• Journal of Korean Society of Transportation
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• v.22 no.1 s.72
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• pp.43-62
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• 2004

Conventionally the estimation method of the origin-destination Matrix has been developed by implementing the expansion of sampled data obtained from roadside interview and household travel survey. In the survey process, the bigger the sample size is, the higher the level of limitation, due to taking time for an error test for a cost and a time. Estimating the O-D matrix from observed traffic count data has been applied as methods of over-coming this limitation, and a gradient model is known as one of the most popular techniques. However, in case of the gradient model, although it may be capable of minimizing the error between the observed and estimated traffic volumes, a prior O-D matrix structure cannot maintained exactly. That is to say, unwanted changes may be occurred. For this reason, this study adopts a conjugate gradient algorithm to take into account two factors: estimation of the O-D matrix from the conjugate gradient algorithm while reflecting the prior O-D matrix structure maintained. This development of the O-D matrix estimation model is to minimize the error between observed and estimated traffic volumes. This study validates the model using the simple network, and then applies it to a large scale network. There are several findings through the tests. First, as the consequence of consistency, it is apparent that the upper level of this model plays a key role by the internal relationship with lower level. Secondly, as the respect of estimation precision, the estimation error is lied within the tolerance interval. Furthermore, the structure of the estimated O-D matrix has not changed too much, and even still has conserved some attributes.

• Journal of the Korean earth science society
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• v.43 no.6
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• pp.680-690
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• 2022

Tephrochronology uses regional tephra for age dating and stratigraphic correlations. Regional tephras are important in Quaternary geology and archaeology because they can be used as stratigraphic time-markers. In this review, identification and dating methods of tephra are summarized. In addition, the characteristics of regional tephras in terrestrial deposits of the Korean Peninsula are elaborated, and geological applications and limitations of the regional tephra layers are also discussed. So far, AT, Ata, and Kb-Ks tephra layers from Kyushu, Japan have been found in Pleistocene paleosol, marine terrace deposits, and lacustrine deposits in Korea. Also, although not officially confirmed, Aso-4 tephra is likely to occur in terrestrial deposits. The regional tephra layers are vital for dating, especially with regard to sediments over 50 ka beyond the range of radiocarbon dating, and for dating of active faults. Furthermore, it can provide important information for preparing countermeasures against volcanic disasters. However, in order to use the tephra layer geologically, it must be confirmed whether it is a primary deposit based on sedimentological study.

• Proceedings of the Optical Society of Korea Conference
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• 2005.07a
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• pp.28-29
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• 2005

본 논문에서는 MEH-PPV와 DFPP의 폴리머 물질을 이용하여 photovoltaic device가 제작되었고, 그림 1에 두 물질의 분자 구조가 보여진다. Photovoltaic cell의 전기-광학적 특성은 활성층의 폴리머 물질에 의해 결정된다. 이러한 특성을 알아보기 위해서 홉수 스펙트럼이 측정되었다. DFPP는 chloroform, chlorobenzen, THF, acetone에 잘 녹았으며, 본 논문에서는 chloroform이 용매로 사용되었다. 제작 공정은 다음과 같다. 인듐 주석 산화물 (ITO)이 증착된 유리기판은 photolithography 공정을 거친 후, 왕수(HNO$_{3}$ + HCL)로 식각됨으로서 전극의 패턴이 제작되었다. 그리고 ITO 전극 패턴 된 유리기판 위에 PEDOT (CH8000, Baytron)이 코팅된 후 Ar이 주입되는 Convection Oven을 이용하여 120$^{\circ}$C에서 2시간 동안 열처리되어 수분이 제거되었다. 활성층에는 MEH-PPV와 DFPP가 9:1과 2.33:1로 혼합된 폴리머가 사용되었고, 이것은 0.3 %w.t.가 되도록 chloroform에 넣어 5시간 동안 스핀바를 돌려서 용해되었다. 이 용액은 ITO 전극 패턴이 형성된 글라스 위에 3000 rpm으로 45 초간 스핀코팅 되었다. 이 때 얻어진 유기물 박막층은 80$^{\circ}$C의 Ar이 주입되는 convection oven에서 3시간 동안 경화되었다. 경화된 단층 유기물 박막층 위에 Li-Al이 1000 ${\AA}$의 두께로 증착되어 전극이 형성되었고, 이후 질소가 채워진 globe box에서 소자는 encapsulation되어 산소와 수분에 대한 영향으로부터 차단되었다. 상기의 공정으로 제작된 소자의 박막구조는 그림 2에서 보여진다. 그림 3은 MEH-PPV와 DFPP를 혼합했을 때의 흡수 스펙트럼이다. 최대 흡수 파장은 511 nm였다. 그리고 photovoltaic cell의 V-I 특성 결과가 그림 4와 같이 측정되었다. 측정에서는 300${\sim}$700 nm의 파장대를 갖는 태양광 모사계가 사용되었고, 셀의 면적은 10 mm$^{2}$였다. 그림 5의 I-V 특성으로부터 MEH-PPV와 DFPP가 9:1 로 혼합했을 때보다 2.33:1 로 혼합했을 때, photovoltaic device의 효율이 향상됨을 확인할 수 있다. 빛이 75 mW/cm$^{2}$ 의 세기로 조사될 때 9:1과 2.33:1로 혼합된 소자의 open circuit voltage (V$_{oc}$)는 비슷하지만, short circuit current Density (J$_{sc}$)는 각각 -1.39 ${\mu}$A/cm$^{2}$ 와 -3.72${\mu}$A/cm$^{2}$ 로 약 2.7배 정도 증가되었음을 볼 수 있다. 이러한 결과를 통해 electron acceptor인 DFPP의 비율이 높아질수록 photovoltaic cell의 conversion efficiency가 더 크게 됨을 확인할 수 있다. 그러므로 효율이 최대가 되는 두 폴리머의 혼합 비율이 최적화되는 조건을 찾는 것은 매우 중요한 연구가 될 것이다.

• The Journal of Engineering Geology
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• v.17 no.1 s.50
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• pp.15-25
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• 2007

In general, the life and asset casualties that occur due to landslide or slope failure in urban areas are larger than that in rural areas. In order to reduce the casualties, a slope management program is necessary to categorize slopes based on properties and to manage them systematically. The slope management system is the establishment of the data base for the geological and geotechnical factor according to slope stability, and the utilization of the data base to manage slopes. The suitable system must develop to slopes in urban area through the survey, analysis and evaluation process. Based on the above necessity, the slope management program which is applicable to slope management in an urban area has been developed at Hwangryung Mt. in Busan as a target area. The developed slope management program has various functions such as slope ID number of each slope or sub-region of a mountain, making a slope data sheet, analysis and grouping of slope stability, and establishment of a data base. The slope management program is constructed by use of GIS, and the survey, test and analysis data according to all slopes can be input and edited into the program. The program can also be utilized practically by end users due to the convenient input, edition printing, management and operation of slope data. Therefore, the slope management system has been established on the application of the developed program in Busan which is located in slope area. As the system is widely applied to other cities, the slope in urban area can be managed systematically and the slope hazards can be minimized.

• Journal of the Institute of Electronics Engineers of Korea CI
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• v.44 no.2 s.314
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• pp.37-46
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• 2007

In this paper, we propose technologies for enhancing the immersive realization of virtual objects in AR-based product design. Generally, multimodal senses such as visual/auditory/tactile feedback are well known as a method for enhancing the immersion in case of interaction with virtual objects. By adapting tangible objects we can provide touch sensation to users. A 3D model of the same scale overlays the whole area of the tangible object so the marker area is invisible. This contributes to enhancing immersion. Also, the hand occlusion problem when the virtual objects overlay the user's hands is partially solved, providing more immersive and natural images to users. Finally, multimodal feedback also creates better immersion. In our work, both vibrotactile feedback through page motors, pneumatic tactile feedback, and sound feedback are considered. In our scenario, a game-phone model is selected, by way of proposed augmented vibrotactile feedback, hands occlusion-reduced visual effects and sound feedback are provided to users. These proposed methodologies will contribute to a better immersive realization of the conventional AR system.

• The Journal of Engineering Geology
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• v.25 no.4
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• pp.557-576
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• 2015

Groundwaters in granite, gneiss, and two-mica granite formations, including faults, in the Hoengseong area are examined to determine the relationship between their uranium and radon-222 contents and rock types. The chemical compositions of 38 groundwater samples and four surface water samples collected in the study area were analyzed. Sixteen of the samples showing high uranium and radon-222 contents were repeatedly analyzed. Surface radioactivities were measured at 30 points. The uranium and radon-222 concentrations in the groundwater samples were in the ranges of 0.02-49.3 μg/L and 20-906 Bq/L, respectively. Four samples for uranium and 35 samples for radon had concentrations exceeding the alternative maximum contaminant level of the US EPA. The chemical compositions of groundwaters indicated Ca(Na)-HCO₃ and Ca(Na)-NO₃(HCO₃+Cl) types. The pH values ranged from 5.71 to 8.66. High uranium and radon-222 contents in the groundwaters occurred mainly at the boundary between granite and gneiss, and in the granite area. The occurrence of uranium did not show any distinct relationship to that of radon-222. The radon-222, an inert gas, appeared to be dissolved in the groundwater of the aquifer after wide diffusion along rock fractures, having been derived from the decay of uranium in underground rocks. The results in this study indicate that groundwater of neutral or weakly alkaline pH, under oxidizing conditions and with a high bicarbonate content is favorable for the dissolution of uranium and uranium complexes such as uranyl or uranyl-carbonate.