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Table 4

Comparison of the heavy PUI composition derived from CTOF data with the solar-wind composition (von Steiger et al. 2000; Shearer et al. 2014) and the modelled composition that one would expect from the production scenario proposed by Wimmer-Schweingruber & Bochsler (2003).

Ion M / Q Solar wind Simulation x / x + / x ++ Simulation x / x + / x ++ Simulation x / x + / x ++
[amu e-1] rmin = 30 R, D = −1 rmin = 30 R, D = −1.3 rmin = 4 R, D = −1.3

C+ 12 1 1 1 55/43/2 1 51/47/2 1 20/58/23
N+ 14 0.13 ± 0.04 0.23 ± 0.02 0.07 ± 0.03 75/24/2 0.07 ± 0.03 72/26/2 0.09 ± 0.04 34/39/26
O+ 16 1.49 ± 0.19 0.56 ± 0.04 0.64 ± 0.08 80/18/2 0.65 ± 0.08 78/20/2 0.83 ± 0.11 37/32/31
Ne+ 20 0.25 ± 0.06 0.16 ± 0.01 0.09 ± 0.02 83/16/2 0.09 ± 0.02 82/17/1 0.16 ± 0.04 44/36/20
Mg+ 24 0.21 ± 0.09 0.28 ± 0.02 a 0.27 ± 0.11 36/55/10 0.26 ± 0.10 34/56/10 0.27 ± 0.11 14/74/12
Mg2 + 12 0.08 ± 0.02 b 0.05 ± 0.02 0.04 ± 0.02 0.04 ± 0.02
Si+ 28 0.20 ± 0.07 0.21 ± 0.02 a 0.39 ± 0.08 3/86/11 0.37 ± 0.08 2/87/11 0.27 ± 0.06 1/81/19

Notes. For the model, three different parameter sets were chosen (see text). The column x/x+/x++ denotes the fractions of neutral, x, single-charged, x+, and doubly-charged, x++, particles of a certain element at 1 AU in percent.

(a)

Possibly affected by a large systematic error.

(b)

Sensitive to background subtraction.

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