Energy
and Environment into the
Twenty-First Century: The Challenge to Technology and Ingenuity*
WILLIAM L. FISHER
Search and Discovery Article #70003 (2000)
Department of Geological Sciences and Bureau of Economic Geology, The University of Texas at Austin, Austin, TX 78713
* Slight adaptation for online presentation from article of same title published in Environmental Geosciences. Volume 6, Number .4. 1999, p. 191-199.
ABSTRACT
Traditional
energy
resources, chiefly fossil fuels, are adequate to meet likely global
energy
demands as the transition to a hydrogen and renewable
energy
economy is made
over the next three to five decades. Long-term trends in efficiency in
energy
development, use, and conversion will continue and be enlarged. Reliance on
fossil fuels for the transition should not cause unacceptable environmental
impact, especially with the likely increased emphasis on low-carbon natural
gas. The historical economic growth of 3% per annum can be maintained for a
global population that will probably stabilize at ~10 billion by the middle
part of the twenty-first century.
INTRODUCTION AND BASIC TRENDS
The challenge of meeting the resource and environmental needs of the global society over the next century is a daunting one. The requirements must not only be met but met in a way that balances what to many seem to be conflicting goals. Inherent in resource development and consumption is exploitation; inherent in maintaining the global environment is preservation or at least conservation, seemingly opposites.
As
we stand at the end of the twentieth century, a number of long-term trends
have been established that are of positive benefit in meeting future resource
demands and do so in an environmentally acceptable manner. Most of these
trends will surely extend into the next century and will most likely be
enlarged. The first salutary trend, well established in the latter part of
this century, has been the remarkable reduction in birth rates in almost all
parts of the globe. Many demographers now project global population, currently
at ~5.6 billion, reaching 10 billion, stabilizing, then declining slightly
sometime in the first half of the next century. In fact, in many parts of the
industrial world, population is now declining and poses a major challenge in
the maintenance of economic growth in those nations. Although population may
only increase by 40-80% over the next century, it is the aspirations of
the global population for
economic growth and the
energy
and material resources such growth requires
that pose the greatest challenge.
Energy
and material resource demand is being substantially moderated through
efficiency in use as measured in unit of
energy
or materials used per unit of
economic product. This trend
is long-running in the industrial world and recently in the formerly centrally
planned economies and in the rest of the world. From the first steam engine in
1700 to today's best gas turbines, efficiency in
energy
use has increased 50-fold,
and conversion efficiencies of 85% are in sight; in lighting, efficiency has
improved by two orders of magnitude in the past 150 years (Figure
1).
Energy
use per unit of economic activity has been reduced by well over half in the
industrial nations this century and by the end of the next should be only one-quarter
of today's level and may be much less (Figure 2). The rest of the world should
follow in similar progression.
Efficiency
has come not only in use ,and conversion but also from the
energy
mix with the
long-term movement to higher hydrogen content fuels (Figure
3). The global
energy
mix is now entering the methane economy and should be, with
extrapolation of the long-term trend, in a hydrogen economy by the middle of
the next century, with the source of hydrogen from natural gas, a nonfossil
energy
source, or both. The long-term relentless drive for
energy
efficiency,
driven by economic forces, carries with it a substantial decarbonization of
fuel consumption. Carbon intensity of the world's
energy
mix has been
declining at an average annual rate of 0.3% over the long term; by 2050 it
should be 50% lower than now and with the advent of the hydrogen economy
probably much lower (Figure 4). Another well-established trend, one also
driven by technology and market forces, is what is termed dematerialization,
in which needs are met through technologies and systems requiring less
energy
input. Heavier materials are being substantially replaced by lighter weight
materials; recycling of materials is expanding rapidly, especially recycling
of metals, and generally involves less
energy
use and less environmental
impact.
Finally,
a notable trend essential to meeting requirements and enhancing economic
growth is in the cost of
energy
and material resources to the world's
consumer. Efficiencies, even in the face of depletable resources, have led to
real decline in commodity
prices of
energy
and mineral materials over the long term. The price of
gasoline, as an example of a pervasively used commodity, has declined 80%
since 1920, discounting a couple of aberrations. Gasoline benefits from efficiency
in oil finding and production, now the highest in history, and efficiencies in
refining, which now, even with strong environmental regulations in place,
are at all-time highs.
Most
of these basic, long-term trends-use efficiency, resource finding and
development efficiency, environmental cleanness, declining commodity prices,
and dematerialization, along with anticipated population stabilization-are
positive, lessening both environmental and resource impacts. All are driven by
technology and human ingenuity, in turn driven in most cases by market forces.
They are sure to be maintained and likely to be enlarged. Even so, with
conservative population growth and maintenance of historical levels of economic
growth, future demand levels for
energy
and material resources will be very
large.
Figure
1: Historical trends in
energy
conversion efficiencies (from Ausubel, 1996).
Figure
2: Trends and projections in
energy
use intensity (from Bookout, 1989). BoE,
barrels of oil equivalent.
Figure
3: Ratio of hydrogen (H) to carbon © for global primary
energy
consumption
since 1860 and projections for the future (from Ausubel, 1996).
Figure
4: Carbon intensity of global
energy
consumption. tC, tons of carbon; toe,
tons of oil equivalent (from Ausubel, 1996).
GLOBAL
ENERGY
REQUIREMENTS
Global
economic growth over the past 100 years has averaged ~3% yearly, with
several ups and downs.
Energy
has clearly been
the driver for this economic growth. So far, nearly 1.8 trillion barrels of
oil equivalent in total
energy
has been consumed in the world, and beyond the
traditional biomass, 90% has been the fossil fuels and 90% has been consumed
this century.
What
will the twenty‑first century require? Specifically in the case of
energy
requirements, Dupont-Roc and Khor (1994) of Royal Dutch Shell's
Corporate Centre laid out two contrasting scenarios that give a measure of the
twenty-first century global
energy
requirements (Figure
5). Both scenarios
assume adequate
energy
resources to support a continuing world economic growth
of 3% per year, the same growth rate as that achieved over the last 100 years.
Population growth is assumed to follow the World Bank base case, reaching 8.5
billion by 2030 and stabilizing at some 10-12 billion in the second half of
the next century, as economic development progresses. By 2060, the world
average Gross Domestic Product (GDP) per capita would reach $17,000, similar
to today's level in the United Kingdom, and approximately four times the
current global GDP per capita level.
One
of the Shell scenarios is what they call "sustained growth."
Abundant
energy
is produced at competitive prices, growth paths of this
century continue, and
energy
demand per capita, ~4 barrels of oil equivalent (boe)
at the beginning of the century and 13 today, goes to 25 boe by 2060, roughly
Japan's level of demand today, and to 54 boe by the end of the twenty-first
century. A second scenario is what they call "dematerialization," in
which needs are met through
technologies and systems requiring much less
energy
input. Per capita demand
moves only to 15 boe by 2060 and to 19 boe by the end of the next century. The
key difference is pace of
energy
use efficiency. Under sustained growth,
energy
demand growth of 2%o supports an economic growth rate of 3%. This
sustained growth calls for an increase in
energy
efficiency of ~1%
yearly, or what the United
States has managed in the twentieth century. Under dematerialization,
efficiency gradually increases to 2%, a rate achieved in the past but only for
relatively short periods. The difference in the two scenarios is profound as
regards to the long-term demand for
energy
. Under sustained growth, annual
energy
demand reaches 250 billion boe by 2060, four times the current level,
and ~540 billion boe per year (assuming a world population of 10 billion) by
the end of the twenty-first century as per capita consumption increases. By
contrast, the dematerialization scenario, showing the massive impact of
increased efficiency in
energy
use, increases to 150 billion boe by 2060 and
only 190 billion boe by the end of the next century, approximately one-third
of the sustained growth century-end requirement. Either way, the twenty-first
century
energy
requirements are huge, some 15 trillion boe under
dematerialization and >25 trillion boe under the sustained growth scenario.
As reference, these volumes are 10 to more than 15 times the total
energy
consumption of mankind to date.
Where
will
energy
in such volumes come from? The vast bulk of historical supply has
been and is today from fossil fuels, so-called nonrenewable resources-oil,
gas, and coal-with smaller amounts from nonfossil fuel resources such as
nuclear
power, hydropower, and wood, among others. Most analysts see fossil
fuels continuing to supply much of world
energy
needs for at least the next
two, and more likely, the next five decades, providing a transition, sooner or
later, to a new way of
energy
transformation.
Figure
5: Contrasting scenarios of global
energy
requirements for the twenty-first
century (from Dupont-Roc and Khor, 1994). cap, per capita.
Can
the traditional
energy
resources meet the huge demands of the next century?
And if they can, what role should they play?
Oil
Foremost
in consideration is oil, the world's transportation fuel and its most relied
upon
energy
resource, making up 40% of the total
energy
demand. The argument
about how much oil exists or remains to be found and developed has been
around, with varying intensity, since the first barrel was discovered. It
continues today. Recent estimates of ultimate recoverable conventional oil
vary by a factor of two, from as little as 1.8 trillion barrels, with 900
billion barrels remaining, to 3.8 billion barrels (Figure
6). Those with the
lower estimates tend to discount the generally reported proved reserves of 1.1
trillion barrels, contending they are politically overstated. They discount or
disregard reserve growth, the addition of new reserves in older, existing
fields by drilling based on new technologies and concepts of unrecovered
mobile oil and one of the most remarkable trends of the past 20 years,
contending such potential reserves are already accounted for in calculations
of proved reserves. Furthermore, they observe crude oil discovery levels of
the past 20 years, expectedly low in a period of very low oil prices and
during a period of emphasis on reserve growth strategies, and conclude that
future discovery volumes must be quite low. Accordingly, these analysts
generally predict a near-term peaking of conventional oil production. A recent
example is Campbell and Laherrère (1998), who projected peaking of
conventional oil production over the next decade, possibly within as little as
5 years, after which global oil production would decline at an average annual
rate of ~3.8% (Figure 7). Campbell earlier this decade (1991) predicted
peaking over this current
decade at a level lower than that currently predicted by Campbell and Laherrère
(1998).
Analysts predicting near-term peaking generally use the symmetrical life cycle method of Hubbert (1982). This method assumes that the amount of oil to be recovered is known and that the peak in production will come at the midpoint of the total recoverable resource volume. The volume of oil ultimately to be discovered and developed is impacted but little by technology and economics. As a matter of record, the estimate of the amount of recoverable oil is dynamic, and over time it has tended to increase primarily with new technologies and new exploration and development concepts. Furthermore, there is no technical justification from examining production histories that midpoint in exhaustion of the resource represents peak production, or vice versa. Those analysts calculating larger ultimate recoverable volumes of hydrocarbons tend to emphasize the role of technology and new concepts in enlarging the recoverable resource base. Field reserve growth, for example, is a critical element of reserve additions, especially in complex reservoirs where new sensing technology such as 3-D seismic permits better understanding of reservoirs and permits fuller exploitation of the field. In many reservoirs, less than half of the movable oil originally contained is drained with existing levels of development. Entirely new trends and provinces are accessed by technology, most notably in recent years the ultradeep-water provinces of the Atlantic and the Gulf of Mexico.
The U.S. Geological Survey has noted (1997) that over the 12-year period from 1981-1993 when they have made assessments, identified global oil reserves increased by 379 billion barrels; over that same period, 254 billion barrelswas removed from reserves in the form of production, so that a total of 633 billion barrels was added to reserves (Figure 8). Reserves were thus added at a rate 2.5 times that of production during the period. Approximately 80% of the total additions were from reserve growth in existing fields.
Emphasizing the role of technology on the oil and gas resources base worldwide yields estimates of ultimately recoverable oil in excess of 3.8 trillion barrels with >3.0 trillion barrels of conventional oil remaining. Proved reserves make up 1.1 trillion barrels, future discovery potential is estimated to be 1.0 trillion barrels, and future reserve growth is estimated to be 950 billion barrels (Table 1). Nonconventional resources of oil, including tar sands, very heavy oils, and shale oil, add substantially to the global resource base.
Table
1. Estimated global oil and natural gas accounts.
Natural Gas
Certainly one of the most dramatic examples of the role of technology has been the changed perception of the natural gas resource base in the United States. As recently as the early 1980s, the natural gas resource base of the United States was widely judged to be near exhaustion. Production was in sharp decline, and by statute, certain uses of natural gas were prohibited. Prices were projected to increase several-fold while production was projected to continue in decline. Over the past 15 years, during a period of low gas prices, vigorously developed and applied technology along with some changed concepts on the residency and recovery of natural gas has vastly changed the perception. Natural gas is now widely viewed as a plentiful and abundant resource, with estimates of the amount remaining to be found and developed an order of magnitude greater (Figure 9). Forward projections of wellhead prices in real terms are now essentially flat through the next decade. Production, once projected to fall drastically, is now projected by many industry and governmental analysts to reach levels over the next 15 years 50% greater than the previous peak in production. Ultimately recoverable natural gas resources are estimated to be nearly 28,000 trillion cubic feet (Tcf), with nearly 26,000 Tcf remaining. Of this, current proved reserves account for nearly 6000 Tcf; nonconventional resources., 5000 Tcf; tobe-discovered conventional resources, 12,000 Tcf; and estimated future reserve growth, 3000 Tcf. The near-at-hand technology to convert natural gas to middle distillate liquids for easy transport makes much of the global oil and natural gas resource base interchangeable. The total oil and gas resource base is estimated to be 7.3 trillion boe, a volume some six times greater than total global consumption to date.
Figure
9: Estimates of remaining natural gas in the United States.
Coal
The other traditional fossil fuel, of course, is coal; it represents ~30% of both current and historical fossil fuel consumption. Proved reserves of coal exceed 5 trillion boe, and
the
total technically recoverable resource base is on the order of 23 trillion boe.
A number of constraints exist to recovery of the full resource base or even a
major portion of it, but by any measure the coal resource is huge. Global coal
production, although significant, has grown only ~2% over the past 15 years.
However, it is projected by
Energy
Information Administration (1998) to
increase 67% by 2020, with 95% of the projected growth in China (80%), India
(8%), and the United States (7%).
Nuclear
and Hydropower
Nuclear
power and hydropower, both used almost exclusively for electrical power
generation, make up nearly 10% of primary
energy
consumption. Both have a
continuing role in the world's
energy
supply. Even with the eventual large-scale
introduction of the largely intermittent renewable
energy
sources, baseload
backup will be required, and
nuclear
and hydropower could meet such
requirement.
Nuclear
power carries with it what has become an almost
intractable problem of waste disposal. Uranium resources are adequate to keep
the present fleet of world reactors in operation through the middle of the
next century. There are new breeder reactor technologies that could overcome
many of the problems associated with uranium supply and radioactive waste
disposal, but the high projected investment costs and huge additional
development and demonstration costs make the future of breeder reaction
technology uncertain (Linden, 1998). Hydropower has all the desirable
attributes of a baseload renewable power source but faces growing resistance
by the environmental community both in the industrial world, where potential
is limited, and in the developing world (Linden, 1998).
TRADITIONAL FUELS IN TRANSITION
Proved
or developable resources of traditional fuels, especially the fossil fuels and
including conventional oil resources, are adequate to supply
energy
needs
throughout the transition to new methods of developing
energy
sources. There
is sufficient conventional oil and gas to maintain the historical role of the
fuels throughout the next century under Shell's dematerialization scenario.
Even under the sustained growth scenario, oil and gas could maintain its role
through most of the first half of the next century, although the total oil and
gas resource base is barely 30% of the total
energy
requirement for sustained
growth throughout the entire century. Among the fossil fuels, there is ample
coal to make up the balance of needs even for the sustained growth scenario.
But exhausting the fossil fuel base, especially coal, is not likely. In many
cases for coal, the methane trapped in certain deposits may well prove more
important than the coal itself.
FOSSIL FUELS AND THE ISSUE OF GLOBAL WARMING
In
weighing the role of traditional fuels, especially the fossil fuels, as
transition
energy
sources, al major current controversy lies in the issue of
global warming and the significance of burning hydrocarbons as causative. The
issue of global warming as the result of anthropogenic emission of carbon
dioxide is much debated and largely unresolved. Furthermore, whether a warmer
Earth, whatever the cause, is good or bad is likewise not resolved. But in
regard to the issue, Linden (1998) has made some interesting calculations and
observations. The proved reserve base of fossil fuels contains ~1130 gigatons
of carbon (GtC), and the total resource base contains slightly >5000 GtC,
~85% of which is tied up in coal (Table 2). The Intergovernmental Panel on
Climate Change (IPCC) business-as-usual scenario projects carbon dioxide
concentrations in the atmosphere reaching 800 ppmv by 2085 and triple the
pre‑industrial level of 280 by 2100. For the century, total carbon
emissions would amount to 2190 GtC, less than halt the fossil fuel base
content. Stabilizing the atmospheric concentration of carbon dioxide at twice
the pre-industry level, say ~550 ppmv, is considered by many to be reasonable
and, according to the IPCC estimates of climate sensitivity on doubling of
atmospheric carbon dioxide, gives an equilibrium temperature increase of only
~1.6°C. This concentration calculates to a next century emission of ~1000 GtC.
That level of emission would allow depletion of the entire estimated natural
gas and oil resource base over the next century and further permit the current
level of global coal production for the next 100 years. By these calculations
of Linden (1998), utilization of the fossil fuels, with the certain reliance
on natural gas, as transition fuels does not pose a problem. But the real
driver in historical
energy
use and assuredly the driver of the next century
is efficiency-efficiency driven by market forces. The historical direction is
toward a hydrogen economy-less carbon-with the initial source of hydrogen
methane and subsequently from noncarbon sources.
RENEWABLE
ENERGY
SOURCES
The
so-called renewable
energy
sources-biomass, wind, solar, among others-will
play a critical and increasingly important role into the next century, despite
the intermittent character of many of them. The eventual transition from the
traditional sources will require a new
way of
energy
transformation, possibly
nuclear
fusion. The new
energy
source,
as commonly envisioned, would allow the cheap production of electricity, which
in turn would be used to produce liquid hydrogen from water instead of natural
gas. Timing of this new
energy
source is probably not before the middle of the
twenty-first century, but it could be earlier.
CONCLUSIONS
The
challenge of supplying the
energy
and material resources for a growing, more
affluent world population and reconciling associated economic growth with
environmental and other societal needs is huge. There is plenty in human
history, especially the demonstrated human ingenuity to develop the technology
and concepts and to apply them rigorously and as needed, to indicate the
challenge can be met.
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Ausubel, J. H. (1996). Can technology spare the earth'? Am Sci, 84, 166-178.
Bookout,
J. F. (1989). Two centuries of fossil fuel
energy
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Campbell, C. J. (1991). The golden century of oil: 1950-2050: The depletion of a resource. Boston: Kluwer Academic Publishers.
Campbell, C. J., and Laherrère, H. (1998). The end of cheap oil. Sci Am, March, 1998, 78-83.
Dupont-Roe,
G., and Khor, A. (1994). The evolution
of the world's
energy
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Centre.
Energy
Information Administration (1998). International
energy
outlook. U.S. Department of
Energy
Publication No. DOE/EIA-0484(98).
Washington, DC: U.S. Department of
Energy
,
Energy
Information Administration.
Hubbert, M. K. (1982). Techniques of prediction as applied to the production of oil and gas. In S. I. Gass, (Ed.), Oil and gas supply modeling: proceedings of a symposium (pp. 16-141). Washington, DC: National Bureau of Standards Special Publication 631.
Linden,
H. R. (1998). Achieving sustainability-Sprint or marathon. In Proceedings
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the Aspen Institute
Energy
Forum. Aspen, CO.
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ABOUT THE AUTHOR
William L. Fisher
William L. Fisher is the Leonidas T. Barrow Centennial Chair in Mineral Resources and Director of the Geology Foundation at The University of Texas at Austin. He is the former Director of the Bureau of Economic Geology and former Chairman of the Department of Geological Sciences. Dr. Fisher is a long-time adviser to state and federal officials and testifies frequently to the U.S. Congress. He lectures extensively and has published more than 200 articles, reports, and books.
Dr.
Fisher is a member of the National Academy of Engineering and currently serves
on the National Petroleum Council, the Advisory Council of the Gas Research
Institute, and the board of Pogo Producing Company. He is a former member of
the White House Science Council, The President's Council of Advisors on
Science and Technology,
Energy
Research Panel, and the Secretary of
Energy
Advisory Board. Dr. Fisher is a member of the Board on
Energy
and
Environmental Systems and past Chairman of the Board on Earth Sciences and
Resources of the National Academy of Sciences. He is past president of the
American Association of Petroleum Geologists, the American Geological
Institute, the American Institute of Professional Geologists, the Association
of American State Geologists, the Gulf Coast Association of Geological
Societies, and the Austin Geological Society. Dr. Fisher is a Fellow and
former Councilor of the Geological Society of America. He is the recipient of
the Powers Medal (AAPG), the Parker Medal (AIPG), the Campbell Medal (AGI),
and the Hedberg medal (ISEM).
Dr.
Fisher served as Assistant Secretary of the Interior for
Energy
and Minerals
and as a member of the White House
Energy
Resources Council during the Ford
Administration. He holds a B.S. and D.Sc. (Hon.) from the Southern Illinois
University and an M.S. and Ph.D. in Geology, University of Kansas.