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Layer: 300 m geoenergiapotentiaali (1)

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Description: Tässä kuvauksessa ja esitettävissä kartoissa käytetään nimitystä geoenergia kuvaamaan maankamaran ylimmästä 300 metristä hyödynnettävissä olevaa lämpöenergiaa ja lämmitystehoa. Kansainvälisessä tieteellisessä kirjallisuudessa käytetään geoenergian synonyymeinä termejä shallow geothermal energy ja low enthalpy geothermal energy. Geoenergia erotetaan tässä yhteydessä syvästä geotermisestä energiasta (engl. deep geothermal energy), joka kuvaa syvältä kallioperästä hyödynnettävissä olevaa korkean lämpötilan energiaa. 300 m geoenergiapotentiaali kuvaa maankamaran ylimmältä 300 metriltä saatavaa, lämpöarvoltaan matalaa lämpöenergiapotentiaalia, joka on hyödynnettävissä rakennusten lämmittämiseen ja/tai viilentämiseen kalliosta poratusta energiakaivosta. Maankamaralla tarkoitetaan sekä kiteistä kallioperää että sitä peittäviä irtaimia maalajeja. Geoenergiapotentiaali arvioitiin laskennallisesti simuloimalla lämmönsiirtymistä maankamarassa aksiaalisymmetrisen energiakaivomallin avulla. Energiakaivon aktiivinen kokonaissyvyys vakioitiin 300 metriin sisältäen kallioperän ja sitä mahdollisesti peittävät maalajit. Geoenergiapotentiaalin arvioinnissa on hyödynnetty seuraavia digitaalisia aineistoja: - Kallioperä 1:1 000 000 - Maaperä 1:200 000 (maalajit) - Maapeitepaksuus 1:1 000 000 - GTK:n tekemiä lämpötilaluotauksia - Ilmatieteen laitoksen ilman vuotuinen keskilämpötila (Pirinen et al., 2012) - Suomen kallioperän tiheys (Pirttijärvi et al., 2013) - Suomen geokemiallinen atlas (Gustavsson et al. 1987) Aineisto Suomen 300 m geoenergiapotentiaalista koostuu kahdesta rasterimuotoisesta kartasta, jotka sisältävät laskennalliset arviot (1) varastoituneen lämpöenergian määrästä [GWh] ja (2) jatkuvasti uusiutuvasta lämmöntuottotehosta [W], kun kyseessä on 300 m syvä energiakaivo. Ne osoittavat geoenergiapotentiaalin aluekohtaisen saatavuuden ja vaihtelun. Arvioilla pyritään antamaan lisätietoa Suomen geoenergian hyödyntämisen potentiaalista Työ- ja elinkeinoministeriön (TEM) laatiman kansallisen ilmasto- ja energiastrategian tavoitteisiin sekä vastaamaan EU:n energia- ja ilmastotavoitteisiin. Kartat on tuotettu geoenergiapotentiaalin yleistarkasteluun mittakaavassa 1:1 000 000. Ne eivät sovellu kiinteistökohtaiseen suunnitteluun tai mitoitukseen, eivätkä suurimittakaavaiseen (yli 1:500 000) tarkasteluun. Karttojen solukoko on yksi neliökilometri. / In this metadata document and in the maps, the term geoenergy is used to describe the thermal energy and renewable heating power that can be extracted from the uppermost 300 meters of the ground. In scientific literature, the terms shallow geothermal energy and low enthalpy geothermal energy are used as synonyms for geoenergy. In contrast to geoenergy, geothermal energy refers to high temperature thermal energy that is extracted from depths below 300 meters and can be used for heating and electrical power generation. The 300 m geoenergy potential dataset describes the low enthalpy geothermal potential that can be extracted from the uppermost 300 metres of the ground and be used for space heating and/or cooling. The term ground is used to refer to both the crystalline bedrock and to the quaternary sediments that overlay it. The geoenergy potential was estimated computationally by simulating heat transfer in the ground using an axisymmetric borehole model. The active depth of the borehole was fixed to 300 metres and it includes the effects of both the bedrock and the quaternary deposits that possibly overlay the bedrock. The following digital datasets were utilized in the computations: - Bedrock of Finland 1:1 000 000 - Superficial deposits of Finland 1:200 000 (sediment polygons) - Superficial deposits thickness 1:1 000 000 - Borehole temperature logs by GTK - Mean annual air temperature map by the Finnish Meteorological Institute (Pirinen et al., 2012) - Density map of Finland by Pirttijärvi et al. (2013) - Geochemical Atlas of Finland by Gustavsson et al. (1987) The 300 m geoenergy potential dataset comprises two raster maps that provide computational estimates of (1) the stored thermal energy, and (2) the renewable heating power extractable from a 300 m deep borehole. The maps show the areal availability and variation of the geoenergy potential. The maps are intended to provide further information concerning the availability of geoenergy in order to facilitate the national climate and energy strategy of the Finnish Ministry of Economic Affairs and Employment (TEM) and the climate and energy policy of the European Union (EU). The maps were produced to provide a general overview of the geoenergy potential at the scale of 1:1 000 000. They are not suitable for the sizing of ground source energy systems at the level of individual properties nor for large scale investigations (scales larger than 1:500 000). The cell size of the raster maps is 1 km x 1 km.

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Description: Tässä kuvauksessa ja esitettävissä kartoissa käytetään nimitystä geoenergia kuvaamaan maankamaran ylimmästä 300 metristä hyödynnettävissä olevaa lämpöenergiaa ja lämmitystehoa. Kansainvälisessä tieteellisessä kirjallisuudessa käytetään geoenergian synonyymeinä termejä shallow geothermal energy ja low enthalpy geothermal energy. Geoenergia erotetaan tässä yhteydessä syvästä geotermisestä energiasta (engl. deep geothermal energy), joka kuvaa syvältä kallioperästä hyödynnettävissä olevaa korkean lämpötilan energiaa. 300 m geoenergiapotentiaali kuvaa maankamaran ylimmältä 300 metriltä saatavaa, lämpöarvoltaan matalaa lämpöenergiapotentiaalia, joka on hyödynnettävissä rakennusten lämmittämiseen ja/tai viilentämiseen kalliosta poratusta energiakaivosta. Maankamaralla tarkoitetaan sekä kiteistä kallioperää että sitä peittäviä irtaimia maalajeja. Geoenergiapotentiaali arvioitiin laskennallisesti simuloimalla lämmönsiirtymistä maankamarassa aksiaalisymmetrisen energiakaivomallin avulla. Energiakaivon aktiivinen kokonaissyvyys vakioitiin 300 metriin sisältäen kallioperän ja sitä mahdollisesti peittävät maalajit. Geoenergiapotentiaalin arvioinnissa on hyödynnetty seuraavia digitaalisia aineistoja: - Kallioperä 1:1 000 000 - Maaperä 1:200 000 (maalajit) - Maapeitepaksuus 1:1 000 000 - GTK:n tekemiä lämpötilaluotauksia - Ilmatieteen laitoksen ilman vuotuinen keskilämpötila (Pirinen et al., 2012) - Suomen kallioperän tiheys (Pirttijärvi et al., 2013) - Suomen geokemiallinen atlas (Gustavsson et al. 1987) Aineisto Suomen 300 m geoenergiapotentiaalista koostuu kahdesta rasterimuotoisesta kartasta, jotka sisältävät laskennalliset arviot (1) varastoituneen lämpöenergian määrästä [GWh] ja (2) jatkuvasti uusiutuvasta lämmöntuottotehosta [W], kun kyseessä on 300 m syvä energiakaivo. Ne osoittavat geoenergiapotentiaalin aluekohtaisen saatavuuden ja vaihtelun. Arvioilla pyritään antamaan lisätietoa Suomen geoenergian hyödyntämisen potentiaalista Työ- ja elinkeinoministeriön (TEM) laatiman kansallisen ilmasto- ja energiastrategian tavoitteisiin sekä vastaamaan EU:n energia- ja ilmastotavoitteisiin. Kartat on tuotettu geoenergiapotentiaalin yleistarkasteluun mittakaavassa 1:1 000 000. Ne eivät sovellu kiinteistökohtaiseen suunnitteluun tai mitoitukseen, eivätkä suurimittakaavaiseen (yli 1:500 000) tarkasteluun. Karttojen solukoko on yksi neliökilometri. / In this metadata document and in the maps, the term geoenergy is used to describe the thermal energy and renewable heating power that can be extracted from the uppermost 300 meters of the ground. In scientific literature, the terms shallow geothermal energy and low enthalpy geothermal energy are used as synonyms for geoenergy. In contrast to geoenergy, geothermal energy refers to high temperature thermal energy that is extracted from depths below 300 meters and can be used for heating and electrical power generation. The 300 m geoenergy potential dataset describes the low enthalpy geothermal potential that can be extracted from the uppermost 300 metres of the ground and be used for space heating and/or cooling. The term ground is used to refer to both the crystalline bedrock and to the quaternary sediments that overlay it. The geoenergy potential was estimated computationally by simulating heat transfer in the ground using an axisymmetric borehole model. The active depth of the borehole was fixed to 300 metres and it includes the effects of both the bedrock and the quaternary deposits that possibly overlay the bedrock. The following digital datasets were utilized in the computations: - Bedrock of Finland 1:1 000 000 - Superficial deposits of Finland 1:200 000 (sediment polygons) - Superficial deposits thickness 1:1 000 000 - Borehole temperature logs by GTK - Mean annual air temperature map by the Finnish Meteorological Institute (Pirinen et al., 2012) - Density map of Finland by Pirttijärvi et al. (2013) - Geochemical Atlas of Finland by Gustavsson et al. (1987) The 300 m geoenergy potential dataset comprises two raster maps that provide computational estimates of (1) the stored thermal energy, and (2) the renewable heating power extractable from a 300 m deep borehole. The maps show the areal availability and variation of the geoenergy potential. The maps are intended to provide further information concerning the availability of geoenergy in order to facilitate the national climate and energy strategy of the Finnish Ministry of Economic Affairs and Employment (TEM) and the climate and energy policy of the European Union (EU). The maps were produced to provide a general overview of the geoenergy potential at the scale of 1:1 000 000. They are not suitable for the sizing of ground source energy systems at the level of individual properties nor for large scale investigations (scales larger than 1:500 000). The cell size of the raster maps is 1 km x 1 km.

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