Volatile
organic compound (VOC) emissions from pyrolysis of widely
used biomass are expected to increase significantly under the carbon
neutrality target. However, the dynamic emissions and evolution mechanism
of biomass-VOCs remain unclear, hindered by complex reactions and
offline measurements. Here, we propose a novel covariant evolution
mechanism to interpret the emission heterogeneities, sequential temperature
responses, and evolved correlations of both VOCs and residual functional
groups (RFGs) during corn straw (CS), wood pellet (WP), and semibituminous
coal (SBC) pyrolysis. An innovative combination of online thermogravimetric–Fourier
transform infrared–gas chromatography/mass spectrometry and
two dimensional-correlation spectroscopy was applied. The relative
percentages of CS/WP-VOCs were higher than those of SBC-VOCs, and
most VOCs tended to have relatively small carbon skeletons as the
average carbon oxidation state increased. With the temperature increased
from low to high during CS/WP pyrolysis, the primary sequential response
of VOCs (acids → phenols/esters → alcohols/ethers/aldehydes/ketones
→ hydrocarbons/aromatics) corresponded to the RFG response
(hydroxyl groups → −CH3/–CH2–/–CH groups → aliphatic ethers and conjugated
ketones). Compared with the relative regularity for CS/WP responses,
the gas–solid products from SBC pyrolysis exhibited complex
temperature-dependent responses and high oxidation-induced variability.
These insights provide favorable strategies for the online monitoring
system to facilitate priority removal of coal and biomass fuels–VOCs.