FIELD: measurement technology.
SUBSTANCE: invention relates to methods for determining the composition and concentration of positive ions in the Earth's ionosphere. Method for determining the atomic mass of metal ions in a sporadic layer E (Es) includes formation of artificial periodic inhomogeneities of ionospheric plasma, radiation in the ionosphere of probing pulses at the stage of disappearance (relaxation) of artificial periodic inhomogeneities, reception of a signal back scattered by artificial periodic inhomogeneities of the ionospheric plasma, measurement of amplitude and determination of the relaxation time of the backscattered signal as a function of the height h. By decreasing the amplitude of the backscattered signal by e times, at each height, the relaxation time of the inhomogeneities τ(h), which in absence of a sporadic layer E (Es) is due to ambipolar diffusion with a characteristic time τd(h), and for existence of a sporadic layer E (Es) – diffusion with a characteristic time τEs(h), and with respect to times τEs(h) and τd(h) determine the atomic mass or type of metallic ions in the sporadic E (Es).
EFFECT: possibility of remote radiophysical determining of the atomic mass of positive metal ions prevailing in the sporadic layer E (Es) of the ionosphere, id est determination of the type of ions that form this layer, with a significant reduction in the cost of conducting measurements compared with other methods and high accuracy in determining the height of the ion layer.
1 cl, 3 dwg
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Authors
Dates
2018-07-05—Published
2017-06-19—Filed