Superhot conditions exist below geothermal reservoirs where the heat in the rocks is higher than traditional geothermal systems, in excess of 350°C. Superhot systems may not have high enough pressure for fluid to exist as supercritical fluid.
Mau ai ngā āhuatanga pūhanahana i raro iho i ngā māpuna waiwhatu e wera ake ai te wera i ngā pūnaha hanawhatu māori, arā, i te 350°C (tārau). Tērā pea kāore te nui o te pēhanga o ngā pūnaha pūhanahana e rahi kia huri ai te waiwhatu hei waiwhatu tuawhiti.
There's a lot of talk about superhot rocks being a valuable resource for electricity in the future. Even politicians have gotten into the act!
Ka nui ngā kōrero mō ngā toka pūhanahana hei rawa whaihua mo te mahi hiko i ngā tau e haere mai ana. Hei matapaki hoki ma te hunga tōrangapū!
