Assessment of the geoecological state of small water currents in polder lands: methodological approach and cartographic support

S. Zotov, Y. Spirin
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引用次数: 1

Abstract

The watercourses of the Kaliningrad region are one of the most important natural components with a multi-purpose use. Unfortunately, their geoecological state is assessed as unsatisfactory due to the negative impact exerted on them. The region includes unique polder lands, the watercourses of which are highly vulnerable to negative natural and anthropogenic impacts. These watercourses are poorly researched, in the post-Soviet period they were not actually explored, which led to a lack of information in various scientific and practice-oriented areas. All of the above emphasizes the importance of conducting geoecological studies of the watercourses of the polder lands. The aim of the research is to assess the geoecological state of the basins of small watercourses in the polder lands of the Slavsky District with further cartographic visualization of its spatial differentiation. A methodical approach has been developed to obtain a geoecological indicator represented by a quantitative indicator of polluting chemicals in water, leveling the information deficit, by conjugated analysis of available, but very limited hydrological, hydrochemical and geoecological data. Formulas and calculated dependencies are obtained that allow one to find quantitative characteristics of pollution in the rivers of other polder regions, taking into account the designated limits of application. The spatial differentiation of the geo-ecological state of the basins of small watercourses in the Slavsky District was identified and mapped by 13 criteria, divided into interrelated groups: anthropogenic load, water quality, the territory’s ability to self-purify, transit capacity. The geoecological state of the researched watercourses and their watersheds is characterized as “highly stressed”: for the river. Osa—“very tense” (3.95 % of the land); for r. Zlaya—“tense” (5.93 % of land); in the basins of the Shlyuzovaya and Nemoninka rivers—“conflict” (38.96 % of land), the rest of the area—“highly stressed” (51.16 % of land).
圩地小水流地质生态状况评估:方法方法和制图支持
加里宁格勒地区的水道是最重要的自然组成部分之一,具有多种用途。不幸的是,由于对它们的负面影响,它们的地质生态状况被评估为不令人满意。该地区包括独特的圩田,其水道极易受到负面的自然和人为影响。这些水道的研究很少,在前苏联时期,它们实际上没有被探索过,这导致了各种科学和实践导向领域的信息缺乏。所有这些都强调了对圩地水道进行地质生态学研究的重要性。该研究的目的是评估斯拉夫斯基地区圩区小水道流域的地质生态状况,并进一步对其空间分异进行地图可视化。通过对现有但非常有限的水文、水化学和地质生态数据的综合分析,已制订了一种有条理的方法,以取得以水中污染化学物质的数量指标为代表的地质生态指标,弥补资料不足。得到的公式和计算出的依赖关系使人们能够在考虑到指定的应用范围的情况下,找出其他圩区河流污染的数量特征。根据人为负荷、水质、领土自净能力、过境能力等13项指标,确定并绘制了斯拉夫斯基地区小水道流域地质生态状态的空间分异。所研究的水道及其流域的地质生态状态对河流来说是“高度紧张”的。Osa -“非常紧张”(3.95%的土地);r. Zlaya -“紧张”(5.93%的土地);在Shlyuzovaya河和Nemoninka河流域-“冲突”(38.96%的土地),其余地区-“高度紧张”(51.16%的土地)。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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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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