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  • 1
    Publication Date: 2023-07-25
    Description: Not far from the coast of Izola, Slovenia, are twelve funnel-shaped depressions on the seabed containing springs of warm, sulphurous water. These submarine depressions with springs are divided into three groups: from east to west, Izola, Bele skale, and Ronek. Water with similar thermal and sulphuric properties also occurs in the terrestrial spring in Izola. Some of these submarine springs (M03 - Izola, M05 - Bele skale and M10, M11 - Ronek) and the terrestrial spring (K04) were sampled for hydrogeochemical study. Three sampling campaigns took place in June and July 2020, October 2020, and April 2021. In addition, samples of seawater (SW01, SW02, SW03), groundwater from a well (VK01) and local non-sulphuric springs (K01, K02, K03) were taken for comparison. The submarine spring water was sampled using 100-ml syringes. In April 2021, an 8-litre Niskin water sampler (OceanTest Equipment, Inc.) was used in addition to the syringes. Samples collected in April 2021 using two different methods are labeled with an additional letter: /B for syringes and /N for Niskin. In-situ physicochemical parameters - pH, temperature, electrical conductivity, oxidation-reduction potential, and dissolved oxygen - were measured in the samples from the seawater and the submarine springs using a digital Multi 3430 meter (WTW GmbH, Weilheim, Germany) as soon as they were brought aboard the boat. Measurements of the terrestrial waters were performed on site using the same digital meter. A total of 26 water samples were collected for further analysis. All water samples were collected in HDPE bottles, except those for isotopic composition of dissolved inorganic carbon, which was sampled directly to Labco glass ampoules after 0.45 µm pore-sized membrane filtration. The samples were then chemically treated where required and stored in a refrigerator until analysis. The samples were then prepared for further laboratory analysis: geochemical composition (cations, anions), isotopic composition of oxygen (δ¹⁸O) and hydrogen (δ²H), total alkalinity (TA), isotopic composition of dissolved inorganic carbon (δ¹³CDIC), tritium activity (³H), isotopic ratio of strontium (⁸⁷Sr/⁸⁶Sr), and isotopic composition of sulphur (δ³⁴Sₛ₀₄ ‰) and oxygen (δ¹⁸Oₛ₀₄ ‰) in sulphate. This database contains information on the sampling dates and basic characteristics of the sampling sites, as well as the results from field measurements and laboratory analyses.
    Keywords: Alkalinity, total; Alkalinity, total, standard deviation; Aluminium; Antimony; Arsenic; Barium; Beryllium; Bismuth; Bromide; Cadmium; Caesium; Calcium; Cerium; Chloride; Chromium; Cobalt; Comment; Conductivity, electrical; Continuous flow isotope ratio mass spectrometer (CF-IRMS), Sercon, Europa Scientific 20-20, ANCA-TG preparation module; Copper; Date/Time of event; Dual inlet-isotope-ratio mass spectrometer (DI-IRMS), Finnigan MAT GmbH, Finnigan MAT Delta plus; Dysprosium; Element analyser (EA), Costech and continuous flow isotope ratio mass spectrometer (CF-IRMS), ThermoQuest, Finnigan Delta PlusXL; Erbium; Europium; Event label; Fluoride; Gadolinium; Gallium; Germanium; Gran titration; according to Gieskes, 1974; with pH electrode, Mettler Toledo, AG 8603; Group; Hafnium; Holmium; hydrogeochemistry; Indium; Inductively coupled plasma - mass spectrometry (ICP-MS), PerkinElmer, Thermo icapQ; Ion Chromatograph, Thermo Fisher Scientific, Dionex DX-120; Iron; isotopic composition; Izola_K01_1; Izola_K01_2; Izola_K02_1; Izola_K02_2; Izola_K03_1; Izola_K03_2; Izola_K04_1; Izola_K04_2; Izola_K04_3; Izola_M03; Izola_M03/B; Izola_M03/N; Izola_M05_1; Izola_M05_2; Izola_M05/B; Izola_M05/N; Izola_M10; Izola_M11; Izola_M11/B; Izola_M11/N; Izola_SW01; Izola_SW02; Izola_SW03; Izola_SW04; Izola_VK01_1; Izola_VK01_2; karst aquifer; Lanthanum; Latitude of event; Lead; Liquid Scintillation Counting- Guard Compensation Technology (LSC-GCT), PerkinElmer, Quantulus GCT 6220 [Super Low Level LSC]; Lithium; Longitude of event; Lutetium; Magnesium; Manganese; Mercury; Molybdenum; Multi-collector ICP-MS (MC-ICP-MS), Ametek, Nu Plasma II; Multi-parameter meter, Xylem Analytics, Multi 3430; Neodymium; Nickel; Niobium; Nitrate; Nitrite; Oxidation reduction (RedOx) potential; Oxygen, dissolved; pH; Phosphate; Potassium; Praseodymium; Rubidium; Samarium; Sample code/label; Sample ID; Sample method; Scandium; Selenium; Silicon; Silver; Site; Slovenia; Sodium; Strontium; Strontium-87/Strontium-86 ratio; Strontium-87/Strontium-86 ratio, standard deviation; submarine springs; Sulfate; Sulfur; Tantalum; Tellurium; Temperature, water; Terbium; Thallium; Thermal Combustion Elemental Analyzer (TCEA), Thermo Finnigan and continuous flow isotope ratio mass spectrometer (CF-IRMS), Thermo Electron, Delta V; Thorium; Thulium; Tin; Titanium; Tritium; Tritium, standard deviation; Tungsten; Type; Uranium; Vanadium; Water sample; WS; Ytterbium; Yttrium; Zinc; Zirconium; δ13C, dissolved inorganic carbon; δ13C, dissolved inorganic carbon, standard deviation; δ18O, sulfate; δ18O, sulfate, standard deviation; δ18O, water; δ18O, water, standard deviation; δ34S, sulfate; δ34S, sulfate, standard deviation; δ Deuterium, water; δ Deuterium, water, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 2307 data points
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  • 2
    Publication Date: 2024-06-12
    Description: The Učja aquifer, located in the E-W-orientated Učja Valley in NW Slovenia, presents a potential cross-border water resource. Due to the difficult access and steep mountain morphology and complex structural conditions, only basic geological research was done. Despite the fact that the groundwater is already used as a source of drinking water (public and local supply), comprehensive analysis of the aquifer has not yet been carried out. Water for geochemical and isotopic analysis was sampled at 13 locations in the Učja Valley; groundwater was sampled at 12 locations, and the surface water (Učja River) at one location. The sampling sites were located at different elevations and due to accessibility practically all of them were on the southern slopes of the valley. Water measurements, sampling, and analysis were carried out from December 2017 to March 2019. Physico-chemical parameters (pH, temperature, electrical conductivity, oxidation-reduction potential, and dissolved oxygen) were measured on a monthly basis and in-situ at sampling sites using a digital Multimeter 3430 (WTW GmbH, Weilheim, Germany). The missing measurements from some sampling sites are the result of the springs running dry at the time of sampling. Water samples for further geochemical (cations and anions) and isotopic analysis were collected in HDPE bottles for isotopic composition of oxygen (δ¹⁸O), hydrogen (δ²H), total alkalinity (TA), tritium activity (³H), and in Labco glass ampoules for isotopic composition of dissolved inorganic carbon (δ¹³CDIC). Water samples for cations and δ¹³CDIC were filtered using a 0.45 μm pore-sized membrane, and for some analyses water was also chemically treated and stored in a refrigerator until they were analysed. A total of 22 water samples were collected for geochemical analyses (cations, anions), 37 water samples (seasonally) for isotopic analyses δ¹⁸O, δ²H, total alkalinity and δ¹³CDIC, and 10 water samples for ³H. The database comprises information on sampling sites, sampling dates, and the results of field measurements and laboratory analyses.
    Keywords: Alkalinity, total; Alkalinity, total, standard deviation; ALTITUDE; Aluminium; Antimony; Arsenic; Barium; Beryllium; Bismuth; Bromide; Cadmium; Caesium; Calcium; Cerium; Chloride; Chromium; Cobalt; Comment; Conductivity, electrical; Continuous flow isotope ratio mass spectrometer (CF-IRMS), Sercon, Europa Scientific 20-20, ANCA-TG preparation module; Copper; cross-border karst aquifer; Date; Dual inlet-isotope-ratio mass spectrometer (DI-IRMS), Finnigan MAT GmbH, Finnigan MAT Delta plus; Dysprosium; Erbium; Europium; Event label; Fluoride; Gallium; Germanium; Gran titration; according to Gieskes, 1974; with pH electrode, Mettler Toledo, AG 8603; groundwater; Hafnium; Holmium; hydrogeochemistry; Indium; Inductively coupled plasma - mass spectrometry (ICP-MS), PerkinElmer, Thermo icapQ; Ion Chromatograph, Thermo Fisher Scientific, Dionex DX-120; Iron; isotopic composition; Lanthanum; LATITUDE; Lead; Liquid Scintillation Counting- Guard Compensation Technology (LSC-GCT), PerkinElmer, Quantulus GCT 6220 [Super Low Level LSC]; Lithium; LONGITUDE; Lutetium; Magnesium; Manganese; Mercury; Molybdenum; Multi-parameter meter, Xylem Analytics, Multi 3430; Neodymium; Nickel; Niobium; Nitrate; Nitrite; Oxidation reduction (RedOx) potential; Oxygen, dissolved; pH; Phosphate; Potassium; Praseodymium; Rubidium; Samarium; Sample code/label; Sample ID; Sample method; Scandium; Selenium; Silicon; Silver; Slovenia; Sodium; Strontium; Sulfate; Tantalum; Tellurium; Temperature, water; Terbium; Thallium; Thorium; Thulium; Tin; Titanium; Tritium; Tritium, standard deviation; Tungsten; Type; Ucja_UC1_1; Ucja_UC1_10; Ucja_UC1_11; Ucja_UC1_12; Ucja_UC1_2; Ucja_UC1_3; Ucja_UC1_4; Ucja_UC1_5; Ucja_UC1_6; Ucja_UC1_7; Ucja_UC1_8; Ucja_UC1_9; Ucja_UC10_1; Ucja_UC10_2; Ucja_UC10_3; Ucja_UC10_4; Ucja_UC10_5; Ucja_UC11_10; Ucja_UC11_11; Ucja_UC11_12; Ucja_UC11_2; Ucja_UC11_3; Ucja_UC11_4; Ucja_UC11_5; Ucja_UC11_6; Ucja_UC12_10; Ucja_UC12_11; Ucja_UC12_12; Ucja_UC12_2; Ucja_UC12_3; Ucja_UC12_4; Ucja_UC12_5; Ucja_UC12_6; Ucja_UC12_9; Ucja_UC13_6; Ucja_UC2_1; Ucja_UC2_10; Ucja_UC2_11; Ucja_UC2_12; Ucja_UC2_2; Ucja_UC2_3; Ucja_UC2_4; Ucja_UC2_5; Ucja_UC2_6; Ucja_UC3_1; Ucja_UC3_10; Ucja_UC3_11; Ucja_UC3_12; Ucja_UC3_2; Ucja_UC3_3; Ucja_UC3_4; Ucja_UC3_5; Ucja_UC3_6; Ucja_UC3_7; Ucja_UC3_8; Ucja_UC3_9; Ucja_UC4_1; Ucja_UC4_10; Ucja_UC4_11; Ucja_UC4_12; Ucja_UC4_2; Ucja_UC4_3; Ucja_UC4_4; Ucja_UC4_5; Ucja_UC4_6; Ucja_UC4_7; Ucja_UC4_8; Ucja_UC4_9; Ucja_UC5_1; Ucja_UC5_10; Ucja_UC5_11; Ucja_UC5_12; Ucja_UC5_2; Ucja_UC5_3; Ucja_UC5_4; Ucja_UC5_5; Ucja_UC5_6; Ucja_UC5_7; Ucja_UC5_8; Ucja_UC5_9; Ucja_UC6_1; Ucja_UC6_10; Ucja_UC6_11; Ucja_UC6_12; Ucja_UC6_2; Ucja_UC6_3; Ucja_UC6_4; Ucja_UC6_5; Ucja_UC6_6; Ucja_UC6_7; Ucja_UC6_8; Ucja_UC6_9; Ucja_UC7_1; Ucja_UC7_10; Ucja_UC7_11; Ucja_UC7_12; Ucja_UC7_2; Ucja_UC7_3; Ucja_UC7_4; Ucja_UC7_5; Ucja_UC7_6; Ucja_UC7_7; Ucja_UC7_8; Ucja_UC7_9; Ucja_UC8_1; Ucja_UC8_10; Ucja_UC8_11; Ucja_UC8_12; Ucja_UC8_2; Ucja_UC8_3; Ucja_UC8_4; Ucja_UC8_5; Ucja_UC8_6; Ucja_UC8_7; Ucja_UC8_8; Ucja_UC8_9; Ucja_UC9_1; Ucja_UC9_10; Ucja_UC9_11; Ucja_UC9_12; Ucja_UC9_2; Ucja_UC9_3; Ucja_UC9_4; Ucja_UC9_5; Ucja_UC9_6; Ucja_UC9_7; Ucja_UC9_8; Ucja_UC9_9; Uranium; Vanadium; Water sample; WS; Ytterbium; Yttrium; Zinc; Zirconium; δ13C, dissolved inorganic carbon; δ13C, dissolved inorganic carbon, standard deviation; δ18O, water; δ18O, water, standard deviation; δ Deuterium, water; δ Deuterium, water, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 3448 data points
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  • 3
    Publication Date: 2008-11-07
    Print ISSN: 0172-9179
    Electronic ISSN: 1612-4820
    Topics: Geography , Geosciences
    Published by Springer
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  • 4
    Publication Date: 2016-07-13
    Print ISSN: 0172-9179
    Electronic ISSN: 1612-4820
    Topics: Geography , Geosciences
    Published by Springer
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  • 5
  • 6
    Publication Date: 2019-12-09
    Print ISSN: 0583-6050
    Electronic ISSN: 1580-2612
    Topics: Geosciences
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  • 7
    Publication Date: 2015-12-30
    Print ISSN: 0583-6050
    Electronic ISSN: 1580-2612
    Topics: Geosciences
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  • 8
    Publication Date: 2016-12-09
    Print ISSN: 0037-0746
    Electronic ISSN: 1365-3091
    Topics: Geosciences
    Published by Wiley
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  • 9
    Publication Date: 2019-07-16
    Description: Drenov Grič black limestone is considered to be one of the most beautiful Slovenian natural stones due to its black colour interwoven with white veins. Over the centuries, it has been extracted from two major quarries located west of Ljubljana. One of these quarries has been declared a valuable natural feature of national importance and is protected as a natural monument. This well-stratified, Triassic (Carnian) micritic limestone occurs in 10–80 cm thick beds with thin marl interlayers. The limestone occasionally contains abundant fossil bivalves, gastropods and ostracods. It is relatively rich in carbonaceous and bituminous organic matter, which is responsible for the black colour of the stone. The stone has been widely used in Slovenian monuments. Many indoor and outdoor architectural elements have been constructed using this limestone, particularly during the Baroque period, which was known for its extensive use of black limestones in other European countries as well. The most significant use of this limestone has been recorded in sculpted portals and altars. Some important buildings, which were decorated utilizing this stone, have been declared cultural monuments of local or national importance. Use of this limestone was also documented in other European countries (Italy, Austria, Serbia) and worldwide (USA). When exposed to climatic influences, chromatic and salt weathering are recognized as the main deterioration phenomena for this limestone when used in monuments.
    Print ISSN: 0305-8719
    Electronic ISSN: 2041-4927
    Topics: Geosciences
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  • 10
    Publication Date: 2018-12-01
    Description: The Miocene evolution of the area transitional from the Eastern Alps to the Pannonian Basin System was studied through the paleogeographic evolution of the Slovenj Gradec Basin in northern Slovenia. It is based on mapping, section logging, nannoplankton biostratigraphy, and petrography. The results are correlated with the lithological column of the borehole MD-1/05. The evolution of the basin is connected with the development of the Pannonian Basin System, and the global 3rd order cycles, which influenced the connection with the Mediterranean Sea. Sedimentation started in the Karpatian in a fluvial to lacustrine environment and terminated at the end of the Early Badenian. During this period, three transgression–regression cycles were recorded. The first transgression occurred in the Karpatian and corresponds to the TB 2.2. cycle. The sediments reflect proximity of the hinterland. After a short break in sedimentation, the Early Badenian deposition followed. It marks the second transgression into the SGB, the first Badenian, correlated with the TB 2.3 cycle. There are signs of a transitional environment, which evolved to marine in advanced stages. At the high-stand system tract, the sea flooded the entire Slovenj Gradec Basin. Subsequent reduced quantity and diversity of the microfossils marks the onset of the second regression stage. It is followed by the third transgression, the second in the Badenian, correlated with the TB 2.4 cycle. The late Early Badenian deposition continued in the lower-energy, though occasionally still turbulent environment. Silty sediments with upward increasing content of organic matter indicate shallowing of the basin, until its final diminishing. Layers of fresh-water coal already bear witness to the existence of restricted swamps. After the Early Badenian, the area of the Slovenj Gradec Basin became dry land, exposed to erosion.
    Print ISSN: 1335-0552
    Electronic ISSN: 1336-8052
    Topics: Geosciences
    Published by De Gruyter
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