ANALYSIS OF HYDROGEOLOGICAL CONDITIONS SUPPORTED BY A MATHEMATICAL MODELLING AS THE BASIC STAGE OF INVESTMENT PROJECTS IN THE FIELD OF GEOTHERMY

Journal Title: Biuletyn Państwowego Instytutu Geologicznego - Year 2018, Vol 471, Issue 471

Abstract

Geothermal groundwaters are deposits that must be categorised as a mining property. Their exploitation is possible with a mining concession and permission of use. Geothermal groundwaters in Poland are used in heating, balneotherapy and recreation purposes. Over the last years, investigations have been carried out to intensify the use of geothermal groundwaters. They can be used as new geothermal products, for example as a mineralised concentrate. Investment projects related to geothermal groundwaters should be prepared with care about safe and sustained exploitation in long-term perspective. Using of geothermal groundwaters is determined by technical and economical conditions. However, successful exploitation depends also on natural conditions e.g. water temperature, physical features, chemical composition and durability of parameters, and renewability of resources. Recognition of these elements give a basic information that nowadays can be integrated as mathematical models. The models are created to analyse and simulate the conditions of geothermal systems. It often happens before starting project operating activities. The paper presents examples of projects carried out over the recent years. They have been associated with the using and management of geothermal groundwaters and the key role has been played by mathematical modelling in the field of geothermy and hydrogeology.<br/><br/>

Authors and Affiliations

Barbara TOMASZEWSKA, Marta DENDYS, Leszek PAJĄK

Keywords

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  • EP ID EP385321
  • DOI 10.5604/01.3001.0012.4931
  • Views 52
  • Downloads 0

How To Cite

Barbara TOMASZEWSKA, Marta DENDYS, Leszek PAJĄK (2018). ANALYSIS OF HYDROGEOLOGICAL CONDITIONS SUPPORTED BY A MATHEMATICAL MODELLING AS THE BASIC STAGE OF INVESTMENT PROJECTS IN THE FIELD OF GEOTHERMY. Biuletyn Państwowego Instytutu Geologicznego, 471(471), 179-184. https://europub.co.uk/articles/-A-385321