• 한국해안·해양공학회논문집
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• 제35권6호
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• pp.121-127
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• 2023

바람에 의한 모래이동(비사이동) 연구는 1941년 Bagnold가 사막 조건에서 바람에 의한 모래 이동량 연구를 최초로 수행하며 시작되었다. 비사이동 연구는 사막을 대상으로 주로 수행되었으며, 해안 공학 분야에서는 1980년 이후 Bagnold 공식을 연안에 접목하며 시작되었다. 하지만 해안에 Bagnold 공식을 사용할 경우 비사 이동량을 과대 산정함이 많은 연구에 의해 제시되었다. 현재 간단한 형태부터 다양한 센서를 활용한 비사 포집기가 개발되었고 연구에 활용되고 있다. 하지만 이러한 비사 포집기는 포집기 별로 포집 성능의 차이가 크다는 단점이 있다. 성능의 차이가 크다는 것은 결과의 신뢰성 및 정확성이 낮다는 것을 의미한다. 또한 기존 포집기의 경우 포집된 모래의 양으로만 분석을 수행하며, 비사 이동속도나 농도에 대한 정량적 분석은 어렵다. 따라서 본 연구에서는 이미지 분석 기법을 이용하여 비사의 이동속도 측정 정확도를 평가하고 연구에 활용할 수 있는 방안을 제시한다.

• 한국지형학회지
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• 제24권3호
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• pp.61-81
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• 2017

Traditional approaches to surface moisture problems in the context of aeolian research have focused on the initiation of sand movement, developing various models for predicting threshold velocity on a wet surface. They have been unsatisfactory, however, in explaining field observations because they have not incorporated spatiotemporal variability of surface moisture, the interactions between transported sand grains and surface, and the role of aeolian transport in controlling surface moisture. As Nield (2011) showed, a simplified numerical model can be used to investigate this issue. This research aims to explore the feedback structures between aeolian transport and surface moisture using a modified sand slab model. Key modifications are the introduction of simultaneous updating scheme for all the slabs and moisture-assigning procedures with and without aeolian transport. The major findings are as follows. Moist surface conditions suppress sand slab movement, leading to the development of smaller-scale topography. Available sands for aeolian transport are determined by the vertical patterns of moisture content with its variations from groundwater to the surface. Sand patches on a wet surface act as a localized source area. Sand movement drives immediate changes in surface moisture rather than time-lag reponses, mostly when moist conditions are dominant.

• 한국해양공학회:학술대회논문집
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• 한국해양공학회 2002년도 추계학술대회 논문집
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• pp.234-239
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• 2002

Acoustic sounds generated by a uniform flow around a two-dimensional circular cylinder at Re=200 are simulated using finite difference lattice Boltzmann method. A third-order-accurate up-wind scheme is used for spartial derivatives, and a second-order-accurate Runge-Kutta scheme is used for time marching. The results show that in capturing very small acoustic pressure fluctuation with same frequency of Karman vortex street compared with the pressure fluctuation around a circular cylinder. The propagation velocity of acoustic sound is presented that acoustic which approaches tire upstream due to Doppler effect in the uniform flow slowly propagates, while that for the downstream quickly propagates. It is also apparent that the size of sound pressure is proportional for central distance $r^{-1/2}$ of the cylinder.

• 한국지형학회지
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• 제26권2호
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• pp.15-27
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• 2019

This study tries to reveal transport mechanism and origin of components from fluvial terrace deposits in Danyang and Geum River basins, through grain size partitioning using the Weibull function. Grain size parameters suggest that the samples analyzed in this study can be grouped into the coarse, fine and medium samples. The coarse samples are partitioned into three or four components. More than 65% of the coarse samples consist of components by suspension and saltation by fluvial process, while components by attachment to coarse grains or aggregates and/or by individual grains deposited under non-flow condition are also found in the coarse samples. The fine samples consist of four components and components found in loess deposits in Korea occupy >70%, suggestive of the same transport mechanisms (westerlies and winter monsoon) and common source areas with loess deposits in Korea. However, components by aeolian process from local sources as well as by fluvial process are also found in the fine samples. The medium samples are partitioned into components with similar sizes to the coarse and fine samples, respectively.

• 한국가시화정보학회:학술대회논문집
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• 한국가시화정보학회 2005년도 추계학술대회 논문집
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• pp.11-16
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• 2005

Saltation is the most important mechanism of wind-blown sand transport. Till now the interaction between wind and sand has not been fully understood. In this study the saltation of sand sample taken from Taklimakan desert was tested in a simulated atmospheric boundary layer. The captured particle images containing both the tracers for wind and saltating sand, were separated by a digital phase mask technique. Both PIV and PTV methods were employed to extract the velocity fields of wind and the dispersed sand particles, respectively. The mean streamwise wind velocity field and turbulent statistics with and without sand transportation were compared, revealing the effect of the moving sand on the wind field. This study is helpful to understand the interaction between wind and blown sand (in saltation), and provide reliable experimental data fur evaluating numerical models.

• 한국토양비료학회지
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• 제49권6호
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• pp.635-643
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• 2016

Wine consumers desire to drink a high quality wine. For producing high quality wine, high quality soil is required. Conventionally, soil quality is assessed qualitatively. Using traditional laboratory methods, quantitative data can be obtained for management purpose, but it is time consuming and expensive. Therefore, new technology aims to address these limitations, namely portable X-Ray fluorescence spectrometers (pXRF). This instrument can be used directly in the field, requires no soil sample preparations, and can simultaneously measure a wide range of elements qualitatively that are useful for pedological studies. The chemical composition (Ca, Fe, Ti and Zr) of soils at Tallavera Grove vineyard in New South Wales, Australia, was studied using a pXRF. The analysis of the soil's elemental concentration (i.e. Ca and Fe) using pXRF supports management decisions. Measuring the soil's Ca concentration can be used to identify Ca-rich parent materials (limestone). The limestone indicates good soil conditions for vine production. Fe content was used to identify areas of texture-contrast soils or soil with accumulation of clays in the B horizon. In addition, a soil weathering index was calculated using elemental concentrations (i.e. Ti and Zr) to explore the history of soil formation for making decision of management. This index showed that the soil in the vineyard was affected by two processes: the deposition of materials from elsewhere (Aeolian transport or soil erosion) and mixing of materials from upslope.

• 한국지형학회지
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• 제19권1호
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• pp.17-27
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• 2012

해안사구는 사빈과의 상호작용을 통하여 해안경관을 안정시키고 배후지를 방어한다. 때때로 태풍이 통과할 때 사구가 침식되기도 하지만, 시간이 지나면 원래의 지형을 회복한다. 2010년 9월초에 발생한 태풍 곤파스는 많은 비를 동반하며 폭풍과 파고를 증가시켜 해안지역에 수위를 상승시켰다. 이로 인해, 서해안에 분포하는 사구들이 피해를 입었다. 하지만 침식이나 회복과정은 전안과 사구전면부의 경사, 모래의 공급량, 식생, 바람, 인간의 간섭 등 해빈-사구를 둘러싼 환경에 따라 차이가 있었다. 어떤 사구들은 겨울철 풍성활동에 의해 원래의 단면을 회복했지만, 어떤 사구들은 점점 더 육지 쪽으로 후퇴하였다. 곰솔림이 조성된 해안사구는 초본피복사구에 비해 회복이 더딘 것으로 나타났다. 또한 인공호안이 설치된 사구는 그렇지 않은 사구에 비해 더 심하게 침식되고 덜 회복되었다. 태풍 통과 이후의 조사결과, 모래의 이동과정이 침식된 사구 지형회복에 가장 중요한 역할을 한 것으로 나타났다. 따라서 태풍에 의한 침식극복을 비롯하여, 사구의 효과적인 관리를 위해서는 지형학적 관점에서 사빈과 사구의 상호작용을 적절하게 평가해야 한다.