分光光度法测定氯化氢的实验条件改进

硫氰酸汞分光光度法测定大气中的氯化氢,所使用的硫氰酸汞-乙醇溶液配置时间长,浓度低,曲线线性不好,不适用于环境现场监测。通过对氯化氢测定过程中遇到的问题进行分析,对硫氰酸汞-乙醇溶液的配置方法进行改进,提高该溶液的浓度。实验证明,使用定性滤纸过滤后的0.40%硫氰酸汞-乙醇溶液,曲线线性关系好,标样准确度高,适用于现场监测分析。     

污染源及环境空气中氯化氢含量的测定方法

在芳烃生产过程中,产生一定的氯化氢气体,通过无组织或排放筒排放到大气中,监测无组织排放的污染情况必须准确测定氯化氢含量。用弱碱性溶液吸收富集采样,分别用硫氰酸汞分光光度法和离子色谱法进行定量测定吸收溶液中Cl-含量的方法,并对两种方法进行比较。离子色谱法检出限为0.003mg/m3。能同时满足污染源和环境空气中氯化氢监测的要求。     

硫氰酸汞分光光度法测定空气中氯化氢的条件控制

硫氰酸汞分光光度法测定空气中氯化氢，方法试剂空白不稳定，控制显色温度和硫氰酸汞-乙醇溶液的制备是降低并稳定试剂空白的关键所在。本文使用0．40％硫氰酸汞-乙醇溶液，2cm或3cm比色皿，显色温度25℃左右，标准曲线斜率较高，线性关系和准确度较好。     

原油中硫化氢含量检测方法探讨

原油中的硫化氢会对后续工序产生影响,文章重点研究原油中硫化氢含量的检测方法。结果表明:气相色谱法检测范围广,误差小;碘量法操作简便,但存在较大误差;碘量法、激光法、分光光度法、离子色谱法在检测原油中硫化氢含量之前,均需要吹脱原油样品;而电化学法、气相色谱法可以直接检测原油样品;对传感器的研究是今后热点,但要克服原油腐蚀性、黏稠的问题;便携式硫化氢检测仪适合一线操作员工使用。     

空气中硫化氢浓度测定方法标准化研究

前言测定空气中痕量H_2S的方法很多,主要有分光光度法、荧光法、火焰光度法、离于选择电极法、极谱法、气相色谱法、阴极溶出伏安法、间接原子吸收光谱法和微库仓法等。而目前国内测定空营中痕量H_2S主要采用分光光度法,此外也有用荧光法,气相色谱法、离子选择电极法的。本实验仅对分光光度法中以氢氧化镉碱性悬浊液、醋酸锌溶液、锌铵络盐甘油溶液为吸收液,对三种不同型式的吸收管作回收率、精密度、灵敏度的考察,亦考察了SO_2、NO_2对方法的干忧,并通过现场检测进行对比,而对方法本身需改     

水中丙烯腈含量测定方法研究

为方便、快速、准确地测定水溶液中丙烯腈含量,分别对气相色谱法、折光率法和紫外分光光度法进行了研究。以浓度为自变量作标准工作曲线回归方程,线性相关系数R均大于0.998。将气相色谱法与折光率法测定结果进行比较,考察这两种方法在分析高浓度丙烯腈溶液时的准确性。结果表明:当丙烯腈浓度在100~10 000mg/L时,宜采用气相色谱法分析;当浓度大于10 000mg/L时,可以采用操作简单、分析可靠的折光率法;对于100mg/L以下的痕量丙烯腈分析,宜采用紫外分光光度法。     

消解/分光光度法测定废水中CODCr的研究

文章对废水中CODCr测定方法中的快速消解/分光光度法、微波消解/分光光度法和回流消解/滴定法进行了比较。结果显示:快速消解/分光光度法和微波消解/分光光度法两种方法的准确度和精密度都达到质量控制的要求,两种方法分光光度法与回流消解/滴定法测定标准水样的方法相比,CODCr测定结果稍微偏高,但对于废水样品,两种方法的测定结果没有显著差异。快速消解/分光光度法和微波消解/分光光度法值得在环境监测工作中推广应用。     

红外分光光度法测定水和废水中油类的改进

本文对红外分光光度法测定水和废水中的油类的萃取和吸附操作进行了改进。结果表明,该方法的精密度和准确度能达到国家标准的要求,且操作更加方便、快捷,可以应用于日常环境监测分析。     

不同红外光度法对水中石油类分析的研究

本文用两种不同的红外光度法(分散红外分光光度法和非分散红外光度法)分别测定了水中油，对两种不同的红外光度法在分析测试过程中的各种情况进行了分析研究。分析研究结果表明，分散红外分光光度法对不同组成的样品有更好的适应性。     

腐蚀性气体硫化氢测定方法的探讨

腐蚀性气体硫化氢的测定方法最常见的是亚甲基蓝分光光度法和碘量法,这两种测定方法都受到众多因素的影响。对于亚甲基蓝分光光度法而言,采样,标准曲线的绘制,以及样品的分析等过程都会影响硫化氢测定结果的可靠性;同样,对于碘量法,采样,硫代硫酸钠标准溶液的配制,以及样品的分析等过程也都会对测定结果造成影响。     

Some properties of a sequencing batch reactor for treatment of wastewater containing thiocyanate compounds

Thiocyanate (SCN) compounds in photo-processing wastewater (PPWW) could be treated by an SBR system without any release of thiocyanate to the atmosphere during the aeration step. An SCN loading greater than 84 g m(-3)d(-1) showed negative effects on the growth of bio-sludge and removal efficiencies of the system. The acclimatization period of the system was increased with an increase in SCN concentration or loading. The COD, BOD(5), TKN, and SCN removal efficiencies were 96.0 +/- 1.6%, 72 +/- 2%, 49 +/- 5%, and 82 +/- 3%, respectively, under an SCN loading of up to 84 g m(-3)d(-1). The removal efficiency of the system was repressed by SCN due to the repressed growth rate of nitrification bacteria. However, the removal efficiency could be increased with an increase in HRT or a decrease in SCN loading. Also, increases in HRT or decreases in SCN loading led to increased sludge age or solid retention time (SRT) and decreased the sludge volume index (SVI) value. The SRT and SVI of the system with synthetic wastewater containing 840 mg l(-1) SCN under an HRT of 3 days (SCN loading of 280 g m(-3)d(-1)) were 3.9 +/- 0.7 days and 65 +/- 4 ml g(-1), respectively, while they were 11.2+/-0.8 days and 55 +/- 6 ml g(-1), respectively under an HRT of 10 days (SCN loading of 84 g m(-3)d(-1)).     

Mercury speciation in highly contaminated soils from chlor-alkali plants using chemical extractions

A four-step novel sequential extraction procedure (SEP) was developed to assess Hg fractionation and mobility in three highly contaminated soils from chlor-alkali plants (CAPs). The SEP was validated using a certified reference material (CRM) and pure Hg compounds. Total, volatile, and methyl Hg concentrations were also determined using single extractions. Mercury was separated into four fractions defined as water-soluble (F1), exchangeable (F2) (0.5 M NH4Ac-EDTA and 1 M CaCl2 were tested), organic (F3) (successive extractions with 0.2 M NaOH and CH3COOH 4% [v/v]), and residual (F4) (HNO3 + H2SO4 + HClO4). The soil characterization revealed extremely contaminated (295 +/- 18 to 11 500 +/- 500 mg Hg kg(-1)) coarse-grained sandy soils having an alkaline pH (7.9-9.1), high chloride concentrations (5-35 mg kg(-1)), and very low organic carbon content (0.00-18.2 g kg(-1)). Methyl Hg concentrations were low (0.2-19.3 microg kg(-1)) in all soils. Sequential extractions indicated that the majority of the Hg was associated with the residual fraction (F4). In Soils 1 and 3, however, high percentages (88-98%) of the total Hg were present as volatile Hg. Therefore, in these two soils, a high proportion of volatile Hg was present in the residual fraction. The nonresidual fraction (F1 + F2 + F3) was most abundant in Soil 1 (14-42%), suggesting a higher availability of Hg in this soil. The developed and validated SEP was reproducible and efficient for highly contaminated samples. Recovery ranged between 93 and 98% for the CRM and 70 and 130% for the CAP-contaminated soils.     

Influence of eutrophication on the distribution of total mercury and methylmercury in hydroelectric reservoirs

The distribution of mercury (Hg) and the characteristics of its methylation were investigated in Wujiangdu (WJD) and Yinzidu (YZD) reservoirs in Guizhou province, China. The two reservoirs are characterized by high and low levels of primary productivity, respectively. Mercury species in water samples from depth profiles in both reservoirs and from interface water in the WJD were analyzed each season during 2007. The concentrations of total Hg (HgT(unf)) and methylmercury (MeHgT(unf)) in unfiltered water samples from the WJD varied from 3.0 to 18 pmol dm(-3) and from 0.17 to 15 pmol dm(-3), respectively; ranges were 2.0 to 9.5 pmol dm(-3) for HgT(unf) and 0.14 to 2.2 pmol dm(-3) for MeHgT(unf) in the YZD. Elevated methylmercury concentrations in water samples from the bottom water and water-sediment interface demonstrated an active net Hg methylation in the downstream reach of the WJD. There was no discernable Hg methylation occurring in the YZD, nor in the upstream and middle reaches of the WJD. The results suggest that high primary productivity resulting from cage aquaculture activities in the WJD is an important control on Hg methylation in the reservoir, increasing the concentrations of MeHg in water in the Wujiang River basin Southwestern China.     

炸药爆轰气体产物中无机组份的离子色谱分析方法研究

采用超纯水、Na2CO3-NaHCO3NaOH3种不同的吸收液吸收爆轰气体产物、离子色谱进行样品分离、外标法定量,建立了爆轰气体产物中HF、HCl、HCN无机污染物的离子色谱分析方法。研究表明,炸药爆轰气体中合有一定量的HF、HCl和少量的HCN,选择3．2mmol／LNa2C03与1．0mmol／LNaHCO3混合溶液作为爆轰产物中无机组份的吸收液,吸收效率均值太于90％;离子色谱分析方法的相对标准偏差（RSD）小于5．0％,相关系数达到0．9990以上;进样量为100μL时,HF、HCl、HCN的检测限分别为0．04mg／m^3、0．03mg／m^3、0．05mg／m^3。该方法灵敏度高,回收率好,且样品预处理简单。     

Adsorption-desorption characteristics of mercury in paddy soils of China

Mercury (Hg) has received considerable attention because of its association with various human health problems. Adsorption-desorption behavior of Hg at contaminated levels in two paddy soils was investigated. The two representative soils for rice production in China, locally referred to as a yellowish red soil (YRS) and silty loam soil (SLS) and classified as Gleyi-Stagnic Anthrosols in FAO/UNESCO nomenclature, were respectively collected from Jiaxin County and Xiasha District of Hangzhou City, Zhejiang Province. The YRS adsorbed more Hg(2+) than the SLS. The characteristics of Hg adsorption could be described by the simple Langmuir adsorption equation (r2 = 0.999 and 0.999, P < 0.01, respectively, for the SLS and YRS). The maximum adsorption values (Xm) that were obtained from the simple Langmuir model were 111 and 213 mg Hg(2+) kg(-1) soil, respectively, for the SLS and YRS. Adsorption of Hg(2+) decreased soil pH by 0.75 unit for the SLS soil and 0.91 unit for the YRS soil at the highest loading. The distribution coefficient (kd) of Hg in the soil decreased exponentially with increasing Hg(2+) loading. After five successive desorptions with 0.01 mol L(-1) KCl solution (pH 5.4), 0 to 24.4% of the total adsorbed Hg(2+) in the SLS soil was desorbed and the corresponding value of the YRS soil was 0 to 14.4%, indicating that the SLS soil had a lower affinity for Hg(2+) than the YRS soil at the same Hg(2+) loading. Different mechanisms are likely involved in Hg(2+) adsorption-desorption at different levels of Hg(2+) loading and between the two soils.     

The potential of cost-effective coconut husk for the removal of toxic metal ions for environmental protection

Coconut (Cocos nucifera) husk, an agricultural waste, has been thoroughly investigated for the removal of toxic Cd(II), Cr(III) and Hg(II) ions from aqueous media. The parameters like nature and composition of electrolyte, concentration of toxic ions, dosage of coconut husk, and equilibration time between the two phases were optimized for their maximum accumulation onto the solid surface. The effect of common ions on the uptake of metal ions has been monitored under optimal conditions. The variation of retention of each metal ion with temperature was used to compute the thermodynamic quantities DeltaH, DeltaS and DeltaG. The values 18.1+/-0.6 kJmol(-1), 74+/-2 Jmol(-1)K(-1), and -3.8+/-0.04 kJmol(-1) at 298 K; 10.8+/-0.8 kJmol(-1), 48.8+/-2.7 Jmol(-1)K(-1), and -4.6+/-0.3 kJmol(-1) at 298 K; and -37.4+/-2k Jmol(-1), 105+/-7 Jmol(-1)K(-1) and -2.58+/-0.5 kJmol(-1) at 298 K were obtained for Cd(II), Cr(III) and Hg(II) ions, respectively. The sorption data were analysed by applying different sorption isotherms. The sorption capacity and energy were evaluated for each metal ion. The values of the Freundlich constants 1/n and C(m) were 0.92+/-0.04 and 52.6+/-22.2 mmolg(-1); 0.85+/-0.05 and 56.0+/-0.03 mmolg(-1); and 0.88+/-0.03 and 6.84+/-0.45 mmolg(-1) for Cd(II) Cr(III) and Hg(II) ions, respectively. Similarly, the Dubinin-Radushkevich (D-R) constants beta, X(m,) and E were evaluated for the three metal ions. To check the selectivity of the sorbent, sorption of a number of elements was measured under similar conditions. Separation of Zn(II) from Cd(II); Cr(III) from I(I), Zr(IV), Se(IV), and Hg(II) from Se(IV) and Zn(II) can be achieved using this sorbent. This cheap material has potential applications in analytical chemistry, water decontamination, industrial effluent treatment and in pollution abatement.     

微波消解火焰原子吸收光谱法测定茶叶中的锌

采用微波消解样品,用火焰原子吸收法直接测定茶叶中的锌含量。回收率85.98%~118.62%,相对标准偏差为1.7%。方法准确、操作简便,可实现同一样品的快速测定,且最大限度地减少了对测定的干扰。微波消解作为一种样品制备方法,在茶叶样品预处理方面,避免了传统湿法消解的限制,具有传统碱式干法消解与酸浸提法无法比拟的优点。     

满度漂移对红外分光光度法测定废水中石油类物质的影响

红外分光光度法是测废水中石油类物质的国家标准分析方法,但仪器在使用过程中,满度会发生变化。满度的漂移对实验数据准确性的影响很大,尤其是低浓度水样。本文讨论了红外分光光度法测定水体中石油类物质满度对实验数据的影响。     

单标多点校正组合英蓝超滤测定地表水中多种阴离子

建立了利用组合单标多点校正和英蓝超滤单元的离子色谱法测定地表水中F-、C1-、NO3-、S0424—4-种离子的方法,方法操作简便,灵敏度高,线性范围广,抗干扰能力强,可同时快速测定不同数量级浓度的离子,降低了配置标准品和样品前处理的复杂性,减少了因前处理带来的干扰。     

Mercury sequestration in forests and peatlands: a review

Nearly all Hg in vegetation is derived directly from the atmosphere. Mass of Hg in forest vegetation (roughly 0.1 mg m(-2)) is about an order of magnitude smaller than that in the forest floor (1 mg m(-2)) and two orders of magnitude smaller than that in the mineral soil (10 mg m(-2)). Mass of Hg in peat (20 mg m(-2)) is greater than the sum of that in mineral soil and the forest floor; wetlands usually sequester more Hg than associated uplands. The strong relationship of Hg to organic matter, associated with binding by reduced S groups, is fundamental to understanding Hg distribution and behavior in terrestrial systems. The stoichiometry of the Hg-C relationship varies; Hg-S relationships, though less variable, are not constant. Because of the Hg-organic matter link, landscape conditions that lead to differential soil organic matter accumulation are likely to lead to differential Hg accumulation. The ratio of methylmercury (MeHg) to total Hg is generally low in both vegetation (near 1.5%) and soil (<1%), but areas of poorly drained soils and wetlands are sites of MeHg production. The annual emission of anthropic Hg from the 48 contiguous states of the USA (144 Mg) is two orders of magnitude less than the pool of Hg in forests of those states (30,300 Mg). Peatlands, less than 2% of total land area, sequester more than 20 times annual emissions (2930 Mg). If global climate change affects C storage it will indirectly affect Hg storage, having a major effect on the balance between emissions and sequestration and on the global Hg cycle.