous format was more effective than the homologous format, being more sensitive, more specific to parathion and more tolerant of matrix interferences. The best competitive hapten was found to have a moderate heterology and the opposite electronic distribution to the immunizing hapten. The detection limits for parathion using the preferred heterologous strip were 1 μg/L in water samples and 5 μg/kg in soil and food samples.     

Removal of genotoxicity in chlorinated secondary effluent of a domestic wastewater treatment plant during dechlorination

Purpose  

Dechlorination with tetravalent sulfur is widely used in wastewater treatment processes after chlorination. Dechlorination can remove certain genotoxic disinfection by-products (DBPs). However, the reactions occurring during dechlorination of chlorinated secondary effluent and their genotoxic chemicals are still very complex, and the related genotoxicity changes remain unknown. Therefore, the effects of dechlorination on genotoxicity in secondary effluent and its fractions and typical genotoxic chemical after chlorination were evaluated.     

Characteristics of precipitation chemistry at Lushan Mountain, East China: 1992–2009

Introduction

Trends in precipitation pH and conductivity during 1992?C2009, and in ionic compositions from January 2007 to June 2009, are reported from Lushan Mountain, one of the highest mountains in mid-east China. Annual mean pH was in the range of 4.35?C5.01 and showed a statistically very significant (P?P?Results and discussions Over the period of study, Lushan Mountain received more rainfall in spring and summer. The pH values varied seasonally with winter minima. The winter multiyear seasonal mean pH was 4.35. The corresponding summer value was 4.88. SO ₄ ^2? and NO ₃ ^? were the main anions, and NH ₄ ⁺ and Ca²⁺ the main cations. The anion to cation ratio was 0.8?C1.0, and that of [SO ₄ ^2? ] to [NO ₃ ^? ] was 2.4-3.0, much lower than that of the 1980s. However, sulfuric acid was still the main acid present. The ratio of [NH ₄ ⁺ ] to [Ca²⁺] was about 1.0, suggesting that these two alkaline substances provided close acid neutralizing capacity. The ratio of [Cl^?] to [Na⁺] was about 0.67, somewhat lower than that of natural precipitation.

Conclusions

Ionic composition varied seasonally and was closely correlated to the amounts of rainfall and pollution. Trajectory analyses showed that the trajectories to Lushan Mountain could be classified in six clusters and trajectories originating from the South Sea and the areas surrounding Lushan Mountain had the greatest impacts on precipitation chemistry.     

不同基质在人工湿地脱氮中的应用及其研究进展

在比较了不同基质脱氮效率的基础上,认为基质作为人工湿地的重要组成部分,在为植物和微生物提供生长介质的同时,也能通过沉淀、过滤和吸附等作用直接去除污染物质,其中基质的类型、级配等因素会影响基质作用的发挥;不同基质对脱氮性能存在较大差异,沸石和蛭石是目前研究中脱氮效率较高的两种基质。在归纳了脱氮机制和影响因素的基础上,认为不同基质由于脱氮机制不同,脱氮性能和脱氮效率也存在较大差异;人工湿地基质所有理化性状都可能影响到它对污水的脱氮效率。最后,对今后的相关研究方向进行了展望。     

脱氮吸附剂深度脱除模拟含氮油中氮化物的研究

将磷钨酸、甲醛气体负载于介孔分子筛SBA-15中制备脱氮吸附剂,其中SBA-15、磷钨酸、甲醛的质量比为10∶7∶3.以喹啉、吲哚和咔唑为目标氮化物,二甲苯及二甲苯和十二烷的混合液为溶剂配制模拟含氮油,考察了反应温度、氮化物类型对脱氮反应速率的影响以及磷钨酸、甲醛的脱氮机制.结果表明,磷钨酸可以有效脱除碱性氮化物和低浓度非碱性氮化物,甲醛能强化吸附剂对非碱性氮化物的选择性.在70℃、脱氮吸附剂与高浓度模拟含氮油质量比为2.0∶30.0的条件下,模拟含氮油中的氮化物在90 min内可以被深度脱除.磷钨酸对碱性氮化物的脱除机制为磷钨酸和碱性氮化物间的配合作用和酸碱反应,磷钨酸对非碱性氮化物的脱除机制为氮化物和甲醛在酸催化下缩合反应生成聚合物.反应吸附剂再生回用后的脱氮能力随氮化物碱性的增强而减弱.     

氢氧化铁用于污水污泥原位恶臭控制的研究

考察了添加不同剂量氢氧化铁对于污水污泥处置过程中的恶臭污染的控制效果。结果表明,在厌氧发酵32d时,添加0.05%、0.10%、0.25%(质量分数,下同)的氢氧化铁分别使污水污泥处理中硫化氢的平均去除率(与未添加氢氧化铁相比)达到81.3%、93.7%、97.5%;氢氧化铁的添加对污水污泥厌氧发酵中氨气的释放量没有明显影响。利用冷扩散连续萃取法考察了厌氧发酵过程中污水污泥中硫的形态分布,发现在氢氧化铁的作用下生成了硫化亚铁、二硫化亚铁、单质硫,从而降低了硫化氢的释放速率,有效控制了污水污泥厌氧发酵中的恶臭。氢氧化铁是一种可以用于污泥处理的高效除臭剂。     

SO2-4/TiO2光催化降解苯酚

以工业硫酸氧钛为原料水解制得SO42-/TiO2光催化剂,并以苯酚为目标降解物,考察了SO24-/TiO2的光催化性能。结果表明:随着SO42-/TiO2制备过程中焙烧温度的升高,其光催化活性逐渐增加,650℃焙烧获得的SO24-/TiO2的光催化活性最好,此后再升高温度会因催化剂中硫的挥发而下降;在确定苯酚原液初始浓度为50 mg/L条件下,SO42-/TiO2的光催化降解苯酚的最佳工艺条件为反应时间2 h、苯酚pH为7、催化剂用量1 g/L。XRD、SEM和FTIR的分析结果显示实验温度下制得的SO42-/TiO2均为锐钛型TiO2;其间掺杂的SO24-在TiO2表面分散性较好,没有聚集成大的颗粒;红外分析的结果初步判定低温(<550℃)焙烧制得的催化剂SO42-在TiO2表面是螯合双配位吸附,高温焙烧时(>550℃)SO42-在TiO2表面是桥式配位吸附。     

湘江株洲段丰水期镉污染负荷总量测算及分配

以2010年8月湘江干流株洲段代表性断面水质与底泥监测资料以及其他资料为基础,采用WASP7模型模拟该江段丰水期镉浓度,并进行镉污染负荷测算与分配。研究结果表明,WASP7模型较好地重现了镉浓度的变化规律,8月份该河段上游镉入流量2 446.33 kg,下游出流量3 076.44 kg,区间增量630.12 kg,其中点源负荷量241.67 kg,占38.4%,面源负荷量304.49 kg,占48.3%,内源负荷量为83.96 kg,占13.3%。     

层状双氢氧化物的合成及其对硼酸根的吸附

对不同层间阴离子类型的Zn-Al型层状双氢氧化物(Zn-Al-LDHs)进行了共沉淀合成,将合成的不同层间阴离子类型的Zn-Al-LDHs用于吸附模拟废水中的硼酸根。实验结果表明:当层间阴离子为NO_3~-时,Zn-Al-NO_3~--LDHs对硼酸根有最大的吸附量;在硼酸根初始质量浓度为100mg/L、废水pH为9、振荡时间为3 h时,Zn-Al-NO_3~--LDHs对硼酸根的吸附量为3.014 mg/g,吸附趋于饱和。