By Victor G. Gorshkov
It is widely known that the biochemical procedures of existence in the world are maintained via the exterior sunlight radiation and will be diminished to the synthesis and decomposition of natural subject. guy has additional the synthesis and decomposition of assorted in dustrial items to those normal techniques. On one hand, organic synthesis may well in simple terms be performed in the fairly slender margins of parameters of the environ ment, together with temperature, humidity, concentrations of the inorganic components utilized by lifestyles (such as carbon dioxide, oxygen, etc.) nonetheless, the actual and chemical composition of our environment suffers major alterations in the course of these procedures of synthesis and decomposition. the utmost attainable expense of such switch because of the job of residing beings can exceed the typical geophysical charges of swap of our surroundings as a result of task ofterrestrial depths and cosmic strategies by way of an element usually thousand. within the absence of a inflexible correlation among the organic synthesis and decomposition, the surroundings will be enormously disturbed inside of a decade and pushed right into a country undeserving for all times. a dull Earth, in spite of the fact that may undergo related alterations merely after a few hundred thousand years. renovation of the prevailing nation of our environment is just attainable with strict equality among the charges of organic synthesis and decomposition, that's, whilst the biochemical cycles of topic are almost closed.
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Additional info for Physical and Biological Bases of Life Stability: Man, Biota, Environment
Provided the population of the planet remains at its present level or even grows, the modem standard of living available in the developed regions can only be given to every man on Earth at the cost of the complete destruction of the environment fit for life. Supporting a stable level with the natural biota and environment remaining intact is only possible for a human population that is an order of magnitude smaller than the present one. If some unused natural resources are still available, the rate of economic growth and the standard of living of the whole population may be increased if a working part of the population (labor force) is imported.
Now fluctuations, which had been rare at lower energy levels, may be permanently sustained, and fluctuations which had been extremely rare may become more frequent. If a system sustaining a stationary macroscopic process of low order is introduced to such a flux of energy, that process appears to be unstable in that flow, and within a measurable finite period of time it transforms into a more ordered stable state of dynamic equilibrium, corresponding to the average level of order in the flux of energy fed to it.
Thus any initial condition may only be described to within the margin of such errors. Forecasts of the development of such systems, following the laws of their behavior, will all contain certain ambiguities (stemming from those initial conditions). After certain systems proce~d past their threshold levels in the flux of external energy, that uncertainty begins to grow exponentially with time so that such a system may proceed from any initial to practically any final condition or state. That system will still retain its stability in the sense that all its final states will not deviate too far from its given average (will be "attracted" to a certain fixed value).