用积雪状况评价中国城市环境的技术性污染

IF 0.7 Q4 GEOSCIENCES, MULTIDISCIPLINARY
E. Bondarevich
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引用次数: 1

摘要

分析了外贝加尔湖契塔市积雪中重金属(Zn、Cd、Pb、Cu)的污染情况,并将其污染水平与邻近地区的相似特征进行了比较。反演伏安法可以发现,雪中水溶性有毒微量元素的含量是中国以外其他定居点的几倍。然而,这些值(指标)的中位数很接近。在生态和地球化学系数中也发现了类似的结果(指标),根据这些结果,中国城市可能属于平均污染水平(ZC = 35.66)的地区。其他城市积雪中重金属流动形态的积累趋势也具有类似的特征,这是由Saet系数的低值(ZC < 32)引起的。结果表明,积雪中液体部分的电荷系数较高。因此,为了安全使用,渔业用水应用清水稀释75.24倍,经济用水和饮用用水应用清水稀释9.4倍。积雪粉尘部分重金属含量较低,但工业区和住宅多层建筑区所有微量元素浓度均超过最大允许值(TLV阈值)。与此同时,其他居民点的类似数据值更大,超出TLV值(最大允许浓度)的数十倍和数百倍。考虑化学元素毒性的总污染指数(ZC = 72.5) (ZCT = 98.8)表明,中国的地球化学条件处于平均水平。对于大多数其他城市,Saet系数值较小32,对应于低和中等污染水平。根据粉尘负荷水平,赤塔市的污染程度较高(Pn≥10吨/公里),意味着降尘量在8000吨以上。从总负荷指数(Zp = 493.5)来看,中国城市化地区粉尘分值为高污染地区,其中镉(Cu = 255.47)是主要污染源。将我们的结果与其他研究人员的结果进行比较,可以得出这样的结论:在21世纪初苏联解体期间,积雪的污染明显减少。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Assessment of technogenic pollution of the urban environment in Chita by the snow cover state
The pollution of the snow cover in the city of Chita (Transbaikalia) with heavy metals (Zn, Cd, Pb, and Cu) is analyzed, and a level of its pollution is compared with similar characteristics in the cities of neighboring regions. The method of inversion voltammetery made possible to find that the content of water-soluble forms of toxic trace elements in the snow is several times greater than in other settlements outside Chita. However, the median values of these values (indicators) are close. Similar results (indicators) were also noted in the ecological and geochemical coefficients, according to which the city of Chita may be attributed to areas with the average level of pollution (ZC = 35.66). Trends in the accumulation of mobile forms of heavy metals in the snow cover of other cities were similar features as it follows from low values of the Saet coefficient (ZC < 32). The charge coefficient calculated for the liquid fraction of the snow cover was found to be high. Therefore, for safe use, melt water should be diluted with clean water 75.24 times for fishery purposes and 9.4 times for economic and drinking use. Rather low content of heavy metals was found in the dust fraction of the snow cover, but in the industrial zone and the zone of residential many-storeyed buildings concentrations of all trace elements exceeded the maximum permissible values (TLV threshold limit value). At the same time, similar data for other settlements had still greater values, and the exceedings were tens and hundreds times greater the TLV values (the maximum permissible concentrations). The total pollution index (ZC = 72.5) with consideration for the toxicity of chemical elements (ZCT = 98.8) shows that the geochemical conditions in Chita is at the average level. For most other cities, values of the Saet coefficient were smaller 32 that corresponds to low and medium pollution levels. According to the level of dust load Chita is characterized by a high level of pollution (Pn ≥ 10 tons/km), and it means that more than 8000 tons of dust fall to the snow cover. It has been found that by the total load index (Zp = 493.5) the dust fraction characterizes urbanized territory of Chita as highly polluted, and in this case cadmium (Cu = 255.47) is the main polluter. Comparison of our results with those of other researchers allows making the conclusion that during the period of the Soviet Union disintegration by the beginning of the XXI century pollution of a snow cover notably reduced.
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来源期刊
Led i Sneg-Ice and Snow
Led i Sneg-Ice and Snow GEOSCIENCES, MULTIDISCIPLINARY-
CiteScore
1.50
自引率
42.90%
发文量
11
审稿时长
8 weeks
期刊介绍: The journal was established with the aim of publishing new research results of the Earth cryosphere. Results of works in physics, mechanics, geophysics, and geochemistry of snow and ice are published here together with geographical aspects of the snow-ice phenomena occurrence in their interaction with other components of the environment. The challenge was to discuss the latest results of investigations carried out on Russia’s territory and works performed by Russian investigators together with foreign colleagues. Editorial board works in collaboration with Glaciological Association that is professional community of specialists in glaciology from all republics of the Former Soviet Union which are now new independent states. The journal serves as a platform for the presentation and discussion of new discoveries and results which help to elucidate the state of the Earth’s cryosphere and the characteristics of the evolution of the snow-ice processes and phenomena under the current conditions of rapid climate change.
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