大气中氯苯类化合物在常用吸附剂上的性能探讨

通过比对6种吸附剂对氯苯类化合物的吸附性能,同时考察不同废气温度、湿度条件下活性炭对氯苯类化合物的吸附-解吸性能,表明活性炭对氯苯类化合物的吸附性能及在二硫化碳介质中的解吸效能与标准规定的GDX系列无显著性差异。将活性炭管吸附采样用于监测某化工企业厂界无组织排放废气中的氯苯类化合物,结果 1,4-二氯苯和1,2,4,5-四氯苯检出。     

固相膜萃取-高效液相色谱法测定地下水中的多环芳烃

采用C18固相膜萃取对地下水中15种多环芳烃进行富集净化,以二氯甲烷作洗脱溶剂,高效液相色谱法,荧光检测器测定。对萃取、浓缩和色谱条件进行优化,在1．ooixg／L～40．0μg／L范围内测定标准系列溶液并绘制标准曲线,相关系数R2〉0．999;15种多环芳烃的仪器检出限为0．4ng／L～3．0ng／L;对地下水样品加标,平均回收率在75．7％～96．7％之间;标准溶液平行测定7次的RSD为3．1％～11．9％。     

高氟水沸石除氟的效果研究

通过静态搅拌实验和恒温震荡实验,研究了接触时间、pH、温度及反复使用次数对沸石除氟效果的影响.结果表明,在适宜的条件下,沸石除氟效果随着使用次数的增多有上升趋势,除氟效果良好,适用于我国高氟水地区.     

高效液相色谱法同时测定苯酚及其氯化中间产物

采用高效液相色谱法同时测定次氯酸钠氧化降解苯酚过程中苯酚及其5种氯化中间体,确定了检测波长,讨论了pH值对测定的影响。方法线性良好,苯酚、2-氯苯酚、4-氯苯酚、2,6-二氯苯酚、2,4-二氯苯酚、2,4,6-三氯苯酚的检出限分别为0．01mg／L、0．02mg／L、0．02mg／L、0．02mg／L、0．02mg／L、0．02mg／L,标准溶液测定的相对标准偏差≤0．8％,样品加标回收率为96．0％～102％。     

气相分子吸收光谱法测定硝酸盐氮时还原时间的影响

<水和废水监测分析方法>(第四版)要求将装有水样和盐酸溶液反应瓶置于70±2℃的恒温水浴中恒温10min后接回仪器管路,加入0.5ml三氯化钛溶液,启动仪器测定吸光度.     

多环芳烃测定中净化方法的研究

对多环芳烃测定中的净化方法进行研究,为了选出最佳净化柱,在一定条件下分别采用硅胶LC-Si、弗罗里LC-Florisil和C18固相萃取净化柱对一定浓度的多环芳烃标准溶液进行净化,测定吸附后流出液多环芳烃浓度,计算吸附率;测定洗脱后流出液多环芳烃浓度,计算洗脱率。测定结果为硅胶、弗罗里和C18固相萃取净化柱对多环芳烃的吸附率分别在87．1％～100％,99．5％～100％和96．6％～100％之间,洗脱率分别在0～106％,78．7％．109％和79．0％～115％之间。结果表明,GC／MS内标法测定样品中多环芳烃使用最理想的净化柱为弗罗里净化小柱,其次为C18净化小柱,最后为硅胶净化小柱。     

区域土壤中氯苯类化合物测定及分布研究

以区域内16个土壤样品为研究对象,采用超声波萃取法对样品中的氯苯类污染物进行提取,并用气相色谱仪分类和测定,以保留时间定性,外标法定量。结果表明,利用超声波提取土壤中氯苯类是可行的,并能够进行分类检出;预处理中提取的最佳、合理的溶剂为正己烷;实验还得出了11种氯苯类化合物在18min内全部流出的最佳色谱条件。检测数据显示区域土壤内主要氯苯类污染物为二氯苯、四氯苯和六氯苯。     

紫外分光光度法测定水和废水中硫化物

对紫外分光光度法测定水和废话中硫化物的方法进行了研究,试验了稳定时间、干扰物质、碱溶液浓度对测定的影响,提出了最佳测定条件。该方法检测限为０．０４ｍｇ／Ｌ,相对标准偏为１．４％,加标回收率在９１．６％～１０１．９％之间。     

高效液相色谱法测定饮用水中苯并[a]芘

本文采用高效液相色谱-荧光检测器法,用反相C18柱,在乙腈：水（V／V）=90：10作为流动相,检测波长：λEx=265nm,λEm=410nm,流速为1．5mL／min的条件下对饮用水中苯并[a]芘进行了方法学考查,本方法对苯并[a]芘的线性相关系数等于0．9998,RSD为1．46％,平均回收率为93．1％,方法操作简便、准确可靠、灵敏度较高。     

密闭微波消解电感耦合等离子体发射光谱(ICP-AES)法同时测定大气颗粒物PM10中的18种无机元素

建立了测定大气颗粒物PM10中18种无机元素的密闭微波消解电感耦合等离子体发射光谱法。考察了微波消解体系和消解条件,选取了适宜的仪器工作条件和最佳的分析谱线,合理地进行了背景扣除,并对共存元素的干扰情况进行了研究。样品采用硝酸-盐酸-过氧化氢-氢氟酸体系进行消解并经饱和硼酸溶液络合后上机测定,测定值与参考样品标准值相符,主量元素的方法精密度(RSD%)小于3%,次量、微量元素的方法精密度小于10%。各元素的检出限在0.0001~0.0141mg/L之间,回收率在90%~110%之间,应用建立的方法对北京市的颗粒物膜样品进行了分析。     

Determination of CH4, CO2 and N2O in air samples and soil atmosphere by gas chromatography mass spectrometry, GC-MS

A method for determination of the climate gases CH4, CO2 and N2O in air samples and soil atmosphere was developed using GC-MS. The method uses straightforward gas chromatography (separation of the gases) with a mass spectrometric detector in single ion mode (specific determination). The gases were determined with high sensitivity and high sample throughput (18 samples h(-1)). The LOD (3sigma) for the gases were 0.10 micro L L(-1) for CH4, 20 microL L(-1) for CO2 and 0.02 microL L(-1) for N2O. The linear range (R2 = 0.999) was up to 500 microL L(-1) for CH4, 4000 microL L(-1) for CO2 and 80 microL L(-1) for N2O. The samples were collected in 10 mL vials and a 5 microL aliquot was injected on column. The method was tested against certified gas references, the analytical data gave an accuracy within +/-5% and a precision of +/-3%. The presence of < or = 10% by volume of C2H2 (often used experimentally to prevent N2 formation from N2O) did not interfere with detection for the targeted trace gases.     

Study on determination of iron,cobalt, nickel,copper, zinc and manganese in drinking water by solid-phase extraction and RP-HPLC with 2-(2-quinolinylazo)-5-diethylaminophenol as precolumn derivatizing reagent

A new method for the determination of iron, cobalt, nickel, copper, zinc and manganese in drinking water by the reversed-phase high-performance liquid chromatography (RP-HPLC) with 2-(2-quinolinylazo)-5-diethylaminophenol (QADEAP) as precolumn derivatizing reagent was studied in this paper. The iron, cobalt, nickel, copper, zinc, and manganese ions react with QADEAP to form color chelates in the presence of cetyl trimethylammonium bromide (CTMAB) and acetic acid-sodium acetic buffer solution medium of pH 4.0. These chelates were enriched by solid-phase extraction with a Waters Nova-Pak C18 cartridge and eluted the retained chelates from the cartridge with tetrahydrofuran (THF). The enrichment factor of 100 was achieved. Then the chelates were separated on a Waters Nova-Pak C18 column (3.9 x 150 mm, 5 microm) by gradient elution with methanol (containing 0.2% of acetic acid and 0.1% of CTMAB) and 0.05 mol L(-1) acetic acid-sodium acetic buffer solution (containing 0.1% of CTMAB) (pH 4.0) as mobile phase at a flow rate of 0.5 ml min(-1), and monitored with a photodiode array detector from 450 approximately 700 nm. The detection limits (S/N = 3) of iron, cobalt, nickel, copper, zinc and manganese are 0.8, 1.1, 0.9, 1.1, 1.5 and 2.0 ng L(-1), respectively, in the original sample. This method can be applied to determination at the microg L(-1) level of iron, cobalt, nickel, copper, zinc and manganese in drinking water with good results.     

Adsorption studies and the removal of dissolved metals using pyrolusite as adsorbent

The adsorption of metals from aqueous solutions of Pb²⁺, Zn²⁺ and Mg²⁺ on naturally occurring pyrolusite have been studied. The chemical stability of the pyrolusite has been determined in NaOH, H₂SO₄, HNO₃, HCl, NaCl and NK₄Cl solutions of various concentrations. Adsorption of the metal ions followed the order Pb²⁺>Zn²⁺>Cd²⁺.The maximum adsorption of Pb²⁺ (100%) occurred at pH 7. the relation between the amount of Pb²⁺ adsorbed per unit weight of pyrolusite and the concentration of Pb²⁺ at equilibrium follows the Freundlich adsorption isotherm.The efficiency of pyrolusite has been demonstrated by removing lead from synthetic waste water. 100% and 96% removal of lead have been achieved from synthetic waste water containing 5 mg l^–1 and 120 mg l^–1 of Pb²⁺ respectively at pH 7. The results of these studies suggest that pyrolusite might provide an economical method for the removal of lead from industrial waste water.     

原生动物与BOD_5相关性的研究

本文着重研究了原生动物平衡期及密度与ＢＯＤ５浓度的相关性。研究结果表明，原生动物平衡期与ＢＯＤ５的浓度有着ｙ＝１５６２７·ｅ０２４０·ｘ的指数关系，相关性为显著相关；原生动物密度与ＢＯＤ５浓度有着ｙ＝１１３４＋００３６·ｘ的线性关系，相关性为高度相关     

Development of a novel passive sampling system for the time-averaged measurement of a range of organic pollutants in aquatic environments

A new sampling system has been developed for the measurement of time-averaged concentrations of organic micropollutants in aquatic environments. The system is based on the diffusion of targeted organic compounds through a rate-limiting membrane and the subsequent accumulation of these species in a bound, hydrophobic, solid-phase material. It provides a novel and robust solution to the problem of monitoring in situations where large temporal fluctuations in pollutant levels may occur. Accumulation rates are regulated by choice of diffusion-limiting membrane and bound solid-phase material and have been found to be dependent on the physico-chemical properties of individual target analytes. Two separate prototype systems are described: one suitable for the sampling of non-polar organic species with log octanol/water partition coefficient (log P) values greater than 4, the other for more polar species with log P values between 2 and 4. Both systems use the same solid-phase material (47 mm C18 Empore disk) as a receiving phase but are fitted with different rate-limiting membrane materials (polysulfone for the polar and polyethylene for the non-polar analytes). The two systems complement each other and together can be used for sampling a wider range of organic analytes than generally possible using current passive sampling techniques. Calibration data are presented for both devices. In each case, linear uptake kinetics were sustained, under constant conditions, for deployment periods of between 1 and 9 days. The effects of water temperature and turbulence on sampling rates have been quantitatively assessed. The performance of the system was further investigated by means of field exposures for one and two weeks in marine environments where calibrated samplers were used to determine the time-averaged concentrations of the polar biocides diuron and irgarol 1051. The quantitative results obtained using the passive sampler were compared with those obtained using spot sampling.     

环境样品中C2-C5脂肪羧酸的直接电导离子色谱法分析

叙述离子排斥色谱法分析环境样品中的C2-C5脂肪羧酸,以4%的正丁醇水溶液代替无机酸溶液作淋洗液,使分析物质得到较好地分离,尤其本底电导降低,可使用电导检测器直接检测,不需抑制,从而使灵敏度有很大提高,适合环境样品的分析.     

Soil Organic Carbon (SOC) Equilibrium and Model Initialisation Methods: an Application to the Rothamsted Carbon (RothC) Model

Carbon (C) emissions from anthropogenic land use have accelerated climate change. To reduce C emissions, dynamic models can be used to assess the impact of human drivers on terrestrial C sequestration. Model accuracy requires correct initialisation, since incorrect initialisation can influence the results obtained. Therefore, we sought to improve the initialisation of a process-based SOC model, RothC, which can estimate the effect of climate and land-use change on SOC. The most common initialisation involves running the model until equilibrium (‘spin-up run’), when the SOC pools stabilise (method 1). However, this method does not always produce realistic results. At our experimental sites, the observed SOC was not at equilibrium after 10 years, suggesting that the commonly used spin-up initialisation method assuming equilibrium might be improved. In addition to method 1, we tested two alternative initialisations for RothC that involved adjusting the total or individual SOC pool equilibrium values by regulating the C input during the entire spin-up initialisation period (method 2) and initialising each SOC pool with recently measured SOC values obtained by SOC fractionation (method 3). Analysis of the simulation accuracy for each model initialisation, quantified using the root mean square error (RMSE), indicated that a variant of method 2 that involved adjusting the equilibrium total SOC to observed values (method 2-T) generally showed less variation in the individual SOC pools and total SOC. Furthermore, as total SOC is the sum of all SOC pools, and because total SOC data are more readily available than the individual SOC pool data, we conclude that method 2-T is best for initialising RothC.     

Natural and anthropogenic enrichments of molybdenum, thorium, and uranium in a complete peat bog profile, Jura Mountains, Switzerland

A core from an ombrotrophic Swiss bog representing 12 370 (14)C years of peat accumulation was evaluated as a possible archive of atmospheric deposition of Mo, Th and U. Calcium, Sr, and Ba were also determined to quantify weathering inputs, Mn to follow possible redox transformations, and Rb to identify plant uptake. Each of these elements was determined using ICP-MS, following digestion in a microwave heated autoclave using 3 ml HNO(3) and 0.1 ml HBF(4). Calcium and Sr clearly identify the thickness of the ombrotrophic zone because they are enriched in the minerogenic zone relative to the concentration of mineral matter. The concentration of Ba, however, is proportional to the concentration of mineral matter in all samples, and is not added to peat column by weathering reactions at the peat-sediment interface. The lowest element concentrations are found during the Holocene climate optimum (5320 to 8030 (14)C year BP) with the following natural background values (n= 18): Mo 0.08 +/- 0.02 microg g(-1), U 0.029 +/- 0.008 microg g(-1), Ba 5.2 +/- 2.6 microg g(-1), Th 0.070 +/- 0.022 microg g(-1) and Rb 0.63 +/- 0.09 microg g(-1). By far the highest concentrations of Ba, Mn, Rb and Th were found during the Younger Dryas cold climate event (10 590 (14)C year BP) when the flux of atmospheric soil dust was at its post-glacial maximum. Molybdenum and U are elevated in concentration throughout the minerogenic zone because of sediment weathering and this masks the atmospheric signal in samples older than ca. 8000 (14)C year BP (ca. 9000 calendar years). Enrichment factors (EF) calculated using Sc as a conservative, lithogenic element shows that minerogenic peats are enriched in Mo up to 18x and U 26x, relative to the natural "background" values. During the two millennia prior to industrialisation, the accumulation rate of atmospheric Mo averaged 0.23 +/- 0.13 microg m(-2) year(-1). With the onset of the Industrial Revolution, Mo accumulation rates rapidly and continuously increased to approximately 10 microg m(-2) year(-1) in the late 1980s. These data suggest that Mo in atmospheric aerosols today is derived predominately from anthropogenic emissions. Uranium does not show the same enrichment pattern which suggests that steel-making rather than coal combustion is the primary source of atmospheric Mo contamination at this site.     

Water quality test based on dielectrophoretic measurements of fresh water algae Selenastrum capricornutum

A method is described whereby dielectrophoresis of algal cells is used to perform rapid water quality analysis, specifically detecting the presence of CuSO4. The dielectric collection spectrum of the fresh water alga Selenastrum capricornutum was determined for a range of concentrations of CuSO4 from 25 mg L(-1) to 0.25 mg L(-1) for exposure times of 15 min and 18 h. In all cases increasing the concentration of CuSO4 reduced cell collection, but a step reduction was observed in collection between 2 mg L(-1) and 5 mg L(-1). This method has potential for forming a rapid, low-cost test for water quality with broad specificity and significantly reduced analysis time compared to current methods.     

On-road emission factors from light-duty vehicles measured in Hsuehshan Tunnel (12.9 km), the longest tunnel in Asia

This study is based on 82 days of continuous air-quality monitoring using two mobile monitoring vans provided by the Taiwan Environmental Protection Administration (TEPA). The purpose of the study is to reveal variations of air quality without forced ventilation from on-road emissions of light-duty vehicles (LDV) inside the Hsuehshan Tunnel. Since it was opened to traffic in June 2006, only LDV have been allowed to pass the Hsuehshan Tunnel, the longest tunnel in Taiwan and in Asia. The hourly concentrations of air pollutants at four monitoring sites inside the tunnel (pollutant: downslope entrance, downslope exit, upslope entrance, upslope exit) are as follows: (CO: 6.9 +/- 5.4, 13.6 +/- 8.7, 4.6 +/- 3.2, 14.6 +/- 8.0 ppm), (NO(X): 534 +/- 311, 1198 +/- 640, 460 +/- 242, 1704 +/- 692 ppb), (SO2: 7 +/- 5, 18 +/- 10, 9 +/- 4, 26 +/- 10 ppb), (NMHC: 1.9 +/- 2.5, 3.5 +/- 3.0, 0.8 +/- 0.9, 2.7 +/- 1.9 ppm), (PM10: 50 +/- 28, 62 +/- 29, 59 +/- 25, 85 +/- 30 microg m(-3)), and (PM(2.5): 31 +/- 18, 45 +/- 22, 35 +/- 18, 62 +/- 23 microg m(-3)). The emission factors (EFs) from LDV in this study (pollutant: downslope EF, upslope EF in mg veh(-1) km(-1)) is estimated respectively as follows: (CO: 909 +/- 469, 1468 +/- 631), (NO(X): 145 +/- 67, 331 +/- 166), (SO2: 3 +/- 2, 6 +/- 3), (NMHC: 96 +/- 65, 121 +/- 63), (PM10: 2 +/- 2, 5 +/- 4), and (PM(2.5): 2 +/- 2, 4 +/- 3). It shows that the upslope pollutant EFs are twice as big as those of the downslope. However, among these EFs, the NMHC EF is less affected by the road gradient. Likewise, its upslope EF is only 1.3 times as big as that of the downslope. In summary, the results are useful for examining the emissions from the local fleet of vehicles under the driving conditions present during the study and for observing the changes in fleet emission rates upon future replication of the study.