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Detection of Electro-Magnetic Emissions Transmitted from Earthquake Regions
MISSION
Determination of the electromagnetic signal waveform observed in the ionosphere.
Detection and characterization of the transient very low frequency electromagnetic phenomena.

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The satellite was placed on june 29, 2004, on a quasi Sun Synchroneous circular orbit (inclination 98.23°) at 715 km, with an ascending node at 22h15.
The orbit was then lowered to 660 km in december 2005, without change in the ascending node.
 

The wave field experiment uses magnetic and electric sensors with wide frequency ranges that can work at high sampling rate. This allows to record the electromagnetic signal waveform observed in the ionosphere and to determine its frequency distribution.

The DEMETER novelty as compared to other missions studying the Earth radio environment is the detection and characterization of the transient very low frequency (VLF) electromagnetic phenomena. Thus, the instrument uses a neuronal network processing system.

The payload will work along two main modes :

    Survey Mode
    Beside the control analogical parameters, average and/or reduced scientific data are generated. On board processing are applied in order to reduce the transmitted flux in the mass memory (MM); the transferred data rate is about 25 kbits / second.
     
    Burst Mode
    The acquired scientific data are transmitted with very few or no processing. This high rate mode is mainly activated above seismic zones; the maximal rate is about 1.7 Mbits / second.

Characteristics of the mesured parameters by the different experiments on board DEMETER

  Frequency range, B  10 Hz - 18 kHz
  Frequency range, E  DC - 3 MHz
  Sensitivity B : 1 10-5 nT Hz-1/2 at 1 kHz
  Sensitivity E : 0.2 V Hz-1/2 at 500 kHz
  Particules : electrons 30 keV - 10 MeV
  Ion Density : 5 10² - 5 106 ions/cm³
  Ion Temperature : 1000 K - 5000 K
  Ion Composition : H+, He+, O+, NO+
  Electron Density : 10² - 5 106 cm-3
  Electron Temperature : 500 K - 3000 K
 

Latest Update 04/12/2006