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| Content Provider | Springer Nature Link |
|---|---|
| Author | Ferguson, Grant Grasby, Stephen E. |
| Copyright Year | 2013 |
| Abstract | The Winnipeg and Deadwood formations form deep clastic reservoirs in Saskatchewan, Canada, with temperatures exceeding 40 °C over most of southern Saskatchewan and reaching 100 °C in southwestern Saskatchewan. At these temperatures, the formations have geothermal potential for development of direct use and electricity generation systems. Numerous disposal wells operating at rates of 30 L/s or more are currently installed in these formations, suggesting that electricity could be generated at rates exceeding 2 megawatts of electrical output (MW$_{e}$) from individual wells. These basal clastic units, thus, could provide significant energy supply over a broad region of Saskatchewan.Les formations Winnipeg et Deadwood constituent des réservoirs détritiques profonds dans le Saskatchewan au Canada, avec des températures dépassant les 40 °C sur la plus grande partie du Sud du Saskatchewan et atteignant 100 °C dans le Sud-Ouest du Saskatchewan. A ces températures les formations ont un potentiel géothermique pour le développement d’usage direct et de systèmes de générateurs d’électricité. De nombreux forages exploités à des débits de 30 L/s ou plus sont à présent creusés dans ces formations, suggérant que la puissance électrique produite pourrait dépassant 2 mégawatts (MW$_{e}$) à partir de puits individuels. Ces formations détritiques basales pourraient ainsi fournir un approvisionnement en énergie électrique significatif sur une vaste région du Saskatchewan.Las formaciones Winnipeg y Deadwood forman reservorios clásticos profundos en Saskatchewan, Canadá, con temperaturas que exceden 40 °C sobre la mayor parte del sur de Saskatchewan y alcanzan 100 °C en el sudoeste de Saskatchewan. A estas temperaturas las formaciones tienen un potencial geotermal para desarrollar uso directo y sistemas de generación eléctrica. Numerosos pozos residuales que operan en caudales de 30 L/s ó más están actualmente instalados en estas formaciones, sugiriendo que la electricidad podría ser generada a ritmos que exceden los 2 Megawatios de salida eléctrica (MW$_{e}$) a partir de pozos individuales. Estas unidades clásticas basales así podrían proveer un abastecimiento significativo de energía sobre una amplia región de Saskatchewan.As formações de Winnipeg e Deadwood formam reservatórios clásticos profundos em Saskatchewan, no Canadá, com temperaturas que excedem os 40 °C em quase todo o sul de Saskatchewan e atingem os 100 °C no sudoeste de Saskatchewan. A estas temperaturas, as formações têm um potencial geotermal para o desenvolvimento do uso direto e de sistemas de geração de eletricidade. Numerosos furos operando a taxas de 30 L/s ou mais estão atualmente instalados nestas formações, sugerindo que eletricidade poderia ser gerada a taxas excedendo 2 megawatts de saída elétrica (MW$_{e}$) em furos individuais. Estas camadas clásticas basais poderiam então providenciar uma produção energética significativa para uma região abrangente de Saskatchewan. |
| Starting Page | 143 |
| Ending Page | 150 |
| Page Count | 8 |
| File Format | |
| ISSN | 14312174 |
| Journal | Hydrogeology Journal |
| Volume Number | 22 |
| Issue Number | 1 |
| e-ISSN | 14350157 |
| Language | Portuguese |
| Publisher | Springer Berlin Heidelberg |
| Publisher Date | 2013-11-30 |
| Publisher Institution | International Association of Hydrogeologists |
| Publisher Place | Berlin, Heidelberg |
| Access Restriction | One Nation One Subscription (ONOS) |
| Subject Keyword | Canada Thermal conditions Sedimentary rocks Injection wells Heat flow Hydrogeology Hydrology/Water Resources Geology Waste Water Technology Water Pollution Control Water Management Aquatic Pollution |
| Content Type | Text |
| Resource Type | Article |
| Subject | Earth and Planetary Sciences Water Science and Technology |
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