본 연구는 토양과 온도조건이 질소무기화율, 인지질 지방산유래 미생물 분포와 군집구조에 미치는 영향을 평가하고자 수행하였다. 화산회토양 30 g에 입상유기질비료, 음식물퇴비, 돈분퇴비를 각각 2 g씩 잘 혼합한 후 $10^{circ}C$, $20^{circ}C$, $30^{circ}C$에서 항온배양을 하면서 질소 무기화율과 인지질 지방산 함량을 분석하였다. 질소 무기화율은 온도와 비례하여 증가하였으며 음식물퇴비>입상유기질비료>돈분퇴비 순으로 질소무기화율이 높았다. 지방산 유래 미생물 그룹의 분포는 온도, 유기물종류에 따라 차이를 보였으며 시간이 경과 할수록 미생물의 밀도는 감소하는 경향을 나타냈다. G-/G+, F/B, Unsat/sat 비는 온도가 $10^{circ}C$씩 올라갈수록 감소하였고 cy19:0/$18:1{omega}7c$비는 음식물퇴비와 돈분퇴비에서 증가하였다. PLFA 함량을 이용한 주성분 분석 결과 초기 (75일)는 $10^{circ}C$, 후기 (270일)는 $30^{circ}C$에서 온도요인에 따라 뚜렷하게 미생물 군집을 보였으며 시간이 경과 할수록 군집이동이 나타냈다.
This study was carried out to evaluate effect of temperature condition on nitrogen mineralization of organic matter, distribution of microbial group by PLFA profiles, and soil microbial community structure in volcanic ash soil. Dried soil 30 g mixed well each 2 g of pellet (OFPE) organic fertilizers, pig manure compost (PMC), and food waste compost (FWC). And then had incubated at $10^{circ}C$, $20^{circ}C$, and $30^{circ}C$, respectively. Nitrogen mineralization rate increased with increasing temperature and that was in the order of FWC>OFPE>PMC. Distribution ratio of microbial group by PLFA profiles were different significantly caused by incubation temperature and the type of organic matter. As incubating time passed, density of microbial group decreased gradually. The Gram-bacteria PLFA/Gram+ bacteria PLFA, Fungi PLFA/Bacteria PLFA, and Unsaturated PLFA/saturated PLFA ratios were decreased according to the increasing temperature gradually. But cy19:0/$18:1{omega}7c$ ratio increased both FWC and PMC treatment. Principal component analysis using PLFA profiles showed that microbial community structure made up clearly at both 75 days ($10^{circ}C$) and 270 days ($30^{circ}C$) by temperature factor. As incubating time passed, microbial community structure shifted gradually.
