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Published byElfrieda Lloyd Modified over 6 years ago
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RESTORATION OF THE MARSIS SIGNAL FOR SUBSURFACE SOUNDING
N.A. Armand Russian academy of sciences Institute of Radio Engineering and Electronics Mokhovaya str., 11,125009, Moscow, Russia
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SIGNAL COMPRESSION
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PHASE SHIFT CAUSED BY IONOSPHERE
SIGNAL DEFINITION SIGNAL SPECTRUM PHASE SHIFT CAUSED BY IONOSPHERE WAVE NUMBER TIME RELATIVELY TO THE GROUP ONE ENERGY OF THE SIGNAL
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HIGH-FREQUENCY APPROXIMATION
DIMENSIONLESS TIME COEFFICIENT OF BROADBANDNESS DIMENSIONLESS RELAX. TIME
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Coefficient of broadbandness
IONOSPHERIC MODEL Band number 1 2 3 4 Center frequency, MHz 1.8 3.0 4.0 5.0 Coefficient of broadbandness 0.28 0.17 0.13 0.10 33.1 8.06 3.32 1.59
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DISTORTION OF THE MARSIS PULSES
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INVERSE FILTER
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RESTORATION OF THE SIGNAL
PRELIMINARY CORRECTION SECOND STEP CORRECTION
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SPLITTING OF THE SIGNAL
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COEFFICIENT OF SIMILARITY
UNIFORM SPECTRUM ARRIVAL TIME
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KOTELNIKOV’S THEOREM ARRIVAL TIME KOTELNIKOV’S HARMONICS
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UNIFORM SPECTRUM UNDISTORTED SIGNAL HAS ONLY ONE KOTELNIKOV’S COMPONENT
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DISTORTION OF THE FOURTH CHANNEL
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DISTORTION OF THE THIRD CHANNEL
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DISTORTION OF THE SECOND CHANNEL
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DISTORTION OF THE FIRST CHANNEL
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COEFFICIENT OF DISTORTION
UNIFORM SPECTRUM
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