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Processes of acidification or alkalization of soils are treated,
taking the qualitative changes in soil chemistry into
consideration. Following a theoretical background of ecosystem
proton budgets, the application for assessing external and internal
acid loads are demonstrated. The chemistry of organic matter and
the oxides of aluminum, iron, and manganese are treated in the
context of being sources and sinks for acid loads in soils. Special
attention is payed to the assessment of solubility and reaction
kinetics of aluminous minerals. The formation of toxic elements in
soil solution resulting from the solubilization of inorganic oxides
as well as aspects of changes in the nutrient status of soils,
changes of fertility and processes leading to a transfer of acidity
from soils to surface are discussed.
The world needs for food and fiber continue to increase. Population
growth in the developing countries peaked at 2. 4% a year in 1965
and has fallen to about 2. 1%. However, in many developing
countries almost half the people are under 15 years of age, poised
to enter their productive and reproductive years. The challenges to
produce enough food for this growing population will remain great
Even more challenging is growing the food in the areas of greatest
need. Presently the world has great surpluses of food and fiber in
some areas while there are devastating deficiencies in other areas.
Economic conditions and the lack of suitable infrastructure for
distribution all too often limit the alleviation of hunger even
when there are adequate supplies, sometimes even within the country
itself. World hunger can be solved in the long run only by
increasing crop production in the areas where the population is
growing most rapidly. This will require increased efforts of both
the developed and developing countries. Much of the technology that
is so successful for crop production in the developed countries
cannot be utilized directly in the developing countries. Many of
the principles, however, can and must be adapted to the conditions,
both physical and economic, of the developing countries.
The world needs for food and fiber continue to increase. Population
growth in the developing countries peaked at 2. 4 percent a year in
1965 and has fallen to about 2. I percent. However, in many
developing countries almost half the people are under 15 years of
age, poised to enter their productive and reproductive years. The
challenges to produce enough food for this growing population will
remain great. Even more challenging is growing the food in the
areas of greatest need. Presently the world has great surpluses of
food and fiber in some areas while there are devastating
deficiencies in other areas. Economic conditions and the lack of
suitable infrastructure for distribution all too often limit the
alleviation of hunger even when there are adequate supplies,
sometimes even within the country itself. World hunger can only be
solved in the long run by increasing crop production in the areas
where the population is growing most rapidly. This will require
increased efforts of both the developed and developing countries.
Much of the technology that is so successful for crop production in
the developed countries cannot be utilized directly in the
developing countries. Many of the principles, however, can and must
be adapted to the conditions, both physical and economic, of the
developing countries. This series, Advances in Soil Science.
The study of soils today has taken on increased importance because
a rapidly expanding population is placing demands on the soil never
before experienced. This has led to an increase in land
degradation. Land degradation is one of the most severe problems
facing mankind. Volume 11 of Advances in Soil Science was devoted
entirely to this critical area of soil science. From the beginning
of agriculture until about 1950, increased food production came
almost entirely from expanding the cropland base. Since 1950,
however, the yield per unit of land area for major crops has
increased dramatically. Much of the increase in yields was because
of increased inputs of energy. Between 1950 and 1985, the farm
tractor fleet quadrupled, world irrigated area tripled, and use of
fertilizer increased ninefold. Between 1950 and 1985, the total
energy used in world agriculture increased 6. 9 times. Until
recently, sustainability was seldom, if ever, mentioned in
agricultural literature. Now, it is one of the most widely used
terms. The high costs ofirriga tion development, escalating energy
costs during the 1970s, public concern over potential negative
impacts of fertilizer and pesticides on water supplies, soil ero
sion, soil compaction and salinity problems, and other concerns
have caused many people to question whether many of the present
agriculture systems can be sustained. As a result, soil science is
beginning to focus more on sustaining the resource base."
Soil is formed from the physical and chemical weathering of
rocks-processes described historically becau'se they involve eons
of time-by glaciation and by wind and water transport of soil
materials, which are later deposited in deltas and loessial planes.
Soil undergoes further transformations over time and provides a
habitat for biological life and a base for the development of
civilizations. Soil is dynamic-always changing as a result of the
forces of nature and particularly by the influences of man. Soil
has been studied as long as history has been documented. Numerous
references to soil are found in historical writings such as
Aristotle (384-322 Be), Theophrastus (372-286 Be), Cato the E1der
(234-149 Be), and Varro (116-27 Be). Some of the earliest
historical references have to do with the erosional forces of wind
and water. The study of soils today has taken on increased
importance because a rapidly expanding population is placing
demands never before experienced on the soil. This has led to an
increase in land degradation. Land degradation is one of the most
severe problems facing mankind. Volume 11 of Advances in Soil
Science was devoted entirely to this critical area of soil science.
This series, Advances in Soil Science, was established to provide a
forum for leading scientists to analyze and summarize the available
scientific information on a subject, assessing its importance and
identifying additional research needs.
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