生物陶粒流化床-污泥滤层脱氮工艺的试验研究

采用生物陶粒流化床-污泥滤层工艺对含氮有机废水处理进行试验研究,研究结果表明:系统内可固着生长不受抑制的硝化菌种群,氨氮去除率可以达到93%￣95%;三相分离区形成稳定的污泥滤层,可使总氮去除率得以显著提高;当HRT为1.5h,曝气量为0.25m3/h,BOD容积负荷为9.2～10.4BOD5/m3.d,总氮容积负荷0.65kgTN/m3.d条件下,可得到BOD5的去除率85%,总氮去除率74%的处理效果。     

生物反应器填埋场渗滤液及其处理对策

根据垃圾的降解和稳定机理分析了生物反应器填埋场渗滤液的动态变化规律，并对其处理对策进行了探讨。生物反应器填埋场前期产生的渗滤液可全部回灌，后期再根据实际情况排放处理部分过量的渗滤液。在对渗滤液水量和水质全面直观认识后，再对生物反应器填埋场渗滤液处理工艺进行针对性的选择和设计，并宜采用物化法处理方式。     

城市垃圾渗滤液场内循环处理的探讨

本文对城市垃圾渗滤液的产生量、水质特征及其影响因素进行了分析，介绍了当前国内外垃圾渗滤水场内循环处理的两大研究流派-以欧美国家为主的生物反应器填埋技术和以日本为主的循环式准好氧填埋技术。根据我国城市垃圾有机物含量高的特点，提出了适合我国国情的、将准好氧填埋技术与生物反应器填埋技术特点相结合的城市垃圾填埋场渗波液场内循环处理的设计思路。     

小型炭素焙烧炉沥青烟气净化技术初探

阐述了颗粒层吸附技术在小型炭素焙烧沥青烟气净化中的应用。     

垃圾填埋场封场工程施工安全措施

对生活垃圾填埋场封场工程施工过程中的防火防爆问题进行了探讨，并介绍了主要对应措施。     

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.     

厌氧-准好氧型填埋的渗滤液实验研究

通过室内模拟试验，在渗滤液回灌的厌氧填埋柱基本进入稳定状态后，改用准好氧运行方式。同时监测了渗滤液中有机物浓度以压温度、pH值的变化。改变模拟垃圾柱的运行方式两个月以后。氨氯浓度由2000mg／L迅速下降至101．48mg／L，试验结果显示，准好氧运行方式可以解决生物反应器填埋场进入稳定阶段后存在的氨氮浓度高的问题，加速填埋场的稳定。     

"地球表层"再讨论

对"地球表层概念"的界定与发展和基于新概念的地球表层系统(结构)等进行了综合讨论和阐述;定义了地球表层概念的内涵,提出:地球表层是指地表和近地表各圈层相互作用和渗透的地球部分,是地球上部多态(固、液、气、生物和有机态)物质相互渗透、交融并不断进行物能交换、转化和作用而结合形成的具有内部协同性和一定系统结构的有机整体,是地球生物的生存环境和地表生态系统发生、发展和演化的基础;进一步确立了地球表层的空间位置和范围(外延),即包括地球表面上下的岩石圈、水圈、大气圈、生物圈和物理(能量)场及其相关作用在内的地球空间,其下界是软流圈(以软流圈为过渡层),上界为大气圈最外层,至少应包括磁层在内;岩石圈以下的地幔和地核与大气圈以外的宇宙空间均为地球表层的环境.     

垃圾填埋场渗滤液回流技术研究进展

垃圾填埋场渗滤液回流能有效降低渗滤液中污染物的浓度，提高填埋场稳定化程度，具有广泛的应用前景。本文综述了国内外学者对该技术的研究情况，包括技术特点及相关机理、渗滤液特性研究及回流效果的影响因素，指出了该技术现存的不足之处和尚待解决的理论和技术问题。     

上保护层开采瓦斯综合治理的试验研究

借助于一般的保护层开采理论,对上保护层开采合理参数和保护范围进行了综合分析研究,结合潘东公司具体情况设计了试验方案,现场试验结果表明了该方案的合理性,同时也表明上保护层开采对下临近突出煤层的突出危险消除效果明显,上保护层开采带来的经济和社会效益十分显著。试验结果对类似开采条件的矿井防治煤与瓦斯突出及瓦斯综合治理具有一定指导意义。