• 제목/요약/키워드: Salt affected soils

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간척지 염해토양의 특성과 제염기법 (Properties and Disalinization of Salt-affected Soil)

  • 손재권;송재도;신원태;이수환;류진희;조재영
    • 한국유기농업학회지
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    • 제24권2호
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    • pp.273-287
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    • 2016
  • Accumulation of excessive salt in Reclaimed coastal tidelands can reduce crop yields, reduce the effectiveness of irrigation, degradation of soil structure, and affect other soil properties. These salts has shown to cause specific ions in the plant over a period of time leads to ion toxicity or ion imbalance and a continuous osmotic phase that prevents water uptake by plants due to osmotic pressure of saline soil solution. This review focuses on the characteristics of salt-affected soils, mechanisms of salt-tolerance plants, desalinization technology, and soil management to maintain sustainable agro-ecosystem in salt-affected soils.

염류집적 유형이 다른 토양의 교환성 양이온 측정 (Determination of Exchangeable Cations in Soils Affected by Different Types of Salt Accumulation)

  • 이예진;윤홍배;김록영;이종식;송요성;성좌경;양재의
    • 한국토양비료학회지
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    • 제45권2호
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    • pp.135-142
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    • 2012
  • 염류집적 토양의 교환성 양이온을 분석할 때 수용성 양이온이 많이 존재하는 경우 교환성 양이온이 높게 측정될 수 있으므로 수용성 양이온을 제외한 교환성 양이온을 측정하여야 한다. 수용성 양이온을 제거하기 위하여 전처리 과정 중 알콜 등으로 세척을 하거나 전체 양이온을 구한 후 포화 용액 중 녹아있는 수용성 양이온을 빼는 방법이 있다. 본 실험 결과 시설재배지 토양의 경우 전처리에서 세척하는 방법을 사용해도 타당할 것으로 판단되나, Na 함량이 높은 간척지 토양은 포화용액에 녹아있는 수용성 양이온을 빼야 정확한 교환성 나트륨을 구할 수 있다고 판단되었다. 또한 $EC_e$가 4 이하인 토양에서는 수용성 양이온을 제외할 필요가 없었다.

간척지 염해토양의 Phytoremediation에 의한 제염 (Desalinization of Salt-affected Soil by Phytoremediation)

  • 손재권;송재도;신원태;이수환;류진희;조재영
    • 한국유기농업학회지
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    • 제24권3호
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    • pp.583-598
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    • 2016
  • Salted-affected soil is a major environmental constraint with severe negative impacts on agricultural productivity and sustainability in reclaimed tidelands. This review focuses on the phytoremediation of reclaimed tidelands. We address the process of phytoremediation of these soils, comparison of phytoremediation with other amelioration approaches, driving forces contributing to the process, selection of phytoremediation crops, and the role of cropping in securing environmental integrity under salt-affected soils.

간척지 토양의 제염과정중 수리전도도의 변화 (Changes of Hydraulic Conductivity During Desalmization of Reclaimed Tidelands)

  • 구자웅;은종호
    • 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.

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Determination of Nutrient Contents and In vitro Gas Production Values of Some Legume Forages Grown in the Harran Plain Saline Soils

  • Boga, M.;Yurtseven, S.;Kilic, U.;Aydemir, S.;Polat, T.
    • Asian-Australasian Journal of Animal Sciences
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    • 제27권6호
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    • pp.825-831
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    • 2014
  • The aim of this study was to determine the nutritive value of some legume species in salt-affected soils of South-East Anatolian region using chemical composition and in vitro gas production kinetics. In this study, Lotus corniculatus, Trifolium alexandrinum, Medicago sativa were sown and tested in four different locations. A 3 by 4 factorial design with 3 legume species and 4 salt levels (non salty electrical conductivity (EC)<4 dS/m; low salt: 4 dS/m>EC<8 dS/m, medium saline: 8 dS/m>EC<16 dS/m and high salt: 16 dS/m>EC) was used in the study. Results indicated that salinity and plants had no significant effect on ash and ether extract. Dry matter (DM), acid detergent fiber, digestible dry matter, dry matter intake (DMI) were affected by plant, salinity and plant${\times}$salinity interaction. On the other hand neutral detergent fiber, relative feed value (RFV), and DMI were affected by salinity and plant${\times}$salinity interaction. Mineral contents were affected by plant species, salinity and salinity${\times}$plants interactions. In vitro gas production, their kinetics and estimated parameters such as were not affected by salinity whereas the gas production up to 48 h, organic matter digestibility, metabolizable energy (ME), and net energy lactation ($NE_L$) were affected by plant and plant${\times}$salt interaction. Generally RFVs of all species ranged from 120 to 210 and were quite satisfactory in salty conditions. Current results show that the feed value of Medicago sativa is higher compared to Lotus corniculatus and Trifolium alexandrinum.

Physiological Responses of Tomato Plants and Soil Microbial Activity in Salt Affected Greenhouse Soil

  • Sung, Jwakyung;Lee, Suyeon;Nam, Hyunjung;Lee, Yejin;Lee, Jongsik;Almaroai, Yaser A.;Ok, Yongsik
    • 한국토양비료학회지
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    • 제45권6호
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    • pp.1065-1072
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    • 2012
  • Crop productivity decreases globally as a result of salinization. However, salinity impact on greenhouse-grown crops is much higher than on field-grown crops due to the overall concentrations of nutrients in greenhouse soils. Therefore, this study was performed to determine the short-term changes in growth, photosynthesis, and metabolites of tomato plants grown in greenhouse under heavily input of fertilizers evaluated by microbial activity and chemical properties of soils. The soils (< 3, 3.01~6, 6.01~10 and > 10.01 dS $m^{-1}$) from farmer's greenhouse fields having different fertilization practices were used. Results showed that the salt-accumulated soil affected adversely the growth of tomato plants. Tomato plants were seldom to complete their growth against > 10.0 dS $m^{-1}$ level of EC. The assimilation rate of $CO_2$ from the upper fully expanded leaves of tomato plants is reduced under increasing soil EC levels at 14 days, however; it was the highest in moderate or high EC-subjected (3.0 ~ 10.0 dS $m^{-1}$) at 28 days. In our experiment, soluble sugars and starch were sensitive markers for salt stress and thus might assume the status of crops against various salt conditions. Taken together, tomato plants found to have tolerance against moderate soil EC stress. Various EC levels (< 3.0 ~ 10.0 dS $m^{-1}$) led to a slight decrease in organic matter (OM) contents in soils at 28 days. Salinity stress led to higher microbial activity in soils, followed by a decomposition of OM in soils as indicated by the changes in soil chemical properties.

낮은 구속압에서 고결화 혼합재의 미소변형강성 (Small Strain Stiffness of Salt-Cemented Granular Media under Low Confining Pressure)

  • 쭝꽝훙;변용훈;짠밍콰;이종섭
    • 한국지반공학회:학술대회논문집
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    • 한국지반공학회 2010년도 춘계 학술발표회
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    • pp.448-456
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    • 2010
  • The mechanical behavior of granular soils is affected by particle bonding including natural cementation. This study addresses a simple model of small strain stiffness and salt concentration based on wave measurements of salt-cemented particulate media. Published models of artificially cemented soils with different curing methods and several types of cementation agents are reviewed. Glass beads with the median diameter of D50 = 0.5mm are prepared in rectangular cells using the water-pluviated method in salt water with different concentrations. Piezo disk elements and bender elements embedded in the cell are used for the measurements of compressional and shear waves. The relationships between elastic wave velocities and salt concentration show an exponential function. The measured small strain stiffness matches well the predicted small strain stiffness based on micromechanics for simple cubic monosized sphere particles. This study demonstrates that the salt concentration in salt-cemented specimen may be evaluated by using elastic wave velocities.

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가로변 반송 염해정도에 따른 토양 및 식물체 내 염류이온의 계절별 변화 (Seasonal Variations of De-icing Salt Ions Harvested from Soils and Plants according to the Salt Damage of Pinus densiflora f. multicaulis on Roadsides)

  • 이재만;박선영;윤용한;주진희
    • 한국환경과학회지
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    • 제29권4호
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    • pp.395-402
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    • 2020
  • This study was conducted to analyze seasonal variations of de-icing salt ions harvested from soils and plants according to salt damage of Pinus densiflora f. multicaulis, a evergreen conifer, on roadsides. Pinus densiflora f. multicaulis was divided into three groups referred to SD, ND, and WD (serious salt damage (SD) = 71-100%, normal salt damage (ND) = 31-70%, and weak salt damage (WD) = 0-30%) based on the degree of visible foliage damage, and measured acidity (pH), electrical conductivity(EC), and de-icing salt ions (K+, Ca2+, Na+, and Mg2+) harvested from soils and plants. The results indicated that acidity, electrical conductivity, and de-icing salt ions of soils and plants were significantly affected by seasonal variation and salt damage. In addition, a strong positive liner relationship was observed in plants between the concentration of de-icing salts and salt damage in spring, while the relationship among seasonal variation and salt damage in soil were not significant. The results from this study has important implications for the management of conifer species in relation to salinity and roadsides maintenance.

AgCl 침전 전후 전기전도도 변화를 이용한 염해지 포화침출액의 염소 이온 신속 정량 (A rapid determination of chloride in saturated paste extracts of salt-affected soils using EC change upon AgCl precipitation)

  • 이예훈;김지윤;이정수;;박지원;한광현
    • Journal of Applied Biological Chemistry
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    • 제60권3호
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    • pp.279-282
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    • 2017
  • 염해토양에서 염소이온은 작물에 대한 독성이 가장 큰 음이온이다. 일반적으로, 이온 크로마토그래피와 전위차 적정법 등 정밀한 기기분석이 염소이온 분석에 이용되고 있으나, 본 연구에서는 간단한 EC 메터를 이용해 신속히 그리고 비교적 정밀하게 염해지 염소이온이 정량 가능하다는 것을 확인하였다. $Cl^-$이 AgCl로 침전될 때 수반되는 전기전도도 변화도(dEC)는 염소이온 농도와 매우 직선적인 비례 관계가 있었으며, 감도, 검량 구간, 정량한계, 정밀도 및 분석 적응성 모두 양호한 것으로 조사되었다. 또한, 이 Ag-dEC법으로 분석된 전남 고흥군 간척지 일원 토양침출액의 염소이온 농도는 이온 크로마토그래피의 분석결과와 매우 잘 일치하였다.

고화준설토의 역학적 특성에 대한 염분의 영향 (Effect of Salinity on Mechanical Characteristics of Stabilized Dredged Soil)

  • 김윤태
    • 한국지반공학회논문집
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    • 제27권9호
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    • pp.47-53
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    • 2011
  • 항로유지 준설과 해안건설 현장에서 채취된 해양준설토는 일반적으로 점토 성분 내에 다량의 염분을 함유하고 있다. 본 논문은 염분이 포함된 고화준설토(S-SDS)와 염분이 포함되지 않은 고화준설토(N-SDS)의 역학적 특성에 대한 염분의 영향을 분석하였다. 이를 위해 염분이 포함된 준설토와 염분이 포함되지 않은 준설토에 각각 동일한 양의 시멘트를 혼합하여 여러 개의 시편을 제작하였다. 7일 혹은 28일 양생된 N-SDS와 S-SDS 시편에 대하여 전자현미경 분석, 일축압축시험 및 구속압축시험을 수행함으로써 고화준설토의 미세 흙구조, 강도 및 압축 특성을 비교 및 분석하였다. 실험결과 점토에 포함된 염분은 고화준설토의 미세 흙구조 형성 뿐만 아니라 고화토의 강도발현에 영향을 주는 것으로 나타났다. 또한 S-SDS의 압축지수와 팽창지수는 N-SDS 보다 크게 나왔다. 이것으로부터 염분은 고화토의 압축성을 증가시킨다는 것을 알 수 있다. 염분은 고결화된 준설토의 강도발현 및 압축성에 악영향을 주었다.