• Title/Summary/Keyword: 토양입경

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Effects of Grain Size on Relationship between Microtopographic Roughness and Soil Erosion Rate (토양 입경이 미세지형의 거칠기와 토양침식률 간의 관계에 미치는 영향)

  • Soyoung Kim;Dae-Hong Kim;Tae-young Sohn
    • Proceedings of the Korea Water Resources Association Conference
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    • 2023.05a
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    • pp.216-216
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    • 2023
  • 가속적인 토양침식은 토지의 환경 및 생태계의 지속성에 부정적 영향을 미치므로, 그 양을 예측하여 토양침식을 방지하는 것은 중요하다. 이에 따라 식생, 지형, 토양의 입도분포 등과 같은 토양침식에 영향을 미치는 인자에 관한 연구가 꾸준히 이뤄지고 있다. 특히 자연 지형에서 보편적으로 나타나는 'cm' 규모의 미세지형이 토양침식에 미치는 영향을 분석한 기존 연구 결과를 살펴보면, 유역 출구 지점에서 관측된 총 유사유출량에만 근거하고 있을 뿐 아니라 토양침식에 미치는 미세지형의 영향에 관한 상반된 결과가 혼재하고 있다. 이는 유역의 토양침식과정에 대한 이해도와 토양침식량에 대한 예측 정확도를 저하시킬 우려가 있으므로 미세지형이 토양침식에 미치는 영향을 유역 전반에 걸쳐 살펴본 후, 명확하게 하는 것이 필요하다. 본 연구에서는 동역학파 모형에 기반한 침식 모형을 이용하여 미세지형에서의 강우-유출 및 토사 입자별 침식 및 유출 현상을 수치적으로 모의하였다. 모의 결과에 따르면, 동일한 강우-유출 조건에서도 미세지형의 거칠기에 따라 유역의 토양침식량 및 침식 특성이 달라질 수 있으며, 토양 입경이 미세지형의 거칠기에 따른 유사유출량의 증감 현상을 결정하는 데에 있어 중요한 요소로 작용함을 제시하였다. 미세지형이 거칠어짐에 따라 비교적 굵은 입자인 모래 함량이 높은 지반에서는 토양침식률이 감소하였으나 이와 대조적으로 미세토사 함량이 높은 지반에서는 토양침식률이 증가하였다. 이는 미세지형이 유역 전반에 걸쳐 입경에 따른 토사의 부상, 이류 및 퇴적 특성에 영향을 미쳐, 유역의 유사 분급 및 장갑화 현상에 깊게 관여하였기 때문이다. 본 연구를 통해 토양유실에 미치는 미세지형의 영향에 관한 상반된 연구 결과를 미세지형과 토양 입경분포의 상호작용으로 설명할 수 있다. 따라서, 본 연구는 유역 내 미세지형적 거칠기 입경분포에 대한 정확한 정보에 기반하여 토양의 유실량 및 침식량을 산정해야 함을 강조한다.

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Effects of Soil Particle Size on Relationship between Microtopography Roughness Height and Soil Erosion Rate: Harisine-Rose Model analysis (토양 입경에 따른 미세지형적 거칠기와 토양 침식률 간의 관계)

  • Kim, Soyoung;Kim, Dae-Hong;Jeong, Minyeob
    • Proceedings of the Korea Water Resources Association Conference
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    • 2022.05a
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    • pp.199-199
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    • 2022
  • 선행 연구들을 통해 미세지형이 유역에서의 유사 유출량에 영향을 끼침을 알 수 있다. 그러나 여전히 유사-유출에 대한 미세지형의 영향이 불분명하여 유역 내 토양 침식 과정에서 미세지형적 거칠기를 고려할 때 혼란이 야기될 수 있다. 따라서, 유사유출량과 토양침식량에 대한 보다 정확한 예측 및 산정을 위해 미세지형이 토양 침식에 미치는 영향을 명확하게 하는 것이 필요하다. 본 연구에서는 Hairsine-Rose 침식 모형과 동역학파(Dynamic wave) 모형을 사용하여 강우-유출에 따른 미세지형의 유사-유출 과정을 수치적으로 모의하였다. 모의 결과에 따르면, 미세지형은 동일 강우 및 유출 조건에서도 유역 내 유사 유출량을 변화시켰다. 또한, 본 연구의 모의조건 하에서 지반이 비교적 미세토사로 구성된 경우 미세지형이 거칠수록 침식률이 증가하는 반면 지반의 토사가 대부분 굵은 입경을 가질 때는 매끄러운 지형보다 거친 미세지형에서 토양 침식률이 감소함을 확인하였다. 따라서, 지형의 미세지형 변동 정도와 토양침식률 사이에 비례 또는 반비례 관계가 형성됨을 보이고, 이러한 관계를 형성하는 과정에 입경 분포가 미치는 영향을 제시하였다. 마지막으로, 본 연구 결과를 통해 장갑화(armoring) 과정이 입경 분포뿐만 아니라 미세지형의 거칠기에 따라 유역별로 다르게 나타나는 것을 확인하였다. 따라서 유사-유출에 대한 미세지형의 영향을 적절하게 고려하기 위해 부상(Pick-up), 이류 및 퇴적 등 입경 별 퇴적물 이동이 다중 물리적으로 고려되어야 한다는 점을 강조한다. 본 연구를 통해 지표면의 미세지형적 거칠기 및 토양 입경에 대한 정확한 정보가 필요함을 알 수 있으며, 이를 충분히 고려한다면 강우 유출에 의한 토양 침식 메커니즘에 대한 이해도와 토양침식량에 대한 정량적 예측의 정확도가 향상될 것으로 예상된다.

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Removal Characteristics of Lead-contaminated Soil at Military Shooting Range by Using Soil Washing Process (토양세척공정을 이용한 군사격장 납 오염토양의 제거특성)

  • Ahn, Sung-Kyun;Kim, Chul;Lee, Joung-Man;Lee, Gang-Choon;Shon, Zang-Ho;Jung, Byung-Gil;Yoon, Tae-Kyung
    • Clean Technology
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    • v.18 no.4
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    • pp.390-397
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    • 2012
  • Removal characteristics of lead-contaminated soil at the military shooting range located in the Changwon city were studied experimentally using soil washing process. As a washing solution, hydrogen chloride (HCl) concentrations of 0.001, 0.01, 0.1 and 0.2 N were used, and soil : solution ratios were 1 : 2, 1 : 3, 1 : 4, and 1 : 5. Particle diameter of contaminated soil of 4-0.075 mm, and washing period of 5, 10, 15, 20, 30, 60, and 120 min were used as operating parameters. The optimum concentration of HCl solution was 0.1 N (56.3% of Pb removal efficiency) with 15 minutes operation period in views of economics, and the optimum soil : solution ratio was determined as 1 g : 3 mL for 69.7% of Pb removal efficiency with 0.1 N HCl and 15 minutes washing period. As washing period increased, removal efficiency was increased until 20 min of the removal efficiency of 75.3%, and then almost stable. Pb removal efficiency in soil particle diameters of 0.075 mm or more was ranged from 77.0% to 82.0%, but it was decreased to 52.8% in diameter of less than 0.075 mm. Therefore, the optimum cut-off size of the soil particle diameter was found less than 0.075 mm. Combined HCl solution and ultrasonic washing method showed better removal efficiency compared to only water or HCl washing method for particle sizes above 0.075 mm.

Spatial Variability for Particle Size Distribution of Two Soils -II. Fitting Variogram Models and Kriging (토양(土壤)의 입경분포(粒徑分布)에 대(對)한 공간변이성(空間變異性) 분석(分析) -II. 입경공간변이성(粒徑空間變異性)의 Variogram 적합(適合)과 Kriging)

  • Park, Cang-Seo;Kim, Jai-Joung;Cho, Seong-Jin
    • Korean Journal of Soil Science and Fertilizer
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    • v.17 no.4
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    • pp.319-324
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    • 1984
  • Spatial variability of sand, silt, and clay contents on Hwadong SiCL and Jungdong SL was studied by using geostatistical concept. The measurements were made within a $33{\times}14m^2$ area at the nodes of 2 by 2m grids. The validity of all assumptions (stationarity, variogram models, etc.) was proved by Jack-knifing procedure and frequency distribution performed on the original data grids. The variogram of sand content on Hwadong SiCL was different from the linear model and that of clay content of Jungdong SL the linear and the spherical model in calculation of both kriged values and kriged variances in identification of its choice for simplicity.

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Analysis of physical conditions and vegetation distribution characteristics in Han river estuary (한강하구습지에서 물리적 조건과 식생분포 특성 분석)

  • Chung, Sang-Joon;Ahn, Hong-Kyu;Oh, Joon-Seok;Kim, Si-Nae
    • Proceedings of the Korea Water Resources Association Conference
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    • 2011.05a
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    • pp.208-208
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    • 2011
  • 하구는 하천의 담수와 염수가 교차되고 혼합되는 기 수역으로서 수생 생태계의 중요한 서식처이며 바다와 하천의 중요한 생태통로가 되고 있다. 국내에서는 4대 하천 중에서 한강하구가 유일하게 하구 둑이 없는 자연하구이며 나머지 대하천은 둑으로 인해 담수와 해수의 자연스러운 흐름이 제한되고 생태적인 연결이 단절된 형태이다. 한강하구에는 대규모 습지가 분포하고 있으며 특히 장항습지는 종단길이 약 7.5km, 폭 최대 500m에 달하는 대규모 습지로서 고라니를 비롯한 동물과 줄, 선버들을 비롯한 식물의 대규모 군락이 분포하는 등 생태적 가치가 높은 지역이다. 본 연구에서는 한강하구의 장항습지와 산남습지를 대상으로 특정구간의 물리적 특성, 식생의 분포특성을 파악하고 연관성을 분석하고자 하였다. 이를 위해 1차적으로 포괄적인 현장조사를 통해 전체 식생군락과 분포를 파악하고 특징적인 식생군락을 선정하였다. 2차적으로는 선정된 줄 및 선버들 군락지를 대상으로 토양단면, 토양입경을 분석하고, 새섬매자기 군락지를 대상으로 측량을 실시하였다. 3차적으로는 대상 군락의 지하수위를 측정하여 상호관계를 분석하였다. 이 결과는 우선 한강하구의 지역적 특징에 국한되지만 향후 타 지역과의 비교연구가 수행된다면 대상 식생과 물리적 생장조건과의 정량적인 관계가 도출될 것으로 판단된다.

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Remediation of Pb-Contaminated Soil by Soil Washing using Hdrochloric Acid (염산을 사용한 납 오염 토양의 토양 세척에 의한 정화)

  • Baek, Ki-Tae;Kim, Do-Hyung;Seo, Chang-Il;Yang, Jung-Seok;Lee, Jae-Young
    • Journal of Soil and Groundwater Environment
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    • v.12 no.3
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    • pp.17-22
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    • 2007
  • The feasibility of soil washing was investigated to remediate Pb-contaminated field soil. Hydrochloric acid was used as a washing agent. As mixing time increased from 5 min to 120 min, removal efficiency of Pb from contaminated soil increased from 69.3% to 81.9%. Two times washing with 0.2 M HCl showed 96% removal efficiency even at mixing time of 10 min. The Pb content in soil increased sharply as particle size of soil decreased, and removal efficiency was highly dependent on mixing time and temperature. Based on this result, acid washing technologies can be applied to remediate the Pb-contaminated soil used in this study.

Differences in Fraction of Na-Zeolite Particles Passed through Sand Columns Filled with Sand Particles in Different Sizes (입경(粒徑)이 다른 모래의 Column 내에서 시용(施用)된 Na-Zeolite의 이동입경별(移動粒徑別) 이동양상(移動樣相))

  • Kang, Shin-Jyung;Choi, Jyung
    • Korean Journal of Soil Science and Fertilizer
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    • v.18 no.3
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    • pp.240-246
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    • 1985
  • This study was conducted to estimate the proper particle size of Zeolite particle as the soil conditioner for sandy soil. On sand columns filled with different size of sand fractions, Zeolite particles of different size were applied. Tap water was percolated through those columns under the same water level as paddy soil during rice growth. The > 0.1mm fraction of Zeolite was not vertically moved although the water was percolated for 96 hours. The < 0.1mm fraction of Zeolite was moved out 85.7% in 2-1mm, 32.64% in 1-0.5mm, and 24.5% in 0.5-0.25mm sand column, respectively. The proper diameter of Zeolite particle for amelioration of sandy soils widely distributed around river side in Korea was estimated as 0.25-0.1mm fraction in consideration of its pore size.

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A Field Survey and Analysis of Ground Water Level and Soil Moisture in A Riparian Vegetation Zone (식생사주 역에서 지하수위와 토양수분의 현장 조사·분석)

  • Woo, Hyo-Seop;Chung, Sang-Joon;Cho, Hyung-Jin
    • Journal of Korea Water Resources Association
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    • v.44 no.10
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    • pp.797-807
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    • 2011
  • Phenomenon of vegetation recruitment on the sand bar is drastically rising in the streams and rivers in Korea. In the 1960s prior to industrialization and urbanization, most of the streams were consisted of sands and gravels, what we call, 'White River'. Owing to dam construction, stream maintenance, etc. carried out since the '70s, the characteristic of flow duration and sediment transport have been disturbed resulting in the abundance of vegetation in the waterfront, that is, 'Green River' is under progress. This study purposed to identify the correlation among water level, water temperature, rainfall, soil moisture and soil texture out of the factors which give an effect on the vegetation recruitment on the sand bar of unregulated stream. To this purpose, this study selected the downstream of Naeseong Stream, one of sand rivers in Korea, as the river section for test and conducted the monitoring and analysis for 289 days. In addition, this study analyzed the aerial photos taken from 1970 to 2009 in order to identify the aged change in vegetation from the past to the present. The range of the tested river section was 361 m in transverse length and about 2 km in longitudinal length. According to the survey analysis, the tested river section in Naeseong Stream was a gaining river showing the higher underground-water level by 20~30 m compared to Stream water level. The difference in the underground water temperature was less than $5^{\circ}C$ by day and season and the Stream temperature did not fall to $10^{\circ}C$ and less from May when the vegetation germination begins in earnest. The impact factor on soil moisture was the underground water level in the lower layer and the rainfall in the upper layer and it was found that all the upper and lower layer were influenced by soil particle size. The soil from surface to 1 m-underground out of 6 soil moisture-measured points was sand with the $D_{50}$ size of 0.07~1.37 mm and it's assumed that the capillary height possible in the particle size would reach around 14~43 cm. On the other hand, according to the result of space analysis on the tested river section of unregulated stream for 40 years, it was found that the artificial disturbance and drought promoted the vegetation recruitment and the flooding resulted in the frequency extinction of vegetation communities. Even though the small and large scales of recruitment and extinction in vegetation have been repeated since 1970, the present vegetation area increased clearly compared to the past. It's found that the vegetation area is gradually increasing over time.

Distribution of phosphorus in particle-size separates and specific gravity separates of soils (입경 및 비중별(比重別) 토양분화과 인산분포(燐酸分布))

  • Hong, Jung-Kook
    • Korean Journal of Soil Science and Fertilizer
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    • v.12 no.4
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    • pp.179-187
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    • 1980
  • 1) Soils (volcanic ash and muck) were fractionated into particle-size separates (200 - 20, 20 - 2, 2 - 0.5 and finer than $0.5{\mu}$ in diamter), and of which the silt fraction was further fractionated into specific gravity separates (more than 2.0, 2.0 - 1.7, 1.7 - 1.4 and less than 1.4 in $g/cc^3$). And total organic and inorganic phosphorus in the separates were determined. 2) The amounts of total, organic and inorganic phosphorus distributed in the particle-size separates were as follows fine clay > coarse clay > silt > fine sand fraction. The increase rate in the amounts of phosphorus was great in the separates finer than $20{\mu}$, and greatest in the fine clay fraction. 3) The amounts of total, oganic and inorganic phosphorus distributed in the specific gravity separates were as follows: 2.0 - 1.7 > 1.7 - 1.4 > heavier than 2.0 fraction. The increase rate in the amounts of phosphorus was in the following order 2.0 - 1.7 > 1.7 - 1.4 > heavier than 2.0 fraction. 4) Distribution of carbon, amorphous aluminum and free iron oxides in the particle-size separates and the specific gravity separates were examined, and the distribution and the formes of organo-minera1 complexes in the separates were discussed to shed light on the factors affecting the distribution of phosphorous into the separates. And it was estimated that there was close relation among the distribution of organic and inorganic phosphorus, and the distribution and the formes of organo-minera1 complexes.

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A Study on the Application of Physical Soil Washing Technology at Lead-contaminated Shooting Range in a Closed Military Shooting Range Area (폐 공용화기사격장 내 납오염 사격장 군부지의 물리적 토양세척정화기술 적용성 연구)

  • Jung, Jaeyun;Jang, Yunyoung
    • Journal of Environmental Impact Assessment
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    • v.28 no.5
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    • pp.492-506
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    • 2019
  • Heavy metal contaminants in the shooting range are mostly present in a warhead circle or a metal fragment present as a particle, these fine metal particles are weathered for a long period of time is very likely that the surface is present as an oxide or carbon oxide. In particular, lead which is a representative contaminant in the shooting range soil, is present as more fine particles because it increases the softness and is stretched well. Therefore, by physical washing experiment, we conducted a degree analysis, concentration of heavy metals by cubic diameter, composition analysis of metallic substances, and assessment of applicability of gravity, magnetism and floating selection. The experimental results FESEM analysis and the measurement results lead to the micro-balance was confirmed thatthe weight goes outless than the soil ofthe same size in a thinly sliced and side-shaped structure according to the dull characteristics it was confirmed that the high specific gravity applicability. In addition, the remediation efficiency evaluation results using a hydrocyclone applied to this showed a cumulative remediation efficiency of 71%,twice 80%, 3 times 91%. On the other hand, magnetic sifting showed a low efficiency of 17%,floating selection -35mesh (0.5mm)target soil showed a relatively high efficiency to 39% -10mesh (2mm) efficiency was only 16%. The target treatment diameter of soil washing should be 2mm to 0.075mm, which is applied to the actual equipment by adding an additional input classification, which would require management as additional installation costs and processes are constructed. As a result, it is found that the soilremediation of shooting range can be separately according to the size of the warhead. The size is larger than the gravel diameter to most 5.56mm, so it is possible to select a specific gravity using a high gravity. However, the contaminants present in the metal fragments were found to be processed by separating using a hydrocyclone of the soil washing according to the weight is less than the soil of the same particle size in a thinly fragmented structure.