A Computer Research Program For Solving The Reaction Rate Equations In The E Ionospheric Region PDF Download

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A Computer Program for Solving the Reaction Rate Equations in the E Ionospheric Region

A Computer Program for Solving the Reaction Rate Equations in the E Ionospheric Region
Author: Thomas J. Keneshea
Publisher:
Total Pages: 88
Release: 1962
Genre: Ionosphere
ISBN:

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In studies of the mechanisms responsible for the formation of the ionized regions of the atmos phere, one of the problems encountered is the solution of the set of differential equations describing the time dependence of the number density of the chemical species present. For simple cases where only one or two species are involved, there is no particular problem. When all the important constituents are included, however, the solution of these equations becomes very complex. A computer technique is pre sented that will solve any size set of these differential equations involving any number of chemical reactions. (Author).


Atmospheric Transport Processes

Atmospheric Transport Processes
Author: Elmar R. Reiter
Publisher:
Total Pages: 392
Release: 1971
Genre: Dynamic meteorology
ISBN:

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Environmental Research Papers

Environmental Research Papers
Author:
Publisher:
Total Pages: 166
Release: 1967
Genre: Environmental geology
ISBN:

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Report on Research at AFCRL.

Report on Research at AFCRL.
Author: Air Force Cambridge Research Laboratories (U.S.)
Publisher:
Total Pages: 264
Release: 1962
Genre: Geophysics
ISBN:

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A Technique for Solving the General Reaction-rate Equations in the Atmosphere

A Technique for Solving the General Reaction-rate Equations in the Atmosphere
Author: T. J. Keneshea
Publisher:
Total Pages: 158
Release: 1967
Genre: Atmosphere
ISBN:

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With the availability of numerical techniques for solving an extensive set of nonlinear differential equations and high-speed computers for performing the calculations, interest in solving the unrestricted reaction-rate equations is growing among ionospheric researchers. In view of this a refinement is given of the techniques previously developed in PB-163 071 and AD-424 173. The computer code is written to solve the photochemical behavior of 15 atmospheric species; these species are electrons, O( - ), O2( - ), O3( - ), NO2( - ), O(+), O2(+), N2(+), NO(+), NO, N, NO2, O3, N2O, and O. Built into the code are 168 reactions that can conceivably take place among these constituents. Several examples of the results obtained using the code are presented, including the buildup of ionization from zero concentrations at altitudes in the D and E regions and the deionization of an atmosphere with high initial electron densities. The diurnal variation of the atmospheric constituents is also presented along with profiles for the above-mentioned species from 60 km to 120 km. The computer codes are included in their entirety with complete explanations on their usage. (Author).


OAR Quarterly Index of Current Research Results

OAR Quarterly Index of Current Research Results
Author: United States. Air Force. Office of Aerospace Research
Publisher:
Total Pages: 800
Release: 1959
Genre: Aeronautics, Military
ISBN:

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A Solution to the Reaction Rate Equations in the Atmosphere Below 150 Kilometers

A Solution to the Reaction Rate Equations in the Atmosphere Below 150 Kilometers
Author: Thomas J. Keneshea
Publisher:
Total Pages: 142
Release: 1963
Genre: Chemical kinetics
ISBN:

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One way to acquire a better understanding of the formation and destruction of ionization in the atmosphere is through the solution of the system of time-dependent reaction rate equations. These ordinary differential equations form a simultaneous set each question of which describes the time rate of change of a particular atmospheric constituent. In the general problem, all the molecules and atoms whether neutral, charged, or excited, as well as the free electrons would be included. A computer program is presented for developing the numerical solution to this problem. The method of solution of the set of equations uses a fourth order Runge Kutta integration with a variable mesh. When a species enters its quasi-equilibrium state, its differential equation is removed from the set and its equilibrium equation is inserted into the simultaneous algebraic set. The algebraic set is solved by the method of successive substitutions. The over-all solution is obtained by iteration between the differential and the algebraic sets. The ability of the computer program to develop extensive solutions is demonstrated by several examples taken under different conditions.