72
ENVIRONMENT, POLLUTION, DEVELOPMENT: THE CASE OF UZBEKISTAN
4.2.4. Phosphorus biogeochemical cycle
The environ mental processes and the quality of the environ-
ment depend not only on macro-elements but also on substances
that occur only in very small amounts in nature. Examples of such
substances include phosphorus, many metals and their compounds
and other
elements, such as iodine, bromine, arsenic, selenium
and others. Phosphorus is particularly important for sustaining life
processes in living organisms, as it is a component in the genetic
information carrier molecules – deoxyribonucleic acid (DNA) and
ribonucleic acid (RNA), in many proteins as well as in the molecules
responsible for cellular energy transport – adenosine triphosphate
(ATP) and adenosine diphosphate (ADP). The phosphorus cycle
(Figure 4.26) has a pivotal significance because phosphorus is often
a limiting factor for the development of living organisms, i.e. the
amount of phosphorus available for the development of organisms
determines the intensity of their growth.
Soils
Rivers
Runoff
Agricultural,
industrial,
household
utilisation
Terrestrial living
organisms
Vegetation
Production of phosphate
fertilisers and compounds
Sedimentation
Marine living organisms
Phosphate
sedimentary rocks
The phosphorus cycle differs from the cycles of other elements
(carbon, nitrogen, sulphur and others) because it does not contain
substances in gas phase as most
phosphate compounds are non-
volatile or solid. The amount of phosphorus compounds in the atmo-
sphere is small, and they are usually extracted from the litho sphere’s
sedimentary rocks in the form of various apatites (mostly in the
form of calcium phosphates) that have formed in shallow seas tens
of millions years ago. When herbivores consume plants, phosphates
Figure 4.26.
Phosphorus
biogeochemical cycle
4.
HUMANS AND THE ENVIRONMENT
73
enter the bodies of these animals. With their excrements or decay
after death phosphates are returned to the soil and waters. Part of
phosphorus compounds are bound as stable chemical compounds
in the soil and marine sediments, forming phosphate sedimentary
rocks. The natural cycling of phosphorus
com pounds is not in tense;
there fore, sedimentary rocks that contain phosphorus are con-
centrated in just a few regions of the world, and their weathering
takes place slowly.
Phosphorus compounds are predominantly (~90%) used as in-
or ganic fertilisers in agriculture. The estimated global utilisation
of fertilisers is 15 million tons per year. The second major area of
phos phorus compound utilisation is in detergents. Phosphorus com-
pounds are added to detergents as water-softeners. Just like after the
de composition
of living organic matter, virtually all areas of use of
phos phorus compounds end up with their runoff into the hydrosphere
after utilisation, intensifying the processes of eutrophication in
waterbodies. In any case, human activity has cardinally changed the
nature of phosphorus flow in its biogeochemical cycle.
References
Begon M., Townsend C., Harper J. L. (2005) Ecology.
From Individuals to
Ecosystems. Boston: Blackwell Pub.
Berner E. K., Berner R. A. (1996) Global Environment. Water, Air and
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Botkin D., Keller E. (2000) Environmental Science: Earth as a Living Planet.
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Enger E. D., Smith B. F. (2006) Environmental Science: A Study of
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ed.). Boston: McGraw Hill.
Geochemical Cycles. (1991) Chapter 23 in Inorganic Geochemistry
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Lovelock J. (2007) The Revenge of Gaia. London: Penguin Books.
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Rydén L. (ed.) (2003) Environmental Science. Uppsala: Baltic University
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Biogeochemical Cycles. Accessible:
www.enviroliteracy.org/subcategory.
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www-micro.msb.le.ac.uk/109/
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www.lep.org/.
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http://materials.wri.org/topic_data_
trends.cfm.
5. GLOBAL ENVIRONMENTAL PROBLEMS
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