Saturated and Unsaturated Water Flow in Inclined Porous Media

This paper considers the two-dimensional saturated and unsaturated flow of water through inclined porous media, namely a waste dump or hill slope. Since the partial differential equation governing this water flow transforms from being parabolic to elliptic as the water flow varies from unsaturated to saturated, an iterative, finite differencing scheme is used to develop a numerical solution. The model can be used to investigate the effects that hill slope angle, depth of soil cover and hilltop width have on water accumulation in the dump and the time required for saturation to occur at different areas in the dump domain. The accuracy and reliability of the computer based solution is tested for two different boundary conditions – (1) no flow on all boundaries (i.e., the internal redistribution of soil moisture to steady state) and (2) a constant rainfall flux on the dump surface. Numerical studies then show the effects of changing the hill slope angle, depth of layer, and dump geometry on the flow characteristics in the dump.     

重庆长寿地区垂直温度结构特征分析

本文根据在长寿地区进行的一系列大气边界层探空试验资料,分析了大气温度垂直结构特征以及与逆温有关的大气扩散条件。     

电除尘器粉尘层反电晕击穿厚度理论与试验

为了合理地确定静电除尘器清灰振打周期,通过理论与试验方法确定静电除尘器粉尘层反电晕击穿厚度很有必要的。首先基于静电学理论导出带电粉尘层内的电量分布和电场分布数学模型,然后根据粉尘层反电晕发生条件,得出粉尘层反电晕击穿厚度的计算式,结果表明,反电晕击穿厚度是粉尘比电阻、电晕电流密度及极配的函数。通过对高比电阻不同厚度的粉尘层的反电晕击穿试验研究,结果表明,各击穿点的连线呈较连续光滑的弧线,提出了利用伏安特性曲线确定粉尘层反电晕击穿厚度的简易图解法。     

The Influence of Synoptic-scale Air Flow and Local Circulation on the Dust Layer Height in the North of the Taklimakan Desert

The present study investigates the influences of synoptic-scale air flows and local wind circulations on the dust layer height (DLH) in the Taklimakan Desert, based on lidar observations performed in the north of the desert in March 2003. The DLH fluctuates approximately every three days between 2500 m (above sea level) and 5000 m, including diurnal variations. Meteorological analyses and numerical simulations show that the three-day fluctuation of DLH corresponds with variations in synoptic-scale air flows over the Taklimakan Desert, and the diurnal variations are linked to downdrafts and updrafts that are formed over the north of the desert as part of local circulations. When strong northerly winds prevail in the upper troposphere and a developed valley wind blows toward the Tienshan Mountains in the lower troposphere, the downdrafts strengthen in the middle troposphere over the north of the desert, lowering the DLH to about 2500 m. In contrast, the DLH rises to about 5000 m when the updrafts develop between strong southerly winds in the upper troposphere and a developed mountain wind blowing from the Tienshan Mountains. Simulations for the local circulation behavior without the presence of the Tienshan Mountains demonstrate that the valley and mountain winds on the southern slope of the Tienshan Mountains control the intensity of the downdrafts and updrafts, thereby influencing the DLH over the north of the Taklimakan Desert.     

Improvements in Air Quality Modelling by Using Surface Boundary Layer Parameters derived from Satellite Land Cover Data

Many atmospheric dispersion models include only simpletreatment of surface features to estimate the wind profilesand stability parameters. Detailed characterisation of theland cover, particularly in large and complex urbanconurbations, is especially important, as the surfacefeatures can vary significantly over the area. This paperdiscusses the use of satellite land cover data to derivespatially resolved surface boundary layer (SBL) parameters.These parameters have been used in an air quality model,PEARL (Prediction Air Quality in Urban and RegionalLocations) for estimating monthly and annual COconcentrations. Land cover data, derived from LANDSATThematic Mapper Imagery, has been used to estimate SBLparameters (surface roughness length, albeedo, Bowen ratioand anthropogenic heat flux) for a study area of 10000km² encompassing Greater London and the surroundingcounties. The SBL parameters have been assigned according tomajor land cover types for the whole area at a spatialresolution of 1 × 1 km. Predictions from two versions of the PEARL model (one with land cover data and one without)have been compared with each other and with measured data forannual and monthly CO concentrations from seven London airquality monitoring sites. This comparison shows thatdifferences between predicted and observed values can bereduced by up to a factor of three. The use of SBLparameters derived from land cover data also yields moredetailed predicted annual CO spatial patterns especially inand around suburban areas. The performance of both versionsof the model for monthly CO concentrations has been comparedwith a range of statistical measures. This comparisonconfirms that improved agreement is observed betweenmodelled and measured monthly CO concentrations when use ismade of spatially resolved SBL parameters.     

曲靖电厂灰渣性质及其用作水泥混合材的试验研究

在对粉煤灰及炉渣的主要物理、化学性质进行分析测试的基础上，对它们用作水泥混合材所表现出的性能及存在的问题进行了分析研究。     

长江中游砂山的磁组构特征及古气候环境意义

为了建立长江中游风成砂的磁组构识别标志,讨论磁组构参数与古气候、古环境之间的关系,对新近发现的江西九江新港砂山剖面进行了野外考察和磁化率定向样品的采集和测试,结果表明：①新港风成砂剖面中砂层和古土壤化的亚黏土层的磁组构参数值具有较大的不同,亚黏土层的磁化率（〖WTBX〗κ〖WTBZ〗）在剖面中表现为峰值（均值143.27（10-6SI））,各向异性度（〖WTBX〗P〖WTBZ〗）值却表现为曲线的较低值段。砂层却与亚黏土层相反,〖WTBX〗κ〖WTBZ〗值为谷值（均值为2181（10-6SI））,〖WTBX〗P〖WTBZ〗值总体为高值段,但波动较大。②在新港风成砂剖面中大多数亚黏土层样品的磁面理度（〖WTBX〗F〖WTBZ〗）值大于磁线理度（〖WTBX〗L〖WTBZ〗）,而砂层中只有部分样品的〖WTBX〗F值大于L〖WTBZ〗,说明亚黏土层的磁面理发育程度较砂层的要好。③相对于河流和湖泊沉积物（河流沉积物长轴的倾角一般小于10°,短轴的倾角大于80°）而言,新港剖面风成砂的磁化率量值椭球体的长轴的倾角较大（22°～24°）,短轴的倾角较小（45°～51°）。④新港剖面风成砂的磁基质颗粒度（〖WTBX〗q〖WTBZ〗）的平均值（0668 8）比长江中游河流沉积物的〖WTBX〗q〖WTBZ〗值（024）偏大,反映风成砂的分选较河流沉积物的要差。上述特点可作为长江中游水成和风成沉积物的磁组构识别标志。⑤在325～262 m的地层剖面中共有9层发育程度不同的古土壤化的亚黏土层,说明在这一期间气候不仅有9次由干冷向暖湿的转变,且每次变化的强度也有所不同。〖     

典型耐候钢在江津大气环境中暴晒1 a的腐蚀行为

目的 研究3种典型耐候钢在江津大气环境中暴晒1 a的初期腐蚀行为。方法 采用户外大气挂片、腐蚀质量损失、SEM、XRD、电化学等方法,研究Q355NH、Q460FRW、Q690的腐蚀速率、锈层形貌、锈层物相和锈层电阻,并与Q345碳钢进行对比。结果 耐候钢和碳钢在大气暴晒初期的腐蚀规律是一致的,Q355NH、Q460FRW、Q690和Q345碳钢的腐蚀速率分别为0.050 9、0.053 6、0.047 8、0.055 mm/a,Q690的腐蚀速率最小,约为碳钢的87%。耐候钢和碳钢的锈层都主要由α-FeOOH、γ-FeOOH和Fe₂O₃组成,耐候钢的锈层更致密,裂纹更少。Q355NH、Q460FRW、Q690的锈层电阻值分别为821.3、1 005、1 080?·cm²,碳钢为101.68?·cm²,耐候钢的锈层电阻值约为碳钢的10倍。Cr和Cu元素在耐候钢的锈层中富集明显。结论 耐候钢的腐蚀速率低于碳钢,3种耐候钢的耐蚀性顺序为Q690>Q355NH>Q460FRW。Cr和Cu元素在...     

汽车环境风洞地面区域流场数值仿真

目的 探究汽车环境风洞地面区域流场规律,获取风洞边界层抽吸装置的最佳抽吸率和底盘测功机对风洞地面区域边界层厚度、风速、总压和静压的影响规律,并比较MRF法和旋转壁面法对底盘测功机转毂转动模拟的精度。方法 运用计算流体动力学方法对汽车环境风洞流场进行数值仿真计算。结果 边界层抽吸装置对应于喷口风速120 km/h时的最佳抽吸率为0.048。底盘测功机区域总压呈现下降趋势。相比于存在底盘测功机,汽车环境风洞无底盘测功机时,底盘测功机区域内相同位置的边界层厚度会增加1.28～12.22 mm。在前转毂的前侧、上侧、后侧和后转毂的上侧和后侧会有一个高风速区域,区域内风速比设定风速高1%～4%,与无底盘测功机相比,区域内静压值低0.32～46.02 Pa。在前后转毂前侧和后侧与地面相连接的凹部会有一个低风速区域,区域内风速比设定风速低1%～5%,与无底盘测功机相比,区域内静压值高0.08～49.34 Pa。底盘测功机转毂的转动会使附近区域的地面边界层厚度变大。在前转毂前侧,采用旋转壁面法进行模拟比MRF法地面边界层厚度增加近8 mm,而在其他位置,2种模拟方法对边界层厚度的模拟差别在1.5 mm...