• 한국지형학회지
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• 제28권2호
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• pp.15-30
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• 2021

This study tried to reveal distribution of incision rate and the factors from fluvial terrace deposits on the western and eastern slopes in the Middle Sobaek Mountain Range, using OSL age dating and topographical analysis. An average incision rate of 0.220 m/ka was estimated in the western slope streams, while the streams on the eastern slope showed a lower average incision rate of 0.121 m/ka. These results seem to indicate that the study area experienced an asymmetric uplift. Patterns of incision rate in the study area were different from those in the Northern Sobaek Mountain Range, probably suggesting that the Sobaek Mountain Range experienced spatially different uplift patterns. Among the factors, which were considered to influence on distribution of incision rate in the study area (e.g., altitude of sampling point, distance from divide, distance from axis, channel width, and bedrock type), distance from axis showed the strongest relationship with incision rate. Therefore, uplift is thought to be the most significant factor in distribution of incision rate in the Middle Sobaek Mountain Range.

• 한국지형학회지
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• 제27권3호
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• pp.41-51
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• 2020

This study tried to reveal incision rate distribution of streams on the northern part of the Sobaek Mountain Range with OSL age dating and geomorphic analysis, and factors influencing on the distribution were also discussed. With results from the previous studies, a total of 10 sites from 7 streams in the study area showed the rates ranging from 0.220 m/ka to 0.297 m/ka. Namhan-gang and Geum-cheon indicated the highest and lowest rates, respectively. Both sides in the northern section in the study area showed similar rates, while the western side in the middle section and the eastern side in the southern section showed higher rates than the other sides. Higher rates were also found from the eastern and northern sides where the Range runs N-S and E-W directions, respectively. Certain relationships with altitude and distance from the divide can be recognized from the rates and may be attributed to active incision with altitude and location of the uplift axis near the present divide. The rates on granite and sedimentary rock were higher than those on metamorphic rock, indicating that bedrock type is one of the important factors influencing on stream incision. Tectonic movement seemed to play some roles in the rates, because areas with lineaments showed lower rates. This study suggests that incision rate distribution of streams on the northern part of the Sobaek Mountain Range reflects various local geomorphic and geologic conditions.

• Animal cells and systems
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• 제1권2호
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• pp.305-311
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• 1997

Dermaptera was investigated, examined and reviewed in taxonomy and for distribution in Youngnam region. Based on the data, the local species groups were measured to choose priority-conservation-area by taxonomic root weighting and distribution analysis at 232 geographical conservation units. Eleven species belonging to 4 families and 8 genera were recorded mounting up to 68.75% of species diversity known in Korea. Found remarkably were the rare and endangered Challia fletcheri Burr at Sobaek Mountain National Park, and unusually Anisolabis maritima (Bonelli) in Taegu, Euborellia pallipes (Shiraki) at Island Geoje and E. plebeja (Dohrn) at Hwanho near Pohang. The highest species diversity was found at the temple Huibang area at Sobaek Mountain National Park with 8 species, which was measured also as the primary priority-conservation-area with 83.41 % of accumulated taxonomic root weighting indices in percentage. Geoje and Hwanho both measured as 12.18% of accumulated taxonomic root weighting index in percentage and complimentary to Sobaek Mountain National Park but supporting 5 and 3 species, respectively. The priority goes to the geographical conservation unit supporting higher species richness between two geographical conservation units in comparison. By the rule, the second priority-conservation-area should be Geoje and the third Hwanho. It is, thus, demonstrated how 11 species can be all conserved by choosing 3 priority-conservation-areas out of 232 geographical conservation units to maintain maximum species in minimum areas.

• 한국지형학회지
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• 제25권4호
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• pp.1-19
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• 2018

This study tries to identify distributional characteristics of stream incision rates at 23 points in the northern part of the Taebaek Mountains. Soyang-gang, Naerin-cheon, Odae-cheon, Dong-gang and upper reaches of Okdong-cheon Rivers closed to the Range show higher incision rates and the rates clearly decrease with distance from the Range. Therefore, the incision process in the northern part of the Range has been greatly influenced by uplift around the Range, and the Sobaek Mountain Range seem to play a role in the incision process. Limestone areas show lower incision rates due to degradation of terrace surface by dissolution. This study suggests that local hydrological, geological and geomorphological conditions can be regarded as an important factor in stream incision rates, although stream incision rates are greatly influenced by regional uplift.

• 자원환경지질
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• 제2권4호
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• pp.73-90
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• 1969

The area studied is a southwestern part of Okcheon geosynclinal zone which streches diagonally across the Korean peninsula in the mid-central parts of South Korea, and is bounded by Charyeong mountain chains in the north and by Sobaek mountain chains in the south. The general trend of the zone is of NE-SW direction known as Sinian direction. Okcheon system of pre-Cambrian age occupies southwestern portion of Okcheon geosynclinal zone, and Choseon and Pyeongan systems of Cambrian to Triassic age in northeastern portion of the zone. It was defined by the writer that the former was called "Okcheon Paleogeosynclinal zone" and the latter "Okcheon Neogeosynclinal zone," although T. Kobayashi named them "Metamorphosed Okcheon zone" and "Non-metamorphosed Okcheon zone" respectively and thought that sedimentary formations in both zones were same in origin and of Paleozonic age, and C.M. Son also described that Okchon system was of post-Choseon (Ordovician) and pre-Kyeongsang (Cretaceous) in age. According to the present study two zones are separated by great fault so that the geology in both zones is not only entirely different in origin and age, but also their geolosical structures are discontinuous. Stratigraphy and structure of Okcheon system are clearly established and defined by the writer and its age is definitely pre-Cambrian. It is clarified by present study that the meta-sediments in and at vicinity of Charyeong mountain chains are correlated to Weonnam series of pre-Cambrian age which occupies and continues from northeast to southwest in and at south of Sobaek mountain chains, and both metasediments constitute basement of Okcheon system. Pyeongan, Daedong and Kyeongsang systems were deposited in few narrow intermontain basins in Okcheon paleogeosynclinal zone after it was emerged at the end of Carboniferous period. Granites of Jurassic and Cretaceous ages and volcanics of Cretaceous age are cropped out in the zone. Jurassic granite is aligned generally with the trend of Okcheon geosynclinal zone, whereas Cretaceous granite lacks of trend in distribution. Many isoclinal folds and thrust faults caused by Taebo orogeny at the end of Jurassic period are also parallel with Sinian directieon and dip steeply to northwest. Charyeong, Noryeong, Sobaek, and Deogyu mountain chains are located in areas of anticlinorium, and Kyongsang system in narrow synclinal zones. Folds in Okcheon neogeosynclinal zone are generally of N 70-80W direction but deviate to Sinian direction at the western parts of the zone. This phenomena is interpreted by the fact that the folds were originated by Songrim disturbance at the end of Triassic period and later partly modified by Taebo orogeny. Thrust faults of Taebo orogeny coentinue from Okcheon paleogeosynclinal zone into neogeosynclinal zone, forming imbricated structure as previously described. Strike-slip faults perpendicular to Sinian direction and shear faults diagonally across it by 55 degrees also prevail in neogeosynclinal zone. It is concluded from viewpoints on geology and geological structure that l)Okchon geosyncline had changed its location and affected by numerous disturbances through geologic time, and 2)mountain chains in the area such as Charyeong, Noryeong, Sobaek, and Deogyu were originated as folded mountains. Differing from others, however, Sobaek range was probably formed at the time of Songrim disturbance and modified later by Taebo orogeny. It is cut by Danyang-Jeomchon fault at the vicinity of Joryeong near Munkyeong village and does not continue to southwest beyond the fault, whereas southwestern portion of erstwhile Sobaek range continues to Taebaek rangd northeastward from Deogyusan passing through Sangju, Yecheon, and Andong. From these evidences, the writer has newly defined the erstwhile Sobaek range in such a way that Sobaek range is restricted only to northeastern portion and Deogyu range is named for the southwestern portion of previous Bobaek range.

• 동의생리병리학회지
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• 제16권6호
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• pp.1260-1262
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• 2002

A particular type of ginseng that grows in mountainous regions of Korea is known as Sansam, a term meaning literally mountain grown ginseng. Sansam has recently gained a reputation among some Korean people who believe its health benefits are superior to that of other types of ginseng. Misuse of Sansam has resulted from misinformation that has circulated about the health benefits of its use. Due to insufficient study and research, Korean Oriental Medicine academia does not presently have enough credible information about Sansam to properly educate the public in its use. However, we do have a responsibility to perform adequate study and research so that correct information may be provided. To date, only cursory investigation of the physical characteristics of the Sansam plant have been conducted. This limited investigation was performed in July 2002, at Sobaek Mountain. The branches, leaves, stems, peduncles, fruits, and roots (head, main and fine roots) were observed. The fine roots grew and spread in a large area around the main roots so that harvesting the plants required digging out the soil a considerable distance from the main roots. The plants grew in a northwesterly direction, with a gradient of 40 degrees. They had four branches. Three of the branches had six leaves, while one had five leaves. Each plant had 40 fruits. The roots of the plants grew in a shape similar the Chinese character for mountain. The roots were milky in color. The average weight of the plants was 42.5 grams.

• 한국산림과학회지
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• 제88권3호
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• pp.408-418
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• 1999

전나무 천연집단의 유전적 다양성 및 유전적 구조를 추정하기 위해서 RAPD 표지자를 사용하였으며, 이의 통계적 분석에 AMOVA 방법을 이용하였다. 전나무 집단 전체의 평균 다형성 RAPD 표지자 비율은 71.9%였으며, 전체 변이량의 대부분은 집단내 개체간의 차이(80.2%)로 설명이 가능하였다. 집단간의 유전적 분화정도(${\Phi}_{ST}$)는 0.198로 조사되었다. 전체 집단을 태백산맥과 소백산맥 두 지역으로 나누어 분석하였을 때, 지역간 차이로 설명할 수 있는 변이량이 8.5%로 나타났으며, 통계적 유의성을 확인할 수 있었다. Bartlett 통계량에 의해 집단간 분산의 이질성을 조사한 결과, 태백산 집단과 가리왕산 집단이 특히 이 질적인 것으로 나타났으며, 전반적으로 태백산맥 지역의 집단들이 소백산맥 지역의 집단들 보다 상대적으로 유전적 이질성이 큰 것으로 나다났다. 마지막으로 기존 통계량과의 비교를 통해서 유전변이 분석에 있어서 AMOVA 방법의 적용 가능성에 대해서 논의하였다.

• 태양에너지
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• 제16권2호
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• pp.49-63
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• 1996

측정지의 고도는 일사량 측정에 영향을 주는 중요한 요소이다. 대기중에 내포되어 있는 영속성개스 즉, 오존과 수증기 등은 대기의 순수한 혼합물 성분은 그 농도가 고도와 밀접한 함수관계를 갖기 때문에 해당 측정지 고도는 그 지역의 대기를 구성 하고 있는 성분에 상대적으로 비례하여 일사에 영향을 준다. 이에따라 소백산과 그인접 저지대인 풍기를 대상으로 일사강도를 측정하여 지역별 일사량자원의 특성과 향후 에너지자원으로서의 가능성을 목표로 두고 고지대와 저지대사이의 상호 비교가 가능하도록 하였다. 현지 측정사업의 내용을 중심으로 지금까지 나타난 결과를 살펴보면, 1) 소백산의 연평균 수평면 전일사량 조건은 청명한 날을 기준으로 하루에 4,093 $kcal/m^2$로 나타났다. 2) 소백산에서의 일사강도는 인접 저지대인 풍기보다 $6{\sim}7%$ 정도 높게 나타났다. 3) 대기청명도는 동일한 위도상인 소백산과 풍기지역간의 격차가 현저하게 존재 하였다. 는 점으로 요약된다.

• 한국우주과학회:학술대회논문집(한국우주과학회보)
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• 한국우주과학회 1992년도 한국우주과학회보 제2권1호
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• pp.14.1-14
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• 1993

BV observation of AW Cam (BD.69'0389, HD48049, Bv412) have been carried outusing a CCD Camera attached to 61-cm telescope, at Sobaek mountain Astronomical Observatory. BD 159'0385 were employed for the comparison. A total of 350obserrations were obtained during 3 nights between Jan. 28 and Feb. 19 1993. The light curve have been analyzed by the method of Wilson and Devinney different ialcorrection. The results were compared with the previous solutions.

• 한국제4기학회지
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• 제3권1호
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• pp.17-34
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• 1989

1) 우리나라의 감입곡류의 분포는 태백산맥 서사면과 소백산맥 북.서사면에 집중 분포해 있고 동해사면과 소백산맥 동.남사면에는 상대적으로 감입곡류의 발생률이 낮다. 하천별로는 한강, 금강, 섬진강, 낙동강 순으로 나타나고 특히 남한강 상류에서 높게 나타난다. 2) 지질적으로 감입곡류의 발생률은 조선계, 평안계, 대동계, 변성암, 경상계, 화강암 순으로 높게 나타나고, 풍화에 강한 암석일수록, 층상구조를 하고있는 지질일수록, 지질배열이 유로와 직교할수록, 지질 접촉부에 위치할수록 높게 나타났다. 3) 1/250,000 지형도를 기도로 한 하천차수구분에서 감입곡류의 발생률은 5차, 4차, 6차수 하천에서는 높은 발생률을 보이고 이보다 차수가 높아지거나 낮아질수록 발생률이 급격히 낮아진다. 4) 감입곡류하는 하천의 현재 하상고도는 100~200m 고도에 높은 빈도를 보이고, 절봉면도(7.5km 이하의 곡을 이곡하여 작성)에서는 400~600m 고도에 높은 빈도를 보여 이 절봉면을 원면으로 가정할 때 300~400m의 하각이 이루어진 것으로 볼 수 있다. 5) 감입곡류의 분포적 특성으로 미루어 볼 때 태백산맥 뿐만 아니라 소백산맥도 한반도의 비대칭곡운동의 축일 가능성이 큼을 시사하고 있다. 6) 가상 절봉면 상에서와 하천 차수별 감입곡류 분포 특성을 미루어 볼 때 현재 감입곡류하고 있는 유로는 과거 고위 및 중위 침식면을 흐르던 선행곡류 하천에서부터 유래한 것으로 보는 것이 해석에 유리하였다.