微库仑法和离子色谱法测定土壤中可吸附有机卤素

采用振荡吸附处理土壤样品，用微库仑法和离子色谱法分别测定土壤中的可吸附有机卤素(AOX)。通过优化样品前处理条件以提高AOX的提取效率，上述两种方法检出限分别为15.3 mg/kg和16.3 mg/kg, 4-氯苯酚作为标准物质的加标回收率分别为92.2%～95.0%和77.7%～80.2%。两种方法测定实际土壤样品中AOX,6次测定结果的RSD为5.4%～19.2%。GSS系列标准土壤试验结果表明，振荡吸附处理样品，用微库仑法和离子色谱法在测定样品中AOX时测定结果区别不大，土壤中AOX含量与卤素含量无直接关系。     

水样中可吸附有机卤化物(AOX)的测定

采用微库仑法对天然水样、自来水及工业废水中的可吸附有机卤化物(AOX)进行了测定。对比柱吸附法和振荡吸附法分析结果,表明柱吸附法在系统空白值、方法检测限、回收率和精密度方面都要优于振荡吸附法,其方法检测限为7·07μg(Cl)/L,回收率为99·3%~104·2%。去干扰实验表明,加入适量的亚硫酸钠溶液可以有效消除游离氯对AOX测定的影响。     

微库仑法测定新疆棉浆粕企业废水中可吸附有机卤素AOX

建立微库仑滴定法测定水质中可吸附有机卤素AOX的方法,考察3种活性炭柱对于空白的影响。实验结果表明,AOX的检出限为2.19μg/L,相对标准偏差为2.80%,纯水中高、中、低加标回收率在92.5%~107%,新疆棉浆粕企业废水中加标回收率为96.0%~101%。实验室空白也只有新购开封的耶拿原装活性炭小柱能满足标准要求的空白值(<30μg/L)。     

造纸工业总排水及漂白废水中AOX监测方法的研究

运用TOX测定仪对造纸工业废水及漂白废水中AOX(可吸附有机卤素)测定;水样用硝酸调pH＜2后,以双根活性炭玻璃填充柱连续吸附;将吸附有机物的活性炭在氧气流中燃烧热解、用微库仑法测定其卤化氢.样品前处理比现行活性炭振荡吸附法样品及试剂用量少、快速、重现性好.方法测定浓度下限为3.73μg/L.     

对氯苯酚在水环境可吸附有机卤素监测中的应用

选用对氯苯酚固体和市售对氯苯酚标准溶液分别配制成2种可吸附有机卤素(AOX)标准溶液和标准样品进行实验。结果表明,使用对氯苯酚固体配制的AOX标准溶液,其分析曲线和带标分析结果良好,检出限为6.6μg/L,加标回收率为80.1%~106%;使用市售对氯苯酚标准溶液配制的AOX标准样品,其测定结果均在参考不确定度范围内,加标回收率为94.0%~103%,测定值与真值的相对误差为-6.0%~2.5%。可见,选用对氯苯酚作为标准物质和标准样品应用于环境地表水和工业废水中AOX监测分析的质控过程是可行的。     

废水中可吸附有机卤化物的来源、测定方法及去除技术的研究进展

简述了废水中可吸附有机卤化物(AOX)的定义、来源和危害,以及国内外废水中AOX排放的相关法规。详细介绍了微库仑法、中子活化法、三维荧光法等AOX测定方法,以及物理法、化学法、生物法3种AOX去除技术的研究进展。并对工业废水中AOX的检测、表征及其针对性处理提出了今后的研究方向。     

水中可吸附有机硫的测定--库仑滴定法

采用智能测硫仪,使吸附在活性炭上的有机硫在高温空气流中燃烧、分解,定量地转化为二氧化硫,用库仑滴定法测定。水中无机硫化物的干扰用乙酸铜均匀沉淀法去除。     

红外分光光度法测定水中油类物质吸附方法的比较

吸附处理是红外法测定石油类的一个重要环节.通过实验对吸附柱法和振荡吸附法进行对较,结果表明动植物油质量浓度为0.560 mg/L～145 mg/L的水样,振荡吸附法吸附效率高于吸附柱法.振荡吸附法还具有操作时间短、硅酸镁耗量低、对操作人员危害性小、样品可批量分析的优点.     

LLE-GC-MS法测定水中27种有机农药

建立了同时测定水中27种有机农药的LLE-GC-MS法。该法前处理前需调节水样pH值2,不加甲醇作为改性剂,以1:1(V/V)正己烷-石油醚为萃取溶剂进行液液萃取,GC-MS法进行检测。方法在各目标化合物质量浓度0.010~0.500 mg/L范围内线性良好,相关系数R2均0.995,检出限为0.021~0.250μg/L,加标回收率为73.6%~113.6%,相对标准偏差RSD为4.0%~14.1%,适用于水中27种有机农药的检测。     

活性炭吸附-毛细管柱气相色谱法测定大气中吡啶

以活性炭吸附大气中的吡啶,用二硫化碳解析、毛细管柱分离、FID检测器分析,采用保留时间定性、峰面积外标曲线法定量。方法在0～367mg/L范围内线性关系良好,当采样体积为20L时,最低检出质量浓度为0.007mg/m3,标准溶液平行测定的RSD≤2.0%,加标回收率为97.9%～104%。     

燃烧氧化-非分散红外吸收测定水中总有机碳方法的改进

总有机碳测定的方法分为差减法和直接法。现对测定方法进行改进,将差减法和直接法测定结果结合,先将样品进行酸化初步吹扫,再使用差减法测定总有机碳。试验结果显示,无论在标准曲线、精密度试验、加标回收试验还是标准样品测定方面,改进法均优于直接法测定结果,且能较好地缩短测量时间。     

万峰湖总有机碳空间分布特征

于2012年9月对万峰湖(水库)的总有机碳(TOC)空间分布特征进行研究,结果显示:TOC含量范围为0.41~3.94 mg/L。TOC在纵向分布上的差异不显著,在垂向分布上,总体呈现出上层中层下层的趋势。TOC在垂向上的分布差异主要源于万峰湖属于深水水库,不同深度水层因光照和温度差异所导致生物量的多寡是致使万峰湖出现上层TOC浓度明显高于中层和下层的主要因素。     

呼伦贝尔地区草原表层土壤中总有机碳与有机质初探

通过非分散红外线吸收法测定呼伦贝尔地区具有代表性的16个草原表层土壤(0~20 cm)中总有机碳、溶解性有机碳,使用重铬酸钾容量法测定有机质,并对其总有机碳与有机质水平及两者相关性进行了分析。初步分析了造成各样品之间总有机碳水平差异的原因。结果表明,只以打草场作为利用方式的土壤总有机碳含量较常年放牧场的总有机碳含量高。从草原类型和土壤类型上看,草甸草原总有机碳含量明显高于典型草原,黑钙土总有机碳含量明显高于栗钙土。综上,过度放牧会使草原土壤总有机碳大量释放。总有机碳含量与有机质含量有显著正相关性,相关系数达到0.902。     

Modelling Dissolved Organic Carbon Turnover in Humic Lake Örträsket, Sweden

The organic carbon balance of a lake with high input of allochthonous organic carbon is modelled integrating physical, chemical and biological processes. The physical model captures the behaviour of real thermal stratification in the lake for different flow situations during the period 1993–1997. The dissolved organic carbon model is based on simulated trajectories of water parcels. By tracking parcels, account is kept of environmental factors such as temperature and radiation as well as DOC quality for each parcel. The DOC concentration shows seasonal variations primarily dependent on inflow. The organic matter degradation (bacterial- and photodegradation) in the lake amounts to 1.5–2.5 mg C l^–1 yr^–1, where photooxidation is responsible for approximately 10%. The estimated DIC production in the lake is large compared to sediment mineralisation and primary production. The main conclusion is that the model with the selected parameterisations of the degradation processes reasonably well describes the DOC dynamics in a forest lake.     

Natural and Anthropogenic Factors Controlling the Dissolved Organic Carbon Concentrations and Fluxes in a Large Tropical River, India

Carbon studies in tropical rivers have gained significance since it was realized that a significant chunk of anthropogenic CO₂ emitted into the atmosphere returns to the biosphere, that is eventually transported by the river and locked up in coastal sediments for a few thousand years. Carbon studies are also significant because dissolved organic carbon (DOC) is known to complex the toxic trace metals in the river and carry them in the dissolved form. For the first time, this work has made an attempt to study the variations in DOC concentrations in space and time for a period of 19 months, and estimate their fluxes in the largest peninsular Indian river, the Godavari at Rajahmundry. Anthropogenic influence on DOC concentrations possibly from the number of bathing ghats along the banks and domestic sewage discharge into the river are evident during the pre-monsoon of 2004 and 2005. The rise in DOC concentrations at the onset of monsoon could be due to the contributions from flood plains and soils from the river catchment. Spatial variations highlighted that the DOC concentrations in the river are affected more by the anthropogenic discharges in the downstream than in the upstream. The discharge weighted DOC concentrations in the Godavari river is 3–12 times lower than Ganga-Brahmaputra, Indus and major Chinese rivers. The total carbon fluxes from the Godavari into the Bay of Bengal is insignificant (0.5%) compared to the total carbon discharges by major rivers of the world into oceans.     

Multi N/C2100S总有机碳分析仪校准方法的建立

以德国Analytikjena公司Multi N/C 2100S分析仪为例,研究建立了合理可行的总有机碳分析仪校准方法.在总有机碳分析仪检定规程JJG 821-2005的基础上,增加零点漂移、直线性、标准曲线线性和检出限4项特性指标,改变了准确性特性的判定方法.根据仪器的使用频率和稳定性,建议校准周期不超过2年.     

Isolation and fractionation of natural organic matter: evaluation of reverse osmosis performance and impact of fractionation parameters

Dissolved organic matter (DOM) from three surface waters was isolated using reverse osmosis (RO) and subsequently fractionated using resin adsorption chromatography (RAC). Efficacy of RO was evaluated by closing mass balances for dissolved organic carbon (DOC). RAC was evaluated by investigating the effect of column operational parameters (column capacity factor, k', and solute initial concentration, C0) on DOM fractionation and subsequent disinfection by-product formation. Efficacy of RO was dependent on both isolation conditions and source water characteristics. In general, RO more effectively isolated DOM in high specific ultraviolet absorbance (SUVA254) water than low SUVA254 water, and showed higher DOM recovery at ambient pH (approximately 7) than at low pH (approximately 4). The fractionation of the isolated DOM indicated that the relative amount of the hydrophobic fraction decreased with increasing k', thus affecting the overall distribution of DOM. However, the distribution of DOM fractions was not influenced by varying C0 up to 150 mg l(-1) at k' of 15. The effect of k' on the formation and speciation of trihalomethanes (THM) and haloacetic acids (HAA) was not significant up to k' of 30.     

Capillary microextraction for simultaneous analysis of multi-residual semivolatile organic compounds in water

Capillary microextractor (CME) in combination with a gas chromatograph-mass spectrometer (GC-MS) was employed for the determination of trace priority hazardous substances in water. Three groups of semivolatile organic compounds (SVOCs), i.e., chlorinated hydrocarbons, pesticides and polycyclic aromatic hydrocarbons (PAHs), were simultaneously determined. SVOCs were extracted from 7 mL of water samples on a 100 cm commercial gas chromatographic column (0.32 mm id x film thickness 0.25 microm, HP-5 capillary column) and eluted with only 3 microL of acetonitrile. The extractant was analyzed by GC-MS in the selected ion monitoring mode. The method showed good linearity over the concentration range 10 ng L(-1) to 3.0 mg L(-1) with correlation coefficients (r) greater than 0.99 and low limits of detection ranged from 10 ng L(-1) to 1.0 mg L(-1). High recovery (more than 80%) was obtained with relative standard deviation less than 10%. The method was successfully applied for trace level analyses of SVOCs in water samples.