Estimates of pollutant temporal and spatial variability in commercial buildings from the joint urban 2003 field experiments

In this paper, we report on the indoor concentrations from a suite of full-scale outdoor tracer-gas point releases conducted in the downtown area of Oklahoma City in 2003. A point release experiment consisted of releases of sulfur hexafluoride (SF₆) in multiple buildings and from different outdoor locations. From the measurements, we are able to estimate the concentration variations indoors for a building operating under “typical” operating conditions. The mean indoor spatial coefficients of variation are 30% to 45% from a daytime outdoor release are around 80% during an outdoor evening release. Having estimates of the spatial coefficient of variation provides stakeholders, including first responders, with the likely range of concentrations in the building when little is known about the building characteristics and operating behavior, such as developing urban-scale hazard and consequence analyses. We show differences in indoor measurements at different distances to the release points, floors of the building, and heating, ventilation, and air conditioning system (HVAC) operation. We also show estimates at different time resolutions. The statistics show that in the studied medium to large commercial buildings, spatial differences would result in peak indoor concentrations in certain parts of the buildings that may be substantially higher than the building average. To our knowledge, very few tracer gas measurements have been conducted in buildings of this scope, particularly with measurements on multiple floors and within a floor. The resulting estimates of spatial variability provide a unique opportunity for hazard assessment, and comparison to multi-zone models.     

示踪剂技术在秦家屯油藏开发中的应用

秦家屯油田位于松辽盆地南部东南隆起区十屋断陷东北部,属于非均质断块层状油藏,通过示踪剂监测技术可以了解区块内井间连通情况,判断油井见水、来水方向及油层水驱动用程度,结合油藏静态资料研究,指导油田开发,改善开发效果,达到了稳产的目的。     

胜利油区放射性同位素测井的粒径选择

根据胜利油区的地层渗透率、孔隙度，在２７个低渗透油田和４６个中、高渗透油田的放射性同位素测井中进行了粒径为１００～３００μｍ、３００～６００μｍ、６００～９００μｍ放射性同位素１３１Ｂａ微球粒径选择实验，确定了放射性同位素１３１Ｂａ微球的选择原则。当油藏渗透率Ｋ＜１００×１０－３μｍ２、孔隙度＜２０％时，放射性同位素粒径为１００～３００μｍ；当油藏渗透率Ｋ＞１００×１０－３μｍ２、孔隙度＞２０％时，放射性同位素粒径为３００～６００μｍ或６００～９００μｍ。在此基础上得到胜利油区选用同位素粒径明细表，对于指导施工，提高放射性测井资料的可靠性具有重要意义。     

川中地区上三叠统天然气地球化学特征及成藏过程探讨

川中地区上三叠统是一套自生自储的天然气成藏系统，天然气中甲烷含量为88%～96％，重烃（C2＋）含量一般在6％～9％之间，二氧化碳和硫化氢等非烃气体含量普遍较低；天然气干燥系数（C1／C2＋）为5～15，并且随深度增加而呈现升高的趋势；天然气和凝析油轻烃中的甲基环己烷、庚烷和异庚烷值变化表明天然气主要来源于腐殖型母质；天然气甲烷和乙烷碳同位素分别为-39．00‰～-41．00‰和-25．00‰～-27．00‰，具有典型煤成气特征。川中地区上三叠统烃源岩在燕山期持续沉降埋藏过程中，达到高成熟早期阶段；在喜山期，该地区大约2500m地层的剥蚀，使地层温度和压力大幅度降低，故储层中早期低成熟残余天然气的卸压膨胀作用和水溶气的脱溶作用为晚期天然气聚集成藏提供了重要的气源，同时也使气藏中甲烷碳同位素变轻。     

柴达木盆地天然气中稀有气体同位素特征

为了确定柴达木盆地勘探新层系，测试并分析了该盆地5个油气田的8个天然气样品的氦、氩同位素比值，探讨了其在大地构造背景、大地热流和气源方面的示踪意义。研究结果如下：①柴达木盆地8个天然气样品³He/⁴He值分布在2.0×10^-8～5.48×10^-8的范围，总体平均为3.7×10^-8，均在10^-8量级，体现了典型的壳源成因氦同位素的特征。②据³He/⁴He计算的大地热流值较低，分布于41.2~48.2 mW/m²之间，平均44.9 mW/m²，低于东部地区大地热流平均值73 mW/m²，表明该盆地具有较稳定的构造背景。③根据天然气⁴⁰Ar/³⁶Ar的年代积累效应，结合烃源岩分布特征推测，柴达木盆地东部凹陷区伊克雅乌汝构造伊深1井天然气应源于上第三系；西部坳陷区尕斯油田尕斯8-6井和尕斯475井天然气应源于下第三系；碱山构造碱1井天然气应源于侏罗系，碱山构造碱2井的天然气应源于上第三系；北缘块断带南八仙油气田仙试1井的天然气应源于侏罗系；南八仙油气田仙试8井和马北构造马北1井的天然气可能主要源于侏罗系。     

稳定同位素井间示踪技术在深层块状稠油油藏水驱特征研究的应用

经对冷43块深层块状普通稠油水驱注水5个试验井组开展的稳定同位素示踪测试，利用中子活化技术分析样品，采用先进的示踪剂定量分析与流动模拟相互结合的方法，以示踪数值模拟为手段，评价了油井连通、油层平面及纵向上的非均质性、隔层的封隔性等因素对水驱控制程度及动用状况的影响，通过优化注水推进方向及速度，强化动态调整措施，提高了稳产基础。     

注入剖面双相态放射性测井方法研究

文章结合注入剖面同位素示踪和放射性相关流量两种测井方法的特点,提出了固态微球同位素和液态同位素同时使用的综合测井方法.应用放射性相关流量测井的直观性,量化同位素示踪测井中的不确定因素,达到提高测井成功率和资料解释精度的目的.     

Evaluation of Handheld Radionuclide Identifiers

Characterization of commercially available instruments for measurement and identification of unknown radionuclides was carried out in support of the development and testing of the American National Standards Institute (ANSI) standard, N42.34, “Performance Criteria for Hand-held Instruments for the Detection and Identification of Radionuclides.” Measurements were based on the performance of the devices, i.e., the capability of the detectors to ensure a correct radionuclide identification in a given time interval for various radioactive sources.