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Bacillus subtilis가 함유된 목질계 인공토양의 물리·화학적 특성이 참싸리 생육에 미치는 영향
Effects of the Physicochemical Properties of Lignocellulosic Artificial Soil Containing Bacillus subtilis on the Growth of Lespedeza cyrtobotrya 원문보기

목재공학 = Journal of the Korean wood science and technology, v.47 no.4, 2019년, pp.393 - 407  

Kim, Ji-Su (Division of Environmental Forest Science, Major of Environmental Materials Science, Institute of Agriculture & Life Science, Gyeongsang National University) ,  Jung, Ji young (Division of Environmental Forest Science, Major of Environmental Materials Science, Institute of Agriculture & Life Science, Gyeongsang National University) ,  Ha, Si Young (Division of Environmental Forest Science, Major of Environmental Materials Science, Institute of Agriculture & Life Science, Gyeongsang National University) ,  Yang, Jae-Kyung (Division of Environmental Forest Science, Major of Environmental Materials Science, Institute of Agriculture & Life Science, Gyeongsang National University)

초록
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본 연구에서는 Bacilluls subtilis가 함유된 목질계 인공토양(피트모스:펄라이트:폭쇄처리된 참나무:미생물제형=3:1:3:3, w/w/w/w)을 제조 하였으며, 이를 대조구토양과 0%, 25%, 50%, 75% 및 100% 비율로 혼합하여 참싸리 종자 파종 후 소규모 야외포트 현장적용 하였다. 현장적용에 따른 대조구토양, 혼합토양(대조구토양+인공토양) 및 인공토양의 물리 화학적 특성을 분석하였고 참싸리 줄기 및 뿌리생장을 비교하였다. 혼합토양에서는 $0.04g/cm^3$ 이하의 용적밀도, 85 % 이상의 공극률, pH 4.3 - 4.7, 0.5 dS/m 이하의 전기전도도, 15.0 - 26.5의 탄질비, 23.6% - 43.2%의 유기물 함량 및 $157{\times}10^6CFU/g-624{\times}10^6CFU/g$의 미생물밀도를 나타냈다. 인공토양이 25% 및 50% 함유된 혼합토양에서는 참싸리 줄기 및 뿌리생장이 대조구토양보다 높게 나타났고 참싸리의 생장에 영향을 미치는 토양 인자는 용적밀도, 공극률, 수분보유력, 탄질비, 유기물함량 및 미생물함량으로 나타났다.

Abstract AI-Helper 아이콘AI-Helper

In this study, we prepared lignocellulosic artificial soil that contains Bacillus subtilis (peat moss/perlite/ steam-exploded oak wood/microbial culture = 3:1:3:3, w/w/w/w) for use in the restoration of damaged soil areas. The prepared lignocellulosic artificial soil was mixed with soil at ratios of...

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  • 3%, respectively. These findings demonstrate the positive correlation between water-holding capacity and the mixing ratio of the artificial soil. The water-holding capacity of the soils in all the experimental plots (except the control) was > 60%, which is considered adequate (Yeager et al.
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