| Title: | Hydrogeological characterization of karst springs of the white (Proteus anguinus anguinus) and black olm (Proteus anguinus parkelj) habitat in Bela krajina (SE Slovenia) |
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| Authors: | ID Koren, Katja (Author)
ID Brajkovič, Rok (Author)
ID Bajuk, Manca (Research coworker)
ID Vraničar, Špela (Research coworker)
ID Fabjan, Vesna (Research coworker) |
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| Files: |  PDF - Presentation file, download (13,65 MB)
MD5: 4C96A280F56463BE6F9C1EA28AEADD09
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| Language: | English |
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| Typology: | 1.01 - Original Scientific Article |
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| Organization: |  GeoZS - Geological Survey of Slovenia
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| Abstract: | The springs west of Črnomelj, in SE Slovenia, are the habitat of the black (Proteus anguinus parkelj) and the white olm (Proteus anguinus anguinus). Some of these springs are also the only known habitat in the world of endemic species of black olm. A steady decline in olm populations has been observed in this area over the past decades. Owing to the rapid runoff and groundwater flow high-resolution monitoring is essential in providing better insight into the hydrogeological characterization of the catchment area of springs. Specific factors and critical parameters of water behind said olm degradation have not yet been defined. Because the olm’s environment is largely aquatic, one potential critical parameter could be the higher water temperatures (>12 °C) or higher nitrate concentration (>9.2mg/l). The six-month observation of the springs (July – December 2021) point to water temperature as a potential critical parameter since the water temperature of the springs exceeded 12 °C in months July and August. Nitrate concentrations could also be a second critical parameter in the degradation of the olm’s habitat. Maximum nitrate concentrations above 9.2mg/l throughout much of the observation period (except for Dobličica spring). Due to less agricultural activity in December in the spring catchment area and a higher dilution rate due to reduced evapotranspiration and increased effective precipitation during this time of the year, the nitrate concentrations are decreased. The results of the measured parameters of groundwater could show the hydrogeological connection between the Otovski and Pački breg springs and between Šotor, Jamnice and Dobličica. The Obršec spring has an independent catchment area. A detailed estimation of the springs catchment area is possible due to a detailed geologic map. It is necessary to determine the origin of the nitrate (nitrate isotope analysis), to quantify the threshold values of the critical parameters, to define precisely all the causes of the olm deterioration, and to make proposals for appropriate measures to limit or even stop the decline of the olm population. |
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| Keywords: | hydrogeology, olm, ecology, nitrate, monitoring |
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| Publication status: | Published |
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| Publication version: | Version of Record |
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| Publication date: | 04.08.2023 |
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| Publisher: | Geološki zavod Slovenije |
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| Year of publishing: | 2023 |
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| Number of pages: | str. 151-166 |
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| Numbering: | vol. 66, no. 1 |
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| PID: | 20.500.12556/DiRROS-17835  |
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| UDC: | 556.3 |
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| ISSN on article: | 0016-7789 |
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| DOI: | 10.5474/geologija.2023.006 |
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| COBISS.SI-ID: | 164544259 |
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| Note: |
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| Publication date in DiRROS: | 16.01.2024 |
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| Views: | 550 |
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| Downloads: | 165 |
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