Effects of temperature, reaction time, atmosphere, and catalyst on hydrothermal liquefaction of Chlorella

Hydrothermal liquefaction (HTL) is the direct conversion of wet biomass into bio-oil at high temperature (200-400?) and high pressure (10-25 MPa). In this work, we investigated HTL with 4.5 g of Chlorella and 45 ml of water/ethanol (1:1 vol. ratio) in a 100 ml reactor. Bio-oils produced are characterized via elemental analysis, thermogravimetric analysis, and gas chromatography-mass spectrometry (GC-MS). HTL of Chlorella was investigated at 240 and 250? for 0 and 15 min under an air or H-2 atmosphere and with and without 5% zeolite Y. Temperature increased the bio-oil yield from 38.75% at 240? to 43.04% at 250? for 15 min reaction time. Longer reaction time increased the bio-oil yield at 250? from 39.14% for 0 min to 43.04% for 15 min. The H-2 atmosphere had a significant effect for HTL at 240?. Zeolite Y increased the bio-oil yield significantly from 32.03% to 43.06% at 250? for 0 min. The carbon content of bio-oil increased with the temperature while the oxygen content decreased. The boiling point distribution of bio-oils in the range of 110-300? varies with temperature, and atmosphere. At 240? for 15 min, the 110-300? range increased from 31.19% in air (240-15-air) to 39.25% in H-2 (240-15-H-2). The H-2 atmosphere increased the content of hydrocarbons, alcohols, and esters from 69.61% in air (240-0-air) to 82.83% in H-2 (240-0-H-2). Overall, temperature, reaction time, atmosphere, and catalyst all significantly influenced the yield and/or quality of bio-oils from HTL of Chlorella.