Table 3: Mass flux in the jet and filling factors.
knot $v_{\rm tan}$a $r_{{\rm jet}}$b $\dot{M}$( $n_{\rm H},r_{\rm j},v_{\rm j}$)c $\dot{M}$([S II])d ff([S II])e $\dot{M}$([Fe II])d $\dot{M}$(H2)f
  km s-1 arcsec $M_{\odot}$ yr-1 $M_{\odot}$ yr-1   $M_{\odot}$ yr-1 $M_{\odot}$ yr-1
L-I 300 0.1 1.8 $\times $ 10-7 2.4 $\times $ 10-7 1.3 2.2 $\times $ 10-7 4.7 $\times $ 10-9
H 300 0.15 1.6 $\times $ 10-7 3.6 $\times $ 10-8 0.2 7.1 $\times $ 10-8 4.7 $\times $ 10-10
G 305 0.2 2.4 $\times $ 10-7 6.9 $\times $ 10-8 0.3 1.0 $\times $ 10-7 1.9 $\times $ 10-9
F 300 0.3 3.1 $\times $ 10-7 3.7 $\times $ 10-8 0.1 5.2 $\times $ 10-8 8.9 $\times $ 10-10
E 281 0.3 2.3 $\times $ 10-7 1.8 $\times $ 10-8 0.08 4.4 $\times $ 10-8 1.3 $\times $ 10-9
D 300 0.35 1.5 $\times $ 10-7 1.5 $\times $ 10-8 0.1 3.8 $\times $ 10-8 1.8 $\times $ 10-9
C 296 0.4 9.7 $\times $ 10-8 1.1 $\times $ 10-8 0.1 2.9 $\times $ 10-8 1.6 $\times $ 10-9
B 317 0.5 1.7 $\times $ 10-7 7.5 $\times $ 10-9 0.04 2.4 $\times $ 10-8 2.1 $\times $ 10-10
A 311 0.5 7.6 $\times $ 10-8 5.1 $\times $ 10-9 0.07 2.8 $\times $ 10-9 1.1 $\times $ 10-9
a Taken from the proper motion study by Bally et al. (2002). Total velocities ( $v_{{\rm jet}}$) have been derived from these values assuming an inclination angle of 10$^{\circ}$.
b Taken from the FWHM intensity transverse profiles in HST images of Reipurth et al. (2000).
c $\dot{M}$( $n_{\rm H},r_{\rm j},v_{\rm j}$) = $\mu~m_{\rm H}~n_{\rm H}$ $\times $ $\pi~r_{{\rm jet}}^2~v_{{\rm jet}}$, where $n_{\rm H}$ is the total density reported in Table 2. Volume filling factors equal to unity are assumed.
d $\dot{M}$ measured from the luminosities of the [S II]$\lambda $$\lambda $ 6716, 6731 lines and [Fe II]1.64 $\mu $m line.
e Volume filling factor estimated from the ratio between the observed and predicted line luminosities (see text). They are also equal to the ratio between $\dot{M}$ and $\dot{M}$( $n_{\rm H},r_{\rm j},v_{\rm j}$) derived from line luminosities.
f $\dot{M}$ measured from the luminosity of the H2 2.12 $\mu $m line, assuming the H2 temperature estimated from the ratio of the different H2 observed lines.

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