ATMOSPHERIC CONTROLS OF WATER EXCHANGE IN GREAT LAKES BASIN1

ABSTRACT Existing meteorological controls of water exchange by precipitation and evaporation on the Great Lakes are almost entirely inadvertent and related to man's urban-industrial complexes and their effect upon precipitation processes. These inadvertent effects have led to 10 to 40% increases in precipitation in localized areas within the basin. Envisioned growth of urban-industrial complexes within the Great Lakes region should lead to more inadvertent weather modification in the Basin. The only existing planned weather modification efforts are those at Lake Erie which are attempting to eliminate by redistribution the concentration of lake-derived heavy snowfall along the south shore. It appears reasonable to assume that practical increases of lake precipitation on the order of 5-20% could be achieved on an operational basis over the Great Lakes in the next 10 years, but the time of accomplishment will depend on national priorities, international cooperation, and economic factors. These activities would certainly produce a sizeable increase in the water quantity of the Great Lakes and should result in an improvement in water quality. Operational methods of evaporation suppression applicable to the lakes are just not available. Meteorological controls to ameliorate certain undesirable lake-effect snowstorms are a near reality.     

PREDICTIVE MODELS FOR GREAT LAKES HYDROLOGY1

ABSTRACT: The individual hydrologic components are assumed to be normally distributed for each month and linear regression equations are estimated for predicting the value of the individual monthly hydrologic components. It is shown that some of the hydrologic components for downwind (in this case downstream) lakes are dependent upon hydrologic events for the upwind lakes. This is particularly so for precipitation in the downwind lake basins which appears to be dependent upon evaporation values for upwind lakes.     

ESTIMATING EVAPORATION FROM UTAH'S GREAT SALT LAKE USING THERMAL INFRARED SATELLITE IMAGERY1

ABSTRACT: Water surface temperatures can be obtained from satellite thermal remote sensing. Landsat and other satellites sense emitted thermal infrared radiation on a regular basis over much of the earth's surface. Evaporation is accomplished by the net transport of mass from the water surface to the atmosphere. The evaporative transfer predominantly determines the water surface temperature. Hence, there should be good correlations between evaporation and surface temperatures. Previous investigations on Utah Lake with satellite-derived temperatures and pan- and model-derived evaporation values have produced good correlations. However, more study was required with additional satellite data and evaporation measurements for saltwater conditions. The applicability of this method for estimating evaporation on Utah's Great Salt Lake was of particular interest at this time because of the unprecedented rise of this terminal lake. Satellite thermal data and evaporation data from four different years were obtained for the Great Salt Lake and the surrounding region. More than 350 correlation and linear regression analyses were performed on the temperature and evaporation data. The lake salt concentrations were also factored into the analyses in several different ways. The correlation results were generally very good and a methodology for using satellite-derived water surface temperatures along with salt concentrations was developed to estimate evaporation.     

新型喷雾式蒸氨设备的研究

试验设计了一种新型的蒸氨反应器,创新之处在于采用雾化喷头代替了传统的填料.废水经过加压雾化后与上升的气流逆向接触,通过增加接触面积达到提高去除率的目的.通过试验验证了使用这种新型的蒸氨反应器处理含高浓度氨氮的废水,在温度80 ℃,pH值11,鼓风量为1.63 m3/min,蒸氨时间为30 min的条件下,能达到高于90%的去除率.     

碳青霉烯系列医药中间体生产废水治理技术应用研究

采用“气浮＋三效蒸发＋Ic＋CASS＋BAF”工艺处理碳青霉烯系列医药中间体生产废水。总处理水量为84t／d：进水水质：COD：58650mg／L、氨氮：203mg／L、盐分：106000mg／L。经该工艺处理后,废水中的COD、氨氮、盐分等指标均能迭标排放。     

基于遥感的千烟洲人工林蒸散及其组分模拟研究

论文通过改进遥感蒸散模型的关键参数,结合遥感数据和气象观测数据,对2003—2008年江西千烟洲人工林生态系统蒸散及其组分进行模拟,并利用涡度相关技术获取的蒸散实测数据对模型模拟结果进行验证和评价。结果表明:①年均蒸散总量模拟值比实测值偏低2.4%,决定系数与均方根误差分别为0.83和0.61 mm·d^-1。②土壤蒸发、林冠截留蒸发和植被蒸腾分别占总蒸散量的12%、23%和65%。其中,土壤蒸发季节及年际变化相对稳定;林冠截留蒸发季节变化明显且在不同年份差异较大;植被蒸腾季节变化明显,但年际变异较小。③1—3月植被光合作用较弱,植被蒸腾与蒸散比小于30%。随着植被蒸腾的增强,从4月开始植被蒸腾与蒸散比迅速增加,在生长旺季(7月底)可达到约90%。由于该模型所需数据在区域尺度较易获取,从而为开展区域尺度中亚热带人工林生态系统蒸散及其组分模拟提供方法支撑。     

垃圾填埋场渗滤液有机物成分分析及蒸发处理研究

采用GC-MS对某垃圾填埋场渗滤液中的有机物成分进行检测分析。结果表明:渗滤液中至少含有50种有机污染物,相对含量最高的有机污染物是尼古丁和3-甲酚。研究真空度、蒸发温度和pH值对渗滤液蒸发过程中冷凝液的COD、TOC和氨氮浓度的影响,并对冷凝液进行有机物成分检测,结果表明:蒸发速率和冷凝液COD值均随蒸发温度和真空度的增加呈增加趋势,蒸发温度和真空度对冷凝液TOC值影响不大,随蒸发温度升高冷凝液中氨氮含量整体呈下降趋势;在蒸发温度60～120℃范围内,冷凝液的有机物成分以烷烃类有机物和尼古丁为主;烷烃类有机物的析出仅与蒸发温度有关,苯酚类有机物的析出与真空度和蒸发温度均有关;在酸性条件下蒸发冷凝液的COD值和TOC值均远大于在中性和碱性条件下的数值,但氨氮含量相反;酸性条件下冷凝液有机物成分主要为有机酸和烷烃类有机物。     

装置进气口宽度对不同尺寸油盘火旋风燃烧特性影响的研究

为探究进气口宽度对火旋风燃烧特性的影响,利用自然驱动的四面边墙夹缝式装置对不同进气口宽度使用１５０,２００,２５０ mm 3种直径进行实验研究。由燃料质量随时间变化曲线得出准稳态阶段火旋风的质量燃烧速率;利用摄像机记录火焰的连续图像并获得火焰高度。结果表明:针对实验室小型火旋风（150~250 mm）,在进气口宽度为35 mm左右时,火旋风的燃烧速率最大,即火旋风的燃烧强度存在1个最佳的进气口宽度;当火焰高度达到最高时,环量也存在1个临界值。     

油田高含盐污水雾化蒸发的数值模拟

基于FLUENT软件,对油田高含盐污水的雾化蒸发过程进行了数值模拟,得到了逆流型雾化蒸发塔内的流场分布特性,对比分析了不同操作参数对蒸发效果的影响。结果表明:液滴蒸发速率沿塔体中心轴线自上而下呈加快趋势;进口空气流速与温度是影响液滴蒸发的关键操作参数,提高流速及温度均可加快液滴的蒸发速率;当进口空气流速达到0.4 m/s后,对蒸发速率的影响减弱;当进口空气温度达到313 K后,对蒸发速率的提高作用不大;喷雾锥角的变化对蒸发速率影响不明显;液滴越细化,蒸发速率越快。     

百脉泉泉群泉水氢氧稳定同位素时空变化特征

研究泉水氢氧稳定同位素时空变化特征,探究泉水的补给来源,对水资源管理及旅游业可持续发展具有重要指导意义。以百脉泉泉群为研究区,通过分析降水及泉水中的氢氧稳定同位素特征,获取了本地大气降水线、泉水同位素时空变化特征及蒸发线,并探究了百脉泉泉水的补给来源。结果表明：大气降水中δ²H的波动范围为-151.55‰δ¹⁸O—-4.28‰,δ¹⁸O的波动范围为-19.93‰δ¹⁸O—-0.52‰,δ²H和δ¹⁸O在时间上的分布规律相似,均呈现双峰状(“M”型),本地大气降水线(LMWL)为：δ²H=7.58×δ¹⁸O+4.17。百脉泉泉水的δ²H的波动范围为-65.23‰δ¹⁸O—-37.01‰,δ¹⁸O的波动范围为-8.99‰δ¹⁸O—-4.04‰。泉水δ²H—δ¹⁸O均落在本地大气降水线上或...