Subjects:
- Levels of organization of living matter,
2
- Populations, communities, ecosystems,
2,
3,
4,
5
- Forms of biological relationships in the community
- Positive attitude,
2
- Negative attitude,
2,
3
- Neutral attitude,
2
- Circulation of matter and energy,
2,
3,
4,
5,
6,
7,
8
- The structure of the biosphere,
2
- Evolution of the biosphere,
2,
3,
4
- The current state of the environment
- Atmosphere - the outer shell of the biosphere,
2
- Biological productivity of ecosystems,
2,
3
- Conservation and sustainable environmental futures,
2,
3,
4,
5
Environmental problems of the biosphere
- Human impact on flora and fauna,
2
- Limits of stability,
2,
3
- Natural resources and their use,
2,
3
- Radioactive contamination of the biosphere
- Contamination of soil (
contamination)
- Contamination of natural waters (
the steady,
one type)
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Symposium Introduction
Contamination of soil mercury (with toxic chemicals and waste
industrial), lead (lead smelter and from vehicles),
iron, copper, zinc, manganese, nickel, aluminum and other metals
(near major centers of ferrous and nonferrous metallurgy), radioactive
elements (as a result of rainfall from nuclear explosions or
disposal of liquid and solid industrial wastes, nuclear power stations
or research institutes associated with the study and
use of atomic energy), persistent organic compounds,
used as a pesticide. They accumulate in the soil and water, and
importantly, included in the ecological food chain: moving from the soil and water in
plants, animals, and eventually transform into a human body with food.
Inept and uncontrolled use of any fertilizers and pesticides
leads to disruption of the circulation of substances in the biosphere.
Among the anthropogenic changes in soil erosion is (from the Latin
erosio - fret). Destruction of forests and natural grass cover,
repeated plowing of land without complying with the rules of farming led to erosion
soil - the destruction of topsoil and run-off water and wind. Widely
common and most destructive water erosion. It occurs on
slopes, and develops if not cultivation. However, melting and
rainwater from the fields each year is carried away in the river and the sea, millions of tons of soil.
Wind erosion is most pronounced in the southern steppe regions of our
country. It occurs in areas with a dry bare soil, c sparse
vegetation. Overgrazing in the steppes and semi -
contributes to wind erosion and the rapid destruction of grass cover. For
restoring soil layer thickness of 1 cm in natural conditions required
250-300 years.
Considerable areas of soils formed are removed from
agricultural turnover due to open ways to develop
minerals, occurring at shallow depth.
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Division of Agriculture and Natural Resources Communication Services WebMaster and Partners :
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ANR Non-Discrimination Statement
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Organizing sponsors:
University of California
cal poly with major support and assistance from the Buy California and Specialty Crop programs of
contact email:
mail@calagsymposium.org
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