The objective of this study is to investigate and evaluate that a roadside tree root intrudes sewer network systems. Two approaches were performed to assess the characteristics of tree root intrusion. First, the characteristics of tree roots that had invaded sewers were directly observed by means of closed-circuit television inspection robot. Second, the intrusion proportions of tree root into rain gutters in the sampling area were investigated. As tree species of low intrusion proportions, the results indicated that Ginkgo biloba Linn. and Acer buergerianum Miq. were 1.7% and 4.3%. On the other hand, tree species of high intrusion proportions were Metasequoia glyptostroboides Hu et Cheng, Ulmus davidiana var. japonica Nakai and Zelkova serrata Makino as 22.2%, 20.4%, and 17.6% respectively. In particular, sewers and gutters around Zelkova species should be the focus of maintenance work because of the high proportion of these trees on roadsides.

This study observed the upper tropospheric ozone enhancement in the northern Atlantic for the Aerosols99 campaign in January-February 1999. To find the origin of this air, we have analyzed the horizontal and vertical fields of Isentropic Potential Vorticity (IPV) and Relative Humidity (RH). The arch-shaped IPV is greater than 1.5 pvus indicating stratospheric air stretches equatorward. These arch-shaped regions are connected with regions of RH less than 20%. The vertical fields of IPV and RH show the folding layer penetrating into the upper troposphere. These features support the idea that the upper tropospheric ozone enhancement originated from the stratosphere. Additionally, we have investigated the climatological frequency of stratospheric intrusion over the tropical north Atlantic using IPV and RH. The total frequency between the equator and 30˚N over the tropical north Atlantic exhibits a maximum in northern winter. It suggests that the stratospheric intrusion plays an important role in enhancing ozone in the upper troposphere over the tropical north Atlantic in winter and early spring. Although the tropospheric ozone residual method assumed zonally invariant stratospheric ozone, stratospheric zonal ozone variance could be caused by stratospheric intrusions. This implies that stratospheric intrusion influences ozone variance over the Atlantic in boreal winter and spring, and the intrusion is a possible source for the tropical north Atlantic paradox.

우리나라 서, 남해안에 지하수의 해수침투 현상을 관측하기 위해 설치된 관측망 자료를 이용하여, 해당지역별 대수층을 통한 해수침투의 유형을 분석하였다. 분석에 이용된 관측정은 25개 해안지역 소유역의 총 45개 암반관정으로, 지하수위, 수온, 전기전도도를 대상으로 기본통계분석, 상관성 분석 및 변동유형 분류를 수행하였다. 분석 결과 지하수위의 경우 강우 영향을 받거나 양수에 의한 수위강하가 나타나는 관측정에서 큰 폭으로 변동하고 있다. 지하수온은 대부분의 경우 변동폭이 0.2˚C 이내로 안정적인 특징을 보여주고 있으며, 전체적으로 평균 온도가 15˚C 이상으로 나타났다. 전기전도도의 경우 상대적으로 변동폭이 크고 불규칙한 특징을 가지고 있으며, 평균값이 2,000 μS/cm 이내의 관측정이 28개, 10,000 μS/cm를 초과하는 관측정은 9개소로 나타났다. 교차상관도 분석에 의하면, 지하수위는 강우의 영향을 받아 변동하는 형태가 많았지만 수온과 전기전도도는 상대적으로 강우의 영향이 없는 것으로 나타났다. 조석의 경우에는 일부 관측정에서 강우에 의한 영향보다 높은 교차상관도가 나타났다. 본 연구에서는 장기관측자료를 변동형태에 따라 정상형, 추세형, 주기형, 충동형, 계단형, 경사형 등 6가지로 분류하였다. 지하수위의 경우 강우나 양수의 영향을 받는 충동형이 가장 많은 73.3%이며, 조석의 영향은 13.4%에 해당되었다. 지하수온의 경우 변동폭이 일정한 정상형태가 51.2로 가장 높게 나타났으며, 강우나 양수에 의한 충동형이 26.7%에 해당되었다. 전기전도도의 경우는 지하수위나 지하수온과 달리 추세형, 계단형, 경사형 등의 변동형태가 우세한 것으로 나타났다. 전체적으로 동일한 해안지역에 설치된 관측정별로 관측자료의 변동 특성이 상이한 경우가 나타남에 따라, 향후 각 소유역별로 관측정 자료의 정기적인 변동 경향성을 분석하는 것이 필요하다.

Intrusion Detection System (IDS) is intended to detect anomalous usages or attacks on system and network. Even though many IDS models have been developed, they still may have problems, such as involvement of components contaminated by anomalous process, in detecting anomalous behavior patterns. To distinguish anomalous patterns from normal patterns, we propose a Bayesian approach which includes the presentation of the relations among normal pattern components.

Due to recent changes of computer & networks, the IDS(Intrusion Detection System) need to be developed for new intrusion patterns. The current IDS have limited on recognition and correspond to new intrusion patterns on detection speed for multi packet which dealing on the network. Therefore, new technology need to increasing efficiency and speed of detection speed requested. The aim of this research is the development of standard and systematic method on intrusion detection. The core idea is using data mining method to find bundle of patterns on networking program and user behavior patterns as well as apply the feature systems to calculate the classifiers which could recognize the well known or irregular intrusions. In this paper, we will recommend following steps to develop the intrusion detection system: First, we will learn the detection applying technique for multi intrusion cases. Second, we will use data mining technique which fast recognize the current intrusion patterns and new patterns. Third, to recognize intrusion patterns, information of packet on the network and recorded data on the host sessions have studied. Fourth, we will create regulations between intrusion and normal behavior by practical use of logged file abstraction programs. Fifth, we will analysis intrusion detection pattern based on the created regulations and study results.

일본의 28개 전 국립공원에 있어서 언제, 어디서, 어떠한 경관파괴나 침해문제가 발생하였는가 그 특성을 파악하기 위하여 자연환경 전문지를 대상으로 문헌조사하여 문제발생을 요인별, 지역별 그리고 시기별로 정리, 분석하였다. 그 결과, 경관파괴나 침해를 발생시킨 요인으로는 대규모 댐건설, 임업에 의한 작업, 각종 관광시설의 정비, 공원이용자에 의해 발새오디는 문제, 공원계획과 관리상에서 발생되는 문제 등의 8가지 요인군으로 지적할 수 있었다. 한편, 시기별로는 경관문제의 발생건수나 특정지역에서 집중적으로 발생하는 등 4기(1960~1967, 1968~1975, 1976~1985, 1990초반)로 구분할 수 있었고, 특히, 1960년대 후반부터 1970년대 전반에 걸쳐서는 전국적으로 모든 국립공원에서 다양한 경관문제가 발생하였다. 지역별 특성은 本州 중앙(관동지방, 중부지방)에 위치하는 부상상한윤두, 日光, 中部山岳 등의 국립공원에서 경관문제가 다른 지역에 비하여 지속적으로 많이 발생했다. 그 원인으로는 이용객의 지속적인 증가, 고도성장과 산업발전, 국민관광 레크레이션붐, 관광시설의 대규모화, 삼림벌채 등의 임업작업, 1962년과 1969년 2회에 걸친 전국종합개발계획의 실시, 임해매립지에 의한 대규모 공업단지 조성, 모터제너레이션의 발달 등이 활발히 이루어진 사회적 배경 등을 지적할 수 있었다.

Understanding the long-term geochemical evolution of engineered barrier system is crucial for conducting safety assessment in high-level radioactive waste disposal repository. One critical scenario to consider is the intrusion of seawater into the engineered barrier system, which may occur due to global sea level rise. Seawater is characterized by its high ionic strength and abundant dissolved cations, including Na, K, and Mg. When seawater infiltrates an engineered barrier, such dissolved cations displace interlayer cations within the montmorillonite and affect to precipitation/ dissolution of accessory minerals in bentonite buffer. These geochemical reactions change the porewater chemistry of bentonite buffer and influence the reactive transport of radionuclides when it leaked from the canister. In this study, the adaptive process-based total system performance assessment framework (APro), developed by the Korea Atomic Energy Research Institute, was utilized to simulate the geochemical evolution of engineered barrier system resulting from seawater intrusion. Here, the APro simulated the geochemical evolution in bentonite porewater and mineral composition by considering various geochemical reactions such as mineral precipitation/dissolution, temperature, redox processes, cation exchange, and surface complexation mechanisms. The simulation results showed that the seawater intrusion led to the dissolution of gypsum and partial precipitation of calcite, dolomite, and siderite within the engineered barrier system. Additionally, the composition of interlayer cation in montmorillonite was changed, with an increase in Na, K, and Mg and a decrease in Ca, because the concentrations of Na, K, and Mg in seawater were 2-10 times higher than those in the initial bentonite porewater. Further studies will evaluate the geochemical sorption and transport of leaked uranium-238 and iodine-129 by applying TDB-based sorption model.

The compacted bentonite buffer is a key component of the engineered barrier system in deep geological repositories for high-level radioactive waste disposal. Groundwater infiltration into the deep geological repository leads to the saturation of the bentonite buffer. Bentonite saturation results in bentonite swelling, gelation and intrusion into the nearby rock discontinuities within the excavation damaged zone of the adjacent rock mass. Groundwater flow can result in the erosion and transport of bentonite colloids, resulting in bentonite mass loss which can negatively impact the long-term integrity and safety of the overall engineered barrier system. The hydro -mechanicalchemical interactions between the buffer, surrounding host rock and groundwater influence the erosion characteristics of the bentonite buffer. Hence, assessing the critical hydro-mechanicalchemical factors that negatively affect bentonite erosion is crucial for the safety design of the deep geological repository. In this study, the effects of initial bentonite density, aperture, discontinuity angle and groundwater chemistry on the erosion characteristics of Bentonil WRK are investigated via bentonite extrusion and artificial fracture experiments. Both experiments examine bentonite swelling and intrusion into simulated rock discontinuities; cylindrical holes for bentonite extrusion experiments and plane surfaces for artificial fracture experiments. Compacted bentonite blocks and bentonite pellets are manufactured using a compaction press and granulation compactor respectively and installed in the transparent extrusion cells and artificial fracture cells. The reference test condition is set to be 1.6 g/cm3 dry density and saturation using distilled water. After distilled water or solution injection, the axial and radial expansion of the bentonite specimens into the simulated rock discontinuities are monitored for one month under free swelling conditions with no groundwater flow. Subsequent flow tests are conducted using the artificial fracture cell to determine the critical flow rate for bentonite erosion. The intrusion and erosion characteristics are modelled using a modified hydro-mechanicalchemical coupled dynamic bentonite diffusion model and a fluid-based hydro-mechanical penetration model.

Bentonite is a widely used buffer material in high-level radioactive waste repositories due to its favorable properties, including its ability to swell and low permeability. Bentonite buffers play an important role in safe disposal by providing a low permeability barrier and preventing radionuclides migration into the surrounding rock. However, the long-term performance of the bentonite buffer is still an area of research, and one of the main concerns is the erosion of the buffer due to swelling and groundwater flow. Erosion of the bentonite buffer can have a significant impact on repository safety by reducing the integrity of the buffer and forming colloids that can transport radionuclides through groundwater, potentially increasing the risk of radionuclide migration. Therefore, understanding the mechanisms and factors that influence the erosion of the bentonite buffer is critical to the safety assessment of high-level radioactive waste repositories. In this study, we attempted to develop the bentonite buffer erosion model using Adaptive Processbased total system performance assessment framework for a geological disposal system (APro) proposed by the Korea Atomic Energy Research Institute (KAERI). First, the erosion phenomenon was divided into two stages: bentonite buffer penetration into rock fractures and colloid formation. As an initial step in the development of the buffer erosion model, a bentonite buffer intrusion into the fracture and consequent degradation of buffer property were considered. For this purpose, a tworegion model based on the dynamic bentonite diffusion model was adopted which is one of the methods for simulating bentonite buffer intrusion. And, it was assumed that the buffer properties, such as density, porosity and permeability, thermal conductivity, modulus of elasticity, and mechanical strength, are degraded as the buffer erodes. The bentonite buffer degradation model developed in this study will serve as a foundation for the comprehensive buffer erosion model, in conjunction with the colloidal formation model in the future.

Compacted bentonite buffer blocks placed in the engineered barrier system for high-level nuclear waste disposal can undergo swelling, intrusion into rock fractures, and erosion with saturation. Bentonite erosion and intrusion can lead to bentonite mass loss via groundwater flow and can ultimately compromise the overall integrity of the disposal system. To ensure the long-term safety of deep geological disposal, it is essential to assess the hydro-mechanical interactions between the bentonite buffer and surrounding rock. In this study, the impact of bentonite erosion and intrusion on the mechanical properties of the jointed rock mass were assessed via elastic wave propagation measurements using the quasi-static resonant column test. Granite rock discs obtained from the Korea Underground Research Tunnel and Gyeongju bentonite were used to simulate jointed rock specimens with different bentonite intrusion conditions. Different degrees of bentonite intrusion were simulated by mixing bentonite and water to create bentonite paste and gel. The longitudinal and shear wave velocities under different normal stress levels were used to quantify the effects of bentonite intrusion on the mechanical characteristics of the rock joint. Complementary numerical analysis using the three-dimensional distinct element code (3DEC) was conducted to provide improved understanding of wave propagation within bentonite gouge-filled rock mass.

During and after the construction of LILW disposal facilities, the decrease of groundwater head potential has been monitored. In addition, an increase of the electrical conductivity (EC) has been observed in several monitoring wells installed along the coastal coastline. Monitoring activity for groundwater head potential and hydrogeochemical properties is important to reduce the uncertainty in the evaluation of groundwater flow characteristics. However, the data observed in the monitoring wells are spatial point data, so there is a limit to the dimension. Several researchers evaluated groundwater head potential changes and seawater intrusion (SWI) potential for disposal sites using groundwater flow modeling. In case of groundwater flow modeling results for SWI, there is a spatial limit in directly comparing the EC observed in the monitoring wells with the modeling results. In a recent study, it was confirmed that the response of the long-range ground penetraiing radar (GPR) system was severely attenuated in the presence of saline groundwater. In order to reduce the spatial constraint of the groundwater monitoring wells for SWI, the characteristics of SWI within the disposal facility site by using the the results of a recent study of the long-range GPR system were investigated and evaluated in this study.

Near-surface disposal facility is more susceptible to intrusion than underground repository, resulting in more possible pathways for contaminant release. Alike human intrusion, animals (e.g. Ants, Moles, etc.) could intrude into the disposal site to excavate burrows, which could cause direct release of contaminants to biosphere. In this paper, animal intrusion is demonstrated using GoldSim’s commercial contaminant transport module and impact on the integrity of the near-surface disposal facility is evaluated in terms of fractional release rate of the contaminants. In this study, the near-surface disposal facility is modelled with a single concrete vault to contain radionuclide according to LLW concentration limit stated in NSSC notice No.2020-6. The release of contaminants is modelled to occur directly after the institutional control period, and the contaminants are mostly transported from the concrete vault to cover layers via diffusion. To produce mathematical model of the release of the contaminants due to animal intrusion, firstly, the fraction of burrow volume for each cover layer is calculated separately for each animal species, based on their maximum possible intrusion depth. In this study, fractions of burrow volume for ants and moles are calculated based on their maximum possible intrusion depths, where for ants is 2–3 m, and for moles is 0.1–0.135 m. Then, assuming that the contaminants are distributed homogeneously throughout each cover layers by diffusion, fraction of contaminants transported into the uppermost layer via excavation of the burrow is calculated for each layer based on burrow volume, and fraction of contaminants removed from the uppermost layer to the layers below via collapse of the burrow is also calculated based on the burrow volume. Lastly, the net transportation of contaminants into and out of the burrow via excavation and collapse, respectively, is calculated and demonstrated using direct transfer rate function of the GoldSim. Based on the simulated result, the maximum mass flux is too minor to cause a meaningful impact on the safety. The peak mass flux of the most sensitive radionuclide, I-129, is witnessed at around year 1,470, with a flux value of 5.36×10−6 g·yr−1. This minor release of the contaminants could be due to cover layers being much thicker than the maximum possible intrusion depth of the animals, preventing the animal intrusion into the deeper layers of higher radionuclide concentration. In future, this study can be used to provide a guidance and fundamental data for scenario development and safety evaluation of the near-surface disposal facility.

본 연구에서는 SEAWAT을 이용하여 여수지역의 해수침투 피해 면적을 파악하고, 기후변화 시나리오 적용에 따른 미래의 해수침투 피해 예상 면적을 산출하였으며 해수침투 피해 저감 대책의 피해면적 저감 능력을 분석하였다. 2015년 기준 여수지역의 해수침투 피해 면적은 14.90 km2로 나타났고, 기후변화 시나리오를 적용하였을 때 2099년 여수지역의 예상 해수침투 피해 면적은 RCP 4.5의 경우 19.19 km2이며, RCP 8.5의 경우 20.43 km2로 나타났다. 이에 대한 저감대책으로 인공함양을 고려하였을 때, 총 300 m3/d, 100 m3/d, 50 m3/d의 함양 시나리오를 설정하였을때 RCP 4.5의 경우 해수침투 면적은 평균 7.03%, RCP 8.5의 경우 8.32% 감소하였다. 물리적 차수벽 대책의 경우는 차수벽의 두께를 0.8 m, 1.3 m, 1.8 m 로 설정하였을 때 RCP 4.5의 경우 해수침투 면적은 평균 9.80%, RCP 8.5의 경우 10.30% 감소하였다. 본 연구는 연안지역의 해수에 의한 지하수 오염과 그에 수반한 2차적인 피해를 막기 위한 대비책을 결정하기 위한 정량적인 근거로서 사용될 수 있을 것으로 기대된다.

중·저준위방사성폐기물 표층처분시설 인간침입시나리오의 ‘평가/해석에 대한 불확실성’의 관리를 위해 GENII를 이용 한 평가결과를 오염토양에 대한 방사선영향평가를 위해 개발된 RESRAD를 이용하여 검증하였다. 중저준위방사성폐기물 표 층처분시설의 인간침입시나리오로 시추후거주시나리오를 선정하여 각 코드의 현상 모사에서 발생하는 한계점을 파악하고 동일한 입력데이터 조건에서 두 코드의 평가결과를 비교분석함으로써 모델링의 불확실성을 분석하였다. 평가결과 각 코드 에서 일부 핵종의 거동모사에 대한 차이는 있었으나 폐쇄후관리기간 이후 선량평가 결과 모든 피폭경로에 대한 경향이 유사 함을 확인하였다. 또한 RESRAD에서 확인한 선량평가 결과를 바탕으로 입력인자에 대한 민감도 분석을 수행하고 주요입력 인자를 도출하였다. 이를 통해 모델링 결과 및 입력인자에 대한 불확실성을 분석하고 안전성평가 결과에 대한 신뢰성을 확 인하였다. 본 연구의 결과는 중저준위방사성폐기물 처분시설의 Safety Case 구축에 활용될 수 있다.