采用分层采样技术对场地地下水污染物进行三维空间描述

地下水单一混合层采样所需建井及采样技术较简单,曾被广泛应用于地下水监测,但根据该技术所得地下水污染物数据进行污染场地地下水污染羽和污染程度描述,常常存在较严重的偏差。以某氯代烃污染场地为例,详细阐述了巢式监测井的建井及分层采样技术,并以该场地主要污染物氯乙烯和氯仿为例,对比了来自不同采样技术的两个主要污染物数据,证实了采用分层采样技术对污染场地地下水进行调查,具有更好的准确性和可靠性。     

Matrix diffusion coefficients in volcanic rocks at the Nevada test site: influence of matrix porosity, matrix permeability, and fracture coating minerals

Diffusion cell experiments were conducted to measure nonsorbing solute matrix diffusion coefficients in forty-seven different volcanic rock matrix samples from eight different locations (with multiple depth intervals represented at several locations) at the Nevada Test Site. The solutes used in the experiments included bromide, iodide, pentafluorobenzoate (PFBA), and tritiated water ((3)HHO). The porosity and saturated permeability of most of the diffusion cell samples were measured to evaluate the correlation of these two variables with tracer matrix diffusion coefficients divided by the free-water diffusion coefficient (D(m)/D*). To investigate the influence of fracture coating minerals on matrix diffusion, ten of the diffusion cells represented paired samples from the same depth interval in which one sample contained a fracture surface with mineral coatings and the other sample consisted of only pure matrix. The log of (D(m)/D*) was found to be positively correlated with both the matrix porosity and the log of matrix permeability. A multiple linear regression analysis indicated that both parameters contributed significantly to the regression at the 95% confidence level. However, the log of the matrix diffusion coefficient was more highly-correlated with the log of matrix permeability than with matrix porosity, which suggests that matrix diffusion coefficients, like matrix permeabilities, have a greater dependence on the interconnectedness of matrix porosity than on the matrix porosity itself. The regression equation for the volcanic rocks was found to provide satisfactory predictions of log(D(m)/D*) for other types of rocks with similar ranges of matrix porosity and permeability as the volcanic rocks, but it did a poorer job predicting log(D(m)/D*) for rocks with lower porosities and/or permeabilities. The presence of mineral coatings on fracture walls did not appear to have a significant effect on matrix diffusion in the ten paired diffusion cell experiments.     

Field comparison of disjunct and conventional eddy covariance techniques for trace gas flux measurements

A field intercomparison experiment of the disjunct eddy covariance (DEC) and the conventional eddy covariance (EC) techniques was conducted over a grass field. The half-hourly water vapor fluxes measured by the DEC were within the estimated uncertainty from the fluxes measured by the EC. On the average there was a slight overestimation (<10%) of the fluxes measured by the DEC during the day and underestimation during the night as compared to the fluxes measured by the EC. As this bias does not appear in the simulated DEC measurements it is likely to be due to instrumental problems. The insensitivity of the quality of the fluxes measured by the DEC method to the deficiencies in the gas analysis shows the robustness of this new approach for measuring the surface-atmosphere exchange of trace gases.     

Self-ignition and explosion during discharge of high-pressure hydrogen

The phenomenon of self-ignition and explosion during discharge of high-pressure hydrogen was investigated. To clarify the ignition conditions of high-pressure hydrogen jets, rapid discharge of the high-pressure hydrogen was examined experimentally. A diaphragm was used to allow rapid discharge of the high-pressure hydrogen. The burst pressure was varied from 4 to 30 MPa. The downstream geometry of the diaphragm was a flange and extension pipes, with the pipe length varying from 3 to 300 mm. The diameter of the nozzle was 5 or 10 mm. When short pipes were used, the hydrogen jet did not ignite. However, the hydrogen jet showed an increasing tendency to ignite in the pipe as the length of the pipe became longer. At higher burst pressures, a diffusion jet flame was formed from the pipe. The blast wave from the fireball formed on self-ignition of the hydrogen jet resulted in an extremely rapid pressure rise.     

天然气处理厂放空火炬影响分析与模拟计算

根据天然气处理厂的地理和气象条件,提出需要进行危险性评估的4种工况;采用喷射扩散模式计算喷射火焰的热辐射,模拟不同工况下,风速不同时的热辐射强度曲线;采用高斯三维模型计算气体扩散浓度,得出不同工况下,风速不同时气体扩散长度和高度,并对放空火炬紧急工况时不同风速下的气体扩散进行模拟。通过影响分析和模拟,得出该放空火炬在不同风速下,不使人员产生热辐射影响的最小安全距离。     

气田井喷硫化氢风洞模拟试验研究

为研究高含硫气田发生井喷事故后硫化氢的扩散运动规律,以重庆开县"12·23"井喷事故为研究对象,利用北京大学的2号环境风洞,制作了1∶2000的比例模型,利用乙烯和丙烯的混合气为示踪气体,采用长采样管方法测量浓度,首次在国内进行了井喷事故后硫化氢扩散的风洞试验,获得了低风速下(源处10m高风速为0.5m/s)N,NE,E,SE,S,SW,W,NW8个风向情况下的硫化氢浓度分布随时间的演化动画,定量地给出了各风向情况下硫化氢的最大浓度分布和各点的浓度时间序列,认为在低风速下,最大硫化氢浓度区域在撞山爬坡时出现,而爬过山坡后在背风区的硫化氢浓度会迅速降低。研究成果将为气田的井喷风险分级以及井喷事故后的应急处理提供参考。     

ESP粉尘二维输运方程中紊流掺混系数及边界条件的确定

求解电除尘器ESP(Electrostatic Precipitator)电场粉尘输运方程中粉尘浓度分布时,确定紊流掺混系数及边界条件至关重要.根据紊流传质原理,推导出紊流掺混系数; 通过雷诺数将电风影响引入紊流掺混系数,推导出紊流掺混系数随电晕线到极板距离的增大而增大.极板附近存在具有一定厚度的层流边层.分析层流边层中荷电粒子迁移输运行为,得到极板处粉尘浓度变化规律,这可作为求解输运方程时极板处的边界条件.用Matlab程序求解输运方程.经验证,理论计算的数值结果与试验结果一致,这表明本文所推导的紊流掺混系数和边界条件是正确的.本文使ESP收尘过程的理论研究更加深入,对提高ESP的收尘效率也具有重要意义.     

Obtaining the porewater composition of a clay rock by modeling the in- and out-diffusion of anions and cations from an in-situ experiment

A borehole in the Callovo–Oxfordian clay rock in ANDRA's underground research facility was sampled during 1 year and chemically analyzed. Diffusion between porewater and the borehole solution resulted in concentration changes which were modeled with PHREEQC's multicomponent diffusion module. In the model, the clay rock's pore space is divided in free porewater (electrically neutral) and diffuse double layer water (devoid of anions). Diffusion is calculated separately for the two domains, and individually for all the solute species while a zero-charge flux is maintained. We explain how the finite difference formulas for radial diffusion can be translated into mixing factors for solutions. Operator splitting is used to calculate advective flow and chemical reactions such as ion exchange and calcite dissolution and precipitation. The ion exchange reaction is formulated in the form of surface complexation, which allows distributing charge over the fixed sites and the diffuse double layer. The charge distribution affects pH when calcite dissolves, and modeling of the experimental data shows that about 7% of the cation exchange capacity resides in the diffuse double layer. The model calculates the observed concentration changes very well and provides an estimate of the pristine porewater composition in the clay rock.     

断面污染物分布均匀度及影响因素研究

水质监测在跨行政区、跨水域功能区、排污总量控制区的水质控制与管理方面有着非常重要的作用,而断面污染物分布均匀与否是水环境监测断面采样是否具备可靠性、合理性和代表性的关键。本文根据监测采样要求提出了断面污染物分布均匀度的概念,即断面污染物分布均匀度是指在污染带内任一垂直于水流方向断面上某一污染物最小浓度值与最大浓度值之比。并就污染物排放量、河流环境水文特征、河流背景浓度、排污方式等断面污染物分布均匀度影响因素进行了分析研究,借助水质模拟技术,反演在上游有排污口情况下如何布置排污方式以满足下游监测采样的要求。这对跨界河流的水质交接、流域水环境质量管理、排污总量控制、水环境监测断面设置等方面的应用具有重要指导和借鉴意义。     

An Evaluation of Qualitative Indexes of Physical Habitat Applied to Agricultural Streams in Ten U.S. States1

Hughes, Robert M., Alan T. Herlihy, and Philip R. Kaufmann, 2010. An Evaluation of Qualitative Indexes of Physical Habitat Applied to Agricultural Streams in Ten U.S. States. Journal of the American Water Resources Association (JAWRA) 46(4): 792-806. DOI: 10.1111/j.1752-1688.2010.00455.x Abstract: Assessment of stream physical habitat condition is important for evaluating stream quality globally. However, the diversity of metrics and methods for assessing physical habitat condition confounds comparisons among practitioners. We surveyed 51 previously sampled stream sites (0.0-6.3 m wide) located in regions of row-crop agriculture in Oregon, California, North Dakota, South Dakota, Nebraska, Iowa, Minnesota, Pennsylvania, Maryland, and West Virginia to evaluate the comparability of four indexes of physical habitat condition relative to each other. We also compared the indexes to previously calculated indexes of fish and macroinvertebrate condition. The physical habitat indexes included the Stream Visual Assessment Protocol Version 2 of the Natural Resources Conservation Service, the qualitative habitat evaluation index of the Ohio Environmental Protection Agency, the rapid bioassessment protocol of the United States Environmental Protection Agency (USEPA), and a qualitative physical habitat index based on USEPA quantitative physical habitat measurements. All four indexes were highly correlated with each other, but low-to-moderately correlated with biotic index scores for fish and macroinvertebrate assemblages. Moderately high correlations occurred between some macroinvertebrate biotic index scores and quantitative metrics. We conclude that additional research is needed to increase the predictive and diagnostic capabilities of qualitative physical habitat indexes.