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The green revolution has modified natural ecosystems into a highly simplified and nutrient-rich state. A handful of plants, bred into entirely new strains, have become the dominant plants on the planet. The four main grain crops wheat, rice, maize and barley occupy a total of some 500 million hectares1, mostly in those countries with the highest populations. The green revolution was not all good, however. It spread a farming method that relies heavily on chemical fertilizers, monocultural cropping practices and decreased fallow times, coupled with more intensive plowing. Local water supplies became degraded and crop diversity decreased, leading to land degradation and erosion. Concern has increased over the implications of pests that thrive on now dominant strains of grain and maize. Chemical applications to fields have soared. The doubling of agricultural production during the past 35 years has required a 600 percent increase in nitrogen fertilizer and a 250 percent increase in phosphate fertilizer. This has been accompanied, over the same period, by a 70 percent increase in irrigated cropland, but only a 10 percent increase in the area of cultivated land2. One immediate effect of such high fertilizer use is that human activity has taken over from nature as the dominant source of fixed nitrogen in the environment. Natural sources from soil bacteria, algae and lightning release 140 million tons of fixed nitrogen a year; human sources now total 210 million tons per year, of which 86 percent comes from agricultural activity, with fertilizer responsible for most of it3. More than half of all the commercial fertilizer ever produced has been applied to fields since 1984. However, largely because of widespread overuse, a half of that application never reached plant tissue, but evaporated or washed into rivers. The result has been a nitrogen overload of natural ecosystems, particularly in Western Europe and East Asia, where average annual applications on arable land are highest4. Application rates generally reflect wealth or the pressure in densely populated countries to raise food production.
Changes caused by nitrogen overload range from the seemingly harmless, such as the spread of nettles in English hedgerows, to toxic algal blooms in lakes, rivers and coastal waters, resulting from a process called eutrophication, and the leaching of key nutrients such as calcium and magnesium from soils5. In addition, nitrogen evaporation from soils (along with methane emissions from rice paddies) is contributing to global emissions of greenhouse gases. Worldwide pesticide use has also soared, reaching 5 million tons annually6.
Three quarters of pesticides, predominantly herbicides, are applied in
Europe, North America and Japan, where farmers can most easily afford
them. In tropical developing countries the greatest need is for the more
toxic broad-spectrum insecticides, largely applied to export crops such
as cotton, bananas and coffee. In such export crop plantations, acute
pesticide poisoning can affect 10 percent of the workforce7.
But the pesticide poison cycle reaches further. Pesticides evaporate into
the atmosphere at the point of use and circulate the planet, eventually
distilling out in the chill air of the Arctic where they poison polar
bears, whales and even humans. Hectare for hectare, most irrigated land is more productive
than rainfed land, and in some regions, such as the Nile delta and the
Sind in Pakistan, it is essential to crop production. The amount of irrigated
land worldwide has tripled since 1950 to cover 270 million hectares, accounting
for more than a third of the global harvest8.
Most of this is in densely populated regions of Asia, where it allows
two or three crops a year, and in the Middle East, where without it there
would be virtually no agriculture. In many parts of the world, countries
are reaching absolute limits of the availability of water (much as they
did with farmable land 40 years ago) and must improve the efficiency of
its use if they are to raise production. Increases in large stands of monoculture crops have had
important ecological consequences. With this type of cultivation the range
of plant pests becomes less diverse, but more abundant, reflecting the
plants themselves. Organic matter in the soil is lost, altering the soil
biota and generally involving a loss of soil fertility. These changes
increase the need for pesticides and fertilizers and, combined with the
physical impacts of erosion, cause soil degradation. Croplands tilled and then left without the protective
cover of vegetation are particularly vulnerable to soil loss through wind
and water erosion. Worldwide an estimated 12 million hectares of croplands
fall out of use for this reason each year. Economists have estimated the
value of this lost soil, in terms of nutrients and water-holding capacity,
at about US$400 billion a year9.
Erosion rates are highest in Asia, Africa and South America, estimated
at typically 30 or 40 tons per hectare annually, while about half that
amount is being lost in Europe and North America10.
The high rates reflect poor land management, poverty and the cultivation
of marginal and sloping land, as well as population density and the resulting
pressure to cut fallow periods and grow several crops a year. Land is
also degraded by salinization generally as a result of the waterlogging
of irrigated land, which can bring salts to the surface, forming a white
crust toxic to most plants. The rate of soil degradation raises questions about the long-term sustainability of yield increases without a rising tide of inputs11, while concern for sustainability has increased interest in new methods of farming, based on lower inputs and greater attention to ecological principles using local knowledge and natural biological means of pest control12. Typical methods include using organic fertilizer from farm animals and
planting leguminous crops to fix nitrogen in the soil, growing plants
that repel pests, protecting soils by terracing and reducing tillage,
and harvesting rainwater in arid regions.
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Copyright AAAS 2000. |