• Title/Summary/Keyword: Sand bars

Search Result 77, Processing Time 0.028 seconds

Thematic and geometric analysis of Bangpo beach based on UAV Remote Sensing (무인항공기반 태안반도 방포해빈의 지형분석)

  • Bae, Sungji;Yu, Jaehyung;Jeong, Yong-Sik;Yang, Dongyoon;Han, Min
    • Journal of The Geomorphological Association of Korea
    • /
    • v.23 no.1
    • /
    • pp.117-128
    • /
    • 2016
  • High resolution aerial photographs and digital elevation models for Bangpo beach using UAV were generated in this study to analyze the thematic and geometric characteristics of coastal features. Based on 728 aerial images acquired on September 10, 2016 by the UAV, a image mosaic at 2.2 cm spatial resolution and a digital elevation model at 4.4 cm spatial resolution were developed. This study found out that Bangpo beach consisted of intertidal zone and supratidal zone. The intertidal zone can be subdivided into lower part and upper part with distinctive geomorphological characteristics. While the lower part included sand bars and ripple marks along the coastline, the cusps and sand dunes were the major coastal features of the upper part. Part of the intertidal zone was occupied by shore platform with average slope of 0.9 degree containing various sizes of gravels. The supratidal zone slanted toward ocean with berms on the surface with an interval of 15 m. These coastal features indicated the flow intensity towards to the land and tidal effect. It validated that the UAV application in coastal research was very effective analyzing to examine coastal processes.

Short-term Change in Channel Morphology of the Naeseong Stream before the Operation of Yeongju Dam, Korea (영주댐 운영 전 내성천에서 하도 형태의 단기 변화)

  • Lee, Chanjoo;Kim, Donggu
    • Ecology and Resilient Infrastructure
    • /
    • v.4 no.1
    • /
    • pp.12-23
    • /
    • 2017
  • The Naeseong Stream is a meandering sand-bed stream flowing through mountains and has so long maintained its geomorphological uniqueness characterized by extensive braided bare bars. Recently, its long-lasting landscape has been changed due to encroachment of vegetation. In this study being a part of long-term monitoring research morphological changes of the 56.8 km long study reach of the Naeseong Stream, which occurred during the period of 2012 - 2016 were analyzed. Airborne LiDAR and terrestrial cross-section surveys were carried out. Hydrological and on-site investigation data were also collected. Among the main four sites, two bend reaches showed point bars enlarged, while along the other two straight reaches mid-channel bars were either newly formed or increased in area and height. At the highest deposition point of each bar, vertical changes which were caused by one or two times of sediment deposition amounted to 0.6 - 1.4 m. On the contrary channel bed degradation was not obvious. Overall morphological changes in the study reach were attributed to deposition of sediment which occurred during the flood in July 2016 on the bar surfaces vegetated during the precedent dry seasons. These kind of geomorphological processes are thought to be the same as those related to the existing mid-channel islands along the mid- and downstream reach of the Naeseong Stream.

Understanding on Characteristics of the Sand Bars' Movement in the Meandering Reaches by a Movable-Bed Experiment (이동상 수리모형실험을 통한 만곡부 모래사주의 거동특성 분석)

  • Lee, Sam-Hee;Hwang, Seung-Yong;Park, Jae-Min
    • Proceedings of the Korea Water Resources Association Conference
    • /
    • 2007.05a
    • /
    • pp.1679-1683
    • /
    • 2007
  • 최근 우리나라에서 하천 및 유역 환경의 급격한 변화로 인하여 하천 형태가 많이 변하고 있는 추세이다. 특히 사행하는 모래 하천에서 만곡부 사주의 형태 변화가 커지고 있다. 이 연구에서는 이와 같은 모래 하천의 만곡부에서 사주의 변화 특성을 평가하고 그 원인을 파악하기 위하여 이동상 수리모형 실험을 실시하였다. 실험에서 하천 및 유역의 여러 상황 변화를 감안하여 유량, 유사 공급량, 공급 시간, 하천 변형 등 다양한 조건을 상정하였다. 연구 대상하천은 낙동강 본류이며, 중점 수리모형 실험대상 구간은 우리나라의 전통민속마을인 안동 하회마을을 태극형으로 감싸면서 사행하는 만곡부이다. 이동상 실험규모는 수평축적 1/110, 수직축적 1/50로 왜곡도가 2.2로써 비교적 대규모이다. 모형 하상재료는 입경 0.29 mm의 석탄분(anthracite)을 채택하였으며, 현장에서 하상재료조사와 상사해석을 통해 결정하였다. 실험 결과, 유량과 유사 공급량 변화에 따른 사주 변화가 밀접한 관계가 있는 것으로 나타났다. 특히 유사 공급이 이루어지지 않을 때 국지적 퇴적양상을 보였다. 이는 사주 내 식생활착으로 이어지는 계기가 될 수 있음을 확인할 수 있었다. 그리고 설계홍수량 규모에서 구하도와 과거 사주가 재현되었는데, 이는 지역주민을 통해 입증되었다. 또한 천연기념물인 만송정 주변의 모래둔덕의 형성과정이 입증되었다.

  • PDF

An Investigation of Flora on Archaelogical Districts of Han River Side, Amsadong, Daeshimli and Hunbaukol (한강유역(암사동, 대심리, 혼암리)의 석기출토지의 식물상 조사)

  • 이영노
    • Journal of Plant Biology
    • /
    • v.15 no.s
    • /
    • pp.33-49
    • /
    • 1972
  • Recently two thousand year old several villages ruins discovered at Amsadong, Daeshimli and Hunbaukol near the Han River side in Korea. An investigation of the present flora of these three localities was done. There are 84 families including 419 species of vascular plants. The vegetations of flora in the localities of the Han River side are very similar. the forests are poorly developed and appear as the secondary vegetations. The reforest plants can be recognized as Pinus rigida, quercus acutissima, Q. serrata, Robinia pseudoacacia and Alnus hirta. Herbaceous plants of Miscanthus sacchariflorus and Phragmitis japonicus bind up the soiles of the Han River side. Populus nigra grows abundantly in the moist places of sand bars which are located on the river side south of Daeshimli and on the northern side of the Han River across from Hunbaukol. These three area are fully cultivated but still many primitive farm techniques are employed. Farm produce crops include rice, corn, barley wheat, other vegetables, and a few ornamental plants. In this study the author found flower color variations ranging from a dark blue to a pale blue, and chromosome number differences existing between the populations of Commelina communis. The dark blue flowered taxa chromosome number is 44 and in the pale blue taxa it is 72. The wild white flowered Chrysanthemum is Chrysanthemum zawadskii Herb. ssp. acutilobum and which has finely lobed leaves, and has 54 chromosome in the root tip cells.

  • PDF

Bond Performance of FRP Reinforcing Bar for Concrete Structures after Chemical Environmental Exposure (화학적 환경에 노출된 콘크리트 보강용 FRP 보강근의 부착 성능)

  • Park, Chan-Gi;Won, Jong-Pil
    • Journal of The Korean Society of Agricultural Engineers
    • /
    • v.46 no.3
    • /
    • pp.73-81
    • /
    • 2004
  • FRP reinforcing bars(rebars) are produced through a variety of manufacturing process includes pultrusion, and filament winding and braiding etc. Each manufacturing method produces a different surface condition of FRP rebar. The surface properties of FRP rebar is an important property for mechanical bond with concrete. Current methods of providing surface deformation to FRP rebars include helical wrapping, surfaces and coating and rib molding. The problem with the helical wrapping method is that it can not provide enough surface deformation for good bond and it can be easily sheard off from the FRP rebars. Sand coating and rib molding provide surface deformation only to the outer FRP skins. Therefore, FRP rebar has about 60% of bond strength of steel rebar. The main objective was to evaluate the bond properties of FRP rebar after environmental exposure. Five types of FRP rebar includes CFRP ISO, GFRP Aslan, AFRP Technora CFRP(Korea), and GFRP(Korea) rebars performed direct bond tests. Also, FRP rebar bond specimens were subjected to exposure conditions including alkaline solution, acid solution, salt solution and deionized water etc. According to bond test results, CFRP(Korea) and CFRP(Korea) rebars were found to have better bond strength with concrete than previous FRP rebars. Also, FRP(Korea) rebar had more than about 70% in bond strength of steel rebar.

Depositional Characteristics and Seasonal Change of Surface Sediment and Sedimentary Strucutre on the Doowoovi Tidal Flat, Southwestern Coast of Korea (한국 서남해안 두우리 조간대에서 표층 퇴적물 및 퇴적구조의 특성과 계절변화)

  • Baek Young Suk;Chun Seungsoo
    • The Korean Journal of Petroleum Geology
    • /
    • v.10 no.1_2 s.11
    • /
    • pp.10-17
    • /
    • 2004
  • The Doowoo-ri tidal flat in the southwestern Korean coast is a typical open-coast tidal flat which has no barriers in the offshore such as barrier island and sand bars. The difference of induced wave energy with seasons is affected directly on the distribution of surface sediment and the formation of sedimentary structures because the sedimentation by wind wave is relatively much important element in this open-coast tidal flat. This open-coast tidal flat can be classified into tidal beach, intertidal flat and lower mudflat according to the pattern of geomorphology and sediment type. The intertidal flat can be again divided into 3 types: sand flat, mixed flat and mud flat based on the primary sedimentary structure and sand/mud ratio. Doowoori tidal flat shows a seasonal change in the surface sedimentary facies based on sediment composition and primary sedimentary structure. The change is closely related to the direction and magnitude of monsoon wind and also to storm frequency. In winter and spring, when northwesterly wind is most dominant and strong and also storms are common, sand-flat facies is largely distributed on the intertidal flat, whereas mud-flat facies is most dominant during summer when weak southeasterly wind is common. In the fall season, mixed-flat facies is dominant on the flat. The Doowoori intertidal flat is covered by mud sediment which is ca. 20 cm in thickness in summer season. In winter season, surface sediment is changed from mud to sand because the summer mud is mostly eroded by strong wave action. Can-core peels in the intertidal flat show that parallel laminated mud or sand/mud and climbing ripple cross-laminated sandy silt are dominant on the upper intertidal flat $(0-1.3 {\cal}km)$ during summer season. On the other hand, on lower intertidal flat $(1.7-2.3 {\cal}km)$, dominant sedimentary facies is homogeneous mud. In winter, it is changed into parallel laminated and ripple cross-laminated sand facies.

  • PDF

A Study of the Geomorphological Process and Vegetation Distribution of Sand-bars on the Tan-cheon River (탄천 하도사주의 지형 형성과정과 식생분포 연구)

  • Choi, Mi-Kyoung;Lee, Sam-Hee;Choi, Jung-Kwon
    • Journal of the Korean Institute of Landscape Architecture
    • /
    • v.37 no.6
    • /
    • pp.96-105
    • /
    • 2010
  • This study identified the dynamic process of sandbar and vegetation distribution of the sandbar on the Tan-cheon River. The study area is located in the lower reaches of the Tan-cheon River that has been managed as an Ecosystem Reserve Area since 2002. For the study, the geomorphological process was analyzed through mapping analysis using a satellite image followed by analysis of the vegetation distribution through an on-site survey. The major findings were as follows : First, In the fluvial geomorphic process, various kinds of sandbars were developed in 1990s, the morphologic characteristics changing continuously. Second, In the distribution of vegetation on the sandbar, the sandbar shore was covered with bare sand substrate or intermittent annual vegetation because of the periodic fluctuation of the water-level due to intensive disturbances. Third, In the relationship between the sandbar formation and vegetation, four types of sandbars were classified: channel-shore stable bar, channel-shore unstable bar, mid-channel stable bar and mid-channel unstable bar, according to the fluvial disturbance & vegetation process. The study verifies that the vegetation distribution is reciprocally related to the geomorphological process. Accordingly, it is meaningful in the selection of plant species and the planting area of the sand bar. However, it is limited to the planting guidelines on river restoration projects. More diverse on-site experimental studies should be conducted.

The Evaluation for Pullout Performance of Steel Strip Reinforcements with Deformed-Bars as Transverse Members (지지부재로 이형철근을 설치하는 띠형 강보강재의 인발성능 평가)

  • Jung, Sung-Gyu;Kim, Juhyong;Cho, Samdeok;Lee, Kwangwu
    • Journal of the Korean Geosynthetics Society
    • /
    • v.12 no.4
    • /
    • pp.77-86
    • /
    • 2013
  • Laboratory pullout tests were conducted to evaluate pullout performance of steel strip reinforcements with deformed steel bars as transverse members. The steel strip reinforcement has an installation hole to assemble a deformed steel bar. Jumunjin standard sand is used to form a relative density of ground model to 80%. Frictional resistance of steel strip reinforcement without transverse member increases sharply at the initial displacement and quickly decreases with displacement. Maximum frictional resistance increases linearly as normal pressure increasing, and soil-reinforcement interaction friction angle(${\rho}_{peak}$) of a steel strip reinforcement is estimated to $14.64^{\circ}$. Passive resistance increases with displacement and converge into maximum passive resistance in most cases. Maximum passive resistance increases linearly as normal pressure increasing irrespective of shape of the steel reinforcement. Pullout force of steel strip reinforcements with installation holes or transverse members largely increases about 4 to 7 times compared to frictional resistance force of steel strip reinforcements when embedment length($L_e$) of steel strip reinforcements is 500 mm. In the case of using 2 transverse members, interference effect is observed due to the spacing of 2 transverse members and location of assembly holes and transverse members.

Flexural Behaviors of GFRP Rebars Reinforced Concrete Beam under Accelerated Aging Environments (GFRP Rebar 보강 콘크리트 보의 급속노화환경에서의 휨 거동에 관한 연구)

  • Park, Yeon-Ho;Choi, Yeol
    • Journal of the Korea Concrete Institute
    • /
    • v.25 no.2
    • /
    • pp.137-144
    • /
    • 2013
  • The use of fiber-reinforced polymer (FRP) reinforcing bars in concrete structures has been increased as an alternative of steel reinforcement which has shown greater vulnerability to corrosion problem. However, the long-term performance of concrete members with FRP reinforcement is still questioned in comparison to the used of steel reinforcement. This study presents the results of an experimental study on the long-term behaviors of GFRP (glass fiber reinforced polymer) bar reinforced concrete beams after exposed to accelerated aging in an environmental chamber with temperature of $46^{\circ}C$ ($115^{\circ}F$) and 80% of relative humidity up to 300 days. The objectives of this research was to compare strength degradation and change of ductility between GFRP reinforced concrete beams and steel reinforcement beams after accelerated aging. Two types (wrapped and sand-coated surface) of GFRP bars and steel were reinforced. in concrete beams. Test results show that the failure modes of GFRP bar reinforced concrete beams are very similar with traditional RC beams, and the change of load-carrying capacity of steel reinforcing concrete beam is greater than that of GFRP bar reinforcing concrete beam under the accelerated aging. Test result also shows that the use of GFRP reinforcing in concrete could be introduced more brittle failure than that of steel reinforcing for practical application. The deformability factor up to compression failures indicates no significant variation before and after exposure of accelerated aging.

Soil Erosion and river-bed change of the Keum river basin using by GIS and RS (GIS와 RS를 이용한 금강유역 토양침식과 하상변화 연구)

  • Lee, Jin-Young;Kim, Ju-Young;Yang, Dong-Yoon;Nahm, Wook-Hyun;Kim, Jin-Kwan
    • The Korean Journal of Quaternary Research
    • /
    • v.20 no.2
    • /
    • pp.1-10
    • /
    • 2006
  • Flooding hazard caused by natural and artificial environmental changes is closely associated with change in river bed configuration. This study is aimed at explaining a river-bed change related to soil erosion in the Keum river basin using GIS and RS. The USLE was used to compute soil erosion rate on the basis of GIS. River-bed profiles stretching from Kongju to Ippo were measured to construct a 3D-geomorphological map. The river-bed change was also detected by remote sensing images using Landsat TM during the period of 1982 to 2000 for the Keum river. The result shows that USLE indicates a mean soil erosion rate of $1.8\;kg/m^2/year$, and a net increase of a river-bed change at a rate of $+5\;cm/m^2$/year in the Kangkyeong area. The change in river-bed is interpreted to have been caused by soil erosion in the downstream of the Keum river basin. In addition river-bed change mainly occurred on the downstream of the confluence where tributaries and the main channel meet. Other possible river-bed change is caused by a removal of fluvial sand aggregates, which might have resulted in a net decrease of exposed area of sediment distribution between 1991 and 1995, while a construction of underwater structures, including a bridge, a reclamation of sand bars for rice fields and dikes, resulted in an increase of the exposed area of river-bed due to sediment accumulation.

  • PDF