Fieldsite St. Gallen Sample Clauses

Fieldsite St. Gallen. The St. Gallen deep geothermal project is located in the Swiss Molasse Basin between Xxxx Xxxxxxxxx and the Alps. The project is being run by St. Galler Stadtwerke, the local energy supplier and 100% owned by the city of St. Gallen, Switzerland. A high-resolution 3D seismic survey was conducted between 2009 and 2010 to image details of the target fault zone, a system of major NNE-SSW striking normal faults constituting the St. Gallen Fault Zone (SFZ) (Heuberger et al., 2016). A geothermal doublet was planned on the basis of this survey and the first 4,253 m deep well (St. Gallen GT-1) was drilled into fractured Mesozoic limestones, stimulated and tested for water (brine) and natural gas in 2013. Extensive wireline logging and sampling campaigns (water, gas and rocks) were executed forming a comprehensive data set. A microseismic network was established in cooperation with the Swiss Seismological Service (SED) and went online almost 12 months before the start of the drilling operation in 2013. Only one event of ML = 2.1 was detected on the eastern branch of the SFZ in June 2012 (Xxxxx et al., 2017). Initially observed low productivity was attempted to be enhanced by chemical stimulation. After the chemical stimulation in July 2013, a gas kick had to be controlled leading to induced seismicity of up to ML = 3.5. After a preliminary project development stop, the project works were resumed in October 2013 with a modified drill stem test producing gas and water allowing for the collection of additional data on the developed aquifer within the regionally prominent SFZ. Because of very low hot water flow rates, yet high natural gas rates produced, and associated high risks for felt induced seismicity, the geothermal project was halted in May 2014. Currently, the St. Gallen GT-1 well is temporarily conserved. Pressure is monitored from the surface and seismicity is monitored by a local monitoring system, which consisted of 12 surface seismometers and a downhole geophone deployed at 205 m depth during project phase (Xxxxx et al., 2017). Structural model of the St. Gallen geothermal project including well GT1, layers and faults as well as induced seismicity is shown in Figure 14. Figure 14: Structural model of St. Gallen displaying the well path of the geothermal well, top Paleozoic and faults (as interpreted from the 3D seismic survey, Heuberger et al. 2016) as well as hypocenters of the induced seismicity (from the SED). View from north-east. Since drilling at UDD...
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