One of the more controversial bioforming techniques makes use of
the ability for certain microbes to accumulate rare earth metals, and
more worrying span the gap between biological life and nuclear power.
Table showing some
uranium concentrations of common crustal rocks, and other sources
Source Material
|
Uranium
concentration, parts per million (ppm)
|
Source Material
|
Uranium
concentration, parts per million (ppm)
|
Average of crust
|
2.0
|
Andesite
|
2.0
|
Sea water
|
0.003
|
Shale
|
3.2
|
Granite
|
4.0
|
Limestone
|
2.2
|
Basalt
|
0.5
|
Sandstone
|
1.3
|
Taking only one element
into consideration, uranium, we can see that although relatively little
is present in a variety of materials, and very much dispersed, but as
soon as we start to process rock on metres cubed scale we can quickly
accumulate significant amounts of uranium. A tonne (or put another way, a million grams) will
on average contain a few grams of uranium, and also some other
radioisotopes, and engineered bacteria will quite happily extract this
for free. (Also uranium oxidation is an exothermic process providing the
bacteria with a potential energy source to drive their cellular
processes)
Bacteria have already been
extensively used to dissolve away rock, to generate large subterranean
cavities, usually for terraforming projects, the projects generate huge
caverns which can stably hold water, or accommodate for storage of other
things, which is useful when one wants to start engineering an existing
environment. The outcome of this is that the solutions that the rock
eating bacteria generate will contain significant amounts of rare earth
metal, and the processes tend to generate millions of metres cubed of
excavation, meaning literally tonnes of uranium.
Reactorbacillus is a
engineered microbe made from a combination of different existing
bacteria which have some bioleaching abilities, as well as the inclusion
of completely new genes which have artificially developed, some species
of reactor bacillus work independently of mining microbes slowly
dissolving the rock themselves, others are part of a greater community
of engineered microbes, but all have one ability, to accumulate rare
earth metals. Usually uranium and other rare earth metals are fused into
‘sulphur clusters’ that reside in the cell, the relatively small
amounts of rare metals, even in the increased concentration in the cell
do little to harm it. However of cell death, the precipitation of these
bacteria from the medium form highly enriched deposits. It is in this
increased concentration that the accumulated radio-nucleotides begin to
function as a reactor, as enough material is in such close proximity.
In this way biological agents
can be used to generate natural reactors, nearly anywhere. As far as
terraforming projects are concerned this is of remarkable benefit as
these natural reactors can provide vast amounts of heat, with no real
energy required in their generation. The process also prevents the
accumulation of a critical mass of radioisotopes, as the heat and
radiation given off by the functioning reactor act to sterilize the
immediate environment, prevent further accumulation of fuel from the
bacteria. Most systems equilibrate over time generating a low output
reactor which is continuously fed by the lifecycle of the microbes. It
could be thought that this process would generate an unenviable amount
of radioactive waste, but these reactors are usually hundreds of metres
below ground, and the reactor in a very small confined area, though
there is some risk of losing radioisotope through water seepage, the
complexes of metals formed are relatively insoluble and inert and so
stay put.
In addition to this reactor formation process other bacteria have
been developed to take advantage of other earth metals, such as
plutonium 238, generated in the reactors, and concentrate this to form
‘natural’ radiothermal sources where the energy comes from the
natural decay of the isotope.
Additional notes
Formation of a natural
reactor using uranium is dependent on the concentration of 235U, when
proportions of this isotope fall below 1% (in relation to 238U) then no
amount of uranium accumulation will result in criticality. For this
reason this method is restricted either to younger planets (higher
relative abundance of 235U), or to particularly nuclide rich worlds.
Also
the natural formation of a layer rich in uranium, but also rich in
organic material and water allows for some moderation of neutrons, which
help regulate reactor stability. Also in the event of rapid reaction,
the water within the mass will vaporize, and the loss of this moderating
medium will temporarily halt the reaction.
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