• Journal of IKEEE
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• v.8 no.1 s.14
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• pp.73-78
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• 2004

In this paper, it is designed for 5.8GHz Wireless LAN sub harmonic resistive mixer. Sub harmonic resistive mixer is constituted by advantage of sub harmonic mixer and resistive mixer. Sub harmonic resistive mixers mix harmonics of LO with RF and obtain IF frequency. Therefore, it was possible to use decreasing LO frequency than conventional mixers. And, Sub harmonic resistive mixer has low IMD because of using unbiased channel resistance of GaAs FET. When LO power is 13dBm, the conversion loss of manufactured sub harmonic resistive mixer is 10.67 dB. And IIP3 of mixer is 21.5dBm.

• Journal of the Korean Geophysical Society
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• v.7 no.3
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• pp.225-232
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• 2004

To investigate the depositional environment and the geological structure of the Jeju Basin in the South Sea of Korea, we acquired 54-channel seismic data of about 1,980 line-km. The study area lies at the northeastern part of the East China Sea Trough, a Tertiary back-arc basin. The sedimentary basin formed by rifted activities resulted in the formation of graben and/or half-graben structures. The basin is composed of pre-rift, syn-rift and post-rift sediments bounded by regional unconformity. The pre-rift and syn-rift sediments consist of Oligocene, Early and Middle Miocene sequence, whereas the post-rift sediments consist of Late Miocene and Plio-Pleistocene sequences. Seismic and well data from the Jeju Basin indicate that Oligocene-Miocene sediments were deposited under fluvial and lacustrine depositional conditions. Following compressional tectonic movements in the Late Miocene time and a subsequent period of erosion, regional subsidence during the Pliocene time brought the Jeju Basin under marine conditions, resulting in the deposition of dominantly marine sediments.

• Proceedings of the KIEE Conference
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• 2006.07c
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• pp.1297-1298
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• 2006

Omega-shaped-gate (OSG) nanowire-based field effect transistors (FETs) have been attracted recently attention due to their highdevice performance expected from theoretical simulations among nanowire-based FETs with other gate geometries. OSG FETs with the channels of ZnO nanowires were successfully fabricated in this study with photolithographic processes. In the OSG FETs fabricated on oxidized Si substrates, the channels of ZnO nanowires with diameters of about 60 nm are coated surroundingly by $Al_{2}O_{3}$ as gate dielectrics with atomic layer deposition. About 80 % of the surfaces of the nanowires coated with $Al_{2}O_{3}$ is covered with gate metal to form OSG FETs. A representative OSG FET fabricated in this study exhibits a mobility of 98.9 $cm^{2}/Vs$, a peak transconductance of 0.4 ${\mu}S$, and an Ion/Ioff ratio of $10^6$ the value of the Ion/Ioff ratio obtained from this OSG FET is the highest among nanowire-based FETs, to our knowledge. Its mobility, peak transconductance, and Ion/Ioff ratio arc remarkably enhanced by 11.5, 32, and $10^6$ times, respectively, compared with a back-gate FET with the same ZnO nanowire channel as utilized in the OSG FET.

• Journal of The Geomorphological Association of Korea
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• v.28 no.1
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• pp.13-33
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• 2021

Successful sediment management at the watershed scale requires an understanding of the erosion, transport and sedimentation processes at the specific site scale. However, studies on the sediment runoff characteristics in a small uppermost watershed, which serves as a sediment supply function, are very rare. Therefore, this study attempted to investigate the fluctuations in major sediment supply areas and sediment runoff in the uppermost mountain small watershed, and for this purpose, ArcSWAT (Soil and Water Assessment Tools with GIS interface) was applied to the Woldong reservoir catchment located in Gosam-myeon, Anseong-si, Gyeonggi-do. The model results were manually calibrated using the monitoring data of the Woldong reservoir sedimentation rate from 2005 to 2007. It was estimated that annual average of 34.4 tons/year of sediment was discharged from the Woldong reservoir basin. This estimate almost coincided with the monitoring data of the Woldong reservoir during the low flow period but tended to be somewhat underestimated during the high flow period. Although the SWAT model does not fully reflect the erosion process of gully and in-channel, this underestimation is probably due to the spatial connectivity of sediment transport and the storage and reactivation of the sediment being transported. Most of the forested hillslopes with a well-developed organic horizon were evaluated as having a low risk of erosion, while the places with the highest risk of erosion were predicted to be distributed in the logged area with some weeds or shrubs (classified as pasture) with relatively steeper slopes, and in the bare land. The results of this study are expected to be useful in developing strategies for sediment control and reservoir management.

• The Korean Journal of Petroleum Geology
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• v.5 no.1_2 s.6
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• pp.9-15
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• 1997

The study area is located in the Central Bransfield Basin, Antarctica. To analyze the morphology of seafloor, structure of basement, and seismic stratigraphy of the sedimentary layers, we have acquired, processed, and interpreted the multi-channel seismic data. The northwest-southeastern back-arc extension dramatically changes seafloor morphology, volcanic and fault distribution, and basin structure along the spreading ridges. The northern continental shelf shows a narrow, steep topography. In contrast, the continental shelf or slope in the south, which is connected to the Antarctic Peninsula, has a gentle gradient. Volcanic activities resulted in the formation of large volcanos and basement highs near the spreading center, and small-scale volcanic diapirs on the shelf. A very long, continuous normal fault characterizes the northern shelf, whereas several basinward synthetic faults probably detach into the master fault in the south. Four transfer faults, the northwest-southeastern deep-parallel structures, controlled the complex distributions of the volcanos, normal faults, depocenters, and possibly hydrocarbon provinces in the study area. They have also deformed the basement structure and depositional pattern. Even though the Bransfield Basin was believed to be formed in the Late Cenozoic (about 4 Ma), the hydrocarbon potential may be very high due to thick sediment accumulation, high organic contents, high heat flow resulted from the active tectonics, and adequate traps.

• Journal of Korea Water Resources Association
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• v.36 no.6
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• pp.925-936
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• 2003

The objective of this study is to suggest new drawing methods of isochrones using GIS. For this purpose the Unit Hydrograph (UH) of studied watershed for instantaneous rainfall suggested by Clark have been determined by routing the time-area curve through a single linear reservoir. To evaluate constructing methods of isochrones three methods has been examined; Channel Profile and Clark-kict method; Laurenson method; Average velocity method of S.C.S. Also, these methods have been recomposed by GIS in this study. To apply first method, spatial modeling, the vector based on the stream network and Route_System measuring a distance between points has been used. A raster based on the flow direction grid from burn DEM and the slope grid from original DEM has been applied for the second method. The third method has been applied by a raster based on the landuse grid and a velocity function expressed by slope. Results by these three methods have been evaluated with observed hydrograph, and the method using average velocity method of S.C.S shows more reasonable results comparatively.

• 한국방재학회:학술대회논문집
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• 2011.02a
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• pp.211-211
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• 2011

지형은 강우에 의한 유역 유출응답을 결정하는 중요한 인자이다. 따라서 유역의 지형형태학적 인자를 수문해석에 이용하기 위한 시도는 긴 역사를 갖는다(Rodriguez-Itube and Valdes, 1979). 지형을 구성하는 대표적인 요소로 하천망과 사면을 들 수 있다. 당연히 이들이 어떤 방식으로 결합되는지에 따라 유출특성의 차이가 발생하게 된다(Zevenbergen and Thorne, 1987; Brierley and Fryirs, 2005). 이에 본 연구에서는 하천유역에서 사면과 하천망의 방향적 특성을 정량화하고, 그 둘 사이의 관계를 살펴보고자 한다. 만일 사면의 방향성과 하천의 방향성이 일정한 관계를 가지고 정량화될 수 있다면, 이러한 특성은 보다 간단히 강우-유출 모형에 고려될 수 있을 것이다. 일례로 확률밀도함수 형태로 제시되는 사면과 하천 방향성을 GIUH 이론에 근거하여 재해석할 수 있다. 궁극적으로는 호우 방향성에 의한 유출응답의 차이를 파악할 수 있게 된다. 본 연구에서는 내성천 유역을 대상으로 하였으며, 대상유역의 수치지형도를 수집하여 DEM을 구축하였다. 하천망 추출을 위해 ArcGIS의 Hydro Tool을 이용하였다. 이들 하천망의 방향성은 von Mises 분포에 적용하여 정량화하였으며, 이를 통해 하천유역에서 하천망의 방향적 특성을 살펴보았다. 추가로 하천망과 사면의 방향적 구조를 확인함으로써 이들 특성이 강우-유출 모형에 유연하게 고려될 수 있도록 하였다. 본 연구의 결과를 요약하면 다음과 같다. (1) 본 연구에서 고려한 von Mises 분포는 하천망의 방향적 특성을 적절히 표현할 수 있음을 확인하였다. 방위 기준으로 정리한 하천망의 방향성은 하나의 mode 특성이 뚜렷하고, 하천 합류점 하천을 기준으로 정리할 경우에는 두 개의 mode 특성이 뚜렷해짐을 알 수 있었다. (2) 하천망의 방향성은 사면의 방향성과 뚜렷한 관계를 갖는 것을 알 수 있었다. 하천망과 사면의 방향적 결합 구조는 유역의 특성을 보다 현실적으로 묘사할 수 있고, 이들 관계를 가정하고 하천망의 방향성이 정량화된다면, 강우-유출 모형에 이들 특성이 쉽게 반영될 수 있을 것으로 기대된다. (3) 하천망의 방향성은 고차 하천일수록 뚜렷한 mode 특성을 나타냄을 확인하였다. 이러한 결과는 고차 하천일수록 그 방향성이 한반도의 주구조선과 잘 일치하는 것으로 기존 연구성과와도 일치하는 것이다. (4) 하천망의 주방향은 하천연장에 대한 영향을 크게 받음을 알 수 있었다. 이는 대상 하천유역의 유역응답에서 하천유출이 사면유출보다 상대적으로 큰 영향력을 갖기 때문이다. 강우-유출 모형에 하천망 방향성을 고려하기 위해서도 하천연장을 고려하여 이들 방향성을 정량화하는 것이 호우 방향에 보다 뚜렷한 유출반응 특성을 나타낼 것으로 보인다. (5) 본 연구에서 고려한 하천망의 방향성 정량화 방안을 이용할 경우 이들 결과는 유출모형에 고려될 수 있을 뿐만 아니라 유출응답 특성을 정량적으로 파악하는데 이용될 수 있다. 방위 기준으로 정리한 하천망 방향성은 실제 유역에 대한 유출모형에 적용이 가능하며, 하천 합류점을 기준으로 정리한 결과는 호우의 방향성에 대한 유출응답의 반응을 정량적으로 살펴보는데 이용될 수 있다.

• Proceedings of the Korean Society of Marine Engineers Conference
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• 2011.06a
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• pp.235-235
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• 2011

Lau basin of south Pacific, as an active back arc basin, is promising area bearing seafloor massive hydrothermal deposit that is located in a subduction zone between the Pacific ocean plate and Indo-Australian continental plate. Korea Ocean Research and Development Institute tracked from 2004 to 2006 the hydrothermal activity to the extension of the northeast Lau Basin, targeting seamount. hydrothermal activity by tracking was found hydrothermal evidences. In this study, Marine seismic survey was carried out in the Lau basin seamount of the possibility of hydrothermal deposit. In particular, Marine magnetic survey and seismic survey was carried out at the same time in TA-12 seamount and noise characteristics were found in the seamount. the main process of data processing is Bandpass filter, FK filter, Deconvolution for noise attenuation such backscatter and multiple reflections. the migration is performed to compensate for reflection points followed by seamount of a slope. In this study, bedrock and upper strata could be identified and in the Future, the comparative method with Multi Beam Echo Sounder(MBES) are likely to derive the correct velocity model, the marine magnetic survey results should be considered.

• The Journal of Korean Medicine Ophthalmology and Otolaryngology and Dermatology
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• v.12 no.1
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• pp.179-214
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• 1999

The result were as follows: 1. Yu Wan So(劉完素) regarded the cause of surgical disease as the heat(熱). He used the three method to drain(疏通), promoting pus drainage(托裏) and the balance between ying-energy(營氣) and wei-energy(衛氣). 2. Jang Jong Jeung(張從正) only refered to medicines without entire theory. 3. Lee Dong Won(李東垣) regarded the cause of surgical disease as the greasy diet(膏梁厚味), damp air(濕氣), wetness heat(濕熱). For each treatment he used the method of Yu Wan So's treatment and emphasized the balance between ying-energy(營氣) and wei-energy(衛氣), stomach energy(胃氣). 4. Ju Jin Heung(朱震亨) distinguished the cause of surgical disease from enternal(內), external(外) and channel(經). For each treatment he used the method to drain(疏通), promoting pus drainage(托裏) and the balance between ying-energy(營氣) and wei-energy(衛氣). The first stage used the clearing away heat and toxic materials(淸熱解毒) and the last stage used the invigoration and dispersion(補托). 5. Yu Wan So(劉完素) used to be very busy of Moschus(麝香), Alumen(白礬), Olibanum(乳香), Coptidis Rhizoma(黃連), Minium(黃丹) and Scutel1ariae Radix(黃芩) In classification of the medical action, great part of the medicine are activating blood circulation to dissipate blood stasis(活血祛瘀), clearing away heat and toxic materials( 淸熱解毒) and external application(外用). 6. Jang Jong Jeung(張從正) used to be very busy of Olibanum(乳香), Angelicae Gigantis Radix(當歸), Minium(黃丹), Myrrha(沒藥), Calomelas(輕粉), Rhei Radix Et Rhizoma(大黃) and Phellodendri Cortex(黃柏). In classification of the medical action, great part of the medicine arc activating blood circulation to dissipate blood stasis(活血祛瘀), clearing away heat and toxic materials(淸熱解毒) and diverged wind-cold evil(發散風寒). 7. Lee Dong Won(李東垣) used to be very busy of Forsythiae Fructus(連翹), Scuteliariae Radix(黃芩), Angelicae Gigantis Radix(當歸). Astragali Radix(황기), Glycyrrhizae Radix(炙甘草), Bupleuri Radix(紫胡), Phellodendri Cortcx(黃柏), and Coptidis Rhizoma(黃連). In classification of the medical action, great part of the medicine are activating blood circulation to dissipate blood stasis(活血祛瘀), regulating vital energy(理氣) and clearing away heat and toxic materials(淸熱解毒). 8. Ju Jin Heung(朱震亨) used to be very busy of Glycyrrhizae Radix(甘草), Astragali Radix(황기), Angelicae Gigantis Radix(當歸), Phellodendri Cortex(黃柏), Scutellariae Radix(黃芩), Ginseng Radix(人蔘), Qlibanum(乳香). In classification of the medical action, great part of the medicine are clearing away heat and toxic materiaIs(淸熱解毒), activating blood circulation to dissipate blood stasis(活血祛瘀) and diverged wind-cold evil(發散風寒).

• The Sea:JOURNAL OF THE KOREAN SOCIETY OF OCEANOGRAPHY
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• v.5 no.2
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• pp.95-104
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• 2000

Depths to four seismic sequence boundaries and the thickness of each sequence were estimated and mapped based on multi-channel seismic data in the Ulleung Basin. These depth-structure and isopach maps were incorporated into the interpretation of gravity and magnetic anomaly maps. The sediment thickness ranges from 3,000 m to 4,000 m in the central basin, while it reaches 6,000 m locally along the southwestern, western, and southeastern margins. The acoustic basement forms a northeast-southwest elongated depression deeper than 5000 m, and locally deepens up to 7,500 m in the southwestern and western margins. Low gravity anomalies along the western and southern margins are associated with basement depressions with thick sediment as well as the transitional crust between the continental and oceanic crusts. Higher gravity anomalies, dominant in the central Ulleung basin, broaden from southwest toward northeast, are likely due to the shallow mantle and a dense crust. A pair of magnetic elongations in the southeastern and northwestern margins appear to separate the central Ulleung basin from its margin. These magnetic elongations are largely dominated by intrusive or extrusive volcanics which occurred along the rifted margin of the Ulleung basin formed during the basin opening. The crust in the central Ulleung Basin, surrounded by the magnetic elongations, is possibly oceanic as inferred from the seismic velocity. The oceanic crust can be mapped in the central zone where it widens to 120 km from the southwest toward northeast. Bending of the crustal boundary in the southern part of the Ulleung Basin suggests that the Ulleung Basin has been deformed by a collision of the Phillipine plate into the Japan arc.