喹啉降解菌的降解效果考察

为了探索石油污染土壤中含氮杂环化合物的降解情况，在考察石油污染土壤理化性质的基础上，选择喹啉作为目标污染物，采用选择性富集培养的方法，从45份石油污染土壤样品中，分离得到155株降解喹啉污染物的高效降解菌株，从中选择降解效率较高的2株喹啉降解菌命名为Q5和Q24，进行喹啉的降解性能研究，比较了单一优势菌株、人工复合菌群和土壤中的自然菌群对喹啉的降解情况。实验结果表明，石油污染土壤中自然菌群对喹啉的降解效果好于单一的优势菌株和人工复合菌群。     

改进式曝气生物滤池处理高氨氮废水的研究

针对化肥氨氮废水排放量大、氨氮浓度高、C/N低等特点,通过实验研究探讨了添加高效菌种后采用改进式曝气生物滤池对化肥氨氮废水的处理性能、机理及实用性,并与SBR、普通BAF(Biofor)工艺和未添加高效菌种的改进式曝气生物滤池进行了对比。实验结果表明,添加高效菌种后改进式曝气生物滤池可以将氨氮≤200 mg/L,COD≤150 mg/L的化肥废水有效地处理至氨氮≤5 mg/L,COD≤50 mg/L,同时对总氮去除率达60%以上。     

Distribution of total mercury and methylmercury in lake sediments in Arctic Ny-Ålesund

The toxicities and bioavailabilities of total mercury (THg) and methylmercury (MeHg) in aquatic systems have made them the subjects of recent research. In this study, we collected a lake sediment core from Ny-Ålesund in Svalbard and analyzed the distributions of THg and MeHg in the sediments. The increased trend of THg was caused by anthropogenic contamination since the 14th century through long-range transportation, especially after the industrial era. However, the peak values of Hg in surface sediment samples could be explained by the increased algal scavenging process in recent decades. All the biogeochemical proxies (e.g., pigments and diatom biomass) revealed recent sharp increases in aquatic primary production due to the current climate warming. Rock-Eval analyses indicated that algal-derived organic matter took up a large portion, and quantitative calculation showed that 89.6-95.8% of the Hg in post-1950 could be explained by scavenging. The distribution of MeHg has a close relationship with total Hg and organic matter. The oxidation-reduction condition is one of the possible factors affecting the methylation rates in H2 lake sediments. Higher algal productivity and organic matter actually led to the increased trend of methylation in the uppermost sediment. This study supports some new key hypotheses on climate-driven factors affecting Hg and MeHg cycling in High Arctic lake sediments.     

Irreversible fouling during multicycle microfiltration of wastewater effluent

This study focused on irreversible fouling during microfiltration of primary and secondary effluents from municipal wastewater treatment plants. Flow resistances were calculated from the sum of clean membrane resistances, resultant cake layer resistances, and consequent irreversible fouling resistances. Results from a dead-end cell experimental system showed that the accumulated cake resistance was dominating for microfiltration of primary/secondary effluents. Suspended solids in the primary and secondary effluents had a similar compressibility index, n, with a value of approximately 0.5, indicating that they were moderately compressible particles. The value of irreversible resistance is dependent on the intensity of membrane cleaning; however, for a given membrane cleaning strategy, this value steadily increased and reached a maximum after approximately 6 cycles of filtration and cleaning. This study provided an explanation for the significant drop of throughput flux in the early application of membrane processes, and a plateau flux approached correspondingly.     

短程硝化-铁炭微电解工艺处理焦化废水

以废刚玉石墨粉末和废铁屑作为电极，分别采用铁炭微电解工艺和短程硝化一铁炭微电解工艺对焦化废水进行脱氮处理。实验结果表明，采用短程硝化一铁炭微电解工艺对焦化废水脱氮效果好于只采用铁炭微电解工艺。铁炭微电解的最佳反应条件：废水初始pH为3．0，反应时间为70min，铁炭质量比[m（Fe）：m（C）]为1．0：1．3，混凝pH为9．0。在此最佳反应条件下，铁炭微电解工艺TN去除率为8．0％，短程硝化一铁炭微电解工艺NO2--N的去除率为57．0％，TN的去除率为50．0％。     

基于MODIS植被指数的浑善达克沙地植被物候变化

基于近20a MODIS的2种植被指数数据，利用Logistic曲线曲率极值法和动态阈值法，对浑善达克沙地植被物候进行了提取，分析其时空变化，并利用研究结果数据，分析植被物候对高程和气象因子的响应.结果表明，2000~2019年间研究区的植被物候呈微弱波动趋势，浑善达克沙地植被返青期（SOS）主要集中在110~140d，枯黄期（EOS）主要集中在250~280d，整体呈微弱推迟趋向（0.28d/a），生长季长度（LOS）主要集中在120~170d，整体呈微弱延长趋向（0.23d/a）.在空间分布上，占研究区51.51%的区域植被SOS呈提前趋势；占研究区67.02%的区域植被EOS呈提前趋势，并且占研究区32.98%的区域植被EOS呈推迟趋势.占研究区62.71%的区域植被LOS呈延长趋势.在海拔900~1500m区间，随着海拔升高，SOS显著推迟，EOS不显著提前，LOS显著缩短.前一年11、12月和当年1、2、4月降水量对SOS有提前作用.6、7、8、9月份气温和降水都对EOS推迟有明显的作用.总的来说，浑善达克沙地植被物候与气候因子的相应规律比较复杂，表现出季节性的差别及地形的差异性.     

赤泥在控制沉积物磷释放中的应用研究

利用烧结法赤泥中富含Ca、Fe等金属元素的氧化物而具有吸附性的特点，通过室内模拟研究赤泥投加对沉积物中各种磷形态含量及分布比例的影响，进而探讨利用赤泥控制沉积物中磷释放的可行性。对经过处理后的沉积物磷形态分析后表明，投加赤泥能促使沉积物中铁铝磷向钙磷转化（Pearson相关分析，r=-0.892，P<0.01，n=9），且赤泥的强碱性使沉积物pH值逐渐升高。确定了赤泥最佳投加比例为5%，此时沉积物的pH为9.03，铁铝磷含量由初始的148 mg/kg降至107 mg/kg，占总磷比例也由18.1%降至13.4%，钙磷含量由486 mg/kg升至546 mg/kg，其占总磷比例则由60%增至68.7%，铁铝磷和钙磷之间的转化已基本完成，继续增加赤泥投加量对沉积物中磷形态间的相互转化影响甚微。由于铁铝磷较钙磷活性高而易释放，可见投加赤泥能降低沉积物中磷的释放风险。赤泥可以作为吸附材料被应用于沉积物磷污染控制技术中，为有效控制水体内源磷负荷提供一种新思路和廉价材料。     

Effect of lead on the sorption of 2,4,6-trichlorophenol on soil and peat

The effect of lead on the sorption of 2,4,6-trichlorophenol (2,4,6-TCP) on soil and peat was investigated using a batch equilibration method. Lead markedly diminished the sorption of 2,4,6-TCP, and 2,4,6-TCP had little effect on lead sorption. Peat was a more effective adsorbent for 2,4,6-TCP than soil. The desorption hysteresis of 2,4,6-TCP verified the presence of high-energy sorption sites. Mechanisms of lead suppression effect on the 2,4,6-TCP sorption included the following: Firstly, lead accelerated the aggregation of colloids, the aggregates covered the surface in part and shrunk the pore sizes of the adsorbents, hence decreased the sorption of 2,4,6-TCP. Secondly, X-ray absorption and Fourier transform infrared spectroscopy study suggested that lead competed with 2,4,6-TCP for carboxylic, phenolic and Si-OH groups of organic matter and clay minerals. Such competition was partly responsible for the overall suppression effect of lead on the sorption of 2,4,6-TCP.