Fig. 5

Dependence of the particle size on parameter of the polarization maximum (Pmax ). The filled circles indicate size-sorted carbon samples (Hadamcik et al. 2009). The filled squares and filled triangles denote two size-sorted carbonaceous chondrites (e.g., Orgueil and Allende meteorites, Worms et al. 2000; Hadamcik et al. 2011), respectively. The 3 μm and 160 μm lines are qualified from the Itokawa sample limits. The 63 μm line originates from the spectral resemblance of the heated Murchison meteorite (Sect. 4.1). The Pmax values of 1998 KU2 correspond to the lower limit from our observation (solid line) and the estimate made with the Lumme and Muinonen function (Eq. (7)) in Figure 2 (dashed line).
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