터널과지하공간 (Tunnel and Underground Space)

  • 제22권5호
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  • Pages.321-329
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  • 2012
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  • 1225-1275(pISSN)
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  • 2287-1748(eISSN)
한국암반공학회 (Korean Society for Rock Mechanics and Rock Engineering)
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미생물에 의한 티탄철석의 물리적 특성 변화

Changes on Physical Property of Ilmenite due to Microorganism

  • 박영호 (조선대학교 에너지자원공학과) ;
  • 강대완 (조선대학교 에너지자원공학과) ;
  • 강성승 (조선대학교 에너지자원공학과)
  • 투고 : 2012.08.27
  • 심사 : 2012.09.18
  • 발행 : 2012.10.31
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초록

미생물의 유무에 따른 티탄철석의 물성변화를 살펴보기 위하여 공극률, 흡수율, 종파속도 및 일축압축강도(UCS) 등의 실내시험을 수행하였다. 물리적 성질 변화는 미생물을 배양하지 않은 무기적 산화와 미생물을 배양한 생물학적 산화의 조건에서 배양기간에 따라 정량적으로 비교하였다. 그 결과, 배양기간 45일까지 측정된 pH는 무기적 산화의 경우 3.82-4.26 범위에 분포하는 반면, 생물학적 산화에 의한 pH 값은 2.20-2.57 범위 내에서 분포를 보였다. 미생물 유무와 배양기간에 따라 측정된 흡수율의 경우 무기적 산화는 최종단계에서 0.052%, 생물학적 산화는 0.073%로 나타났다. 공극률의 경우 무기적 산화는 최종단계에서 0.206%, 생물학적 산화는 0.281%를 보였다. 미생물에 의한 생물학적 산화는 무기적 산화에 비해 전반적으로 높은 값을 보였다. 종파속도는 배양기간이 지남에 따라 전반적으로 초기 평균값에 비해 낮은 속도 분포를 보였으며, 무기적 산화는 최종단계에서 1886 m/s로, 생물학적 산화는 최종단계에서 1410 m/s로 나타났다. 일축압축강도는 배양기간 따라 모든 시험편에서 감소를 보이며, 무기적 산화의 경우 최종단계에서 241.4 MPa로, 생물학적 산화의 경우 140.0 MPa로 나타났다. 결론적으로 배양기간에 따른 티탄철석의 물리적 특성 변화는 미생물에 의한 영향이 크게 작용하였음을 의미한다.

Laboratory tests for measuring absorption, porosity, P-wave velocity and uniaxial compressive strength (UCS) were performed to examine weathering characteristics of ilmenite by microorganism. Physical property changes were quantitatively estimated with comparing culture period on the condition of abiotic oxidation without microorganism and biooxidation with microorganism. As a result, the measured pH during 45 days was distributed in the range from 3.82 to 4.26, on the other hand, biooxidation showed the range from 2.20 to 2.57. The measured absorption according to microorganism and culture period represented 0.052% at final stage in the case of abiotic oxidation and 0.073% in the case of biooxidation. Porosity showed 0.206% at final stage in the case of abiotic oxidation and 0.281% in the case of biooxidation. In general, the values by biooxidation showed higher than that by abiotic oxidation. Change range of P-wave velocity with culture period showed that the measured value as 1410 m/s at final stage in the case of biooxidation was lower than 1886 m/s of that in the case of abiotic oxidation. The UCS was decreased with increasing culture period in all specimens and represented 241.1 MPa at final stage in the case of abiotic oxidation and 140.0 MPa in the case of bioxidation. In conclusion, it implies that influence of physical property on ilmenite by biooxidation related with microorganism was larger than that by abiotic oxidation.

키워드

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