斯洛文尼亚东北部Pomurje浅层冲积含水层的地下水位振荡分析

Q3 Earth and Planetary Sciences
Urška Pavlič, P. Souvent
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引用次数: 0

摘要

自1952年以来,斯洛文尼亚一直在对国家一级的地下水数量进行系统的水文监测。对长期地下水位数据的深入了解使我们能够描绘出具有类似地下水位振荡特性的含水层部分,并识别这些特性随时间的变化。我们使用了各种统计方法来识别地下水体(GWB)Murska-kotlina的地下水位振荡的长期行为。结果表明,地下水位随时间的波动反映了一系列复杂的事件,这些事件源于自然或人为干扰。通过将百分位分析与聚类分析相结合,我们能够分离出地下水波动相关的区域。月地下水位的长期数据趋势分析结果表明,研究区气候对地下水位长期和季节波动的影响。除了自然原因外,通过对地下水位数据进行趋势分析,我们能够确定过去人类对环境的一些干预措施。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Groundwater level oscillation analysis in shallow alluvial aquifers in Pomurje, NE Slovenia
Systematic hydrologic monitoring of groundwater quantity at the national level in Slovenia has been ongoing since 1952. An insight into long-term groundwater level data enables us to delineate parts of aquifers with similar groundwater level oscillation properties as well as to identify changes of those properties in time. We used variety of statistical methods to identify long-term behaviour of groundwater level oscillation of groundwater body (GWB) Murska kotlina. Results showed that fluctuation of groundwater level in time reflect complex set of events that originate in natural or anthropogenic interferences. Using percentile analysis in combination with cluster analysis, we were able to isolate areas with a related groundwater fluctuation. Results of long-term data trends analyses of monthly groundwater level showed the impact of the research area climate on long-term and seasonal groundwater level fluctuation. In addition to natural causes, by performing trend analysis on groundwater level data, we were able identify some human induced interventions into the environment made in the past.
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来源期刊
Geologija
Geologija Earth and Planetary Sciences-Geophysics
CiteScore
1.00
自引率
0.00%
发文量
10
审稿时长
10 weeks
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