Due to the perceived complexity of relaxation tests, the relaxation respons
e of geosynthetics has, in the past, been predicted from isochronous curves
generated from creep tests. However, the validity of such an approach has
not been extensively investigated. Using experimental data from in-isolatio
n creep and relaxation tests performed on eleven different geogrids, the va
lidity and limitations of using creep isochronous curves to predict relaxat
ion response of geogrids has been investigated. Acceptable agreement betwee
n predicted and experimental relaxation responses was rather limited, being
observed for specimens tested at low initial load levels and for materials
exhibiting relatively large creep strains. With minor exceptions, the expe
rimentally measured force relaxation was under-predicted by using the isoch
rone approach. Nonetheless, it appears that for the geogrids tested, overal
l accurate relaxation response cannot be predicted from isochronous curves
constructed using creep data.