含氰水样中硫化物和碳酸盐去除方法探讨

含氰水样中含有硫化物或碳酸盐时会严重干扰测定,需加以消除.水样中硫化物的去除方法,在文献中介绍的是硫化物沉淀法,即先把水样加碱调到pH>11,然后加硝酸银或碳酸镉,形成硫化物沉淀,再将沉淀过滤、洗涤,弃掉沉淀物,滤液供蒸馏用.笔者认为,此法有许多不妥之处.①水样调pH>11后,氰离子和硫离子碱性条件下生成硫氰离子,产生负干扰.②加入硝酸银或碳酸镉量难以掌握,加入量少,硫化物去除不完全;加入量太多,一方面造成浪费,另一方面氰化物与其     

有机硫自动分析仪在石化园区环境空气监测中的应用

有机硫化物是环境空气典型恶臭物质,因环境浓度低和化学稳定性差,其定性定量分析是公认的难题。研究筛选5台市场主流有机硫自动分析仪,在石化园区开展实测以考察仪器在复杂环境下的适用性。结果表明:各仪器能对环境空气中有机硫物质持续有效监测,多数仪器所测甲硫醇、甲硫醚、二甲二硫醚和二硫化碳浓度的时间变化趋势较一致,其中D和E仪器的4种有机硫监测数据均呈显著相关,其相关系数分别为0.67、0.80、0.67和0.70(P0.01)。不同仪器测得有机硫数据呈正偏态分布,但浓度分布区间差异较大,表明部分仪器对污染物的富集、脱附和检测等环节仍需改进。D和E仪器监测的有机硫浓度明显升高时,监测点位附近的GC-FID/PID测得总挥发性有机物浓度较其他时段升高,且周边区域异味投诉量增加,说明这2台仪器监测数据能较好地反映该园区有机硫化物的污染特征。研究可为石化园区有机硫自动监测仪的设备选型提供依据。     

酸化吹气-气相分子法测定固体废物中硫化物

采用酸化吹气装置结合气相分子吸收光谱仪对固体废物中硫化物进行测定。考察酸性试剂的选取、加入量及酸化吹气反应时间对测定结果的影响,得出最佳的前处理条件为加入10 mL体积比为1∶1的磷酸,酸化吹气45 min。为确保吸收液中硫化物不被氧化,向吸收液中加入一定量抗氧化剂。结果表明:当抗氧化剂加入量为5 mL时,吸收液中硫化物的浓度可在6 h内保持稳定。方法的标准曲线相关系数为0.999 9,检出限为0.19 mg/kg,实际固体废物样品的相对标准偏差为2.7%～6.1%,加标回收率为91.0%～93.0%。将气相分子吸收光谱法和亚甲基蓝分光光度法进行比对,结果表明2种方法对固体废物中硫化物的测定无显著差异。     

荧光光度法测定水样中痕量硫化物

研究了以汞 ( ) -2 -(2′-羟基苯基 )苯并咪唑荧光熄灭体系测定痕量硫化物的新方法。实验表明 ,当硫离子浓度在 1 .0× 1 0 - 8～ 9.5× 1 0 - 6 mol/ L范围内时 ,体系荧光强度与硫离子浓度呈线性关系 ,检测下限达 9.0× 1 0 - 9mol/ L,采用酸化 -吹气法可消除共存离子的影响。方法具有很高的灵敏度 ,同时表现出良好的稳定性和重现性。用于实际水样中硫化物的测定 ,获得了满意的结果     

气相色谱法测定土壤中挥发性硫化物

采用带硫化学发光检测器的气相色谱(GC-SCD),同时分离并测定土壤中硫化氢、羰基硫、甲硫醇、甲硫醚、二硫化碳和二甲基二硫等6种挥发性硫化物。通过优化仪器工作条件,使该方法在0.521μg/L~65.7μg/L范围内线性良好,方法检出限为0.58μg/L~1.76μg/L,标准气体5次测定结果的RSD为0.9%~8.3%。用该方法分析土壤在强还原条件下挥发性硫化物的排放量,结果表明,上述6种挥发性硫化物均有产生,且随培养时间的延长排放速率增加,硫化氢是其主要气体产物,占挥发性硫化物排放总量的79.1%。     

吹扫捕集-气相色谱联用同时测定水中致嗅挥发性有机硫化物

建立了一种利用吹扫捕集(PT)-气相色谱(GC)/火焰光度检测器(FPD)同时测定水中16种致嗅类有机硫化物的分析方法。研究并优化了捕集阱类型、吹扫温度、吹扫时间,解吸温度以及解吸时间对PT的影响。实验表明:大部分硫醚类和硫醇类化合物分别在1~100 ng/L和3~300 ng/L范围内线性良好,线性相关系数大于0.99;相对标准偏差小于9.47%(n=6);加标回收率为81.68%~115.18%。定量下限(10倍信噪比)范围从0.19 ng/L(二乙基二硫醚)到2.67 ng/L(2-甲基-1-丙硫醇)。采用此方法对北京市3条河流水样进行了检测,除1-丙基二硫醚和2-甲基-2-丙硫醇外,其他14种有机硫化物都有检出,质量浓度为1.95~1 282.35 ng/L。     

SUMMA罐采样-GC×GC-TOFMS同时测定空气中有机硫化物

研究了SUMMA罐采样-全二维气相色谱-飞行时间质谱法测定环境空气中有机硫化物。采用SUMMA罐采集样品,自动进样器进样,三级冷阱预浓缩样品,全二维气相色谱-飞行时间质谱法(GC×GC-TOFMS)测试分析,以较长的非极性柱Rxi-5MS(30 m×320μm×1.0μm)作为第一维柱,较短的中等极性柱DB-17MS(2.0 m×0.1 mm×0.1μm)作为第二维柱,对环境空气中的有机硫化物进行了定性定量分析。结果表明,该方法特性不仅满足方法学要求,而且比《空气和废气监测分析方法》(第4版)推荐的方法更加优异,能够准确、快速地检测环境空气中有机硫化物。     

流氰酸盐分光光度法测定水和废水中硫化物

目前硫化物的测定方法有对氨基二甲基苯胺光度法、碘量法、硫离子选择电极电位滴定法等。这些方法都存在干扰物质多且难以消除,测定范围窄,精密度和准确度都差的缺点。为了寻求一个快速灵敏的测定硫化物方法,本研究对试剂加入量、pH范围、曲线变化情况、颜色稳定时间、空白值、精密度、准确度、本法与其它方法的对比试验等都进行了分析,确定了最佳测定条件。     

气质联用法测定环境空气中有机硫化物

采用 SUMMA罐采集空气样品，在预浓缩系统中经3级冷阱捕集后，用气相色谱-质谱联用技术测定环境空气中7种痕量有机硫化物。对试验条件进行优化，使得甲硫醇、乙硫醇、甲硫醚、二硫化碳、噻吩、乙硫醚和二甲二硫醚等7种有机硫化物在21．47μg/m3～336．43μg/m3范围内线性良好。试验表明，7种有机硫化物的方法检出限为0．004μg/m3～0．036μg/m3；标准气体平行测定6次结果的 RSD为2．7％～6．2％，加标回收率为92．2％～97．5％。用该方法测定实际空气样品，并与傅立叶红外光谱法测定的结果进行比对，结果令人满意。     

典型恶臭有机污染自动监测技术与应用探究

对比6种主流有机硫自动监测仪的4种有机硫混标测试结果,表明80%仪器的性能指标能满足国家恶臭排放标准中厂界监测的定量要求。复杂环境适用性研究显示,有机硫化物间测定影响相对较小,高浓度标气有残留,定性受到常见挥发性有机物中个别物质干扰。优选3种检测器为FPD的仪器现场连续实测,结果表明甲硫醇、甲硫醚、二甲二硫醚和二硫化碳为石化园区的有机硫常检出物种;3种仪器的监测数据可较好地反映该石化园区空气恶臭污染特征。     

Accumulation of different sulfur fractions in Chinese forest soil under acid deposition

Atmogenic sulfur (S) deposition loading by acid rain is one of the biggest environmental problems in China. It is important to know the accumulated S stored in soil, because eventually the size (and also the "desorption" rate) determines how rapidly the soil water pH responds to decrease in S deposition. The S fractions and the ratio of total carbon/total sulfur (C/S) of forest soil in 9 catchments were investigated by comparing soils at the rural and urban sites in China. The S fractions included water-soluble sulfate-S (SO(4)-S), adsorbed SO(4)-S, insoluble SO(4)-S and organic S. The ratio of C/S in soil at the rural site was significantly (p < 0.05) greater than that at the urban site. C/S of soil in the A horizon was significantly (p < 0.05) and negatively correlated with the wet S-deposition rate. The ratio of C/S presents a better indicator for atmogenic S loading. Organic S was the dominant form in soils at rural sites; contributing more than 69% of the total S in the uppermost 30 cm soil. Organic S and adsorbed SO(4)-S were the main forms of S in soil at urban sites. High contents of water-soluble SO(4)-S and adsorbed SO(4)-S were found in uppermost 30 cm soils at urban sites but not at rural sites. Decades of acid rain have caused accumulation of inorganic SO(4)-S in Chinese forest soil especially at the urban sites. The soil at urban sites had been firstly acidified, and the impacts on the forest ecosystem in these areas should be noticed.     

A decade of monitoring at Swiss Long-Term Forest Ecosystem Research (LWF) sites: can we observe trends in atmospheric acid deposition and in soil solution acidity?

Trends in atmospheric acid deposition and in soil solution acidity from 1995 or later until 2007 were investigated at several forest sites throughout Switzerland to assess the effects of air pollution abatements on deposition and the response of the soil solution chemistry. Deposition of the major elements was estimated from throughfall and bulk deposition measurements at nine sites of the Swiss Long-Term Forest Ecosystem Research network (LWF) since 1995 or later. Soil solution was measured at seven plots at four soil depths since 1998 or later. Trends in the molar ratio of base cations to aluminum (BC/Al) in soil solutions and in concentrations and fluxes of inorganic N (NO(3)-N + NH(4)-N), sulfate (SO(4)-S), and base cations (BC) were used to detect changes in soil solution chemistry. Acid deposition significantly decreased at three out of the nine study sites due to a decrease in total N deposition. Total SO(4)-S deposition decreased at the nine sites, but due to the relatively low amount of SO(4)-S load compared to N deposition, it did not contribute to decrease acid deposition significantly. No trend in total BC deposition was detected. In the soil solution, no trend in concentrations and fluxes of BC, SO(4)-S, and inorganic N were found at most soil depths at five out of the seven sites. This suggests that the soil solution reacted very little to the changes in atmospheric deposition. A stronger reduction in base cations compared to aluminum was detected at two sites, which might indicate that acidification of the soil solution was proceeding faster at these sites.     

Recovery of sulfate saturated soils in the Plynlimon catchments, mid-Wales following reductions in atmospheric S inputs from the 1980s to 2011

Sulfate adsorption capacity of B-horizons of base-poor, predominantly stagnopodzol, soils from the Plynlimon catchments, mid-Wales was determined by combination of laboratory adsorption and desorption isotherms. Results show that sulfate adsorption capacity of a range of stagnopodzol (Histic-stagno-podzol (Leptic), WRB), brown podzolic soil (Histic-umbrisol (Leptic), WRB) and stagnohumic gley (Histic-stagno-gleysol, WRB) B-horizons was positively related to the amounts of extractable (pyrophosphate and oxalate) Fe + Al, with the stagnopodzol and brown podzolic soil Bs horizon having the largest adsorption capacity and stagnohumic gley Bg horizon the smallest adsorption capacity. Results show that dissolved organic carbon (DOC) has a negative but limited effect on sulfate adsorption in these soils. Results obtained from a set of historical soil samples revealed that the grassland brown podzolic soil Bs horizon and afforested stagnopodzol Bs horizon were highly saturated with sulfate in the 1980s, at 63% and 89% respectively, whereas data from some recently sampled soil from two sites revisited in 2010-11 indicates that percentage sulfate adsorption saturation has since fallen substantially, to 41% and 50% respectively. Between 1984 and 2009 the annual rainfall-weighted mean excess SO(4)-S concentration in bulk precipitation declined linearly from 0.37 mg S l(-1) to 0.17 mg S l(-1). Over the same period, flow weighted annual mean stream water SO(4)-S concentrations decreased approximately linearly from 1.47 mg S l(-1) to 0.97 mg S l(-1) in the plantation afforested Hafren catchment compared to a drop from 1.25 to 0.69 mg S l(-1) in the adjacent moorland catchment of the Afon Gwy. In flux terms, the mean decrease in annual stream water SO(4)-S flux has been approximately 0.4 kg S ha(-1) yr(-1), whilst the recovery in stream water quality in the Afon Cyff grassland catchment has been partly offset by loss of SO(4)-S by desorption from the soil sulfur pool of approximately 0.2 kg S ha(-1) yr(-1).     

Atmospheric aerosol concentration level and chemical characteristics of water-soluble ionic species in wintertime in Beijing,China

Total suspended particulate (TSP) samples were collected during wintertime from November 24, 1998 to February 12, 1999 in Beijing. Ionic species including Cl-, NO3(-), SO4(2-), Na+, NH4(+), K+, Mg2+ and Ca2+ were determined by Ion Chromatography (IC). The sum average concentration of all the determined ions accounted for 18.9% of the TSP concentration, and SO4(2-) appeared the dominant ion with an average concentration of 30.84 microg m(-3); the sum mass concentration of SO4(2-), NO3(-), Ca2+ and NH4(+) accounted for about 83.2% of all the eight ions measured. The study indicated that the chemical form of sulfate and ammonium varies with TSP concentration levels. During heavy pollution periods, the average TSP concentration was 0.66 mg m(-3), and the NH4(+)/SO4(2-) molar ratio was low (0.58). It indicated that sulfate may present as CaSO4 and (NH4)2SO4 x CaSO4 x 2H2O. When TSP concentration (average 0.186 mg m(-3)) was relatively low, the NH4(+)/SO4(2-) molar ratio was 1.94, close to the theoretical ratio of 2 of (NH4)2SO4. Under this condition (NH4)2SO4 is expected to exist as the major form of sulfate. When the TSP concentration level was medium (average 0.35 mg m(-3)), the NH4+/SO4(2-) molar ratio appeared an average value (1.27), (NH4)2SO4, (NH4)2SO4 x CaSO4 x 2H2O and CaSO4 are expected to be present in those aerosol particles. Meteorological conditions including wind speed and wind direction were related to the TSP concentration level.     

Mineral Soil and Solution Responses to Experimental N and S Enrichment at the Bear Brook Watershed in Maine (BBWM)

Buried mineral soil-bags and natural solutions were studied as indicators of forest ecosystem response to elevated N and S inputs at the Bear Brook Watershed in Maine (BBWM). The BBWM is the site of a paired watershed manipulation experiment in a northern New England forested ecosystem. The study includes two small (10 ha each) catchments dominated by northern hardwood forests with red spruce in the upper elevations. Treatments consist of (NH4)2SO4 applied to the West Bear watershed six times per year, increasing N and S deposition 3× and 2× above ambient values, respectively. Buried mineral soil-bag changes over time reflected both the native soil environment and the treatments. Most of the treatment effects on mineral soils were evident as higher inorganic S found in the treated watershed soils. Adsorbed SO4 in the buried mineral soil-bags increased by approximately 40% under softwood stands and 50% under hardwood stands over the study period. Hardwood soil solutions responded with significant increases in NO3 and SO4 concentrations that resulted in accelerated cation leaching, primarily Ca and Al. Few differences that could be attributed to treatments were evident in soil solutions under softwoods. No treatment effects were evident in throughfall and stemflow chemistry.     

水和废水中总氮的现场快速分析方法研究

在现行水中总氮分析方法的基础上，利用便携式分光光度计和密封消解管，实验了过硫酸钾氧化、硫酸联氨还原、重氮－偶联反应的最佳条件，讨论了碱性过硫酸钾溶液用量及硫酸联氨溶液用量对分析结果的影响，从而建立了水体总氮的碱性过硫酸盐消解－分光光度分析方法，该方法可在现场简便快速地测定水和废水中的总氮。     

石家庄市大气颗粒物中水溶性无机离子污染特征研究

用超声萃取－离子色谱法分析了石家庄市大气颗粒物中8种水溶性无机离子。结果表明，NO3－、SO2－4、NH4＋及 Ca2＋为主要组分；各个离子的质量浓度均有季节及空间变化差异；不同粒径颗粒物中 SO2－4和 NO3－相关性均很好，NH4＋与 SO2－4、NO3－在细颗粒物中具有良好的相关性，Ca2＋在粗粒子中与 NO3－和 SO2－4的相关性也较好。SO2－4／NO3－质量比季节变化表明，春、夏季固定源与流动源对大气颗粒物贡献相当，秋季流动源贡献较大，冬季固定源贡献较大。PM2．5中SO2与SO2－4、NO2与 NO3－转化率表明，SO2－4、NO3－主要是由二次转化而来。     

Short-term Distributions of Reduced Sulfur Compounds in the Ambient Air Surrounding a Large Landfill Facility

In order to explore the environmental behavior of reduced sulfur compounds (RSC) as malodorous components emitted from diverse source processes, the distribution characteristics of four sulfur (S) compounds - hydrogen sulfide (H₂S), methyl mercaptan (CH₃SH), dimethyl sulfide (DMS: (CH₃)₂S), and dimethyl disulfide (DMDS: (CH₃)₂S₂) – were investigated in a municipal landfill area. In the course of this study, their ambient concentration levels were measured during two time periods from 13 individual spots selected as a function of distance from the center of the landfill site. The results generally indicated the absolute dominance of H₂S over the other S compounds investigated (up to 5 km radius) such that their mean values were found as 1415 (H₂S), 148 (DMS), 20.6 (CH₃SH), and 14.4 ppt (DMDS). When our data were compared in terms of either varying distance from the source or relationship with meteorological conditions, the H₂S data sets were most evident to reflect the potential effects of strong source processes in the landfill environment, relative to other S gases (or to volatile organic compounds measured concurrently). The results of this study further indicated the relatively good correspondence between the measured H₂S concentration level and humans' intuitive sensory of odor and nuisance.     

Characteristics of malodor pollutants and aromatic VOCs around an urban valley in Korea

In this study, the environmental behavior of malodor pollutants (MPs) [including reduced sulfur compounds (RSCs)] and aromatic volatile organic compounds (AVOCs) were investigated around urban valley areas during several field campaigns (February through December 2006). The MPs measured in the study area include the RSCs (H(2)S, CH(3)SH, DMS, and DMDS), ammonia (NH(3)), and styrene (STY); the AVOCs include benzene (BEN), toluene (TOL), ethylbenzene (EB), m,p-xylene (MPX), and o-xylene (OX). The variation of most MP concentrations (except for DMDS) was found to be larger than that of AVOCs. It was found that STY (2,346 +/- 4,867 ppbv) was the most dominant MP followed by NH(3) (447 +/- 285), CH(3)SH (16 +/- 41), and the others (<8). The magnitude of AVOCs was found in the following descending order: TOL (1.4 +/- 2.2 ppbv), EB (1.0 +/- 2.1), MPX (0.9 +/- 2.0), and the others (<0.8). The concentration levels of most MPs on industrial (I) and downwind (D) sites were up to an order of magnitude higher than those at non-industrial (N) and upwind (U) sites. For most AVOCs, the former was ~3 times higher than the latter. For malodor intensity in RSCs, CH(3)SH was the dominant contributor. The concentration difference in target compounds between the sites/periods is likely to be caused by the combined effects such as emission sources, geographical features (e.g., semi-closed topography), and meteorological conditions (e.g., wind directions) in and outside the urban valley.