水库二维水流泥沙数学模型及应用

建立水库坝区平面二维水流泥沙数学模型,考虑了悬移质非均匀,非饱和输沙特性,采用正交曲线坐标拟合复杂边界、ＳＩＭＰＬＥＣ程式离散求解及动边界技术。用该模型对白沙水库流场和河床变形进行了数值验证,计算了典型年条件下,水库取水口附近流场和河床局部形态。结果表明,坝前取水口漏斗基本保持稳定状态。     

流动显示技术及其在温排放模型试验中的应用

简介了作者的流动显示方法（包括应用塑料示踪剂、间隙曝光装置、定时控制器和普通照相机来拍摄水工整体试验中大范围流动的照片（流谱图））;并利用微机图形处理系统,对实拍流谱图进行图／数处理（包括光学修正、网格插补等预处理和信息处理）,从中识别出流体物理参数及其等值线分布图（包括流速场、流函数场和涡度场等）。作为实例,介绍了应用本流动显示技术和方法,在某电厂温排水整体试验中获得取排水口近区流场定量信息的情     

同相水深-辐射关系率定

介绍了水体同相的概念,利用水体地质、地貌、沉积和水文等条件确定水体同相的方法,以及在水体同相前提下建立水深－辐射关系的实用性,并提出了利用稳定水下地形且测深资料的水域进行水深－辐射关系借地率定的新思路,探索了利用卫星遥感测量水下地形的新方法,该方法弥补了以往遥感测深需要低含沙的清澈水体的缺陷。     

木兰溪两岸浅井水对紫露草四分体微核率的影响

采用紫露草四分体微核技术,对莆田木兰溪下游河溪水和饮用的浅井水进行致突变性监测。结果表明,１０份河溪水能明显诱发紫露草四分体微核率的增高;与对照组相比１０份浅井水也均不同程度提高了四分体微核效应,８份已达到显著或极显著水平（Ｐ〈０．０５或Ｐ〈０．０１）,且与诱发的紫竹梅四分体微核效应显著相关,ｒ＝０．９７７７。说明浅井水内存在致植物细胞染色体畸变物质,提示当地居民上消化道肿瘤高发与饮水污染有一定相     

化学法清洗硅片过程中清除颗粒的机理(英文)

对化学法清洗硅片过程中消除颗粒的机理作了定量的探讨。颗粒的清除是由于化学蚀刻和颗粒与表面排斥力共同作用的结果。首次提出了最浅蚀刻深度和最小蚀刻速度的概念。最浅蚀刻深度可通过颗粒与表面间作用能的关系进行计算。是小蚀刻速度则可通过蚀刻侧形进行计算。研究结果对于优化化学法清洗过程和设计高性能清洗液都具有重要意义。     

Isolation of Some Soluble and Dispersed Materials of Oregano Water

Recent results obtained on determining the extraction efficiency and composition of organic volatiles in Oregano Water obtained from Origanum onites L. are described. Oregano Water was subjected to liquid-liquid extraction with a range of solvents with different polarities and each extract was analyzed by GC/MS.     

Voltammetry in Undiluted Acetic Acid. In Situ Determination of Water

Water present in undiluted acetic acid can be monitored in situ with Pt and Au microelectrodes using differential pulse and square‐wave voltammetries. Both reduction and oxidation peaks can be obtained. The best quantitative analytical results were obtained for the anodic peak, the Pt microelectrode, and differential pulse voltammetry. The anodic water peak is located at +1.55 V vs. the quasi reference Pt electrode. The voltammetric peak obtained at Pt electrode is apparently not a diffusional one, however, the calibration plot obtained by employing this peak is linear over a wide concentration range, up to 4 mol dm^?3. The detection limit has been estimated as 2.3 mM or 0.0043 v/v%. The developed method may be particularly useful, since the Karl Fischer method can not be used to determine water in glacial acetic acid due to the estrification reaction of acetic acid with methanol. A voltammetric wave of undiluted acetic acid could not be obtained in the positive and negative ranges of potential.     

Interactions of Pb(II) with particles of a polluted river

Pb(II) interactions with the surface of suspended matter from a polluted river was studied using differential pulse anodic stripping voltammetry (DPASV) technique. Three sampling sites were selected and studies have been done with samples collected in different times of the year (winter, autumn and summer). The values have been compared with those obtained in spring in the same conditions [Sci. Total Environ. 151 (1994) 101].Particles were separated by centrifugation and suspensions of the freeze-dried particles were titrated with Pb(II), being measured the labile metal fraction by DPASV. For comparison, suspensions of river water without any separation have also been titrated.Results show that surface metal complexes are inert, within the time scale of the analytical technique and desorbed organics from surfaces, form labile Pb(II) complexes in solution. For each sample it was determined the capacity for Pb complexation of particles and desorbed organics and the differential function has been estimated. Despite the heterogeneity of ligands, the systems interpreted in a discontinuous way, present one or two kinds of dominant ligands with Pb affinity.     

Cathodoluminescence Depth Profiling in SiO2:Ge Layers

 For investigation of the luminescent center profile cathodoluminescence measurements are used under variation of the primary electron energy E ₀ = 2…30 keV. Applying a constant incident power regime (E ₀·I ₀ = const), the depth profiles of luminescent centers are deduced from the range of the electron energy transfer profiles dE/dx. Thermally grown SiO₂ layers of thickness d = 500 nm have been implanted by Ge⁺-ions of energy 350 keV and doses (0.5–5)10¹⁶ ions/cm². Thus Ge profiles with a concentration maximum of (0.4 – 4) at% at the depth of d_m≅240 nm are expected. Afterwards the layers have been partially annealed up to T _a = 1100 °C for one hour in dry nitrogen. After thermal annealing, not only the typical violet luminescence (λ = 400 nm) of the Ge centers is strongly increased but also the luminescent center profiles are shifted from about 250 nm to 170 nm depth towards the surface. This process should be described by Ge diffusion processes, precipitation and finally Ge nanocluster formation. Additionally, a Ge surface layer is piled-up extending to a depth of roughly 25 nm.     

Influence of Cycle Temperatures on the Thermochemical Heat Storage Densities in the Systems Water/Microporous and Water/Mesoporous Adsorbents

The adsorption equilibrium of water on microporous adsorbents (zeolites of NaA-, NaY- and NaX-type as well as their ion exchanged forms) and on mesoporous adsorbents (different silica gels and composite material i.e. silica gel + salt hydrate) has been studied experimentally and theoretically. Using the Dubinin theory of pore filling the characteristic curves of the adsorption systems and other relevant dependences such as isotherms, isobars, isosteres and the curve of the differential heat of adsorption were calculated. For all systems investigated the adsorption were calculated. A_ads and the desorption potential A_des of the closed heat storage system were estimated. These values define the working range of the adsorption/desorption cycle and allow to calculate the specific heat storage density Δ h_sp. On the basis of Δ h_sp the different adsorbents were compared in order to select the optimal porous storage material for a given application. The presented experimental and theoretical investigations show that the adsorption systems water-zeolite and water-composites are promising working pairs for thermochemical heat storage processes for hot tap water supply and space heating of single family dwellings. The advantage of the water-composite system is the low desorption temperature (solar energy) the main shortcoming the low temperature lift. The advantage of the water zeolite system is the high temperature lift, the shortcoming are the relative high desorption temperatures.