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Basics of the Method

When a passive electric antenna is immersed in a stable plasma, the thermal motion of the ambient particles produces electrostatic fluctuations, which are completely determined by the particle velocity distributions. This quasi-thermal noise can be measured at the terminals of an antenna connected to a sensitive radio receiver; the analysis of the voltage power spectrum enables us to measure in situ plasma parameters [Meyer-Vernet & Perche, 1989] It yields an accurate determination of the electron density since the electron thermal motions excite Langmuir waves, which produce a spectral peak just above the plasma frequency tex2html_wrap_inline1082 . Moreover, the electrons passing around the antenna induce voltage pulses on it, producing above tex2html_wrap_inline1082 a noise level which decreases as the observing frequency increases and a plateau just below this frequency. The spectrum level and the shape on both sides of tex2html_wrap_inline1082 give the bulk temperature. The method is currently being generalized [Issautier et al., 1996] to measure the plasma bulk speed. Because the proton thermal velocity is much smaller than the plasma bulk velocity, the proton noise spectrum is strongly Doppler-shifted, and it can be observed far above the proton characteristic frequencies. The solar wind speed is thus deduced from the analysis of the proton contribution to the low-frequency thermal spectrum.

Practically, a plasma diagnostic is performed by (1) assuming a model of the velocity distribution (we describe the distribution of the electrons by the superposition of a cold (c) and a hot (h) Maxwellian [Feldman et al., 1975] and that of the protons by one drifting Maxwellian), (2) calculating the theoretical spectrum produced by these distributions, and (3) deducing the parameters of the model by fitting the theory to the data.

The observations were performed with the URAP radio receiver [Stone et al., 1992] connected to the 2 x 35 m electric thin dipole antenna located in the spacecraft spin plane. The receiver is linearly swept through 64 equally spaced frequency channels (of bandwidth 0.75 kHz and duration 2 s), covering the low-frequency band from 1.25 to 48.5 kHz in 128 s. This receiving mode is well suited to measure plasma thermal noise spectra on Ulysses with a good frequency resolution.

Figure 1 shows a typical example of the observed voltage power spectrum. The solid line represents the best fit of the theoretical electron-plus-proton QTN to the observed spectrum; the fit is good since the tex2html_wrap_inline1092 is less than 2%. The model fitting yields the total electron density tex2html_wrap_inline1042 , deduced from the plasma line, the core electron temperature tex2html_wrap_inline1040 , the proton bulk speed V and temperature tex2html_wrap_inline1100 , and the electron suprathermal parameters tex2html_wrap_inline1102 , tex2html_wrap_inline1104 . The latter parameters have large statistical uncertainties (which are obtained from the fitting procedure) because suprathermal particles are revealed by the detailed shape of the spectral peak [Chateau & Meyer-Vernet, 1991] whose measurement requires a better frequency resolution. Preliminary results on the solar wind speed generally give a precision of 10-30% on it depending on the latitude. The best accuracy is obtained for the total electron density which is known with an accuracy of a few percent since it is derived from the measurement of a frequency and is thus independent of the receiver gain calibration, and on the core temperature on which the uncertainty is generally smaller than 10% for in-ecliptic measurements and better than 25% at high latitude. It is noteworthy that the uncertainty on tex2html_wrap_inline1040 is now better than when the drift velocity is neglected [Meyer-Vernet et al., 1997]

   figure50
Figure 1: Example of voltage power spectrum (in tex2html_wrap_inline1016 ) measured with the URAP dipole antenna on Ulysses at 1.34 AU heliocentric distance. The solid line is the theoretical spectrum of the electron plus proton quasi-thermal noise (plus shot noise) which best fits the data (dots), with the plasma parameters shown.

Note that in the following section we selected the core temperature and the electron density data for which the fitting of the voltage power spectrum to the observations (see Figure 1) is the best; i.e., the sigma of the fit is better than 2.5%.


next up previous
Next: Overview of the Pole-to-Pole Up: Quasi-Thermal Noise Method and Previous: Quasi-Thermal Noise Method and

Karine Issautier
Fri Nov 27 18:47:01 MET 1998