波兰低地地下水动态状况:以Gwda河集水区为例

IF 0.9 Q3 GEOLOGY
Geologos Pub Date : 2019-12-01 DOI:10.2478/logos-2019-0021
Izabela Jamorska, Katarzyna Kubiak-Wójcicka, A. Krawiec
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引用次数: 3

摘要

摘要本研究的目的是在1981 - 2015年的35年间,监测Gwda河集水区第四纪和新近纪含水位线的地下水位变化。此外,由于集水区某些地区的年总降水量差别很大,因此试图确定降水对地下水位位置的影响。通过对地下水位与气象参数(降水)的相关性分析,发现前一年的降水对地下水位的影响最大。此外,在地下水位波动中无法看出集水区南部的总降水量较低,这与观测井在排水区内的位置以及较深含水层的升水有关。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Dynamics of the status of groundwater in the Polish Lowland: the River Gwda catchment example
Abstract The aim of the present study is to monitor changes in the location of the groundwater table in the catchment area of the River Gwda within the Quaternary and Neogene water-bearing level over a 35-year period, between 1981 and 2015. In addition, on account of very diverse total annual precipitation levels in particular parts of the catchment, attempts were made to determine the influence of precipitation on the location of the groundwater table. By correlating groundwater level and meteorological parameters (precipitation), it was discovered that precipitation in the previous year made the largest impact on the groundwater table. Moreover, low precipitation totals in the southern part of the catchment are not discernible in groundwater table fluctuations, which is linked to the location of the observation well within the drainage zone as well as to water ascension from deeper aquifers.
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来源期刊
Geologos
Geologos GEOLOGY-
CiteScore
1.70
自引率
0.00%
发文量
7
审稿时长
12 weeks
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