Ionic imbalance due to hydrogen carbonate from Asian dust

In an attempt to identify the ionic imbalance, hydrogen carbonate, HCO₃⁻ (bicarbonate), was determined together with the commonly determined nine major ions because the imbalance was frequently encountered in the chemical analysis of samples with high pHs. Titration method was applied for the determination of the samples with pH higher than 5.6. These samples amounted to 102 of the 1536 samples collected in Hokkaido, Northern Japan, from April 1998 to December 2002. Of the 102 samples, 74 (Group A) showed an acceptable ion balance without including HCO₃⁻. In the other 28 (Group B), however, inclusion of HCO₃⁻ successfully improved the ion balance. These results suggested that hydrogen carbonate was a potential candidate for explaining the imbalance. The hydrogen carbonate concentrations showed a strong correlation with the corresponding non-sea salt calcium (nss-Ca²⁺) concentrations, which implied that hydrogen carbonate was derived from calcium carbonate particles incorporated into falling raindrops or cloud droplets. For Group A, the relationship between hydrogen carbonate and the nss-calcium ion concentration was very similar to that for commonly suspended particles in Hokkaido. On the other hand, Group B exhibited a stronger but significantly different correlation. To the samples of Group B, a back-trajectory analysis was applied to demonstrate that the samples were associated with aerosol travelling from Northern China or Mongolia, which indicated that alkaline aerosol affected the chemistry. In consideration of these findings, the current standard of the ion balance should be critically reviewed for modification in regard to the contribution of hydrogen carbonate not only in source areas but also in receptor areas of alkaline aerosol.     

Effects of SO2 and H2O on low-temperature NO conversion over F-V2O5-WO3/TiO2 catalysts

F-V_2 O_5-WO3/Ti02 catalysts were prepared by the impregnation method.As the content of F ions increased from 0.00 to 0.35 wt.%,the NO conversion of F-V_2 O_5-WO_3/TiO_2 catalysts initially increased and then decreased.The 0.2 F-V_2 O_5-WO_3/TiO_2 catalyst(0.2 wt.% F ion)exhibited the best denitration(De-NOx) performance,with more than 95% NO conversion in the temperature range 160-360℃,and 99.0% N2 selectivity between 110 and 280℃.The addition of an appropriate amount of F ions eroded the surface morphology of the catalyst and reduced its grain size,thus enhancing the NO conversion at low temperature as well as the sulfur and water resistance of the V_2 O_5-WO3/Ti02 catalyst.After selective catalytic reduction(SCR) reaction in a gas flow containing SO_2 and H_2 O,the number of NH3 adsorption sites,active component content,specific surface area and pore volume decreased to different degrees.Ammonium sulfate species deposited on the catalyst surface,which blocked part of the active sites and reduced the NO conversion performance of the catalyst.On-line thermal regeneration could not completely recover the catalyst activity,although it prolonged the cumulative life of the catalyst.In addition,a mechanism for the effects of S02 and H_2 O on catalyst NO conversion was proposed.     

活性炭吸附低浓度SO_2烟气的研究

利用水洗再生活性炭吸附法，对模拟火力发电厂烟气及克劳斯炉尾气进行脱除ＳＯ２的试验研究，ＳＯ２脱除率大于９０％．     

铸态不锈钢光亮钝化新工艺研究

依据不锈钢钝化的几种理论现点和钝化机理,对工艺流程与若干工艺参数的选择进行了探讨。并列出了工艺配方的主要组份,从结构和蟹合两方面使H_2O_2稳定以获得显著效果。经本工艺处理的不锈钢,表面质量稳定,从根本上消除了氮氧化物及氟污染,环境效益与经济效益明显。     

低中放废物处置场核素经地下水迁移对环境影响预测

研究了我国某民用低中放固体废物处置场核素迁移的途径，对核素在地下水中的迁移进行了详细分析与计算，假定正常释放或一次降水量达到６００ｍｍ，处置场底浸泡一个月，存在６ｍ的包气带时，对该处置场处置的７种核素进行预测，结果表明，包气带是延迟核素迁移的主要屏障，在５００年内，可以使＾６０Ｃｏ＾１３７Ｃｓ＾９０Ｓｒ、＾６３Ｎｉ等核素延迟，其中＾２３９Ｐｕ降低６个月数量级，但不能延迟＾３Ｈ和＾１４Ｃ的迁移，穿过     

氧化塘合理的设计与操作

氧化塘不但可以低费用的降解废水，而且可以提供有用的生物量，其关键是进行合理的设计、操作和去除污泥．本文综合国外的文献资料，提出合理的设计和操作方案，并且引用国外试验者开发的预测模型；同时提出操作过程加入适当的ＣａＣｌ２化学添加剂可以促进藻类生物量的絮凝，以保证出水的质量和提供可利用的生物量．     

难降解有机废水处理新技术

介绍了光氧化法、超临界氧化和低温等离子体化学三种废水处理新技术的原理,国内外研究的现状和未来的发展前景,分析了这些新技术在优化污染物废水处理方面得到工业应用所必须解决的主要技术问题.     

Reduction of sera requirements in amniotic fluid cell culture

Reduction in serum requirement for culture of primary human amniotic fluid cells can be achieved by the addition of 10 growth-promoting factors to the nutrient medium. This supplemented medium preserves cell types normally found in amniotic fluid cell cultures supplemented with 20–30 per cent fetal bovine serum. The volume of amniotic fluid required to initiate culture can be as little as 1 ml. Amniotic fluid samples contaminated with red blood cells with no visible clot also grow well in the low serum medium. Cell-free amniotic fluid combined with equal parts of supplemented medium is useful in initiating cell culture.     

在降雨量极少的条件下日本琵琶湖北湖主要环境因子的动态变化和机理的研究(Ⅰ)(英文)

琵琶湖是日本第一大淡水湖,20世纪60年代以来,由于经济的发展,湖水水质逐步变坏。1977年湖的北部出现赤潮,1 983年湖的南部出现了湖泊富营养化的产物微囊藻。多年来,在深水区湖水温度分层情况下,叶绿素α或浮游植物主要分布在湖的表层。但在1 994年夏季降雨量极少的情况下,在深水区叶绿素α或浮游植物主要分布在温跃层的附近,这种现象在琵琶湖是罕见的。分析发现叶绿素的峰值在湖水温度分层时出现在温跃层的上部,而且底边界层同时出现了低溶氧和高浊度的现象。叶绿素α和溶氧、浊度的对应关系表明温跃层是一光合成活跃的区间。本文通过流体力学方程计算,结果表明随着温度的降低,粘滞力就会增加,在温跃层出现了随水深增加,粘滞力急剧增大的情况。由此可见颗粒物在温跃层顶的上部沉降速度比温跃层内快,因此颗粒物高浓度出现在温跃层内。计算结果同时发现,在水深10～20 m(对应于温跃层),分子扩散系数最小,一旦颗粒物进入这一区间就不易扩散出去。由于温跃层是一分子扩散系数小、粘滞力高的区间,所以温跃层是颗粒物和营养盐的富集区,出现了藻类和叶绿素浓度的峰值。     

在降雨量极少的条件下日本琵琶湖的环境因子的分布(英文)

琵琶湖是日本第一大淡水湖,20世纪60年代以来,由于经济的发展,湖水水质逐步变坏。1977年湖的北部出现赤潮,1983年湖的南部出现了湖泊富营养化的产物微囊藻。多年来,在深水区湖水温度分层情况下,叶绿素a或浮游植物主要分布在湖的表层(Tezuka,1984)。但在1994年夏季,降雨量极少的情况下,在深水区叶绿素a或浮游植物主要分布在温跃层附近,这种现象在琵琶湖是罕见的(Nakanishi,1995)。最近,琵琶湖北湖的藻类爆发显著增加了溶氧的消耗,导致了湖底层溶氧的减少。如果湖底层溶氧持续减少,底泥储存的磷就会释放到湖水中,从而加快湖泊富营养化的进程。本文分析了琵琶湖南北10个点1994年4月至1995年3月每月1次的常规观测资料,深入剖析了全湖物理化学参数的时空分布,不仅发现叶绿素的峰值在湖水温度分层时出现在温跃层的上部,而且湖底边界层同时出现了低溶氧和高浊度的现象。分析认为绿素a和溶氧、浊度的对应关系表明温跃层是一光合成活跃的区间。