【摘 要】
:
Ultrafine particles(UFPs)are harmful to human beings,and their effective removal from the environment is an urgent necessity.In this study,a dielectric barrier
【机 构】
:
School of Environmental and Safety Engineering,Advanced Plasma-Catalysis Engineering Laboratory for
论文部分内容阅读
Ultrafine particles(UFPs)are harmful to human beings,and their effective removal from the environment is an urgent necessity.In this study,a dielectric barrier discharge(DBD)reactor packed with porous alumina(PA)balls driven by a pulse power supply was developed to remove the UFPs(ranging from 20 to 100 nm)from the exhaust gases of kerosene combustion.Five types of DBD reactors were established to evaluate the effect of plasma catalysis on the removal efficiency of UFPs.The influences of gas flow rate,peak voltage and pulse frequency of different reactors on UFPs removal were investigated.It was found that a high total UFP removal of 91.4%can be achieved in the DBD reactor entirely packed with PA balls.The results can be attributed to the enhanced charge effect of the UFPs with PA balls in the discharge space.The UFP removals by diffusion deposition and electrostatic attraction were further calculated,indicating that particle charging is vital to achieve high removal efficiency for UFPs.
其他文献
Plasma activated water(PAW)was prepared for 10 min to be applied one tofive times as a foliar spray to rice plants,to investigate plant growth,yield and the concentrations of total soluble protein and sugar in the rice grains produced.The results reveal th
近年来,非常规页岩油气勘探开发的成功,为获取油气资源指出了新方向,同时提醒石油地质家重新审视传统的油气地质理论,需要将页岩油气的地质认识进展与传统的油气地质理论结合起来形成新的含油气系统理论。本文基于从常规与非常规在生烃、储层方面的研究进展,初步探讨涵盖常规和非常规的统一的含油气系统和二者协同的勘探思维。生烃研究由以往主要关注生油气高峰时的生烃量延伸到对油气生成、排出、滞留全过程的刻画;储层研究由关注无机矿物成岩演化中形成的米级—毫米级无机孔隙向成岩作用—成烃协同作用形成的微米级—纳米级有机质孔隙延伸;在
《中国扬子区兰多维列统特列奇阶及其与英国的对比》一书(陈旭和戎嘉余,1996)有以下结论:①将回星哨组、茅山组、西坑组等的层位归属于特列奇阶上部;②将回星哨组、茅山组及其相当地层与英国特列奇阶对比;③将扬子区特列奇阶的顶界置于回星哨组、茅山组及其相当地层之顶;④将回星哨组、茅山组、西坑组等地层资料编制的古地理图称为特列奇期晚期古地理图;⑤将回星哨组、茅山组、西坑组等地层与上覆中泥盆统—中二叠统之间的不整合面代表的上升运动,称为“特列奇期的扬子上升”。笔者等依据多年对扬子地台志留纪地层剖面的实地考察和近数十
热储温度是开展地热资源研究的关键参数之一。地热勘查中常用基于地热流体化学和同位素数据的经验公式来评价没有钻孔或者钻孔未达到实际热储层情况下深部热储的温度。SiO2地温计应用最为广泛,对于发生了绝热沸腾的地热流体,通常采用Fournier等提出的100℃沸腾条件下的校正公式。考虑到海拔会影响沸点,本文从SiO2溶解度方程和温度相关性着手,评价了SiO2地温计沸腾校正方法在高原地区的适用性。结果表明Fournier(1977)及Fournier
The phase shift characteristics reflect the state change of electromagnetic wave in plasma sheath and can be used to reveal deeply the action mechanism between
南华盆地成冰系大塘坡组锰矿是我国最重要的锰矿产出层位之一,它形成于成冰纪Sturtian冰川事件之后,其成矿背景及形成机理一直是研究的重点。在系统总结Sturtian冰川事件起始与结束时间、南华裂谷盆地结构演化及古气候演变等重大地质事件的最新研究进展的基础上,综合分析了南华盆地大型沉积型锰矿成矿作用过程与这些重大地质事件之间的联系。揭示了南华盆地Sturtian冰期的启动和结束与全球其他地区基本一致,分别发生在~717 Ma和~660 Ma之前。同时,对南华系大塘坡锰矿成矿时代进行了约束,大约形成于~66
The dielectric barrier discharge(DBD)in air at atmospheric pressure is not suitable for industrial applications due to its randomly distributed discharge filame
黄绿山地区位于柴达木盆地北缘造山带西段,区内花岗岩广泛分布,相对匮乏同位素的研究成果以及岩浆活动和变质作用的地质记录。本文对前人在地质填图中认为原属于华力西期的奥长花岗斑岩侵入体进行岩相学、年代学、地球化学和全岩Sr-Nd同位素研究,探讨其成因类型和源区,并在此基础上讨论了其地球动力学意义。LA-ICP-MS锆石U-Pb定年结果显示,黄绿山奥长花岗斑岩结晶时代为466±3 Ma,为加里东期中奥陶世的产物。样品具有高SiO2和Na2O,低K2
根据历史文献记载及档案查询,追寻中国地质学会成立时期的初心,传播科学精神,激励新时代地质人牢记使命,为实现中国梦努力奋斗。
在经历了漫长的飞行后,我国"天问一号"火星探测器按照预定计划成功降落在火星表面。"天问一号"负责执行的任务充满艰辛和挑战,它的成功实施标志着我国在深空探测领域向前迈进了一大步。经"祝融号"火星车(由"天问一号"搭载)发回的遥测信号确认,"天问一号"火星探测器的着陆巡视器于2021年5月15日7时18分,成功着陆于火星乌托邦平原南部。当时,远在3.2亿千米外的北京航天飞行控制中心的指挥大厅顿时掌声雷