
Nina RmanGeološki zavod Slovenije
Nina Rman
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Citations since 2017
Publications
Publications (57)
The distribution of the high concentrations of arsenic (As) and fluoride (F-) in groundwater on a Pan-European scale could be explained by the geological European context (lithology and structural faults). To test this hypothesis, seventeen countries and eighteen geological survey organizations (GSOs) have participated in the dataset. The methodolo...
This study discusses 1) the national legislative frameworks, terminologies, and criteria for the recognition of natural mineral waters and thermal waters in selected European countries (Austria, Bosnia and Herzegovina, Denmark, France, Hungary, Iceland, Italy, Lithuania, Poland, Portugal, Romania, Serbia, Slovenia, and Spain), and 2) it provides a...
Bottled natural mineral waters from an andesitic aquifer in Slovenia are enriched in magnesium (1.1 g/l), sulphate (2.2 g/l) and dissolved inorganic carbon (204 g/l). We analysed major ions, trace elements, tritium activity, ¹⁴ C, δ ¹⁸ O H2O , δ ² H H2O, δ ¹³ C DIC , gas composition and noble gases in six wells. In addition, ⁸⁷ Sr/ /86 Sr, δ ³⁴ S S...
It is a notice on 6th European geothermal congress in 2019, its main topics, field trips and conclusions
In northeastern Slovenia, the most geothermally utilized region and belonging to the geothermally anomalous Pannonian Basin, no significant progress with new deep drillings was achieved in geothermal development for direct heat use of thermal water during the last five years. The geothermal energy use in Slovenia stagnates. It does not develop. Imp...
A comparative analysis of step-drawdown tests was performed in order to estimate the well performance in
Slovenian thermal and mineral water wells. Tests were performed in 30 wells, each having its own maximum
production rate determined in the concession decrees. The main focus of well performance analysis, using
graphical analysis of the Jacob app...
The Alps represent an area where many deep groundwater circulations occur as thermal springs. In the Bled case study, the thermal water temperature, at it is discharged to the surface, is between 19–23 °C. In order to determine the extent (e.g., geometry) and the origin of the pronounced deep circulation system in the Bled area, chemical and isotop...
Data on thermal water sources with outflow temperature of 30 °C and above were analyzed from the N-ern parts of Bosnia and Herzegovina, Serbia and Croatia, S-ern parts of Hungary, W-ern parts of Romania, and NE-ern parts of Slovenia, altogether from an area of 99,347 km2. The overview identified 771 geothermal sources; only 7 were thermal springs....
Teaching of geological contents in elementary school and gymnasiums has not yet been systematically
addressed. Under the auspices of Slovenian Geological Society, members of the Task Group for the Popularization
of Geology, have set themselves the goal of gaining insight into the teaching of geological contents in elementary
schools and gymnasiums....
Study Region: Pannonian Basin, Central and Eastern Europe. Study focus: This study, carried out by the geological surveys of Hungary, Slovenia, Austria and Slovakia, combines a joint characterization of a transboundary thermal groundwater system based on harmonised geological and hydrogeological data, with hydrodynamic modelling, delivering recomme...
Natural CO
2 springs and groundwater rich in free gas in Slovenia occur mainly in the Slovenske gorice hills.
Within the frame of fildwork performed in 2014–2015 we investigated 11 springs: Ihovska slatina, Ivanjševska
slatina, Lokavska slatina, Polička slatina, Radvenska slatina, Mofette Rihtarovci, mofettes Stavešinske Slepice,
and Strmec, Ujters...
Executive Summary
Based on the results of the Geothermal ERA-NET work package (WP) 2 „Information exchange on national
incentives and status of geothermal energy“, and WP4 “Development of joint activities”, the topical field of
operational issues of geothermal energy installations was identified as one of the main barriers for the
development of ge...
Geothermal energy use in Slovenia in 2016.
Geothermal energy use in Slovenia has been followed
on regular basis since 1994. Only a small progress was
achieved in geothermal development during the last
three years, in its northeastern part, belonging to the
Pannonian Basin geothermal region. New geothermal
borehole was drilled there with good characteristics
and depth of 1.2 km. Greenhouse a...
Geothermal energy use in Slovenia in 2016.
The article presents the latest status of geothermal energy use worldwide and the comparison with the previous
period, both in electricity generation as well as in the various categories of direct use. Electricity production takes
place in 26 countries and has at the end of 2014 reached 73,700 GWh from geothermal power plants with nearly
12.8 GW of...
The aim of the study was to develop and test an optimal and cost-effective regional quality monitoring system in depleted transboundary low-temperature Neogene geothermal aquifers in the west Pannonian basin. Potential tracers for identification of seasonal and long-term quality changes of the Pleistocene thermal waters were investigated at four mu...
In the paper, a new transboundary Upper Pannonian thermal groundwater body was identified which extends over 22,128 km2 in Austria, Hungary, Slovakia, Slovenia and Croatia. The presented joint numerical simulation of freshwater and geothermal aquifers in the Pannonian sedimentary basin and weathered basement rocks provided new insights into the reg...
This paper investigates depletion rates and available thermal water resources of the transboundary Upper Pannonian loose sandstone geothermal aquifer of the Mura Formation in the Mura-Zala sedimentary basin in north-eastern Slovenia, and outlines a regional reinjection strategy to mitigate depletion. The research monitoring network of 12 geothermal...
The aim of the study was to develop and test an optimal and cost-effective regional quality monitoring system in depleted transboundary low-temperature Neogene geothermal aquifers in the west Pannonian basin. Potential tracers for identification of seasonal and long-term quality changes of the Pleistocene thermal waters were investigated at four mu...
The Mura-Zala sedimentary Basin is a Neogene basin with many competing geopotentials, spanning parts
of Slovenia, Austria, Croatia and Hungary. Here we present the 3D regional geological model of the Slovenian
part of the Mura-Zala Basin, which was developed to integrate the latest information on the geological
structure of NE Slovenia and to publi...
We present new isotope (C, He, Ne, Ar, partly N) and compositional data from the free gas phase of fourteen degassing sites in the westernmost part of the Pannonian Basin near the Austria/Slovenia borderline. Based on these data, the origin of the gases and the degree of modification of the gas signatures due to interaction processes during migrati...
The already exploited geothermal resources in the Mura-Zala basin are planned to be further developed.
In this study I investigated thermal water abstraction and its impact on both the fissured basement
aquifers and the intergranular Neogene siliciclastic aquifers. Total abstraction of thermal water in northeast
Slovenia summed to 3.1 million m3 in...
This study gives a brief and general overview of the hydrogeology and hydrogeochemistry of the transboundary geothermal resources in the western part of the Pannonian Basin, carried out within the framework of a joint Hungarian, Slovenian, Slovakian and Austrian project (TRANSENERGY). Chemical and isotope data were used to describe the different fl...
Forty-five adults, which do professionally not deal with geology or groundwaters, filled a voluntary questionnaire
on groundwater dynamics in Slovenia. The survey pointed out that about a fifth to a quarter of them has a weak
knowledge on this topic. Groundwater occurrence, production and pollution are quite well known, excluding a
widely spread op...
Geothermal energy use in Slovenia has been followed on regular basis since 1995. In the last period 2007 -2012 there is no growth but slow and constant increment of the energy contribution from direct use of thermal water. Three district heating systems are operating; the additional one is under construction. A significant potential of existing the...
Thermal water in the Slovenian part of the Mura-Zala
basin, which appertains to the SW part of the
Pannonian basin, is produced from low enthalpy
geothermal system set in the Neogene sediments as
well as from basement aquifers in the Pre-Neogene
metamorphic and carbonate rocks. The water
discharges from 26 geothermal wells managed by 14
users. Thei...
Historical utilization of regional and transboundary
geothermal resources was identified between Austria,
Hungary, Slovakia and Slovenia. Its status was
determined for the period 2010-2011 and based on a
unified methodological approach and field inspections.
The assembled data were verified and harmonized in a
database with three levels applied: or...
Managing transboundary groundwater resources requires accurate and detailed knowledge of aquifers and groundwater bodies. The Pannonian Basin is the largest intracontinental basin in Europe with a continuous succession of more than 7 km of Miocene to Quaternary sediments and with an average geothermal gradient of about 5 °C/100 m. Geographically th...
Large transboundary Upper Miocene geothermal sandy aquifers which are widely utilized by both countries for balneological and direct heat purposes exist in the Slovenian-Hungarian border region. In NE Slovenia the total direct heat use was 382 TJ in 2010, while in SW Hungary it was 648 TJ, including utilization from basement reservoirs. The total i...
Many thermal water users are known in the transboundary area between Austria, Hungary, Slovenia and Slovakia, but no detailed estimation on their actual use has been known for a long time. The conducted research enabled collection of the harmonized transb
Demand for thermal water in the Mura-Zala basin, situated between Slovenia, Austria, Hungary and Croatia, is constantly increasing,
with the sandy geothermal aquifer within the Neogene Mura formation being the most exploited. During the water concession
granting process various problems were identified, together with the need for elaboration of the...
To be able to phrase recommendations for the joint, harmonized thermal groundwater management in the Mura–Zala Basin, which was the ultimate goal of the T-JAM project, it was important to get a coherent picture about the current utilization scehems. This was done by a questionanire survey based on the tempates, elaborated earlier by the Internation...
Tourist society for the care and improvement of a district Ponikva opened two tourist educational trails in2010: the Trail of Ponikva's Three Notable Inhabitants and the Karstic Water Educational Trail of Stanko Buser.The first describes mainly cultural-historical remarkableness of the area, but the spot at Šamec sand pit presentsalso Ponikva’...
Systematical teaching of geology is (yet) not established in primary and secondary school in Slovenia. In primaryschool, geological topics are divided among numerous subjects and levels therefore they receive more attention onlyif alternative courses or geological circles are realized. With help of the Geological Survey of Slovenia we have beensucc...
Direct use of geothermal waters continues to be the only
type of use from geothermal reservoir sources in Slovenia,
at 29 localities at present. A small progress was achieved in
geothermal development during the last five years with four
new users appearing in the north-eastern part of Slovenia,
belonging to the Pannonian Basin geothermal region. T...
High mountainous lake Jezero na Planini pri Jezeru is located in the
Triglav National Park at the Julian Alps in Slovenia. It fills a
depression covered with Pleistocene fine-grained sediments and glacial
till on intensively karstified plateau. In the past many investigations
were performed on the lake and its surrounding without knowledge about
hy...
Geothermal energy is an important alternative and local heat source in Slovenia. As long as natural, technological and legislative conditions and boundaries are considered, geothermal heat pumps represent ecologically acceptable heat source at a reasonable price. Thermal water direct use, especially in connection with tourism, district and greenhou...
The article describes the results of detailed geological mapping of the wider environs of Planina pri Jezeru north of Bohinj. In the literature the Upper Triassic massive and bedded limestone, Jurassic limestone, Cretaceousclastic rocks and Pleistocene sediments have been reported in this area up to now. The article supplements existing lithostrati...
Projects
Projects (2)
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The main aim of WATSON is to collect, integrate, and synthesize current interdisciplinary scientific knowledge on the partitioning and mixing of water in the critical zone taking advantage of the unique tracing capability of water isotopes. These efforts will allow going beyond the current fragmented knowledge providing a novel conceptual framework on the interactions between groundwater recharge, soil water storage, and vegetation transpiration useful for water resources management across a variety of climatic settings.
Context:
Understanding water exchange within the critical zone, i.e.the dynamic skin of the Earth that extends from vegetation canopy to groundwater, is vital for addressing key environmental problems linked to the sustainable management of water resources.
Approach:
The Action activities are based on a network of early career and senior scientists from different complementary disciplines who are experts in the use of water isotopes, and stakeholders from governmental agencies and private companies from 19 COST countries and one Near Neighbour Country. Meetings and training events will involve scientists and water managers, facilitating communication between academia and stakeholders, promoting the transfer of the latest scientific findings, and helping to identify research gaps and management priorities.
Deliverables:
The ultimate goal of the network is to build capacity in the use of robust isotope approaches for water resource management. The deliverables include practical tools, such as maps of groundwater recharge and water sources used by vegetation in different European regions that will enable the translation of scientific cutting-edge knowledge into tangible recommendations to support European agencies responsible for water management in agro-forest systems.