\begin{table}%t2 \caption{Determinations of the geometric albedo of 21 Lutetia.}\label{albedo_tab} %\tabcolsep0.1pt %\centering \par \begin{tabular}{lcc} %\noalign{\smallskip} \hline \hline \noalign{\smallskip} Author & Method & Albedo \\ \hline Tedesco \& Veeder (\cite{Tedesco92}) & Thermal & 0.221 $\pm$ 0.02 \\ Zellner \& Gradie (\cite{Zellner76}) & Pol. (h) & 0.10 \\ Lupishko \& Mohamed (\cite{Lupishko96}) & Pol. & 0.10 \\ Magri et~al. (\cite{Magri99}) & Radar & 0.19 $\pm$ 0.07 \\ Mueller et~al. (\cite{Mueller06}) &Thermal & 0.208 $\pm$ 0.025 \\ Gil-Hutton (\cite{Gil-Hutton07}) & Pol. ($P_{\rm min}$) & 0.11 $\pm$ 0.01 \\ Gil-Hutton (\cite{Gil-Hutton07}) & Pol. (h) & 0.20 $\pm$ 0.04 \\ Carvano et~al. (\cite{Carvano08}) & Thermal & 0.13 $\pm$ 0.03 \\ Shepard et~al. (\cite{Shepard08}) & Radio & 0.24 $\pm$ 0.07 \\ Weaver et~al. (\cite{Weaver09}) & Vis + 3D model & 0.16 $\pm$ 0.02\\ Belskaya et~al. (\cite{Belskaya10}) & Pol. (h) & 0.13/0.16 $\pm$ $0.02^{*}$ \\ This work & Vis + 3D model & 0.18 $\pm$ 0.02 \\ \hline \end{tabular} \tablefoot{$^{*}$ $p_{V} = 0.13 \pm 0.02$ when using the calibration based on albedos of meteorites (Zellner \& Gradie \cite{Zellner76}) and $p_{V}$ = 0.16 $\pm$ 0.02 when using the calibration based on IRAS albedos (Cellino et~al. 1999).} \end{table}