Mathematics of Geothermal Energy(ebsco.com) |
Mathematics of Geothermal Energy(ebsco.com) |
Like, clearly Earth's crust supports temperature gradients which are steep enough to make the juice worth the squeeze. Presumably you're not going to find gradients so steep in the case of a runaway greenhouse effect, but whatever gradients you do find, are there fundamental limits preventing them from being steep enough?
This is a very brief, high-level overview. It weirdly dives deep into some less-relevant topics and glosses over a LOT of things.
It is not irrelevant, but not terribly reliable either. The "Mathematics" in the title is self-evidently clickbait.
YMMV.
There are (at the very least) 2 reasonable places I can think of off the top of my head in which to look around for answers -- both are organizations that run annual meetings on the topic of geothermal energy.
One is the Geothermal Rising professional organization [1]. There is a claim on the website that the papers from the annual meeting (roughly a month back) are available for free download by anybody. I can't find the actual head-link for those papers. A search engine is your friend. (I would not trust an LLM for this particular job.)
A second one is the Stanford Geothermal Workshop [2]. That is also an annual meeting. Again, use a search engine.
Sorry to not be more helpful, but this is a pretty large topic.
[1] https://www.geothermal.org/2026-geothermal-rising-conference... [2] https://geothermal.stanford.edu/events/workshop/past-proceed...
Iceland has unlimited geothermal energy and a cold climate. Seems a lot easier than going to space for solar energy