Author: Lee W. Parker
Publisher:
ISBN:
Category : D region
Languages : en
Pages : 132
Book Description
The theory of ion collection at the center of a moving electrically charged blunt-electrode (probe) in the ionospheric D region is considered at high velocities such that the boundary layer is thin. The stagnation-point boundary-layer analysis of Sonin (1967) is reviewed where diffusion, mobility, and convection are coupled within the thin boundary layer at infinity Debye length. A critical parameter is the ion Péclet number P, which is essentially equal to the flow Reynolds number. When the voltage is large compared with (kT/e) square root P, the attracted-ion current is given by the simple linear mobility relation where the current is proportional to the voltage, independent of the flow. Associated with this proportionality is the fact that the attracted-ion concentration is the same at the edge of the boundary layer as it is at infinity. At finite Debye length, the current can depend on the flow and can depend nonlinearly on the voltage. The nonlinearity is associated with a reduction in the attracted-ion concentration at the edge of the boundary layer, due to the presence of space charge. A charge-layer model is used for the space-charge analysis in which the layer (or sheath) is assumed thick compared with the boundary layer but thin compared with the probe radius. Diffusion is neglected, but convection and mobility are included. The nature of the repelled particles must be considered. If the repelled particles are ions, the linear mobility current-voltage relation holds for a restricted range of voltages, independent of the flow. For higher voltages, the relation becomes nonlinear and depends on the flow.
Theory of Ion Collection in the D-region by a Rapidly Moving Blunt Probe Or Mass Spectrometer
Author: Lee W. Parker
Publisher:
ISBN:
Category : D region
Languages : en
Pages : 132
Book Description
The theory of ion collection at the center of a moving electrically charged blunt-electrode (probe) in the ionospheric D region is considered at high velocities such that the boundary layer is thin. The stagnation-point boundary-layer analysis of Sonin (1967) is reviewed where diffusion, mobility, and convection are coupled within the thin boundary layer at infinity Debye length. A critical parameter is the ion Péclet number P, which is essentially equal to the flow Reynolds number. When the voltage is large compared with (kT/e) square root P, the attracted-ion current is given by the simple linear mobility relation where the current is proportional to the voltage, independent of the flow. Associated with this proportionality is the fact that the attracted-ion concentration is the same at the edge of the boundary layer as it is at infinity. At finite Debye length, the current can depend on the flow and can depend nonlinearly on the voltage. The nonlinearity is associated with a reduction in the attracted-ion concentration at the edge of the boundary layer, due to the presence of space charge. A charge-layer model is used for the space-charge analysis in which the layer (or sheath) is assumed thick compared with the boundary layer but thin compared with the probe radius. Diffusion is neglected, but convection and mobility are included. The nature of the repelled particles must be considered. If the repelled particles are ions, the linear mobility current-voltage relation holds for a restricted range of voltages, independent of the flow. For higher voltages, the relation becomes nonlinear and depends on the flow.
Publisher:
ISBN:
Category : D region
Languages : en
Pages : 132
Book Description
The theory of ion collection at the center of a moving electrically charged blunt-electrode (probe) in the ionospheric D region is considered at high velocities such that the boundary layer is thin. The stagnation-point boundary-layer analysis of Sonin (1967) is reviewed where diffusion, mobility, and convection are coupled within the thin boundary layer at infinity Debye length. A critical parameter is the ion Péclet number P, which is essentially equal to the flow Reynolds number. When the voltage is large compared with (kT/e) square root P, the attracted-ion current is given by the simple linear mobility relation where the current is proportional to the voltage, independent of the flow. Associated with this proportionality is the fact that the attracted-ion concentration is the same at the edge of the boundary layer as it is at infinity. At finite Debye length, the current can depend on the flow and can depend nonlinearly on the voltage. The nonlinearity is associated with a reduction in the attracted-ion concentration at the edge of the boundary layer, due to the presence of space charge. A charge-layer model is used for the space-charge analysis in which the layer (or sheath) is assumed thick compared with the boundary layer but thin compared with the probe radius. Diffusion is neglected, but convection and mobility are included. The nature of the repelled particles must be considered. If the repelled particles are ions, the linear mobility current-voltage relation holds for a restricted range of voltages, independent of the flow. For higher voltages, the relation becomes nonlinear and depends on the flow.
Nuclear Science Abstracts
Author:
Publisher:
ISBN:
Category : Nuclear energy
Languages : en
Pages : 658
Book Description
Publisher:
ISBN:
Category : Nuclear energy
Languages : en
Pages : 658
Book Description
Monthly Catalog of United States Government Publications
Author:
Publisher:
ISBN:
Category : Government publications
Languages : en
Pages : 2834
Book Description
Publisher:
ISBN:
Category : Government publications
Languages : en
Pages : 2834
Book Description
A Portable, Frequency-coherent Spectrum Analyzer for Radar Applications
Author: Ben B. Balsley
Publisher:
ISBN:
Category : Coherent radar
Languages : en
Pages : 544
Book Description
Publisher:
ISBN:
Category : Coherent radar
Languages : en
Pages : 544
Book Description
Monthly Catalog of United States Government Publications, Cumulative Index
Author: United States. Superintendent of Documents
Publisher:
ISBN:
Category : United States
Languages : en
Pages : 1466
Book Description
Publisher:
ISBN:
Category : United States
Languages : en
Pages : 1466
Book Description
NOAA Technical Report ERL.
Author:
Publisher:
ISBN:
Category :
Languages : en
Pages : 632
Book Description
Publisher:
ISBN:
Category :
Languages : en
Pages : 632
Book Description
AL.
Author:
Publisher:
ISBN:
Category : Atmosphere, Upper
Languages : en
Pages : 776
Book Description
Publisher:
ISBN:
Category : Atmosphere, Upper
Languages : en
Pages : 776
Book Description
Meteorological & Geoastrophysical Abstracts
Author:
Publisher:
ISBN:
Category : Cosmic physics
Languages : en
Pages : 920
Book Description
Publisher:
ISBN:
Category : Cosmic physics
Languages : en
Pages : 920
Book Description
Meteorological and Geoastrophysical Abstracts
Author:
Publisher:
ISBN:
Category : Cosmic physics
Languages : en
Pages : 710
Book Description
Publisher:
ISBN:
Category : Cosmic physics
Languages : en
Pages : 710
Book Description
NOAA Technical Report ERL.
Author: United States. National Oceanic and Atmospheric Administration
Publisher:
ISBN:
Category :
Languages : en
Pages : 132
Book Description
Publisher:
ISBN:
Category :
Languages : en
Pages : 132
Book Description