• Journal of the Korean Geotechnical Society
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• v.27 no.3
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• pp.75-83
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• 2011

Emerging issues related with fully coupled Thermo-Hydro-Mechanical (THM) behavior of unsaturated soil demand the development of a numerical tool in diverse geo-mechanical and geo-environmental areas. This paper presents general governing equations for coupled THM processes in unsaturated porous media. Coupled partial differential equations are derived from three mass balances equations (solid, water, and air), energy balance equation, and force equilibrium equation. With Galerkin formulation and time integration of these governing equations, finite element code is developed to find nonlinear solution of four main variables (displacement-u, gas pressure-$P_g$), liquid pressure-$P_1$), and temperature-T) using Newton's iterative scheme. Three cases of numerical simulations are conducted and discussed: one-dimensional drainage experiments (u-$P_g-P_1$), thermal consolidation (u-$P_1$-T), and effect of pile on surrounding soil due to surface temperature variation (u-$P_1$-T).

• Korean Journal of Heritage: History & Science
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• v.43 no.3
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• pp.26-47
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• 2010

When the term conservation is used with regard to excavated features, it means not only conservation but also restoration. Restoring the features here does not imply restoring their original form but restoring their form at the moment of excavation. That means, the conservation of excavated features includes the concept of both reparation and restoration. The way of conserving excavated features can be largely categorized into on-site conservation and transfer conservation. On-site conservation means to conserve excavated features as they were at the excavation site. It can be further categorized into soil-covered on-site conservation, in which excavated features are covered with soil to prevent them from being damaged, and exposed on-site conservation in which the features were conserved as they were exposed. Transfer conservation is operated on the premise that excavated features are transferred to another place. It can be further categorized into original form transfer, transcribing transfer, reproduction transfer, and dismantlement transfer. Original form transfer refers to the method of moving the original forms of excavated features to another place. Transcribing transfer refers to moving some of the surfaces of excavated features to another place. Reproduction transfer refers to restoring the forms of excavated features in another place after copying the forms of excavated features at the excavation site. Dismantlement transfer refers to the method of restoring excavated features in a place other than the excavation site in the reverse order of dismantlement after dismantling the features at the excavation site. The most fundamental issue regarding conserving excavated features is the conservation of their original forms. However, the conservation of excavated features tends to be decided depending on a variety of conditions such as society, economy, culture, and local situations. In order to conserve excavated features more effectively, more detailed and specialized conservation methods should be created. Furthermore, continuing research is needed to find the most effective way of conserving them through exchange with other neighboring academic fields and scientific technology.

• Proceedings of the Korea Water Resources Association Conference
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• 2019.05a
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• pp.260-260
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• 2019

해안과 만나는 하천의 하구부에서는 해수의 흐름에 따른 연안토사의 이동과 유황에 따른 하천상류에서의 토사유입량에 의해 하구부가 빠르게 변화한다. 본 연구대상지인 가곡천은 유로연장이 짧고 경사가 급한 산지하천의 특징을 가지고 있어 집중호우시 토사가 하류로 빠르게 유입되어 일반하천에 비하여 하구부의 지형변화가 크게 일어난다. 가곡천 하구부는 모래사장으로 이루어져 있는 호산해수욕장과 경관적 및 자연적 가치로 인해 보존 필요성이 대두되고 있는 하중도인 솔섬이 위치해 있다. 그러나 현재 솔섬 주변 하구부 인근의 일반산업단지 건설과 고향의 강 조성사업에 따른 하도환경의 변화로 하도를 유하하는 유수의 흐름 및 침퇴적 양상의 변화를 가져와 홍수의 원활한 소통에 지장을 초래하고 있다. 또한 현장조사 및 모니터링 결과 하구 지형변화로 인해 하도안정 유지관리에도 막대한 영향을 끼치는 것으로 확인되었다. 따라서 본 연구에서는 가곡천 하구부의 하도환경 변화에 따른 수리학적 특성 및 하천형태학적인 변화를 분석하여 하도안정을 파괴하는 요인을 규명하기 위한 연구를 수행하였다. 연구방법은 가곡천 하천정비기본계획의 빈도별 홍수량, 기점홍수위를 경계조건으로 2차원 수리해석 모형인 SRH-2D모형을 이용하여 하도환경 변화 전 후의 대상구간에 대해 수리특성 및 하상변동 양상을 모의하였다. 모의결과 하도환경 변화(홍수터 및 징검여울 등의 하천시설물 조성)에 따른 수리특성변동양상과 침 퇴적지점에 대한 변동경향을 확인할 수 있었다. 본 연구의 결과는 동해안 하구부에 위피한 하천의 다양한 변화 해석시 참고자료로 활용할 수 있을 것으로 사료된다.

• Conservation Science in Museum
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• v.4
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• pp.47-55
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• 2003

Among many artifacts donated by Yoo Chang-jong, we duplicated and performed conservation treatment for a colored brick(J3432), a roof tile with monster-mask design(J1886) and a mould for roof tiles with monster-mask design(J1882). We focused on the restoration of the paint layer for the colored brick. As for the roof tile with monster-mask design, we cleared the existing poorly repaired part and then performed a complete conservation treatment. We would like to present the process to duplicate a roof tile with monster-mask design using a real mould, for the special exhibition entitled "Donated Tiles of Yoo Chang-jong".

• Journal of The Korean Association For Science Education
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• v.24 no.3
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• pp.417-428
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• 2004

Conservation reasoning makes operational thought possible as a functional tool and it is the essential concept not only in the area of science and mathematics but also in several aspects of daily life. The abilities to solve mathematical problems and that of scientific reasoning and abstract way of thinking depend on whether thereis conservation reasoning or not and they are critical concepts that enables us to confirm the steps of cognitive development. Therefor in the study, we emphasized the issue that is the ways to speed up the scientific era by analyzing the correlation between the formation of conservation reasoning and neuro-cognitive variables. About 50% of 1-3 grade students did not had conservation reasoning skills. The formation of conservations was not linear. Scientific reasoning ability, planing and inhibiting ability were significantly different in levels of conservation, And, conservation reasonings were significantly correlated with cognitive variables. Scientific reasoning and planning ability significantly explained about 20% of the conservation reasoning ability of 1-3 grades.

• Journal of the Korean Geographical Society
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• v.39 no.6 s.105
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• pp.863-872
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• 2004

The coastal alluvial plain, sand dune, tidal nat might be the most prominent coastal landscape in western coast of Korea. The purpose of this paper is to examine the irrigation and drainage systems of the alluvial plain in the tidal coast. This study is concerned on the geomorphological and cultural landscapes of the alluvial plain in the western coast of the South Jeolla Province. The alluvial deposits have developed mainly by the actions of tidal currents, rather than transporting sediments by stream. The transformation of plain has been affected by human agency since 1920's. Dwellers have constructed the reservoir, banks, dammed pools, lock gates, and tide-dykes for the reclamation, irrigation, and drainage on the alluvial plain, coastal sanddune, and tidal flats.

• Journal of the Korean Society of Groundwater Environment
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• v.5 no.1
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• pp.21-29
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• 1998

Groundwater exploitation from fissured bedrocks is increasing in Korea and over-withdrawn from a lot of production wells may cause exhaution of groundwater in the fissured aquifer. To conserve groundwater resources, it is needed to exactly determine the optimal yield of production wells. The optimal yield of the production wells can be determined as using suitable aquifer models with appropriate hydraulic parameters and natural recharge of the region. We applied the technique for evaluating optimal yield to the pumping test conducted in Mountain Geumryeon of Pusan City and analyzed its applicability.

• Water for future
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• v.27 no.1
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• pp.101-109
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• 1994

Characteristics of the vortex structure and the secondary scour at downstream part of the hydraulic structure such as drainage sluice or spillway ere studied. Mean shear velocity in the scour hole could be derived by the theory of energy conservation and the amount of a vortex erosion could be obtained using entrainment equation for given value of a shear velocity. Comparison of erosion rates with others showed a large value at low shear velocity due to the continuous and strong upward flow of the macroturbulence different from the conventional vortex formed in the lee-side of a sand ripple. For a design purpose, if the flow depth at the end of an apron and the properties of bed material are given, the amount of vortex erosion can be known.

• Proceedings of the Korea Water Resources Association Conference
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• 2008.05a
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• pp.2085-2089
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• 2008

수자원 개발이 자연 하천 생태계에 미치는 다양한 악영향들은 하천에 서식하는 동 식물의 생태서식지의 변화를 초래할 수 있다. 하천생태계를 보전하고 복원하기 위해서는 수리학과 생물학이 연계된 생태수리학적 모형을 지속적으로 연구 개발하여 수자원 개발에 따른 장래의 물리적인 거동을 비교적 정확하게 분석 및 예측하는 것이 필요하다. 본 연구의 목적은 21세기 프론티어 연구사업 'RAMS (River Analysis and Modeling System) 적용' 과제 중 개발된 RAM2, RAM4, RAM6 해석 모형으로부터 유속, 수위, 수온, SS, 하상고, 하상재료 데이터를 받아들여 GIS와 연계하는 2차원 하천 생태 모형 (RAM 8)을 개발하는 것이다. 그리고 개발에 따른 모형 검증을 위해서 우리나라 4대 강 중 유일하게 하구둑이 설치되어 있지 않아 자연적인 하천지형과 기수역 생태계가 잘 보존된 한강 하구부를 적용구간으로 선정하여, 서식지 적합성을 판단하고 그에 따른 적정 유량을 산정하여 1차원 서식처 모형인 PHABSIM을 이용한 결과와 비교한다.

• Proceedings of the Korea Water Resources Association Conference
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• 2023.05a
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• pp.516-516
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• 2023

하천 만곡부 외곽 하안부의 빠른 유속은 침식을 유발하고 내측의 느린 유속은 토사 퇴적의 원인이 된다. 이는 하천 지형을 지속적으로 변화시키는 원인이 되고 나아가 하천 주변의 환경뿐만 아니라 안정성에도 문제를 일으킨다. 하천의 안정성과 수생태계 보존을 위해서는 수제와 같은 인공 구조물을 설치하여 하도의 안정을 유지할 수 있다. 수제는 후류에 느린 유속을 발생시켜 침식을 예방하고 제방과 하안을 보호한다. 그러나 수제 주변에서 발생하는 강한 와류는 국부 세굴을 유발하여 구조물의 안정성을 저해하기도 한다. 본 연구에서는 이동상 수리실험을 통해 수제 주변에서 발생하는 국부 세굴 및 후류에서의 하상 변동을 측정하였다. 수리실험은 길이 10 m, 폭 0.44 m, 높이 0.59 m인 수로에서 D50 = 2.98 mm인 모래를 사용하였고 하상변동은 하상이 평형상태에 이르렀을 때 물의 흐름을 멈추고 측정하였다. 실험 결과를 바탕으로 평형상태의 하상변동과 시간 변화에 따른 세굴심 변화를 도출하였다.