Channel flow and trichloroethylene treatment in a partly iron-filled fracture: experimental and model results

Technical developments have now made it possible to emplace granular zero-valent iron (Fe(0)) in fractured media to create a Fe(0) fracture reactive barrier (Fe(0) FRB) for the treatment of contaminated groundwater. To evaluate this concept, we conducted a laboratory experiment in which trichloroethylene (TCE) contaminated water was flushed through a single uniform fracture created between two sandstone blocks. This fracture was partly filled with what was intended to be a uniform thickness of iron. Partial treatment of TCE by iron demonstrated that the concept of a Fe(0) FRB is practical, but was less than anticipated for an iron layer of uniform thickness. When the experiment was disassembled, evidence of discrete channelised flow was noted and attributed to imperfect placement of the iron. To evaluate the effect of the channel flow, an explicit Channel Model was developed that simplifies this complex flow regime into a conceptualised set of uniform and parallel channels. The mathematical representation of this conceptualisation directly accounts for (i) flow channels and immobile fluid arising from the non-uniform iron placement, (ii) mass transfer from the open fracture to iron and immobile fluid regions, and (iii) degradation in the iron regions. A favourable comparison between laboratory data and the results from the developed mathematical model suggests that the model is capable of representing TCE degradation in fractures with non-uniform iron placement. In order to apply this Channel Model concept to a Fe(0) FRB system, a simplified, or implicit, Lumped Channel Model was developed where the physical and chemical processes in the iron layer and immobile fluid regions are captured by a first-order lumped rate parameter. The performance of this Lumped Channel Model was compared to laboratory data, and benchmarked against the Channel Model. The advantages of the Lumped Channel Model are that the degradation of TCE in the system is represented by a first-order parameter that can be used directly in readily available numerical simulators.     

超声波/零价铁(US/Fe)协同降解氯酚类化合物的QSPR研究

在同一反应条件下测定US/Fe协同降解6种氯酚类化合物的降解速率常数(κ).采用软件Chemoffice2005内置的MOPAC2002计算氯酚类化合物的分子结构参数,运用偏最小二乘(PLS)回归分析方法,对氯酚类化合物进行定量结构-性质相关(QSPR)研究,得到预测性较好的模型.模型结果显示,影响US/Fe协同降解性能(logK)的主要因素是Vp、Ehomo、logKow、(Elumo-Ehomo)2和Elumo-Ehomo.推测在US/Fe协同体系中:(1)氯酚类化合物的降解反应不是以空化泡内热解反应为主;(2)Fe表面的吸附作用对降解反应起决定影响,且氯酚化合物与·OH的氧化反应占主导作用.     

速度场常数及其自动检测装置

通过对烟道“速度场常数”的研究,提出利用速度场常数监测烟道烟气平均流速的方法,同时研制出速度场常数自动检测装置。解决烟道烟气平均流速自动监测的技术难题。     

快速生物活性测定方法的仪器化

好氧活性污泥法在污水处理中应用广泛.保持污泥活性,是良好处理效果的前提,也是运行控制的主要目标.活性污泥的呼吸速率,或者氧利用速率(oxygen uptake rate,OUR),能够指示污泥的活性变化.本研究开发的快速生物活性测定仪(rapid biological activity tester,RBAT),能够快速测定污泥活性参数,满足工程设计与运行的迫切要求.     

pH值和碳氮比对亚硝酸型反硝化影响的研究

利用序批式反应器中长期驯化好的以亚硝酸盐为主要基质的纯种污泥,做锥形瓶实验,分别研究pH和碳氮比对亚硝酸型反硝化的影响。结果表明,亚硝酸型反硝化适宜的pH范围在7.7～8.6,最佳pH值在8.2左右;碳氮比（C/N）大于1.94,可实现连续稳定的脱氮效果,起始亚硝氮比基质降解速率随C/N的增加而增加,大于3.11速率几乎不再增加,通过动力学分析,得出该实验条件下C/N的饱和常数Ks为9.36。     

SBR系统中活性污泥内源呼吸速率的研究

在SBR污水处理系统中应用呼吸速率测定仪对活性污泥的呼吸速率进行测定,探讨了污泥浓度和温度对内源呼吸速率的影响.对大量的比内源呼吸速率数据进行处理后发现,在混合液温度基本不变的基础上,内源呼吸速率与污泥浓度变化趋势一致,即比内源呼吸速率与污泥浓度无关;而温度对比内源呼吸速率的影响十分显著.这些结论为呼吸速率成为SBR工艺的控制参数提供了基础.     

蒽和菲的酶促降解条件及动力学特征

研究了蒽和菲酶促降解的最佳反应条件及其动力学特性.结果表明,利用黄杆菌FCN2产生的胞内酶降解蒽、菲时的最佳pH为6,而且在弱酸性介质中胞内酶的活性较高;在30℃-35℃之间胞内酶能保持较好的降解活性,32℃时胞内酶活性最高.对蒽和菲酶促降解的米氏常数分别为3×10-4 mol·l-1和4×10-4 mol·l-1,相同实验条件下,对蒽降解的最大反应速率为2×10-6mol·l-1·min -1,对菲的最大反应速率为1×10-6mol·l-1·min -1.酶促降解蒽的反应级数接近于0.93,表观速率常数的对数lgk为-1.86,而降解菲的反应级数接近于0.76,表观速率常数的对数lgk为-2.05.     

单因子超载的综合环境承载力计算方法研究

文章分析了当前普遍使用的矢量模法计算综合环境承载力的不足,建立了单因子超载的环境承载符号函数法模型,提出了以环境占用率为表征的环境承载占用率法;验证结果表明新模型和方法较矢量模法更为合理。     

东海春季赤潮前后沉积物-海水界面营养盐交换速率的研究

应用实验室培养法现场研究了3～5月东海硅藻赤潮发生前后10个站位的营养盐在沉积物-海水界面的交换,并应用连续函数拟合法计算了营养盐的界面交换速率.结果显示,NO^-₃-N在赤潮前向沉积物中汇聚［-1.33～－0.68 mmol/(m²·d)］,赤潮后却基本由沉积物向海水中释放［－0.69～0.82 mmol/(m²·d)］.NH⁺₄-N在赤潮前后大都从沉积物中释放［－0.65～1.46 mmol/(m²·d)］,赤潮后释放速率小于赤潮前.NO^-₂-N赤潮前后除Zc17站外都向沉积物中汇聚［－0.09～0.05 mmol/(m²·d)］,赤潮后汇聚速率稍高.SiO^2-₃-Si在所有站位都由沉积物向海水释放［0.85～9.23 mmol/(m²·d)］,其赤潮后速率高于赤潮前.PO^3-₄-P在赤潮前向沉积物中汇聚［－0.06～－0.01 mmol/(m²·d)］,在赤潮后却由沉积物向海水中释放［0～1.26 mmol/(m²·d)］.NO^-₃-N和PO^3-₄-P向东海近海沉积物的汇聚在春季不利于硅藻赤潮的暴发,但其在硅藻赤潮暴发后从沉积物的大量释放为后面紧接的大面积甲藻赤潮的暴发提供了重要的营养物质补充.