含硫酸盐高浓度有机废水预处理的试验研究

在含硫酸盐高浓度有机废水浸泡铁刨花的静态试验的基础上，进行了“铁床”处理高浓度糖厂生产废水的动态试验。通过稳定工况之后，“铁床”CODcr平均下降41．3％，SO4^2-平均下降56．2％，有利于后续厌氧生物处理，并达到以废治废的目的。     

加压曝气生物反应器及其工艺设计

介绍了加压曝气生物反应器及其处理系统的工艺设计 ,包括反应器原理、工艺流程、运行参数 ,工艺设计特点等     

微量营养物质对有机废水厌氧消化过程的调控作用

通过向处理酸性葡萄酒蒸馏废水的厌氧移动床生物膜反应器中投加微量营养物质的试验,得出利用微量营养物质调控厌氧消化过程在技术上是可行的。Fe、Ni、Co组合不仅能加快挥发性有机酸(VFA),特别是丙酸的降解速率,进而提高厌氧反应器的溶解COD去除率,同时,还有利于厌氧反应器有机负荷的快速提升和较强pH缓冲能力的形成。B族维生素对厌氧移动床生物膜反应器运行效果影响不大。Fe对厌氧移动床生物膜反应器运行有一定影响,但效果也不十分明显。     

一种新型复合式生物流化反应器混合特性的研究

对新型蜂窝状断面复合生物流化反应器进行了液体循环速率和水力停留时间分布曲线的测定，实验表明新型反应器具有抗冲击负荷强，接近CSTR反应器的特点，反应器随气量增大、载体投加量减少和进水量减少而更近似于CSTR反应器，通过理论分析，证明了影响液体循环速率的参数主要有气体流量(气含率)、反应器沿程和局部阻力系数以及Ad/Ar，并且得出液体循环速率与反应器高度的0．5次方成正比。     

利用PCR-DGGE技术分析生物陶粒硝化反应器中微生物群落动态

为了揭示生物陶粒硝化反应器中活性污泥的微生物种群多样性,从运行不同时期的反应器中提取活性污泥,利用PCR-DGGE技术初步分析了生物陶粒反应器细菌的种群演替情况.结果表明,随着进水COD值的逐阶段降低,氨氮去除率逐步提高到64.38%.群落结构和优势种群的数量具有时序动态性,微生物多样性与废水的处理效果出现协同变化的特征.测序结果表明,生物陶粒反应器中运行第21天的优势种群除了自养细菌,还有异养细菌存在.其中自养细菌为Nitrosospira.sp和Nitrobacter.sp,异养细菌为Bacillus.sp、Pseudomonas.sp和Pseudochrobactrum.sp.     

脉冲电晕放电治疗有机废气的研究—放电反应器结构

对脉冲电晕法治理甲苯有机废气进行了实验，考察了放电反应器结构及参数对其性能的影响。结果表明，对线－筒式反应器，当直径较小时，去除率较高，但易发生火花放电，实验条件下直径２０ｍｍ的反应器效果较好。若采用陶瓷管反应器，其效果较金属管明显提高，脉冲峰值电压Ｖｐ为４２ｋＶ时，可使甲苯的去除率由４０％提高到６１％左右。对线－板式反应器，放电间隙越大，甲苯的去除率越低，使用陶瓷板反应器可使甲苯去除率明显提高，     

序批式活性污泥法在炼油化工废水处理中的应用

炼油化工废水处理的传统处理工艺中存在一定的弊端。为此,玉门炼油化工总厂对其废水处理设施进行了改建和扩建,其生物处理系统采用了序批式活性污泥法处理工艺。经过 3年运行的结果表明:该系统运行效果良好,处理后的水质可达到《GB8978-1996》(石化)一级排放标准的要求;化学需氧量(COD)和生化需氧量(BOD)分别降低78.6%和91.2%,硫化物去除率为98.2%,挥发酚去除率为99.6%。而且该反应器具有较强的耐冲击负荷能力,进水中COD在600 mg/L以下且有大幅度波动时,该系统仍可稳定地运行,处理后的水可达标排放。     

移动床生物膜反应器充氧能力的试验研究

对移动床生物膜反应器的充氧能力进行了试验研究，结果表明：反应器充氧能力在添加填料比无填料时大；在悬浮载体能够均匀流化的填充率范围内，反应器充氧能力随着填充率的增大而增大；当填充率大于可以均匀流化的最大填充率时，反应器的充氧能力略有下降。     

Numerical Simulation of Synoptic Condition on a Severe Sand Dust Storm

By using observational data and MM5, an observational analysisand numerical study was conducted on the synoptic condition of a severe dust storm that was caused by a Mongolian cyclone whichoccurred from 6 to 8 April 2001. Results illustrated thatthe cyclogenesis was due to the isentropic potential vorticity (IPV) advection in the upper troposphere and the terrain modifiedbaroclinicity in the mid-lower troposphere. The Altai-Sayan complex of mountains blocked the lower level cold air and made the isentropic surface sharply steep. When the air slid down along the isentropic surface the increasing of baroclinicity anddecreasing of stability blew up the vertical vorticity development.The formation of the dust storm was a result of a cyclonic cold front passing across the area. The occurrence of this dust stormwas closely related to the strong surface wind, which was accompanied by a cold front passing, rather than the cyclogenesis, itself. Hence, the reason for the pre-front dust storm formulation was the formation of heating convection. Reasons behind the formation of a black storm (visibilitylower than 50 m), which occurred in the mid-north part ofInner Mongolia, lay in several aspects. Firstly, in thisarea the surface wind was strong, a direct result of thedownward transport in mid-lower troposphere. Secondly,the cold front passed over the effected area near sunsetso the air obtained much more surface heating to form adeeper mixed layer (ML). Thirdly, cooperation between thelower level wind and the terrain made the atmosphere inthis area and acquired the maximum advective contributionnecessary to form a deep post-front ML. The sensitivityexperiment revealed that surface heat flux was important to the frontal lifting. In addition, the forcing of surface heating wasalso seen as the primary forcing mechanism of frontogenesis. Meanwhile, removal of the surface heat flux made the atmosphericstratification became stable and the pre-storm ML very shallow,which weakened the strength of the dust storm.