본 연구는 담액수경재배(Deep Flow Technique, DFT)로 재배된 잎들깨(Perilla frutescens)의 생장 및 생리 적 반응에 미치는 인산결핍의 영향을 분석하였다. 인산 결핍 처리는 야마자키 표준 배양액을 수정하여 0% (대조 구), 30%, 50%, 70%, 100%의 5 수준으로 달리 조성하였다. 처리 20일부터 80일까지 인산 결핍 수준이 증가함에 따라 초장, 엽수, 마디 수, 경직경이 유의미하게 감소하였다. 80일째에는 100% 인산 결핍 처리에서 초장이 10.1cm, 엽수는 식물체당 2.7장으로 급감하였으며, 이는 대조구의 73.5cm 및 12.8장에 비해 현저한 생장 저해를 나타냈다. 또한, 인산 결핍 조건에서 생체중과 건물중 모두 현저히 감소하였으며, 대조구의 생체중은 93.4g 이었으나 100% 인산결핍 처리구에서는 2.1g으로, 건물중은 11.8g에서 0.4g으로 크게 감소하였다. 인산 결핍 정도가 증가할수록 하 부엽에서 황화(Chlorosis) 및 괴사(Necrosis)와 같은 생리장해 증상이 뚜렷하게 나타났다. 이러한 결과는 인산이 잎 들깨의 영양생장과 건물생산량 증가에 필수적인 역할을 수행함을 나타내었다.

Deep geological disposal with multiple barriers composed of engineered and natural barriers has been considered as the most suitable disposal method for high level nuclear wastes. In terms of the geological evaluation factors, brittle structures such as fractures and faults should be characterized around the repository site, because radionuclides transfer mainly with groundwater in the subsurface and groundwater flows through discontinuous brittle structures. The geological survey for the characterization of deep geological repository sites is widely conducted by narrowing the survey area from regional scale down to local scale, which could be divided into three steps: 1) using remote sense or geophysical survey, 2) trench and drill core logging including field survey based on the first step, 3) detailed geological survey in the tunnel. In this study, we analyzed the distribution of geological structures to derive the history of brittle deformation in and around the KURT (KAERI Underground Research Tunnel) site located in the KAERI (Korea Atomic Energy Research Institute). The bedrock of the KURT site is mainly consist of Jurassic two-mica granite, which is extensively intruded by andesitic dikes of Cretaceous with N-S to NE-SW strikes. The two-mica granite in the study area was deformed in a ductile deformation environment and has been overprinted by major geological structures such as faults, dikes, veins, and joints. From this study, we identified 8 brittle deformation events based on the cross-cutting relationship among the geological structures, which are obtained from the analyses in and around the KURT. In order to evaluate the reactivation and fluid flow potential of brittle structures, it is essential to determine the characteristics and ages of the brittle structures and the composed rocks around the site.