In September 1991 four men and four
women entered the world’s largest glass bubble, known as Biosphere II, to test
the idea that humans could design and build a totally self-contained ecosystem,
a model for some future colony on another planet. Biosphere II (Earth is
considered Biosphere I) was a 3-acre mini-world, complete with a tropical rain
forest, savanna, marsh, desert, and working farm that was intended to be fully
self-sufficient. This unique experiment was to continue for 2 to 3 years, but
almost immediately there were signs that the project could be in jeopardy.
Soon after the bubble had been
sealed, sensors inside the facility showed that the concentration of oxygen in
Biosphere II’s atmosphere had fallen from its initial level of 21 percent (by volume),
while the amount of carbon dioxide had risen from a level of 0.035 percent (by volume),
or 350 ppm (parts per million). Alarmingly, the oxygen level continued to fall
at a rate of about 0.5 percent a month and the level of carbon dioxide kept
rising, forcing the crew to turn on electrically powered chemical scrubbers,
similar to those on submarines, to remove some of the excess CO2.
Gradually the CO2 level stabilized around 4000 ppm, which is high but
not dangerous. The loss of oxygen did not stop, though. By January 1993—16
months into the experiment—the oxygen concentration had dropped to 14 percent,
which is equivalent to the O2 concentration in air at an elevation
of 4360 m (14,300 ft). The crew began having trouble performing normal tasks.
For their safety it was necessary to pump pure oxygen into Biosphere II.
With all the plants present in
Biosphere II, the production of oxygen should have been greater as a
consequence of photosynthesis. Why had the oxygen concentration declined to
such a low level? A small part of the loss was blamed on unusually cloudy
weather, which had slowed down plant growth. The possibility that iron in the
soil was reacting with oxygen to form iron(III) oxide or rust was ruled out
along with several other explanations for lack of evidence. The most plausible
hypothesis was that microbes (microorganisms) were using oxygen to metabolize
the excess organic matter that had been added to the soils to promote plant growth.
This turned out to be the case.
Identifying the cause of oxygen
depletion raised another question. Metabolism produces carbon dioxide. Based on
the amount of oxygen consumed by the microbes, the CO2 level should
have been at 40,000 ppm, 10 times what was measured. What happened to the
excess gas? After ruling out leakage to the outside world and reactions between
CO2 with compounds in the soils and in water, scientists found that
the concrete inside Biosphere II was consuming large amounts of CO2 !
Concrete is a mixture of sand and
gravel held together by a binding agent that is a mixture of calcium silicate
hydrates and calcium hydroxide. The calcium hydroxide is the key ingredient in the
CO2 mystery. Carbon dioxide diffuses into the porous structure of
concrete, then reacts with calcium hydroxide to form calcium carbonate and
water:
Ca(OH)2(s)
+ CO2(g) → CaCO3(s) + H2O(l)
Vegetations in Biosphere II
Under normal conditions, this reaction goes on
slowly. But CO2 concentrations in Biosphere II were much higher than
normal, so the reaction proceeded much faster. In fact, in just over 2 years,
CaCO3 had accumulated to a depth of more than 2 cm in Biosphere II’s
concrete. Some 10,000 m2 of exposed concrete was hiding 500,000 to
1,500,000 moles of CO2.
The water produced in the reaction between
Ca(OH)2 and CO2 created another problem:
CO2 also reacts with water to form
carbonic acid (H2CO3), and hydrogen ions produced by the acid
promote the corrosion of the reinforcing iron bars in the concrete, thereby
weakening its structure. This situation was dealt with effectively by painting
all concrete surfaces with an impermeable coating.
In the meantime, the decline in oxygen (and
hence also the rise in carbon dioxide) slowed, perhaps because there was now
less organic matter in the soils and also because new lights in the
agricultural areas may have boosted photosynthesis. The project was terminated
prematurely and in 1996, the facility was transformed into a science education
and research center. As of 2007, the Biosphere is under the management of the
University of Arizona.
The Biosphere II experiment is an interesting project
from which we can learn a lot about Earth and its inhabitants. If nothing else,
it has shown us how complex Earth’s ecosystems are and how difficult it is to
mimic nature, even on a small scale.
ps: Adapted with permission from “Biosphere II: Out of Oxygen,” by Joe Alper, CHEM MATTERS, February, 1995, p. 8.
Copyright 1995 American Chemical Society.