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Environmental
Problems in Perspective
Broadcast ABC Radio
National
6 November 2005
Duncan Brown
Every animal species has
functional characteristics, behavioural as well as
physiological, which contribute to its identification as a
species. As well as unique manual dexterity, there are two
behavioural characteristics of homo sapiens that, in my
opinion, have underpinned just about every impact we have
had, and are having, on the planet’s ecology and general
environment. The first is a remarkable ability to focus on
details while overlooking or not understanding the
functioning of complex dynamic systems, or what Paul Keating
called ‘the big picture’. This detailed focus lies at
the heart of the extraordinary achievements in virtually all
fields of science and technology, but it can have its
problems in an ecological context.
The second human characteristic is a widespread tendency to
accept conventional wisdoms, be they religious, economic or
scientific. History is studded with examples of the
penalties imposed on those with unorthodox opinions, such as
suggesting that the earth is round and, as well as rotating
on its own axis, might actually circle the sun.
In this talk I shall try to put the environmental problems
that we face into some sort of perspective. Serious
environmental problems are widely acknowledged. They are
mostly identified as specific challenges, such as
deforestation, soil and water degradation, loss of
biodiversity, and of course, global warming. The essence of
my argument is that all of these challenges, while very
serious, are actually symptoms of a much more dangerous
predicament, a human population that is too large and too
dependent on technology to be sustainable.
But let me begin with some comments on global warming, the
symptom that currently seems to receive most attention and
is discussed almost entirely in the context of the
‘greenhouse effect’. This is an interesting example of
widespread acceptance of a conventional wisdom while other
more significant factors are largely overlooked or ignored.
To simplify: the earth’s average atmospheric temperature
is estimated to have risen by about 0.6 degrees Celsius over
the past century. This heating is attributed predominantly
to absorption by carbon dioxide of infrared radiation. The
current average atmospheric concentration of carbon dioxide
is estimated to be 372 parts per million, thought to be the
highest for at least 420,000 years. But water also absorbs
infrared radiation, and there is much more of that in the
atmosphere than there is of carbon dioxide.
Many factors have contributed to heating the atmosphere
since the advent of agriculture. They include major changes
to the earth’s surface, especially deforestation with its
associated loss of cooling by ‘evapotranspiration’; the
growth of cities, which are recognised as ‘urban heat
islands’; an increase in the total biomass of mammals; and
most significantly, the heat produced by enormous increases
in rates of combustion.
The quantity of so-called ‘fossil’ carbon burnt in 2003
amounted to some 6 Giga tonnes. Fossil carbon occurs in a
wide range of substances which are not identified in that
statistic; but to oversimplify and assume for example that
it was distributed equally among anthracite coal and three
significant components of motor fuel: pentane, hexane and
decane, the heat produced amounted to 74 billion Giga
calories for the year. Ignoring a range of atmospheric
variables which are virtually impossible to quantify, that
amount of heat has the capacity to raise atmospheric
temperature by 0.06 degrees Celsius annually. Variables or
not, that would seem to be enough to make a very substantial
contribution to an increase of 0.6 degrees Celsius over a
century. And that takes no account of other significant
types of combustion, such as bushfires.
One of the curious aspects of the overwhelming focus on
carbon dioxide and the ‘greenhouse effect’ is that it
attributes the heating process entirely to radiation and
ignores direct heating by contact and conduction. Of course
primary solar heating occurs by radiation and heat is lost
from the planet by radiation. But much, and indeed probably
most of the heat transfer within the planet’s boundaries
involves conduction. Carbon dioxide at its present
concentration is irrelevant to direct heating of the
atmosphere in that way.
The focus on greenhouse gases would not matter at a
practical level if it led to a reduction in overall
combustion. But if it provokes chemical binding of carbon
dioxide, or its geosequestration, which amounts to burying
it underground, or the use of alternative fuels such as
hydrogen, the primary heating problem will not be addressed
and there will certainly be a range of disturbing,
unintended consequences.
If global warming and the other challenges mentioned earlier
are symptoms, what is the primary cause of our environmental
predicament? It began 10,000 years ago with the advent of
agriculture. Before farming, the human biomass, like that of
any other animal species, was ultimately limited by the rate
of food production, basically of green plants. In other
words, the relation between the human population and its
food supply was one of negative feedback. What is negative
feedback? A simple example is the process that regulates the
temperature of a thermostatically controlled oven. When the
temperature reaches the preset limit, the input of energy is
either reduced or cut off.
With agriculture, that relation changed to positive
feedback. That is to say when the population reached the
limit of what could be supported by existing rates of food
production, the response was to produce more food. In my
bok, ‘Feed or Feedback’ I have proposed nine ‘Laws of
Ecological Bloody-mindedness’, the second of which says,
‘Any system in a state of positive feedback will destroy
itself unless a limit is placed on the flow of energy
through that system’. To revert to the previous
comparison, it does not take much imagination to recognise
what would happen if the hotter the oven became, the more
heat was applied to it.
In a social context, systems in a state of positive feedback
are usually called ‘vicious circles’. They are typified
by communal relations, such as war and vendettas, by drug
addictions, by building freeways and parking lots to deal
with traffic congestion.
Agriculture however, produced a range of side effects with
their own vicious circles. With practice and experience,
farming techniques improved and the farm surplus increased.
This enabled or obliged some of the population to go
somewhere else, and do something else for a living. That
something else included making tools, some of which further
increased the farm surplus and generated another vicious
circle. It also led to the genesis and growth of cities, a
process with a wide range of unintended consequences. Those
consequences included severe deterioration of hygiene and
public health, leading to increases in death rates and a
substantial fall in population, especially in urban Europe.
Dealing with these problems included, among other things,
sewers, which in turn had their own unintended consequences.
Improvements in urban sanitation eventually led to a
resumption of population growth, one results of which was an
increase in the area of farmland. Food now had to be
transported over greater distances from farms to cities.
That, together with the development of sewers, meant that
food wastes and human excrement, which formerly had been
returned to farmland, were no longer recycled but, for the
most part, at least in the case of sewage, were discharged
ultimately into the sea. As a result, some essential
nutrient elements came to be used in a way that was, and is,
irreversible. The most vulnerable of these elements is
phosphorus, reserves of which, allowing for the inevitable
uncertainties, will probably last somewhere between 85 and
190 years.
Responses to this type of problem, and indeed to most
environmental challenges, all too often amount to treating
the symptoms, usually by invoking technology. Some years
ago, after mentioning the phosphorus situation in a talk to
engineers, I was asked if a substitute for phosphorus was
available. The problem there is that the element whose
chemical properties are closest to those of phosphorus is
arsenic. More recently, a physicist commented that if we
could develop hydrogen fusion, there would be no problem in
meeting the energy requirements of recovering phosphorus
from the sea. Such arguments take little or no account of
the dynamics of these processes. The concentration of
phosphorus in the sea is such that, to meet current rates of
fertiliser application, sea water would have to be processed
at a daily rate of 646 cubic kilometres. That is more than
50 times the global rate of consumption of fresh water. Not
only would it require enormous amounts of energy, it would
effectively destroy the marine ecosystems.
The present global human population has passed 6 billion. It
is expected to reach about 9 billion by mid-century. But let
us look briefly at some of the basic implications of
sustaining 6 billion people. The environmental impact of any
population of animals is fundamentally a result of the
combined effects of many different types of process
operating at different rates. All of those rates are
functions of the number of individuals. Citing rates in
isolation cannot lead to any firm conclusions, but it can
give some feeling for the dimensions of a problem. For
example, if a human population of 6 billion eats on average,
50 grammes of protein per capita daily, that amounts to a
total of 208 tonnes a minute. If it were all eaten as steak
the total rate of consumption would be 1040 tonnes a minute.
If it were all wheat, the gross rate would be 2080 a minute.
Production of food at such rates makes huge demands on a
range of factors, including fertilisers and energy, the
latter both in producing the food and transporting it to
where it is eaten.
The basic problem of feeding a large and growing population
is widely recognised, but not usually in the way I have just
mentioned. A question commonly asked however is How are we
to feed a population x billion? The answer usually expected
is, Another Green Revolution. Recent statistics shed some
light on that approach. Over a 40 year period, global grain
production increased almost threefold, from 631 million tons
in 1950 to 1780 million tons in 1990. But in the later
stages of that period and beyond, production per capita
decreased progressively from 356 kilograms in 1984 t5o 308
kilograms in 2000.
The most fundamental environmental problem, however, is a
progressive simplification of the global ecosystems. In
other words, we are destroying our own habitat. If that
should lead to human extinction, which is possible, it would
be an impressive achievement. Over the ages, many species
have become extinct for various reasons, including human
activities. For a species to bring out its own extinction by
its own deliberate activities would be a world first and
would have the essential ingredients of a particularly
diabolical joke. We need to acknowledge our biology. We are
a species of animal, which despite our sophistication and
technological achievements, depends for survival on the same
fundamental principles as all other species. Economics and
technological sophistication can affect the quantitative
details of that dependence, but not the basic principle.
Duncan Brown
Emeritus Professor
Department of Biological Sciences
University of Wollongong
Publications:
Feed or Feedback
Author: Duncan Brown
Publisher: International Books
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