• The Korean Journal of Archival Studies
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• no.65
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• pp.365-396
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• 2020

I examined the archival basis of two historians who wrote history books with the same title of 'History'; Simaqian of ancient China and Herodotus of Halikarnassos. I examined a prejudice to these two history books, a misunderstanding of them as an imagination rather than a history. How can an imagination become a history? First, I explained the common characteristics found in their compilation and writing of 'History.' Simaqian and Herodotus did their field-works in historical sites, gathered oral-histories, and arranged archives they collected. These two historians heavily engaged in archival works in terms of verifying authenticity and reliability of their sources on the basis of historical empiricism. There are some misunderstanding on their archival endeavor and on the very nature of archives and historical studies as empirical studies. Furthermore, this misunderstanding regarding them as literature came from a confusion over the concept of literature. The creativity of literature is not equal to the "fictitiousness" of history despite historical works sometimes may give us an impression by the way of describing and providing insight into a certain event(s) and a person(s). As Herodotus said, a recognition of the differences of each race and human is a departure of historical archiving of the valuable experiences of human-beings. By doing so, natural results of archival behaviors, preservation of the records, and consistent inquiry of historian-archivists become a humanistic passage overcoming the current wrong trends of historical studies confined to a narrow nation-history.

• The Journal of the Petrological Society of Korea
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• v.15 no.1 s.43
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• pp.1-9
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• 2006

Sr isotopic compositions are determined from the syenite of Sancheong area, yielding age of $211{\pm}23(2\sigma)$ Ma and $^{87}Sr/^{86}Sr$ initial ratio of $0.70598{\pm}0.00060$. Such result confirms that Sancheong syenite was emplaced during the Mesozoic around the Triassic-Jurassic boundary. Rather low initial $^{87}Sr/^{86}Sr$ ratio suggests insignificant influence of old crustal materials. There are strong contrast in rock types of plutonic associations between Sancheong-Macheon area and adjacent Hamyang-Geochang area to the north, i.e. syenite-diorite-gabbro and granite-granodiorite respectively. $^{87}Sr/^{86}Sr$ initial ratios also show distinction between these areas. Such differences suggest regional contrast in tectonic environments between them.

• Proceedings of the Korea Water Resources Association Conference
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• 2019.05a
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• pp.206-206
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• 2019

이 연구는 유출토사량의 저감을 위해 설치되는 식생대의 특성에 따른 효율을 살펴보는 것을 목적으로 한다. 검토하는 식생대의 특성으로는 식생의 종류와 식생대의 높이가 포함된다. 식생대의 효율을 평가하기 위해서는 VFSMOD-W 프로그램을 이용한다. 식생대가 적용되는 대상지역은 금강의 지류인 금마천이다. 금마천 유역은 나지를 다수 포함하고 있어 식생대의 설치에 따른 변화를 잘 살펴볼 수 있는 지역으로 판단된다. 해당 지역에서의 강우량은 시간당 최대강우량이다. 식생대의 특성을 나타내기 위해 보정되는 매개변수는 조고이며 VFSMOD-W 프로그램에서 제공하는 식생의 종류를 입력하였다. 사용된 프로그램에서는 식생대의 간격, 규모 등을 고려할 수 있므려 총 36개 종류의 식생대가 검토된다. 본 연구의 결과를 통해서 가장 먼저 나타나는 점은 식생대의 설치간격이 좁아질 때 보다 많은 양의 토사를 저감할 수 있다는 것이다. 하천으로 유출되는 유역토사의 저감을 식생대를 좁게 설치하는 과정을 통해 유도할 수 있다는 점이 확인된다. 식생대의 조도계수 역시 토사저감에 큰 영향을 미치는 것으로 나타났다. 나지의 경우 0.012, Bermuda Grass의 경우 0.41로 조도계수를 설정하고 수치실험을 시행한 결과 조도계수의 증가가 유출 토사량 감소에 큰 영향을 준다는 점이 확인된다. 식생대의 최대 높이가 주는 영향을 살피기 위해서 1 cm에서부터 100 cm까지의 식생대 높이를 적용하고 결과를 분석하였다. 식생대의 특성 및 설치방식을 고정된 조건으로 두고 식생대의 높이에 따른 영향만 살펴보았다. 그 결과 식생대의 최대높이는 유출 토사량에 큰 영향을 주지 않는 것이 나타났다. 이를 통해 유출 토사량 저감 효율을 증가시키고자 할 때 식생의 높이보다는 식생의 종류와 조고 등에 보다 집중하여 식생대를 조성하는 것이 바람직하다는 점을 알 수 있다.

• Journal of The Geomorphological Association of Korea
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• v.18 no.4
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• pp.193-202
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• 2011

Kompsat EOC-1 imagery, high resolution air-photo imagery and Shalstab model were used to analyze the geomorphic characteristics of the place of debris flow occurred by typhon "RUSA" in 2002, Macheon-Myen, Gyeongsang prefecture, Republic of Korea. On gully-head over 35 degree of slope angle, almost debris flow started, where slope angle is more than internal friction angle. The result simulated by Shalstab model presented larger vulnerable area to debris flow than the area where debris flow really occurred, this error would be attributed to the assumption for steady-state condition with full saturated surface. To predict the debris flow accurately, further study for rainfall and soil water flow will be needed.

• Journal of Environmental Science International
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• v.7 no.3
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• pp.275-280
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• 1998

In order to clarify the seasonal composition and abundance of zooplankton commuuty In Macheon Bay. the study was carried out trimonthly during the period from April 1996 to January 1997. 1 species of Cnidana. 1 species of Annelida, 2 Ima of Moiluscs.3 species of Rotifera, 4 species and 4 larspecies was Tintinnopsis beroidea In the spring, Copepodite In the summer, Tintinnopsis beroidea In the autumn and Ceratium risus In the winter. Abundance of zooplankton ranged firom 4.720 to 41,215 Inds./1 It was high In the summer (41,215 inds./l) and low In the spring 14,720 inds./l). Dominant index ranged from 0.133 (in the spring) to 0.551 (in the winter). Species diversity inden ranged from 1.114 (in the winters to 1.996 (in the spring).

• Proceedings of the Korean Association of Geographic Inforamtion Studies Conference
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• 2010.06a
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• pp.231-237
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• 2010

이상기후에 의한 집중호우나 태풍의 영향으로 예전에는 기록이 없었던 백두대간과 전국 국립공원의 자연사연에서 산사태가 많이 발생하고 있으며 특히 지형이 험준하고 고도가 높은 지리산의 경우, 다른 국립공원에 비해서 그 발생빈도가 높게 나타난다. 본 연구에서는 지리산 북쪽지역으로 경상남도 함양군 마천면과 전라북도 남원시 산내면에 걸쳐서 발생한 산사태를 중심으로 산사태를 발생시키는 영향인자를 GIS와 원격탐사를 이용하여 분석하였다. 먼저 산사태 발생 지역의 지형특성을 분석하였고 산사태 발생과 산사태 발생에 영향을 끼친 인자들의 상관관계를 알아보기 위해서 빈도비를 사용하였으며 가중치를 도출하기 위해서 다중 회귀분석을 실시하였다.

• Proceedings of the Plant Resources Society of Korea Conference
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• 2018.10a
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• pp.48-48
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• 2018

본 연구는 경남 함양군 삼봉산의 관속식물을 조사한 후 식물상 현황과 특정식물종 및 귀화식물 등을 정리하였으며, 차후 식물상의 보호 관리에 있어 기초 자료로 활용하고자 실시하였다. 삼봉산은 전북 남원시 산내면 중황리, 인월면 상우리와 경남 함양군 마천면 구양리, 함양읍, 죽림리가 접하는 지역으로 남쪽으로는 국립공원 지리산의 연봉이 길게 늘어서 있고 북쪽으로는 광주대구 고속도로 건너 함양군의 백운산과 괘관산 등 1,000m가 넘는 산이 많은 지역내에 위치하고 있다. 삼봉산지역에 자생하는 관속식물은 총 80개과 182개속 254개 종이 생육하는 것으로 나타났다. 삼봉산 지역의 특정식물종은 식물구계학적 특정식물 V등급인 승마 Cimicifuga heracleifolia Kom.)와 IV등급인 도깨비부채(Rodgersia podophylla A.Gray), 점현호색 (Corydalis maculata B.U.Oh & Y.S.Kim), 솔붓꽃 (Iris ruthenica KerGawl.), 산복사나무 [Prunus davidiana (Carriere) Franch.] 등이 분포하는 것으로 확인되었다. 조사결과 가흥지역에서 환경부 멸종위기종은에 해당하는 분류군은 없었으며 특정식물종 V등급에 해당되는 승마와 IV등급에 해당되는 4개 분류군이 확인되었다. 국립공원지리산 근처의 1,000m이상의 산지임에도 전체적으로 50년 전부터이루어진 조림과 능선 바로 아래까지 경작지가 존재하는 등 식생의 파괴가 심하여 전체적인 관속식물의 다양성은 낮은 것으로 확인되었다.

• Korean Journal of Plant Taxonomy
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• v.44 no.1
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• pp.1-5
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• 2014

The newly recorded species, Crepidomanes schmidtianum (Zenker ex Tasch.) K. Iwats. (Hymenophyllaceae) was collected from forests in Mt. Jirisan, Baegmu-dong, Macheon-myeon, Hamyang-gun, Gyeongsangnam- do. C. schmidtianum (vernacular name: 'Du-me-goe-bul-i-kki') was distinguished from other Korean congeners of the genus Crepidomanes by having pseudo-vein, almost wingless in stipe, and involucres cup shaped with dilated. A new Korean name, 'Du-me-goe-bul-i-kki', was given based on its habitat. Descriptions and illustrations of this taxon and its photograph in the habitat are provided along with a key to the species of Crepidomanes from Korea.

• The Korean Journal of Pharmacology
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• v.5 no.2
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• pp.87-92
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• 1969

The effects of dephenylhydantoin, strychnine, coramine, d-amphetamine and chlorpromazine on $QO_2$ and non-inulin space $Na^+$, $K^+$ concentration of rat cerebral cortical slices incubated in pH 7.4 glycylglycine glucose saline was investigated. In general, there are decreased non-inulin space $Na^+$ concentration or increased non-inulin space $K^+$ concentration or both when the ratio of respiration to non-inulin space is greater than control group except in case of chlorpromazine $10^{-4}\;M$. And it is suggested that the ratio of respiration to non-inulin space is responsible more closely for the non-inulin space Na, K concentration than $QO_2$ expressed per tissue wet weight. Effects of diphenylhydantoin and several other agents on electrolytes and the electroshock seizure threshold are discussed.

• Korean Journal of Mineralogy and Petrology
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• v.34 no.2
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• pp.107-120
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• 2021

The Komdok Pb-Zn deposit, which is the largest Pb-Zn deposit in Korea, is located at the Hyesan-Riwon metallogenic zone in Jiao Liao Ji belt included Paleoproterozoic Macheolryeong group. The geology of this deposit consists of Paleoproterozoic metasedimentary rocks, Jurassic Mantapsan intrusive rocks and Cenozoic basalt. The Komdok deposit which is a SEDEX type deposit occurs as layer ore and vein ore in the Paleoproterozoic metasedimentary rocks. Based on mineral petrography and paragenesis, dolomites from this deposit are classified four types (1. dolomite (D₀) as hostrock, 2. early dolomite (D₁) associated with tremolite, actinolite, diopside, sphalerite and galena from amphibolite facies, 3. late dolomite (D₂) associated with talc, calcite, quartz, sphalerite and galena from amphibolite facies, 4. dolomite (D₃) associated with white mica, chlorite, sphalerite and galena from quartz vein). The structural formulars of dolomites are determined to be Ca_1.00-1.20Mg_0.80-0.99Fe_0.00-0.01Zn_0.00-0.02(CO₃)₂(D₀), Ca_1.00-1.02M_0.97-0.99Fe_0.00-0.01Zn_0.00-0.02(CO₃)₂(D₁), Ca_0.99-1.03Mg_0.93-0.98Fe_0.01-0.05Mn_0.00-0.01As_0.00-0.01(CO₃)₂(D₂) and Ca_0.95-1.04Mg_0.59-0.68Fe_0.30-0.36Mn_0.00-0.01 (CO₃)₂(D₃), respectively. It means that dolomites from Komdok deposit have higher content of trace elements (FeO, MnO, HfO₂, ZnO, PbO, Sb₂O₅ and As₂O₅) compared to the theoretical composition of dolomite. These trace elements (FeO, MnO, ZnO, Sb₂O₅ and As₂O₅) show increase and decrease trend according to paragenetic sequence, but HfO₂ and PbO elements no show increase and decrease trend according to paragenetic sequence. Dolomites correspond to Ferroan dolomite (D₀, D₁ and D₂), and Ferroan dolomite and ankerite (D₃), respectively. Therefore, 1) dolomite (D₀) as hostrock was formed by subsequent diagenesis after sedimentation of Paleoproterozoic (2012~1700 Ma) silica-bearing dolomite in the marine evaporative environment. 2) Early dolomite (D₁) was formed by hydrothermal metasomatism origined metamorphism (amphibolite facies) associated with intrusion (1890~1680 Ma) of Paleoproterozoic Riwon complex. 3) Late dolomte (D₂) was formed from residual fluid by a decrease of temperature and pressure. and dolomite (D₃) in quartz vein was formed by intrusion (213~181 Ma) of Jurassic Mantapsan intrusive rocks.