• 제목/요약/키워드: Erosion depth

검색결과 270건 처리시간 0.025초

고랭지 농업의 작물별 객토량 변화에 따른 토양유실 저감 분석 (Analysis of Soil Erosion Reduction Ratio with Changes in Soil Reconditioning Amount for Highland Agricultural Crops)

  • 허성구;전만식;박상헌;김기성;강성근;옥용식;임경재
    • 한국물환경학회지
    • /
    • 제24권2호
    • /
    • pp.185-194
    • /
    • 2008
  • There is increased soil erosion potential at highland agricultural crop fields because of its topographic characteristics and site-specific agricultural management practices performed at these areas. The agricultural upland fields are usually located at the sloping areas, resulting in higher soil loss, pesticides, and nutrients in case of torrential rainfall events or typhoon, such as 2002 Rusa and 2003 MaeMi. At the highland agricultural fields, the soil reconditioning have been performed every year to decrease damage by continuous cropping and pests. Also it has been done to increase crop productivity and soil fertility. The increased amounts of soil used for soil reconditioning are increasing over the years, causing significant impacts on water quality at the receiving water bodies. In this study, the field investigation was done to check soil reconditioning status for potato, carrot, and cabbage at the Doam-dam watershed. With these data obtained from the field investigation, the Soil and Water Assesment Tool (SWAT) model was used to simulate the soil loss reduction with environment-friendly and agronomically enough soil reconditioning. The average soil reconditioning depth for potato was 34.3 cm, 48.3 cm for carrot, and 31.2 cm for cabbage at the Doam-dam watershed. These data were used for SWAT model runs. Before the SWAT simulation, the SWAT ArcView GIS Patch, developed by the Kangwon National University, was applied because of proper simulation of soil erosion and sediment yield at the sloping watershed, such as the Doam-dam watershed. With this patch applied, the Coefficient of Determination ($R^2$) value was 0.85 and the Nash-Sutcliffe Model Efficiency (EI) was 0.75 for flow calibration. The $R^2$ value was 0.87 and the EI was 0.85 for flow validation. For sediment simulation, the $R^2$ value was 0.91 and the EI was 0.70, indicating the SWAT model predicts the soil erosion processes and sediment yield at the Doam-dam watershed. With the calibrated and validated SWAT for the Doam-dam watershed, the soil erosion reduction was investigated for potato, carrot, and cabbage. For potato, around 19.3 cm of soil were over applied to the agricultural field, causing 146% of more soil erosion rate, approximately 33.3 cm, causing 146% of more soil erosion for carrot, and approximately 16.2 cm, causing 44% of more soil erosion. The results obtained in this study showed that excessive soil reconditioning are performed at the highland agricultural fields, causing severe muddy water issues and water quality degradation at the Doam-water watershed. The results can be used to develop soil reconditioning standard policy for various crops at the highland agricultural fields, without causing problems agronomically and environmentally.

고령토 퇴적저면의 침식특성에 대한 실험적 연구 (A Laboratory Study on Erosional Properties of the Deposit Bed of Kaolinite Sediments)

  • 김용묵;김현민;황규남;양수현
    • 대한토목학회논문집
    • /
    • 제34권4호
    • /
    • pp.1181-1190
    • /
    • 2014
  • 본 연구에서는 환형수조를 이용한 침식실험을 통하여 국내 최초로 퇴적저면의 침식매개변수들이 정량적으로 산정되었다. 퇴적저면은 고농도의 고령토 슬러리를 기 설정된 시간 동안 압밀시켜 조성되었으며, 각기 다른 압밀구조를 갖는 퇴적저면 조건 하에서 총 4회의 침식실험이 수행되었다. 침식실험 결과에 따르면, 흐름전단응력 ${\tau}_b$에 대한 저항력을 나타내는 저면전단강도 ${\tau}_s$는 압밀시간 및 저면(퇴적층) 깊이가 깊어짐에 따라 증가하는 것으로 나타났다. 한편, 침식률${\epsilon}$은 흐름전단응력과 저면전단강도의 차로 주어지는 잉여전단응력 ${\tau}_b-{\tau}_s$과 상관성이 매우 큰 것으로 나타났는데, ${\tau}_b-{\tau}_s{\leq}0.1N/m^2$인 경우에 침식률의 로그 값은 잉여전단응력과 선형적 관계에 있으나, ${\tau}_b-{\tau}_s{\leq}0.1N/m^2$인 조건에서는 잉여전단응력이 작아질수록 침식률이 급격하게 작아지는 경향이 있는 것으로 나타났다. 또한 본 연구에서는 과거 연구결과와의 비교검토를 통하여 본 침식실험 결과에 대한 타당성이 입증되었으며, $0.1N/m^2$ 이하의 잉여전단응력 구간에서 침식률을 보다 잘 표현할 수 있는 새로운 침식률 산정식이 제시되었다.

하안침식을 고려한 복렬사주의 동적 거동 특성 분석 (Dynamic Characteristics of Multiple Bars in the Channels with Erodible Banks)

  • 장창래
    • 한국수자원학회논문집
    • /
    • 제46권1호
    • /
    • pp.25-34
    • /
    • 2013
  • 본 연구에서는 복렬사주의 모드를 객관적으로 판단할 수 있는 2중 퓨리에 해석을 수행하여 하폭의 변화에 따른 복렬사주의 발달 과정을 정량적으로 분석하였다. 초기에 직선하도에서 하안침식이 발생하고, 하폭 대 수심의 비가 증가하면서 복렬사주가 발달하였다. 사주가 하류로 이동하면서 성장하고, 사주의 주변에서 흐름이 분리되어 하안 침식을 가속시키면서, 지형이 지속적으로 변하여 유사의 유출특성에 영향을 주었다. 2중 Fourier 해석에 의한 하상파(wave)의 분포와 지배적인 성분의 변화를 분석한 결과, 초기에1-1 모드(mode)인 교호사주가 지배적이지만, 시간이 지나면서 하폭이 증가하여 상대적으로 수심이 감소하면서 2-3 모드가 지배적인 것으로 나타났으며, 교호사주의 강한 비선형 특성이 상호작용하기 때문이다. 하안침식이 진행되면서 하폭 대 수심의 비가 증가하고, 무차원 소류력이 감소하였다. 하폭 대 수심의 비가 증가할수록 사주의 이동속도가 감소하고, 사주의 파장은 증가하였다. 무차원 소류력이 증가하면서, 사주의 이동속도는 증가하였다.

해양 환경 하에서 16.7Cr-10Ni-2Mo 스테인리스강의 표면 손상에 미치는 캐비테이션의 영향 (Effect of cavitation on surface damage of 16.7Cr-10Ni-2Mo stainless steel in marine environment)

  • 정상옥;한민수;김성종
    • Corrosion Science and Technology
    • /
    • 제14권5호
    • /
    • pp.239-246
    • /
    • 2015
  • Stainless steel is generally known to have characteristics of excellent corrosion resistance and durability, but in a marine environment it can suffer from localized corrosion due to the breakdown of passivity film due to chloride ion in seawater. Furthermore, the damage behaviors are sped up under a cavitation environment because of complex damage from electrochemical corrosion and cavitation-erosion. In this study the characteristics of electrochemical corrosion and cavitation erosion behavior were evaluated on 16.7Cr-10Ni-2Mo stainless steel under a cavitation environment in natural seawater. The electrochemical experiments have been conducted at both static conditions and dynamic conditions inducing cavitation with different current density parameters. The surface morphology and damage behaviors were compared after the experiment. After the cavitation test with time variables morphological examinations on damaged specimens were analyzed by using a scanning electron microscope and a 3D microscope. the galvanostatic experiment gave a cleaner surface morphology presented with less damage depth at high current density regions. It is due to the effect of water cavitation peening under the cavitation condition. In the cavitation experiment, with amplitude of $30{\mu}m$ and seawater temperature of $25^{\circ}C$, weight loss and cavitation-erosion damage depth were dramatically increased after 5 hours inducing cavitation.

침식률 측정결과를 사용하는 유사이동모형의 적용 (Application of Sediment Transport Model Using Observed Erosion Rates)

  • 정태성;크랙 죤스;월버트 릭
    • 한국수자원학회논문집
    • /
    • 제37권12호
    • /
    • pp.1033-1041
    • /
    • 2004
  • 현장에서 교란하지 않고 채취한 유사 시료의 침식률을 측정한 결과를 직접 활용하여 침식률을 계산하는 2차원 유사이동 수치모형을 수립하고, 적용성을 검토하기 위하여 미국 팍스강에서 홍수시 유사 수송과정을 모의하였다. 큰 전단응력 하에서도 침식률 측정이 가능한 Sedflume을 사용하여 현장에서 채취된 시료의 침식률이 깊이별, 전단응력 별로 측정되었다. 수치모형은 침식률 측정자료를 모형에서 직접 사용하며, 부유사와 소류사 이동을 모두 고려한다. 개발된 모형은 1차원 직선수로에서 유사수송에 대해 검증되었다. 홍수시 팍스강의 유사 수송과정을 모의하고 부유사 농도의 시간변화에 대해 검증한 결과, 모의결과가 관측치와 잘 일치하여 현장 침식률 값을 직접 사용하는 모형이 효과적임을 확인할 수 있었다.

피복공법 적용 시 파랑에 의한 피복재 침식 실험 연구 (Experimental Investigation on In-Situ Capping Erosion by Waves)

  • 공진영;김영택;유병현;이장근
    • 한국지반환경공학회 논문집
    • /
    • 제17권10호
    • /
    • pp.33-43
    • /
    • 2016
  • 피복공법의 설계에서 피복재의 선정은 중요한 설계 변수로 파랑에너지로 발생하는 해저면 유속에도 피복재가 침식되지 않게 설계되어야 한다. 피복공법 관련된 기존 연구는 파랑에너지에 따른 깊이별 유속과 유효입경을 주로 시공경험과 수치해석에 의존하여 수행되었기 때문에 현장에서 시공경험이 미흡한 기술자가 사용하기에는 어려움이 예상된다. 본 연구에서는 파랑에너지에 따른 깊이별 유속과 피복재의 입경에 따른 침식을 판단할 수 있는 간편식을 제시하고 모형수조를 이용한 실내실험을 통해 신뢰성을 확인하고자 한다. 실내실험에서 측정된 깊이별 유속은 이론식과 상당히 일치하며, 유속추정 이론식을 침식 해석에 적용하여 유효입경을 예측하면 침식 유무 판단이 가능하다.

Influence of Spatial Differences in Volcanic Activity on Vegetation Succession and Surface Erosion on the Slope of Sakurajima Volcano, Japan

  • Teramoto, Yukiyoshi;Shimokawa, Etsuro;Ezaki, Tsugio;Nam, Sooyoun;Jang, Su-Jin;Kim, Suk-Woo;Chun, Kun-Woo
    • Journal of Forest and Environmental Science
    • /
    • 제33권2호
    • /
    • pp.136-146
    • /
    • 2017
  • We selected 6 plots ($100m^2$) located 2.2-3.8 km from Minamidake Crater on the north flank of Sakurajima Volcano. We conducted a field study to investigate the effects of volcanic activity on vegetation succession and surface erosion rate. The results showed that trees growing in plots further from the crater had a greater diameter at breast height (DBH), total height, and age. In addition, these plots had a greater number of woody plants and species, as well as a greater total cross-sectional area at breast height. The Fisher-Williams index of diversity (${\alpha}$) and the proportion of evergreen broad-leaved trees were higher in plots located further from the crater. Vegetation succession in these plots was not at the level of a climax forest. From 1972 to 2015, the timing for active volcano, the depth of volcanic ash layer, the dry density, and the pH of ground surface were lower for plots located further from the crater. Furthermore, the average annual sheet erosion from 1972 to 2015 was also lower for plots located further away from the crater. Overall, plots further away from the crater have a better environment for vegetation growth and a lower dry density of the volcanic ash surface layer. It is thought that lower dry density results in increased soil permeability, which impedes surface flow. In order to prevent debris-flow disasters, caused by mud and rock flow resulting from impaired soil penetrability, it is essential to promote soil development and restore penetrability by artificial vegetation restoration.

Evaluation of the Acromioclavicular Joint Morphology for Minimizing Subacromial Erosion after Surgical Fixation of the Joint Using a Clavicular Hook Plate

  • Kim, Sung-Jae;Kee, Young-Moon;Park, Dong-Hyuck;Ko, Young-Il;Lee, Bong-Gun
    • Clinics in Shoulder and Elbow
    • /
    • 제21권3호
    • /
    • pp.138-144
    • /
    • 2018
  • Background: Subacromial erosion remains a major concern after surgical fixation of acromioclavicular (AC) joint using a clavicular hook plate. To minimize postoperative subacromial erosion, we investigated the structural relationship between distal clavicle and acromion around the AC joint by considering the surgical fixation of the joint using the hook plate technique. Methods: Computed tomography scans of 101 AC joints without any inherent pathology were analyzed. The angle between the distal clavicle and acromion around the AC joint (AC angle), depth of the acromion, differences in height between distal clavicle and acromion (AC height difference), and thickness of distal clavicle and acromion at the AC joint were measured. Descriptive statistics were calculated for each anatomical parameter, and all results were compared between gender groups. Results: The mean AC angle was $17.1^{\circ}$(range, $-8.0^{\circ}$ to $39.0^{\circ}$), and the mean AC height difference was 3.5 mm (range, -0.7 to 8.7 mm). Both factors showed very high variability (coefficients of variation=62.6% and 46.6%, respectively). The mean AC angle was significantly higher in the female gender than in the male gender ($19.8^{\circ}$ vs. $13.8^{\circ}$, p=0.048). The mean acromion thickness and distal clavicular thickness were both significantly thinner in the female group than in the male group (p<0.001). Conclusions: Taken together, we believe our results might be helpful in minimizing postoperative subacromial erosion when performing surgical fixation of the AC joint using the hook plate, and be valuable in improving future design of the hook plate.

An automatic rotating annular flume for cohesive sediment erosion experiments: Calibration and preliminary results

  • Steven Figueroa;Minwoo Son
    • 한국수자원학회:학술대회논문집
    • /
    • 한국수자원학회 2023년도 학술발표회
    • /
    • pp.319-319
    • /
    • 2023
  • Flows of water in the environment (e.g. in a river or estuary) generally occur in complex conditions. This complexity can hinder a general understanding of flows and their related sedimentary processes, such as erosion and deposition. To gain insight in simplified, controlled conditions, hydraulic flumes are a popular type of laboratory research equipment. Linear flumes use pumps to recirculation water. This isn't appropriate for the investigation of cohesive sediments as pumps can break fragile cohesive sediment flocs. To overcome this limitation, the rotating annular flume (RAF) was developed. While not having pumps, a side-effect is that unwanted secondary circulations can occur. To counteract this, the top and bottom lid rotate in opposite directions. Furthermore, a larger flume is considered better as it has less curvature and secondary circulation. While only a few RAFs exist, they are important for theoretical research which often underlies numerical models. Many of the first-generation of RAFs have come into disrepair. As new measurement techniques and models become available, there is still a need to research cohesive sediment erosion and deposition in facilities such as a RAF. New RAFs also can have the advantage of being automatic instead of manually operated, thus improving data quality. To further advance our understanding of cohesive sediment erosion and deposition processes, a large, automatic RAF (1.72 m radius, 0.495 m channel depth, 0.275 m channel width) has been constructed at the Hydraulic Laboratory at Chungnam National University (CNU), Korea. The RAF has the ability to simulate both unidirectional (river) and bidirectional (tide) flows with supporting instrumentation for measuring turbulence, bed shear stress, suspended sediment concentraiton, floc size, bed level, and bed density. Here we present the current status and future prospect of the CNU RAF. In the future, calibration of the rotation rate with bed shear stress and experiments with unidirectional and bidirectional flow using cohesive kaolinite are expected. Preliminary results indicate that the CNU RAF is a valuable tool for fundamental cohesive sediment transport research.

  • PDF

연행작용을 고려한 우면산 토석류 모의 매개변수 특성분석 (Analysis of debris flow simulation parameters with entrainment effect: a case study in the Mt. Umyeon)

  • 이승준;안현욱;김민석;임현택
    • 한국수자원학회논문집
    • /
    • 제53권9호
    • /
    • pp.637-646
    • /
    • 2020
  • 산지 사면에서 발생하는 토석류는 지형변화에 큰 영향을 미치는 대표적인 자연재해 중 하나이다. 특히, 도심지역에서 발생된 토석류는 유동 및 퇴적과정에서 막대한 재산피해와 인명피해를 야기할 수 있으며 이러한 토석류로 인한 피해를 줄이기 위해서는 토석류의 유동과 피해규모를 예측하기 위한 해석모형들이 필수적이다. 하지만 아직 토석류 모형들의 매개변수에 대한 분석은 충분하지 않으며, 특히 토석류의 유동과정 및 피해 규모에 큰 영향을 미치는 연행작용에 대한 연구는 미비한 실정이다. 본 연구에서는 국내에서 개발된 토석류 유동해석 모형인 Deb2D 모형을 통하여 토석류의 매개변수 변화에 따른 흐름, 피해지역에 미치는 영향 그리고 침식과정에 대하여 분석하였다. 2011년 우면산에서 발생한 산사태에 적용하였으며, 수치모형의 객관적인 정확성 판단을 위해 현장 조사를 통해 얻어진 토석류의 피해 범위, 총 퇴적량, 특정 지점에서 관측된 최대 퇴적 높이, 토석류의 첨두 유속를 검토하였다. 또한 매개변수 변화가 연행작용에 미치는 영향에 대하여 침식 형상 및 깊이를 통해 분석하였다. 연행작용을 고려한 래미안 아파트와 신동아 아파트 유역의 모의는 성공적으로 수행되었다. 매개변수 변화에 따른 두 유역에서의 민감도 분석을 통해 각 매개변수의 영향성을 판단할 수 있었다.