• 한국농공학회지
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• 제31권2호
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• pp.92-103
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• 1989

This study was performed in order to produce the basic data for devising irrigation project and desalinization countermeasure through analyzing salt movement and desalinzation effects. The Desalinization experiments with water management practices were carried out, using the soil samples collected in New Manguem tideland. The changes of electrical conductivity, exchangeable sodium percentage, pH and hydraulic conductivity during the desalinization experiments, and the correlations between various factors influencing desalinization, were analyzed by the statistical method. The results obtained from this study were summarized as follows: 1. The sample soils used in this study were salin-sotlic soils with the high electrical conductivity and the high exchangeable sodium percentage, and the soil texture was silt loam. 2. A large amount of the soluble salts was removed in the begining of desalinization experiments. The initial electrical conductivity and the initial exchangeable sodium percentage decreased considerably in the beginning, and were gradually slow in the rate of decrease 3. The value of pH showed a tendency to increase during the desalinization and were little by little slow in the rate of increase, and could be estimated by the regression equation. 4. The initial hydraulic conductivity were raised greatly with gypsum treatment and the penmeability was maintained adequately, The hydraulic conductivity and the leaching time elapsed during the desalinization could be estimated by the regression equation. 5. The water requirement for desalinization with various water management practices could be estimated for a given electrical conductivity, exchangeable sodium percentage, and pH reading respectively.

• 한국농공학회지
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• 제31권1호
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• pp.96-105
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• 1989

This laboratory study was performed to produce basic data for the estimation of water requirements for desalinization, through analyzing changes of the electrical conductivity and the exchangeable sodium percentage during the desalinization of reclaimed tidelands. Desalinization experiments were carried out by two water management practices, namely, the leaching method by subsurface drainage and the rinsing method by surface drainage, using samples of silt loam soil and silty clay loam soil collected in reclaimed tidelands. The results obtained from this study were summarized as follows : 1. The sample soils used in this study were saline-sodic soils with the high electrical conductivity and the high exchangeable sodium percentage. 2. Changes of the electrical conductivity and the exchangeable sodium percentage with water requirements for desalinization showed a similar tendency in the desalinization experiment by the same water management practice. 3. The regression equation between the relative electrical conductivity(EC/EC) and water requirements for desalinization(Dw/Ds) could be described by Dw/Ds=O. 29x(EC/EC.) -0.982 (Leaching method), Dw/Ds=3. 678X0. 030(EC/EC ) (Rinsing method). 4. The regression equation between the relative exchangeable sodium percentage (ESP/ESP ) and water requirements for desalinization (Dw/Ds) could be expressed in Dw/Ds = 0.039 x (ESP/ESP. ) - 1. 134 (Leaching method), Dw/Ds=7. 197X0. 024(ESP/ESP ) (Rinsing method). 5. It was estimated that water requirements for the adequate desalinization would be Dw/Ds=0.3 (Leaching method) and Dw/Ds=3.0 (Rinsing method)

• 한국농공학회지
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• 제30권4호
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• pp.127-133
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• 1988

This study was performed to obtain the basic data analyzing salt movement and desalinization effects, and two different desalinization experiments through leaching and rinsing were carried out, using samples of silt loam soil and silty clay loam soil collected in reclaimed tidelands. The relationships between the electrical conductivity of saturation extract and the electrical conductivity at various dilutions, and the correlations between electrical conductivity, total salt concentration, exchangeable sodium percentage and pH during the desalinization of reclaimed tidelands, were analyzed by the statistical method. The results obtained from this study were summarized as follows: 1.The sample soils used in this study were saline-sodic soils in accordance with the USDA classi- fication system of salt affected soils. 2.The electrical conductivity of saturation extract could be estimated conveniently, using the electrical conductivity of extract from various different soil-water suspensions. 3.The total salt concentration could be expressed in the electrical conductivity, but there was a little difference by soil textures. 4.The regression analysis showed that the relationship between the electrical conductivity of saturation extract and the exchangeable sodium percentage during the desalinization of reclaimed lands could be described by a linear regression equation. 5.The value of pH showed a tendency to increase according as the exchangeable sodium percentage decreased during the desalinization of reclaimed tidelands.

• 한국토양비료학회지
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• 제48권5호
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• pp.326-331
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• 2015

High salinity and sodicity of soils play a negative role in producing crops in reclaimed tidal lands. To evaluate the effects of soil ameliorants on salt removal in a highly saline and sodic soil of reclaimed tidal land, we conducted a column experiment with treating gypsum, compost, and phosphate at 0-2 cm depth and measured the salt concentration of leachate and soil. Electrical conductivity of leachate was $45-48dSm^{-1}$ at 1 pore volume (PV) of water and decreased to less than $3dSm^{-1}$ at 3 PV of water. Gypsum significantly decreased SAR (sodium adsorption ratio) of leachate below 3 at 3 PV of water and soil ESP (exchangeable sodium percentage) below 3% for the whole profile of soil column. Compost significantly decreased ESP of soil at 0-5 cm depth to 5% compared with the control (20%). However, compost affected little the composition of cations below a depth of 5 cm and in leachate compared with control treatment. It was concluded that gypsum was effective in ameliorating reclaimed tidal lands at and below a soil layer receiving gypsum while compost worked only at a soil layer where compost was treated.

• 한국환경농학회지
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• 제37권4호
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• pp.317-323
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• 2018

우리나라 관개논의 여름철 강우기 Middleton's 분산성 점토는 불검출 ~ 4.8%의 범위로 나타났으며 최대값은 점토 함량 18% 이상 토양에서 나타났으나 점토 분산성은 점토 함량 18% 미만 토양에서 높게 나타났다. 대상지역의 60%에서 40마력이상 농기계를 사용한 경작연수가 길수록 분산성 점토 함량이 높은 값을 나타내었다. 단, 치환성 나트륨 함량 퍼센트의 차이가 큰 간척논은 예외로 나트륨함량이 높을수록 분산성 점토가 높았다.

• Journal of Microbiology and Biotechnology
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• 제21권4호
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• pp.341-346
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• 2011

To study the effects of salinity-sodicity on bacterial population and enzyme activities, soil samples were collected from the Bay of Yellow Sea, Incheon, South Korea. In the soils nearest to the coastline, pH, electrical conductivity ($EC_e$), sodium adsorption ratio (SAR), and exchangeable sodium percentage (ESP) were greater than the criteria of saline-sodic soil, and soils collected from sites 1.5-2 km away from the coastline were not substantially affected by the intrusion and spray of seawater. Halotolerant bacteria showed similar trends, whereas non-tolerant bacteria and enzymatic activities had opposite trends. Significant positive correlations were found between EC, exchangeable $Na^+$, and pH with SAR and ESP. In contrast, $EC_e$, SAR, ESP, and exchangeable $Na^+$ exhibited significant negative correlations with bacterial populations and enzyme activities. The results of this study indicate that the soil chemical variables related with salinity-sodicity are significantly related with the sampling distance from the coastline and are the key stress factors, which greatly affect microbial and biochemical properties.

• 한국토양비료학회지
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• 제31권2호
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• pp.120-127
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• 1998

우리나라 간척지 토양의 물리 화학적 특성을 체계적으로 정확히 분석하여, 개발초기 고염도 간척지의 합리적인 제염대책을 수립하기 위한 제염예측기법을 개발하는데 기초자료를 제공하고자 본 연구를 수행하였다. 전국 대단위 기존 간척지구, 현재 시행중에 있는 간척사업지구 및 간척 예정지구를 대상으로 11개 간척지구에서 채취한 306점의 공시토양을 분석하여 얻은 결과를 요약하면 다음과 같다. 간척사업 준공지구, 시행중지구, 예정지구별 가비중과 진비중의 평균값은 각각 1.30, 1.34, 1.32 및 2.62, 2.64, 2.65이고 전체평균은 1.33 및 2.64로 나타났다. 또한 공극율과 포화도의 평균값은 각각 50.4, 49.3, 50.2% 및 54.7. 57.1, 54.0%이고 전체평균은 49.6% 및 56.3%로 조사되었다. 조사지역의 토성분포는 전체 306개 조사지점중에서 미사토가 약45%, 미사질양토가 약45%, 양토가 약 10%를 차지하고 있으며, 토성이 미사토와 미사질양토인 지역을 합하면 전체의 약 90%에 달하였다. 따라서 우리나라 간척지의 토성은 대부분 미사를 다량으로 함유하고 있는 미사토 또는 미사질양토인 것으로 나타났다. 조사지역 토양의 염분농도는 전체 306개 조사지점중에서 전기전도도(EC) $20{\sim}30dS\;m^{-1}$인 토양이 약 63%, $30{\sim}40dS\;m^{-1}$인 토양이 약 23%의 분포를 보이고 있어 전체의 약 86%정도가 $20{\sim}40dS\;m^{-1}$ 범위내에 있으며, 개발초기 간척지토양의 염분농도를 대략 $20{\sim}40dS\;m^{-1}$ 범위로 볼수 있다고 판단된다. 조사지역 토양의 pH값은 전체적으로 6.5~7.9 범위내에 분포되어 있고, 전체평균값은 7.2로 조사지역별로 큰 차이가 없다. 공시토양의 치환성나트름백분율(ESP)은 38%가 ESP 30~40%, 53%가 ESP 40~50%로 전체의 약 90%이상이 ESP 30~50 % 범위내에 분포되어 있으며, 개발초기 간척지의 치환성나트륨백분율은 대략 30~50%범위내에 있다고 본다. 기존의 관련 실험결과와 본 조사지역 토양의 염분농도(전기전도도), 치환성나트륨백분율 및 pH 등 이화학적성질을 종합해서 분석해 볼 때, 우리나라 간척지토양은 U. S. Salinity Laboratory의 염해토양분류법상 염류알칼리토양에 속한다고 판단된다.

• 한국환경복원기술학회지
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• 제13권1호
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• pp.24-31
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• 2010

This study was carried out to analyze vegetation and soil characteristic, and ordination of Scrophularia takesimensis population, Ulleung Island. The Scrophularia takesimensis population was classified into Aster spathulifolius for. oharai dominant population, Vitis amurensis dominant population and Scrophularia takesimensis typical population. The Scrophularia takesimensis population was located in elevation of 1m to 6m, in Ulleung Island. In the study sites, soil organic matter, nitrogen, available phosphorous, exchangeable potassium, exchangeable calcium, exchangeable magnesium and exchangeable sodium concentration, and cation exchange capacity, and soil pH were 9.1~19.1%, 0.19~0.52%, 87.1~196.7mg/kg, 2.0~2.8cmol+/kg, 5.4~5.9cmol+/kg, 5.9~8.8cmol+/kg, 4.4~4.8cmol+/kg, 20.3~26.7cmol+/kg, and 6.8~8.0, respectively. The Vitis amurensis dominant population was mainly found in the high percentage of total nitrogen, organic matter, CEC in comparison with Aster spathulifolius for. oharai dominant population.

• 한국농공학회지
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• 제30권4호
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• pp.85-93
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• 1988

This laboratory study was carried out in order to produce fundamental data for analyzing salt movement and desalinization effects, using samples of silt loam soil collected in Gyehwado and Daeho reclaimed tidelans, and samples of silty clay loam soil collected in Kimie tideland. Desalinization experiments with gypsum treatment were performed to analyze changes of the hydraulicc conductivity with changes of the soil property and the salt concentration during the desalinization of reclaimed tideland soils by leaching through the subsufface drainage, and correlations between factors infl uencing the reclamation of salt affected soils were analyzed by the statistical method. The results were summarized as follows: 1. The reclaimed tideland soils used in this study were saline-sodic soils with the high exchangeable sodium percentage and the high electrical conductivity. 2. Changes of the hydraulic conductivity with the amount of leaching water and the leaching time elapsed were affected by the amount of gypsum except exchangeable sodium and clay contents. The regression equation between the depth of water leached per unit depth of soil (Dw / Ds : X) or the square root of the leaching time elapsed (T $^1$ $^2$ : X) and the relative hydraulic conductivity (HCr:Y) could be expressed in Y=a . bx. 3. The more exchangeable sodium and clay contents regardless of the amount of gypsum, the more the leaching time was required until a given volume of water was leached through the soil profile. The regression analysis showed that the relationship between the depth of water leached per unit depth of soil(Dw /Ds:X) and the square root of the leaching time elapsed(T$^1$$^2$ :Y) could be described by Y=a . Xb. 4. The hydraulic conductivity was influenced to a major degree by the salt concentration provided that the electrical conductivity was below 10 mmhos / cm during the desalinization of reclaimed tideland soils. The regression equation between the relative electrical conductivity ( ECr : X) and the relative hydraulic conductivity (HCr:Y) could be expressed in Y=a + b . X-$^1$. 5. In conclusion, the hydraulic conductivity, leaching requirements and the leaching time elapsed can be estimated when the salt concentration decreases to a certain level during the desalinization of reclaimed tidelands, and the results may be applied to the analysis of salt movement and desalinization effects.

• 한국관개배수논문집
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• 제8권1호
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• pp.48-60
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• 2001

This study was performed in order to produce the basic data for the estimation of water requirements for desalinization and developing prediction techniques of desalinization to be applicable in the beginning of tidal land reclamation through analyzing ch