污水处理厂运营管理评价模型及其工程应用研究

随着环境污染的日益加重、环境资源的日益紧缺,污水处理厂的环境管理变得越来越重要.文章首先介绍了污水处理厂运营管理评价的发展状况并指出每个阶段存在的问题,然后通过对比选择污水处理厂运营管理评价的最优模型,同时还论述印度、北京等污水处理厂使用偏最小二乘法、平行因子分析法、熵权物元法以及神经网络等评价模型在工程实际中的应用,最后阐述如何改善现有预测与评价体系,以期进一步提升污水处理厂的运营管理效率,改善日益严重的水污染问题,保护我们珍贵的地球生态水资源.     

基于MATLAB的城市表层土壤重金属污染空间分布的研究

为全面了解某城市表层土壤重金属污染的空间分布特征,对城市表层土壤中重金属元素As、Cd、Cr、Cu、Hg、Ni、Pb、Zn进行采样分析,采用域法识别特异值进行数据处理。通过Matlab软件,利用克里格法进行空间插值,绘出各重金属浓度与各坐标投影的一维空间分布图,并绘出全城等高地形图,再以数字大小标注样本点的污染浓度,拟合各元素浓度与海拔、平面坐标之间的关系模型,将重金属空间分布特征定量化、模型化。     

不同扰动强度下城市重污染河道底泥对磷吸收和固定的影响

以重污染河道底泥和上覆水为材料,研究了周期性加入外源磷条件下,不同扰动强度下底泥吸附和固定磷的作用机制.结果表明,扰动可以增加底泥对外源磷的吸附,而且扰动强度越大,底泥对外源磷吸附效率越高.另外,尽管加入的磷以溶解性磷酸盐(DIP)形态存在,但扰动强化了DIP向颗粒态磷(PP)的转化,从而降低了水体中生物可利用磷含量.内源磷形态分析表明,弱吸附态磷(NH4Cl-P)呈降低趋势,而铁铝结合态磷(Fe/Al-P)、钙结合态磷(HCl-P)和残渣磷(Res-P)均呈增加趋势,但以Fe/Al-P增加幅度最大(占总磷的百分比超过80%,以3种扰动强度下平均值计).结合到非闭蓄态Fe/Al-P中的外源磷逐渐增加占Fe/Al-P净增加量的百分比分别为37.49%(100 r·min-1)、42.32%(200 r·min-1)、54.24%(300r·min-1),导致闭蓄态铁铝结合态磷净增加量占总磷净增加量的百分比随扰动强度增加有所降低,同样,钙结合态磷的变化趋势也基本一致.说明在较短的时间尺度上和较大的扰动强度下,连续加入的外源磷主要以易释放态磷形式存在,即底泥对外源磷的吸附以暂时性的持留为主.     

Effects of copper and palladium on the reduction of bromate by Fe(0)

Bromate reduction by Fe(0) with incorporation of copper or palladium was investigated in batch tests. The incorporation of copper led to an increase in the rate of bromate reduction, while incorporation of palladium did not show any effect on bromate reduction by Fe(0), regardless of the bimetal application techniques (either simultaneous addition of Cu(II) or Pd(IV) into the Fe-BrO3- reaction system or using copper or palladium amended iron for bromate removal). Surface analyses by X-ray photoelectron spectroscopy (XPS) and X-ray powder diffraction (XRD) techniques indicated that aqueous Cu(II) was reduced and incorporated into the iron surface to form Cu2O and Cu(0). Among these two species, pure Cu(0) is not an active electron donor to the bromate reduction reaction, as shown by there being no reduction from using Cu(0) powders alone and no enhancement by Fe(0) when physically mixed with Cu(0). Although it has been proposed in the literature that the enhancement of adsorption also contributes to the enhancement of chemical reduction, this is not the case here because adsorption decreased when Cu increased. The enhanced bromate reduction rate in the presence of copper observed here is most likely the result of the newly formed active Cu(I). The presence of PdO was evidenced by XPS but yielded no enhancement in bromate reduction. Finally, the Cu2O present on the iron surface because of copper impurities in commercially available iron was found to be involved in the bromate reduction and to accelerate the reduction rate.     

ATR-FTIR investigation of the role of phenolic groups in the interaction of some NOM model compounds with aluminum hydroxide

The role of phenolic groups in the interaction of natural organic matter (NOM) with metal hydroxides was investigated with ATR-FTIR spectroscopy and adsorption tests by employing a series of dihydroxybenzoic acids (DHBAs) as the NOM surrogates and aluminum hydroxide as the adsorbent. All DHBAs examined in this study were found to be adsorbed on aluminum hydroxide by forming inner-sphere complexes. Carboxylic groups governed the complexation of DHBAs with aluminum hydroxide at low pH or in cases when the two hydroxyl groups were not adjacent to each other and neither of them was ortho to the carboxylic group. The involvement of the phenolic groups, ortho to another phenolic group or ortho to the carboxylic groups, in the complexation increased with increasing pH as the deprotonation of phenolic groups was easier at higher pH. The presence of phenolic groups increased the electron density of the carboxylic groups and facilitated the inner-sphere complexation of the carboxylic groups with metal hydroxide. The correlation between the pK_a values and the amount of organic acid adsorbed on the aluminum hydroxide revealed that the adsorption of DHBAs at acidic pH was largely dependent on the surface chelate formation rather than on the electronic effect.     

Atmospheric mercury emission from artisanal mercury mining in Guizhou Province,Southwestern China

Mercury (Hg) mining is an important anthropogenic source of atmospheric Hg emissions. The Guizhou Province in Southwestern China is a region with extensive artisanal mercury mining (AMM), but little Hg emission data from this area is available. Using a mass balance method, we estimated emission factors from artisanal mercury mining in Wuchuan mercury mining area (WMMA) and Gouxi area (GX). Average emission factors were 18.2% in WMMA (ranging from 6.9% to 32.1%) and 9.8% in GX (ranging from 6.6% to 14.5%), respectively, which were 2.2–36.4 times higher than the literature values used to estimate Hg emission from Hg mining. Furthermore, the average Hg emission factor of AMM in WMMA was much higher than that in GX, indicating that double condensation processes practiced in GX resulted in higher recoveries and lower emission factors compared to single condensation process applied in WMMA. Atmospheric Hg emission was estimated to be 3.7–9.6 metric tons in 2004 for WMMA and 1.3–2.7 metric tons in 2006 for GX, indicating artisanal Hg mining was an important atmospheric Hg emission source in the study area.     

SIMULATING THREE-DIMENSIONAL GROUND WATER RESPONSE IN A SMALL MOUNTAINOUS WATERSHED1

ABSTRACT: Snowmelt from deep mountainous snowpacks is seldom rapid enough to exceed infiltration rates; thus, the source of streamflow in many mountainous watersheds is snowmelt recharge through shallow ground water systems. The hydrologic response and interaction between surface and sub-surface flow processes in these watersheds, which is controlled by basin structure, the spatial distribution of snowmelt, and the hydrogeology of the subsurface, are not well understood. The purpose of this study was to test a three-dimensional ground water model using simulated snowmelt input to simulate ground water response to spatially distributed snowmelt on the Upper Sheep Creek Watershed located within the Reynolds Creek Experimental Watershed in Southwestern Idaho. The model was used to characterize the mountainous aquifer and to delineate the subsurface flow mechanisms. Difficulty in finding a reasonable combination of grid spacing and time stepping within the model was encountered due to convergence problems with the Picard solution to the non-linear variably saturated ground water flow equations. Simulation results indicated that flow may be either unconfined or confined depending on inflow rate and hydrogeologic conditions in the watershed. The flow mechanism had a much faster response time when confined flow occurred. Response to snowmelt from a snow drift approximately 90 m away took only a few hours when flow was confined. Simulated results showed good agreement with piezometer measurements both in magnitude and timing; however, convergence problems with the Picard solution limited applicability of the model.     

从废催化剂中回收钼的新工艺

确定了用新型复合浸取剂从废催化剂中回收钼的最佳工艺条件废催化剂颗粒度１００目焙烧温度７５０℃,焙烧时间１ｈ复合浸取剂中助浸剂质量为５％,浸取固液质量比１：３,浸取温度６０℃,浸取时间６ｈ,在该条件下,钼的浸取率达到９２．７％～９５．５％。