Measurements,Theories and Simulations of Particle Deposits on Super-Heater Tubes in a CFB Biomass Boiler

The present investigation involves theories, simulations and experiments on deposit layers on super-heater tubes in a circulating fluidised bed in Västerås in Sweden. Simulation of particle trajectories in the vicinity of two super-heater tubes is conducted in a Eulerian-Lagrangian mode for the flue gas and the ash particles from the combustion process. Particle impingements on the tubes are investigated for different particle sizes. Measurements of the buildup of deposit layers in the super-heater environment are conducted using a deposit probe. Deposit layer growth and growth rate is analysed for different probe temperatures, as well as the aspect of sintering on the probe ring surface. Analysis of the probe deposit material and deposits from the super-heaters and from textile filters are chemically analysed. The temperature dependence of the deposit materials viscosity is predicted from the chemical analysis of the samples. A model is included to simulate the effect of the deposit layer thickness on the tube heat exchange. The results from the particle trajectory simulations show that particle larger than 10 mm will mainly impinge on the front of the first tube and that smaller particles are more dispersed due to turbulence and thermophorectic forces, enabling a more even impingement on the whole surface of the tubes. The probe deposit layer growth measurements show significant temperature dependence. The deposit material sintering and distribution is proven to be dependent on; temperature, particle size and exposure time. The stickiness of the deposit material is shown to be dependent on the SiO₂ and alkali relation in the samples, estimated through a viscosity model.     

重金属铊在典型排放源周边大气颗粒物中的形态及来源分析

采用分级提取法,考察了某典型排放源周边大气颗粒物(PM_(10)、PM_(2.5))的形态分布特征,同时采用富集因子法和因子分析法探讨了大气颗粒物中铊的可能来源。结果表明,无论是在PM_(10)还是PM_(2.5)中铊均是以分布在可氧化态为主,在环境中具有较强的迁移性;大气颗粒物中的铊主要来自人为污染源,其中PM_(10)中的铊主要来自焙烧渣扬尘和污染源排放的废气,而PM_(2.5)中铊则主要是来自污染源排放的废气。     

珠江口三维水质与底泥耦合模型的验证及应用

基于一维河网与三维河口耦合水动力模型,建立了可描述珠江口水体-底泥中营养盐动态变化的三维水质-底泥模型,利用1999年和2006年夏季观测数据对模型进行了验证,在此基础上,模拟分析了珠江口主要水质因子和底泥营养盐通量的分布特征,以及底泥通量对珠江口营养盐输入的贡献.验证结果表明,模型能较好地反映出水体和底泥中的营养盐及溶解氧浓度的时空分布特征,各水质因子的模拟值与观测值的相对误差均小于38%;另外,底泥营养盐通量的模拟值与文献报道的实测结果较为接近,表明模型能合理地刻画出底泥主要生化过程及通量变化特征.模拟结果显示,夏季珠江口氨氮(NH_4~+-N)和活性磷酸盐(PO_4~(3-)-P)通量主要从底泥向水体输送,底泥是水体氮磷元素的源,而硝态氮和亚硝态氮(NO_3~-+NO_2~-,NO23)的通量输送方向则与之相反,底泥呈现“汇”的效应;底泥营养盐通量主要从河口向外海递减,伶仃洋NH_4~+-N、NO23、PO_4~(3-)-P的通量变化范围分别为0.24~8.88、-10.06~-0.14、-0.37~0.41 mmol·m~(-2)·d~(-1),珠江口近海的通量变化范围分别为-0.01~4.14、-1.45~0.68、-0.12~0.09 mmol·m~(-2)·d~(-1).整体而言,底泥营养盐通量对珠江口营养盐输入有明显贡献,夏季经底泥释放进入水体的NH_4~+-N和PO_4~(3-)-P最大相当于陆源总氮、总磷输入量的12%和22%.     

El Niño影响下春季南海北部表层水体CO2分压变化

采用走航连续观测系统分别在2011年5月和2015年5月对南海北部表层水体温度、盐度、溶解氧、叶绿素a和pCO_2进行了现场观测.在El Nio影响下,2015年5月华南地区及广东省降雨量偏多,大量冲淡水入海,南海北部冲淡水区域海表盐度显著降低,2015年5月冲淡水区域海表盐度平均值为(28.05±6.18),低于2011年5月的海表盐度平均值(29.65±2.58),同时实测冲淡水区域海表温度平均升高约2.10℃.冲淡水携带的营养物质和适度升高的海表温度共同促进了冲淡水区域浮游植物的繁殖.浮游植物光合作用不断地将海水中的游离CO2转化为有机碳,同时释放出氧气,使得水体pCO_2降低,2015年5月冲淡水区域pCO_2平均值为(286±95)μatm,低于2011年5月的pCO_2平均值(300±42)μatm.2015年5月实测获得离岸海域pCO_2平均值为(421±9)μatm,高于2011年5月pCO_2平均值(386±13)μatm,二者差值为35μatm,海表温度是离岸海域pCO_2的主要影响因子,2015年5月El Nio期间离岸海域SST升高1.96℃.El Nio影响下冲淡水区域的碳汇作用增加,离岸海域的碳源作用增强,冲淡水区域碳汇增加与离岸海域碳源增强基本抵消,2015年5月南海北部整体仍是CO_2弱汇区,约为-0.40 mmol·m~(-2)·d~(-1),与2011年5月通量值-0.58 mmol·m~(-2)·d~(-1)差别不明显.     

典型聚合物材料平行双板水平火蔓延规律研究

为了研究固体可燃物多火焰火蔓延规律及传热控制机理,开展了竖向水平排列的PMMA单一平板和平行双板火蔓延规律研究。基于水平火蔓延实验台,考虑平板尺寸、平行双板的竖直间距两个主要因素,分析此类条件下的火蔓延速度、火焰高度和火焰宽度等参数。实验研究发现,PMMA板水平火蔓延过程中,热解前锋呈V型,预热区长度随平板间距的增大先增大后减小。平行双板工况下,在研究考虑的间距范围内火焰始终保持合并,火蔓延速度、火焰高度及宽度明显大于单一平板,且均随间距的增加先增大后减小,三者峰值出现的位置与样件尺寸有关。上层PMMA板上下表面的辐射热流随间距的变化规律与火蔓延速度变化规律一致,因此推断辐射作用在平行双板水平火蔓延中起到主导作用。     

Transpiration rates of urban trees, Aesculus chinensis

Transpiration patterns of Aesculus chinensis in relation to explanatory variables in the microclimatic, air quality, and biological phenomena categories were measured in Beijing, China using the thermal dissipation method. The highest transpiration rate measured as the sap flux density of the trees took place from 10:00 am to 13:00 pm in the summer and the lowest was found during nighttime in the winter. To sort out co-linearity, principal component analysis and variation and hierarchical partitioning methods were employed in data analyses. The evaporative demand index (EDI) consisting of air temperature, soil temperature, total radiation, vapor pressure deficit, and atmospheric ozone (O₃), explained 68% and 80% of the hourly and daily variations of the tree transpiration, respectively. The independent and joint effects of EDI variables together with a three-variable joint effect exerted the greatest influences on the variance of transpiration rates. The independent effects of leaf area index and atmospheric O₃ and their combined effect exhibited minor yet significant influences on tree transpiration rates.     

长白山温带森林单萜烯排放模拟

于2010年夏季,采用松弛涡度积累(Relaxed Eddy Accumulation)技术在长白山温带森林铁塔上测量了挥发性有机物(VOC)冠层尺度的排放通量,同步测量了气象参数、光合有效辐射(PAR)等,初步获得长白山阔叶林单萜烯的排放通量.同时,利用PAR能量守恒原理,建立了冠层尺度上单萜烯排放的经验模式.结果发现,模拟结果与测量结果比较一致,平均而言,模拟值高出测量值约20%～40%.采用不同方法对经验模式进行了检验,结果表明,采用比较各个采样时段平均值的方法可行,而且经验模式对于2010年夏季不同采样时段的平均值也给出了较好的模拟结果,其模拟值高出测量值约20%～24%.     

污染河口区沉积物-水界面营养盐交换通量的实验研究

采集青岛市李村河口下游沉积物柱状样品,通过实验室培养实验,研究了溶解氧、温度、盐度、生物扰动等环境因素对沉积物-水界面营养盐交换通量的影响。结果表明,NO3-N、NH4-N、PO4-P在贫氧环境下的交换通量要高于富氧条件下,NO2-N受溶解氧含量的影响较小;随着温度的升高,NO3-N、NH4-N、PO4-P的交换通量增大,而NO2-N的交换通量减小;NO2-N和NH4-N的交换通量随盐度增大而增大,NO3-N减小,而PO4-P受盐度的影响较小;生物扰动对营养盐在沉积物-水界面的交换通量的影响显著。     

Experimental study of the influence of particle size on Minimum Explosible Concentration of sulfur dust

Despite the extensive use of sulfur in the industry, very little information is available in the literature on its key dust explosion properties. The work presented in this paper contributes to filling the current knowledge gaps on sulfur dust explosion properties and focuses on the experimental determination of the MEC of sulfur dust using a Modified Hartmann Tube and a 20 L dust explosion sphere. First, the MEC of sulfur dust samples collected at a sulfur production facility from areas prone to the generation of fine sulfur dust was measured. The results showed that these sulfur dust samples are fine enough to cause dust explosions with 55 ± 5< MEC <105 ± 5 g/m³. Second, the influence of the particle size of sulfur dust was investigated with both equipment. The use of the Modified Hartmann Tube for MEC determination showed that the MEC increases with increasing particle size in the particle size range of 0–2000 μm. Unlike the Modified Hartmann Tube, MEC experiments done in the 20 L Sphere did not allow the quantification of the influence of the particle size on the MEC. These results were explained by the phenomenon of particle breakage induced by the 20 L Sphere's dispersion mechanism. Additional experiments with the 20 L sphere confirmed the particle breakage of sulfur dust particles and showed that it is inversely proportional to dust concentration and proportional to the dust's original particle size distribution.     

三醋酸纤维(CTA)正渗透膜活性层朝向对正渗透过程的影响

本文通过在线实时监测研究了三醋酸纤维(CTA)正渗透膜的活性层在朝向料液(AL-FS)和汲取液(AL-DS)两种模式下的正渗透水通量、反向溶质通量、特性反向溶质通量等因素及其变化规律。在实验室条件下模拟了三醋酸纤维膜(CTA)对于不同浓度苦咸水的处理,当苦咸水浓度为2000ppmNaCl、5000ppmNaCl、8000ppmNaCl时,CTA膜活性层朝向对脱盐率几乎没有影响,AL-FS模式和AL-DS模式的脱盐率分别为96.49%和96.13%、97.40%和96.38%、98.04%和96.81%。研究结果对于进一步开发CTA正渗透系统和实用化具有重要意义。