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EN
The article presents the results of laboratory tests of thermal conductivity of mineral soils. Measurements were performed on the basis of the previously developed methodology. Knowledge of values of the thermal conductivity coefficient of soil is essential for the design of installations that use thermal properties of subsoil for energetic purposes. The results of the measurements are stored in the rock and soil thermal properties database, in which additional physical parameters of soils are collected as well. Based on the information from the database, the authors presented the relationship between soil moisture (non-cohesive soils), the liquidity index (cohesive soils), and their thermal conductivity.
EN
In this article, we summarize the most important engineering geological research over the past 100 years in the Polish Geological Institute and analyze its present and future development.
EN
Fulfilling the binding national, EU and other international regulations and requirements on climate and energy implies significant growth of renewables share in the total mix of energy production in Poland. Low-temperature geothermal energy extracted with the use of the ground source heat pumps (GSHP) is an efficient and reliable source for space heating, cooling and seasonal thermal energy storage and recovery, thus it contributes to reduction of low emissions and improvement of air quality. GSHP effectiveness is to a high degree determined by local geological and hydrogeological settings, therefore identification of natural properties of the subsurface is crucial for appropriate design and subsequent operation of the GSHP installations. The thermal conductivity λ of rocks and soils, a key geothermal parameter, depends on such features as the mineral composition of rocks and soils, their texture and water content. Relevant geological data is retrieved from thematic databases, atlases and serial maps and can be gathered in a unitary database with a uniform structure to enable spatial analysis with the use of GIS techniques. Reclassification of lithological properties into geothermal parameters and subsequent calculations of λ values (W/m·K) of rock and soil types can be made using a specific algorithm. The results of these calculations enables computation of four spatial layers of average geothermal conductivity coefficient λ (W/m·K), respectively for the depth intervals of 0-40, 41-70, 71-100 and 101-130 metres b.g.l.
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