Insight of microbial degradation of n-hexadecane and n-heneicosane in soil during natural attenuation and bioaugmentation by Compound-specific Stable Isotope Analysis (CSIA)

Abstract

Microbial degradation of n-hexadecane (n-C16) and n-heneicosane (n-C21) in soil during natural attenuation (NA) and bioaugmentation (BA) were investigated by compound-specific stable isotope analysis (CSIA), microbial community and key enzyme genes analysis. In both NA and BA treatments, more than 95% of n-C16 and n-C21 were degraded within 3 and 6 days, respectively, with a slight faster degradation in BA than NA. According to CSIA, n-C16 showed a reverse hydrogen isotope fractionation effect, while n-C21 had a normal hydrogen isotope fractionation effect, and the degree of hydrogen isotope fractionation in BA were greater than NA. Isotope enrichment factors (εH) of n-C16 and n-C21were 3.50 ± 0.60‰ and − 2.11 ± 0.57‰ in NA, and 5.18 ± 0.46‰ and − 2.73 ± 0.39‰ in BA, respectively. The dominant genera in BA and NA were significantly different for n-C16 and n-C21 degradation and few strains added during BA remained active, such as Rhodococcus in both n-C16 and n-C21, and Brevundimonas only in n-C21, which showing high application potential in alkanes contamination remediation. Both alkB and almA genes played more key roles than Cytochromes P450 in n-C16 and n-C21 biodegradation, but alkB was much more promoted by n-C16 while almA was more motivated by n-C21. The different types of alkane-degrading bacteria with different enzyme reaction kinetics might be the reason of opposite hydrogen isotope fractionation of n-C16 and n-C21 during their biodegradation. Above all, CSIA can be a proper technology to quantitatively evaluate the biodegradation of different alkane during NA and BA bioremediation process in contamination sites.