Earticle

Magnetic separation technology for small paramagnetic particles has been desired for the volume reduction of contaminated soil from the Fukushima nuclear power plant accident and for the separation of scale and crud from nuclear power plants. However, the magnetic separation for paramagnetic particles requires a superconducting high gradient magnetic separation system applied, hence expanding the bore diameter of the magnets is necessary for mass processing and the initial and running costs would be enormous. The use of high magnetic fields makes safe onsite operation difficult, and there is an industrial need to increase the magnetic separation efficiency for paramagnetic particles in as low a magnetic field as possible. Therefore, we have been developing a magnetic separation system combined with a selection tube, which can separate small paramagnetic particles in a low magnetic field. In the previous technique we developed, a certain range of particle size was classified, and the classified particles were captured by magnetic separation. In this new approach, the fluid control method has been improved in order to the selectively classify particles of various diameters by using a multi-stage selection tube. The soil classification using a multi-stage selection tube was studied by calculation and experiment, and good results were obtained. In this paper, we report the effectiveness of the multi-stage selection tube was examined.

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.

본(本) 논문(論文)은 과거(過去) 13년간(年間)(1974~1986) 주택공사(住宅公社)가 전국(全國) 74개(個) 도시(都市), 176개(個) 주택단지(住宅團地)에서 실시(實施)한 제반토질시험결과(諸般土質試驗結果)를 통일분류법(統一分類法)에 의(依)한 흙의 종류별(種類別), 토질정수(土質定數)의 분산(分散)의 정도(程度)를 확률적(確率的)으로 분석(分析)한 것이다. 이 논문(論文)에서 분석(分析)한 토질정수(土質定數)는 자연함수비(自然含水比), 토립자(土粒子)의 비중(比重), 아터버그 한계(限界), 표준매입시험치(標準買入試驗値), 일축압축강도(一軸壓縮强度), 압축지수(壓縮指數) 그리고 강도정수(强度定數) 등(等)이다. 연구분석(硏究分析)한 결과(結果), 물리적(物理的) 저성질(藷性質)은 통계변수(統計變數)인 변동계수(變動係數)를 기준으로 하여 비교(比較)할때 변동(變動)의 범위(範圍)가 비교적(比較的) 적은 반면(反面)에, 강도정수(强度定數)는 40%, 압축지수(壓縮指數)는 32% 정도(程度)의 변동계수(變動係數)를 가지며, 비중(比重)은 사질도(砂質土)에서 0.87-2.49%, 점성토(粘性土)에서 0.91-5.03%로 분산(分散)의 정도(程度)가 매우 작음을 확인(確認)하였다.

This paper probabilisticly analyses the variance of the soil parameters on kinds of soil by conducting statistical analysis through the Unified Soil Classification System. Data used are the result of soil test which the Korea National Housing Corporation conducted in 176 sites of 74 cities throughout the country during the past 13 years from 1974 to 1986. In this paper, soil parameters such as natural water contents, specific gravity of soil particle, Atterberg limits, N-values, unconfined compression strength, compression index and shear strength parameter etc., is analysed. The result of the analysis is as follows. 1) The variance in physical properties of the soil is, when compared with coefficient of variation which is statistical variable, comparatively small. 2) The shear strength parameter is proved to be about 40% and compression index is about 32%. 3) The variance in specific gravity is 0.87-2.49% in granular soil and 0.91~5.03% in cohesive soil respectively. So, the degree of the variance is very small.

지반을 대상으로 하는 일련의 활동에서 지층의 구성에 관한 정보는 필수적인 요소이다. 일반적으로 시추를 통해 지층 구성을 알 수 있으나, 배출되는 작업수와 슬라임, 굴진속도, SPT 시료 등을 참고하여 작성되는 다소 경험적인 면이 있다. 더욱이 최근 시추장비의 고성능화로 인해 얇은 토사층의 경우 구분이 점점 어려워지고 있는 것이 현실이다. 피에조콘관입시험은 주로 점토층을 대상으로 시행되었으나 최근 모래층 및 실트층으로 사용이 확대되고 있는 실정이다. 연속적인 데이터를 확보할 수 있다는 이점이 있어 흙분류에 적용하기 위한 연구가 많이 진행되었고 다양한 도표가 제안되어 사용되고 있다. 하지만, 국내에서는 이에 대한 검증 없이 적용하고 있는 것이 현실이며, 이에 대한 검증을 바탕으로 국내지반과 현실에 맞는 새로운 흙분류 시스템의 개발이 필요한 실정이다. 본 연구에서는 국내 17개 지역에서 수행된 피에조콘 관입시험 결과와 채취된 시료들에 대한 흙분류 결과를 데이터베이스화하였고, 피에조콘 결과를 이용하도록 제안된 국 내외 흙분류차트 7종류들의 국내지반에 대한 적용성을 토질 종류별로 검토하였다. 또한 종합적으로 국내지반의 흙분류에 가장 적합한 흙분류차트와 사용 변수들을 도출하였고 선정된 도표의 영역별 설명과 국내 기술자들에게 익숙한 통일분류결과와의 상관성에 대하여 고찰하였다.

Soil profiling is one of the most important work among geotehnical engineering practice. Generally, soil profile is estimated from the observation of soil samples during subsurface exploration but such estimation also includes some experiencing aspects such as flushed water from the borehole, slime colour, boring speed and so on. In addition, since the capacity of hydraulic drill rig is significantly increased, thin layers might be easily missed. So, continuous soil profile is almost impossible over all depth to be bored from conventional subsurface exploration. While CPT or CPTu can serve continuous soil profile information over all depth generally in 5cm interval. Many charts or methods for soil profile from CPT result have been proposed during last several decades over the world. However they have not been verified in local ground condition in Korea. In this research, CPT results and soil classification results based on USCS were compiled from 17 sites over the Korea. Soil classification results by using 7 CPT soil classification charts were compared with those of USCS for the compiled database. Most proper CPT soil classification chart for Korean soil characteristics was evaluated and effective parameters for the soil classification from CPT were discussed. Finally interrelationship between CPT soil classification chart and USCS soil classification was evaluated.

Hydrologic soil group is one of the important factors to determine runoff potential and curve number. This study was conducted to classify the hydrologic soil groups of Korean soils by considering saturated hydraulic conductivity and depth of impermeable layer. Saturated hydraulic conductivity of Korean soils was estimated by pedotransfer functions developed in the previous studies. Most of paddy soils were classified as D type due to shallow impermeable layer and low saturated hydraulic conductivity in B soil horizon. For upland and forest, soils classified to A and D types increased compared with former classification method because underestimated permeabilities and overestimated drainages were corrected and rock horizon in shallow depth was regarded as impermeable layer. Soils in mountainous land showed the highest distribution in A type, followed by D type. More than 60 % of soils in mountain foot-slope, fan and valley, alluvial plains, and fluvio-marine deposits were classified to D type because of land use such as paddy and upland.

연구방법: 지반을 구성하고 있는 각각의 재료들의 공학적 구분을 위하여 토사, 자갈, 호박돌 등의 용어가 사용되고 있으나, 기관별로 제시된 기준의 차이와 관용적 사용으로 인하여 지 반에 대한 정확한 표현상의 어려움이 발생하고 있으므로 각 기관별로 상이한 용어 및 크기 에 대한 분석을 수행하였다. 연구목적: 시추 기술자의 경험적 판단에 의한 지층 판별이 관행적으로 이루어지는 문제점 이 있다. 이러한 것들이 지반분야의 혼란을 야기할 수 있다. 따라서, 통일된 기준을 제시하 고자 하였다. 연구결과: 본 논문에서는 이러한 문제점을 해결하기 위하여 각 기관별로 상이한 용어 및 크기에 대한 정리를 통하여 합리적인 기준을 제시하였다. 결론: 시추에 의한 지반조사에서 모래, 자갈, 호박돌 등 채취된 시료의 중량비, 출현빈도 및 시료길이 등을 활용하여 비교적 객관적으로 토층을 분류할 수 있는 합리적인 모델을 제시 하였다.

Purpose: It is necessary to set up a standardized method for classifying mixed soil layer that contains sand, gravel and boulder for engineering purposes. Method: Different size of soils was classified mixed soil layer by suggests unified soil classification method. Results: This paper suggests unified soil classification model for different size of soils where many authorities have their own system. Conclusion: Soil stratum classification method using appearing frequencies of gravels and weight ratio of boulders could be used to judgement in many cases.

본 논문에서는 국내 125개 지반에 대한 지층 구성, 전단파속도 주상도, 기반암 깊이 등을 기존 자료의 수집 및 부분 시험 수행을 통해 확보하여 지진응답해석을 수행하였고, 이를 바탕으로 기반암이 얕아 대부분의 지반조사가 기반암까지 이루어지는 국내 지반조건에 적합하도록 기반암 깊이와 토층 평균 전단파속도를 동시에 고려하는 2-매개변수 지반분류 방법을 새롭게 제안하였다. 우선, 기반암 깊이(H)에 대해 10m와 20m를 경계 값으로 설정하여 $H_1$ 지반(H<10m), $H_2$ 지반($10m{\leq}H<20m$) 그리고 $H_3$ 지반($H{\geq}20m$)으로 분류하고 이후, 토층 평균 전단파속도($V_{s,soil}$)를 추가 변수로 하여 총 7개의 지반그룹으로 세분화 하였다. 또한 각 지반그룹에 대하여, 지진응답해석 결과로부터 획득한 지반 증폭계수의 경향성과 그 분산정도를 분석하여 새로운 지반분류 방법의 타당성을 입증하고, 각 지반그룹별 대표 지반 증폭계수 및 설계응답스펙트럼도 함께 제안하였다. 제안된 지반 증폭계수와 이를 대표하는 추세선은 암반노두 가속도의 변화에 따른 지반의 비선형성을 일정한 경향성과 함께 효율적으로 표현하고 있다. 또한 지진응답해석으로부터 획득한 스펙트럴 가속도의 평균값과 제안된 설계응답스펙트럼을 비교한 결과, 일부 지반그룹에서 차이가 발생하였고, 추후 지반 증폭계수 계산을 위한 적분구간을 국내 지반조건에 적합하도록 개선할 필요가 있음을 확인하였다.

Site response analyses were performed based on equivalent linear technique using the local geologic and dynamic site characteristics, which include soil profiles, shear wave velocity profiles and depth to bedrock for 125 sites collected in Korean Peninsula. From the results of site response analyses, 2-parameters site classification system based on the combination of mean shear wave velocity of soil and depth to bedrock was newly recommended for regions of shallow bedrock depth in Korea. First, as the borders of bedrock depth (H) for site classification were determined as 10m and 20m, the soil sites were divided into 3 classes as $H_1$, $H_2$ and $H_3$ sites. And then, the 3 site classes were subdivided into 7 classes based on the mean shear wave velocity of soil ($V_{s,soil}$). The feasibility of new site classification system was verified and the representative site coefficients ($F_a$ and $F_v$) and design response spectrum were suggested by analyzing uniform trend and dispersion of site coefficients for each site class. The suggested site coefficients and the regression curves present the nonlinear characteristics of soils according to the change of rock outcrop acceleration with uniform trend effectively. From the comparison between the mean values of response spectrum which was acquired from the site response analysis and the suggested design response spectrum, there was a little difference in some of site classes and it was verified to adjust the integration interval to make it more suitable for the site condition in Korea.

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.

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.

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.

This paper discusses the development of an up-to-date computerized CPT (Cone Penetration Test) based soil engineering classification system to provide geotechnical engineers with a handy tool for their daily design activities. Five CPT soil engineering classification systems are incorporated in this effort. They include the probabilistic region estimation and fuzzy classification methods, both developed by Zhang and Tumay, the Schmertmann, the Douglas and Olsen, and the Robertson et al. methods. In the probabilistic region estimation method, a conformal transformation is used to determine the soil classification index, U, from CPT cone tip resistance and friction ratio. A statistical correlation is established between U and the compositional soil type given by the Unified Soil Classification System (USCS). The soil classification index, U, provides a soil profile over depth with the probability of belonging to different soil types, which more realistically and continuously reflects the in-situ soil characterization, which includes the spatial variation of soil types. The CPT fuzzy classification on the other hand emphasizes the certainty of soil behavior. The advantage of combining these two classification methods is realized through implementing them into visual basic software with three other CPT soil classification methods for friendly use by geotechnical engineers. Three sites in Louisiana were selected for this study. For each site, CPT tests and the corresponding soil boring results were correlated. The soil classification results obtained using the probabilistic region estimation and fuzzy classification methods are cross-correlated with conventional soil classification from borings logs and three other established CPT soil classification methods.

This study was aimed to classify soil desalination area for cultivation using NDVI (Normalized difference vegetation index) of high-resolution satellite image because the soil salinity affects the change of plant community in reclaimed lands. We measured the soil salinity and NDVI at 28 sites in the Saemangeum reclaimed land in June 2013. In halophyte and non-vegetation sites, no relation was found between NDVI and soil salinity. In glycophyte sites, however, we found that the soil salinity was below 0.1% and NDVI ranged from 0.11 to 0.57 which was greater than the other sites. So, we could distinguish the glycophyte sites from the halophyte sites and non-vegetation, and classify the area that soil salinty was below 0.1%. This technique could save the time and labor to measure the soil salinity in large area for agricultural utilization.

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.

Of actinomycetes isolated from volcanic compost soils, 115 representative strains which showed distinctive morphologicla features were numerically classified, compared with reference strains of Streptomyces. One hundred and twenty unit characters were tested and the average probability of error was 4.27%. The cluster analysis resulted in two groups: group A included strains of actinomycetes except streptomycetes. Group A was divided into 2 major clusters (over 5 strains), 10-diaminopimelic acid. Group B was divided into 5 clusters, of which 4 clusters contained mesodiminopimelic acid and 1 cluster LL-diaminopimelic acid. The major clusters of group A showed higher abilities of substrate utilization and degradation, and higher resistance to inhibitors, whereas the minor and single member clusters of group A showed relatively higher antimicrobial activities. On the other hand, all clusters of group B showed relatively lower abilities of substrate utilization and degradation and lower resistance to inhibitors.

Halophyte communities have been established to reduce dust from the Saemangeum reclaimed land. Growth of large-scale artificial halophyte communities was assessed, and the relationship between halophyte community growth and soil chemical properties was examined through three-year halophyte monitoring and soil analysis. Halophyte community growth was classified in 230 quadrats from 2006 to 2008, and the statistical significance between halophyte community growth and soil chemical properties was determined by Duncan's multiple range test. Overall, the yearly percentage of Class1 and Class 2 quadrats increased from 40% in 2006 to 87% in 2008. Over 90% of the 29 common quadrats consecutively surveyed for three years belonged to Class 1 or Class 2. Soil electrical conductivity (EC) decreased from 3.3 $dSm^{-1}$ in 2006 to 2.0 $dSm^{-1}$ in 2008. Available phosphate content increased from 28 mg $kg^{-1}$ in 2007 to 115 mg $kg^{-1}$ in 2008. Among soil properties, soil EC had a significantly negative relationship with halophyte community growth. A significant relationship was also observed between halophytic height and soil EC ($R^2$=0.95). These results indicate that halophyte community growth could be classified into five classes based on plant height and coverage closely related to soil EC in the reclaimed land.

우리나라의 토양조사는 미농무성(USDA)의 분류방법에 따라 개략토양조사($'65{\sim}'67$년), 정밀토양조사($'68{\sim}'79$년), 논토양배양사업 10개년계획($'80{\sim}'90$년), 그리고 밭토양세부정밀토양조사($'95{\sim}'99$년) 등을 실시하였다. 현지에서의 토양조사는 지형, 배수등급, 토성, 자갈함량, 유효토심, 경사 등 현지의 지형지물 및 환경을 통하여 많은 정보를 얻을 수 있으며, 이를 통하여 전국에 대한 토양조사 결과, 토양통 (심토의 특성이 유사한 토양) 390개, 토양구(표토의 토성을 세분) 536개, 토양상(경사도 및 침식등급을 세분) 1,321개로 분류되어 있다. 우리나라 토양형성 발달에 미친 기후인자는 습윤권역(Udic moisture regime)과 토양온도는 mesic과 일부 남해안과 제주지역의 thermic인 토양온도(Soil moisture regime)였으며, 식생인자는 높은 지역의 경우에는 산림이 낮은 저지대 평탄지는 자연초지가 대부분이다. 지형인자는 동고서저지형으로 동부는 산악지, 서부는 경사가 완만한 구릉지며, 한강 등 대부분이 서남방향으로 흐르는 지형이다. 모재는 다양하나 70%이상이 화강암, 화강편마암이 주를 이루고 있었다. 시간인자의 경우에는 기간이 매우 오래되었으나, 지형이 복잡하여 토양발달이 약한 Inceptisol과 층위발달이 없는 Entisol이 대부분이며, 다음으로 Ultisol과 Alfisol이 뒤를 이었다. 일부 Andisol, Mollisol, Histosol이 존재하였다. 우리나라의 토양분류는 Soil Taxonomy에 의해 분류되었는데, 이것은 토양의 단면내에 존재하는 감식층위(Diagnostic Horizon)의 유무 및 종류에 따른 분류이다. 토양분류 결과 최고 상위분류 단위인 목(order)이 7개, 아목(suborder) 14개, 대군(great group) 27개, 아군(sub group) 67개, 속(family) 161개로 분류되었으며, 가장 저차단위인 통(series)이 390개 분류되었다. 또한 작물이용측면에서 실용적 분류를 실시하였는데, 논토양의 경우 보통논, 미숙논, 사질논, 습논, 염해논, 특이산성논으로 분류할 경우 각각의 분포면적이 31.9%, 23.0%, 31.9%, 9.1%, 3.9%, 0.2%이었다. 밭토양의 경우에도 보통밭, 사질밭, 미숙밭, 중점밭, 고원밭, 화산회밭으로 6개 유형으로 분류할 경우 각각의 분포면적은 41.9%, 23.3%, 17.5%, 13.9%, 1.1. 2.2% 이었다. 도시화 및 도로확대 등 다양한 토지이용 및 지형개변으로 과거의 토양정보가 많이 변경되었다. 그래서, 앞으로는 인공위성자료 및 항공사진을 이용하여 빠르고 쉽게 활용할 수 있는 토양조사 방법개발과 기 구축된 토양도의 수정, 보완 작업이 필요한 절실히 요구되고 있는 현실이다.

토양정밀조사결과 우리나라에서 밝혀진 235 개(個)의 토양통에 대하여 분류체계를 확립(確立)코저 미국(美國)의 신토양분류법에 준(準)하였는바 60개(個)의 아군으로 구분할 수 있었다. 그러나 수도재배기간중(水稻栽培期間中) 담수상태(湛水狀態)를 유지(維持)하게되는 답토양들은 신분류법(新分類法)에 분류기준(分類基準)이 확립(確立)되어 있지않아 토양형태적특성에 입각(立脚)하여 분류(分類)코저 할때 무리(無理)가 있음을 알 수 있었다. 답토양의 분류상(分類上) 문제시(問題視)된 것은 토양아군의 수준(水準)에서 18개(個)였으며 이들 새로운 아군에 대하여 분류기준(分類基準)을 설정(設定)(Setup)하였는 바 그 분류시안(分類試案)의 내용(內容)을 요약(要略)하면 다음과 같다. Anthro aquic, Aquic Udipsamments; 관개수(灌漑水)의 영향(影響)을 받아 표토(表土)로 부터 50cm이상(以上) 회색화작용(灰色化作用)을 받은 사질계충적토(砂窒系沖積土)이며 사두(沙頭)및 김천통등(金川統等)이 이에 속(屬)한다. Anthroaquic Udipsamments; 관개수(灌漑水)의 영향(影響)을 받아 표토(表土)로 부터 50cm 이내(以內)에서 회색화작용(灰色化作用)을 받은 사질계충적토(砂窒系沖積土)로 백수통(白岫統)이 이에 속(屬)한다. Halic Psammaquents; 개답년대(開畓年代)가 오래되지 않은 간척지의 염해답으로 낙천통이 이에 속(屬)한다. Anthroaquic, Aquic Udifluvents; 관개수(灌漑水)의 영향(影響)을 받아 표토(表土)에서 50cm이상(以上) 회색화작용(灰色化作用)을 받은 사양질 및 식양질계 충적토로 마영통(馬嶺統)이 이에 속(屬)한다. Anthroaquic Udifluvents: 관개수(灌漑水)의 영향(影響)을 받아 표토(表土)로부터 50cm이내(以內)에서 회색화작용(灰色化作用)을 받은 사양질 및 식양질계 충적토로 행곡통(杏谷統)이 이에 속(屬)한다. Fluventic Haplaquepts: 지하수위(地下水位)가 높아 토양은 전층이 회색화(灰色化)된 습답으로 유기물(有機物)의 함량(含量)은 토심(土深)이 깊어짐에 따라 불규칙적(不規則的)으로 감소(減少)되는 회색토(灰色土)로 백구 및 학성통등(鶴城統等)이 이에 속(屬)한다. Fuventic Thapto-Histic Haplaquepts: Fluventic Haplaquepts와 유사(類似)하나 토양단면내에 유기물층이 개재된 습답으로 공덕(孔德) 및 서탄통(西炭統)이 이에 속(屬)한다. Fluventlc Aeric Haplaquepts: Fluventic Haplaquepts보다 지하수위(地下水位)가 비교적(比較的) 낮으므로 토양배수가 약간 불량(不良)한 회색토(灰色土)로 만경(萬頃) 및 전북통등(全北統等)이 이에 속(屬)한다. Fluventic Thapto-Histic Aeric Hapldquepts: Fluventic Thapto-Histic Haplaquepts보다 지하수위(地下水位)가 비교적(比較的) 낮으므로 토양배수가 약간 불량(不良)한 회색토(灰色土)로 봉남통(鳳南統)이 이에 속(屬)한다. Fluventic Aeric Sulfic Haplaquepts: Fluventic Aeric Haplaquepts에 비(比)하여 토심(土深) 50~150cm 사이에 황색반문(黃色斑紋)(PH<4.0)인 유화물집적층이 있는 회색토(灰色土)로 등구통이 이에 속(屬)한다. Fluventic Sulfaquepts: 이들 토양은 주(主)로 강하류(江下流)에서 바다로 유입(流入)되는 지점(地点) 및 간석 소택지에 분포(分布)되며 표토(表土)에서 50cm이내(以內)에 유화물집적층이 있는 습답으로 봉림(鳳林) 및 해척통(海拓統)이 이에 속(屬)한다. Fluventic Aeric Sulfaquepts: Fluventic Sulfaquepts 보다 지하수위(地下水位)가 비교적(比較的) 깊으므로 토양 배수(排水)가 약간 불량(不良)한 회색토(灰色土)로 김해통(金海統)이 이에 속(屬)한다. Anthro aquic Fluvaquentic Eutrochrepts: 관

According to Soil Taxonomy which has been developed over the past 20 years in the soil conservation service of the U. S. D. A, Soils in Korea are classified. This system is well suited for the classification of the most of soils. But paddy field soils have some difficulties in classification because Soil Taxonomy states no proposals have yet been developed for classifying artificially irrigated soils. This paper discusses some problems in the application of Taxonomy and suggestes the classification of paddy field soils in Korea. Following is the summary of the paper. 1. Anthro aquic, Aquic Udipsamments : The top soils of these soils are saturated with irrigated water at some time of year and have mottles of low chroma(2 or less) more than 50cm of the soil surface. (Ex. Sadu, Geumcheon series) 2. Anthroaquic Udipsamments : These sails are like Anthroaquic, Aquic Udipsamments except for the mottles of low chroma within 50cm of the soil surface. (Ex. Baegsu series) 3. Halic Psammaquents : These soils contain enough salts as distributed in the profile that they interfere with the growth of most crop plants and located on the coastal dunes. The water table fluctuates with the tides. (Ex. Nagcheon series) 4. Anthroaquic, Aquic Udifluvents : They have some mottles that have chroma of 2 or less in more than 50cm of the surface. The upper horizon is saturated with irrigated water at sometime. (Ex. Maryeong series) 5. Anthro aquic Udifluvents : These soils are saturated with irrigated water at some time of year and have mottles of low chroma(2 or less) within 50cm of the surface soils. (Ex. Haenggog series) 6. Fluventic Haplaquepts : These soils have a content of organic carbon that decreases irregularly with depth and do not have an argillic horizon in any part of the pedon. Since ground water occur on the surface or near the surface, they are dominantly gray soils in a thick mineral regolith. (Ex Baeggu, Hagseong series) 7. Fluventic Thapto-Histic Haplaquepts : These soils have a buried organic matter layer and the upper boundary is within 1m of the surface. Other properties are same as Fluventic Haplaquepts. (Ex. Gongdeog, Seotan series) 8. Fluventic Aeric Haplaquepts : These soils have a horizon that has chroma too high for Fluventic Haplaquepts. The higher chroma is thought to indicate either a shorter period of saturation of the whole soils with water or some what deeper ground water than in the Fluventic Haplaquepts. The correlation of color with soil drainage classes is imperfect. (Ex. Mangyeong, Jeonbug series) 9. Fluventic Thapto-Histic Aeric Haplaquepts : These soils are similar to Fluventic Thapto Histic Haplaquepts except for the deeper ground water. (Ex. Bongnam series) 10. Fluventic Aeric Sulfic Haplaquepts : These soils are similar to Fluventic Aeric Haplaquepts except for the yellow mottles and low pH (<4.0) in some part between 50 and 150cm of the surface. (Ex. Deunggu series) 11. Fluventic Sulfaquepts : These soils are extremely acid and toxic to most plant. Their horizons are mostly dark gray and have yellow mottles of iron sulfate with in 50cm of the soil surface. They occur mainly in coastal marshes near the mouth of rivers. (Ex. Bongrim, Haecheog series) 12. Fluventic Aeric Sulfaquepts : They have a horizon that has chroma too high for Fluventic Sulfaquepts. Other properties are same as Fluventic Sulfaquepts. (Ex. Gimhae series) 13. Anthroaquic Fluvaquentic Eutrochrepts : These soils have mottles of low chroma in more than 50cm of the surface due to irrigated water. The base saturation is 60 percent or more in some subhroizon that is between depth of 25 and 75cm below the surface. (Ex. Jangyu, Chilgog series) 14. Anthroaquic Dystric Fluventic Eutrochrepts : These soils are similar to Anthroaquic Fluvaquentic Eutrochrepts except for the low chroma within 50cm of the surface. (Ex. Weolgog, Gyeongsan series) 15. Anthroaquic Fluventic Dystrochrepts : These soils have mottles that have chroma of 2 or less within 50cm o

본 연구에서는 피조콘관입시험 결과를 활용한 토질분류법 중 가장 일반적으로 사용되고 있는 Robertson 방법과 최근 발표된 최신 분류법인 Schneider 방법을 비교분석하였다. 이를 위하여 경기해안 지역의 연약지반을 대상으로 두 방법 및 통일분류법의 토질분류 결과를 고찰하였다. 연구결과, 두 방법에 의한 결과 차이는 크지 않았으나 전반적으로 Schneider 방법이 점토지역에서, Robertson 방법이 사질토에서 보다 정밀한 결과를 보였다. 보다 신뢰도 높은 토질분류를 위하여 콘 시험의 데이터베이스, 정규화된 콘저항치, 간극수압 및 배수조건에 대한 심층 연구가 필요하다.

In this study, the method by Robertson which has been most commonly used for classifying soils, using piezocone test results, was compared with that by Schneider which was most recently proposed. Both methods were applied to the soils in Gyeonggi province and the classifying results were investigated. It has been found that the difference between the results according to the methods was not so large and Schneider's method showed slightly better results for clay region and vice versa. Such factors as large field database, normalized tip resistance, pore water pressure, and drain condition were found to need further research for more reliable soil classification.