The decomposition of formic acid (0.05mol/L~0.70mol/L) in supercritical water was investigated under 550℃~650℃, 24MPa~30MPa, and a residence time of 16s~46s. The results showed that the gaseous products from the decomposition are mainly H2, CO2 and CO; the yields of H2 and CO2 are much higher than that of other products. High temperature is in favor of H2 production, while the pressure exhibits less effect on formic acid decomposition at high temperature (> 600℃). With the increase of the residence time from 16s to 20s, the molar fraction H2 in the gaseous products is increased steadily, along with the rapid increase of carbon gasification efficiency. The reaction routes are dependent largely upon the feedstock concentration. With a low concentration of formic acid in the feed (< 0.1mol/L), the decomposition includes decarboxylation and dehydration routes; the former is the dominant pathway. Higher formic acid concentration may bring on many sidereactions. Alkaline additives are harmful for the hydrogen production from formic acid decomposition.