Karst groundwater protection in the Kupa River catchment area and sustainable development

被引:21
作者
Biondic, B
Biondic, R
Kapelj, S
机构
[1] Univ Zagreb, Fac Geotech Engn, Varazhdin 42000, Croatia
[2] Croatian Geol Survey, Dept Hydrogeol & Engn Geol, Zagreb 10000, Croatia
来源
ENVIRONMENTAL GEOLOGY | 2006年 / 49卷 / 06期
关键词
Kupa River catchment area; Karst springs; protection system; groundwater; hydrogeology; Croatia;
D O I
10.1007/s00254-006-0178-4
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
One of the most significant water resources in the Republic of Croatia is the catchment area of the Kupa River, located in the region bordering the Republic of Slovenia. About 88% of the total amount of water in this catchment originates in Croatia and just 12% from Slovenia; therefore, the largest part of the catchment area (about 1000 km(2)) is on the Croatian side of the border. It is a typical karst area of the Dinarides with aquifers characterized by a relatively rapid water exchange, high groundwater flow velocities and aquifers open to human impact from the surface. Consequently, the aquifers are highly vulnerable and at risk. Due to the availability of large quantities of high-quality spring water (about 6 m(3)/s), the entire area has a strategic importance within the context of any future development strategy pertaining to the western part of Croatia. The catchment area on the Croatian side was investigated using a wide range of research methods that included a classical hydrogeological approach, the detailed hydrologic calculation of water balance to the hydrogeochemical analyses and modelling. The objective was to determine protection zones and protection measures for the whole area. The difficulties are increased due to the fact that the karst catchment area is crossed by major traffic corridors, oil pipelines and a railway and that many settlements and a highly developed wood industry are present. The combination of protecting water resources with adequate prevention measures and necessary remedial activities that should satisfy the very strict requirements necessary for the protection of the karst aquifers while still allowing for present and future human activities is difficult - but not impossible - to achieve. One good example is the present highway with a closed dewatering system and waste water treatment before the water passes into the karst underground system.
引用
收藏
页码:828 / 839
页数:12
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