环境空气质量不同监测方法的对比

在对环境空气质量的监测中，有些城市存在着人工采样实验室测定和连续自动监测系统监测并行的情况。为考察这两种方法监测结果的异同，于夏季连续20d和冬季连续15d进行了对比监测。监测项目为SO2，NO2和PM10。在对比监测中采取了质量控制措施。对人工采样实验室测定进行了综合采样器流量校正，现场空白样和全程序平行样测定；在自动监测系统中，对SO2，NO2监测仪器作零点，标点校正，PM10监测仪作K0校正。对所测得的209个日均值进行了统计分析，结果表明：SO2，PM10两方面测定结果方差相同，NO2两种方法在冬夏两季方差间均有显著性差异；夏季SO2，PM10，冬季NO2两种方法监测结果一致；冬季SO2，PM10，夏季NO2两种方法监测结果有显著性差异；样品浓度水平及天气状况对两种方法测定结果的差异亦产生较大的影响。     

环境空气自动监测方法检出限相关问题探讨

探讨了环境空气自动监测中实际评估方法检出限的意义,详细介绍了常规气态污染物自动监测方法检出限的评估方法。并以EC 9850型SO2分析仪为例,说明了环境空气自动监测的测定步骤和方法检出限的计算。     

兰州市空气中三项污染物自动与手工监测值比较

通过对自动监测和手动监测兰州市大气中SO2、NO2（NOx）、PM10（TSP）的二组数据分析．在非采暖期二组数据有较大相关性，而在采暖期，SO2和NO2（NOx）具有相关性外，PM10（TSP）则没有相关性．     

CO对定电位电解法测定SO2的影响及对策探讨

采用定电位电解法测定固定污染源废气中SO2,根据CO标准气体干扰SO2 测定的规律建立数学模型,并在实验室用CO标气对数学模型进行验证.用该数学模型对5家企业固定污染源废气中SO2 监测,将测定结果与碘量法的测定结果比对,绝对误差与相对误差在允许范围内.     

Filter badge SO_2捕集-离子色谱法测定空气中二氧化硫

用Filter badge SO2捕集空气中SO2。用双氧水将捕集到的SO2氧化成SO42-,再用离子色谱法测定SO42-的浓度,按公式f SO2=2082×103×(T/τ)X计算,即可得到捕集时间内的平均SO2浓度f SO2(ppb)。     

基于傅里叶红外光谱法测定燃煤电厂烟气中SO3与H2SO4

基于傅里叶红外光谱法(FTIR)监测燃煤电厂烟气处理流程中的SO3与H2 SO4.结果表明,布袋除尘进口、出口和烟囱出口的SO3与H2SO4之和(SO3+H2SO4)分别为(29.33±2.30)mg/m3、(25.15±1.63)mg/m3和(12.13±1.26)mg/m3;布袋除尘与湿法脱硫对SO3+H2 SO4...     

分光光度比浊法测定氢氟酸中SO_4~(2-)

在混合稳定剂的存在下,利用BaSO4的比浊法测定氢氟酸中的SO42-。SO42-浓度在0—50mg/L保持线性,2 5　工作曲线和灵敏度SO42-形成稳定的相应盐类。最低检出量为1mg/L。该方法已用于实际样品的测定。按实验方法测定其吸光度,SO42-的质量浓2 2　酸度的控制     

大气中二氧化硫测定方法的改进

在甲醛冲溶液吸收-盐酸副玫瑰苯胺分光光度法测定SO2中，将原10mLB 管改为25mL比色管，测定SO2的效果较好。     

空气自动监测与连续监测测定值的对比分析

确定空气自动监测与连续监测的相关性,对保证监测数据的连续性、可比性和正确判断环境空气质量的变化规律有重要的作用。对比实验空气的自动监测系统和连续监测系统,两者的监测值存在一定差异。1　实验1 1　分析方法SO2、NO2、PM10的自动监测方法和连续监测方法见表1。表1　SO2、NO2、PM10的自动监测方法和连续监测方法项目自动监测连续监测SO2ISO/CD10498紫外-荧光法GB/T15262-94甲醛吸收副玫瑰苯胺分光光度法NO2ISO7996化学发光法GB/T15435-95Saltzman法PM10β射线法GB6921-86重量法1 2　主要仪器自动监测仪(采样系统为…     

南昌市一次降水自动监测结果的综合分析

利用降水自动监测仪和空气自动监测系统的同步监测结果,分析了一次34 5mm连续降水中全过程的pH、EC和同期SO2、PM10、NO2的变化情况。降水中pH值为7 23～4 08、EC为488 8～7 6μS cm,pH、EC在降水初期变化较大。pH与EC、SO2呈现负相关趋势,降水过程中PM10、NO2基本保持较低水平,SO2变化较大。     

双道氢化物原子荧光法测定水和土壤中的砷

用AFS-2201双道氢化物发生原子荧光法测定水、土壤样品中的砷含量,方法简捷、快速、准确,二次污染物少.HNO3浓度大于5ppm时,对测量结果有影响.主机通过与微机相联可直接得出监测数据,大大减轻了监测人员的工作量,测定结果令人满意.     

原子吸收测定污水中可溶性硫化物试验研究

无火焰原子吸收法测定可溶性硫化物的基本原理是使水中硫化物与硝酸银反应，生成硫化银沉淀，沉淀过滤后用原子吸收分光光度计测定剩余银含量，间接测定硫化物含量。本文通过对无火焰原子吸收法测定银含量过程中的各种条件试验，并加以分析研究。实验表明此方法具有测定灵敏度高，背景值测定具有优越性等特点，完全满足污水中硫化物监测的需要。     

改进的还原偶氮光度法同时快速测定水中硝基苯和苯胺

对测定方法进行了改进,建立了用还原-偶氮分光光度法同时快速测定水中硝基苯和苯胺的分析方法。根据实验原理,对样品前处理装置进行了改进,实验步骤得到了简化,避免了样品溶液过滤转移过程造成样品损失,使样品前处理实验效率提高了90%以上;改进后的测定方法不仅可快速测定样品中硝基苯,还可同时测定样品中苯胺;达到了用一种分析方法同时测定样品中两种污染物的目的。方法精密度测定结果,相对标准偏差(n=6,RSD)为1.9%~3.2%;对硝基苯、苯胺混合标准样品以及实际废水样品进行了测定,并与原测定方法及苯胺国标测定方法进行了比对实验;测定结果具有一致性。加标实验回收率为96%~101%,表明方法准确可靠,可用于水和废水中硝基苯或硝基苯和苯胺的同时测定。     

乌鲁木齐市空气中氮氧化物的污染特征及来源分析

通过引用新华南路测点的二氧化氮和氮氧化物污染浓度值，归纳乌鲁木齐市氮氧化物的污染动态变化规律并分析原因。     

比色法测定水中微量三氯杀螨醇

使用比色法测定水中微量三氯杀螨醇的浓度。首先用正己烷萃取浓缩水中的三氯杀螨醇,比较了加入不同量的去离子水,不同浓度、不同量的NaOH,不同的反应显色温度和反应时间以及吡啶用量等对体系吸光度的影响。得出最佳的显色条件:0.2ml去离子水,0.1ml质量浓度为45%的NaOH溶液,与2.0ml吡啶混合,于100℃水浴中反应3.0min,反应液在4000r/min离心2.0min,取出反应液在530nm处测定吸光度值。此方法的标准工作曲线相关系数为0.9914,方法的绝对检出限为0.2μg三氯杀螨醇。样品加标回收率为83.7%~114.1%,相对标准偏差小于10%。     

氯气检测管的研制

经过条件优化试验，研制出氯气检测管。检测管显色长度与氯气浓度呈线性相关，对氯气标气7次测定的变异系数为13．8％，平均相对误差为5．2％，小于15％；一次测定最大相对误差为20％，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。干扰物有溴和氯化氢气体以及高浓度二氧化氮。检测管寿命为1a。     

Evaluation of the seasonal variation on the geochemical parameters and quality assessment of the groundwater in the proximity of River Cooum, Chennai, India

The seasonal variations of the chemical budget of ions were determined from the hydrochemical investigation of the groundwater. Though the effect of monsoon does not change the order of abundance of cations, but it does change the concentration of various ions and it is found that there was a considerable change in the case of all major ions. The unique characteristic of the ground water is the linear relationship among the principal ions. Hydrochemical characteristics of ions in the groundwater were studied using 1:1 equiline diagrams. The nature of the water samples were determined using the piper diagram. The correlation studies and R-mode factor analysis were carried out on the various groundwater parameters. The study of factor scores reveals the extent of influence of each factors on the overall water chemistry at each sampling stations. The trace metal concentration in the water was determined. The quality of the groundwater in the study area has been assessed using Percent sodium, SAR and Wilcox diagrams. The groundwater results of the premonsoon shows the dominance of excessive evaporation, silicate weathering and anthropogenic activities whereas in postmonsoon, dilution predominates over that of other factors.     

Assessment of pumped mercury vapour adsorption tubes as passive samplers using a micro-exposure chamber

Mercury vapour adsorption tubes manufactured for pumped sampling and analysis have been evaluated for their performance as passive samplers. This has been done by exposing these tubes in a novel micro-exposure chamber. The uptake rates of these tubes have been found to be low (approximately 0.215 ml min(-1)) as compared to bespoke passive samplers for mercury vapour (typically in excess of 50 ml min(-1)). The measured uptake rates were shown to vary significantly between tubes and this was attributed to the variability in the air-sorbent interface and the proportion of the cross sectional area removed by the crimp in the quartz tubes used to secure the sorbent material. As a result of this variability the uptake rate of each tube must be determined using the micro-exposure chamber prior to deployment. Results have shown that the uptake rate determined in the micro-exposure chamber is invariant of concentration, and therefore these uptakes rates may be determined at a high mercury vapour concentration for many tubes at once in less than one hour. The uptake rate of the adsorption tubes under these conditions may be determined with a precision of 5%. Measurements made on a limited field trial in indoor and outdoor ambient air have shown that these tubes give results in acceptable agreement with more traditional pumped sampling methods, although longer sampling periods are required in order to reduce the uncertainty of the measurement, which is currently approximately 30%.     

Identification and evaluation of hydrogeochemical processes on river Cooum, South India

The salient features of the river water chemistry and the seasonal variations on the individual chemical parameter were evaluated and characterized. The order of abundance of the ions in the water is determined for both seasons. The contribution of chemical weathering to the water chemistry has been determined using the (Ca²⁺ + Mg²⁺)/(Na⁺ + K⁺) ratio, ternary, and Gibb’s diagrams. The results show that the chemical composition of river water during premonsoon is controlled mainly by evaporation–crystallization, while in the postmonsoon, the rock–water interaction dominates. The unique characteristic of the river water is the linear relationship among the principal ions. Hydrochemical characteristics of ions in the water were studied using 1:1 equiline diagrams. The nature of the water samples was determined using the piper diagram. The influence of trace metals on the chemical composition and the quality of the river water in the study area has been assessed using Wilcox and US Salinity Laboratory diagrams.     

Classification and mapping forest sites using geographic information system (GIS): a case study in Artvin Province

The productivity of forest sites has been indirectly determined with solo wood production objective in forest management. Forest site productivity should, however, be determined directly in order to implement ecosystem based multipurpose forest management philosophy. This article tackles the problem in distinguishing and mapping forest sites using both direct method and indirect method in Genya Mountain located in central of Artvin State Forest Enterprise. About 112 sample plots were designed and distributed over the area. In each sample plot, soil samples were collected and the classical timber inventory measurements were taken. According to direct method, Soil Moisture Regime (SMR) method is preferred due to a water deficiency in the study area. Water holding capacity was used as an essential criterion for the classification of the forest site. Forest site classifications were assigned regarding the physiographic factors such as landform, aspect, and slope. Five different forest sites classes; dry, moderate fresh, fresh, humid and hygric were determined. According to direct method, the guiding curve was used to generate anamorphic site index (SI) equations and three site index classes; good (SI=I–II), medium (SI=III) and low (SI=IV–V) were determined. Some important differences between the methods were realized. The forest sites determined with site index estimation method indicate that site index I and II is 505.99 ha, III 1095.79 ha and IV and V 992.95 ha, whereas forest sites determined with direct method related to dry site of 937.58 ha, moderate fresh site of 931.90 ha, fresh site of 1,797.71 ha, humid site of 80.48 ha and hygric site of 356.55 ha. The forest site maps of both methods were created using GIS functions. The forest sites of open and degraded areas should be determined according to direct method.