Education Piece - Geothermal 101
Welcome back to another issue of ClimateRoots! These next two issues we are going to be talking about a super interesting method of energy production: Geothermal!
Before we dive too deep, let’s take a step back and talk about the planet we call home. Harnessed in the Earth is an insane amount of heat and pressure, thanks to billions of years of radioactive decay and non-stop heat loss from the planet’s formation. The steep temperature gradient near the surface means that going down into the crust even just a bit will reward us with enough thermal energy to do a lot of cool things! Geothermal relies on using steam to spin a turbine to produce power (check out our piece on steam turbines to see how generators work). There are three ways of doing this that are widely used in power plants scattered across the world: dry steam, flash steam, and binary steam.
Dry Steam
The oldest and arguably easiest form of geothermal production, dry steam power plants work by directly pumping steam from underground reservoirs up into a turbine/generator. From there, the steam is condensed into water and pumped back into the ground to become steam again. Northern California lays host to the largest dry steam energy production in the world, a site known as “The Geysers”.
Flash steam
Flash steam production is much harder to come by as it requires an underground reservoir of fluid in excess of ~182 degrees celsius, although it is currently the most common method used globally. At greater depths, the higher pressure will allow fluids to remain in a liquid state at warmer than normal temperatures because its boiling point will be greater as well. Flash steam power plants will pump this fluid up to the surface where the pressure is much lower, and thus its boiling point is as well, causing the fluid to “flash” into a vaporized state. This vapor is then pumped into a turbine and later condensed to be pumped back into the reservoir.
Binary cycle
Finally we have binary cycle, which sounds way more technical than it actually is. This process takes advantage of a heat exchange to vaporize a secondary fluid, instead of relying on the primary underground fluid itself. This secondary fluid has a much lower boiling point than that of water, so it can more easily vaporize.
So what’s the catch?
Geothermal energy is often touted as the future of carbon-free power generation, and while it’s true that there is only a fraction of carbon emissions compared to other energy production methods like fossil fuels, there are still of course some drawbacks.
For starters, the process of geothermal power production can cause harmful gases to enter the atmosphere that would have otherwise been trapped underground. Additionally, geothermal energy is very location-specific. With most geothermal power plants existing on or near a tectonic fault line, not only does this severely limit the potential for expansion, there also comes problems with seismic instability.
At the end of the day, it is important to remember that no method of power production is perfect. Renewable energy is naturally very fickle, but any step away from fossil fuels is a good one. Geothermal is also by no means a perfect solution to our power crisis, but there is little doubt that the benefits outweigh the drawbacks. There are even some rather cool applications of geothermal on a small scale that we didn’t touch on today that are being used in homes worldwide.
To read this full piece with works cited, check it out on our blog!