Aging of oily soils produces difficult-to-remove yellow stains on fabrics.
This study examines the effect of different textile substrates on yellowing
and removal of aged oily soils. Model oily soils, squalene and artificial
sebum, were aged at 40 degreesC on cotton, nylon, and polyester fabrics for
8 wk. Radiotracer and spectrophotometric analyses were used to quantify vo
latilization and color change of soiled fabrics upon aging as well as soil
and color removal after laundering. Differences in volatility of oils from
three substrates were insignificant, although cotton and nylon fabrics prod
uced significantly more yellowness than polyester fabrics. Aging of oily so
il enhanced detergency from all three fabrics. The largest increase in remo
val upon aging was found with cotton. Difference in removal from the three
substrates became very small after aging. The effect of substrate was prono
unced on yellowing due to aging with cotton and nylon having higher yellown
ess indices. Cotton visually appeared to be cleaner than indicated by the a
ctual amount of residual oil present after washing, whereas nylon had less
residual oil present even though it visually appeared more yellow than cott
on. For polyester, the amount of residual oil correlated well with appearan
ce after washing. We conclude that discoloration mechanisms differ among co
tton, polyester, and nylon substrates. For polyester, discoloration is sole
ly discoloration of oily soil that is physically bound in the fibrous struc
ture, whereas for cotton, discoloration is a result of discoloration of oil
as well as additional yellowing caused by retention of chromophores chemic
ally bound to the cotton substrate, In the case of nylon, yellowing of nylo
n itself is an additional factor contributing to yellowness even though mos
t of the oil is removed upon washing. These results illustrate the importan
ce of the method of detergency evaluation. Measuring color change in yellow
ness or reflectance is not the same as soil removal based on a quantitative
measurement of soil mass. Thus, it may be necessary to measure both color
and quantity of residual soil.