特强沙尘暴灾害性天气的研究及展望

总结特强沙尘暴天气的研究进展,梳理分析特强沙尘暴天气的基本特征以及动力学触发机制,提出进一步的研究问题,以期加深对特强沙尘暴天气过程机理的认识.分析结果表明特强沙尘暴天气事件的季节性分布特征显著,春季居多,且多发生在下午到傍晚时段,其典型特征为突发性、局地性,持续时间相对较短,对局地的大气环境质量短时产生重大影响.旺盛的地面混合层热对流胞运动和中尺度（反）气旋性涡旋过境是特强沙尘暴天气出现的必要条件.在沙尘源区,由于午后近地层温度升高,热对流加剧,近地层热层结极不稳定,易形成地面混合层热对流胞运动;沙尘源区的热对流胞与混合层上部的中尺度（反）气旋性涡旋耦合作用,涡量通过热对流胞下传促使近地层层结内的热对流胞发展成群发性旋转对流胞,特强沙尘暴天气出现.进一步理解特强沙尘暴的风沙流特征及能量快速耗散机制,提高预测预警能力,需要加强特沙尘暴的气象观测数据积累和多尺度数值模拟.     

Influence of particle size on the aggregation behavior of nanoparticles: Role of structural hydration layer

More and more attention has been paid to the aggregation behavior of nanoparticles, but little research has been done on the effect of particle size. Therefore, this study systematically evaluated the aggregation behavior of nano-silica particles with diameter 130–480 nm at different initial particle concentration, pH, ionic strength, and ionic valence of electrolytes. The modified Smoluchowski theory failed to describe the aggregation kinetics for nano-silica particles with diameters less than 190 nm. Besides, ionic strength, cation species and pH all affected fast aggregation rate coefficients of 130 nm nanoparticles. Through incorporating structural hydration force into the modified Smoluchowski theory, it is found that the reason for all the anomalous aggregation behavior was the different structural hydration layer thickness of nanoparticles with various sizes. The thickness decreased with increasing of particle size, and remained basically unchanged for particles larger than 190 nm. Only when the distance at primary minimum was twice the thickness of structural hydration layer, the structural hydration force dominated, leading to the higher stability of nanoparticles. This study clearly clarified the unique aggregation mechanism of nanoparticles with smaller size, which provided reference for predicting transport and fate of nanoparticles and could help facilitate the evaluation of their environment risks.     

城区与郊区PM2.5污染及传输特征差异性

基于云高仪激光雷达、飞机AMDAR数据和常规站点等多源观测数据,并与数值模拟（CAMx-PSAT模型）相结合,以京津冀典型城市——北京城区与郊区（密云）和石家庄城区与郊区（平山）为案例研究区域,对城区和郊区边界层高度差异（ΔPBLH）、地面PM_2.5浓度差异（ΔSurf_PM_2.5）、高空PM_2.5浓度差异（ΔVert_PM_2.5）和传输通量强度及高度分布特征差异进行分析.结果表明,由于人为热源、短波辐射和热力湍流等因素,导致城区年均边界层高度（PBLH）较郊区高8%~29%,且不同季节下城区PBLH月均较郊区高2%（石家庄4月）~47%（北京7月）.由于人为排放、逆温和大气湍流等共同作用,在0~1260 m之间等高度城区年均ρ（PM_2.5）较郊区高0.1（石家庄）~29.7（北京）μg ·m^-3,随高度增加而减小.城区年均总净通量强度远大于郊区,城区表现为流出,郊区表现为流入,是由于城区低压和郊区高压,形成城郊热力环流.北京城区和郊区与周边的年均总净通量强度之和（44.77 t ·d^-1）大于石家庄（34.44 t ·d^-1）.受风速和PM_2.5浓度的影响,在0~1260 m之间,城区和郊区与周边的净通量随离地高度的增加通量强度呈现明显增大趋势,其中1月城区和4月郊区与周边的传输交换对环境影响最为明显.不同季节下城区和郊区最大净通量的强度差异明显,两者相差2.23~4.48倍;但最大净通量强度的高度特征差异较小,主要位于611~1260 m.     

Partial trisomy 20p resulting from recombination of a maternal pericentric inversion: case report of a prenatal diagnosis by chorionic villus sampling

We report a case of prenatal diagnosis of trisomy 20p resulting from a maternal pericentric inversion. The diagnosis was confirmed on both chorionic villi and amniotic cells. This case underlines the fact that prenatal ultrasound diagnosis of this structural anomaly is difficult. The only early sonographic feature was increased nuchal translucency. Copyright © 2006 John Wiley & Sons, Ltd.     

膜生物反应器生物降解与膜分离共作用特性研究

膜生物反应器实质是生物降解与膜分离相互影响,共同作用的过程,污泥浓度与通量之间存在一定的相关关系,膜分离对生和性能尤其是细菌活性有着重要的影响,而生物反应器内细菌胞外聚合物,溶解性有机物及微细胶体可能成为形成凝胶层导致通量下降的主要因素。     

不同温湿度条件下微米硼的氧化过程研究

目的 探究不同温湿度条件下微米硼的氧化层结构特征。方法 利用高温水浴浸泡处理去除原料微米硼的表面氧化层,然后在恒温恒湿条件下对微米硼进行加速氧化,利用扫描电子显微镜、透射电子显微镜和X射线光电子能谱对加速氧化后硼颗粒的氧化层厚度及组成进行分析,总结表面氧化层结构及成分组成变化规律,揭示温湿度条件下微米硼的氧化机制。结果 微米硼经高温水浴浸泡处理后,表面氧化层去除率达到50%。随着加速氧化时间的延长,硼颗粒氧化层的厚度逐渐增大,由内向外硼颗粒表面可以用B-BxOy-B2O3三层结构来表示,BxOy总是伴随着B2O3同时出现的,且随着氧化反应的进行,颗粒表面BxOy的含量将超过B的含量。结论 不同温湿度条件下微米硼的氧化机制为O2向B颗粒内部单向扩散的反应机制,B先与O2反应,形成低氧化物BxOy,BxOy进而与O2反应生成B2O3。随着氧化层厚度的增加,O2向B颗粒内部扩散的阻力增大,氧化反应速率随之降低。相比湿度的影响,温度的升高可显著加快硼表面氧化层的形成;温度一定时,湿度的增加可促进硼氧化层的形成。     

兰州冬季城市烟雾层辐射效应的观测分析研究

冬季兰州城市上空形成浓厚的烟雾层。利用1990年11月兰州大学和离城市地面625m高南山顶的辐射和探空资料,分析和计算了烟雾层的辐射效应。兰州城市烟雾层具有浑浊度系数大波长指数小的特点。对到达地面的太阳辐射有很强的削弱。浑浊度系数最大时,烟雾层内的平均加热率为6.16℃/d,。大气层对各波段的消光强弱不同,对可见光削减最大。同时烟雾层使到达兰州地面的大气逆辐射比南山顶增加5.2％,总的入射辐射比南山顶小5.6％,地面辐射差额比南山顶小67.8％。烟雾层的存在增加了城市边界层的稳定性。     

Influence of floc dynamic protection layer on alleviating ultrafiltration membrane fouling induced by humic substances

Cake layer formation is inevitable over time for ultrafiltration (UF) membrane-based drinking water treatment. Although the cake layer is always considered to cause membrane fouling, it can also act as a “dynamic protection layer”, as it further adsorbs pollutants and dramatically reduces their chance of getting to the membrane surface. Here, the UF membrane fouling performance was investigated with pre-deposited loose flocs in the presence of humic acid (HA). The results showed that the floc dynamic protection layer played an important role in removing HA. The higher the solution pH, the more negative the floc charge, resulting in lower HA removal efficiency due to the electrostatic repulsion and large pore size of the floc layer. With decreasing solution pH, a positively charged floc dynamic protection layer was formed, and more HA molecules were adsorbed. The potential reasons were ascribed to the smaller floc size, greater positive charge, and higher roughness of the floc layer. However, similar membrane fouling performance was also observed for the negative and positive floc dynamic protection layers due to their strong looseness characteristics. In addition, the molecular weight (MW) distribution of HA also played an important role in UF membrane fouling behavior. For the small MW HA molecules, the chance of forming a loose cake layer was high with a negatively charged floc dynamic protection layer, while for the large MW HA molecules it was high with a positively charged floc dynamic protection layer. As a result, slight UF membrane fouling was induced.