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One of the biggest challenges facing mankind today is our quest to transition to renewable
energy. Overhauling our entire electricity grid requires drastic changes to be made in
the way we produce, transport, use and store electricity. We have explored in past videos,
that with the lowering cost of solar and wind, we are beginning to hit a point of imbalance
in the grid. Where places like California are wasting massive amounts of energy in the
summer months, when solar is at its peak and not producing enough in the winter. To deal
with this problem California is now installing gigantic battery storage facilities in places
like Moss Landing to store that excess for later use, but the amount of battery storage
that they will require as our percentage of renewables increases is going to cost the
state billions, if not trillions.
We could drastically decrease this dependence on batteries, if we could find a nice stable
energy source that did not harm our planet. Some want to turn to nuclear energy, but what
if I told you the solution may be lying directly under our feet.
Imagine an ancient, hidden energy source, deep within every square meter of our planet’s
surface. It’s clean, flexible, virtually limitless, completely renewable, never turns
off and virtually carbon free. Geothermal energy, the energy produced by the earth itself
in the form of heat, can be that solution.
Geothermal energy is produced by the Earth’s inherent heat. The center of the earth (On
screen: 6500km deep) is as hot as the surface of the sun (6000 °C). Through convection,
that heat warms the outer layers of the planet. But where does this heat come from? Much of
it comes from gravitational forces when the planet first form 4 billion years ago, some
heat is generated from friction as denser elements make their way to the earth's core.
The other source of Earth’s internal heat occurs in the upper mantle and crust, where
the decay of radioactive isotopes, like Potassium-40, creates energy, and in turn, heat. If we could
find a way to safely and cost effectively access that heat our energy problems would
be solved in years.
That heat does come to the surface in some easily accessible locations. At temperatures
of 700 °C or more, rocks become partially melted, becoming magma, driving a variety
of geothermal phenomena. If magma flowing underground heats gases or water it can create
bubbling hot springs and geysers, undersea hot vents, and natural steam vents. These
features can provide water that’s more than 200 °C, more than enough to run a steam turbine.
Geothermal hot spots like this are found near the boundaries of tectonic plates, like Iceland,
in volcanically active areas, like Turkey, or in some places where Earth’s crust is
thin, like America’s Yellowstone National Park. These places provide low hanging fruit
to harvest the earth’s heat for our energy needs.
Each year enough heat flows (44 TWth) to the planet’s surface to meet total global energy
consumption twice over [1]. And the geothermal reservoir is boundless: heat within 10km of
Earth's surface contains roughly 50,000 times more energy than all fossil fuel resources
worldwide [2].
Yet geothermal energy makes up less than 1% of global installed electricity capacity.
This isn’t even a technology issue, of the global potential for geothermal power using
off-the-shelf technology, only 7% has been tapped [3]. So in the fight to transform our
global energy system, why haven’t we adopted this energy source in a serious way?
Let’s first look at our low hanging fruit, that are not being used to their full potential.
Naturally occurring hydrothermal reservoirs feature hot water that percolates near the
surface through porous or cracked rock layers. This is the easiest form of geothermal energy
to harvest, and can be tapped in several ways, which we have been doing for centuries.
Human societies have used the heat from low-temperature (150 °C) geothermal energy for millennia.
Among the most famous examples may be the hot springs of Bath, England, established
by Roman engineers in 60 CE. Here 1 million litres of water percolate to the city centre
of bath every day at a temperature of about 45 degrees, heating recreational baths and
heating some buildings. This hot water replenishes itself as rain that falls in nearby hills
seeps through porous limestone deep underground where it is heated and rises back to the surface.
[4]
But convenient locations like this where the right combination of a water cycle, with porous
rocks underground and a heat source close enough to the surface to heat it, are rare,
and ones that can provide water with enough heat and pressure to run a steam turbine are
even rarer. This particular source is not suitable, as 45 degrees is far off the lowest
temperature we can employ.
There are three basic types of geothermal energy generators. All three share the same
basic idea. Take hot water or steam from a geothermal reservoir
and run it through a steam turbine where it loses energy and condenses before being pumped
back underground to keep the cycle going. Dry Steam generators take the steam directly
from the source to run a turbine. A flash steam power plant takes extremely hot water
under pressure above 100 degrees, and expands it quickly to lower its boiling point and
turn it steam to run the steam turbine.
These both require higher temperature sources that are rare, [5] but they are relatively
common in geothermally active regions like Iceland, Italy, Austria and around the Pacific
ring of fire, and in these locations geothermal energy is common and is expected to grow as
much at 28% in the next 4 years, with countries in South East Asia expected to see the largest
growths like Indonesia and the Philippines. [6]
But we want to exploit geothermal energy outside of these regions. No matter how much power
we can extract we can’t transport it far before power losses due to resistance in the
cables saps it away. The third type of generator provides the highest potential for expanding
geothermal energy as it can utilise the lowest temperature sources.
This system is called a binary cycle system. In a binary cycle power plant, warm water
from a geothermal source passes through a heat exchanger where it exchanges heat with
a closed loop containing a fluid with a low boiling point, like pentane, which has a boiling
point of 36 degrees. The lower boiling point allows it to transition to a gas at a much
lower temperature, allowing it to run a turbine at a lower temperature.
This system has allowed countries like Germany [7], which lacks any shallow depth geothermal
resources, to grow their geothermal energy market in recent years with temperatures as
low as 100 degrees celsius being utilised. That figure is important, because the higher
the temperature the deeper we have to drill.
Different areas have different geothermal gradients, which is a measure of how quickly
temperatures rise as we drill down. This map shows a rough estimate of the geothermal gradient
across the US [8], with the highest gradients being found in Oregan and Idaho reaching as
high as 70 degrees per kilometre. This is important, as to access this heat in areas
where it doesn’t naturally come to the surface in an accessible way we need to drill down
and the further down we need to drill the more expensive it becomes.
Typically we have only used geothermal resources where the natural permeability of the rock
allows a convective heat cycle, but a new technology by the name of Enhanced Geothermal
Systems or EGS, may open the door to geothermal energy to more regions.
It works like this. The first step is to drill an injection well into a formation of hot
rocks. Then engineers inject fluid at pressure to form cracks or enlarge existing ones, this
increases the area over which heat exchange with the rocks can occur. To increase this
area even further a non-toxic and degradable material is pumped down to fill these cracks
and allow the pressure to form new cracks as we drill further down. Once we have opened
an adequate number of passages for the water to fill we can drill additional holes that
can take act as an outlet for our hot water as we pump more underground.
A report by MIT in 2006 [9] found that EGS could provide electricity at a cost as low
as 3.9 cents per kilowatt hour, roughly equivalent to a coal-fired power plant. The United States
government estimates [10] that new geothermal power plants could produce 60 gigawatts of
electric power on American soil by 2050, mostly through EGS systems.
Now I know what you are thinking, this sounds a lot like the controversial practice of fracking,
but it doesn’t use toxic fracking fluid which can seep into our water cycle, it uses
water and some safe additives, but it’s not all plain sailing. [11] To make this work
we need to create great volumes of fractures and cracks and this can have some disastrous
consequences.
In 2017 drilling at a proposed site for EGS in Pohang, South Korea [12], is thought to
have triggered an earthquake of 5.4 magnitude that injured 135 people. A previous incident
occurred at an EGS plant in Basel, Switzerland in 2006, when drilling may have caused a quake
of magnitude 3.4, and several buildings were damaged. Both projects were cancelled as a
result.
Red tape is a huge obstacle for Geothermal Energy. In the United States, for example,
there’s less environmental paperwork and fewer approvals required for drilling for
oil than drilling a geothermal well. Tax credits for wind and solar power project are 30% while
the tax credit for geothermal is only 10%. [13]
On top of all this, drilling is very expensive and as we have seen doesn’t guarantee a
successful geothermal plant. You could waste months of your time digging a 2 kilometre
hole in the ground and the productivity of the well could be too small to make the project
worthwhile. That makes it difficult to find investors willing to bet their money on it.
It simply makes more sense to invest in solar and wind.
Despite the challenges, there’s real hope for expanding geothermal energy. The industry
can build off of recent improvements in drilling technology. [14] Engineers are developing
new kinds of drills for geothermal wells, and better techniques for cementing wells
drilled into hot rocks. The earthquake risk is real, but engineers have protocols for
monitoring with seismometers to ensure that the seismic risk can be assessed early on.
In the case of the Basel accident, the EGS facility was located over a seismic fault,
due to the proximity of hot rocks to the surface. Once the shaking started, fluid injection
was halted immediately. So far, geothermal projects haven’t attracted strong political
support in the West, but they also haven’t drawn major opposition, suggesting that easing
permitting rules for the technology may not be so challenging. As commercial interest
in this clean energy source rises, political support for it should follow, especially if
some smart politician realises it can be a rallying call for getting out of work oil
drilling techs back to work.
Sometimes the struggle to convert the global energy system to renewables can seem out of
reach and feel hopeless. But in the case of geothermal energy, there’s an exciting source
of electricity and heat that could power our future, and it’s right below our feet.
As I said at the start of the video, much of the energy present within earth is formed
as a result of gravitational forces. You can learn everything gravity is capable of by
taking this course on Brilliant.
This course will take you from the very basics of what gravity is and build your knowledge
up to the point of being able to apply Kepler’s laws of planetary motion and understand orbital
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Or you could complete one of Brilliant’s daily challenges. Each day Brilliant presents
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