• 제목/요약/키워드: Agricultural soil

검색결과 6,323건 처리시간 0.032초

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.

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.

토양의 형태 및 물리적 특성을 고려한 복분자 재배적지 기준설정 (Establishment of Soil Suitability for Korean Black Raspberry by Soil Morphological and Physical Properties)

  • 현병근;조현준;손연규;박찬원;전현정;송관철;문용희;노대철;윤관희;김명숙;이덕배
    • 한국토양비료학회지
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    • 제46권2호
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    • pp.92-98
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    • 2013
  • The objective of this study was to establish the decision criteria of soil suitability for Korean Black raspberry using soil morphological and physical properties. The investigation was carried out in Gochang, Sunchang, Jeongeup, Pohang, and Hoengseong districts in Korea. The obtained results showed that factors related to the decision criteria of the soil suitability for Korean Black raspberry cultivation were soil texture, soil drainage class, land slope, and available soil depth. The criteria of the best suitability soil for Korean Black raspberry was valley/fan or hill geomorphology, well or moderately drainage class, B-slope(2-7%), coarse loamy soil texture family, less than <15% gravel contents, and available soil depth deeper than 100cm. The area criteria of soil suitability for Korean Black raspberry of Gochang was more than 50% including best and suitable areas.

SMAP 토양수분 이미지를 이용한 농업가뭄 평가 기법 개발 (Development of Agricultural Drought Assessment Approach Using SMAP Soil Moisture Footprints)

  • 신용철;이태화;김상우;이현우;최경숙;김종건;이기하
    • 한국농공학회논문집
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    • 제59권1호
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    • pp.57-70
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    • 2017
  • In this study, we evaluated daily root zone soil moisture dynamics and agricultural drought using a near-surface soil moisture data assimilation scheme with Soil Moisture Active & Passive (SMAP, $3km{\times}3km$) soil moisture footprints under different hydro-climate conditions. Satellite-based LANDSAT and MODIS image footprints were converted to spatially-distributed soil moisture estimates based on the regression model, and the converted soil moisture distributions were used for assessing uncertainties and applicability of SMAP data at fields. In order to overcome drawbacks of the discontinuity of SMAP data at the spatio-temporal scales, the data assimilation was applied to SMAP for estimating daily soil moisture dynamics at the spatial domain. Then, daily soil moisture values were used to estimate weekly agricultural drought based on the Soil Moisture Deficit Index (SMDI). The Yongdam-dam and Soyan river-dam watersheds were selected for validating our proposed approach. As a results, the MODIS/SMAP soil moisture values were relatively overestimated compared to those of the TDR-based measurements and LANDSAT data. When we applied the data assimilation scheme to SMAP, uncertainties were highly reduced compared to the TDR measurements. The estimated daily root zone soil moisture dynamics and agricultural drought from SMAP showed the variability at the sptio-temporal scales indicating that soil moisture values are influenced by not only the precipitation, but also the land surface characteristics. These findings can be useful for establishing efficient water management plans in hydrology and agricultural drought.

Soil Classification of Anthropogenic Soils in a Remodeled Area Using Soil Taxonomy and World Reference Base for Soil Resources

  • Lee, Seung-Been;Chun, Hyen-Chung;Cho, Hyun-Jun;Hyun, Byung-Keun;Song, Kwan-Cheol;Zhang, Yong-Seon;Sonn, Yeon-Kyu;Park, Chan-Won
    • 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.

Analysis of Soil Total Nitrogen and Inorganic Nitrogen Content for Evaluating Nitrogen Dynamics

  • Lee, Seul-Bi;Sung, Jwa-Kyung;Lee, Ye-Jin;Lim, Jung-Eun;Song, Yo-Sung;Lee, Deog-Bae;Hong, Suk-Young
    • 한국토양비료학회지
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    • 제50권2호
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    • pp.100-105
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    • 2017
  • Various methods for assessing soil total nitrogen (TN) and inorganic N content have been developed to manage nutrient and to understand N cycle in soil. This paper address the technical procedures in arable soil samples to conduct soil sampling, sample preparation, and measuring total N and inorganic N. Among various methods for measuring soil total nitrogen contents, Kjeldahl distillation and Indophenol blue method have widely used due to reliability and economic advances. Also, two methods can analyze more samples at the same time compared with other nitrogen measuring methods. For evaluating inorganic N content, mainly in forms of nitrate-N ($NO_3{^-}-N$) and ammonium-N ($NH_4{^+}-N$), extraction with a single reagent such as 2M KCl has been employed, followed by Kjeldahl distillation or indophenol blue methods.

Analysis of components and applications of major crop models for nutrient management in agricultural land

  • Lee, Seul-Bi;Lim, Jung-Eun;Lee, Ye-Jin;Sung, Jwa-Kyung;Lee, Deog-Bae;Hong, Suk-Young
    • 농업과학연구
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    • 제43권4호
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    • pp.537-546
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    • 2016
  • The development of models for agriculture systems, especially for crop production, has supported the prediction of crop yields under various environmental change scenarios and the selection of better crop species or cultivar. Crop models could be used as tools for supporting reasonable nutrient management approaches for agricultural land. This paper outlines the simplified structure of main crop models (crop growth model, crop-soil model, and crop-soil-environment model) frequently used in agricultural systems and shows diverse application of their simulated results. Crop growth models such as LINTUL, SUCROS, could provide simulated data for daily growth, potential production, and photosynthesis assimilate partitioning to various organs with different physiological stages, and for evaluating crop nutrient demand. Crop-Soil models (DSSAT, APSIM, WOFOST, QUEFTS) simulate growth, development, and yields of crops; soil processes describing nutrient uptake from root zone; and soil nutrient supply capability, e.g., mineralization/decomposition of soil organic matter. The crop model built for the DSSAT family software has limitations in spatial variability due to its simulation mechanism based on a single homogeneous field unit. To introduce well-performing crop models, the potential applications for crop-soil-environment models such as DSSAT, APSIM, or even a newly designed model, should first be compared. The parameterization of various crops under different cultivation conditions like those of intensive farming systems common in Korea, shortened crop growth period, should be considered as well as various resource inputs.

고랭지 농업의 작물별 객토량 변화에 따른 토양유실 저감 분석 (Analysis of Soil Erosion Reduction Ratio with Changes in Soil Reconditioning Amount for Highland Agricultural Crops)

  • 허성구;전만식;박상헌;김기성;강성근;옥용식;임경재
    • 한국물환경학회지
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    • 제24권2호
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    • pp.185-194
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    • 2008
  • There is increased soil erosion potential at highland agricultural crop fields because of its topographic characteristics and site-specific agricultural management practices performed at these areas. The agricultural upland fields are usually located at the sloping areas, resulting in higher soil loss, pesticides, and nutrients in case of torrential rainfall events or typhoon, such as 2002 Rusa and 2003 MaeMi. At the highland agricultural fields, the soil reconditioning have been performed every year to decrease damage by continuous cropping and pests. Also it has been done to increase crop productivity and soil fertility. The increased amounts of soil used for soil reconditioning are increasing over the years, causing significant impacts on water quality at the receiving water bodies. In this study, the field investigation was done to check soil reconditioning status for potato, carrot, and cabbage at the Doam-dam watershed. With these data obtained from the field investigation, the Soil and Water Assesment Tool (SWAT) model was used to simulate the soil loss reduction with environment-friendly and agronomically enough soil reconditioning. The average soil reconditioning depth for potato was 34.3 cm, 48.3 cm for carrot, and 31.2 cm for cabbage at the Doam-dam watershed. These data were used for SWAT model runs. Before the SWAT simulation, the SWAT ArcView GIS Patch, developed by the Kangwon National University, was applied because of proper simulation of soil erosion and sediment yield at the sloping watershed, such as the Doam-dam watershed. With this patch applied, the Coefficient of Determination ($R^2$) value was 0.85 and the Nash-Sutcliffe Model Efficiency (EI) was 0.75 for flow calibration. The $R^2$ value was 0.87 and the EI was 0.85 for flow validation. For sediment simulation, the $R^2$ value was 0.91 and the EI was 0.70, indicating the SWAT model predicts the soil erosion processes and sediment yield at the Doam-dam watershed. With the calibrated and validated SWAT for the Doam-dam watershed, the soil erosion reduction was investigated for potato, carrot, and cabbage. For potato, around 19.3 cm of soil were over applied to the agricultural field, causing 146% of more soil erosion rate, approximately 33.3 cm, causing 146% of more soil erosion for carrot, and approximately 16.2 cm, causing 44% of more soil erosion. The results obtained in this study showed that excessive soil reconditioning are performed at the highland agricultural fields, causing severe muddy water issues and water quality degradation at the Doam-water watershed. The results can be used to develop soil reconditioning standard policy for various crops at the highland agricultural fields, without causing problems agronomically and environmentally.

한국 토양정보시스템 소개 (An Introduction of Korean Soil Information System)

  • 홍석영;장용선;현병근;손연규;김이현;정석재;박찬원;송관철;장병춘;최은영;이예진;하상건;김명숙;이종식;정구복;고병구;김건엽
    • 한국토양비료학회지
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    • 제42권1호
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    • pp.21-28
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    • 2009
  • 토양정보는 식량생산, 지속적인 토지이용 계획, 종다양성 평가에 사용되는 기본적인 자료이다. 본 논문에서는 우리나라 토양조사의 역사, 다양한 축척의 토양도 구축과 토양검정, 토양도와 토양검정 자료의 특성, 농업환경 변동 모니터링을 통한 일반농경지 및 취약농경지 토양, 토양정보의 전산화에 따른 토양데이터베이스와 토양정보시스템 소개, 구축된 토양정보의 활용과 향후 방향에 대해 논하였다. 40여년 동안 수행되었던 국책 토양조사 사업 결과 두 종류의 토양 데이터베이스가 구축되었는데, 다양한 축척의 토양도(1:250,000, 1:50,000, 1:25,000, 1:5,000)를 GIS DB로 전산화한 수치토양도 DB와 필지단위로 조사된 화학성 위주의 토양분석 성적을 구축한 토양비옥도 DB이다. 최근에는 친환경농업육성법 시행령에 따른 경작형태 및 오염원별 농경지 토양의 이화학성 및 중금속 함량 조사 자료를 GIS DB로 구축하여 공간적인 분포와 시계열적인 변화를 분석하는 자료로 활용하고 있다. 한국토양정보시스템(http://asis.rda.go.kr)에서 제공하는 토양전자지도는 총 89종으로 토성, 경사, 지형, 모재, 배수등급, 자갈함량, 유효토심 등 토양 GIS 주제도 50종, 사과, 배, 마늘, 수박 등 작물 재배적지 39종 이고, 62종의 토양통계 정보를 제공하고 있다. 토양 변동 정보는 농업환경자원 인벤토리에 기반하여 국립농업과학원에서 구축중인 농업환경자원정보시스템을 통하여 일반농경지의 화학성의 공간적인 분포와 시간적인 변화 정보를 제공될 예정이다. 또한, 기존의 자료를 기반으로 최소한의 실측 자료만으로도 토양의 기능과 환경변화를 예측을 할 수 있는 디지털 지도 작성 기술이 절실히 요구되고 있어 정보시스템은 이를 뒷받침할 수 있어야 할 것이다.