Observations oflight curves and stellaroccultations suggest the surface exhibits large concave areas.[5]Polarimetric study of this asteroid reveals anomalous properties that suggests theregolith consists of a mixture of low and highalbedo material. This may have been caused by fragmentation of an asteroidsubstrate with the spectral properties of CO3/CV3carbonaceous chondrites.[6] It is the prototype for a class of asteroids called "Barbarians" that display a strong infrared absorption band at 2μm, which is a characteristic of anFeO–enrichedspinel mineral. Multiple other examples of this class have since been discovered.[7]
Observations made in 2009 withESO'sVery Large Telescope Interferometer (VLTI) suggested that 234 Barbara may be abinary asteroid,[8] although a paper published in 2015 states that "the VLTI observations can be explained without the presence of a large satellite".[5]