북한산국립공원 북동사면에서 동결융해침식 및 토사유출이 계류수질에 미치는 영향

박재현(Jae Hyeon Park) 한국산림과학회 2001 한국산림과학회지 Vol.90 No.4

This study was conducted to investigate influences of solifluction and sediment runoff on the stream water qualities during the spring season. The study sites were four points in the northeastern area of the Bukhansan National Park. And, field surveys were carried out in the spring of 1999, 2000 and 2001. The results of this study were summarized as follows; During the investigation period, the amounts of sediment caused by solifluction on stream side slopes in the downstream were 1.3∼1.7 times as large as those in the upstream. The pH of sediment caused by solifluction was a potential influence on the pH of stream water. Amounts of dissolved Cl^-, NO₃^- and SO₄^(2-) in stream water were proportion to the average amounts of Cl^-, NO₃^- and SO₄^(2-) in the sediment caused by solifluction. In the spring, the average pH of stream water was lower than the first class of the river water quality standard because of increasing chemical concentration as well as the contents of anions(Cl^-, NO₃^- and SO₄^(2-)) in the spring season. Also, the average electrical conductivity of water in downstream was about 2.3-3.3 times higher than that in upstream. The amounts of anions(Cl^-, NO₃^- and SO₄^(2-)) of water in downstream were about 1.2∼7.4, 1.1∼3.9, 1.1∼1.4 times higher than those in upstream, respectively. Therefore, these results showed that the water quality of downstream was worse than that of upstream. As a result of regression analyses, the linear and exponential equation of pH and water quantity was pH = 1.7926 × stream water quantity + 5.9577(R² = 0.46), and those of electrical conductivity and water quantity was EC = 34.417e^(3.6334 × stream water quantity(m/sec) (R² = 0.44).

일본(日本)에서 한류변(漢流邊)의 환경부원(環境復元) 발전전략(發展戰略)(I)

박재현,우보명,이헌호,Park, Jae-Hyeon,Woo, Bo-Myeong,Lee, Heon-Ho 한국환경복원기술학회 2000 한국환경복원기술학회지 Vol.3 No.1

This study was carried out to introduce current status and development strategy for an environmental restoration of stream side in Japan, and to consider a methodology which could be effectively applied for the environmental restoration of stream side in Korea. Since the end of 20th century, the native ecology and landscape of Japan remained only a limited areas such as stream side, water side and forest areas. Therefore, recently the works of forest conservation and erosion control of environmental restoration on stream side tended to increased. The strategic prospects of environmental restoration in Japan were summarized as follows : 1. From the ecological point of view, we have to develop a certain method and technology in construction of forest conservation and erosion control to prevent environmental problem from erosion control works. 2. We have to restore not only a continuity of stream side forest from a primitive area to an estuary but also the stream side forest to preserve and restore a stream side vegetation on a primitive watershed areas. 3. We have to improve a method of construction or removal of a structure which were constructed in the stream to restore a water side environment and an interaction system for an integration on a forest land, stream, and erosion control. Additionally, we have to establish an integrated evaluation method and an enforcement system after investigation of influences on natural environment, stream, and forest etc. 4. We have to conduct an integrated research to investigate the ecosystem of stream side, and construct environmentally friendly water park and erosion control park which considered natural environment and its landscape. Additionally, we need to introduce and adopt a natural style stream construction method to restore a water side areas.

북한산국립공원의 계류수질 보전 전략(I)

박재현,우보명,김우룡,안현철,조현서,추갑철,김춘식,최형태,Park, Jae-Hyeon,Woo, Bo-Myeong,Kim, Oue-Ryong,Ahn, Hyun-Chul,Cho, Hyun-Seo,Choo, Gab-Chul,Kim, Choon-Sig,Choi, Hyung-Tae 한국환경복원기술학회 2001 한국환경복원기술학회지 Vol.4 No.3

This study was conducted to investigate physicochemical property changes from July 1998 to August 2001 in Mt. Bukhansan National Park. Four water sampling points were selected to measure the quality of stream water in the northeastern part of the Mt. Bukhansan National Park. The results were summarized as follows; In spring, the average pH of stream water was below the first class of the river water quality standard, while it was normal level in summer. The average electrical conductivity was about 2.3~3.3 times higher in downstream water than in upstream water during spring and summer. The contents of anions($Cl^-$, $NO{_3}^-$, $SO{_4}^{2-}$) were about 1.1~7.4 and 0.4~11.4 times higher in downstream than in upstream water, respectively. These results indicate that water quality was poorer in downstream than in upstream water. We suggest that stream water in the Mt. Bukhansan National Park should be protected from impacts of snow melting mineral particles in spring season and human impacts like wastewater of point source in summer season.

지리산국립공원내 칠선계곡 탐방로의 회복에 관한 분석

박재현 ( Jae Hyeon Park ) 한국환경보건기술학회(구 한국환경복원녹화기술학회) 2010 한국환경복원기술학회지 Vol.13 No.2

To investigate the restoration procedure on soil physical properties at the surface of visiting road affected by rest-year system. This study was carried out at visiting roads of stream of Chilsun in Jirisan. Mean soil strength in 20cm of soil depth was lower in the Rest-Year System areas (1.5-1.9 times in Site 2, 1.1-7.5 times in Site 3) than in the control (Site 1). Soil strength was recovered by the Rest-Year System in the national park. Mesopore rate (pF 2.7) in 0-15 cm of soil depth was higher in the Rest-Year System areas (1.2 times) than in the control. This indicates that mesopore rate is rapidly restoring in the Rest-Year System areas. Pore space rate in 0-7.5 cm of soil depth was higher in the Rest-Year System areas (23.2% in Site 2, 23.6% in Site 3) than in the control (22.4% in Site 1). Pore space rate in 7.5-15 cm of soil depth was also higher in the Rest-Year System areas (22.9% in Site 2 and Site 3) than in the control (18.9% in Site 1). Soil pore space was remediable by the Rest-Year System. Bulk density in 0-7.5 cm of soil depth was lower in the Rest-Year System areas (1.674g/cm3 in Site 2, 1.668g/cm3 in Site 3) than in the control (1.723g/cm3 in Site 1). Bulk density in 7.5-15 cm of soil depth was lower in the Rest-Year System areas (1.785g/cm3 in Site 2 and 1.721g/cm3 in Site 3) than in the control (1.721g/cm3 in Site 1). Soil bulk density was decreased in the Rest-Year System areas of the national park. Amount of soil erosion was lower in the Rest-Year System areas (0.017m3/km/yr in site 2, 0.023m3/km/yr in site 3) than in the control (0.054m3/km/yr in site 1).

가압유동층의 수력학적 특성 및 압력 변동

박재현,조성호,한근희,진경태,손재익 ( Jae Hyeon Park,Sung Ho Cho,Keun Hee Han,Gyoung Tae Jin,Jae Ek Son ) 한국화학공학회 1996 화학공학의이론과응용 Vol.2 No.2

진주시 산지골 유역내 땅밀림지 특성에 관한 연구

박재현,김선엽,이상현,강한별,Park, Jae-Hyeon,Kim, Seon Yeop,Lee, Sang Hyeon,Kang, Han Byoel 한국산림과학회 2022 한국산림과학회지 Vol.111 No.1

본 연구는 진주시 집현면에서 발생한 땅밀림지의 지질, 지형 및 물리적 특성을 분석하여 땅밀림 발생 피해방지를 위한 기초자료를 제공하기 위하여 실시하였다. 대상지는 1982년에 1차 땅밀림 이후에 2019년 2차 땅밀림이 발생하였는데, 2차 땅밀림 피해면적은 1차보다 약 11.5배로 나타났다. 주 구성암석은 풍화가 비교적 심해 땅밀림이 쉽게 발생하는 퇴적암 지역이었다. 땅밀림으로 붕괴된 지역은 활동면으로 추정되는 면과 슬라이딩 방향으로 층리와 수직으로 발달한 절리의 조합에 의해 암반이 작은 블록으로 나뉘고 이완되면서 활동면을 따라 슬라이딩이 발생하였고, 암반이 분리되면서 분리된 틈으로 지표수 및 토사가 유입하는 것으로 조사되었다. 아울러 셰일 내의 사암이 층리와 절리의 조합에 의해 블록으로 나뉜 후 지하수 등의 풍화작용에 의해 모서리 부분부터 내부로 풍화가 진행되는 양파구조(Onion Structure)를 보여주는 노두가 나타나고, 이런 과정을 거쳐 핵석이 만들어진 것으로 판단된다. 조사대상지는 지하수에 의한 전형적인 땅밀림형 산사태 지역으로 유형은 凸상미근형으로 붕적토 땅밀림형 산사태에 해당하였다. 땅밀림 대상지의 산사태위험등급은 3~5등급에 해당되어 일반적인 산사태와는 차이가 있었다. 지하수는 북동(NE)방향으로 유동하는 것으로 나타났으며, 지형 경사를 따라 유동하며 땅밀림으로 붕괴된 방향과 일치하였다. 땅밀림지로부터 능선부는 땅밀림 영향을 받지 않은 토양으로 땅밀림으로 붕괴된 하단부보다 토양용 적밀도는 높았으며, 붕괴로 인해 토양의 와해와 교란으로 인해 토양용적밀도는 급격히 낮아지는 것으로 나타났다. This study was conducted to obtain basic data that could help prevent damage caused by slow-moving landslides (land-creep). Specifically, the geological, topographic, and physical characteristics of land-creep were analyzed in Jiphyeon-myeon, Jinju-si. The first and second analyzed land-creeps occurred in 1982 and 2019, respectively. The area damaged in the second land-creep was about 11.5-fold larger than that damaged in the first land-creep. The dominant constituent rock in the land-creep area was sedimentary rock, which seems to be weakly resistant to weathering. The areas that collapsed due to land-creep were related to the presence of separated rocks between the bedding plane in the estimated activity surface over the slope direction and the vertically developed joint surface. Thus, surface water and soil debris were introduced through the gaps of separated rocks. Additionally, the areas collapsed due to the combination of the bedding plane and joint surface shale and sandstone showed an onion structure of weathered outcrop from the edge to inner part caused by weathering from ground water. Consequently, core stones were formed. The study area was a typical area of land-creep in a mountain caused by ground water. Land-creep was classified into convex areas of colluvial land-creep. The landslide-risk rating in the study area was classified into three and five classes. The flow of ground water moved to the northeast and coincided with the direction of the collapse. Soil bulk density in the collapsed area was lower than that in ridge area, which was rarely affected by land-creep. Thus, soil bulk density was affected by the soil disturbance in the collapsed area.

지능형 영상회의를 위한 얼굴검출

박재현,박규식,온승엽,김천국,Park, Jae-Hyeon,Park, Gyu-Sik,On, Seung-Yeop,Kim, Cheon-Guk 한국정보처리학회 2001 정보처리학회논문지B Vol.8 No.1

얼굴검출은 현재 많은 연구가 활발히 진행되고 있는 분야로 보안, 인식 등 다양한 응용분야를 갖는다. 본 논문은 카메라가 화자의 이동에 따라 이를 추적하여 회전하고 회의상황에 맞는 앵글을 유지하는 지능형 영상회의 시스템 개발의 기본요소인 화자검출의 선행단계로 얼굴검출에 대한 새로운 방법을 제안한다. RGB 색 공간의 입력영상을 YIQ 공간으로 변환한 후 IQ 성분은 피부영역검출에 Y 성분은 얼굴의 특성을 추출하는데 사용된다. 색 분포도를 이용하여 피부영역을 검출하고, 마스크를 누적 적용하여 잡음을 제거한 후 얼굴의 구조적인 특성과 명암의 분포를 이용하여 얼굴영역이 검출된다. 실험결과 다양한 배경의 영상에서 여러 명의 얼굴이 오류 없이 검출됨이 관찰되었다.

환경친화적 무독성,무취,고효율 중금속 제거제

박재현,장병만,Park, Jae-Hyeon,Jang, Byeong-Man 한국환경기술인연합회 2007 환경기술인 Vol.24 No.9

복사효과를 고려한 기체-입자 직접접촉식 열교환기 해석

박재현,백승욱,권세진,Park, Jae-Hyeon,Baek, Seung-Uk,Gwan, Se-Jin 대한기계학회 1998 大韓機械學會論文集B Vol.22 No.4

A direct contact heat exchanger using particle-suspended gas as a heat transfer medium is analyzed with an extended emphasis on the radiation, i. e., considering the radiation by both gas and particles. While the Runge-Kutta method is used for a numerical analysis of the momentum and energy equations, the finite volume method is utilized to solve the radiative transfer equation. Present study shows a notable effect by the gas radiation in addition to the particle radiation, especially when changing the chamber length as well as the gas and particle mass flow rate. When the gas and particle mass flow rate is raised, the gas temperature in the particle heater still increases as the gas absorption coefficient increases, which is different from the results for the small scale heat exchanger.

경상북도 경주시 양북면 땅밀림지의 지질 및 토양물리성의 변화

박재현,박성균,Park, Jae-Hyeon,Park, Seonggyun 한국산림과학회 2019 한국산림과학회지 Vol.108 No.2

This study was conducted to measure the changes in the geological and soil properties following slow-moving landslide events in Yangbuk-myun and Gyungju-si, Gyeongsangbuk-do, South Korea. The geological characteristics of the study site comprised black shale in the Gyeongsang nodal group formed in the Cretaceous period and quartz feldspar carcinoma in the east side with conglomerate in the Yeonil group formed in the Quaternary period. The study site exhibited the geologic characteristics of a slow-moving landslide with severely weathered rocks. The maximum collapsing depth of the slow-moving landslide was 12.0 m with colluvial deposits. The strike and joint aspects in the slope areas of the slow-moving landslides were $N46^{\circ}E$ in lower slope and $N62^{\circ}E$ in upper slope, respectively. Soil hardness of ${\leq}20cm$ deep was not measured because of the completely disturbed soil resulting from soil creeping. Soil from 25 to 90 cm deep was 1.4-4.7 times softer in the slow-moving landslide areas than in the undisturbed or natural forests. Soil bulk density was $1.24-1.29g/cm^3$ in land creep areas. Soil bulk in both areas was 1.6 times denser than that in the natural forest. The soil pore space was 51.5-53.3% in the land creep areas. The values are 1.3-1.4 times lower than those within the natural forest. Black shale areas showed the lowest coefficient of permeability (8.75 E-06 cm/s) and mesopore ratio (pF 2.7: 9.8%) compared with those resulting from other study areas. 이 연구는 경상북도 경주시 양북면 일원의 산지 땅밀림의 지질특성 및 땅밀림 후 변화되는 토양의 물리적 특성을 구명하고자 수행하였다. 조사지역의 지질은 생성시대가 백악기의 경상누층군으로 주된 구성 암석은 흑색셰일이며, 동쪽으로는 석영 장석질 반암이 분포하고, 그보다 아래쪽은 제4기 연일층군 역암이 분포한다. 암석은 매우 풍화된 풍화암의 형태를 나타내고 있어 땅밀림 지질로 나타났다. 땅밀림으로 무너진 최대 깊이는 12.0 m까지 붕적층으로 구성되어 있다. 땅밀림 방향은 비탈면 하부는 $N46^{\circ}E$, 땅밀림지 상단부는 $N62^{\circ}E$로 절리 및 주향 방향으로 발생하였다. 땅밀림으로 교란된 토양에서는 토양깊이 20 cm 까지는 토양경도가 기록되지 않는 완전교란상태이었고, 토양깊이 25 cm~90 cm까지는 자연산림지 및 교란이 발생되지 않은 지역에 비해 토양경도는 1.4~-4.7배 낮게 나타났다. 또한 땅밀림지역의 토양용적밀도는 $1.24{\sim}1.29g/cm^2$로 자연산림지보다 각각 약 1.6배 높게 나타났다. 토양의 공극률은 51.5~53.3%로 자연산림지보다 각각 약 1.3~1.4배 낮았다. 흑색 셰일지역의 토양투수계수는 8.75E-06 cm/s, 토양의 조공극률은 9.8%로 가장 낮게 나타났다.