• 제목/요약/키워드: Reclaimed soil

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Prediction of the Salinization in Reclaimed Land by Soil and Groundwater Characteristics

  • Jeon, Jihun;Kim, Donggeun;Kim, Taejin;Kim, Keesung;Jung, Hosup;Son, Younghwan
    • 한국농공학회논문집
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    • 제63권6호
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    • pp.131-140
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    • 2021
  • It is becoming more important to utilize reclaimed lands in South Korea, due to the increasing competition for its usage among different sectors. However, the high groundwater level and poor permeability are exposing them to deterioration by salinization. Salinization is difficult to predict because the pattern changes according to various characteristics of soil and groundwater. In this study, the capillary rising time was studied by the water content profile in the soil. The prediction equation of soil salinity was developed based on simulation result of the CHEMFLO model. to enable prediction considering various soil water content and groundwater level. The two terms constituting the equation showed the coefficients of determination of 0.9816 and 0.9824, respectively. Using the prediction equation of the study, the surface salinity can be easily predicted from the initial surface salinity and the salinity of the groundwater. In the future, more precise predictions will be possible with the results of studies on the hydraulic characteristics of various reclaimed soils, changes in water content profile by seasonal and climate events.

임해매립지의 느티나무 식재 이후 뿌리 생장특성 -뿌리구조 및 세근의 공간적 분포를 중심으로- (Roots Growth Characteristics of Zelkova serrata Makino. after Replanting in the Reclaimed Land from the Sea - On the Root Structure and Spatial Distribution of Fine Root Phytomass -)

  • 김도균
    • 한국조경학회지
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    • 제35권5호
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    • pp.46-55
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    • 2007
  • This study was carried out to analyze both the root structure and the fine root phytomass of the vertical and horizontal distribution of Zelkova serrata Makino. which was transplanted in the reclaimed land from the sea in Gwangyang, Jeonnam, South Korea. The base ground was reclaimed land from the sea. $Z_1$ of the planting ground was filled to a $100{\sim}150cm$ thickness with the improved soil instead of the reclaimed soil from the sea, $Z_2$ of the planting ground was covered to a $20{\sim}30cm$ thickness with the improved soil and $Z_3$ of the planting ground was mounded to 120cm thickness with the improved soil on the reclaimed land from the sea. In addition, $Z_4,\;Z_5\;and\;Z_6$ of the planting grounds were at the large-sized mound on the reclaimed land from the sea. $Z_4$ of the planting ground was located at the lowest level, $Z_5$ planting ground was located at the slope and $Z_6$ planting ground was located at the top of the large-sized mound. The large-sized mounds contain 3 layers, the base layer was reclaimed land from the sea and the second layer was mounded to a $200{\sim}300cm$ thickness with the desalinized soil from the sea on the base layers and the finally layers were mounded to a $80{\sim}120cm$ thickness with improved soil on the second layer. The planting grounds $Z_3,\;Z_4,\;Z_5\;and\;Z_6$ developed roots such as tap roots, lateral roots and heart roots. However, in $Z_1\;and\;Z_2$ roots development were inhibited. The fine-root phytomass of the 6 planting ground types was as follows: $113.5g\;DM/m^2$ for $Z_5$, $105.5g\;DM/m^2$ for $Z_4$, $88.3g\;DM/m^2$ for $Z_3$, $81.0g\;DM/m^2$ for $Z_6$, $73.0g\;DM/m^2$ for $Z_2$, $43.3g\;DM/m^2$ for $Z_1$. The vertical distribution of the fine root phytomass decreased from the upper to the deeper soil profiles in the 6 mound types. The fine root phytomass was $43.3{\sim}71.8%$ in a $0{\sim}20cm$ thickness of soil layer and it decreased according to the distance from the nearest trees. The root growth in the improved soil was better than in the reclaimed soil from the sea. However, root growth decreased more in the disturbed soils even though the planting grounds contained the improved soils. The retarded development of roots and the spatial distribution patterns of the fine root phytomass were closely connected to the reclaimed soil from the sea. In the disturbed soil, the soil hardness and alkalic cation($Na^+,\;K^+,\;Ca^{2+},\;Mg^{2+}$). were high and the soil water was lacking. We suggest that the construction of planting grounds and the improvement of bad soil are necessary for the proper and effective growth of landscaping plants.

Effect of Soil Salinity Levels on Silage Barley Growth at Saemangeum Reclaimed Tidal Land

  • Lee, Sanghun;Bae, Hui-Soo;Lee, Soo-Hwan;Kang, Jong-Gook;Kim, Hong-Kyu;Lee, Kyeong-Bo;Park, Ki-Hoon
    • 한국토양비료학회지
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    • 제46권5호
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    • pp.365-372
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    • 2013
  • Crop development and nutrient availability are strongly influenced by soil salinity levels. This study was conducted to investigate the effect of rice straw and nitrogen (N) fertilizer for silage barley under various soil salinity levels at Saemangeum reclaimed tidal land. Three levels of rice straw (0, 2.5, 5.0 ton rice straw $ha^{-1}$) and N (0, 150, 225 kg N $ha^{-1}$) were applied at 0.04, 0.23, 0.35% soil salinity levels. Biomass yield of silage barley was influenced by the interactions between rice straw application and N fertilization. Although there was no single effect of rice straw application on biomass yield, it was significantly increased with N application and a rice straw application of 5.0 ton $ha^{-1}$. Sodium content in silage barley was significantly lower at 0.04% salinity level, and but it was statistically increased with increasing soil salinity levels. Forage qualities such as total digestible nutrients and relative feed value of silage barley were significantly higher with N application at 0.04% salinity level, but there was no effect of rice straw application. Soil organic matter content was increased with N and rice straw application regardless of soil salinity level. The results of this study showed that the effect of rice straw and N fertilization on silage barley was influenced by soil salinity levels, which indicates that the management practice of silage barley at Saemangeum reclaimed tidal land should consider soil salinity levels.

서해안 신간척지에서 유채-피마자 작부체계시 토양염농도 및 침수가 생육 및 수량에 미치는 영향 (Effect of Soil Salinity and Flooding on Plant Growth and Yield of Rape-Castor Bean Cropping System in the Newly Reclaimed Tidal Land of Western Seaside of Korea)

  • 손용만;전건영;송재도;이재황;박무언
    • 한국토양비료학회지
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    • 제42권5호
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    • pp.355-363
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    • 2009
  • 간척조성지 밭작물 재배기술개발의 일환으로서 바이오에너지 생산을 위한 피마자와 유채를 공시작물로 하는 작부체계로 유지작물의 재배가능성을 검토하였다. 피마자의 생존개체율은 토양염농도 $4dS\;m^{-1}$에서 급격히 감소하는 경향을 보였고, 초장이 50% 정도 단축되는 토양염농도는 $4dS\;m^{-1}$으로 추정되었다. 유채의 초장생육이나 수량은 토양염농도가 증가할수록 감소하여 초장은 $6dS\;m^{-1}$일 때, 수량은 $2{\sim}2.5dS\;m^{-1}$의 범위에서 50%가 감소되는 것으로 추산되었다. 강우가 많은 계절에 재배되는 피마자는 염농도 뿐만 아니라 습해에도 약하여 배수가 불량한 영상강과 화옹 간척지에서 각각 0.8과 $6.5kg\;10a^{-1}$로 적었으나 배수가 좋은 이원 간척지는 $42kg\;10a^{-1}$로서 비교적 높은 경향이었다. 겨울작물인 유채는 비강우기간의 재염화가 심하였던 화옹 간척지에서 전혀 수량을 얻지 못하였으나 출현불량과 염농도의 변이가 심하였던 이원 간척지는 종실수량이 평균 $9kg\;10a^{-1}$로서 매우 낮았고, 염농도가 낮게 유지된 영산강간척지는 $332kg\;10a^{-1}$로서 높은 경향을 보였다. 결론적으로 서해안 간척지에서 피마자와 유채의 생육 및 수량성을 고려해 볼 때 토양염농도가 피마자 $4dS\;m^{-1}$, 유채 $3dS\;m^{-1}$ 이하로 관리되고, 침수피해가 없도록 배수관리가 된다면 유지작물재배가 충분히 가능할 것으로 판단되었다.

간척지산 쌀의 미질에 대한 고찰 및 우리나라 간척지 토양의 특성 조사 (Discussion on Quality of Rice Produced at Reclaimed Tidal Land in Korea and its Soil Characteristics)

  • 이승헌
    • 한국관개배수논문집
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    • 제10권1호
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    • pp.33-43
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    • 2003
  • This study was carried out to obtain the scientific data as high quality rice produced at reclaimed tidal land. Thus we reviewed related papers and reports and, collected and analyzed 90 soil samples at 9 reclaimed tidal lands in Korea. The results were s

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Capillary Characteristics of Water and Cations in Multi-layered Reclaimed Soil with Macroporous Subsurface Layer Utilizing Coal Bottom Ash

  • Ryu, Jin-Hee;Chung, Doug-Young;Ha, Sang-Keon;Lee, Sang-Bok;Kim, Si-Ju;Kim, Min-Tae;Park, Ki-Do;Kang, Hang-Won
    • 한국토양비료학회지
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    • 제47권6호
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    • pp.406-411
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    • 2014
  • Serious problems in reclaimed land agriculture are high soil salinity and poor vertical drainage, so desalinization in these soils is very difficult. Also, although desalinization is accomplished in reclaimed top soils, before long, soils are resalinized according to capillary rise of salts from the subsurface soils. To resolve these problems, multi-layered soil columns with subsurface layer of macroporous medium utilizing coal bottom ash (CBA) were constructed and the effects of blocked resalinization of these soils were investigated. In this experiment soil samples were collected from Munpo series (coarse-loamy, nonacid, mixed, mesic, typic Fluvaquents). The soil texture was silt loam and the EC was $33.9dS\;m^{-1}$. As for groundwater seawater was used and groundwater level of 1 cm from the bottom was maintained. The overall rate of capillary rise was $2.38cm\;hr^{-1}$ in soil 60 cm column, $0.25cm\;hr^{-1}$ in topsoil (30 cm) + CBA (5 cm) + subsurface soil (10 cm) column and $0.08cm\;hr^{-1}$ in topsoil (30 cm) + CBA (10 cm) + subsurface soil (10 cm) column. In multi-layered soil columns with CBA 20, 30 cm layer, wetting front due to capillary rise could not be seen in top soil layer. After 70 days capillary rise experiment water soluble Na+ accumulated in top soil of soil columns with CBA 20, 30 cm was diminished by 92.8, 96.5% respectively in comparison with Na+ accumulated in top soil of soil 60 cm column because CBA layer cut off capillary rise of salts from the subsurface soil. From these results we could conclude that the macroporous layer utilizing CBA placed at subsurface layer cut off capillary rise of solutes from subsurface soil, resulting in lowered level of salinity in top soil and this method can be more effective in newly reclaimed saline soil.

새만금 간척지 포화상태 흙의 제염예측기법 개발 (Development of Prediction Method of Desalination on a Saturated Soil in Saemanguem Reclaimed Area)

  • 서동욱;김현태;장병욱;이상훈
    • 한국농공학회논문집
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    • 제51권2호
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    • pp.29-34
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    • 2009
  • A series of laboratory model tests and numerical analysis is performed to analyze characteristics of desalination and to predict a period of desalination for subsurface saturated soil in Saemanguem reclaimed area. The results show that quantity of desalination is small as salinity of water is increased. On the contrary, quantity of desalination is increased as salinity of soil is high. In order to decrease the salinity to 10 % of initial salinity of soil at depth of 2 m, it takes 11 years to desalinate the soil 50 m away from drainage ditch. For soil at depth of 1.5 m only 1 year to desalinate the soil near drainage ditch. Also, water head of 80 cm is required to desalinate to 10 % of initial salinity for 60 cm thick soil. Because the following results is based upon the Saemangeum soil, an application of this result for another field will be cautious. More research will be required on this matter.

해안간척지토양의 생물학적 토성개량에 관한 연구 5 (Biological improvement of reclaimed tidal land soil (V))

  • 홍순우;하영칠;이광웅
    • 미생물학회지
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    • 제8권1호
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    • pp.13-20
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    • 1970
  • Chenges in respiration of the soils collected from the reclaimed tidal soil in Chogi-ri, Kanghwa Island and treated with organic matters are presented. The measurement of the respiration for the smaples, which were incubated for 0,2,4 and 5 weeks, were carried out by using Warburg's respirometer. While the respirations of the samples added by organic matters were increased 6.7 - 28.0 times compared with that 0 week during the incubation in case of 5-year soil, the respiration in case of 3-year soil were increased 3.3-11.8 times. Thus, the effect of adding organic matters on the respiration of the experimented soils, as this indicates, was much higher for the soil of 5-year area than that of 30-year area. And for the organic matters Salicornia was most effective and then Suaeda and Oryzae. The samples treated with Salicornia and Suaeda showed their highest respiration rate at the 4th week, but the one with Oryzae was measured to increase progressively during 5 weeks experimented. Regarding the salinity, content of organic matters and number of bacteria, in each intact soil experimented, 5-year soil samples had much poor habitat then 30-year soil for the activity of soil microorganisms, but according to the result mentioned above, it is firmly believed that the addition of organic matters on the saline soil is one of the best means to change the reclaimed tidal land into arable land with less time duration.

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석문 간척지에서 돈분액비 및 석고처리가 여름철 사료작물 수량 및 토양이화학성에 미치는 영향 (Effects of Soil Amendment Application on Soil Physico-chemical Properties and Yields of Summer Forage Crops in the Sukmoon Reclaimed Tidal Land in Korea)

  • 최기춘;윤세형;신재순;김동관;한효심;수판자니;이경동
    • 한국환경농학회지
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    • 제29권4호
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    • pp.354-361
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    • 2010
  • Soil physico-chemical properties and microbial densities are affected by organic sources and soil amendment applied to improve soil environments or quality. Generally organic fertilizer effects on forage crops yield and soil properties are partly due to changes of soil composition. We investigated the effects of swine slurry (SS), swine slurry composting-biofilteration(SCB) and chemical fertilizer(F) with gypsum(G) combinations on soil physico-chemical properties and yields of summer forage crop in the Sukmoon reclaimed tidal land in Korea. The forage crops used in this experiment were corn and sorghum$\times$sudangrass hybrid(hereafter sorghum). Our results showed that the soil physico-chemical properties in the combined (F+G, SS+G, SCB+G) treatments increased contents of organic matter and exchangeable $Ca^{2+}$, but exchangeable $Na^+$, $K^+$ and $Mg^{2+}$ reduced to 1-10% for two forage crops, compared to non-combined (F, SS, SCB) treatment. The density of soil microorganism such as bacteria, actinomycetes and fungi, increased significantly by SS+G and SCB+G treatments. This means that treatment of combined organic fertilizer with G lowered salinity levels and improved with microbial growth. The combined treatments also increased the total yields 2.3-6.2% for corn and 2.0-8.7% for sorghum, compared with non-combined treatment. This experiment suggests the combined treatments could increase the total yields of summer forage crops and change of soil physico-chemical properties in the Sukmoon reclaimed tidal land in Korea.

남해안 매립 해성점토의 물리적 특성과 압축지수의 상관성 분석 (Correlation Analysis between Physical Properties and Compression Index for Dredged and Reclaimed Marine Clay in the Southern Coast of Korea)

  • 임석훈;유남재
    • 산업기술연구
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    • 제34권
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    • pp.53-59
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    • 2014
  • The single regression method was used to analyze the correlationship between the compression index with mechanical properties for reclaimed marine clays in the southern coast of Korea. As results of performing regression analysis for 200 samples about reclaimed marine clays in the southern coast of Korea, linear regression lines between compression index and natural water content, void ratio in situ, and liquid limit respectively wer obtained. The changed properties of soil due to disturbance during dredging and reclaiming could be investigated by comparing with the existing empirical correlation equations for the original ground where dredging was performed. These regression equations might be rationally used in the preliminary evaluation of settlement of dredged and reclaimed marine clayey ground in the southern coast of Korea.

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