致变因子COD/SO42-值对废水中硫酸盐去除率的影响研究

利用CSTR 反应器,考察了COD和硫酸盐浓度致变下的COD/SO42-比值对硫酸盐还原的影响.发现在(34±1) ℃、水力停留时间20 h、进水碱度(ALK)300-500 mg/L、pH 6.0-6.2等条件下:①相同 COD/SO42-值下,硫酸盐致变与COD致变时硫酸盐的去除率并不相同,其中硫酸盐致变时的去除率要高于COD致变时的去除率;②要使产酸脱硫反应器保持较高的SO42-去除率(大于80%)和运行稳定性,须将系统的COD/SO42-值控制在不小于2.0的水平.     

Functions of Straw for In Situ Remediation of Acidic Mining Lakes

The addition of straw in combination with Carbokalk, a by-product from the sugar-industry, was successfully used to stimulate microbial alkalinity generation in an acidic mining lake. To get detailed information about functions of straw, anenclosure experiment was carried out. Straw bundles were placedat the sediment surface of an acidic mining lake (ML 111) and thephysiochemical conditions and the microbiology of the sediment-water contact zone were studied. Straw was degraded by anaerobic microorganisms and dissolved organic carbon (DOC) leached from straw bundles. Pigmented flagellates responded to the DOC supply in the water column anda considerable amount of algal carbon was transported to the sediment. Straw addition led to microbial reduction of iron andsulfate in the sediment. Sulfate reduction was observed at a pHof 5.5. The pH, however, was not high enough to precipitate H₂S completely. Thus, some H₂S diffused into the watercolumn, where it was reoxidized. Straw did not create orstabilize an anoxic water body above the sediment. Microbial sulfate reduction and pyrite formation only took place in the sediment,whereas iron reduction also took place in the straw. Straw, however, altered the flow conditions above the sediment surfaceand prevented complete mixing of the profundal water. Straw didnot serve as a substratum for a reactive biofilm. We conclude that the most important function of straw for mining lake remediation is to be a long-term nutrient source for microbialalkalinity generation in the sediment.     

Hysteresis in Reversal of Central European Mountain Lakes from Atmospheric Acidification

Extremely high emissions of S and N compounds in Central Europe (both 280 mmol m^-2 yr^-1) declined by 70and 35%, respectively, during the last decade. Decreaseddeposition rates of SO₄ ^-2, NO₃ ^-, and NH₄ ⁺ in the region paralleled emission declines. The reduction in atmospheric inputs of S and N to mountain ecosystemshas resulted in a pronounced reversal of acidification in the Tatra Mountains and Bohemian Forest lakes. Between the 1987–1990and 1997–1999 periods, concentrations of SO₄ ^-2 and NO₃ ^- decreased (average ± standard deviation) by 22±7 and 12±7 mol L^-1, respectively, in theTatra Mountains, and by 19±7 and 15±10 mol L^-1, respectively, in the Bohemian Forest. Their decrease was compensated in part (1) by a decrease in Ca²⁺ + Mg²⁺ (17±7 mol L^-1) and H⁺ (4±6 mol L^-1), and an increase in HCO₃ ^-(10±10 mol L^-1) in the Tatra Mountains lakes, and (2) by a decrease in Al (7±4 mol L^-1), Ca²⁺ + Mg²⁺ (9±6 mol L^-1), and H⁺ (6±5 mol L^-1), in Bohemian Forest lakes. Despite the rapid decline in lake water concentrations of SO₄ ^-2 and NO₃ ^- in response to reduced S and N emissions, their present concentrations in some lakes are higher than predictionsbased on observed concentrations at comparable emission rates during development of acidification. This hysteresis in chemical reversal from acidification has delayed biological recovery of the lakes. The only unequivocal sign of biological recovery hasbeen observed in erné Lake (Bohemian Forest) where a cladoceran species Ceriodaphnia quadrangular has recentlyreached its pre-acidification abundance.     

酸雨及大气颗粒物中可溶性SO_4~(2-)的流动注射—比浊法测定

本文研究了在一定酸度下,以BaCl_2为沉淀剂,OP(聚乙二醇辛基苯基醚)为保护剂的比浊法测定酸雨及大气颗粒物中SO_4~(2-)含量的分析条件,选择的最佳体系为:BaCl_2·2H_2O(2％)—OP(5％)。SO_4~(2-)含量在0.6—7.2μg1ml范围内呈线性关系,回收率为95～105％,相对平均标准偏差小于2.6％。在此基础上与流动注射仪联用,提高了分析速度,改善了精密度。     

水解酸化-生物接触氧化工艺在抗生素废水处理中的应用

介绍了抗生素废水的难降解、硫酸盐和总氮含量高的特点及其治理的必要性.针对这些特点,水解酸化-生物接触氧化工艺在处理中具有优势.从机理上阐述了该工艺解决上述问题的可行性及实际应用,并进一步指出了需要完善之处.     

从金属切削废料中回收镍和钴生产硫酸镍和氧化钴

以镍钴合金切削废料为原料，通过酸溶、除铁、除铬、镍钴分离等一系列步骤，回收镍和钴，生产硫酸镍和氯化钴，通过试验确定了最佳工艺条件，并对经济效益进行了分析。     

STREAM CHEMISTRY IN THE SOUTHERN BLUE RIDGE: FEASIBILITY OF A REGIONAL SYNOPTIC SAMPLING APPROACH1

ABSTRACT: A pilot study, which was conducted in the Southern Blue Ridge geographical province of the Southeastern U.S., demonstrated the feasibility of a probability-based regional synoptic design for the National Stream Survey, which is a project aimed at estimating the number and percentage of streams in various regions of the U.S. that are acidic or at risk from acid deposition. Estimated population distributions for key chemical variables were not appreciably affected by week-to-week variability in stream chemistry during the spring index period chosen for the study. Differences were observed in estimated acid neutralizing capacity (ANC), nitrate, and pH frequency distributions between spring and summer. Observations made at the downstream node did not represent the chemistry of the entire reach for some variables (ANC and nitrate) as indicated by differences in chemical concentrations between upstream and downstream sampling locations. Coefficients of variation in chemical species were low enough to provide a reasonably stable classification of streams based on ANC. Although median ANC, sulfate, and nitrate concentrations were quite low in the region, the probability of finding streams with ph < 6.3 is less than 1.3 percent at the α= 0.05 confidence level.     

除铊硫酸盐还原菌固定化的优化和表征

采用海藻酸钠和聚乙烯醇等为包埋剂,用包埋法对SRB细菌进行固定化,以固定化小球处理含铊废水的能力和失重率为主要参考指标,通过正交试验确定固定化硫酸盐还原菌(SRB)的最佳比例,并通过研究溶胀度和处理能力来评估该材料的性能。研究发现固定化SRB的最佳包埋比例为:聚乙烯醇为6%,二氧化硅为3%,海藻酸钠为0.5%,活性炭为2%,菌液含量为35%,饱和硼酸中氯化钙为2%。固定化SRB对KCl和Fe Cl3溶液有较强的敏感度,和未包埋细菌空白小球相比,固定化SRB对含铊废水有较强的处理能力,最大处理量能达到207.35 mg/g。通过电镜扫描发现,固定化SRB表面和内部布满密集的微孔,对含铊废水处理起到关键的作用。     

贵阳市水库中硫酸盐还原菌及铁还原菌对甲基汞分布的影响

微生物在汞的甲基化过程中起着关键作用,但关于野外微生物活动对甲基汞分布的影响研究较为缺乏.通过对贵阳市不同污染类型水库中硫酸盐还原菌(SRB)、铁还原菌(DIRB)、甲基汞(MeHg)及相应水质参数分布规律研究,探讨了水库中SRB和DIRB活动在汞甲基化及其分布中所起的作用.在水库上覆水体中,SRB与甲基汞呈显著正相关关系(r=0.398,p0.015,n=37),表明在上覆水体中,SRB为主要的汞甲基化细菌.在污染严重且差异明显的沉积物中,两种微生物对甲基汞分布的影响各不相同.在受矿山酸性废水污染的阿哈水库,由于其过高的SRB含量及其硫酸盐还原活动,导致夏季沉积物表层硫离子大量积累,严重抑制了汞的甲基化过程,使得沉积物孔隙水表层甲基汞明显低于其它两个水库,也低于阿哈水库上覆水体甲基汞含量.在红枫水库,沉积物表层适宜的SRB活动促进了汞的甲基化,硫酸盐还原物硫离子和孔隙水甲基汞存在显著相关性(r=0.674,p0.001,n=31);在百花水库,由于沉积物曾受到严重汞污染,甲基汞峰值主要受到沉积物总汞的影响,和两种微生物活动及其产物均未表现出显著相关性.     

河口潮滩湿地CH4、CO2排放通量对氮硫负荷增强的响应

以闽江河口区高、中潮滩短叶茳芏湿地为研究对象,于2014年6—11月植物生长季进行氮硫负荷增强实验,利用静态箱-气象色谱法测定土壤CH_4、CO_2排放通量,并同步观测相关环境因子.结果表明,氮硫负荷增强对潮滩湿地CH_4、CO_2排放通量的影响不尽一致.与对照相比,NH_4~+-N输入使高、中潮滩CH4排放通量分别提高了(107.53%,7.19%),使高潮滩CO_2排放通量增加了3.39%,中潮滩减少了3.00%;NO_3~--N输入使高潮滩CH4、CO_2排放通量分别增加了(29.99%,16.99%),使中潮滩分别减少了(3.45%,4.77%);SO_4~(2-)-S输入使高、中潮滩CH4排放通量分别减少了(8.99%,7.67%),使高潮滩CO_2排放通量减少了3.87%,中潮滩增加了5.44%;N-S复合输入使高、中潮滩CH4排放通量分别提高了(72.48%,25.66%),CO_2排放通量提高了(13.32%,13.48%).氮硫负荷增强改变了短叶茳芏沼泽生长季CH_4、CO_2排放通量变化规律,但除了NH+4-N处理对高潮滩CH4通量的影响显著外,其他处理影响均未达到显著性水平.相关分析显示,高、中潮滩湿地CH_4、CO_2排放通量与土壤温度,含水率具有显著的正线性相关关系,与土壤电导率相关性不显著.在全球环境问题日益严重背景下,系统研究湿地生态系统温室气体排放的机制与规律,对于准确估算全球温室气体排放量具有重要而直接的意义.