• The Journal of the Korea institute of electronic communication sciences
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• v.15 no.1
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• pp.173-178
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• 2020

A multi-ray model has been used to interpret radio transmission losses in half-canyon structures with slope and to formulate a multi-ray propagation model depending on the angle of slopes. The cut-off angles for the third and fourth paths, which are the slope-sided reflection paths of the transmission and reception radio waves determined by the inclined angles of the slope, were calculated with the height and location of the transmitter and receiver. To predict transmission losses in an inclined plane environment, the embankment environment where the actual slope exists was modeled and simulated to calculate the loss of propagation transmission, and the radio wave transmission loss was confirmed by the measurement for the frequency band 1 to 6 GHz. Simulation results and measurement results showed similar trends in radio transmission loss, and radio transmission loss predictions and measurement results for various terrain information can be used in the design of radio propagation service.

• Proceedings of the Korean Institute of Building Construction Conference
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• 2008.11a
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• pp.193-197
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• 2008

This study enforced to produce the planting concrete block which could be applied to various slopes economically. First of all, the physical properties was investigated with the various types of aggregate and aggregate ratio of the paste for the lead to mixture proportion of the planting concrete. As a result, the orchid stone as aggregate and 30% of aggregate ratio of the paste were used as the basic mixture proportion considering 20~30% of maintained void ratio for the growth of plant, over 20% of capillary suction for holding water, and 3MPa as the minimum strength. For the result of the test to the new planting block which was quite different from existing planting concrete block, it could complement the problems and be possible to produce effectively and economically because various slopes like 40ﾟ~75ﾟ, continual produce by extrusion, and pumping out were possible were possible.

• Proceedings of the Korea Concrete Institute Conference
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• 2008.04a
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• pp.437-440
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• 2008

This study enforced to produce the planting concrete block which could be applied to various slopes economically. First of all, the physical properties was investigated with the various types of aggregate and aggregate ratio of the paste for the lead to mixture proportion of the planting concrete. As a result, the orchid stone as aggregate and 30% of aggregate ratio of the paste were used as the basic mixture proportion considering 20${\sim}$30% of maintained void ratio for the growth of plant, over 20% of capillary suction for holding water, and 3MPa as the minimum strength. For the result of the test to the new planting block which was quite different from existing planting concrete block, it could complement the problems and be possible to produce effectively and economically because various slopes like $40^{\circ}{\sim}75^{\circ}$, continual produce by extrusion, and pumping out were possible were possible.

• 한국전산유체공학회:학술대회논문집
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• 2003.08a
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• pp.69-75
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• 2003

본 연구에서는 격자 생성, 초기유동조건 및 경계조건 설정 등 일련의 전처리 과정을 사용자에게 친숙한 그래픽 인터페이스 환경으로 개발하였다. MFC/Visual C++를 이용하여 개발된 전처리 프로그램은 Windows 계열의 OS와 호환이 가능하며, 기하학적 격자생성, 초기값 설정 및 수치해석 코드의 제어변수를 생성할 수 있다. 한편 사용자의 편의를 위해서 전처리 과정을 격자생성(단일격자생성, 다중격자생성), 유체 물성치정의, 경계조건 생성, 초기조건 생성 및 코드제어로 구분하였다. 개발된 전처리 프로그램의 특성으로서 다중 격자 생성 작업을 단일 격자계의 중첩으로 구성될 수 있도록 각 경계면을 "interface"형을 취하는 기능을 제공하도록 하였으며 개발된 전처리 과정을 16도의 경사면을 가지는 Compression ramp 문제 및 축대칭 Bump 문제에 적용하여 개발된 전처리 과정을 검증하였다.

• Proceedings of the KAIS Fall Conference
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• 2007.11a
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• pp.201-204
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• 2007

본 논문에서 디지털지도를 이용하여 다중경로 전파의 특성을 연구하였다. 일반적으로 목표물에서의 전계의 세기는 직접파와 지면 반사파의 합으로 구해진다. 이 논문에서는 수직면의 장애물인 고압선, 철탑, 산악지형의 경사면 등에 의한 반사파를 고려하여 전체 전계를 계산 하였다. 그리고 지면 반사의 경우, 지면의 경사를 고려하여 목표물에서의 전체 전계의 정확도를 향상시켰다.

• Economic and Environmental Geology
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• v.49 no.2
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• pp.121-134
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• 2016

We characterize the spatial distribution of Cobalt-rich ferromanganese crusts covering the summit and slopes of a seamount in the western Pacific, using acoustic backscatter from multibeam echo sounders (MBES) and seafloor video observation. Based on multibeam bathymetric data, we identify that ~70% of the summit area of this flattopped seamount has slope gradients less than $5^{\circ}$. The histogram of the backscatter intensity data shows a bi-modal distribution, indicating significant variations in seabed hardness. On the one hand, visual inspection of the seafloor using deep-sea camera data exhibits that the steep slope areas with high backscatter are mainly covered by manganese crusts. On the other hand, the visual analyses for the summit reveal that the summit areas with relatively low backscatter are covered by sediments. The other summit areas, however, exhibit high acoustic reflectivity due to coexistence of manganese crusts and sediments. Comparison between seafloor video images and acoustic backscatter intensity suggests that the central summit has relatively flat topography and low backscatter intensity resulting from unconsolidated sediments. In addition, the rim of the summit and the slopes are of high acoustic reflectivity because of manganese crusts and/or bedrock outcrops with little sediments. Therefore, we find a strong correlation between the acoustic backscatter data acquired from sea-surface multibeam survey and the spatial distribution of sediments and manganese crusts. We propose that analyzing acoustic backscatter can be one of practical methods to select optimal minable areas of the ferromanganese crusts from seamounts for future mining.

• Proceedings of the Korea Water Resources Association Conference
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• 2012.05a
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• pp.696-696
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• 2012

호안은 유수의 침입으로부터 제방 및 하안의 침식 피해를 방지하기 위해 제방에 설치되는 구조물이다. 침식에 의한 제방 및 호안의 대표적인 붕괴특성 중에는 만곡부, 하천 급경사, 지형의 간섭효과 등이 있다. 특히, 만곡부는 원심력, 2차류 등에 의한 수위상승 및 유속증가로 제체에 응력 집중이 발생되어 안정성 저하를 유발할 수 있다. 또한, 만곡부의 흐름 방향전환 현상은 하도내 통수능 저하를 발생시켜 홍수피해를 가중시킬 수 있다. 따라서 하천특성상 만곡부에 의해 발생할 수 있는 홍수피해 요소를 저감시킬 수 있도록 적합한 피해저감대책을 마련할 필요가 있다. 제방의 보강대책으로서 활용되고 있는 호안은 역학적인 측면에서 외력과 저항력의 크기에 따라 안정성이 평가되어야 하며 지역여건 등에 따른 만곡부의 수위상승 및 제방 침식 등을 고려한 설계가 수행되어야 한다. 국내 실무에서 적용되고 있는 호안설계방법은 하천설계기준 해설(2009)을 참고하고 있는데, 흐름현상 및 만곡부 특성 등에 대하여 경험과 이론의 양면을 고려한 설계를 수행하도록 제안하고 있다. 이는 호안 안정성에 대한 역학적 검토 방법의 한계로 비합리적 설계가 될 우려가 있다. 따라서 만곡부에 의한 유속 및 소류력 등 흐름특성을 고려한 정량적인 평가기법이 요구되는 상황이다. 본 연구에서는 수리실험을 통해 만곡에 의한 흐름영향과 수리학적 거동 및 설계요소를 파악하고자 만곡부에 사석호안공을 설치하여 흐름전환 및 유속변화에 따른 사석호안공의 이탈현상을 재현하였다. 실험수로는 곡률반경( )이 4.5 m인 만곡부가 3개소 발생하는 폭 2.3 m, 길이 25 m의 다중 사행수로 형태이다. 실험수로 우안의 1V:2H 경사면에 10, 20, 30, 40, 50 mm 사석을 크기별로 설치하여 만곡에 의한 유속변화 등 흐름현상과 호안공 이탈을 관찰하였다. 수리실험은 고정상으로 수행되었으며 정상류 흐름조건에서 공급유량별 하류단 수위 조절을 통해 만곡부내 호안 공 이탈을 발생시키는 설계인자를 도출하고자 유속과 수심을 측정하였다. 실험결과를 바탕으로 사석호안공 설계시 1차원 접근유속에 만곡 영향을 고려하여 대표유속으로 적용하는 방법의 특성을 파악하고, 사석호안공의 이탈유속과 만곡에 의한 흐름특성간의 상관관계를 분석하여 제원결정기법을 제안하였다.

• Journal of the Korean Association of Geographic Information Studies
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• v.19 no.3
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• pp.89-101
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• 2016

This study examined spatial disposition of wildlife highway mortality using road-kill GIS database and Naver panoramic 360 degree views to find out which habitat and road variables most influenced road-kill numbers for each mammal species and how the landscape and road elements are connected on highway. Road-kills on Yeongdong(YD) and Jungbu highway(JB) generally tended to be higher in natural barren, grassland and cropland due to its value of preferred habitats of nocturnal and multihabitat species like water deer(Hydropotes inermis argyropus), raccoon(Nyctereutes procyonoides) and hare(Lepus coreanus). Land cover in YD showed no difference between species (p=0.165) while JB did by species (p=0.001). This may be explained by disparate landscape between mountain and urban or the fact that YD in long term operation might have enabled consistent crossing pattern compared to JB experiencing continuous extension works which may in turn have deviated the road crossing. Although road-kill prevention effect of local topography alone was appreciable, compared to less significant or ineffective fence and guardrail, gentle slope declining in a direction to the road turned out to offset the preventive effect of juxtaposed fence. Furthermore, green patches on road near intersection were deemed a visual stepping stone facilitating wildlife attempted crossing and local roads juxtaposed with a highway were especially left defenceless to road-kill without road barriers.

• Economic and Environmental Geology
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• v.39 no.3 s.178
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• pp.235-253
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• 2006

We interpreted marine seismic profiles in conjunction with swath bathymetric and magnetic data to investigate rifting to breakup processes at the Korean margin leading to the separation of the Japan Arc. The Korean margin is rimmed by fundamental elements of rift architecture comprizing a seaward succession of a rift basin and an uplifted rift flank passing into the slope, typical of a passive continental margin. In the northern part, rifting occurred in the Korea Plateau, a continental fragment extended and partially segmented from the Korean Peninsula, that provided a relatively broader zone of extension resulting in a number of rifts. Two distinguished rift basins (Onnuri and Bandal Basins) in the Korea Plateau we bounded by major synthetic and smaller antithetic faults, creating wide and symmetric profiles. The large-offset border fault zones of these basins have convex dip slopes and demonstrate a zig-zag arrangement along strike. In contrast, the southern margin is engraved along its length with a single narrow rift basin (Hupo Basin) that is an elongated asymmetric half-graben. Rifting at the Korean margin was primarily controlled by normal faulting resulting from extension in the west and southeast directions orthogonal to the inferred line of breakup along the base of the slope rather than strike-slip deformation. Although rifting involved no significant volcanism, the inception of sea floor spreading documents a pronounced volcanic phase which seems to reflect slab-induced asthenospheric upwelling as well as rift-induced convection particularly in the narrow southern margin. We suggest that structural and igneous evolution of the Korean margin can be explained by the processes occurring at the passive continental margin with magmatism intensified by asthenospheric upwelling in a back-arc setting.