核电厂址事故大气弥散因子计算的实验与理论研究

在目前常用的计算核电厂事故概率大气扩散因子的模式基础上提出了考虑内边界层影响的计算模式，根据某待建滨海核电厂址大气弥散实验的实测参数，分别采用本模式和常用模式估算了厂址边界０．５ｋｍ外的最终评价用事故概率扩散因子和各途径的剂量及有效剂量。计算结果表明，无论是事故概率扩散因子还是个人有效剂量，本模式给出的值都是常用模式的５．９倍。因此，在不能忽略内边界层出现频率的滨海厂址，必须考虑内边界层对事故扩散     

Experimental verification for real-time environmental emergency response system: WSPEEDI by European tracer experiment

Japan Atomic Energy Research Institute has developed an emergency response system WSPEEDI to forecast long-range atmospheric dispersions of radionuclides discharged into the atmosphere. The latest version of WSPEEDI consists of an atmospheric dynamic model MM5 for calculating meteorological fields and a particle random-walk model for atmospheric dispersion. The performance of WSPEEDI was evaluated by data obtained from a field tracer experiment over Europe (ETEX) in this paper. The model validation was done with respect to the following points: (1) the dependence of model accuracy on the temporal and spatial resolutions of the meteorological fields and (2) the superiority of an atmospheric dynamic model over a mass-consistent wind model. Regarding (1), it was shown that the calculation accuracy of the new version with high temporal resolution was improved, especially at the edge of the plume. Moreover, although the increase in horizontal spatial resolution of the old version had no substantial effect on the model performance, increase in horizontal resolution of the new version contributed to the significant improvement of the calculation accuracy. These results showed that the dynamically calculated meteorological field with the spatial resolution of the meso-β–γ scale greatly improved calculation accuracy.     

空气微生物研究方法进展与展望

着重论述了空气微生物气溶胶的研究方法，主要有培养基法和非培养基法。培养基法是传统的微生物研究方法，需要花费大量的时间和劳动力，只能够检测活的能够在培养基上生长的微生物，可以大致反映空气中的微生物气溶胶。非培养基法，主要是PCR法，具有敏感性高、快速、特异性强等特点，能够检测出环境样品中绝大多数的微生物，是一种微生物气溶胶检测的有效途径。最后指出实时持续的监测是将来空气微生物研究的努力方向和发展趋势。     

纳米颗粒的分散及其在水与废水处理中的应用

纳米颗粒由于其吸附活性而极易产生自身团聚 ,这不利于纳米颗粒在使用介质中的分散并影响其应用。本文综述了近年来有关纳米颗粒在水中的分散方法、原理及影响因素 ,归纳总结了分散的纳米颗粒在强化水处理中的若干应用。     

Integrating models to predict regional haze from wildland fire

Visibility impairment from regional haze is a significant problem throughout the continental United States. A substantial portion of regional haze is produced by smoke from prescribed and wildland fires. Here we describe the integration of four simulation models, an array of GIS raster layers, and a set of algorithms for fire-danger calculations into a modeling framework for simulating regional-scale smoke dispersion. We focus on a representative fire season (2003) in the northwestern USA, on a 12 km domain, and track the simulated dispersion and concentration of PM_2.5 over the course of the season. Simulated visibility reductions over national parks and wilderness areas are within the ranges of measured values at selected monitoring sites, although the magnitudes of peak events are underestimated because these include inputs other than fire. By linking the spatial and temporal patterns of haze-producing emissions to climatic variability, particularly synoptic weather patterns, and the stochastic nature of fire occurrence across the region, we can provide a robust method for estimating the quantity and distribution of fire-caused regional haze under climate-warming scenarios.     

Steady Shallow-Water Current and Solute Transport around a Semi-Conical Headland

Laboratory experiments have been carried out to investigate the effects of a sloping wall headland on the flow characteristics and the associated concentration distributions from a point source around the headland. A semi-conical headland with a slope of 1:2 was set up in a flow basin, 4.8 m long and 3.8 m wide. In this paper, the experimental results of a steady shallow-water current are reported. Three dimensional flow velocities in the basin were measured using Sontek-ADV instrument. The dye concentration levels in the basin were measured by two fluorometers. The experimental results showed a large-scale re-circulation region behind the semi-conical headland. The peak turbulence energy, at about 53% of the local kinetic flow energy, coincides with the region of high velocity gradient. Significant vertical flows were observed around the area near the downhill slope of the headland, with a maximum ratio of vertical to horizontal velocities being about 22%. Such relatively significant vertical scouring velocities, coupled with strong turbulence energy and high horizontal velocity gradients in the same region, could cause severe bed erosion. The experimental results have also been compared with the predicted results of a depth-averaged numerical model. The predicted eddy structure and the concentration distribution in the re-circulation area were found to compare favourably with the experimental results. However, the discrepancies in the flow velocities and the concentration levels near the headland were apparent. It was observed that the dye concentration continued to spread in the cross-stream direction after passing the headland, whereas only a limited extent of the lateral spreading was predicted by the numerical model further downstream of the headland.     

显像管玻壳铅尘在大气中的迁移扩散规律和污染特征

以石家庄市显像管玻壳厂排放的铅尘为研究对象，通过在该玻壳厂周围土壤表层布点采样，较系统地研究了铅尘在大气中的迁移转化规律及其污染特性。研究结果表明，用高斯模式能成功地预测铅尘在大气中的迁移扩散规律。     

Parameter estimation for fractional dispersion model for rivers

The fractional dispersion model for natural rivers, extended by including a first order reaction term, contains four parameters. In order to estimate these parameters a fractional Laplace transform-based method is developed in this paper. Based on 76 dye test data measured in natural streams, the new parameter estimation method shows that the fractional dispersion operator parameter F is the controlling parameter causing the non-Fickian dispersion and F does not take on an integer constant of 2 but instead varies in the range of 1.4–2.0. The adequacy of the fractional Laplace transform-based parameter estimation method is determined by computing dispersion characteristics of the extended fractional dispersion model and these characteristics are compared with those observed from 12 dye tests conducted on the US rivers, including Mississippi, Red, and Monocacy. The agreement between computed and observed dispersion characteristics is found to be good. When combined with the fractional Laplace transform-based parameter estimation method, the extended fractional dispersion model is capable of accurately simulating the non-Fickian dispersion process in natural streams.     

天然和人工叠加流场下弥散试验研究

在污灌区浅层含水层进行了现场弥散试验,采用氚做为示踪剂,瞬时投放.因为天然流速较弱,通过注水形成天然的和人工的叠加流场.根据流场特性。建立以Φ-Ψ坐标表示的移流弥散数学模型.采用有限差数值方法求解,其中二维模型应用分裂格式.通过计算的浓度曲线与实验曲线拟合,求得纵、横向弥散率.     

中部城市群二氧化硫扩散模型的建立

应用CALPUFF中尺度空气质量扩散模式，建立辽宁中部城市群地区二氧化硫扩散模型，成功地模拟了区域二氧化硫的污染状况。