At 800 meters, the ambient pressure is 80 times that of the atmosphere, high enough that the pressurized injected CO2 is in a “supercritical” phase—one that is nearly as dense as the brine it replaces in geologic formations.
At 800 meters, the ambient pressure is 80 times that of the atmosphere, high enough that the pressurized injected CO2 is in a “supercritical” phase—one that is nearly as dense as the brine it replaces in geologic formations.
在800公尺深处，压力高达大气压的80倍，足以令注入的二氧化碳呈「超临界态」，这种相态的稠密程度，与地质构造中的卤水相近。