Karkonosze国家公园(西苏台德,波兰西南部)活跃交换区水域中的铝

Pub Date : 2019-12-01 DOI:10.2478/bgeo-2019-0018
H. Marszałek, M. Rysiukiewicz
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引用次数: 1

摘要

摘要:本文研究了Karkonosze国家公园(KPN)主要孔隙-裂隙含水层和地表水中铝浓度的变化规律。该分析基于2015年8月在Karkonosze Mts地区进行的采样结果,并辅以2010-2016年在Karkonosze Mts选定集水区进行的水质监测结果,观察到铝浓度的显著空间变异,从几十到超过1090 μg/L,随着测量点的高度而增加。最高的浓度记录在Karkonosze山脉的山脊地带,那里的pH值最低。
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Aluminium in waters of the active exchange zone in the Karkonosze National Park (Western Sudetes, SW Poland)
Abstract The paper presents the variability of aluminum concentrations in groundwater of the main porous-fissured aquifer and surface waters in the area of the Karkonosze National Park (KPN), covering mainly the upper parts of the Karkonosze Mts. The analysis was based on the results of samplings carried out in the area of the KPN in August 2015 and supplemented with the results of water quality monitoring carried out during the period of 2010–2016 in selected catchments of the Karkonosze Mts. Significant spatial variability of aluminium concentrations was observed, from several dozen to over 1,090 μg/L, increasing along with the height of the measurement points. The highest concentrations were recorded in the ridge zone of the Karkonosze Mts, where the pH is the lowest.
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