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10.1038/ncomms8837 http://scihub22266oqcxt.onion/10.1038/ncomms8837 C4525172!4525172!26211617     free     free     free Deprecated: Implicit conversion from float 219.6 to int loses precision in C:\Inetpub\vhosts\kidney.de\httpdocs\pget.php on line 534 Deprecated: Implicit conversion from float 219.6 to int loses precision in C:\Inetpub\vhosts\kidney.de\httpdocs\pget.php on line 534 Deprecated: Implicit conversion from float 219.6 to int loses precision in C:\Inetpub\vhosts\kidney.de\httpdocs\pget.php on line 534 Deprecated: Implicit conversion from float 219.6 to int loses precision in C:\Inetpub\vhosts\kidney.de\httpdocs\pget.php on line 534       Nat+Commun 2015 ; 6 (ä): ä Nephropedia Template TP {{tp|p=26211617|t=2015. Geologic controls on supercritical geothermal resources above magmatic intrusions |pdf=|usr=}}{{26211617}} gab.com Text Geologic controls on supercritical geothermal resources above magmatic intrusions JO: Nat Commun http://www.kidney.de/pget.php?&tw=1&pmid=26211617 #FOAvip A new and economically attractive type of geothermal resource was recently discovered in the Krafla volcanic system, Iceland, consisting of supercritical water at 450?°C immediately above a 2-km deep magma body. Although utilizing such supercritical resources could multiply power production from geothermal wells, the abundance, location and size of similar resources are undefined. Here we present the first numerical simulations of supercritical geothermal resource formation, showing that they are an integral part of magma-driven geothermal systems. Potentially exploitable resources form in rocks with a brittle?ductile transition temperature higher than 450?°C, such as basalt. Water temperatures and enthalpies can exceed 400?°C and 3?MJ?kg?1, depending on host rock permeability. Conventional high-enthalpy resources result from mixing of ascending supercritical and cooler surrounding water. Our models reproduce the measured thermal conditions of the resource discovered at Krafla. Similar resources may be widespread below conventional high-enthalpy geothermal systems. Twit Text FOAVip Geologic controls on supercritical geothermal resources above magmatic intrusions ????Nat Commun http://www.kidney.de/pget.php?&tw=1&pmid=26211617 #FOAvip Twit Text # Free Paper on # # # # # LINK http://www.kidney.de/pget.php?&tw=1&pmid=26211617 #FOAvip English Wikipedia <ref>{{Cite pmid|26211617}}</ref> Geologic controls on supercritical geothermal resources above magmatic intrusions #MMPMID26211617 Scott S; Driesner T; Weis P Nat Commun 2015[]; 6 (ä): ä PMID26211617show ga A new and economically attractive type of geothermal resource was recently discovered in the Krafla volcanic system, Iceland, consisting of supercritical water at 450?°C immediately above a 2-km deep magma body. Although utilizing such supercritical resources could multiply power production from geothermal wells, the abundance, location and size of similar resources are undefined. Here we present the first numerical simulations of supercritical geothermal resource formation, showing that they are an integral part of magma-driven geothermal systems. Potentially exploitable resources form in rocks with a brittle?ductile transition temperature higher than 450?°C, such as basalt. Water temperatures and enthalpies can exceed 400?°C and 3?MJ?kg?1, depending on host rock permeability. Conventional high-enthalpy resources result from mixing of ascending supercritical and cooler surrounding water. Our models reproduce the measured thermal conditions of the resource discovered at Krafla. Similar resources may be widespread below conventional high-enthalpy geothermal systems. äGeologic controls on supercritical geothermal resources above magmatic(epmc).pdf DeepDyve Pubget Overpricing