压力脉冲波法复杂天然气管道堵塞检测实验研究*

为了解决复杂天然气管道堵塞定位难题,快速定位出堵塞位置,提出利用压力脉冲波法检测复杂管道堵塞。改造搭建长18.1 m、包含17个三通结构的压力波堵塞检测实验台,进行不同堵塞率以及气液混输管道的堵塞定位实验。结果表明:管道三通会引起频率范围为150~200 Hz的高频反射波,利用FFT谐波变换方法可以有效地对原始信号进行滤波分析,更利于对堵塞定位分析。在堵塞率100%时,定位误差为1.07%;在堵塞率50%时,定位误差最大,达到1.93%;对于含液率8%的气液混输管道,100%堵塞时,定位误差为0.48%。研究结果有效地证实了压力脉冲法检测复杂输运管道堵塞的可行性,可为该方法的现场应用提供指导和数据支撑。     

废聚氨酯硬泡热处理特性及产物检测分析

利用热重分析仪和管式炉研究了废弃聚氨酯硬泡热处理特性并对热处理产物进行了检测分析。研究结果表明,废聚氨酯硬泡热处理过程呈单一剧烈失重峰,热失重主要发生在200～440℃之间,600℃热分解基本完成;FTIR谱图初步分析发现加热分解过程中有大量CO和CO2产生,且热处理过程中可能有O-H、C-H、C=O及带有苯环的物质生成。通过GC/MS检测分析结果显示热处理液体产物中检出多元醇以及苯胺、p-苯胺、苯甲腈等多种芳香类化合物,气体产物以低碳的烷烃和烯烃为主,可见FTIR和GC/MS分析结果有很好的一致性。研究结果显示,气体产物检测出有机氯化合物,这可能是聚氨酯硬泡生产过程中加入的氟利昂类发泡剂所致。     

葫芦[6]脲对印染废水中染料曙红的吸附特性及影响因素

考察了葫芦[6]脲(CB[6])对印染废水中典型染料曙红的吸附特性,研究了初始pH、吸附剂投加量、共存离子等对吸附效果的影响,并探讨了吸附机理。结果表明:在温度为25 ℃,曙红初始浓度为20 mg/L条件下,CB[6]投加量为0.5 g/L时,2 h吸附去除率为79.5%,吸附动力学特征符合准二级动力学方程;Langmuir等温模型拟合结果比Freundlich模型具更高的相关系数,由Langmuir 模型计算得出的最大吸附容量为413.05 mg/g,且随温度升高,最大吸附容量下降,表明CB[6]对曙红的吸附过程为放热过程;随溶液初始pH由3增至11,吸附容量从33.28 mg/g降至9.14 mg/g;共存阴离子对CB[6]吸附的不利影响顺序为PO^3-₄>CO^2-₃>NO^-₂>NO^-₃;CB[6]具有重复利用性,利用芬顿试剂3次再生后仍保持了原始材料84.9%的吸附容量。通过比表面积、核磁共振氢谱红外图谱和扫描电镜对样品进行表征,采用密度泛函理论计算的静电势分布图分析,揭示了CB[6]可能的吸附原理是其“腰部”与阴离子形式的曙红水解产物产生静电吸引,从而形成超分子外包结构组装体。     

鲤体内芳香烃受体的分离纯化及其与葸的相互作用

从暴露于污染物蒽的鲤肝脏中提取出芳香烃受体,并采用紫外可见分光光度计进行最大吸收波长扫描,再通过离子交换层析法分离纯化鲤体内的芳香烃受体,并采用聚丙烯酰胺凝胶电泳对受体进行鉴定,最后通过傅里叶变换红外光谱探讨芳香烃受体与蒽结合后的结构变化.结果表明,提取的芳香烃受体在280 nm处有特征吸收峰,测得质量浓度为27.3 mg/mL.通过离子交换层析法纯化了单一组分的受体蛋白质,其相对分子质量约为110 kD.测定了芳香烃受体的红外光谱,与蒽结合后其在一定波段的谱峰发生了明显位移,表明污染物配体蒽能与芳香烃受体结合,并对其蛋白二级结构产生明显影响.     

Effects of climatic data low-pass filtering on the ICBM temperature- and moisture-based soil biological activity factors in a cool and humid climate

The air temperature (T_air), total precipitation (TP) and potential evapotranspiration (PET) are standard input data for soil carbon dynamic models, i.e., for calculating temperature and moisture effects on soil biological activity. The resolution needed depends on objectives, the complexity of models and inbuilt pedotransfer functions. The Introductory Carbon Balance Model (ICBM) soil climate front end model calculates a multiplicative soil-temperature (r_{e_temp}) and -moisture (r_{e_wat}) factor with a daily time-step to estimate soil biological activity, i.e., r_{e_crop} = r_{e_temp} × r_{e_wat}. Our objective was to determine how much r_{e_temp}, r_{e_wat} and r_{e_crop} are affected by low-pass filtering of the climatic input data for a cool, humid temperate region. To achieve this we conducted spectral analysis on T_air, TP, PET and r_{e_crop} in the frequency domain. Thereafter we applied Fourier low-pass filters of 5, 15, 30, 60 and 180 days on T_air, TP, PET and tracked their effects through the soil climate model's state variables and outputs. This was done using a sandy and a heavy clay soil and an 89-year daily time-series from a meteorological station in Quebec (Canada). The Fourier spectra showed that the variance for T_air, PET and r_{e_crop} was dominated by an annual cycle, as could be expected. There was no yearly cycle for TP. The variation in r_{e_temp} explained most of the variance in r_{e_crop}. The soil climate module outputs were not sensitive to low-pass filtering of PET. A daily time-step was needed to avoid overestimating r_{e_crop} for the sandy soil. Using a weekly time-step for TP and T_air allowed us to explain about 80% of the variance in r_{e_crop} for the heavy clay soil. This study also indicates that the standard leaf (and green) area index functions for calculating transpiration should receive more attention, since they have significant effects on the state and output variables.     

GENERATING STREAMFLOW SEQUENCES WITH TREND AND CYCLICAL MOVEMENTS1

ABSTRACT: A first-order autoregressive model had been modified with the trend and cyclical movements to generate the streamflow sequences. Three main portions were involved in this modified model, i.e., six-year cycle with trend changing; six-year cycle without trend changing; and both annual and six-year cycles with trend changing. The synthetic sequences of monthly streamflow sequences were compared with the historical records obtained from the Kissimmee River basin by using the Chi-Square test for goodness-of-fit. The results indicated that the newly proposed model has a better solution than the original model because the trend and cyclical movements involved in generating sequences are much closer to the historical records.     

"傅里叶级数部分和逼近和函数"的动态演示

本文主要介绍利用多媒体创作软件Authorware制作教学演示课件，实现对“傅里叶级数的部分和逼近和函数”的过程的形象演示。     

数字地震记录中干扰波的排除

本文介绍了用MATLAB工具软件实现对数字信号进行频谱分析和设计IIR数字滤波器的方法,对数字地震记录中的干扰波进行谱分析和排除,实现了目标要求。     

Concentration field and turbulent fluxes during the mixing of two buoyant plumes

In this work an experimental study of mixing of two identical plumes, carried out in a turbulent neutral boundary layer generated in a wind tunnel, is presented. Measurements have been performed with fast flame ionisation detectors (FFIDs) and a two-component Laser-Doppler Anemometer system. Results allow the study of both the average and the fluctuating concentration field, including the turbulent vertical and longitudinal mass fluxes, in single plumes and during the interaction of two identical plumes. This information gives insight into the details of the mixing phase of the two plumes. Results of trajectories and additional rise (due to plume interactions) have been compared with previous measurements carried out in laminar cross-flows, showing similar behaviour. Concentration distributions in plume cross-sections in turbulent cross-flows differ from those measured in laminar cross-flows. Average vertical and longitudinal velocity measurements into the plume core show the strength of the shielding effect of the upwind plume and some details of interaction between the counter-rotating vortex pairs (CVPs). For large values of the alignment angle φ, between the line joining the stacks and the cross-flow, an average negative vertical velocity is measured in the middle of the plume even if its centre of mass is rising. This downward velocity is induced by the slow interaction of the CVPs and generates a vertical stretching of the plume and negative rise enhancement. Vertical turbulent fluxes change sign on the plume centreline and are of opposite sign with respect to the longitudinal turbulent fluxes. Results indicate a good linearity between vertical turbulent fluxes and concentration gradients, with different proportionality for the top and bottom parts of the plume (especially in the near field) indicating that dispersion could be described by a gradient-transfer model.     

垃圾衍生燃料热重-红外联用法的热解特性

实验以中小城市垃圾典型组分合成RDF,利用热重-傅立叶变换红外光谱(TG-FTIR)联用法对其热解特性进行了研究,并求解了RDF热解反应动力学参数。结果表明城市垃圾合成RDF具有较高的热值,煤的混入具有良好的助燃效果,单一组分及RDF混合组分的热解服从动力学基本方程表征的规律,可以用来获得动力学参数。