Cartographic support of identification of natural and man-made sources of dissolved matter in lake Baikal basin

Y. Semenov, A. Silayev, M. Semenov
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Abstract

A method of GIS mapping was developed to identify and assess the contributions of sources of matter to the composition of surface waters. The basis for the creation of the GIS database was the results of the study of the spatial diversity of the chemical composition of surface waters. Geoinformation analysis included the creation of a digital framework for mapping, vectorization of mapping sources and Earth remote sensing materials, creation of a single database combining cartographic, statistical information and field observation materials, morphometric relief analysis based on a digital relief model, creating a landscape basis for base maps, creating thematic maps, analyzing changes in the components of geosystems, creating electronic cartographic layers allowing to identify participation of solute sources in formation of water composition. The analysis of component changes was based on the results of different-time studies of the composition of water and bottom sediments. Based on the comparison of the chemical composition of the waters of the Baikal tributaries with the chemical and mineralogical composition of rocks, an approach was developed to identify sources of solute and assess their contributions to the formation of macro- and microelement compositions of surface waters. To solve the problems of the study, methods of statistical analysis of data, multicomponent mixing using systems of linear equations, field methods of data collection were used. Three main categories of solute sources (silicate, sulfide-containing silicate, carbonate rocks) were identified and their contributions to the chemical composition of water were calculated. On the basis of microelement tracers, the contributions of silicate rocks were divided into contributions of primary and secondary silicate rocks, ore-containing silicate rocks without sulfides were isolated. By comparing the ratios of concentrations of trace elements in the waters of uncontaminated territories and wastewater of enterprises, tracers were identified that made it possible to identify sources of surface water pollution. Maps of territories that determine a certain chemical composition of surface waters were compiled, which was first classified on the basis of the ratio of the contributions of drained rocks.
贝加尔湖流域溶解物自然和人为来源识别的制图支持
开发了一种地理信息系统制图方法,以确定和评估物质来源对地表水组成的贡献。建立地理信息系统数据库的基础是地表水化学成分空间多样性研究的结果。地理信息分析包括建立数字制图框架,对制图源和地球遥感资料进行矢量化,建立结合制图、统计信息和实地观测资料的单一数据库,基于数字地形模型的地形测量分析,为基础地图创建景观基础,创建专题地图,分析地球系统组成部分的变化,创建电子地图层,以确定溶质来源在水成分形成中的参与。成分变化的分析是基于不同时间对水和底部沉积物组成的研究结果。通过对贝加尔湖支流水的化学组成与岩石的化学和矿物组成的比较,提出了一种确定溶质来源并评估其对地表水宏观和微量元素组成形成的贡献的方法。为了解决研究中的问题,采用了数据统计分析、线性方程组多组分混合、现场数据采集等方法。确定了三大类溶质源(硅酸盐、含硫化物硅酸盐和碳酸盐岩),并计算了它们对水化学成分的贡献。根据微量元素示踪剂,将硅酸盐岩的贡献分为原生硅酸盐岩和次生硅酸盐岩,分离出无硫化物的含矿硅酸盐岩。通过比较未受污染地区的水和企业废水中微量元素浓度的比例,确定了示踪剂,使识别地表水污染源成为可能。绘制了确定地表水的某种化学成分的领土地图,首先根据排水岩石的贡献比例对其进行分类。
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来源期刊
CiteScore
0.90
自引率
0.00%
发文量
2
审稿时长
8 weeks
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