地下水中挥发性有机物的吹扫捕集-气相色谱-质谱法测定

建立了吹扫捕集-气相色谱-质谱法同时测定地下水中卤代烃类、苯系物、氯代苯类等20多种挥发性有机物的方法。对吹扫捕集条件、气相色谱条件和质谱条件进行优化,并对实际水样进行测定。方法检出限为0.03～0.28μg/L,基体加标回收率为88.8%～111.0%,精密度(RSD,n=7)为2.21%～5.31%。方法准确,灵敏可靠,可满足地下水中痕量挥发性有机物的分析要求。     

毛细管气相色谱法测定矿坑水中的苯系物

以国家标准方法和EPA方法为基础, 进行了矿坑排水中苯系物的测定.在测定过程中进行了质量保证和质量控制实验, 用外标法定量.在水样测定的同时对用自动顶空进样器和吹扫捕集浓缩仪两种进样方式测定矿坑排水中苯系物的方法进行了比较, 对进样方式和影响测定的因素进行了讨论.结果表明, 自动顶空进样器的回收率为108.5 8%~116.38%, 方法检出限为5.00~10.00 μg/L; 吹扫捕集浓缩仪的回收率为94.87%~105.6 3%, 方法检出限为0.25~0.50 μg/L.      

闭合超声循环吹扫针捕集动态提取-气相色谱法测定地下水中的4种有机磷农药

基于针捕集适于免溶剂提取气态介质样品的特点,通过蠕动泵将针捕集与水样组成闭合循环吹扫系统,提高目标物的水样/顶空亨利系数,建立了针捕集闭合循环提取耦合气相色谱快速分析地下水中4种半挥发性有机磷农药(敌敌畏、甲拌磷、甲基对硫磷、马拉硫磷)的方法,该方法集采样、提取、净化、浓缩、色谱进样于一体。确定了针捕集提取水样最佳条件为:采样流速11.11 m L/min,水样提取温度40℃,在此条件下获得浓度均为1 mg/L的4种有机磷农药的针捕集吸附穿透体积,其中甲基对硫磷最大为600 m L。以5μg/L、50μg/L和200μg/L三个浓度水平的加标平均回收率为62.3%~103.0%,除敌敌畏低浓度水平的RSD为26.1%外,其余组分的RSD7.7%;方法检出限为0.016~0.157μg/L,接近或优于现行国标及相关研究结果。     

吹扫捕集-气相色谱-质谱法测定土壤中挥发酚的方法研究

文章研究了吹扫捕集-气相色谱-质谱法测定土壤中挥发酚的方法,分析了吹扫捕集各参数对挥发酚测定的影响,优化了吹扫捕集条件和气相色谱-质谱条件。通过与索氏提取技术对比,证明吹扫捕集-气相色谱-质谱法在实际样品检测中具有操作简便、分析周期短、试剂用量少、干扰小等优点,适用于测定沸点较低、溶解度较小的挥发酚,推荐选择经典的索氏提取技术测定沸点较高、溶解度较大的挥发酚。     

重点行业企业用地地下水中60种挥发性有机物的测定分析方法研究

建立了吹扫捕集—气相色谱质谱法测定重点行业企业用地地下水中60种挥发性有机物的分析方法.采用屈臣氏双蒸水作为空白水,选择离子与全扫描模式交替方式进行定性定量,确定了保护剂的种类和用量,优化了吹扫捕集条件.方法检出限范围在0.3～1.2μg/L.该方法的线性范围为0～250μg/L,相关系数R²在0.9907～0.9999之间,3种不同浓度的加标平均回收率为87.2%～117%,相对标准偏差在1.7%～9.7%之间,优于《重点行业企业用地调查质量保证与质量控制技术规定(试行)》对地下水挥发性有机物的质控要求.本方法增加了VOCs的测试种类,线性范围宽,灵敏度高,适合于各类重点行业企业用地地下水中60种挥发性有机物的快速批量分析.     

吹扫捕集-气相色谱／质谱法测定土壤中挥发性有机化合物

建立了吹扫捕集-气相色谱/质谱技术测定土壤中挥发性有机化合物的方法,对标准模拟样品的基体选择、吹扫捕集条件、色谱条件等实验条件进行了考察。结果表明,方法检出限为0.20~0.60μg/kg,精密度(RSD,n=7)为2.78%~9.89%,基体加标平均回收率为81.5%~115.2%。方法准确可靠,用于批量样品的实际分析,检测结果良好。     

岩溶地区垃圾渗透液中36种挥发性有机物的测定

应用吹扫捕集-气相色谱-质谱法测定岩溶地区垃圾渗透液中36种挥发性有机物（VOCs）的含量。获取样品溶液5 mL于吹扫瓶中,利用TELEDYNE TEKMAR型吹扫捕集直接进样,经DB-VRX毛细管色谱柱分离、电子轰击电离（EI）全扫描检测,选择特征离子,再用外标法进行定量测定。结果表明:36种挥发性有机物的质量浓度在1～100 μg·L-1 范围内,与其峰面积呈线性关系,方法检出限在0.03～0.27 μg·L-1 之间,加标回收率在88%～110%之间,相对标准偏差（n=7）在2.32%～6.51%之间。      

吹扫捕集/气相色谱-质谱法测定地下水中30种挥发性有机物

在测定地下水中有机污染物时,捕集阱的填料对分析结果有很大的影响.本文采用吹扫捕集/气相色谱-质谱联用技术,建立了适用于地下水中卤代烃、氯代苯、苯系物等30种挥发性有机污染物的分析方法.对11#捕集阱( VOCARB3000)和10#捕集阱(Tenax/硅胶/碳分子筛)进行比较实验和捕集阱的填料进行选择优化,结果表明,以氮气为吹扫气,11#捕集阱的检出限比10#捕集阱的检出限低,富集效率和响应值更高,更适合分析低含量的地下水样品;Rtx - 502.2毛细柱(60 m×0.32 mm×1.8 μm)对目标组分有更好的分离效果,且柱流失小、色谱峰响应高;利用选择离子扫描方式对目标物进行扫描,采用内标法定量,提高了方法灵敏度,消除了组分的干扰以及整个分析过程中存在的系统误差.方法检出限为0.031 ～0.059 μg/L,精密度(RSD)为1.02％ ～5.19％(n=7),回收率为87.7％ ～118.0％(n=7),各组分相关系数均在0.9991以上.方法操作简便,对环境污染小,可满足大批量地下水中痕量挥发性有机物的分析要求.     

吹扫捕集浓缩仪-气相-质谱联用仪简介

吹扫捕集浓缩仪-气相-质谱联用仪P＆TGC—MSTRACEDSQ是西安地质调查中心实验测试中心于2006年引进的。吹扫捕集浓缩仪作为一种前处理设备,主要处理那些需要由气相色谱（GC）或气相色谱／质谱（GC／MS）进行挥发性有机物质（VOC）分析的样品。其工作原理为：     

吹扫-捕集技术在GC法测定地下水中苯系物的条件研究

吹扫—捕集法由于具有较高的富集效率和无有机溶剂再污染等特点 ,广泛应用于地表水、土壤及大气中挥发性有机物的分析测定 ,但用于测定地下水中有机污染物的报导甚少。本文主要研究吹扫—捕集技术在气相色谱法测定地下水中苯系物 (苯、甲苯、二甲苯 )时的条件 ,得到了良好的实验效果。1实验部分1 .1主要仪器设备及试剂OI45 60吹扫捕集器 (美国 ) ,美国HP5 890气相色谱仪。苯、甲苯、二甲苯 (均为GCgrade) ,二氯甲烷 (AR)。标准溶液配置 :分别吸取 1 0 0 μL苯、甲苯、二甲苯于 3个容量瓶中 ,用二氯甲烷稀释至刻度 ,摇匀备用。1 .2仪器测…     

The terrestrial fauna of the Late Triassic Pant-y-ffynnon Quarry fissures,South Wales,UK and a new species of Clevosaurus (Lepidosauria: Rhynchocephalia)

Pant-y-ffynnon Quarry in South Wales yielded a rich cache of fossils in the early 1950s, including articulated specimens of new species (the small sauropodomorph dinosaur Pantydraco caducus and the crocodylomorph Terrestrisuchus gracilis), but no substantial study of the wider fauna of the Pant-y-ffynnon fissure systems has been published. Here, our overview of existing specimens, a few described but mostly undescribed, as well as freshly processed material, provides a comprehensive picture of the Pant-y-ffynnon palaeo-island of the Late Triassic. This was an island with a relatively impoverished fauna dominated by small clevosaurs (rhynchocephalians), including a new species, Clevosaurus cambrica, described here from a partially articulated specimen and isolated bones. The new species has a dental morphology that is intermediate between the Late Triassic Clevosaurus hudsoni, from Cromhall Quarry to the east, and the younger C. convallis from Pant Quarry to the west, suggesting adaptive radiation of clevosaurs in the palaeo-archipelago. The larger reptiles on the palaeo-island do not exceed 1.5?m in length, including a small carnivorous crocodylomorph, Terrestrisuchus, and a possible example of insular dwarfism in the basal dinosaur Pantydraco.     

The effect of water on accessory phase solubility in subaluminous and peralkaline granitic melts

The solubilities of columbite, tantalite, wolframite, rutile, zircon and hafnon were determined as a function of the water contents in peralkaline and subaluminous granite melts. All experiments were conducted at 1035 °C and 2 kbar and the water contents of the melts ranged from nominally dry to approximately 6 wt.% H₂O. Accessory phase solubilities are not affected by the water content of the peralkaline melt. By contrast, solubilities are affected by the water content of the subaluminous melt, where the solubilities of all the accessory phases examined increase with the water content of the melt, up to 2 wt.% H₂O. At higher water contents, solubilities are nearly constant. It can be concluded that water is not an important control of accessory phase solubility, although the water content will affect diffusivities of components in the melt, thus whether or not accessory phases will be present as restite material. The solubility behaviour in the subaluminous and peralkaline melts supports previous spectroscopic studies, which have observed differences in the coordination of high field strength elements in dry vs. wet subaluminous granitic glasses, but not for peralkaline granitic glasses. Lastly, the fact that wolframite solubility increases with increasing water content in the subaluminous melt suggests that tungsten dissolved as a hexavalent species.     

Quaternary stresses revealed by calcite twinning inversion: insights from observations in the Savonnières underground quarry (eastern France)

Calcite samples were extracted both from the rock matrix and the superficial coating of a karstified fault plane of an underground quarry, located in the eastern border of the Paris basin. The karstification is dated as Quaternary. Analysis of mechanical calcite twinning reveals that only the calcite matrix has also undergone a compression trending WNW that can be attributed to the Mio-Pliocene alpine collision. Both coating and matrix have undergone a strike-slip regime with σ₁ roughly trending north–south, that could correspond to the regional present-day state of stress, a strike-slip compression rather trending NNW, modified by local phenomena. To cite this article: M. Rocher et al., C. R. Geoscience 335 (2003).     

HYDROGEOLOGY

正20141756 Chen Ruige(Mathematical College,China University of Geosciences,Beijing100083,China);Zhou Xun Numerical Simulation of Groundwater Level Fluctuation in a Coastal Confined Aquifer with Sloping Initial Groundwater Level Induced by the Tide(Geological Bulletin of China,ISSN1671-2552,CN11-4648/P,32(7),2013,p.1099-1104,6 illus.,16 refs.) Key words:confined water,groundwater level     

METAMORPHIC PETROLOGY

正20141408 Cai Jia(Institute of Geology,Chinese Academy of Geological Sciences,Beijing100037,China);Liu Fulai Petrogenesis and Metamorphic P-T Conditions of Garnet-Spinel-Biotitebearing Paragneiss in Danangou Area,Daqingshan-Wulashan Metamorphic Complex Belt(Acta Petrologica Sinica,ISSN1000-0569,CN11-1922/P,29(7),     

SERIALS

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GEOPHYSICAL EXPLORATION

正20142386An Guoying(China Aero Geophysical Survey and Remote Sensing Center for Land and Resources,Beijing 100083,China)Application of Satellite Remote Sensing in Regional Hydrogeological Investigation:Taking Cenozoic Strata in Wenquan Sheet(1∶250 000)of Karakoram Range as an Example(Geosci-     

QUATERNARY GEOLOGY & GEOMORPHOLOGY

正20141016An Chengbang(Key Laboratory of Western China’s Environmental Systems,Ministry of Education,Lanzhou University,Lanzhou 730000,China);Zhao Yongtao Lake Records during the Last Glacial Maximum from Xinjiang,NW China and Their Climatic Impli-     

PETROLEUM GEOLOGY

正20141538 Cao Qing(School of Earth Sciences and Engineering,Xi’an Petroleum University,Xi’an 710065,China);Zhao Jingzhou Characteristics and Significance of Fluid Inclusions from Majiagou Formation,Yichuan Huangling Area,Ordos Basin(Advances in Earth Science,ISSN1001-8166,CN62-1091/P,28(7),2013,p.819-828,7 illus.,3 tables,43 refs.)     

GEOCHEMISTRY

正20142002 Wei Hualing(Institute of Geophysical and Geochemical Exploration,Chinese Academy of Geological Sciences,Langfang065000,China);Zhou Guohua Element Content and Mineral Compositions in Different Sizes of Soil in Tongling Area,Anhui Province(Geological Bulletin of China,ISSN1671-2552,CN11-4648/P,32(11),2013,p.1861