• 제목/요약/키워드: SALINE-SODIC SOIL

검색결과 32건 처리시간 0.021초

Effect of Compost and Gypsum Application on the Chemical Properties and Fertility Status of Saline-Sodic Soil

  • Sarwar, Ghulam;Ibrahim, Muhammad;Tahir, Mukkram Ali;Iftikhar, Yasir;Haider, Muhammad Sajjad;Noor-Us-Sabah, Noor-Us-Sabah;Han, Kyung-Hwa;Ha, Sang-Keun;Zhang, Yong-Seon
    • 한국토양비료학회지
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    • 제44권3호
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    • pp.510-516
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    • 2011
  • Salt-affected soils are present in Pakistan in significant quantity. This experiment was conducted to assess the effectiveness of compost for reclamation and compare its efficiency with gypsum. For this purpose, various combinations of compost and gypsum were used to evaluate their efficacy for reclamation. A saline-sodic field having $pH_s$ 8.90, $EC_e$ $5.94dS\;m^{-1}$ and SAR $34.5(mmol\;L^{-1})^{1/2}$, SP (saturation percentage) 42.29% and texture Sandy clay loam, gypsum requirement (GR) $8.75Mg\;ha^{-1}$ was selected for this study. The experiment comprised of seven treatments (control, gypsum alone, compost alone and different combinations of compost and gypsum based on soil gypsum requirements). Inorganic and organic amendments (gypsum and compost) were applied to a saline sodic soil. Rice and wheat crops were grown. Soil samples were collected from each treatment after the harvest of both crops and analyzed for chemical properties (electrical conductivity, soil reaction and sodium adsorption ratio) and fertility status (organic matter, available phosphorus and potassium contents) of soil. Results of this study revealed that compost and gypsum improved chemical properties (electrical conductivity, soil reaction and sodium adsorption ratio) of saline sodic soil to the desired levels. Similarly, all parameters of soil fertility like organic matter, available phosphorus and potassium contents were built up with the application of compost and gypsum.

Breakthrough Curves and Miscible Displacement of Cadmium Through Double-Layered Reclaimed Soils Amended with Macroporous Granule

  • Kim, Hye-Jin;Ryu, Jin-Hee;Kim, Si-Ju;Park, Mi-Suk;Chung, Doug-Young
    • 한국토양비료학회지
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    • 제44권1호
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    • pp.15-21
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    • 2011
  • Transport of heavy metals such as Cd is affected by several rate-limiting processes including adsorption and desorption by exchange reactions in soils. In this study, column transport and batch kinetic experiments were performed to assess Cd mobility in a double-layered soil with a reclaimed saline and sodic soil (SSS) as top soil and macroporous granule (MPG) as a bottom layer. For individual soil layer having different physical and chemical properties, Cd was considered to be nonlinear reactivity with the soil matrix in layered soils. The dispersive equation for reactive solutes was solved with three types of boundary conditions for the interface between soil layers. The adsorption of Cd with respect to the saline-sodic sandy loam and the MPG indicated that the nature of the sites or the mechanisms involved in the sorption process of Cd was different and the amounts of Cd for both of samples increases with increasing amounts of equilibrium concentration whereas the amount of Cd adsorbed in saline-sodic sandy loam soil was higher than that in MPG. The results of breakthrough curve indicating relative Cd retardation accompanied by layer material and sequence during leaching showed that the number of pore volumes to reach the maximum relative concentration of 1 increased in the order of MPG, SSS, and double layer of SSS-MPG. Breakthrough curves (BTCs) from column experiments were well predicted with our double-layered model where independently derived solute physical and retention parameters were implemented.

Hydraulic Property and Solute Breakthrough from Salt Accumulated Soils under Various Head Pressures

  • Lee, Sanghun;Chung, Doug-Young;Hwang, Seon-Woong;Lee, Kyeong-Bo;Yang, Chang-Hyu;Kim, Hong-Kyu
    • 한국토양비료학회지
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    • 제45권5호
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    • pp.717-724
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    • 2012
  • Salt accumulated soil should be reclaimed to lower salt level for crop production. This study was carried out to investigate the characteristics of water flow and transport of mono and divalent solutes on salt accumulated soils with different head pressures. Saturated hydraulic conductivity was measured by constant and falling head methods with maintaining different head pressures. Saturated hydraulic conductivity was influenced by bulk density and organic matter contents in soils, but it had different elusion patterns between saline and sodic soil. While the quantity of water necessary for reclamation could be varies with soil type, it was considered that the supply of one pore volume of water was affordable and economic. Additional head pressure significantly increased the volume of leachate at a given time and it was more effective at low organic matter soils. The results indicate that additional head pressure would be one of the best irrigation practices on desalination method for salt accumulated soils.

Efficiency of Various Nutritional Sources to Improve Physical Properties of Saline-Sodic Soil

  • Noor-Us-Sabah, Noor-Us-Sabah;Sarwar, Ghulam;Ibrahim, Muhammad;Tahir, Mukkram Ali;Iftikhar, Yasir;Haider, Muhammad Sajjad;Han, Kyung-Hwa;Ha, Sang-Keun;Zhang, Yong-Seon
    • 한국토양비료학회지
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    • 제45권1호
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    • pp.93-97
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    • 2012
  • This study was conducted to evaluate the efficiency of various inorganic and organic materials to improve physical properties of soil. Saline sodic soil (saturation percentage = 40.36%, $EC_e=5.15dS\;m^{-1}$, $pH_s=8.70$, $SAR=18.84(m\;mol\;L^{-1})^{1/2}$, bulk density =$1.49Mg\;m^{-3}$) was collected, brought to wire house and filled in pots after laboratory analysis for various parameters. Different sources of organic nutrients like farm manure (FM), press mud, compost, poultry manure and sesbania green manure were analyzed for their chemical composition. The experiment comprised of 12 treatments replicated thrice; $T_1$: control (recommended NPK), $T_2:{\frac{1}{2}}$ recommended NPK, $T_3$: FM at 1.5% by soil weight, $T_4$: pressmud at 1.5% by soil weight, $T_5$: compost at 1.5% by soil weight, $T_6$: poultry manure at 1.5% by soil weight, $T_7$: sesbania green manure at 1.5% by soil weight, $T_8:T_2$ + FM at 0.75% by soil weight, $T_9:T_2$ + pressmud at 0.75% by soil weight, $T_{10}:T_2$ + compost at 0.75% by soil weight, $T_{11}:T_2$ + poultry manure at 0.75% by soil weight, $T_{12}:T_2$ + sesbania green manure at 0.75% by soil weight. These treatments were applied using completely randomized (CR) design and appropriate time was given to decompose these organic nutritional sources. Seeds of wheat cultivar Sahar-2006 were sown. After harvesting the wheat, soil samples were collected from each pot and analyzed for various physical properties like bulk density, porosity and saturation percentage. An improvement in physical properties (bulk density, porosity and saturation percentage) of soil was noticed with the application of various organic nutritional sources but role of compost alone ($T_5$) remained prominent.

Characterization of Kinetics of Urea Hydrolysis in A Newly Reclaimed Tidal Soils

  • Kim, Hye-Jin;Park, Mi-Suk;Woo, Hyun-Nyung;Kim, Gi-Rim;Chung, Doug-Young
    • 한국토양비료학회지
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    • 제44권1호
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    • pp.84-90
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    • 2011
  • It is imperative to study the hydrolysis of urea in high saline-sodic condition of a newly reclaimed tidal land in order to overcome the problems associated with use of urea fertilizer. The methodology adopted in this study tried to get a convenient way of estimating rate for N transformation needed in N fate and transport studies by reviewing pH and salt contents which can affect the microbial activity which is closely related to the rate of urea hydrolysis. The hydrolysis of urea over time follows first-order kinetics and soil urease activity in reclaimed soils will be represented by Michaelis-Menten-type kinetics. However, high pH and less microorganisms may delay the hydrolysis of urea due to decrease in urease activity with increasing pH. Therefore, the rate of urea hydrolysis should adopt $V_{max}$ referring enzyme activity ($E_0$) accounting for urease concentration which is indicative for urea hydrolysis, especially in a high saline and sodic soils.

간척지 토양특성과 토양염류도 변화 개관 (Soil Characteristics and Soil Salinity Changes in the Reclaimed Tideland of Korea)

  • 이승헌
    • 한국토양비료학회지
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    • 제42권Spc호
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    • pp.14-19
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    • 2009
  • 간척지 토양에 대한 기본 자료를 얻기 위하여 9개소의 간척지 과제지역에서 약 90여개의 토양시료를 채취하였다. 조사 결과 토양은 점토(2-35%), 미사(2.0-80%), 모래(8-95%) 정도로 구성되있고 토성은 주로 사질양토 또는 미시질양토로 조사되었다. 토양 pH는 5.5-9.1, 유기물함량은 $0.5-19.2g\;kg^{-1}$, 총 질소함량은 $4-1159mg\;kg^{-1}$ 그리고 유효태 인산함량은 $3.5-147.7mg\;kg^{-1}$, 전기전도도는 $0.6-31.6dS\;m^{-1}$ 그리고 Na와 Mg 함량은 가리나 칼슘함량보다 높았다. ECesms 표층과 심층 모두 높은 것으로 조사되었다.

중국 길림성 백성지역 흑개토의 이화학성 및 인산 흡착 특성 (Physical-chemical Properties and Phosphorus Adsorption Characteristics of Soils in Baicheng, China)

  • 김성애;이상모;최우정;류순호
    • Applied Biological Chemistry
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    • 제44권2호
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    • pp.92-96
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    • 2001
  • 농경지로의 개발 가능성이 높은 중국 길림성 백성지역의 주요한 토양인 흑개토의 이화학성 및 인산 흡착특성을 조사하였다. 토지 이용방식 또는 재배작물이 서로 다른 중국 길림성 백성지역 4곳과 중국 용정에 위치한 연변 대학교 농과대학 부속 시험장 1곳에서 1993년 8월에 토양을 채취하여 실험을 수행하였다, 중국 길림성 백성지역 토양의 $_PH$는 미경작지 10.2, 경작지는 $7.3{\sim}7.6$으로 비교적 높았다. 양이온 치환용량은 20 cmol(+) $kg^{-1}$ 이상이었으며, 치환성 양이온 중 Na는 특히 표토에 많이 존재하였으며, Ca의 함량이 매우 높아 Ca 포화율이 100% 이상을 나타내었다. 토양 포화 침출액의 주요 양이온은 Na이었으며, ECe와 SAR을 기준으로 백성 미경작지 토양은 염류-나트륨성 토양, 경작지 토양은 나트륨성 또는 일반 토양에 해당하였다. 백성지역 토양의 유효인산 함량은 10mg P $kg^{-1}$ 미만으로 아주 낮았으며, 최대 인산흡착량은 $ $ mg P $kg^{-1}$이었다. 길림성 백성지역 토양의 경우 유효인산 함량이 매우 낮아 토양 비옥도 중진을 위한 인산질 비료의 시용과 함께 토양 투수성의 개선 등과 같은 적절한 토양 관리가 필요하며, 용정지역 토양의 경우에는 인산흡착 특성을 고려하여 인의 과잉 축적을 방지하기 위한 인산질 비료의 적정 시용을 권장하여야 한다.

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Crop Residues Management for Rice-Wheat Cropping System in Saline-Sodic Soil

  • Ahmed, Khalil;Qadir, Ghulam;Jami, Abdul-Rehman;Rafa, Hafeezullah;Mehmood, Muhammad Aamer;Han, Kyung-Hwa;Ibrahim, Muhammad
    • 한국토양비료학회지
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    • 제47권4호
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    • pp.269-274
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    • 2014
  • Series of field experiments were conducted to evaluate the long term effect of gypsum and crop residue on crop yield and soil health in rice-wheat crop rotation system in salt affected soil. A saline-sodic field having $EC_e$ (electrical conductivity of the saturation extract) 4.77 ($dSm^{-1}$); pH ($H_2O$) 8.96; SAR 43.78 ($mmol\;L^{-1}$) and gypsum requirement (G.R.) 2.86 (Mg $acre^{-1}$) was selected on Soil Salinity Research Institute Farm. Five treatments consisting of ($T_1$) control, ($T_2$) gypsum at 100% G.R., ($T_3$) gypsum at 25% G.R. + wheat straw at $3Mg\;ha^{-1}$, ($T_4$) gypsum at 25% G.R. + rice straw at $3Mg\;ha^{-1}$, ($T_5$) gypsum at 25% G.R.+ rice and wheat straw at $3Mg\;ha^{-1}$ were replicated four times under completely randomized block design. The data indicated that grain and straw yield of rice and wheat was significantly (P<0.05) increased by all the amendments used either single or in combination. $T_2$ (gypsum at 100% G.R.) significantly (P<0.05) increased grain and straw yield of rice and wheat crops followed by $T_3$ (gypsum at 25% G.R. + wheat straw at $3Mg\;ha^{-1}$) when compared with control. Soil properties were also improved by used amendments, pronounced decreased in $EC_e$, $pH_s$ and SAR were recorded in $T_2$ followed by $T_3$. The efficiency of the treatments could be arranged in following order gypsum at 100% G.R.> gypsum at 25% G.R. + wheat straw at $3Mg\;ha^{-1}$ > gypsum at 25% G.R. + rice and wheat straw at $3Mg\;ha^{-1}$ > gypsum at 25% G.R. + rice straw at $3Mg\;ha^{-1}$ > control.

Halotolerant Plant Growth Promoting Bacteria Mediated Salinity Stress Amelioration in Plants

  • Shin, Wansik;Siddikee, Md. Ashaduzzaman;Joe, Manoharan Melvin;Benson, Abitha;Kim, Kiyoon;Selvakumar, Gopal;Kang, Yeongyeong;Jeon, Seonyoung;Samaddar, Sandipan;Chatterjee, Poulami;Walitang, Denver;Chanratana, Mak;Sa, Tongmin
    • 한국토양비료학회지
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    • 제49권4호
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    • pp.355-367
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    • 2016
  • Soil salinization refers to the buildup of salts in soil to a level toxic to plants. The major factors that contribute to soil salinity are the quality, the amount and the type of irrigation water used. The presented review discusses the different sources and causes of soil salinity. The effect of soil salinity on biological processes of plants is also discussed in detail. This is followed by a debate on the influence of salt on the nutrient uptake and growth of plants. Salinity decreases the soil osmotic potential and hinders water uptake by the plants. Soil salinity affects the plants K uptake, which plays a critical role in plant metabolism due to the high concentration of soluble sodium ($Na^+$) ions. Visual symptoms that appear in the plants as a result of salinity include stunted plant growth, marginal leaf necrosis and fruit distortions. Different strategies to ameliorate salt stress globally include breeding of salt tolerant cultivars, irrigation to leach excessive salt to improve soil physical and chemical properties. As part of an ecofriendly means to alleviate salt stress and an increasing considerable attention on this area, the review then focuses on the different plant growth promoting bacteria (PGPB) mediated mechanisms with a special emphasis on ACC deaminase producing bacteria. The various strategies adopted by PGPB to alleviate various stresses in plants include the production of different osmolytes, stress related phytohormones and production of molecules related to stress signaling such as bacterial 1-aminocyclopropane-1-carboxylate (ACC) derivatives. The use of PGPB with ACC deaminase producing trait could be effective in promoting plant growth in agricultural areas affected by different stresses including salt stress. Finally, the review ends with a discussion on the various PGPB activities and the potentiality of facultative halophilic/halotolerant PGPB in alleviating salt stress.

간척지 염해답토양의 토성별 제염기간 및 단면특성변화를 기준한 분류학적 고려 (A Taxonomical Consideration based on Changes of Salinity and Profile Features of the Texturally Different Two Reclaimed Tidal Soils)

  • 손연규;현근수;서명철;정강호;현병근;정석재;송관철
    • 한국토양비료학회지
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    • 제39권2호
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    • pp.59-64
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    • 2006
  • 중부 서해안에 분포하는 염해답으로 분류되어 있는 토양에서 간척 후 경작년대의 진척에 따른 토양 특성변화를 구명하고, Soil Taxonomy 분류에 따른 문제점을 검토하며, 염해답에서의 제염 소요년수를 추정한 결과는 다음과 같았다. 1. 간척년대가 오래될수록 토색이 밝아지고, 층위가 발달되며, 토양구조의 형성이 진전되는 경향이며, EC는 감소되는 경향이었다. 2. 식양질인 포승통의 경우 분류기준에 따라 분석한 결과를 Salic 층위를 가지고 있는 것으로 판단되었으며, 광활통 등 사양질 토양의 경우에는 아군단위에서의 sodic 특성을 가지고 있는 것으로 판단되었다. 3. Soil Taxonomy 분류기준을 적영하여 분석하였을때에는 식양질 토양에서는 간척년대가 지속되어도 Na 함량이 기준 이하로 떨어지지 않았으며, 사양질 토양에서는 재배를 시작한지 76된 김제시 광활면 지역에 분포하는 토양에서만 Na 함량이 기준 이하로 떨어져 사질답이라 할 수 있었다. 4. 이용 측면에서 염농도의 피해 기준을 dSmX로 판단할 때 식양질토양은 제염이 되는데 약 108년정도가 소요되었으며 사양질 토양에서는 12년 정도가 소요되었다.