Hydrogeological characterization of karst springs of the white (Proteus anguinus anguinus) and black olm (Proteus anguinus parkelj) habitat in Bela krajina (SE Slovenia)

Q3 Earth and Planetary Sciences
Katja Koren, R. Brajkovič, Manca Bajuk, Špela Vraničar, Vesna Fabjan
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引用次数: 0

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 (>9.2 mg/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 9.2 mg/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.
贝拉克拉伊纳(斯洛文尼亚东南部)白榆(Proteus anguinus anguinus)和黑榆(Proteus anguinus parkelj)栖息地岩溶泉的水文地质特征
斯洛文尼亚东南部Črnomelj以西的泉水是黑色(Proteus放血的parkelj)和白色olm(Proteuus放血的)的栖息地。其中一些泉水也是世界上唯一已知的黑色olm特有物种的栖息地。在过去的几十年里,该地区的olm人口一直在稳步下降。由于径流和地下水流迅速,高分辨率监测对于更好地了解泉水集水区的水文地质特征至关重要。所述olm降解背后的水的具体因素和关键参数尚未确定。由于olm的环境主要是水生的,一个潜在的关键参数可能是较高的水温(>12°C)或较高的硝酸盐浓度(>9.2 mg/l)。对泉水的六个月观测(2021年7月至12月)表明,水温是一个潜在的关键参数,因为泉水的水温在7月和8月超过了12°C。硝酸盐浓度也可能是olm栖息地退化的第二个关键参数。在整个观测期的大部分时间里,最大硝酸盐浓度超过9.2毫克/升(Dobličica春季除外)。由于春季集水区12月的农业活动较少,以及每年这个时候蒸发蒸腾量减少和有效降水量增加导致的稀释率较高,硝酸盐浓度降低。地下水测量参数的结果可以显示Otovski和Pački breg泉水之间以及Šotor、Jamnice和Dobličica之间的水文地质联系。Obršec泉有一个独立的集水区。由于有详细的地质图,可以对泉水集水区进行详细估计。有必要确定硝酸盐的来源(硝酸盐同位素分析),量化关键参数的阈值,准确定义olm恶化的所有原因,并提出适当措施的建议,以限制甚至阻止olm种群的下降。
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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