• Title/Summary/Keyword: 제염용수량

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Effect of Flooding Treatment on the Desalting Efficiency and the Growth of Soiling and Forage Crops in a Sandy Soil of the Iweon Reclaimed Tidal Land in Korea (이원간척지 사질 염류토양의 담수제염처리가 제염효과와 녹비.사료작물의 생육에 미치는 영향)

  • Sohn, Yong-Man;Kim, Hyun-Tea;Jeon, Geon-Yeong;Song, Jae-Do;Lee, Jae-Hwang;Park, Moo-Eon
    • Korean Journal of Soil Science and Fertilizer
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    • v.43 no.1
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    • pp.16-24
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    • 2010
  • Effect of flooding on the desalting efficiency and the growth of sudan grass, barnyard grass, sesbania and corn was studied in a sandy soil of the Iweon reclaimed tidal land. Flooding plots were treated by 400 (one time flooding), 800 (two times flooding), and 1,200 mm(three times flooding) of water, respectively, and then soil salinities of the treated plots were compared with salinity of the control plot (not flooded) for estimation of desalting effect. Desalting ratio of 1,200 mm treatment was 78.3% for depth 0-20 cm, 70.5% for depth 20-40 cm and 60.8% for depth 40-60 cm, and then the soil salinity reached at 3~6 dS $m^{-1}$. Consequently, it was considered that sandy saline soil was satisfactorily desalted for upland crops to be cultivated by 1,200 mm flooding, but insufficiently desalted by 400 mm and 800 mm flooding because of high salinity ranged 5~14 dS $m^{-1}$ even after flooding treatment. In addition, it was estimated that soil salinity should be controled lower than 7.7 dS $m^{-1}$ in order to obtain more than 80%of crop emergence when four crops are simultaneously cultivated by inter- or mixed cropping in a field. Dry matter yields (kg $10a^{-1}$) was 1,068 for sudan grass, 696for barnyard grass, 1,426 for sesbania, and 1,164 for corn by 1,200 mm flooding treatment, but only 46.8~74.3% by 800 mm flooding treatment and 2.9~25.5% by 400 mm flooding treatment. Therefore, it is concluded that the flooding treatment more than 1,200 mm is necessary for satisfactory desalinization in order for the low salt tolerance crops to be cultivated in the sandy reclaimed tidal land.

A Laboratory Study on the Estimation of Water Requirements for the Desalinization of Reclaimed Tidelands (간척지토양의 제염용수량산정에 관한 실험연구)

  • 구자웅;한강원;은종호
    • Magazine of the Korean Society of Agricultural Engineers
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    • v.31 no.1
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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)

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Physiology of Forage Crops (사료작물 생리)

  • 이호진
    • Journal of The Korean Society of Grassland and Forage Science
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    • v.12 no.3
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    • pp.70-73
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    • 1992
  • 사료작물 저온발아성(低溫發芽性)은 수수 $\times$ 수단그라스잡종들이 좋았고 옥수수와 수단그라스는 비교적 저조하였고 PGE에 종자침지처리가 이탈리안라이그라스의 저온발아에 효과적이었다. 간척지의 수수파종시 염해 방지에는 모래를 파종후 피복하여 제염(除鹽) 효과를 얻을수 있었다. 수수류의 토양수분조건에 대한 광합성 연구는 포장용수량의 $60\sim80%$의 조건에서 광합성이 가장 왕성하였고 건물수량도 동일한 결과를 나타내었다. 옥수수의 광이용과 초형과의 관계연구는 이삭상부 엽각의 직립화는 밀식 조건에서 광이용성이 증가되었고 건물 및 종실수량에서 종수가 있었다. 또 밀식화에 따라 직립화 경향이 현저하였으며 옥수수의 다수성초형의 육성이 요청되었다. 질소시비에 대한 청예류의 생장 반응 연구들은 수단그라스에서 10a당 40Kg까지는 건물수량생산을 증가시켰으나 80Kg/10a 사용시는 질산태질소함량이 중독위험치를 초과하였다. 이러한 질산태질소의 중독위험은 6엽기까지 존재하였고 청산중독의 위험농도는 4엽기 이전까지, 또 18/$8^{\circ}C$의 저온조건에서 나타났다. 옥수수의 적정재식 밀도는 10a당 16.600본까지 밀식할수록 증가되었으나 가소화수량과 종실수량은 5.500본과 10Kg/10a 에서 최고치를 나타내었고 질소 추비 효과는 대관령 같은 고산지대에서는 나타나지 않았다. 맥류의 총체(總體)사료 이용성은 호밀, 밀, 보리 순(順)으로 저하하였고 파종시기가 빠를수록 월동성이 향상되었으며 수확적기는 출수후 24일경이었다. 호밀의 청예이용에는 월동후 2회예취와 12cm높이가 건물수량과 TDN수량을 높힐 수 있었다. 수수$\times$ 수단잡종의 출수기 이전 예취는 고사 경비율을 줄일 수 있었고 년 2회 예취와 예취높이 10cm가 가장 좋았다. 유채는 생육기간이 길어질수록 수량은 증가하였고 소화율의 감소도 현저하지 않았다.

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Salinity Effects on Growth and Yield Components of Rice (관개용수내 염분농도가 벼 생육 및 수량에 미치는 영향)

  • Choi, Sun-Hwa;Kim, Ho-Il;Ahn, Yeul;Jang, Jeon-Ryeol;Oh, Jong-Min
    • Korean Journal of Ecology and Environment
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    • v.37 no.2 s.107
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    • pp.248-254
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    • 2004
  • This study was conducted to investigate the effects of salinity in irrigation water on the growth, yield components, yield and grain quality of rice plant by the pot experiments. Irrigation waters were supplied with control and amended with NaCl at 1,000, 2,000, 3,000, 5,000, and 7,000 ${\mu}s\;cm^{-1}$ electrical conductivity. A randomized block design was used with four replicates for each treatment and control. As increasing salt concentration, plant height, tiller number, SPAD value, dry weight, content of N, P, and K, ripened grain ratio (%), 1,000 grain weight, and protein content (%) tended to decrease, especially, significant at 3,000 ${\mu}s\;cm^{-1}$ of salt level. Grain yield decreased significantly at all treatments. The percentage of head rice slightly tended to increase as the salt concentration due to the decrease of green kernel. The percentage of green kernel was significantly lower at 3,000 ${\mu}s\;cm^{-1}$ of salt level than the control.