
Such terracing provides a very high level of soil conservation but is possible only
where labor is cheap. On lesser slopes, by ploughing and cultivating in strips along
the contours, runoff of soil can be significantly reduced.
Agricultural land is also highly susceptible to degradation in arid and semiarid
regions. Both overgrazing and excessive cultivation expose the soil directly to ero-
sion by the wind and to rare but fierce rainstorms. In the process of ‘desertization’,
land that is arid or semiarid but has supported subsistence or nomadic agricul-
ture gives way to desert. The process has often been slowed down for a time by
irrigating the land. This gives a temporary remission but lowers the water table
and salts accumulate in the topsoil (salinization). Once salts have started to
accumulate, the process of salinization tends to spread and leads to an expansion
of sterile, white salt deserts. This has been a particular hazard in irrigated areas
of Pakistan.
Forests protect soil from erosion because the canopy absorbs the direct impact
of the rain on the soil surface, the perennial root systems bind the soil and leaf
fall continually adds organic matter. But when forests are clear felled and then
replanted, there is an open ‘window of opportunity’ for soil erosion until the
forest canopy closes again. Cultivation and replanting along contours gives some
control over soil erosion during this danger period, but the best precaution is to
avoid clear felling and extract only a proportion of a forest stand at each harvest.
This can often be technically difficult and more expensive.
12.4.2 The sustainability of water as a resource
In the 1960s and 1970s, the main worry about the sustainability of global resources
concerned energy supplies that were recognized to be finite and exhaustible.
While energy resources remain finite, concern has shifted because exploration
has revealed much larger reserves of oil, gas and even coal than had been entered
into earlier environmental balance sheets. Water has now come into sharper focus.
Fresh water, which is used in crop irrigation and for domestic consumption, is of
crucial importance. On a global scale, agriculture is the largest consumer of fresh
water, taking more than 70% of available supplies and more than 90% in parts
of South America, central Asia and Africa.
There is a fixed stock of water on the globe and it is continually recycled as
it evaporates from vegetation, land and sea and is then condensed and redis-
tributed as precipitation. The human species now uses, directly or indirectly,
more than half of the world’s accessible water supply. The fresh water avail-
able per capita worldwide fell from 17,000 m
3
in 1950 to 7300 m
3
in 1995
and there is very considerable variation in availability from region to region
(Figure 12.14). Many assessments of the problems of water supply suggest that
countries with less than 1000 m
3
per person per year experience chronic scarcity.
Water is widely thought to be the resource that future wars will be fought over.
Even at a national level, the allocation of water resources can cause political
problems, as occur for example in conflicts in California between urban and
agricultural demands for water from the Colorado River. At the international
level, conflict arises between countries that are upstream of their neighbors and
are in a position to dam and divert water supplies. There are bitter cross-border
disputes in South America, Africa and the Middle East between nations that share
river basins.
Part IV Applied Issues in Ecology
410
desertization and salinization
forests protect...but not if
harvested by clear felling
water is a finite global resource
water – the resource that future
wars will be fought over?
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