Parsęta河的水文形态和物理化学条件

Pub Date : 2018-12-01 DOI:10.2478/bgeo-2018-0015
J. Szpikowski, G. Szpikowska
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引用次数: 0

摘要

摘要:根据水框架指令对河流进行水文形态评估。为评价Parsęta河流环境质量,采用河流生境调查法。这项研究于2016年6月进行,提供了水文形态学问题的概述,还涵盖了对其水质的测量和实验室分析。沿河选取了24个测量断面。这些区段的选择考虑了遗传上不同类型河谷的代表性、河谷的大小和流量以及人为压力的变异性。评价结果表明,Parsęta河流自然质量变化较大(HQA指数在17 ~ 61之间),河谷的改造变化较大,但总体较低(HMS指数在0 ~ 33之间)。分析断面中,第2 (II)类和第3 (III)类占79%,第1 (I)类占8%,第4 (IV)类占13%。Parsęta河中部断面自然程度最高,改造程度最低。壶穴成因的河谷段比河流成因的河谷段变形更大。根据其理化参数对Parsęta河水质进行了评价,表明该河水质良好。单个河流水参数通常属于第一(I)类和第二(II)类。任何水质低于“良好”水平的情况都是由于磷酸盐浓度超过第二(II)类,并且包含在Białogard以下15公里的河流范围内。水文形态自然度高的河段水质最差。
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Hydromorphological and physicochemical conditions of the Parsęta River
Abstract Rivers are hydromorphologically assessed in line with the Water Framework Directive. In order to assess the quality of the Parsęta River environment, the River Habitat Survey method was applied. The research studies, conducted in June 2016, provided an overview of hydromorphological issues, and also covered measurements and laboratory analyses on the quality of its waters. There were 24 measuring sections selected along the whole river. The selection of these sections took into account the representativeness of genetically various types of river valley, its size and discharge, and the variability of anthropogenic pressure. The assessment showed that the Parsęta River varies in natural quality (its HQA index ranged from 17 to 61) and that the modification of its valley is variable but generally low (its HMS index ranged from 0 to 33). Seventy-nine percent of the analysed sections were classified to the second (II) and third (III) hydromorphological classes, 8% to the first (I), and 13% to the fourth (IV). The central section of the Parsęta River has the highest degree of naturalness and the lowest degree of transformation. The river valley sections of kettle-hole origin are more transformed than those of fluvial origin. The quality of the Parsęta River waters assessed on the grounds of their physicochemical parameters indicates that the river is in good condition. The individual river water parameters are most often within the first (I) and second (II) classes. Any instances of the quality of waters being below the “good” level are due to phosphate concentrations exceeding the second (II) class and are contained within a 15-km stretch of the river below Białogard. A river section with a high degree of hydromorphological naturalness has the worst quality of waters.
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