1. Razporeditev makrofitov v kraški reki Rak in ocena stanja vodnega ekosistemaDarja Kopitar, Marija Kravanja, Aleksander Trajbarič, Mateja Germ, 2022, original scientific article Abstract: Kraški svet predstavljajo geografsko in geološko izjemno dinamična območja, ki so močno povezana z delovanjem vode. Presihajoča vodna telesa v kraškem svetu s svojim delovanjem močno vplivajo na okolje. V največji meri se morajo na velike spremembe dostopnosti vode prilagajati sesilni organizmi, kakršni so rastline. Njihova prisotnost, abundanca in razporeditev lahko služijo kot indikatorji stanja vodnih ekosistemov. S pomočjo prirejene metode RCE (ang. A Riparian, Channel, and Environmental Inventory) smo reko Rak uvrstili v najvišje RCE kakovostne razrede. Na osnovi indeksa RMI (ang. River Macrophyte Index) smo reko Rak uvrstili v dobro oz. zelo dobro ekološko stanje. Dobra ekomorfološka ohranjenost reke Rak verjetno botruje tudi pojavljanju ogroženih rastlinskih vrst; med 38 popisanimi taksoni smo zaznali prisotnost enajstih vrst, ki so uvrščene na Rdeči seznam ogroženih praprotnic in semenk. V času našega vzorčenja je bila v tej reki prvič zaznana vrsta Zannichellia palustris. Visoka ocena ohranjenosti presihajoče kraške reke Rak potrjuje dosedanje dobro upravljanje in je pomembna pri udejanjanju naravovarstvenih smernic za prihodnost. Keywords: karst, macrophytes, RCE method, RMI, river Rak, kras, vodni makrofiti, RCE metoda, reka Rak Published in DiRROS: 14.01.2026; Views: 81; Downloads: 30
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2. Slovene Classical karst: Kras Plateau and the Recharge Area of Ljubljanica RiverFranci Gabrovšek, Andrej Mihevc, Cyril Mayaud, Matej Blatnik, Blaž Kogovšek, 2022, original scientific article Abstract: The area of the Classical Karst is roughly defined by a triangle with Ljubljana, Trieste and Rijeka as its vertices. This is the area where the first scientific studies of karst phenomena were conducted. Two sub-regions that particularly attracted researchers are presented. Kras/Carso plateau with the Škocjan caves and the underground course of the Reka river. The groundwater flow of Reka-Timavo is characterised by high recharge variability of allogenic inflow of Reka River and flow restrictions in the upper part of subterranean flow, which control regional backfloodings observed in cave systems. The recharge area of Ljubljanica Springs is known for a cascading series of poljes in intermediate cave systems. The area has been in focus of hydrological studies for over a century, but many phenomena have been resolved in the last decade based on results of continuous autonomous monitoring in the last decade. Keywords: Classical Karst, Kras, Škocjanske Jame, Reka-Timavo system, Ljubljanica Recharge Area, Polje Published in DiRROS: 13.01.2026; Views: 82; Downloads: 56
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3. CO₂ and temperature variations during peak tourist season in Lepe jame (Postojna Cave, Slovenia)Matija Perne, Marija Zlata Božnar, Primož Mlakar, Boštjan Grašič, Dragana Kokal, Franci Gabrovšek, 2025, original scientific article Abstract: We present and analyze measurements of CO₂ concentration and air temperature taken during the peak tourist season of 2017 in Lepe Jame, a poorly ventilated passage within Postojnska Jama, Slovenia. During the study, the passage was visited by between 5500 and 6500 visitors per day. Both parameters show pronounced diurnal fluctuations, primarily driven by visitor activity. As part of our campaign, we tested and confirmed the effectiveness of enhanced ventilation—achieved by opening the artificial tunnel connecting Postojnska Jama to Črna Jama—in preventing excessively high CO₂ concentrations. The measure is, however, questionable, as it affects the microclimate in Črna Jama. Although CO₂ concentration and temperature are correlated, notable differences emerge in the shapes of their respective rise and recession curves. Temperature increases more rapidly with the arrival of visitors, while it decreases more slowly after visiting hours compared to CO₂. This lag is attributed to thermal storage: heat from visitors is absorbed by the cave walls during the day and gradually released into the cave during the night. Keywords: karst, cave climate, show cave, carbon dioxide, cave monitoring Published in DiRROS: 10.01.2026; Views: 149; Downloads: 64
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4. Reduced soil quality with cultivation of calcareous soils in subtropical China karst regionMengxia Zhou, Hui Yang, Cheng Zhang, Jianhua Cao, Degen Zhu, 2025, original scientific article Abstract: Cultivation practices significantly impact soil functionality and quality, however, the effects of different cultivation durations remain inadequately quantified in the fragile karst ecosystems of southwestern China. This study employed a chronosequence approach to assess agricultural soil quality changes and identify their key drivers. Five land-use stages were selected and sampled: a natural reserve forest (NR) as a reference, recently burned land (0 a), and cultivated lands with durations of 1, 5, 15, and 30 years (1 a, 5 a, 15 a, 30 a, respectively) in the subtropical karst region of southwestern China. The soil quality index (SQI) was constructed using both the Total Data Set (TDS) and Minimum Data Set (MDS) methods. Principal component analysis (PCA) identified calcium (Ca), silt content and silicon (Si) as the key indicators within the MDS. Both TDS and MDS assessments revealed a progressive decline in SQI with increasing cultivation duration following slash-and-burn practices (R²=0.67 between TDS- and MDS-derived SQIs), indicating that agricultural activities significantly alter soil physicochemical properties and lead to soil degradation. The observed decrease in soil quality may be explained by two main mechanisms: (1) depletion of the soil-forming matrix in shallow karst environments; and (2) accelerated loss of acid-insoluble residues due to enhanced weathering under cultivation. These findings highlight the high vulnerability of karst soils to long-term farming, where inherently limited pedogenic materials and intense chemical weathering collectively exacerbate quality decline. This study provides critical insights for developing sustainable land management strategies in karst regions, emphasizing the importance of practices that conserve soil fertility, reduce residue loss, and maintain essential ecosystem services. With the MDS model explaining 67% of the variance in the TDS-based SQI, it represents an efficient and practical tool for monitoring soil quality in fragile karst environments, thereby supporting evidence-based sustainable land use planning. Keywords: Soil quality index (SQI), Minimum data set (MDS), Total data set (TDS), Cultivation, Karst region Published in DiRROS: 10.01.2026; Views: 120; Downloads: 66
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5. Characteristics and reasons for the discharge interruption of the Iskrets karst spring (Western Balkans, Bulgaria)Aleksey Benderev, Evelina Damyanova, Marin Ivanov, Yordanka Donkova, Peter Gerginov, Doncho Karastanev, Boriana Tchakalova, 2025, original scientific article Abstract: The Iskrets spring is one of the most significant karst springs in Bulgaria. А specific feature of this spring are irregular and abrupt reductions of its discharge after some earthquakes as well as other reasons related to the recharge. This study aims to present a reasonable hypothesis for the reasons of the discharge interruptions. A main feature of the Iskrets karst system is the fact that it is dominated by unconfined water flow in the unsaturated zone with velocities varying in a wide range. This creates conditions for significant erosion, transport and redeposition of the fluvial cave sediments. As a result, in the zones where there is a sharp decrease in the water velocity, a considerable accumulation of sediments occurs which can even fill the entire section of the passage-way and leads to a temporary blocking of the spring discharge. It is supposed that an appropriate section where this happens is located near to the discharge point of the spring. Most likely the main reason for the cave deposit displacement is the soil liquefaction caused by the seismic impact. It has been found that the duration of the discharge interruption period is longer at low water flow rates. Keywords: karst spring, regime, interruption of the flow, cave sediments Published in DiRROS: 10.01.2026; Views: 110; Downloads: 102
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6. Factors influencing the groundwater circulation in Mali me Gropa karst massif, Central AlbaniaRomeo Eftimi, Viacheslav Andreychouk, Peter Malík, Tatiana Orehova, Małgorzata Nita, Perikli Qiriazi, 2025, original scientific article Abstract: There are 23 carbonate karst areas in Albania with a total area of 6440 km2, or 24% of the country’s territory. Karst aquifers are the richest in the country and about 80% of the water supply for the population living in cities is supplied by karst water. One of the most interesting karst massifs of Albania is called Mali me Gropa (MMG) with a total surface area of 157 km2. It is the subject of this paper. Although this massif has attracted attention due to its exceptional development of surface karst landforms (karst pits, sinkholes, swallow holes) and its large and high-quality groundwater resources, it has not been the subject of comprehensive research. In this paper, for the first time, is a summary of the results of a combination of specialized studies, including geomorphological characterization, analysis of long-term groundwater regime observations in relationship with meteorological data, water balance studies applying the recently developed WaterbalANce software method, assessment of groundwater quality and its variability, determination of the groundwater flow velocity with an artificial tracer, and the use of hydrochemistry and runoff data to determine groundwater flow patterns and sensitivity of spring water to contamination. The results of the multi-method studies conducted on the MMG karst massif will inform future studies of the numerous carbonate karst regions in Albania. A final important objective of this article is to raise public awareness about the vulnerability of karst waters and the need to protect the associated ecosystem, especially now that the MMG karst massif is in the spotlight for tourism development. Keywords: MMG karst massif, spring’s regime, effective precipitation, water resources, Albania Published in DiRROS: 10.01.2026; Views: 94; Downloads: 43
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7. Formation of clastic sediments in the Atl cave of the Sierra Zongolica, Veracruz Mexico, and their relationship to the soil coverPamela Garcia, Rafael López-Martínez, Sergey Sedov, Hugo Salgado-Garrido, Teresa Pi Puig, Héctor Cabadas-Báez, 2025, original scientific article Abstract: Allochthonous cave sediments contain important paleontological and archaeological records as well as indicators of recent ecological processes. Correct interpretation of these records requires knowledge about the sediment sources and deposition processes, in particular the interrelation of vertical and lateral sediment transport. Compared to platform karst, knowledge about tropical mountainous karstic geosystems is quite limited. To trace the origin and transportation pathways of sediments, we investigated Atl Cave in the Sierra Zongolica Mountain range, Veracruz, Mexico. Field exploration and mapping have shown that the cave presents two horizontal stages representing phreatic conduits and ancient stability stages and is an epigenetic cave with a point recharge zone at the entrance, which is fed by a stream. A comparative study of the surface soil profiles and the diamicton facies of the cave floor deposits included field morphological description, micromorphological observations, grainsize analysis, colorimetry, bulk chemical composition via XRF, and clay mineral identification by XRD. The results demonstrate that the cave deposits have more similarities with the young alluvial and colluvial soils near the entrance than with mature Terra Rossa developed over the limestone formation that hosts the cave. This proves the predominant role of the lateral alluvial transport by high energy events in the formation of the cave diamicton with very restricted contribution of the vertical erosion of Terra Rossa. The main source rock for alluvial and colluvial materials transported to the cave are siliciclastic sediments of the Necoxtla formation, whereas Terra Rossa soils were formed from tephra of the Orizaba volcano. High CIA values, high clay content with a predominance of kaolinite, point to greater weathering of Terra Rossa in comparison with other studied surface and underground materials. Keywords: Mountainous karst, Atl cave, Cave sediments, Sediment formation, Soil cover, Lateral erosion Published in DiRROS: 10.01.2026; Views: 132; Downloads: 57
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8. Characteristics and importance of protected Karst springs in the southern mountainous region of AlbaniaErmira Jashiku, Ermiona Braholli, Edlira Menkshi, 2025, original scientific article Abstract: Karst formations in Albania cover an area of 6750 km², which represents 24% of the country's territory. The country has 110 karst springs with discharges exceeding 100 litters per second. Among these, Bistrica springs stands out as the largest, with an average discharge of 18.4 cubic meters per second. This study focuses on the Southern Mountain Region of Albania, known for its important karst water resources. In this region, 12 karst springs are protected due to their essential natural, scientific, educational, aesthetic and economic value. The objective of this research is to perform a geoinformatics analysis and evaluation of these protected karst resources. To achieve this, we collected extensive literature on protected springs, as well as reach data about the protected springs of the study area and analysed them using ArcGIS 10.1 software to generate geoinformation about these resources. This geoinformation includes a wide range of geographic and geologic-hydrogeological data. We aim to improve the understanding and promotion of protected karst resources in the Southern Mountain Region of Albania. Keywords: Southern Mountainous Region of Albania, karst spring, geoinformation, geomonument Published in DiRROS: 10.01.2026; Views: 82; Downloads: 56
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9. Modelling flow and transport to assess the influence of subsurface geometry on Alpine karst aquifer vulnerabilityBarbara Fleck, Lukas Plan, Bernhard Grasemann, Cyril Mayaud, 2025, original scientific article Abstract: Karst areas are highly susceptible to contamination due to rapid recharge and throughflow caused by their heterogeneous structure with unknown networks of conduits embedded in a matrix of low conductivity. Vulnerability methods have been used to ensure adequate protection of drinking water resources. However, most of the studies assessing the vulnerability of karst aquifers consider it as a constant value in time and, therefore, under special hydrological conditions in space, which is an oversimplification of reality. In this work, the behaviour of an Alpine karst system characterised by rapid flow and transfer through vertical shafts has been studied by discrete numerical modelling using MODFLOW 6. Six numerical models have been designed with the aim of representing simple common geometrical configurations found in Alpine karst systems. These models simulate how the flow and transport response at the system outlet is influenced by the aquifer geometry and recharge conditions. The results confirm that the arrival of the tracer at the spring strongly depends on the conduit geometry and the recharge conditions. This demonstrates that karst aquifer vulnerability cannot be defined as a constant value but should be specifically assessed depending on the spatio-temporal conditions. Keywords: Alpine karst system, numerical flow and transport modelling, vulnerability, overflow, MODFLOW 6 Published in DiRROS: 10.01.2026; Views: 84; Downloads: 47
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10. Are caves enough to represent karst groundwater biodiversity? Insights from geospatial analyses applied to European obligate groundwater-dwelling copepodsEmma Galmarini, Mattia Di Cicco, Barbara Fiasca, Nataša Mori, Mattia Iannella, Tiziana Di Lorenzo, Francesco Cerasoli, Diana Maria Paola Galassi, 2025, original scientific article Abstract: Caves are recognized as biodiversity hotspots for groundwater fauna, including obligate groundwater-dwelling copepods (Crustacea: Copepoda), exhibiting high species richness, endemism, and phylogenetic rarity. However, the extent to which caves alone provide a representative estimate of copepod species richness in karst areas remains uncertain. Taking advantage of the recently published EGCop dataset, the first expert-validated, Europe-wide occurrence dataset for obligate groundwater-dwelling copepods (hereinafter, GW copepods), this study investigates the distribution of GW copepods into karst areas, comparing species richness in caves versus other karst groundwater habitats (e.g., springs, karst streams, artificial wells), within and among the European karst units. The main aims are: (i) identifying karst areas which represent hotpots of GW copepod species richness; (ii) assessing to which extent caves, as open windows to the subterranean environments, contribute to define hotspots of GW copepods’ species richness into karst areas across Europe. EGCop comprises 6,986 records from 588 copepod species/subspecies distributed among four orders: Cyclopoida (3,664 records, 184 species), Harpacticoida (3,288 records, 395 species), Calanoida (32 records, seven species), and Gelyelloida (two records, two species). To perform geospatial analyses, we filtered the dataset by: (i) selecting only the records with spatial uncertainty in the associated coordinates lower than 10 km; (ii) searching for those records falling within, or very close to, the polygons representing European karst areas. Species richness hotspots were then estimated through geospatial analyses in geographic information system (GIS) environment. Within the selected records, those specifically referring to karst habitats (2,526 records, 369 species) are primarily represented by Harpacticoida (1,199 records, 228 species) and Cyclopoida (1,293 records, 132 species). Among species collected from karst habitats, records from caves (1,867, 73.9%) belong to 318 species (Harpacticoida = 189, Cyclopoida = 122, Calanoida = 7), representing 86.1% of the total species richness of karst habitats. Geospatial analyses reveal that the European hotspots of GW copepods’ species richness recorded exclusively in caves reflect the spatial arrangement of postglacial refugia in southern karst regions, though representing a subset of the broader diversity found across all karst groundwater habitats. Our findings highlight that the contribution of cave systems in groundwater biodiversity assessments and related conservation planning may vary depending on the evolution and morphologies of the target karst regions—often pointing to a high representativeness of caves for subterranean biodiversity, sometimes revealing their lower explanatory power within the broader karst systems. Keywords: copepoda, groundwater, biodiversity, datasets, caves, karst, Europe Published in DiRROS: 19.12.2025; Views: 179; Downloads: 137
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