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1.
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. 相似文献
2.
Molly K. Chambers Daniel M. White Michael R. Lilly Larry D. Hinzman Kristie M. Hilton Robert C. Busey 《Journal of the American Water Resources Association》2008,44(2):316-327
Abstract: Lakes are important water resources on the North Slope of Alaska. Freshwater is required for oilfield production as well as exploration, which occurs largely on ice roads and pads. Since most North Slope lakes are shallow, the quantity and quality of the water under ice at the end of winter are important environmental management issues. Currently, water‐use permits are a function of the presence of overwintering fish populations, and their sensitivity to low oxygen concentrations. Sampling of five North Slope lakes during the winter of 2004‐2005 shed some light on the winter chemistry of four lakes that were used as water supplies and one undisturbed lake. Field analysis was conducted for oxygen, conductivity, pH, and temperature throughout the lake depth, as well as ice thickness and water depth. Water samples were retrieved from the lakes and analyzed for Na, Ca, K, Mg, Fe, dissolved‐organic carbon, and alkalinity in the laboratory. Lake properties, rather than pumping, were the best predictors of oxygen depletion, with the highest dissolved‐oxygen levels maintained in the lake with the lowest concentration of constituents. Volume weighted mean dissolved‐oxygen concentrations ranged from 4 to 94% of saturation in March. Dissolved oxygen and specific conductance data suggested that the lakes began to refresh in May. 相似文献
3.
Boxman AW Peters RC Roelofs JG 《Environmental pollution (Barking, Essex : 1987)》2008,156(3):1252-1259
In a Scots pine forest the throughfall deposition and the chemical composition of the soil solution was monitored since 1984. (Inter)national legislation measures led to a reduction of the deposition of nitrogen and sulphur. The deposition of sulphur has decreased by approximately 65%. The total mineral-nitrogen deposition has decreased by ca. 25%, which is mainly due to a reduction in ammonium-N deposition (−40%), since nitrate-N deposition has increased (+50%). The nitrogen concentration in the upper mineral soil solution at 10 cm depth has decreased, leading to an improved nutritional balance, which may result in improved tree vitality. In the drainage water at 90 cm depth the fluxes of NO3− and SO42− have decreased, resulting in a reduced leeching of accompanying base cations, thus preserving nutrients in the ecosystem. It may take still several years, however, before this will meet the prerequisite of a sustainable ecosystem. 相似文献
4.
Sheppard PR Speakman RJ Ridenour G Witten ML 《Environmental monitoring and assessment》2007,130(1-3):511-518
This paper describes the use of lichen chemistry to assess airborne tungsten and cobalt in Fallon, Nevada, where a cluster
of childhood leukemia has been on going since 1997. Lichens and their rock substrates were collected from Rattlesnake Hill
within Fallon as well as from four different rock outcrops located north, east, south, and west of Fallon and at least 20 km
away from the town center. In the lichens themselves, W and Co are significantly higher within Fallon than in the combined
control site outside of Fallon. In the rock substrates of the lichens, no differences exist in W and Co. The W and Co differences
in lichens cannot be attributed to substrate geochemistry. Fallon is distinctive in west central Nevada for high airborne
W and Co, and given its cluster of childhood leukemia, it stands to reason that additional biomedical research is in order
to test directly the leukogenicity of combined airborne W and Co. 相似文献
5.
大气微生物与气象条件及大气污染物的灰色关联分析 总被引:4,自引:0,他引:4
根据大气微生物浓度、气象因子和大气污染理化因子的监测结果,应用灰色关联分析原理,分析研究大气微生物浓度与气象条件和大气污染物的关联程度,说明气象因子对各类微生物浓度的影响大于大气污染因子,特别是对耐高渗透压霉菌。 相似文献
6.
利用一个三维非静力区域大气化学输送模式与中尺度气象模式MM5相连接构成一个数值模拟系统,模拟了中国地区对流层臭氧与其前体物的分布以及二氧化硫转化为硫酸盐的过程,模式扬地面源排放、大气输送和扩散、干沉积、气相化学反应和云雨过程。结果表明:日间,O3浓度主要由NOx和NMHC的源排放和光化学反应过程支配,大气辐射是光化学反应强弱的决定因子,其强度可使SO2、O3和SO4^2-的生成浓度呈现不同的日变化和季节变化,结果表明高浓度的O3对二氧化硫转化为硫酸盐的化学过程有很大的促进作用,然而,这种作用受NMHC浓度的影响很大,较高浓度的NMHC使O3浓度上升,但同时增加了对OH等自由基的消耗,使SO2的转化率降低。 相似文献
7.
可持续发展概念指导下的化学--绿色化学 总被引:1,自引:0,他引:1
阐述了人类文明发展到绿色文明阶段时所产生的化学思想方法与传统化学思想方法的差别,分析了作为绿色文明积极实践者的绿色化学的产生背景以及从原材料、反应历程、分离技术、产品和包装方面与传统方法的差别,指山了今后绿色化学的发展趋势。 相似文献
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