4-氯酚存在对生物强化系统降解2,4-二氯酚的影响研究

采用生物强化技术降解废水中的难降解有机物 2 ,4 二氯酚 (简称 2 ,4 DCP) ,研究了不同浓度的 4 氯酚 (简称 4 MCP)存在对 2 ,4 DCP降解的影响 ,并通过半连续流实验研究了 4 MCP长期存在下 ,强化系统中 2 ,4 DCP和 4 MCP降解速率的变化趋势 .结果表明 ,第 1次半连续流实验中 ,4 MCP浓度为 5、10、2 0及 30mg L时 ,都会对强化系统中 2 ,4 DCP的降解速率产生一定的抑制作用 ,而且抑制作用随着 4 MCP浓度的增加而增强 .随着半连续流实验次数的增加 ,4 MCP对 2 ,4 DCP降解的抑制作用减弱甚至消失 ,共基质时 2 ,4 DCP的降解速率反而比其单基质半连续流运行时快 .4 MCP与 2 ,4 DCP共基质存在时 ,2 ,4 DCP优先被微生物利用 ,此后 4 MCP才被降解 ,表现出两阶段降解的现象 .     

室内空气中的甲醛检测及控制

随着人们对居室装修要求的不断提高,人造板及油漆等在室内装修中已经广泛使用,随之而来的是由于装修引起的室内空气化学污染问题,室内空气中有害化学物质对人们身体健康的危害也越来越大,其中甲醛对人体的危害尤为严重.室内空气中甲醛的检测及控制已经得到各发达国家和国内的高度重视,对甲醛的检测和控制技术的改进也成为社会各界普遍关注的问题.     

Toxic Effect of a Pesticide, Diflubenzuron on Freshwater Microinvertebrate (Tetrahymena pyriformis)

Harmful bugs affect food production,directly by the qualitativeor quantitative reduction of the harvests,or indirectly while servinglike vectors of several illnesses of the plants and human[1].Many chemical products are used by human for a long time inthe…     

污水灌溉对水稻生长影响的模拟

本文根据各工厂污水排入大通河的负荷量，作污灌模拟试验。试验证明：１．各工厂排污所含有机物质超过一定量便对水稻生长及产量产生严重影响；２．用大通河水灌溉，也会影响水稻的生长及产量。这说明大通河水已受到各工厂污染物的严重污染。     

部分氮杂环类化合物的遗传毒性及其QSAR研究

本文利用蚕豆细胞微核试验评价了１０种氮杂环类化合物的遗传毒性，一化合物的最低未占据轨道能Ｅｌｕｍｏ、分子的量负的原子净电荷ｑ建立了较好的相关方程：ＭＮ＝－２．９６（１．１４）＋４．９３（０．４８）Ｅｌｕｍｏ＋１３．６８（２．７２）ｑ＾－Ｒ＾２＝０．９４ ＳＥ＝０．７１ Ｆ＝５３．９２ Ｐ〈０．０００５推测此类化合物的至于致毒机制可能是它们作为电荷给予体和氢键予体作用于生物受体而引起的突变。     

多效唑对水生生物的急性毒性评价研究

本文以斜生栅藻、大型水蚤和草鱼为试验生物,研究植物生长调节剂多效唑对水生生物的急性毒性效应。多效唑对斜生栅藻EC_(50)-96h为20.62mg/l;对大型水蚤LC_(50)-48h为21.86mg/h;对草鱼苗静态生物检测结果为LC_(50)—120h 16.33mg/l,流水生物检测结果为LC_(50)-96h 14.36mg/l,LC_(50)-120h 9.13mg/l。经多效唑处理后,藻的细胞形态也发生明显改变。根据农药的实验室毒性评价划分标准,多效唑对三种生物的毒性均属低毒;田间安全性预评价的结果也表明其毒性为低毒,故认为多效唑是一种对水生生物危害较小的农药。但其慢性毒性及长期积累效应,尚有待进一步研究。     

炼油厂汽提废水预处理工业试验

炼油厂汽提废水含较高浓度的酚 ,会对污水处理场产生冲击。采用上流式曝气生物滤池对废水进行预处理工业试验 ,取得了满意的试验结果 :出水酚浓度低于 9.0mg/L ,酚降解率 >90 % ,完全可以消除它对污水处理场的冲击。并通过工业试验为工艺设计和工业运行确定了有关参数和运行条件。     

Anomalous transport of colloids and solutes in a shear zone

Transport experiments with colloids and radionuclides in a shear zone were conducted during the Colloid and Radionuclide Retardation experiment (CRR) at Nagra's Grimsel Test Site. Breakthrough curves of bentonite colloids and uranine, a non-sorbing solute, were measured in an asymmetric dipole flow field. The colloid breakthrough is earlier than that of uranine. Both breakthrough curves show anomalously long late time tails and the slope of the late time tails for the colloids is slightly higher. Anomalous late time tails are commonly associated with matrix diffusion processes; the diffusive interaction of solutes transported in open channels with the adjacent porous rock matrix or zones of stagnant water. The breakthrough curves for different colloid size classes are very similar and show no signs of fractionation due to their (size-dependent) diffusivity. It is proposed that tailing of the colloids is mainly caused by the structure of the flow field and that for the colloid transport, matrix diffusion is of minor importance. This has consequences for the interpretation of the uranine breakthrough. Comparisons of experimental results with numerical studies and with the evaluation of the colloid breakthrough with continuous time random theory imply that the tailing in the conservative solute breakthrough in this shear zone is not only caused by matrix diffusion. Part of the tailing can be attributed to advective transport in fracture networks and advection in low velocity regions. Models based on the advection-dispersion equation and matrix diffusion do not properly describe the temporal and spatial evolution of colloid and solute transport in such systems with a consistent set of parameters.     

Estimating fugitive dust emission rates using an environmental boundary layer wind tunnel

Emissions from fugitive dust due to erosion of “natural” wind-blown surfaces are an increasingly important part of PM₁₀ (particulate matter with sizes of 10 μm aerodynamic diameter) emission inventories. These inventories are particularly important to State Implementation Plans (SIP), the plan required for each state to file with the Federal government indicating how they will comply with the Federal Clean Air Act (FCAA). However, techniques for determining the fugitive dust contribution to over all PM₁₀ emissions are still in their developmental stages. In the past, the methods have included field monitoring stations, specialized field studies and field wind-tunnel studies. The measurements made in this paper allow for systematic determination of PM₁₀ emission rates through the use of an environmental boundary layer wind tunnel in the laboratory. Near surface steady-state concentration profiles and velocity profiles are obtained in order to use a control volume approach to estimate emission rates. This methodology is applied to soils retrieved from the nation's single largest PM₁₀ source, Owens (dry) Lake in California, to estimate emission rates during active storm periods. The estimated emission rates are comparable to those obtained from field studies and lend to the validity of this method for determining fugitive dust emission rates.     

Wind Tunnel Experiments and Numerical Simulation of Snow Drifting around an Avalanche Protecting Dam

To learn about wind flow and snow drifting around avalanche dams, experiments were done in the Jules Verne Climatic Wind Tunnel. The paper reports the results from numerical wind flow simulations that were done to support the findings from the wind tunnel. Satisfying the model similitude criteria for the wind tunnel configuration was difficult due to the inevitable small geometric scale of the model, while on the contrary the snow drifting conditions in the facilities were full scale. By comparing numerical wind flow results of full scale and model scale dams with the snow pattern observed in the wind tunnel, it was possible to conclude that albeit poor model similitude, the snowdrifts on the windward side of the wind tunnel model are likely to indicate the full scale natural situation.