2006~2010年珠三角地区SO2特征分析

对广州番禺大气成分站2006~2010年期间的SO2资料进行了分析,讨论了珠江三角洲(珠三角)地区地面SO2体积分数的年、季节、月、日变化特征和概率的分布特征.珠三角地区地面SO2变化特征的分析结果表明,2010年地面SO2体积分数的总体水平相对近年来有一定下降,高浓度事件发生频率降低;冬、春季SO2各项统计值要高于夏、秋季,干季明显高于湿季,可能与大气边界层高度和太阳辐射等因素的季节性变化相关;SO2干湿季的日变化趋势相仿,日最高峰时间相同,只是湿季达次高峰和最低点的时间比干季要提前1 h,这可能与季节性的大气边界层高度和辐射强度变化,以及日照时间长度有关;SO2体积分数的概率分布特征比较复杂,各月谱型分布各有不同,可能与季节性因素的变化规律相关.     

2015年干季佛山一次重空气污染过程形成机理研究

2015年12月21-23日,广东珠三角佛山地区出现了一次PM_2.5重污染过程.利用佛山地区顺德、禅城、三水3个站点风廓线雷达、激光雷达和微波辐射计观测资料,结合地面气象观测数据和污染物浓度数据,分析研究了这次重污染过程的形成机理.结果表明：1形成这次污染过程的主要原因是近地层偏南风和偏北风对峙导致水平风速减小,大气水平输送能力变差;持续时间长且强度达到3℃·km^-1的强逆温抑制了污染物的垂直扩散;800 m以下超过90%的高相对湿度造成气溶胶粒子吸湿增长显著.2持续时间长且比较深厚的小风层是造成这次污染过程的直接原因,小风层厚度是预报空气质量变化的较好工具.与地面风速相比,PM_2.5浓度与小风层厚度的相关系数最多能提高0.36,且具有较长的预报时效.佛山地区小风层的风速阈值为3.8 m·s^-1.3这次污染过程存在两种不同的污染形成机制,污染前期（21-23日中午）主要以本地污染物累积为主,污染后期（23日下午）下风向地区（三水）的污染主要是受上风向地区（顺德和禅城）的污染输送影响.     

桉树叶提取液还原石墨烯电极提高微生物燃料电池产电性能的研究

将桉树叶提取液绿色还原氧化石墨烯(G-rGO)电极和微生物还原氧化石墨烯(B-rGO)电极依次作为微生物燃料电池(MFC)阳极,采用红外光谱(FTIR)、X射线衍射(XRD)、扫描电镜(SEM)对所制备的电极进行表征,并采用循环伏安法(CV)、交流阻抗法(EIS)对比2种电极的电化学性能.结果发现,G-rGO阳极的内阻为243.87Ω,应用于MFC时最大功率密度和最大输出电压分别为18.77 W·m~(-3)和760 mV,对照组B-rGO电极的内阻为299.11Ω,将其应用于MFC时最大功率密度和最大输出电压分别为13.16 W·m~(-3)和635 mV,对照组未修饰阳极的内阻为375.21Ω,最大功率密度和最大输出电压分别为8.97 W·m~(-3)和480 mV.研究表明,G-rGO电极电阻更小,导电性能更优越.     

佛山地区干季边界层垂直风温结构对空气质量的影响

利用佛山地区2013年12月大气边界层观测试验得到的垂直风温资料和相应逐日AQI资料、逐时PM_(2.5)浓度资料,研究了佛山地区大气边界层垂直风温结构对空气质量的影响.结果表明:佛山地区干季持续存在的逆温结构是导致PM_(2.5)污染较重的重要原因.干季污染日近60%的最低逆温层高度低于1000 m,而非污染日低于1000 m的最低逆温层仅占36%,污染日佛山贴地逆温频率高达31.2%.逆温层出现高度较低,将污染物压缩积累在贴地层大气中导致污染较重.在大陆冷高压控制下,佛山地区的边界层结构演化非常典型,最大边界层高度和最大边界层通风量表现出了显著相关,污染日日平均边界层高度始终维持在较低的水平,多数时候不足500 m,最大边界层高度则大部分小于1000 m,日平均边界层通风量主要分布在500~1500 m~2·s~(-1)之间,在极端情况下甚至不足300 m~2·s~(-1),最大边界层通风量大部分处于1500~5000 m~2·s~(-1)之间,导致污染物始终聚集在较低的大气边界层内,使得PM_(2.5)浓度长时间维持在较高的污染水平.佛山地区风场存在显著的3层结构,较小的底层风速意味着大气的输送和扩散能力较弱,高度较低的中层使得污染物进一步被压缩累积在大气底层,垂直风场的不稳定性使得污染日佛山地区局地回流活跃,回流(RF)指数极小值多分布在0.2~0.4之间,污染日RF指数普遍小于非污染日,垂直风场的有效输送能力被显著削弱.     

GIS环境下大区域工程场地地震液化势的二维概率评价方法

用具有概率意义的饱和砂土抗液化强度经验公式来对大区域场地进行地震液化势二维概率评价;在GIS软件ArcGIS的支持下,将取样钻孔处的液化势评价结果等价于数字高程模型(Digital Elevation Model,DEM)中的高程,利用ArcGIS空间分析模块中的Kriging插值法估计大区域场地的地震液化范围。研究表明:将Kriging法应用于岩土工程地质特征的统计推断,有助于揭示勘探孔以外的地层信息,对于大区域场地地震液化范围的判别是一个较好的手段;利用ArcGIS空间分析模块中的Kriging法,通过已勘察点的信息(液化势)来估计未勘测点的土层液化势,能够较好地区划出场地地震液化势的空间分布特征。     

黄孢原毛平革菌处理染料废水过程中细胞结构损伤效应研究

利用透射电子显微镜观察分析白腐真菌(黄孢原毛平革菌)在处理染料废水活性艳红X-3B过程中,染料和盐度对黄孢原毛平革菌的细胞结构产生的毒性作用.结果表明:活性艳红X-3B染料对黄孢原毛平革菌产生生物毒性作用,且随着染料浓度的增加,细胞受损伤程度不断加深.加入100 mg/L的染料活性艳红X-3B后,黄孢原毛平革菌菌丝细胞形态发生变化,出现质壁分离现象;染料浓度进一步加大,菌丝细胞超微结构受到损伤逐渐严重.染料废水中的盐度对黄孢原毛平革菌细胞也会造成损伤,且损伤程度随盐度增大而增大.NaCl浓度为3 g/L时,菌丝细胞发生质壁分离;而当NaCl加入量高于8 g/L时,细胞膜受损,线粒体、细胞核呈现空泡化,表现为受到不可逆的损伤.染料和盐双因子对黄孢原毛平革菌细胞的损伤效应表现为其损伤程度与单因子作用一致,且染料的影响作用占主导.     

Effect of selected organic and inorganic snow and cloud components on the photochemical generation of nitrite by nitrate irradiation

The effect of selected organic and inorganic compounds, present in snow and cloudwater was studied. Photolysis of solutions of nitrate to nitrite was carried out in the laboratory using a UVB light source. The photolysis and other reactions were then modelled. It is shown that formate, formaldehyde, methanesulphonate, and chloride to a lesser extent, can increase the initial formation rate of nitrite. The effect, particularly significant for formate and formaldehyde, is unlikely to be caused by scavenging of hydroxyl radicals. The experimental data obtained in this work suggest that possible causes are the reduction of nitrogen dioxide and nitrate by radical species formed on photooxidation of the organic compounds. Hydroxyl scavenging by organic and inorganic compounds would not affect the initial formation rate of nitrite, but would protect it from oxidation, therefore, increasing the concentration values reached at long irradiation times. The described processes can be relevant to cloudwater and the quasi-liquid layer on the surface of ice and snow, considering that in the polar regions irradiated snow layers are important sources of nitrous acid to the atmosphere. Formate and (at a lesser extent) formaldehyde are the compounds that play the major role in the described processes of nitrite/nitrous acid photoformation by initial rate enhancement and hydroxyl scavenging.     

气浮过滤法处理印染废水

高效气浮工艺是处理印染废水的有效方法,通过在溶气罐中使用高效填料、优化设计溶气释放器及使用双层快滤,可大大提高处理效果。     

The sands of Forvie (Scotland): A case study in geomorphology and conservational management

The Sands of Forvie, National Nature Reserve, Scotland is a complex coastal sand dune system which is associated with the dynamic estuary of the River Ythan. The dune system has developed over more than 5000 years. The south part is a peninsula of dunes, sand hills, sand arcs, erosion and deflation surfaces. The north part is superimposed on a rock plateau with a cliff coastline. This plateau is covered in glacial deposits and is essentially an upland heath landscape. Some of the best examples of large active parabolic dunes in Britain are found in North Forvie. The sequence of geomorphic development is described. As a nature reserve with a rich ecology it has been managed for conservational purposes since 1960s. As such it is an excellent case study of how conservational management has changed to become more flexible and more aware of the importance of dynamic processes.     

A conceptual approach to model sand–gravel extraction from rivers based on a game theory perspective

Sand–gravel mining is a significant parameter of economic development and social welfare function in modern societies. As demand for aggregate increases in construction industry, conflicts for the availability of the resource and environmental impacts become more intense. The present paper describes the contested status quo in riverbed sand–gravel mining activities with an example from Greece, as a case study. The scope is to propose a methodology about good governance of the mining sector that promotes a sustainable sharing of aggregate resource by securing environment and safekeeping revenues in the mining trade market.