九华山隧道开挖爆破对古城墙影响的计算分析

计算分析了南京九华山隧道工程开挖爆破对明古城墙的影响。在对国内外流行的安全标准进行比较的基础上,指出了采用频率与震速结合的爆破震动安全标准的必要性,且采用德国爆破震动安全标准作为计算九华山隧道开挖爆破对古城墙的影响的判据;分别利用目前流行的震动速度和震动频率公式进行计算,判断开挖爆破对古城墙的影响程度及影响范围。结果表明,爆破震动对古城墙安全构成威胁,并计算得出开挖爆破最小安全距离。     

静电放电参数随电极移动速度和空气压强变化的特性分析

在小间隙静电放电(ESD)中,电极移动速度和气体压强会对测量放电参数出现的低重复离散特性产生影响。基于自主研发的新型测试系统,完成气体压强变化和向放电靶移动电极放电相关参数的测量。静电放电模拟器移动距离控制范围在10cm-40cm。在间隙气体压强变化和放电枪以不同速度向靶移动放电的两种情况下,放电电流峰值和波形产生了显著的差异,证明了电极移动速度和空气压强都对放电参数产生显著影响。本文对放电参数受电极移动速度和气体压强变化而出现显著差异的可能机制进行了初步分析。     

原子捕集——火焰原子吸收光谱法测定环境土壤中痕量镉

系统地考察了原子捕集测定环境土壤中镉的条件及10余种常见共存离子的干扰情况，测定环境土壤中镉含量原子捕集灵敏度较常规原子吸收光谱法高112倍，可达0.25μg/L/1%A，方法快速、简便、稳定，令人满意。     

污泥絮体特征与微型动物运动速度相关性研究——以自由运动型微型动物为例

为了克服利用微型动物群落物种变化指示活性污泥运行状态存在的微型动物鉴别误判、分类和统计分析工作量大等问题,通过PCA法的相关性分析判断絮体微观形态参数降维成综合指标的可能性,采用“微型动物运动视频采集+定量图像分析”法表征微型动物的运动速度（平均线速度V和平均角速度W）,分析SBR系统中锐利楯纤虫（A.lynceus）等7种自由运动型微型动物的运动速度与污泥絮体微观特性之间的相关性.结果表明：多个污泥絮体微观形态参数之间存在较好的相关性,可降维成2大综合指标（絮体大小密实度（SC）和絮体形状规则度（SR））.絮体SC和SR指标与须足轮虫属（Euchlanis sp.）、凹扁前口虫（F.depressa）和锐利楯纤虫（A.lynceus）的运动速度之间具有较显著相关性（|r|>0.50,P<0.05）,因此利用典型的自由运动型微型动物运动速度变化能够快速指示污泥絮体的微观形态变化.     

惰性气体抑制瓦斯爆燃火焰传播特性实验研究*

为研究惰性气体抑制瓦斯爆燃火焰传播特性,在自行搭建的中尺度爆炸激波管道上,采用数据采集系统、压电式传感器、火焰传感器、同步控制系统和激光纹影测试系统,通过对比4种不同喷射压力（0.5,1.5,2.5,3.5 MPa）的实验工况,选用N2做为惰性介质时抑制火焰的传播特性与喷射压力密切相关,火焰传播速度随着喷射压力增加呈现先增加后减弱的趋势。研究结果表明:少量N2在管道中扩散,加剧了未反应预混气体的扰动状态,造成火焰阵面褶皱的卷吸能力增强,进而加速化学反应进程,促进预混气体燃烧;喷射压力为1.5 MPa时,火焰阵面拉升、变形最强,火焰传播速度提高,最高可达到250 m/s;喷射压力为3.5 MPa时,火焰阵面出现明显三维凹陷结构,运动发生明显滞后现象,火焰传播速度大幅度降低至5.4 m/s,惰性气体抑制火焰传播效果明显。     

火炬火焰监测技术实验测试及对比研究

基于Labview软件,开展热电偶探测、紫外火焰探测、离子火焰监测系统对火炬长明灯火焰响应的实验研究和数据分析.通过分析比较不同火焰监测系统的响应信号,得出以下结论:热电偶监测技术响应时间较长;紫外监测技术响应时间为2-4s,但其输出电压值较小,且在实际运行过程中无法区分高空点火器火焰及长明灯火焰;火焰离子监测技术响应时间为2-6s,输出信号强,容易实现火焰燃烧状态的快速判断.     

管道内天然气爆炸火焰及压力波传播规律实验研究

天燃气安全不仅仅局限在企业内部,而是面向全社会,关系到社会稳定和市民生命财产安全。随着天然气市场开拓和广泛利用,庞大的管网系统和多样的用气环境给安全工作提出了更高的要求。采用理论分析、实验研究相结合的方法研究了管道内天然气爆炸火焰及压力波的传播规律。应用直径为700mm,长度为93m的管道进行了三次天然气爆炸传播实验。得出爆源点最大压力值并不是整个爆炸过程的最大值;压力波最大压力值在爆源点附近先降低,然后上升到某一峰值之后再逐渐衰减;最大压力值在衰减过程中不是单调衰减,有点起伏;随着天然气浓度的增大,其爆炸平均升压速率反而减小;随着天然气浓度的增大,其爆炸平均升压速率反而在减小;爆源附近火焰传播速度较小,上升到某一峰值后逐渐衰减。     

Radiation heat transfer in transient dust cloud flame propagation

This study investigates the impact of radiation heat transfer and heat conduction on dust cloud combustion. Radiation plays a very important role in the stability of dust cloud flame, and increasing the amount of radiation drastically raises the possibility of instability and explosion in a dust cloud mixture. Flame speed, which is a function of mixture characteristics, can exhibit a fluctuating behavior. By using the discrete heat source method, it would be possible to study the transient propagation of dust flames. Thus, the propagation speed of flame can be obtained, and as time goes by, the transient speed of dust flame will reach its steady state value. By considering the radiation effect, better agreement is observed between the obtained results and experimental data.     

The Analysis of Tecnazene (2,3,5,6-Tetrachloronitro-benzene) and its Metabolites in Water and Fish

A method for the analysis of Tecnazene (2,3,5,6-tetrachloronitrobenzene) and its major metabolites (2,3,5,6-tetrachloroaniline and 2,3,5,6-tetrachlorothioanisole) is presented. This rapid analytical technique was developed to measure these compounds in samples of water and fish produced during the course of toxicological investigations. Water samples were extracted into hexane and analysed by high resolution capillary gas chromatography using flame ionisation detection (HRGC-FID). Fish samples were extracted into hexane, cleaned up on a short alumina micro-column and also analysed by HRGC-FID.     

Correction Factors for Covariance between Concentration and Deposition Velocity on CASTNes HNO3 Deposition Estimates

The covariance between hourly concentration (C) and depositionvelocity (V) for various atmospheric species may act to bias the dry deposition (D) computed from the product of the weeklyaverage C and V. This is a potential problem for the CASTNet filter pack (FP) species, nitric acid (HNO₃). Using ozone (O₃) behavior as a surrogate for HNO₃, correctionfactors (CF) are developed to estimate this bias. Weekly CF for O₃ depend on both site and season, and seasonal average weekly CF for O₃ at a given site may be as high as 1.25.The seasonal magnitude of this CF is generally largest in summerand is ordered: summer fall spring > winter. The CF is drivento a large extent by the diurnal correlation between C andV (i.e., both are generally higher during the day and lower at night). However, since the diurnal C profile at elevated sites is relatively constant, the resulting correlation between C and V is small, and the CF at montane sites is generally negligiblysmall. The sampling protocol using daytime integrated sampling for a week and nighttime integrated sampling for a week capturesthe diurnal correlation between C and V adequately and may be used to aggregate relatively unbiased weekly D estimates. Day-night CF for O₃ are close to unity, and limited results suggest similar behavior for HNO₃. Using these limited FP results, the site- and seasonally-specific weekly CF forO₃are refined to estimate the corresponding CF for HNO₃. Worst-case adjustments for HNO₃ as high as 30% are indicated for summer periods at a given site.