The two most common mass estimators that use velocity dispersions and posit
ions of objects in a stellar system, the virial mass estimator (VME) and th
e projected mass estimator (PME), are revisited and tested using N-body exp
eriments. We consider here only spherical, isolated, and isotropic velocity
dispersion systems.
We have found that the PME can overestimate masses by approximate to 20%, f
or realistic cluster mass profiles, if applied only to regions around the t
otal system's effective radius. The VME can yield a correct mass at differe
nt radii provided that the potential energy term is correctly taken into ac
count and the system is completely sampled; otherwise, it may lead to simil
ar errors as the PME.
A surface pressure (3PV) term recently alluded to be usually neglected when
using the VME and therefore required as a correction term is here found no
t necessarily required, although it can be used to yield a reasonable corre
ction term. The preferred method here, however, is the virial theorem due t
o its simplicity and better agreement with N-body experiments. The possible
reasons for the mass discrepancies found when using the PME and the VME in
some N-body simulations are also briefly discussed.