• 한국토양비료학회지
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• 제48권5호
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• pp.535-541
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• 2015

Korean soil classification system is based on the US soil taxonomy. This study aimed to understand and inform the soil taxonomy of 2010 and 2014 US soil classification systems. Ingwan series belonged to anthropogenic soil was classified to coarse loamy over sandy, mixed, mesic family of Aquic Udorthents based on the soil taxonomy of 2010 and coarse loamy over sandy, mixed, mesic family of Anthroportic Udorthents based on the soil taxonomy of 2014. An anthropogenic soil is increasing in Korea. Considering the domestic relationship depending on US soil taxonomy, it is important to be well-informed of the taxonomy and apply the updated taxonomy system properly to the domestic soil classification. This study of defining the anthropogenic soil will provide useful information on soil management and its utilization.

• 한국토양비료학회지
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• 제46권6호
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• pp.536-541
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• 2013

In Soil Taxonomy system, anthropogenic soils are still classified as Entisols since the International Classification Committee for Anthropogenic Soils is in the process of classifying anthropogenic soils as new orders. In reality, it is difficult to characterize anthropogenic soils because Soil Taxonomy (ST) system does not distinguish between natural and anthropogenic Entisols. On the other hand, World Reference Base for soil resources (WRB) considers human impacts on soils and contains an independent category of anthropogenic soils, which makes easier to understand anthropogenic soil characteristics than Soil Taxonomy system. A remodeled paddy field (Gasan) was selected to classify by ST and WRB. Soil samples were taken to analyze chemical and physical properties. Based on the results of the analyses, the ST system classified Gasan as coarse loamy, mixed, mesic, Aquic Udorthents while the WRB did as Stagnic Urbic Technosols (Oxyaquic, Arenic). As a conclusion, the WRB classification information of the anthropogenic provides more detail characteristics of the anthropogenic soils.

• 한국토양비료학회지
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• 제43권1호
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• pp.113-118
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• 2010

각 나라마다 토양이 생성되는 환경이 다르고, 토양분류가 활용되는 목적이 다르기 때문에 세계적으로 다양한 토양분류체계가 발전되어 왔다. 1998년부터 국제적으로 통용되기 시작한 WRB 분류체계와 미국의 분류체계인 Soil Taxonomy는 그동안 국내에 잘 알려져 왔지만, 위의 두 체계와 분류기준을 달리하는 독일 분류체계인 Soil Systematics는 아직 잘 알려져 있지 않다. 본 논문에서 독일 분류체계의 구성과 분류기준을 소개하고자 한다. German Systematics는 6 단계 구조로 이루어져 있고, 상부에서 하위 순서로, soil divisions, soil classes, soil types, soil subtypes, soil varieties, soil subvarieties로 세분화된다. 독일 토양은 먼저 토양수분상태에 따라 4개의 soil divisions 중 하나로 분류되며, 이들은 육지토양, 반육지토양, 반습지/습지토양, 토탄토양이다. 육지토양은 다시 토양발달상태, 층위분화에 따라 13개의 soil classes로 분류되며, 예로 토양발달이 미약한 O/C-토양, 토양발달이 많이 진전되고 Ae-층을 갖는 Podsole (WRB 명명법: Podzols; U.S. Taxonomy: Spodosols)를 들 수 있다. 반육지토양은 지하수토양, 담수토양, 해수토양, 해변토양의 4개의 soil classes로, 반습지/습지토양은 반습지토양, 습지토양의 2개의 soil classes로, 토탄토양도 자연적, 인위적 토탄토양의 2개의 soil classes로 세분화된다. Soil classes는 U.S. Taxonomy의 orders와 비교될 수 있다. 육지토양의 soil classes는 다시 29개의 soil types로, 토양발달이 미약한 토양은 모재에 따라, 토양발달이 진전된 토양은 토양생성과정에 따라 분류된다. 반육지토양의 soil classes는 토양발달 정도에 따라 17개의 soil types로, 반습지/습지토양의 soil classes는 유기물함량에 따라 5개의 soil types로, 토탄토는 생성과정에 따라 5개의 soil types로 세분화된다. Soil types은 독일 토양조사의 기본 단위이며, U.S. Taxonomy의 great groups과 비교될 수 있다. 토양단면의 미세한 형태학적 차이를 고려하여 다시 약 220개의 soil subtypes, 수천 개의 soil varieties과 soil subvarieties로 세분화될 수 있다.

• 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.

• 한국토양동물학회지
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• 제1권1호
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• pp.24-27
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• 1996

Three soil mites of the Family Parholaspidae are discribed from Korea: Holaspina alstoni (Evans, 1956), H. Shigaensis (Ishikawa, 1969) n. comb. and H. trifurcatus (Ishikawa, 1966) n. comb.

• 한국토양동물학회:학술대회논문집
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• 한국토양동물학회 2004년도 학술대회지
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• pp.20-20
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• 2004

• 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.

• Journal of Forest and Environmental Science
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• 제39권3호
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• pp.180-194
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• 2023

This study characterize, classify and evaluates the function of topography on spatial variability of some selected soil properties to assist in designing land management that support uniform agricultural production. The study site, an agricultural land, was part of the derived savanna zone in southwest Nigeria. Four soil profile pits each were established along two delineated toposequence and described following the FAO/UNESCO guidelines. Samples were collected from the identified genetic horizons. Properties of four soil series developed on different positions of the two delineated Toposequence viz upper, middle, lower slopes and valley bottom positions respectively were studied. The soil samples were analysed for selected physical and chemical properties and data generated were subjected to descriptive and inferential statistics. The results showed that soil colour, depth and texture varied in response to changes in slope position and drainage condition. The sand content ranged from 61 to 90% while the bulk density ranged between 1.06 g cm^-3 to 1.68 g cm^-3. The soils were neutral to very strongly acid with low total exchangeable bases. Available phosphorus value were low while the extractable micronutrient concentration varied from low to medium. Soils of Asejire and Iwo series mapped in the study area were classified as Typic isohyperthermic paleustult, Apomu series as Plinthic isohyperthermic paleustult and Jago series as Aquic psamment (USDA Soil Taxonomy). These soils were correlated as Lixisol, Plinthic Lixisol and Fluvisol (World Reference Based), respectively. Major agronomic constraints of the soils associations mapped in the study area were nutrient availability, nutrient retention, slope, drainage, texture, high bulk density and shallow depth. The study concluded that the soils were not homogenous, shows moderate spatial variation across the slope, had varying potentials for sustainable agricultural practices, and thus, the agronomic constraints should be carefully addressed and managed for precision agriculture.

• Journal of Microbiology and Biotechnology
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• 제3권1호
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• pp.57-60
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• 1993

The herbicidal compound, 3D5 was isolated from the culture broth of strain 3D5, a soil isolate. Based on taxonomic studies, this culture was identified as Streptomyces sp. 3D5.

• 환경생물
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• 제33권2호
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• pp.215-222
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• 2015

During our investigation of ciliates from Korea, four ciliates were isolated from the non-flood Petri dish culture of soil. They were cultured under laboratory condition and studied using standard methods morphologically, including living observations, protargol impregnations, and morphometrics. The four species are Metopus hasei Sondheim, 1929, Urosomoida agiliformis Foissner, 1982, Oxytricha proximata Shibuya, 1930, and Cladotricha sp. in Nie${\ss}$en (1984) respectively.