环境样品中多氯联苯残留物的色谱/质谱定量测定

多氯联苯(简称PCB)是全球性的环境污染物之一,实际上它是由一百多种氯化联苯异构体所组成的。为了测定复杂环境样品中的PCB总残留量,Webb等首先提出了“各峰和”定量法,我们亦在先前的工作中采用二种国产PCB标样建立了相应的填充柱色谱定量方法,即分别定量测定样品中各氯化联苯色谱峰所含的PCB量,叠加后得到PCB总残留量。但是有机氯农药的广泛污染经常使PCB的测定受到干扰。我们研究了PCB及几种国内常用有机氯农药的质谱图,找出了一些能相互抗干扰的特征离子,将这些质量色谱图叠加所得的选择离子流可用于定量分析,使我们有可能同时测定几种化合物(见图1),省略了繁杂的化学分离和提纯步骤,缩短了分析时间,避免了处置过程中痕量样品的损失或沾污,增加了测定的可靠性。     

电站冲灰水烟气脱硫的工业应用

利用燃煤电站锅炉冲灰水中碱性物质的作用 ,设计了一套湿法烟气脱硫系统 ,并在 2台小型机组上进行了应用。系统运行情况表明 ,在选择适当的雾化喷嘴后 ,脱硫塔还可以起到对细粉尘的二次净化作用。这种具有脱硫功能的洗涤器可以使燃煤烟气在液气比不大于 0 7的条件下获得 70 %左右的脱硫效率和 90 %左右的除尘效率     

管道内烟气喷雾脱硫的研究

对不同SO2 初始浓度下 ,竖直管道内利用石灰浆喷雾脱除烟气中二氧化硫的方案做了实验研究 ,以模拟石灰液喷雾对燃煤锅炉尾气中SO2 的吸收效果。结果表明 ,可以在较低的钙硫摩尔比下 ,用这一方法使中等浓度SO2 烟气获得较高的脱硫效率。本研究结合双膜理论和双反应面模型 ,对石灰浆滴吸收SO2 的机理给出了解释 ,说明了实验现象和某些类似实验研究的结果。     

The New England Air Quality Forecasting Pilot Program: development of an evaluation protocol and performance benchmark

The National Oceanic and Atmospheric Administration recently sponsored the New England Forecasting Pilot Program to serve as a "test bed" for chemical forecasting by providing all of the elements of a National Air Quality Forecasting System, including the development and implementation of an evaluation protocol. This Pilot Program enlisted three regional-scale air quality models, serving as prototypes, to forecast ozone (O3) concentrations across the northeastern United States during the summer of 2002. A suite of statistical metrics was identified as part of the protocol that facilitated evaluation of both discrete forecasts (observed versus modeled concentrations) and categorical forecasts (observed versus modeled exceedances/nonexceedances) for both the maximum 1-hr (125 ppb) and 8-hr (85 ppb) forecasts produced by each of the models. Implementation of the evaluation protocol took place during a 25-day period (August 5-29), utilizing hourly O3 concentration data obtained from over 450 monitors from the U.S. Environment Protection Agency's Air Quality System network.     

考虑水分影响的煤层气吸附及渗透机理

为定量分析水分含量和孔隙压力变化对煤层气渗流特征的影响,采用ASAP2020型比表面微孔分析仪进行低温液氮吸附试验,并通过等温吸附装置和三轴伺服渗流装置进行不同含水率条件下的煤岩吸附和渗流试验.在此基础上,建立考虑煤岩水分含量影响的吸附模型和煤层气渗透率模型,采用试验数据验证其合理性.结果 表明:在液氮吸附试验中,当相对压力较小时,煤岩吸附作用主要依靠范德华力;当相对压力较大时,其吸附作用则主要为毛细凝聚.在相对压力变化过程中,氮吸附量随相对压力的增大呈增大趋势,同时在相对压力较小时液氮脱附曲线与吸附曲线重合,且存在显著的吸附滞后现象.当煤岩中水分含量相同时,煤层气吸附量随孔隙压力的增大先增大后趋向于平缓,而当孔隙压力恒定时,煤层气吸附量随水分含量的增大呈减小趋势.在吸附作用的影响下,煤岩表面吸附变形量与煤层气吸附量的变化趋势一致.在水分与吸附作用综合作用下,煤岩渗透率随孔隙压力的增大呈先减小后趋于平缓的趋势.当孔隙压力恒定时,煤岩渗透率随水分含量的增大显著减小.基于吸附理论,建立考虑水分影响的煤岩吸附模型及吸附变形表达式.综合考虑水膜及其分离压的影响,进一步构建考虑煤层气吸附-水分耦合作用的煤岩渗透率模型.模型计算值与试验数据具有一致性,可较好地表征煤岩在不同含水量条件下的渗流规律.     

Daily intakes of naturally occurring radioisotopes in typical Korean foods

The concentrations of naturally occurring radioisotopes ((232)Th, (228)Th, (230)Th, (228)Ra, (226)Ra, and (40)K) in typical Korean foods were evaluated. The daily intakes of these radioisotopes were calculated by comparing concentrations in typical Korean foods and the daily consumption rates of these foods. Daily intakes were as follows: (232)Th, 0.00-0.23; (228)Th, 0.00-2.04; (230)Th, 0.00-0.26; (228)Ra, 0.02-2.73; (226)Ra, 0.01-4.37 mBq/day; and (40)K, 0.01-5.71 Bq/day. The total daily intake of the naturally occurring radioisotopes measured in this study from food was 39.46 Bq/day. The total annual internal dose resulting from ingestion of radioisotopes in food was 109.83 muSv/y, and the radioisotope with the highest daily intake was (40)K. These values were same level compiled in other countries.     

大孔树脂对柠檬黄吸附行为的研究

用三种大孔树脂NDA-7、NDA-99和ND-900作为吸附剂,对水溶液中柠檬黄进行吸附,探讨了温度、盐含量和pH值对不同类型树脂吸附行为的影响。实验结果表明,三种树脂对柠檬黄的吸附均符合Freun-dlich公式,在相同温度下,三种树脂对柠檬黄的吸附量大小顺序为ND-900〉NDA-99〉NDA-7;降温和减小溶液初始pH值均有利于三种树脂对柠檬黄的吸附;盐分对三种树脂的吸附效果均有严重的负效应,但是随着盐含量的增加,三种树脂对柠檬黄的吸附曲线又表现出不同的变化趋势。     

Transfer of 137Cs to rice plants from various paddy soils contaminated under flooded conditions at different growth stages

Soil blocks from 18 paddy fields around three Korean nuclear power plant sites were put into lysimeters. Greenhouse experiments were carried out to investigate the (137)Cs transfer from these paddy soils to rice plants for its deposition at different growth stages. A solution of (137)Cs was applied to the flooded lysimeters at 2-3 different stages. The applied (137)Cs was mixed with the topsoil only at the pre-transplanting application. The transfer was quantified with a transfer factor based on the unit-area deposition (TF(a), m(2)kg(-1)-dry). The TF(a) in the pre-transplanting application showed a remarkable variation with the soils. However, the differences in the mean values among the study sites were not statistically significant. The straw TF(a) was 2-3 times higher than the corresponding seed value. The early-tillering stage and booting stage applications resulted in a higher transfer than the pre-transplanting application by factors of, on an average, 2 and 16 for the straws, and 3 and 25 for the hulled seeds, respectively. The (137)Cs transfer was found to correlate negatively with the soil pH and positively with the organic matter content. Based on the present results, the representative (137)Cs TF(a) values for the rice are proposed for use in the whole of Korea for the deposition at three different growth stages.     

Export of dissolved carbonaceous and nitrogenous substances in rivers of the “Water Tower of Asia”

Rivers are critical links in the carbon and nitrogen cycle in aquatic,terrestrial,and atmospheric environments.Here riverine carbon and nitrogen exports in nine large rivers on the Tibetan Plateau—the"Water Tower of Asia"—were investigated in the monsoon season from 2013 to 2015.Compared with the world average,concentrations of dissolved inorganic carbon(DIC,30.7 mg/L)were high in river basins of the plateau due to extensive topographic relief and intensive water erosion.Low concentrations of dissolved organic carbon(DOC,1.16 mg/L)were likely due to the low temperature and unproductive land vegetation environments.Average concentrations of riverine DIN(0.32 mg/L)and DON(0.35 mg/L)on the Tibetan Plateau were close to the world average.However,despite its predominantly pristine environment,discharge from agricultural activities and urban areas of the plateau has raised riverine N export.In addition,DOC/DON ratio(C/N,~6.5)in rivers of the Tibetan Plateau was much lower than the global average,indicating that dissolved organic carbon in the rivers of this region might be more bioavailable.Therefore,along with global warming and anthropogenic activities,increasing export of bioavailable riverine carbon and nitrogen from rivers of the Tibetan Plateau can be expected in the future,which will possibly influence the regional carbon and nitrogen cycle.