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Atmospheric Environment (1967)最新文献

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Authors' reply 作者的回复
Pub Date : 1989-01-01 DOI: 10.1016/0004-6981(89)90424-1
L.W.A. van Hove, W.J.M. Tonk, E.H. Adema
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引用次数: 0
New patents 新专利
Pub Date : 1989-01-01 DOI: 10.1016/0004-6981(89)90431-9
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引用次数: 0
Author's reply 作者的回复
Pub Date : 1989-01-01 DOI: 10.1016/0004-6981(89)90323-5
Sotirios Glavas
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引用次数: 0
Forthcoming meetings 即将到来的会议
Pub Date : 1989-01-01 DOI: 10.1016/0004-6981(89)90076-0
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引用次数: 0
Development of a dry deposition model for atmospheric coarse particles 大气粗颗粒干沉降模式的建立
Pub Date : 1989-01-01 DOI: 10.1016/0004-6981(89)90007-3
Kenneth E. Noll, Kenneth Y.P. Fang

Atmospheric inertial deposition of coarse particles has been quantified by the evaluation of particle dry deposition flux data collected simultaneously on the top and bottom surfaces of a smooth plate with a sharp leading edge that was pointed into the wind by a wind vane. The deposited particles were weighed and counted. The airborne concentration of coarse particles was measured with a Rotary Impactor. Deposition velocity was determined by dividing the mass flux (plate) by the airborne concentration (Rotary Impactor). The deposition velocity was considered to be due to gravitational settling (VST) and inertial deposition (VI). Deposition to the upper plate surface (VdU) was given by: VdU = VST + VI, while deposition to the lower plate surface (VdL) was given by: VdL = − VST + VI. The inertial deposition velocity was defined as: VI = ̄geAU, where ̄geA is the particle effective inertial coefficient and U is friction velocity. Based on these equations, ̄geA was evaluated as a function of particle size as: ̄geA = 1.12e−30.36/dn, where da is the particle aerodynamic diameter (μm). The correlation coefficient was 0.92, ̄geA varied from 0.1 to 1.0 for particles between 5 and 100 μm diameter.

The particle dry deposition fluxes obtained for the top and bottom surfaces of the plate were extended to the free atmosphere. A particle flux ratio (FR) was defined as: FR = VdLVdU. The mass median aerodynamic diameter MMDa for the atmospheric coarse particle size distribution correlated closely with the geometric mean values of (FR). The flux ratio was also related to the shape of the coarse particle mass distribution. The f

利用风向标指向风的锋利前缘光滑板的上下表面同时采集的颗粒干沉降通量数据,对粗颗粒大气惯性沉降进行了量化。对沉积的颗粒进行称重和计数。用旋转冲击器测量了空气中粗颗粒的浓度。沉积速度由质量通量(板)除以空气浓度(旋转冲击器)确定。沉积速度考虑为重力沉降(VST)和惯性沉积(VI)。上平板表面沉积(VdU)为:VdU = VST + VI,下平板表面沉积(VdL)为:VdL =−VST + VI。惯性沉积速度定义为:VI = geAU∗,其中 geA为粒子有效惯性系数,U∗为摩擦速度。根据这些方程,将 geA计算为粒径的函数: geA = 1.12e−30.36/dn,其中da为颗粒气动直径(μm)。5 ~ 100 μm颗粒的相关系数为0.92,相关系数为0.1 ~ 1.0。得到的颗粒干沉积通量的板的顶部和底部表面延伸到自由气氛。定义粒子通量比FR为:FR = VdLVdU。大气粗粒度分布的质量中值气动直径MMDa与(FR)几何平均值密切相关。通量比还与粗颗粒质量分布的形状有关。粒径小于3 μm的颗粒的通量比小于0.1,且随风速的增大不显著。这与直径小于3 μm的粗颗粒质量分布的最小值相对应。粒径大于50 μm的颗粒的通量比也较小,但随着风速的增大通量比迅速增大。这表明在高风速条件下,较大的颗粒可以保持悬浮状态。实测的大气粗颗粒质量分布表明,随着风速的增加,较大颗粒的质量增加。这与颗粒通量比的增加是一致的。
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引用次数: 82
A photochemical model for air quality assessment: Model description and verification 空气质量评估的光化学模型:模型描述和验证
Pub Date : 1989-01-01 DOI: 10.1016/0004-6981(89)90013-9
G.D. Hess

A hybrid Eulerian-Lagrangian, photochemical model has been developed for the assessment and prediction of the impact of large point sources on air quality. This simple model is based on solving the mass conservation equations which include chemical reaction terms in the cells of a two-dimensional crosswind plane which moves with the air parcel. Testing of the model is done in three ways. First, the chemistry is evaluated using results of smog chamber experiments simulating Melbourne's emissions and meteorological conditions. Second, the accuracy of the emissions inventory is tested using aircraft measurements. Finally the overall performance of the model is evaluated using monitoring station data. In general the model gives good agreement with the measurements, with the predictions for O3 being somewhat better than those for NO2. This result was also found in the three-dimensional study of McRae and Seinfeld (1983, Atmospheric Environment17, 501–522) for the Los Angeles area.

为了评估和预测大型点源对空气质量的影响,建立了一个欧拉-拉格朗日混合光化学模型。这个简单的模型是建立在求解质量守恒方程的基础上的,该方程包含了随空气团移动的二维侧风平面单元中的化学反应项。模型的测试有三种方式。首先,利用模拟墨尔本排放和气象条件的烟雾室实验结果对化学成分进行评估。其次,使用飞机测量来测试排放清单的准确性。最后利用监测站数据对模型的整体性能进行了评价。总的来说,该模型与测量结果吻合得很好,对臭氧的预测比对二氧化氮的预测要好一些。麦克雷和宋飞(1983,大气环境17,501-522)对洛杉矶地区进行的三维研究也发现了这一结果。
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引用次数: 10
Process for cleaning hot waste gas occuring in varying amounts 清洗不同量的热废气的过程
Pub Date : 1989-01-01 DOI: 10.1016/0004-6981(89)90046-2
Christia Schwartzbach
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引用次数: 0
Effect of ambient environmental factors on indoor formaldehyde levels 环境因素对室内甲醛水平的影响
Pub Date : 1989-01-01 DOI: 10.1016/0004-6981(89)90054-1
Thad Godish

The effect of ambient (outdoor) environmental parameters on formaldehyde levels in a temperature controlled urea-formaldehyde foam-insulated (UFFI) house and a mobile home was investigated over a 9-month period (July–March). Strong correlations between formaldehyde levels, solar radiation, ambient temperatures, inside/outside temperature differences and water vapor pressure were observed in the UFFI house and in the mobile home. Stepwise regression revealed a significant independent effect of solar radiation values on indoor formaldehyde levels in the UFFI house but not in the mobile home. Stepwise regression revealed no significant independent effect of the other environmental variables evaluated. The independent effect of solar radiation on formaldehyde levels in the UFFI house indicates that solar radiation can have a significant effect on formaldehyde concentrations, and this effect may explain anomolous results in whole house source interaction studies.

在为期9个月(7 - 3月)的时间里,研究了环境(室外)环境参数对温控脲醛泡沫隔热(UFFI)房屋和活动房屋中甲醛水平的影响。在UFFI房屋和移动房屋中观察到甲醛水平、太阳辐射、环境温度、室内外温差和水蒸气压之间存在很强的相关性。逐步回归显示,太阳辐射值对UFFI房屋室内甲醛水平有显著的独立影响,但对移动房屋没有影响。逐步回归显示其他环境变量的独立影响不显著。太阳辐射对UFFI房屋甲醛水平的独立影响表明,太阳辐射可以对甲醛浓度产生显著影响,这种影响可以解释全屋源相互作用研究中的异常结果。
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引用次数: 5
The laboratory production of the bubbling fraction of the marine aerosol—application to polluted seawater∗ 海洋气溶胶冒泡部分的实验室生产-在污染海水中的应用*
Pub Date : 1989-01-01 DOI: 10.1016/0004-6981(89)90073-5
Duncan C. Blanchard
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引用次数: 3
Evaluation of eight short-term long-range transport models using field data 利用野外资料评价8种长短期输运模式
Pub Date : 1989-01-01 DOI: 10.1016/0004-6981(89)90101-7
R.A. Carhart, A.J. Policastro, M. Wastag, L. Coke

Eight short-term long-range transport models (MESOPUFF, MESOPLUME, MSPUFF, MESOPUFF II, MTDDIS, ARRPA, RADM and RTM-II) have been tested with field data from two data bases involving tracer releases. The Oklahoma data base involved two separate experiments with measurements taken at 100 and 600 km arcs downwind of a 3-h perfluorocarbon release. The Savannah River Plant data base encompassed 15 experiments with measurements taken over 2–5 days at distances of 28–144 km downwind from a 62 m stack release of Kr-85 gas.

Application of the American Meteorological Society statistics to the model/data comparisons showed that six of the eight models predicted within a factor of two of the observed concentrations for all of the following: points paired in space and time, points paired in space only, and for points unpaired in space and time. However, the ratio of the standard deviation of residuals to the average observed value showed improvement as more unpairing was done in the comparison of the models with the data. The statistical comparisons reveal a definite tendency of the models to overpredict plume concentrations. Supplemental graphical comparisons showed that plume concentration overprediction is accompanied with an underprediction of plume spreading, and that a definite time lag is often observed between the time of arrival of the observed plume and the time of arrival of the predicted plume.

The causes of model/data discrepancies can be largely traced to inadequate wind field modeling that leads to an incorrect temporal and spatial positioning of the plume, and the use of the Turner [Workbook of atmospheric dispersion estimates. U.S. Dept of H.E.W. Publication 999-AP-26 (1970)] curves to downwind distances beyond which they can accurately represent the scales of atmospheric turbulence. The use of multilayer wind field models and the use of the Heffter [J. appl. Met.4, 153–156 (1965)] formula for lateral plume dispersion close to the source appear to improve model accuracies.

八个长短期输运模型(MESOPUFF、MESOPLUME、MSPUFF、MESOPUFF II、MTDDIS、ARRPA、RADM和RTM-II)已经用两个涉及示踪剂释放的数据库的现场数据进行了测试。俄克拉何马州的数据库涉及两个独立的实验,分别在3小时全氟碳化合物释放的顺风处100公里和600公里处进行测量。萨凡纳河电厂数据库包括15项实验,测量时间为2-5天,距离下游28-144公里,距离62米的Kr-85气体堆释放。将美国气象学会的统计数据应用于模式/数据比较表明,在8个模式中,有6个模式对下列所有观测浓度的预测在两个因子范围内:空间和时间上成对的点、空间上仅成对的点以及空间和时间上未成对的点。然而,残差标准差与平均观测值之比在模型与数据的比较中,随着更多的解配对,出现了改善。统计比较表明,这些模型有明显的高估羽流浓度的趋势。补充的图形比较表明,羽流浓度的高估伴随着羽流扩展的低估,并且在观测到的羽流到达时间和预测的羽流到达时间之间经常观察到一定的时间滞后。模式/数据差异的原因很大程度上可以追溯到风场建模不充分,导致羽流的时间和空间定位不正确,以及使用特纳[工作手册]估算大气扩散。U.S. department of H.E.W. Publication 999-AP-26(1970)]曲线到下风距离,超过这个距离,它们可以准确地表示大气湍流的尺度。多层风场模型的应用和Heffter的应用[J]。达成。在靠近震源处的羽流横向弥散公式似乎提高了模型的精度。
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引用次数: 7
期刊
Atmospheric Environment (1967)
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