• Title/Summary/Keyword: 토양 유기물함량

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Studies on the Denitrification in the Submerged Paddy Soil -II. The Denitrification Rates Upon Kinds of Applied Organic Matter and Levels of Nitrogen Fertilizer (논토양(土壤)의 탈질작용(脫窒作用)에 관(關)한 연구(硏究) -제(第)II보(報). 유기물(有機物)의 종류(種類) 및 질소시비량차이(窒素施肥量差異)가 탈질(脫窒)에 미치는 영향(影響))

  • Lee, Sang-Kyu;Kim, Seung-Hwan;Park, Jun-Kyu;An, Sang-Bae
    • Korean Journal of Soil Science and Fertilizer
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    • v.19 no.1
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    • pp.76-82
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    • 1986
  • A laboratory experiment was conducted to find out the denitrification rate upon the levels of nitrogen and source of organic matter in submerged sandy and sandy loam soil. The results obtained were sumarized as follows; 1. Evolution of nitrous oxide was increased at 1st and 10 days after incubation. And dinitrogen was increased at 1st and 30 days after incubation. Applications of green manure was enhanced the evolution of nitrous oxide ($N_2O$) and dinitrogen ($N_2$). 2. The cumulative denitrification rates at 50 days was high in Gyuam sandy loam soil (O-M: 1.52%) than that of Hamchang sandy soil (O-M: 3.81%). On the other hand, the cumulative emission of dinitrogen was high in Gyuam sandy loam soil while nitrous oxide was high in Hamchang sandy soil. The total mount of denitrification rate was high in order of green manure > rice straw > compost > control soil. 3. Increases of fertilizer nitrogen was enhanced the rate of emission of dinitrogen and nitrous oxide during the incubation time. 4. According to Michaelis-Menten kinetic equation, denitrification rates and reaction efficiency were remarkably increased by application of readily decomposable organic matter with in higher organic matter content of soil. 5. The negative relationship was observed between the evolution of dinitrogen and carbon ($CO_2+CH_4$) while the nitrous oxide with carbon was positive. 6. Under the this experiment conditions 1 mg of carbon was required for production of 4 mg N as $N_2O$ and 3 mg of N as $N_2$, respectively.

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Adsorption Characteristics of Organophosphorus and Carbamate Pesticides in Four Soils and the Evaluation for Their Leaching Potential Using Two Screening Models (유기인계 및 카바메이트계 농약의 토양흡착성과 간이선발모형을 이용한 용탈 잠재성 평가)

  • Kim, Chan-Sub;Park, Byung-Jun;Ihm, Yang-Bin;Ryu, Gab-Hee
    • Korean Journal of Environmental Agriculture
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    • v.24 no.4
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    • pp.341-349
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    • 2005
  • Soil adsorption study was carried out to define the mobility of pesticides and to evaluate leaching potential in soils. Nine pesticides including metolcarb, molinate, fenobucarb, isazofos, diazinon, fenitrothion, dimepiperate, parathion and chlorpyrifos-methyl were subjected to adsorption experiment for four types of soils, such as upland, paddy, forest and volcanic ash soil. Based on Koc values, metolcarb and molinate were classified as mobile, fenobucarb as mobile or moderately mobile isazofos as moderately mobile, diazinon, fenitrothin, dimepiperate, and parathion as slightly or moderately mobile and chlorpyrifos-methyl as slightly mobile. Two evaluation methods, Groundwater Ubiquity Score (GUS) index and standard indices of soil-chemical adsorption and biodegradation (half-life), were used for the estimation of pesticide leaching potential. Leachabilities of metolcarb, molinate and fenobucarb were evaluated as high, and isazofos, dimepiperate and diazinon as a little potential, while fenitrothion, parthion and chlorpyrifos-methyl showed very low leaching potential. The leaching potential of pesticides was determined on the basis of intrinsic properties of the pesticides and the soil properties. Among the soil properties, organic matter gave a great influence on the leachability in soil. Therefore, leachabilities of the pesticides used were expected less in Sineom soil with relatively higher organic matter than Gangseo, Jungdong and Yesan soil with lower organic matter.

Effect of Different Cropping System and Soil Management on Soil Chemical and Microbiological Quality Assessment in the Daekwanryung Upland Soil (대관령(大關嶺) 지역에서 작부체계 및 토양관리 방법의 차이가 토양화확성 및 미생물상에 미치는 영향)

  • Yun, Sei-Young;Kim, Jeong-Je;Yang, Jae-Wei;Jung, Yeong-Sang;Choi, Joong-Dae
    • Korean Journal of Soil Science and Fertilizer
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    • v.32 no.3
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    • pp.312-318
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    • 1999
  • These experiments were conducted to determine the effects of soils treated with different soil management, methods, fertilizers and crops on soil microflora and its number for constructing the environmentally sound agriculture modeling of the upland soils. These experiments show that physico-chemical soil characteristics was different in upland soils treated with different soil managements and fertilizers applied. Also soil microflora and its number were effected from crops cultivated with different soil managements in these experiments. The number of Erwinia sp. in chinese cabbage cultivated field on Daekwanryung especially was apparently increased in soil cultivated with potato relative to corn. It was appeared that the number of Fusarium sp. in soil was more effected from kind of fertilizer applied than crops cultivated.

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Analysis and Improvement of Soil Physical and Chemical Properties for Transplantation of Damaged Trees (훼손 수목의 이식을 위한 토양의 물리·화학적 특성 분석과 개선 방안)

  • Hyesu, Kim;Jungho, Kim;Yoonjung, Moon;Seonmi, Lee
    • Journal of Environmental Impact Assessment
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    • v.31 no.6
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    • pp.423-437
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    • 2022
  • Parts of damaged trees are being transplanted in accordance with the Environmental Impact Assessment Manual. Problems such as death or poor growth are constantly being addressed in the process of transplanting trees from the forest they originally inhabited to temporary and final transplant sites. The purpose of this study is to analyze the differences in soil properties in the surrounding forest, the temporary transplant site, and the construction site and to suggest methods for improving the soil to make it suitable for the growth of transplanted trees. For 10 development projects, 2 soil samples were sampled from the surrounding forest, temporary transplant site, and construction site. A total of 60 soil samples were analyzed for physical and chemical properties. Among the physical properties such as coefficient of permeability, available moisture, and hardness, and chemical properties such as acidity, organic matter content, total nitrogen, and available P showed significant differences among groups. The soil of the construction site is harder than the surrounding forest because of construction equipments, the coefficient of permeability is higherthan the surrounding forest because of high sand content, and the available moisture was low. It does not retain the moisture necessary for plants in the soil and drains immediately. It is necessary to implement tillage to improve the physical properties and structure of the soil. In addition, it is necessary to cover the surface with wood chips or fallen leaves after adding mature organic matter to improve the physical and chemical properties of the soil together.

Determination of Soil Nitrogen Supplying Capacity Using Pepsin Digestibility (Pepsin 분해방법을 이용한 토양의 질소 공급력 결정)

  • Kim, Yoo-Hak;Kim, Sun-Kwan;Zhang, Yong-Sun
    • Korean Journal of Soil Science and Fertilizer
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    • v.38 no.5
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    • pp.253-258
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    • 2005
  • It is necessary to determine a nitrogen supplying capacity (NSC) of soil for sustainable agriculture. NSC has been decided by directly detecting N mineralization potential (NMP) and inorganic nitrogen or by indirectly approximating from organic matter and chemical properties of soil. NMP is best method for NSC but it takes long period. A study was conducted to find a short-term incubation method using pepsin through 1) determining NMP of 3 upland and 3 paddy soils, 2) establishing analytical condition of pepsin digestion by comparing to NMP, 3) validating with relations to N requirements for maximum yield of rice. NMPs of 6 soils were ranges from $63mg\;N\;kg^{-1}$ to $156mg\;N\;kg^{-1}$. The pepsin digestion method of soil nitrogen was established by determining amino nitrogen from digesting 5 g of soil for 30 minutes by 0.02% pepsin. This method was so highly correlated with a maximum rate of nitrogen fertilizer that it could be used for determining NSC in paddy soil.

The Effect of Long-term Organic Matter Addition on the Physicochemical Properties of Paddy Soil (답토양(沓土壤)에서 퇴비연용(堆肥連用)이 토양(土壤)의 이화학적성질(理化學的性質)에 미치는 영향(影響))

  • Shin, Jae Sung;Shin, Yong Hwa
    • Korean Journal of Soil Science and Fertilizer
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    • v.8 no.1
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    • pp.19-23
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    • 1975
  • In order to find out the effect of long-term annual additions of organic matter on the physico-chemical properties of paddy soil, the soil with and without compost application has been analysed. 1. There was no significant difference in the particle size distribution between compost and uncompost treatment, however, hydraulic conductivity, sedimention volume were remarkedly increased in compost. 2. Bulk density and soil strength were decreased in organic matter additions, but porosity increased. 3. Relative to Atterberg Limits, liquid limit, plastic limit, and elastic index were increased in compost. 4. Aggregate size distribution was slightly increased in additions of organic matter. 5. Regarding to chemical properties, pH, organic matter content, C.E.C. and extractable cation were increased in organic matter additions.

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Classification of Volcanic Ash Soils and contribution of Organic Matter and Clay to Cation Exchange Capacity (화산회토(火山灰土) 분류(分類) 및 CEC에 대(對)한 유기물(有機物)과 점토(粘土)의 기여도(寄與度))

  • Park, Chang-Seo;Kim, Lee-Yul;Cho, Seong-Jin
    • Korean Journal of Soil Science and Fertilizer
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    • v.18 no.2
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    • pp.161-168
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    • 1985
  • The 38 typical profiles representing volcanic ash soils (VAS) in Korea were subjected to multiple regression analysis to determine the relative contribution of organic matter (OM) and clay content to total cation-exchange capacity (CEC). This study, also, was examined the soil characteristics of VAS. VAS in Korea could be classified into 3 Orders, 5 Suborders, 8 Great groups, 15 Subgroups, 23 Families, and 38 Series. Total area of VAS was 139, 162ha and the most of them occured in Jeju Island. Simple correlation coefficients showed significance relations at OM-CEC and clay-CEC in top-soil of VAS. The partial regression coefficients indicated that CEC for each gram of OM as calculated to be 0.46 and 0.40 me per of topsoils for the black volcanic ash soils (BVAS) and the very dark brown volcanic ash soils (VDBVAS), respectively. The clay contributions of topsoils for BVAD and VDBVAS were 0.11 and 0.19 me. The standard partial regression coefficients appeared that OM content of topsoil for BVAS and VDBVAS was 2.97 and 1.23 times as important as clay content in predicting CEC.

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Growth Environment and Vegetation Structure of Native Habitats of Wikstroemia ganpi (Sieb. et Zucc.) Maxim (거문도닥나무(Wikstroemia ganpi (Sieb. et Zucc.) Maxim.) 자생지의 생육환경과 식생구조)

  • Yoon, Jung-Won;Yi, Myung-Hoon;Kim, Yong-Shik
    • Korean Journal of Environment and Ecology
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    • v.28 no.3
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    • pp.331-341
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    • 2014
  • The present study was to survey the site environment, vegetation structure and soil characteristics in the wild habitats of Wikstroemia ganpi in Goheung, Busan and Ulsan, and offers basic information for habitat conservation and restoration. Most of the wild habitats were located at altitudes between 28~242m with inclinations ranged as $0{\sim}40^{\circ}$. The canopy openness was 57.56%. The vegetation structure by the PC-ORD based on the Two Way Cluster Analysis were divided into three groups Community I(Castanea crenata-Pinus densiflora), Community II(Quercus dentata-Pinus thunbergii) and Community III (Pinus thunbergii). The species diversity was 1.3650, and evenness and dominance were found recorded as 0.8666 and 0.1333, respectively. The soil textures were silty loam and sandy loam. The average soil pH was 5.5, electric conductivity was 0.15dS/m, soil organic matter was 2.60% and available phosphorus was 4mg $kg^{-1}$. Correlation coefficients based on environmental factors, vegetation and soil analysis were showed that positive correlations between species diversity and evenness, organic matter and total nitrogen, whereas species slop degree and coverage of herb, diversity and dominance were showed negative correlations.

Effects of No-tillage Rice Cover Crop Cropping Systems on Rice Root Growth (무경운 피복작물 작부체계가 벼 뿌리 생육에 미치는 영향)

  • Son, Daniel;Lee, Young-Han
    • Korean Journal of Soil Science and Fertilizer
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    • v.44 no.3
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    • pp.375-379
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    • 2011
  • This study was conducted to evaluate the effect of rice cover crop cropping systems on rice root growth in a rice field as affected by conventional tillage without rice straw or green manure crop treatment (CTFS, check plot), no-tillage without cover crops (NTNT), no-tillage amended with rape (NTRA), no-tillage amended with rye (NTRY), no-tillage amended with hairyvetch (NTHV), and no-tillage amended with Chinese milk vetch (NTCM). In 0-5 cm soil depth, dry weight of root in NTRS ($128g\;m^{-2}$) was significantly higher than in the other plots (p<0.05) at harvesting stage. In addition, content of active organic matter at 0-5 cm soil depth was $1,684g\;m^{-2}$ in NTCM, $1,309g\;m^{-2}$ in NTRA, $1,295g\;m^{-2}$ in NTRS, $1,072g\;m^{-2}$ in NTRY, $917g\;m^{-2}$ in NTHV, $434g\;m^{-2}$ CTFS, and $426g\;m^{-2}$ in NTNT treatment. In no-tillage rice cover crop cropping system, our findings suggest that NTRS and NTCM should be enhanced root growth and active organic matter in paddy field.

Relative Contribution of Organic Matter and Clay Content to Cation Exchange Capacity in Sandy Soils (사질토(砂質土)에서 염기치환용량(鹽基置換容量)에 대한 유기물(有機物)과 점토(粘土)의 상대기여도(相對寄與度))

  • Park, Chang-Seo;Jung, Kwang-Young;Kim, Jai-Joung;Cho, Seong-Jin
    • Korean Journal of Soil Science and Fertilizer
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    • v.17 no.4
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    • pp.337-342
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    • 1984
  • 224 profiles representing 19 soil series were subjected to multiple regresion analysis to determine the relative contribution of organic matter(OM) and clay content to total cation exchange capacity(CEC) in sandy soil. The independent variables were OM and clay, with the dependent variable CEC. Simple correlation coefficients showed high significance at CEC-OM and CEC-clay. The partial regression coefficients indicated that CEC for each gram of OM was calculated to be 0.549 and 1.351 meq of top and subsoil. The clay contributions of top and subsoil were 0.247 and 0.226 meq, respectively. The standard partial regression coefficients appeared that clay content was 1.23 times as important as orgnic matter in predicting CEC.

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