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[根据土壤和河床质中汞热形态含量对汞进行调控的方法]

[The approach to the regulation of mercury according to the content of its termoforms in soils and bed loads].

作者信息

Bogdanov N A

出版信息

Gig Sanit. 2017;96(2):106-13.

PMID:29446589
Abstract

The article contains the results of the ecological and hygienic diagnostics of conditions of lands of areas of different sizes and varying degrees of urbanization, located in different agro-climatic conditions of European Russia (the southern Astrakhan region, he city of Moscow). Assessments of the state of territories use a new approach to rationing of Hg according to quantitative ratios of the content of its thermoforms in soils, grounds and alluvium (in litho substrate). The method of diagnostics is based on known properties of Hg forms: their geochemical activity (migration mobility) and toxicity decline along with the increment of the Hg temperature threshold of the release in the process of continuous warming up of the litho substrate sample (up to 1100°C). Thermoforms are not tied to specific minerals or chemicals and are conditionally designated as FR (Free: <180°C), CL (Chloride: 180-250°C), FS and CS (physically and chemically sorbed: 250-400°C), SU (Sulfide: 400-500°C) IS (isomorphic: >500°C) Hg forms. Among forms, also conditionally according to complexes of low, medium and high temperature variations(FR + CL, FS + CS and SU + IZ, respectively, there are selected groups of «mobile», «sustainable» and «inert» forms. For technogenic Hg there is characterized the predominance in the sample of «mobile» and to lesser extent degree - «stable» thermoforms. The more intensive this predominance is, the higher is environmental hazard. The natural accumulation is diagnosed by the presence and prevalence of the sum of moderate - and high-temperature inert forms of Hg. According to the ratios of Hg content, its forms and groups, as well as the density of correlationships between them, 6 indices of the conditions of soils and alluvium were developed by ourselves.Main coefficients out of indices on informativeness of results of diagnostics are the following factors: Endogenous input, Geochemical activity and Hg mobility. With regard to the combination of variability in indices, the total amount of Hg, the genesis and intensity of its accumulation (natural or anthropogenic), there were also developed ranking scales of the ecological and hygienic condition of the land areas and surface water bodies. As a result, on the base of such approach to the regulation of Hg the information value of assessments of mercury contamination of land significantly increased. At the objects of assessments there were identified following areas: foci of the manifestation of Hg hypolimnetic emanations on the landscape surface - dispersion halos in the areas of the Earth crust fracture (the dome of the Astrakhan gas condensate field); environmentally dangerous (sometimes even at a low total content of Hg) parts of cities, towns, their districts, as well as beds of watercourses and water reservoirs bottom (the Volga river valley and delta, the Lefortovo quarter in Moscow). There was also diagnosed the threshold of the background distribution of gross Hg content detected = 0.2-0.3 mg/kg. Its magnitude is consistent with domestic and abroad safe levels of Hg accumulation in soils = 0.3-0.4 mg/kg. The approach provides the differentiation of the environmental hazard lands. Technology of the approach can be used in the development of normative Document for the diagnosis of environmental and sanitary condition of territories in the system of Classifications of hazard of waste, in decontamination of territories, water areas and land zoning according to the criteria of natural or anthropogenic Hg accumulation.

摘要

本文包含对位于俄罗斯欧洲部分不同农业气候条件下(阿斯特拉罕地区南部、莫斯科市)不同规模和不同城市化程度地区土地状况进行生态与卫生诊断的结果。对区域状况的评估采用了一种新的汞定量配给方法,该方法依据土壤、地面和冲积层(岩石基质中)汞热形态含量的定量比例。诊断方法基于汞形态的已知特性:其地球化学活性(迁移流动性)以及随着岩石基质样品持续升温(直至1100°C)汞释放温度阈值的增加,其毒性下降。热形态不与特定矿物或化学物质相关联,被有条件地指定为FR(游离态:<180°C)、CL(氯化物态:180 - 250°C)、FS和CS(物理和化学吸附态:250 - 400°C)、SU(硫化物态:400 - 500°C)、IS(同晶态:>500°C)汞形态。在这些形态中,还根据低温、中温和高温变化的组合(分别为FR + CL、FS + CS和SU + IZ),挑选出“可移动”、“稳定”和“惰性”形态组。对于人为源汞,其特征在于样品中“可移动”形态占主导,“稳定”热形态程度较低。这种主导越强烈,环境危害就越高。自然积累通过汞的中高温惰性形态总和的存在和占比来诊断。根据汞含量、其形态和组的比例以及它们之间的相关密度,我们自行制定了6个土壤和冲积层状况指标。诊断结果信息性指标中的主要系数如下因素:内源输入、地球化学活性和汞流动性。关于指标变异性的组合、汞总量、其积累的成因和强度(自然或人为),还制定了陆地区域和地表水体生态与卫生状况的排名量表。结果,基于这种汞调控方法,土地汞污染评估的信息价值显著提高。在评估对象中确定了以下区域:景观表面汞次表层排放表现的焦点区域——地壳断裂区域的扩散晕(阿斯特拉罕气田凝析气顶);城市、城镇及其区域的环境危险部分(有时即使汞总含量较低),以及水道河床和水库底部(伏尔加河流域和三角洲、莫斯科的列福托沃区)。还诊断出检测到的总汞含量背景分布阈值 = 0.2 - 0.3毫克/千克。其数值与国内外土壤中汞积累的安全水平 = 0.3 - 0.4毫克/千克一致。该方法实现了对环境危害土地的区分。该方法的技术可用于制定危险废物分类系统中区域环境与卫生状况诊断的规范性文件,以及根据自然或人为汞积累标准对区域、水域进行去污和土地分区。

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