德拉夫斯科-普图伊斯科平原地下水干旱的统计分析

Q3 Earth and Planetary Sciences Geologija Pub Date : 2019-12-24 DOI:10.5474/geologija.2019.012
Simona Adrinek, M. Brenčič
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引用次数: 1

摘要

干旱是一种复杂的现象,可以用多种方式来定义。这是一个全球性的日益严重的问题,发生的时间从几个月到几年不等。干旱有几种类型,但研究最少的是地下水干旱。在全球范围内,对它的研究是在最近十年才开始的。在斯洛文尼亚,几乎没有关于地下水干旱的数据。在本研究中,我们着重于对单个地下水位站的地下水位图进行统计分析,以确定地下水干旱的时期。使用的第一种方法是基于由较低的百分位数定义的排名统计数据,这表明地下水水位较低。另一种方法是基于单一标准化地下水指数(SGI)。以德拉夫斯科-普图伊斯科平原第四纪无约束含水层为例进行了研究。结果表明:各地下水位站的地下水亏缺是同时发生的,但各干旱期的亏缺强度和持续时间不同;重要的结论是,地下水干旱的强度不取决于事件的长度,而更多地取决于非饱和含水层的厚度
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Statistical analysis of groundwater drouht on Dravsko-Ptujsko polje
Drought is a complex phenomenon and can be defined in many ways. It is a globally growing problem that occurs on a time scale ranging from months to years. There are several types of drought, but the least investigated is groundwater drought. Globally, research on it started relatively recently, in the last decade. In Slovenia, there are almost no data on groundwater drought. In this research, we focused on statistical analysis of groundwater level diagrams of individual groundwater stations, which can determine periods of groundwater drought. The first method used is based on ranking statistics defined by lower percentiles that indicate low groundwater level. Another approach was based on univariant Standardized Groundwater Index – SGI. As a case study, the unconfined Quaternary aquifer of Dravsko-Ptujsko polje was chosen. The results show that the groundwater deficits in the groundwater stations appear simultaneously but differ in intensity and duration of each drought period. The important conclusion is that the intensity of groundwater drought does not depend on the length of an event but more on thickness of the unsaturated aquifer
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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
期刊最新文献
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