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Dive into the research topics where B. Uliasz-Misiak is active.

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Featured researches published by B. Uliasz-Misiak.


Applied Energy | 2003

Renewable energy sources in Guadeloupe

Radosław Tarkowski; B. Uliasz-Misiak

The following types of renewable energy are utilized in Guadeloupe: solar energy, wind energy, water energy, biogas, combined energy sources as well as geothermal energy. Attention is drawn to a specific geographic setting as well as the social and economic situation which influence the demand for energy in this department of France. Steps taken by the department administration to increase the interest of local communities in the use of renewable energy sources are presented. Current and future trends in the production of heat and electric power are discussed and special attention is paid to the role of geothermal energy.


Applied Energy | 2003

Geothermal energy of the Mesozoic Basin in the Carpathian Foredeep, Kraków Region, Poland

A.P Barbacki; B. Uliasz-Misiak

Although the most favourable conditions for the use of geothermal energy are found in the Tatra region, in addition, the Foreland of the Carpathians in Poland is rich in low-temperature geothermal waters, both in Cenomanian sandstones and Middle Jurassic sandstones. The geothermal activity is manifested by thermal waters in boreholes situated between the towns of Wloszczowa, Myslenice and Tarnow. Here the Mesozoic waters occur 200 to 2000 m below the surface and their temperatures vary between 20 and 70 °C. The continuous artesian outflow of geothermal waters was observed in many wells during long-term tests. The maximum artesian outflow of fresh water was observed in the zone north of Cracow, i.e. 100 m3/h with a temperature of about 20 °C. The results of the analyses which were carried out on the Mesozoic formation confirmed considerable zonation and the existence of local constraints on the reservoir parameters which result from the characteristics of the deposited environment. A distinct relationship was also noted between the total thickness and other reservoir parameters. Moreover, a strong correlation was observed between the degree of water mineralization and the distance from the infiltration zone or depth at which the waters occurred. In the western zones, located close to the recharge areas, waters are fresh or nearly fresh and their temperatures are influenced by surface waters. Favourable conditions for the financial investment in geothermal energy in the Mesozoic Basin of this region are associated with the low mineralization (allowing for exploitation with a single well) and shallowness of the aquifers (i.e. low drilling costs). The paper presents results of analyses of the temperature characteristics of the Mesozoic formation, yields from existing wells and the energy potential of geothermal waters from the point of view of future geothermal projects.


Archive | 2009

Indicative Microorganisms as a Tool for Testing the Underground Storage of Carbon Dioxide

Radosław Tarkowski; Wojciech Królik; B. Uliasz-Misiak; Wieslaw Barabasz


Polityka Energetyczna | 2004

Instalacje podziemnego magazynowania dwutlenku węgla

Radosław Tarkowski; B. Uliasz-Misiak


Przegląd Geologiczny | 2003

Podziemne magazynowanie dwutlenku węgla

Radosław Tarkowski; B. Uliasz-Misiak


Przegląd Górniczy | 2006

Geologiczna sekwestracja CO2 - mit czy rzeczywistość

Radosław Tarkowski; B. Uliasz-Misiak; A. Uliasz-Bocheńczyk


Archive | 2006

Deep geological structures as sites to CO2 storage in Poland

Radosław Tarkowski; B. Uliasz-Misiak; Wojciech Królik


Wiertnictwo, Nafta, Gaz | 2005

Metody monitoringu podziemnego składowania CO2

Radosław Tarkowski; B. Uliasz-Misiak; E. Szarawarska


Wiertnictwo, Nafta, Gaz | 2005

Źródła dwutlenku węgla w Polsce dla zaawansowanych technik wydobycia ropy naftowej

Radosław Tarkowski; B. Uliasz-Misiak


Polityka Energetyczna | 2004

Emisja CO2 ze spalania paliw oraz procesów przemysłowych w Polsce

Radosław Tarkowski; B. Uliasz-Misiak

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Wojciech Królik

Polish Academy of Sciences

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A.P Barbacki

Polish Academy of Sciences

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