Groundwater quantitative status assessment for River Basin Management Plan 2022–2027 (RBMP III)

Q3 Earth and Planetary Sciences
P. Souvent, Urška Pavlič, M. Andjelov, Nina Rman, P. Frantar
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引用次数: 0

Abstract

The Groundwater quantitative status assessment is part of River Basin Management Plan 2022–2027 (RBMP III) and is used to evaluate, according to certain criteria, the 21 groundwater bodies (GWBs) in Slovenia. GWB can achieve good or poor quantitative status. The assessment is carried out with four tests, where the impact of groundwater abstraction (pumped quantities) on: groundwater quantity and water balance, the ecological status of associated surface water bodies, groundwater dependent terrestrial ecosystems and the intrusion of saline or poor water quality into the aquifer is analyzed. The final overall assessment of each groundwater body, based on the completed tests, is determined by the criterion of the worst test assessment. Based on the results of the tests, within the assessment period, 20 GWBs in Slovenia achieved good quantitative status. GWB Dravska kotlina achieved poor quantitative status, because the pumping of groundwater causes poor quality water intrusions into the deeper aquifer of that groundwater body. Within the last assessment period 1991–2020, approx. 4 billion m3 of groundwater was available annually in shallow aquifers within groundwater bodies. Groundwater abstraction (pumper quantities) in the period 2014–2019 reached an average of 135 million m3. In the area of deep geothermal aquifers of the Mura basin, abstractions were estimated to sum up to 2.5 million m3 per year. Latest numerical simulations point out induced aquifer recharge of approx. 2.3 million m3 of thermal water.
2022-2027 年河流流域管理计划(RBMP III)地下水定量状况评估
地下水定量状态评估是《2022-2027 年河流流域管理计划》(RBMP III)的一部分,用于根据特定标准对斯洛文尼亚的 21 个地下水体(GWB)进行评估。地下水体的定量状况可达到良好或较差。评估通过四项测试进行,分析抽取地下水(抽水量)对以下方面的影响:地下水水量和水平衡、相关地表水体的生态状况、依赖地下水的陆地生态系统以及含盐或劣质水侵入含水层。根据已完成的测试,每个地下水体的最终总体评估由最差测试评估标准决定。根据测试结果,在评估期内,斯洛文尼亚有 20 个地下水体达到了良好的定量状态。Dravska kotlina 地下水库的定量状况较差,因为抽取地下水导致劣质水侵入该地下水体的深层含水层。在上次评估的 1991-2020 年期间,地下水体中浅层含水层每年可利用地下水约 40 亿立方米。2014-2019 年期间,平均地下水取水量(泵水量)达到 1.35 亿立方米。在穆拉盆地的深层地热含水层地区,每年的取水量估计达 250 万立方米。最新的数值模拟显示,含水层的热能水诱导补给量约为 230 万立方米。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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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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