• 제목/요약/키워드: Soil order

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Australian Soil Classification: an Review

  • Hyun, Byung-Keun;Sonn, Yeon-Kyu;Cho, Hyun-Jun;Jung, Kangho;Choi, Jung-won;Jung, Sug-Jae;Kwak, Woo-Ri;Kim, Woon-Sun;Hong, Se-Eun
    • 한국토양비료학회지
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    • 제49권1호
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    • pp.93-114
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    • 2016
  • As a means of improving Korean Soil Classification System, we have reviewed Australian Soil Classification System by comparing Soil Taxonomy and FAO/WRB Classification System. Australian Soil Classification System is composed of 14 of Order, 87 of Sub-order, 556 of Great-group, 2,451 of Sub-group, and 7,276 of Family. Interestingly, soil order has the Anthroposols which is not classified with Soil Taxonomy, and the classification for some of soils is based on soil texture abruption horizon and soil structure. Seven of 14 soil orders are classified with an old version based on soil color rather than morphological characteristics. The distribution scale of Australian soil order is the largest in Tenosols, and followed by Kandosols, Rudosols, Sodosols and Vertisols in Australia.

자연토양 및 카올린에 대한 코발트, 스트론튬, 세슘의 흡착 특성 (Adsorption Characteristics of Cobalt, Strontium, and Cesium on Natural Soil and Kaolin)

  • 천경호;최정학;신원식;최상준
    • 한국환경과학회지
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    • 제23권9호
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    • pp.1609-1618
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    • 2014
  • In this study, as a fundamental study for the remediation of the radionuclides-contaminated soil, the adsorption of cobalt, strontium, and cesium on natural soil and kaolin were experimently investigated and adsorption characteristics were evaluated by using several adsorption kinetic and isotherm models. The pseudo-first-order kinetic model (PFOM), pseudo-second-order kinetic model (PSOM), one-site mass transfer model (OSMTM), and two compartment first-order kinetic model (TCFOKM) were used to evaluate the kinetic data and the pseudo-second-order kinetic model was the best with good correlation. The adsorption equilibria of cobalt, strontium, and cesium on natural soil were fitted successfully by Redlich-Peterson and Sips models. For kaolin, the adsorption equilibria of cobalt, strontium, and cesium were fitted well by Redlich-Peterson, Freundlich, and Sips models, respectively. The amount of adsorbed radionuclides on natural soil and kaolin was in the order of cesium > strontium > cobalt. It is considered that these results could be useful to predicting the adsorption behaviors of radionuclides such as cobalt, strontium, and cesium in soil environments.

오염된 토양층내의 중금속 이동 특성 (Transport Characteristic of Heavy Metals in Contaminated Soil)

  • 조재범;현재혁;정진홍;김원석
    • 한국지하수토양환경학회:학술대회논문집
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    • 한국지하수토양환경학회 1998년도 공동 심포지엄 및 추계학술발표회
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    • pp.236-239
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    • 1998
  • This research was performed to check the transport characteristics of heavy metals in contaminated soil, that is, the influence of humic acid and phosphate on transport characteristics of heavy metals was studied. From the results of column mode experiments about heavy metal behavior, the order time to reach breakthrough and equilibrium was soil + humic acid( 20g ) > soil + humic acid ( 5 g ) > soil without Humic acid addition > soil+humic acid( 50g ). It is because the dissolved organic carbon content increased as the soil organic matter content increased. As the phosphate increased, so did the time to reach breakthrough and equilibrium. The order of time was soil + phosphate( 50 mg ) > soil + phosphate( 20 mg ) > soil . phosphate( 10 mg ) > soil without phosphate addition. It is because the phosphate ion worked as alkalinity donor and the calcium ion co-injected worked as the accelerator of coprecipitation of heavy metals.

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프로테아제를 응용한 단백질과 지질 혼합오구의 제거 (The Removal of Mixed Soil of Protein and Fat by Protease)

  • 성혜영;이정숙
    • 한국염색가공학회지
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    • 제13권2호
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    • pp.18-18
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    • 2001
  • This study has examined the removal of mixed soil of protein and fat by protease. Cotton and PET fabrics were soiled by spotting of hemoglobin and triolein, respectively. The soiling order and soil concentration were changed in this procedure. The soiled fabrics were aged at 130℃ for 20 minutes. Protease was added in the alcohol ethoxylate(AE) detergent solution. The removal effciency was evaluated by analysis of protein and/or fat on the fabrics before and after washing, respectively. The detergency of PET fabrics was higher than that of cotton fabrics. The removal efficiency of hemoglobin was improved by protease from cotton and PET fabrics. Especially the removal efficiency of hemoglobin was remarkably improved from cotton fabrics. With the increase of hemoglobin and triolein (1:1) mixed soil, the removal of mixed soil was increased in proportion to mixed soil content up to a certain point. but it began to decrease above the point from cotton fabrics, while it was generally increased from PET fabrics. The detergency of total mixed soil from cotton fabrics was higher in case of soiling order with triolein after hemoglobin than in case of soiling order with triolein before hemoglobin. But the soiling order was not greatly effected in the detergency of total mixed soil from PET fabrics.

프로테아제를 응용한 단백질과 지질 혼합오구의 제거 (The Removal of Mixed Soil of Protein and Fat by Protease)

  • 성혜영;이정숙
    • 한국염색가공학회지
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    • 제13권2호
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    • pp.104-113
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    • 2001
  • This study has examined the removal of mixed soil of protein and fat by protease. Cotton and PET fabrics were soiled by spotting of hemoglobin and triolein, respectively. The soiling order and soil concentration were changed in this procedure. The soiled fabrics were aged at $130^\circ{C}$ for 20 minutes. Protease was added in the alcohol ethoxylate(AE) detergent solution. The removal effciency was evaluated by analysis of protein and/or fat on the fabrics before and after washing, respectively. The detergency of PET fabrics was higher than that of cotton fabrics. The removal efficiency of hemoglobin was improved by protease from cotton and PET fabrics. Especially the removal efficiency of hemoglobin was remarkably improved from cotton fabrics. With the increase of hemoglobin and triolein (1:1) mixed soil, the removal of mixed soil was increased in proportion to mixed soil content up to a certain point. but it began to decrease above the point from cotton fabrics, while it was generally increased from PET fabrics. The detergency of total mixed soil from cotton fabrics was higher in case of soiling order with triolein after hemoglobin than in case of soiling order with triolein before hemoglobin. But the soiling order was not greatly effected in the detergency of total mixed soil from PET fabrics.

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염류집적 농경지 제염기술에 대한 경제성분석 - 작물생산량을 기준으로 (Economic Analysis on Desalination Technology for Saline Agricultural Land on the Basis of Crop Production)

  • 김도형;최정희;김이열;남창모;백기태
    • 한국지하수토양환경학회지:지하수토양환경
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    • 제17권5호
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    • pp.40-48
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    • 2012
  • In this study, economic analysis of five desalination technologies for saline agricultural land was carried out. The analysis was comprehensively evaluated by calculating changes in crop production and benefit/cost (B/C) ratio. The analysis of crop production was in the order of tomato > cucumber > a (musk) melon > watermelon > cabbage, and economical efficiency for desalination technology was in the order of soil exchange > soil addition > electrokinetics > under-drainage > subsoil reversal. In cost benefit analysis, B/C ratio was in the order of under-drainage > soil exchange > electrokinetics > soil addition > subsoil reversal, and all desalination technologies used in this study have the ratio higher than 1, which means economical efficiency was high. Based on the net production considering B/C ratio, the general economic analysis was exactly order from that of crop production analysis. As a result, economical efficiency of soil exchange was highest, and economical efficiency of soil addition and electrokinetic was relatively higher than others.

Washita '92 토양수분 자료의 1차원 및 2차원 통계특성 (First-and Second-Order Statistics of Washita'92 Soil Moisture Data)

  • 유철상
    • 한국수자원학회논문집
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    • 제31권2호
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    • pp.145-153
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    • 1998
  • 이 논문에서는 Washita '92 자료를 이용하여 토양수분의 1차원 및 2차원 통계특성을 추출하였다. 아울러, 토양수분과 토양, 밝기온도(brightness temperature), 식생지수 사이의 상관관계가 어떤지를 선형회귀분석에 근거하여 조사해 보았으며 결과로서 토양수분은 밝기온도와 유의할만한 상관성이 있는 것으로 나타났다. 토양수분의 시간에 대한 감쇠(decay)계수를 각각의 토양군별로 추정하였고, 역으로 이 값을 이용하여 관측전 마지막 강우의 시점을 추정해 본 결과 관측기록과 유사한 20일 정도로 나타났다. 토양수분의 2차원 통계특성 분석은 2차원 상관도와 스페트럼을 도출하고 분석함으로서 수행하였으며 토양과 식생지수에 대한 2차원 분석결과와 비교하였다. 이러한 분석 결과로 토양수분은 공간적으로 매우 높은 상관성을 갖는 토양과 상대적으로 낮은 사오간성을 보이는 식생의 중간적인 2차원 통계특성을 나타냄을 알 수 있었다. 즉, 지형이 완만하여 지형적인 영향이 상대적으로 적다고 알려진 Washita 지역의 경우 공간적으로 높은 상관성을 보이는 토양의 공극에 존재하는 토양수분은 상대적으로 낮은 상관성을 보이는 식생에 의해 교란되고 있음을 파악할 수 있었다. 선형저수지의 개념과 공간적인 확산을 고려한 동역학적 토양수분 모형의 유도과정을 보였고 모형의 매개변수가 토양수분의 1차원 및 2차원 통계특성으로부터 효과적으로 추정될 수 있음을 보였다.

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도시 유역 내에서 토지이용에 따른 표토의 특성 비교 및 표토 보전을 위한 시사점 (Comparative Analyses for the Properties of Surface Soils from Various Land Uses in an Urban Watershed and Implication for Soil Conservation)

  • 박은진;강규이
    • 한국환경복원기술학회지
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    • 제12권3호
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    • pp.106-115
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    • 2009
  • Knowledge about how to stabilize soil structure is essential to conserve soil systems and maintain various biogeochemical processes through soil. In urban area, soil structural systems are degraded with inappropriate management and land use and become vulnerable to erosion. We analyzed the structural changes of surface soils with different land uses, i.e., forests, parks, roadside green area, riparian area, and farmlands (soybean fields), in the Anyang Stream Watershed in order to find the factors influencing the stability of soil structure and the implication for better management of surface soil. Soil organic matter contents of other land use soils were only 18~52% of that in forest soils. Soil organic matter increased the stability of soil aggregates in the order of soybean fields < roadsides < riparian < parks < forests and also reduced soil bulk density (increased porosity). The lowest stability of soybean field soils was attributed to the often disturbance like tillage and it was considered that higher stability of park soils comparing to other land use soils except forests was owing to the covering of soil surface with grass. These results suggest that supply of soil organic matter and protection of soil surface with covering materials are very important to increase porosity and stability of soil structure.

인공산성비 처리가 토양의 무기양분 이동에 미치는 영향 (Effects of Simulated Acid Rain on Mineral Nutrient Movement in Soil)

  • 유관식
    • 한국환경농학회지
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    • 제17권4호
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    • pp.362-367
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    • 1998
  • 사양토, 양토, 식양토의 3가지의 토양을 2' column에 충진한 후 인공 산성비( pH 2.0, 4.0, 6.0) 1200㎜를 처리하여 산성비의 토양내 침투수량에 따른 토양 중 무기양분의 이동 양상과 토양내에서의 환경변화에 대한 시험 결과, 산성비의 토양침투에 따른 토양의 pH 변화는 산성비의 pH가 4.0가 6.0에서는 별 차이가 없었으나 pH2.0에서는 토심별로 큰 차이를 보였으며, pH감소는 사양토> 양토> 식양토 순위였다. 산성비의 토양침투에 따른 토양의 토심별 치환성과 수용성 염기의 용탈양은 Ca> Mg> K 순위였으며, 산성비의 pH2.0에서 가장 많은 양이 이동하였다. 이들 염기들의 평균이동거리를 pH2.0의 산성비 처리에서는 사양토, 양토, 식양토 공히 Mg> Ca> K의 순위였으나, 산성비의 pH4.0인 경우 사양토와 식양토는 Mg> K> Ca, 양토의 경우는 K> Mg> Ca의 순위였다. 인산의 경우 평균 이동거리는 다른 성분에 비하여 매우 짧았으며 산성비의 산도가 증가할수록 증가하였고, 일반 강우 조건에서는 거의 이동하지 않았다.

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The Study on Soil Classification in Sri Lanka

  • Hyun, Byung-Keun;Mapa, R.B.;Sonn, Yeon-Kyu;Cho, Hyun-Jun;Shin, Kooksik;Choi, Jung-won;Jung, Seog-Jae;Jang, Byung-Chun
    • 한국토양비료학회지
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    • 제48권3호
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    • pp.153-162
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    • 2015
  • Land information is important for the international agricultural companies. This study investigated the agriculture and soil information in Sri Lanka. This study is the results from investigation of soil properties and agricultural properties determined by the Soil Taxonomy classification system for the soils in Sri Lanka. The order of the main agricultural imports in Sri Lanka was wheat > refined Sugar > dry Onion > Rice > Lentils. The climate of Sri Lanka is divided into three climatic zones. There are a wet zone, an intermediate zone, and a dry zone. Rainfall of the wet zone was $3,000-5,000mm\;year^{-1}$. The rainfall of the dry zone was less than $1,000m^{-1}$. The intermediate zone was in the middle area. Soil series of Sri Lanka were 109 in total. Detailed information of soil series was: 6 of soil Orders, 15 of Suborders, 39 of Great groups, and 56 of Subgroups. Soil texture of topsoil was much more coarse, but subsoil was gravelly coarse soil. Soil of Sri Lanka was classified as a Soil Order. The orders were Entisols > Alfisols > Ultisols > Inceptisols > Histosols > Vertisols.