Volcanoes have
long been associated with valuable mineral and metal deposits. Volcanogenic
massive sulfide deposits are a major source of these ores. The heat and pressure
in the volcanic fluids rearrange molecules in the semi-solids, liquids, and gases and
cause changes in those phases. These fluids also include subsurface water that
may be heated by the adjacent geofluids, resulting in a hydrothermal system
that fills nearby fractures or the porous spaces in nearby rocks with granular
or fracture space for fluids, including sedimentary rocks. Most non-ferrous
metals extracted around the world are linked to magma.
Researchers
from the UK’s Oxford University are studying a dormant volcano on the Caribbean
Island of Montserrat, with the goal of assessing the feasibility of extracting
metals from the metals-rich geofluids under the dormant volcano. Generating
geothermal heat and power would be a co-benefit of these kinds of projects.
Research is in the early stages.
In my deep dive into brine mining, I covered geothermal brines from sedimentary basins, or oilfield brines, and geothermal brines such as those from salar deposits which are concentrated brines under salt flats. Some of these such as the Smackover brine in Arkansas, Louisiana, and Texas, and brine which yields bromine in Japan, are also considered to be magmatic brines. According to Professor Stephen Sparks FRS from the University of Bristol:
“You can have groundwater leaching through cracks and
permeable rock to form saline solutions, for example, and these brines could
also be useful,” he says. “But magmatic brine forms from the magma
itself.” Solid rock can contain water, such as in hydrated salts or that
dissolved into the minerals that comprise the rock. When friction between
tectonic plates melts rock to form magma, that water becomes part of a
homogeneous molten solution. Through a series of complex geological processes
associated with volcanic activity that take place over millions of years,
mineral-rich brines accumulate in the sub-surface.”
“The liquid brine tends to lie two to four kilometres
below the surface in lens-shaped deposits.”
Geothermal drillers usually avoid areas with suspected magmatic brine. One reason is the
heat. These geofluids may be too hot for conventional geothermal development.
Research is ongoing with hot, supercritical geothermal brines. The image
below is of a geothermal power plant in Japan that is being considered for
supercritical geothermal development of deeper magmatic brines. In the 1990s a 3.7km
test hole there in a granite found an unusually metal-rich brine at 520 degrees
C. Since then, it has become cheaper and more technologically feasible to test drill
supercritical geothermal but it is still in its infancy. The flow charts below
show some of the advantages of extracting lithium from brines vs. mining hard
rock for lithium.
UK-based
scientists Olivia Hogg and Jon Blundy writing for Geoscientist lay out their
case for accessing magmatic brines for heat, energy, and metals:
“There is a growing awareness that magmatic brines
have the potential to resolve the resource paradigm in which we find ourselves.
Investing time in technological development and broadening our understanding of
volcanic systems, including drilling into them, is central to evaluating how we
can simultaneously harness geothermal power and metals, and so better equip us
for the energy transition. In many ways, the storage of magmatic fluids in
underground porous rock resembles oil-and-gas reservoirs, meaning that existing
hydrocarbon expertise could be readily repurposed in the hunt for brine
reservoirs.”
It should be
acknowledged that it could take many decades before the hotter magmatic brines and
supercritical geothermal are tapped. Some, like the Smackover formation, which
is being tapped now, is much cooler at about 150 degrees C. Accessing hotter
geothermal has many challenges such as well integrity, O&M issues, scaling
& corrosion, tool damage, and more. Some of these issues are more common
with hotter metals-rich brines. Scaling can occur in the well as thr brines lose
pressure and temperature so that they precipitate as scale as they come closer
to the surface. Hogg and Blundy write:
“For example at Kakkonda, well-bore scales contain up
to 13% per cent weight of copper, 20% zinc and 20 ppm gold, not to mention a
wealth of other valuable metals. Ensuring that this polymetallic bounty is
brought to the surface, rather than precipitating en route is crucial.
Designing novel materials that can sequester metals from hot fluids at the
bottom of the well, and development of well-casing materials that inhibit scale
nucleation, are just two possibilities under consideration.”
They estimate that as many as 2000 dormant volcanoes
could host metalliferous magmatic brines that could one day be tapped.
The volcano at
Montserrat erupted in the 1990s, devastating the island. As a result, its
population was reduced from 12,000 to just 4,000 inhabitants as people left
after the eruption destroyed the island’s biggest town. It has had a continuous
eruption for 20 years but is now showing signs of dormancy. If it could be
tapped for geothermal energy, it could power the island as well as produce metals.
It could replace the diesel generators that currently power the island. The Montserrat
research is expected to go on through October 2026.
References:
Scientists
make energy breakthrough after observing geofluids in dormant volcanoes —
here's what it could mean. Stephen Proctor. The Cool Down. July 25, 2024. Scientists
make energy breakthrough after observing geofluids in dormant volcanoes —
here's what it could mean (msn.com)
Geofluids:
Developments in Microthermometry, Spectroscopy, Thermodynamics, and Stable
Isotopes. A volume in Vapor-Liquid Equilibrium Data Bibliography. Book. 2015. Geofluids
| ScienceDirect
UK
scientists eye dormant volcano juice to extract battery metals, energy. Aleya
Paleja. Interesting Engineering. July 1, 2024. Oxford
eyes dormant volcano juice to extract battery metals, energy
(interestingengineering.com)
Mining
volcanoes for metals. Ingenia. March 2024. Mining
volcanoes for metals | Ingenia
Mining
the brine. Olivia Hogg and Jon D. Blundy. Geoscientist. May 16, 2022. Mining
the brine - GEOSCIENTIST
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