“…Being highly processed in the ISM by supernovae shocks through sputtering and shattering (Draine 2003), silicate dust is expected to have a range of sizes. Without knowing the silicate dust size distribution, Mishra & Li (2015) applied the Kramers-Kronig (KK) relation of Purcell (1969) to estimate that silicate dust contributes to ∼ 48% of the total wavelength-integrated interstellar extinction which is obtained by integrating the observed interstellar extinction over wavelength from the far-UV to the far infrared (IR). Indeed, all modern interstellar dust models assume amorphous silicate to be a major dust species (e.g., Mathis et al 1977, Draine & Lee 1984, Duley et al 1989, Désert et al 1990, Siebenmorgen & Krügel 1992, Mathis 1996, Li & Greenberg 1997, Weingartner & Draine 2001, Li & Draine 2001a, Zubko et al 2004, Jones et al 2013.…”