硼氢化钾吹气—分光光度法测定污水中硫化物

污水样品用硼氢化钾片剂酸性氢化反应,使硫化物同酸作用转化为Ｈ２Ｓ,并被氢气吹出,以ＮａＯＨ溶液吸收,再用对氨基二甲基苯胺光度法测定。为了应急监测,研制了ＬＳ－１型硫化物快速测试预装置,配用ＤＲ／２０００型便携式分光光度计,可在现场进行了水中硫化物的快速监测。．     

离子色谱法同时测定水中的SeO_3~（2－）和SeO_4~（2－）

用抑制型离子色谱法探讨了ＳｅＯ３（２）和ＳｅＯ４（２－）等七种阴离子的洗脱行为，讨论了共存阴离子的干扰及其消除，建立了测定水中ｓｅＯ３（２－）和ＳｅＯ４（２－）等阴离子的方法．ＳｅＯ３（２－）和ＳｅＯ４（２－）的检测限分别为４０μｇ／Ｌ和５０μｇ／Ｌ．     

增压溶样－冷原子荧光法测定煤样中的汞

采用增压溶样器加７：３：５的ＨＮＯ３－Ｈ２ＳＯ４－ＨＣｌＯ４混合酸处理煤样．用冷原子荧光法测定煤样中的总汞含量。该法的加标回收率为９２．７～１１２．５％，结果令人满意。     

高效液膜分离富集测定微量铜

应用高效乳状液膜技术分离、富集水和土壤样品中微量铜（Ⅱ）．研究了流动载体（Ｐ２０４）、表面活性剂（ＳＰａｎ８０）、膜的增强剂（液体石蜡）、膜溶剂（煤油）和内相解吸剂（２．５ｍｏｌ／ＬＨ２ＳＯ４）等液膜体系，对分离富集微量铜（Ⅱ）的影响．确定了Ｓｐａｎ８０—Ｐ２０４─液体石蜡─煤油─Ｈ２ＳＯ４高效液膜体系的最佳组成和最适宜的实验条件．富集后的溶液用１－（２－吡啶偶氮）－２－萘酚（ＰＡＮ）分光光度法测定铜（Ⅱ）．用本法富集水和土壤中微铜（Ⅱ）．回收率在９９％以上。应用于测定水和土壤中的微量铜．相对标准偏差为１．２％～４．５％。     

底质中汞的快速消解方法

底质中汞的快速消解方法王国朝，王鲁海，周春华，刘新凤（新疆乌鲁木齐市环境科研监测站，８３９０００）底质中汞的消解方法有湿法和于法两种。文献［１．２］介绍的湿法有：Ｈ２ＳＯ４－ＫＭｎＯ４电热板加热和水浴加热法；Ｈ２ＳＯ４－ＨＮＯ３－ＫＭｎＯ４电热板加热...     

异相平衡流动注射分光光度法测定水中痕量SO^2—4

根据异相平衡的原理,确立了用流动注射分光光度法测定水样中痕量ＳＯ＾２－４的新方法。利用Ｂａ（Ⅱ）与偶氮氯磷Ⅲ的二元络合显色反应及ＢａＳＯ４＝Ｂａ＾２＋＋ＳＯ＾２－４进入微溶化合物ＢａＳＯ４反应柱前后吸光值的改变,从而求得ＳＯ＾２－浓度。表观摩尔吸光系数ε＝２．３＊１０＾４Ｌ．ｍｏｌ＾－１．ｃｍ＾－１,ＳＯ＾２－４检的线性范围为０－４０ｍｇ／Ｌ,检测限为０．８０ｍｇ／Ｌ,相对标准偏差为１．２％,试     

高效液相色谱法测定环境水样中嘧磺隆

环境水体中的嘧磺隆在ｐＨ＝２－３的Ｈ２ＳＯ４介质中用二氯甲烷萃取富集，然后用高压液相色谱法分离和紫外光（２５４ｎｍ）检测器检测，外标法定量。用此方法测定了井水和生产单位排放的综合污水中的嘧磺隆，结果满意，最大相对标准偏差为５％，样品加标回收率在９３～１０７％之间，最低检测限量为２ｎｇ，最低检出浓度为０．００４ｍｇ／Ｌ。     

高压蒸汽消化法测定废水化学需氧量的再研究

用＂自控式高压蒸汽消解器＂作为高压蒸汽消化法测定废水化学需氧量的消化装置，详细研究了消化条件，最后确定，消化体系中（１／６）Ｋ２Ｃｒ２Ｏ７浓度为０１ｍｏｌ／Ｌ，Ｈ２ＳＯ４浓度为１０．１ｍｏｌ／Ｌ，催化剂Ａｇ＋浓度为０．０３ｍｏｌ／Ｌ，消化温度为１３０℃，恒温时间为２０ｍｉｎ。用此方法和条件测定了１２种单纯有机化合物和１６种不同工业废水的化学需氧量，与标准回流法相比，相对误差在－５．５－６．０％之间。     

大气环境中二硫化碳分析方法的选择研究

应用气相色谱（ＧＣ）Ｎｉ６３电子捕获检测器（ＥＣＤ），在６２０１红色担体为基体，涂１０％ＯＶ－１０１固定液的玻璃柱上，以甲苯作吸收液，对大气环境中微量二硫化碳能够进行定量检测，其最低检出浓度可达６×１０－６ｍｇ／ｍｌ（进液体样品１μｌ）；方法精密度为３．４％，ＳＯ２、Ｈ２Ｓ气体物质不干扰测定。经现场实际环境样品测试，此方法能够适用于大气环境中微量ＣＳ２的分析工作，为大气环境监测微量ＣＳ２的分析建立了一个比较合适的方法。     

用恒波长同步荧光光谱法测定西班牙Galicia地区饮用水和地表水中多环芳香烃

１实验１１试剂使用了萤蒽、苯并［ａ］芘、苯并［ｂ］萤蒽、苯并［Ｋ］萤蒽、茚并－［１２３－ｃｄ］芘和苯并［ｇｈｉ］艹北标准试剂,颗粒状无水Ｎａ２ＳＯ４,正己烷和分析纯Ｈ２ＳＯ４。Ｈ２ＳＯ４在使用前用正己烷洗涤。在测定前,所有试剂的纯度都在分析条件下进...     

流动注射对氨基二甲基苯胺光度法测定水体中的硫化物

为了克服分光光度法反应时间难以控制引起的方法精密度、准确度不高的弱点，采用流动注射技术与分光光度法相结合的方法，用微机化流动注射分析仪准确控制时间，优化了实验条件，建立了测定痕量硫化物的流动注射分光光度方法。分析速度每小时80次，擎一质量浓度在0．02～0．8mg／L与吸光度A具有良好的线性关系。方法直接测定海水和鱼塘水中的硫化物获得满意的结果，回收率分别为100．28％和97．13％。     

Evolution of water chemistry in natural acidic environments in Yangmingshan,Taiwan

In Yangmingshan National Park, located in the northern part of the Taiwan Island, there is a very rare area where fish (Channa asiatica) live in spite of acid environments. The origin of the acid in local acid ponds and rivers and the evolution of the water chemistry are discussed on the basis of sulfur stable isotope ratios and chemical equilibria. One of the sources of the acid is sulfuric acid, which is derived from the oxidation of hydrogen sulfide in volcanic gas gushing out from fumaroles around the area and from acid deposition supplied from Taipei City. It is also derived from the oxidation of pyrite: the sulfur stable isotope ratios of delta 34S of +1@1000 to +4@1000 (relative to CDT) of sulfate in acid pond waters (pH 3-4) could be related to those of hydrogen sulfide in volcanic gas, pyrite in local pond sediments and soils, and sulfate in rain water. One acid source is sulfuric and hydrochloric acids arising in springs from geothermal activity: the delta 34S values were characterised by +13@1000 to +17@1000 sulfate-S, which was provided by a disproportionation reaction of sulfur dioxide in the depths. Another acid source could be the oxidation of iron(II). Under acidic conditions, the water-rock reaction gives rise to high concentrations of aluminium and iron. While flowing down surface streams, iron(II) is oxidised to iron(III) and then hydrolysed to cause further acidification under oxic conditions. The concentrations of iron and aluminium are controlled by redox and dissolution equilibria.     

Feasibility of the hydrogen sulfide test for the assessment of drinking water quality in post-earthquake Haiti

In 2010, a magnitude 7.0 earthquake struck Haiti, severely damaging the drinking and wastewater infrastructure and leaving millions homeless. Compounding this problem, the introduction of Vibrio cholerae resulted in a massive cholera outbreak that infected over 700,000 people and threatened the safety of Haiti’s drinking water. To mitigate this public health crisis, non-government organizations installed thousands of wells to provide communities with safe drinking water. However, despite increased access, Haiti currently lacks the monitoring capacity to assure the microbial safety of any of its water resources. For these reasons, this study was designed to assess the feasibility of using a simple, low-cost method to detect indicators of fecal contamination of drinking water that could be implemented at the community level. Water samples from 358 sources of drinking water in the Léogâne flood basin were screened with a commercially available hydrogen sulfide test and a standard membrane method for the enumeration of thermotolerant coliforms. When compared with the gold standard method, the hydrogen sulfide test had a sensitivity of 65 % and a specificity of 93 %. While the sensitivity of the assay increased at higher fecal coliform concentrations, it never exceeded 88 %, even with fecal coliform concentrations greater than 100 colony-forming units per 100 ml. While its simplicity makes the hydrogen sulfide test attractive for assessing water quality in low-resource settings, the low sensitivity raises concerns about its use as the sole indicator of the presence or absence of fecal coliforms in individual or community water sources.     

梯度淋洗离子色谱法测定饮用水中6种阴离子

采用离子色谱法同时测定饮用水中F-、Cl-、Br-、NO3-、SO24-、PO34-等6种阴离子,水样经0.22μm滤膜过滤,自动淋洗发生器产生20 mmol/L～40 mmol/L KOH淋洗液梯度洗脱,在流量0.25 mL/min条件下采用IonPac AG19保护柱和IonPac AS19分离柱分离和定量。方法线性良好,6种阴离子的检出限为0.005 mg/L～0.057 mg/L,标准溶液平行测定6次,测定值的RSD在0.5%～2.2%之间,水样加标回收率在83%～106%之间。     

热脱附/气相色谱法测定空气中含硫化合物

以固体CO2为冷却试剂，使空气中含硫化合物有效富集在-70℃条件下TANEX复合吸附管内，样品管在热脱附装置中120℃下解吸后，采用气相色谱脉冲式火焰光度检测器测定硫化氢、甲硫醇、二甲二硫和甲硫醚，优化了试验条件。4种含硫化合物检出限为0.1ng—0.5ng，标准管测定的RSD为12.7％—16.3％，实际气样加标回收率为78.3％—87.7％。     

毛细管低温吸附气相色谱法同时测定空气中痕量甲硫醇和硫化氢

建立了毛细管低温吸附气相色谱同时测定空气中痕量甲硫醇和硫化氢的方法，介绍了冷冻吸附装置的制备方法和样品冷凝吸附流程。甲硫醇和硫化氢分别在0.467ng～5.16ng和0.327ng～3.60ng范围内线性良好，当进样体积为1L时，检出限为0．205μg/m^3和0．213μg／m^3，空白加标平均回收率为88．6％和90．2％，RSD为6.0％和6．5％。     

硫化氢检测管的研制

经过条件优化试验，研制出硫化氢检测管，其显色长度与硫化氢浓度呈线性相关，对硫化氢标气7次测定的变异系为14．6％，平均相对误差为2％，小于15％，一次测定最大相对误差为18．8％，小于25％，符合国家标准（GB7230－87）的要求，与化学法比较，2种方法测试结果无显著性差异。     

水中硫化氢的溶解规律

对气体在水中的溶解机制进行了分析，并结合实验数据导出了硫化氢在水中溶解度的预测公式，该预测公式准确度较高，其平均绝对误差及平均相对误差分别为０．０２６ｇ／Ｌ和０．０６２％．     

Preservation of sulfidic waters containing dissolved As(III)

Solutions containing variable concentrations of sulfide (0 to 31 ppm) and arsenite (0.35 to 10 ppm) were subjected to several different preservation treatments. As predicted by equilibrium thermodynamics, at near-neutral pH the experimental solutions were undersaturated with respect to orpiment (As2S3). However, upon acidification to pH 2 with HCl or HNO3, instantaneous precipitation of poorly crystalline As2S3 occurred in sulfidic solutions which resulted in the loss of dissolved arsenite. These results have implications concerning the practice of acidifying water samples containing hydrogen sulfide with HCl or HNO3 for the purpose of preserving total arsenic values. If a near-neutral water sample contains 1 ppm arsenite and as little as 0.4 ppm sulfide, loss of dissolved arsenic will occur upon acidification. An alternative three-step preservation method involving base addition, oxidation, and acidification is proposed and investigated as an appropriate technique for preserving sulfide-bearing aqueous samples for total arsenic.     

Geochemical characteristics of inorganic sulfur in Shijing River, South China

Different inorganic sulfur species distributed in overlying water, pore water and sediment in a heavily polluted river were determined. The concentrations of S(2-) and SO(4)(2-) in the overlying water were much more than those in the pore water. This result perhaps indicates the S(2-) was mainly from discharged wastewater, not from sediment resuspension. In the sediments, acid-volatile sulfide, chromium(ii)-reducible sulfide, and elemental sulfur were determined by a modified diffusion method. The results indicate that acid-volatile sulfide was the dominant component of the reduced inorganic sulfur, making up about 62% of the total reduced inorganic sulfur.