• 제목/요약/키워드: Soil Physical

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오염지역과 비오염지역의 토양의 특성과 토양 미생물의 분포 (The Soil Properties and Microbial Numbers of soil Samples Collected from Polluted and Unpolluted Areas in Korea)

  • 심재욱;이민순;이상선;이태수;이민웅
    • 한국토양환경학회지
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    • 제3권2호
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    • pp.31-39
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    • 1998
  • 오염지역과 비오염지역으로부터 채집한 토양에서 토양의 습도, 유기물의 함량, 토양산도 등 물리적인 특징과 토양미생물의 분포와 같은 생물학적인 특징이 조사되었다. 지역에 따른 유기물의 함량과 토양산도는 큰 차이를 나타내었으나, 식물군락에 의한 토양수분과 유기물 함량의 차이점은 발견할 수 없었다. 토양의 산도는 미생물의 분포수와 상관관계를 나타내었다. 이러한 것은 식물이 자라는 토양에 변이를 주는 것으로 산성비와 관련이 있는 것으로 추정된다.

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사토(砂土)에 있어서 모델 테스트에 의한 차륜(車輪)의 성능(性能) 예측(豫測)에 관한 연구(硏究) (Performance Prediction of Powered-Rigid Wheel by Model Tests)

  • 이규승;이용국;박승제
    • Journal of Biosystems Engineering
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    • 제13권4호
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    • pp.1-8
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    • 1988
  • A series of soil bin experiments was carried out on land to evaluate the soil physical properties whether they are pertinent to soil-wheel system and to investigate if true model theory u applicable to powered rigid wheel-soil system. Four different sized wheels having diameter of 45, 60, 75 and 90 em were wed for the experiment. The following conclusion was derived from the study. (1) True model theory can be sufficiently utilized to study the wheel traction and linkage on lands. (2) For both dry and wet sands, Cone Index(CI) and soil shear parameters (c, ${\phi}$) with bulk density (${\gamma}$) were found to be good measures of soil physical properties which are pertinent to predict the performance of the powered rigid wheel-soil system.

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밭토양의 물리성(物理性)과 수분문제(水分問題) (Soil Physical Properties of Upland Soil in relation to Soil Moisture)

  • 유순호
    • 한국토양비료학회지
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    • 제6권1호
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    • pp.61-65
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    • 1973
  • Analysis of data in the Official Soil Series Description showed the dominant texture of upland soils is SiL, of which available water range is 21.1% highest among textures. Analyses of data in the N, P, K Trials on Barley in 1964/65-1968/69, and N, P, K and Soil Improvement Trials on upland Crops in 1961-1969 were made to relate fertilizer response to the amount of rainfalls during the growing season. Correlation between nitrogen response and the amount of rainfalls was observed but not between P and K and the amount of rainfalls. Some of physical properties were discussed to seek feasible means for increasing available water.

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오수처리용 인공습지내 토양의 이화학적 특성조사 (A Study on the Physical and Chemical Characteristics of the Constructed Wetland Soil for Sewage Treatment)

  • 윤춘경;권태영;우선호
    • 농촌계획
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    • 제5권2호
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    • pp.24-29
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    • 1999
  • The soil from constructed wetland system for sewage treatment was analyzed to examine physical and chemical characteristics. Clogging and lowered permeability were the physical matters of concern, and nutrient and salt accumulation were the chemical matters of concern. However, the soil properties of the constructed wetland system after 3 year operation demonstrated no degradation and still the soil works almost same as the initial stage. Encouragingly, no sludge accumulation was observed inside the system. Therefore, it implies that the wetland sewage treatment system can work continuously as long as it is operated and managed properly not to cause excessive pollutant loading.

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산불이 산림토양의 이화학적 성질에 미치는 영향 (Fire Effects on Soil Physical and Chemical Properties following the Forest Fire in Kosung)

  • 이원규;김춘식;차순형;김영걸;변재경;구교상;박재욱
    • The Korean Journal of Ecology
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    • 제20권3호
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    • pp.157-162
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    • 1997
  • Changes on soil physical and chemical properties following the forest fire in Kosung area in Kangwon province were examined. Twenty seven sampling plots[16 burned (8 low intensity fire, 8 high intensity fire) and 11 unburned plots] from Pinus densiflora community were chosen and soil samples from three depths(0-5, 5-15, 15-25 cm) under the forest floor were collected. Forest fire in the area affected soil chemical properties. Soil pH, available phosphorus, base saturation, K, Ca, and Mg on the surface soil(0-5cm) in the burned areas compared with the unburned areas were increased, while soil properties on the subsurface soil(5-25 cm) were not changed. Organic matter, total nitrogen, available phosphorus, and exchangeable cations following the high in tensity fire on the surface soil were generally lower than those in the low intensity fire areas. This indicates that these nutrients on high intensity fire areas may be volatilized. The results suggest that the fire effects on soil chemical properties were confined mainly to the surface soil and were different between the high and the low intensity fire types.

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전라남도 장성과 화순에 분포하는 석회암풍화토의 물성 및 전단 특성 (The Physical and Shear Strength Properties of the Weathered Limestone Soils in Changsung and Hwasun Area of Chonnam Province, Korea)

  • 김해경
    • 지질공학
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    • 제13권3호
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    • pp.335-344
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    • 2003
  • 본 연구에서는 전라남도 장성과 화순에 분포하는 석회암풍화토의 물성 및 전단 특성을 연구하였다. 석회암풍화토의 교란시료에 대한 물성 및 전단 특성을 파악하기 위하여 실내 시험이 수행되었다. 연구지역의 석회암풍화토에 대한 물성 및 전단 특성은 다음과 같다 비중(Gs)은 2.78~2.80, 액성한계(LL)는 37~38(%), 소성지수(PI)는 13.7~15.4이며 흙의 분류(USCS)는 CL에 해당된다. 불포화 시료의 직접전단시험 (vd, $1.5t/\textrm{m}^3$)에 의한 강도정수는 점착력(c)이 3.07~4.4 ($t/\textrm{m}^2$) 그리고 내부마찰각($\Phi$)은 $34.8~42.4^{\circ}$의 범위를 보인다. 화강암풍화토 (양, 1997; 문. 1998; 박, 1998)와 비교해 보면, 연구지역의 석회암 풍화토의 물리적 특성은 일반적으로 차이를 보이며, 전단 강도정수 중, 내부마찰각은 대체적으로 유사한 경향을 보이는 것으로 나타났다.

하해혼성(河海混成) 식양질(埴壤質) 답(沓)에서 토양물리성(土壤物理性) 개선(改善)이 수도수량(水稻收量)에 미치는 영향(影響) (The Effects of Soil Physical Improvement on Rice Yields at Fine Textured Fluvio-Marine Paddy Field)

  • 조인상;임정남;소재돈;이선용;최대웅
    • 한국토양비료학회지
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    • 제16권2호
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    • pp.92-97
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    • 1983
  • 하해혼함식양질답(河海混咸埴壤質畓)에서 수도수량(水稻收量)을 향상(向上)시킬 수 있는 토양물리성(土壤物理性) 개량방법(改良方法)을 구명(究明)하기 위하여 심토파쇄 및 혼층처리후(混層處理後) 수도생육(水稻生育)과 토양물리성(土壤物理性)을 조사(調査)한 시험결과(試驗結果)는 다음과 같다. 1. 심토파쇄와 혼층처리(混層處理)에 의(依)하여 가비중(假比重), 경도(硬度), 공극률(孔隙率) 및 투수성등(透水性等) 토양물리성(土壤物理性)이 현저(顯著)히 개선(改善)되었다. 2. 토양(土壤)의 물리성(物理性)과 수도(水稻)의 근(根) 발달 및 수량간(收量間)에는 유의성(有意性)있는 상관관계가 성립(成立)되었다. 3. 토양물리성개선(土壤物理性改善)에 의(依)한 수도(水稻)의 증수효과는 약(約) 10%로써 배수효과 5%보다 훨씬 높았다. 4. 토양물리성개선효과는 4년차(年次)까지 지속(持續)되었으며 혼층(混層)이 심토파쇄(深土破碎)보다는 효과가 좋았으나 심토파쇄가 중기계(重機械)를 이용(利用)하여 편리(便利)한 작업(作業)이 가능(可能)하므로 가장 효율적인 개선방법(改善方法)이라고 판단된다. 5. 혼층처리시에 생고시용(生藁施用)은 무시용(無施用)에 비(比)하여 수도수량(水稻收量)이 2~3% 증수되었다.

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Gy의 입자성 물질 시료채취이론에 근거한 토양 시료 채취량 결정 (Determination of Soil Sample Size Based on Gy's Particulate Sampling Theory)

  • 배범한
    • 한국지하수토양환경학회지:지하수토양환경
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    • 제16권6호
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    • pp.1-9
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    • 2011
  • A bibliographical review of Gy sampling theory for particulate materials was conducted to provide readers with useful means to reduce errors in soil contamination investigation. According to the Gy theory, the errors caused by the heterogeneous nature of soil include; the fundamental error (FE) caused by physical and chemical constitutional heterogeneity, the grouping and segregation error (GE) aroused from gravitational force, long-range heterogeneous fluctuation error ($CE_2$), the periodic heterogeneity fluctuation error ($CE_3$), and the materialization error (ME) generated during physical process of sample treatment. However, the accurate estimation of $CE_2$ and $CE_3$ cannot be estimated easily and only increasing sampling locations can reduce the magnitude of the errors. In addition, incremental sampling is the only method to reduce GE while grab sampling should be avoided as it introduces uncertainty and errors to the sampling process. Correct preparation and operation of sampling tools are important factors in reducing the incremental delimitation error (DE) and extraction error (EE) which are resulted from physical processes in the sampling. Therefore, Gy sampling theory can be used efficiently in planning a strategy for soil investigations of non-volatile and non-reactive samples.

Soil Physico-chemical Properties by Land Use of Anthropogenic Soils Dredged from River Basins

  • Park, Jun-Hong;Park, Sang-Jo;Won, Jong-Gun;Lee, Suk-Hee;Seo, Dong-Hwan;Park, So-Deuk
    • 한국토양비료학회지
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    • 제49권4호
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    • pp.341-346
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    • 2016
  • This study was conducted to analyze soil physico-chemical properties of agricultural land composed from the river-bed sediments. We investigated the changes of soil physico-chemical properties at 30 different sampling sites containing paddy, upland and plastic film house from 2012 to 2015. pH, exchangeable calcium and magnesium decreased gradually in paddy soils during the four years, whereas the available $P_2O_5$, exchangeable Ca, Mg and EC increased in upland and plastic film house soil. For the soil physical properties, bulk density and hardness of topsoil were $1.47g\;cm^{-3}$ and 21.5 mm and those of subsoil were $1.71g\;cm^{-3}$ and 25.7 mm in paddy soils. In upland soils, bulk density and hardness of topsoil were $1.48g\;cm^{-3}$ and 15.9 mm and those of subsoil were $1.55g\;cm^{-3}$ and 16.9 mm. In plastic film house soils, bulk density and hardness of topsoil were $1.42g\;cm^{-3}$ and 14.4 mm and those of subsoil were $1.40g\;cm^{-3}$ and 18.5 mm, respectively. The penetration hardness was higher than 3 MPa below soil depth 20 cm, and it is impossible to measure below soil depth 50 cm. As these results, in agricultural anthropogenic soils dredged from river basins, the pH, amount of organic matter and exchangeable cations decreased and soil physical properties also deteriorated with time. Therefore, it is needed to apply more organic matters and suitable amount of fertilizer and improve the soil physical properties by cultivating green manure crops, deep tillage, and reversal of deep soils.

인공위성자료와 디지털 토양자료를 통해 분석한 미중부 대평원 지역 가뭄정도에 미친 물리적 토양특성의 영향 (Influences of Physical Soil Properties on Drought Severity in the Central Great Plains Based on Satellite Data and a Digital Soil Database)

  • Sunyurp Park
    • 대한지리학회지
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    • 제38권6호
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    • pp.935-948
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    • 2003
  • STATSGO 데이터베이스는 주단위의 토양 특성을 분석하는 데에 있어 효과적인 자료다. 본 연구에서는 GIS 기법을 이용하여 STATSGO로부터 8개 주요 토양 특성을 추출하였다: 함수력(available water capacity), 점토비율, 토양깊이, 사면경사. 지하수위까지의 깊이, 배수 특성, 토성, 투수도, 평균적인 NDVI로부터의 편차로 정의된 가뭄 정도(drought severity)에 대해 앞서 열거한 토양 특성이 미치는 영향을 캔자스 중서부 지역을 대상으로 분석하였다. 연구 결과에 따르면, 분석된 8개 변수 중 7개가 통계적으로 유의한 상관관계를 가진 것으로 나타났는데, 상관계수는 -0.89에서 0.85에 이르렀다. Moderate Resolution Imaging Spectroradiometer(MODIS)로부터 취득된 지표복사열(thermal emission) 자료는 평균 NDVI에 대한 편차로 표현되는 가뭄정도와 통계적으로 유의한 상관관계를 가졌으며, 식물생육기간에 걸친 가뭄지역의 공간적 변화를 잘 나타내었다. 토양수분의 결핍양이 많아질수록, 복사열 시그널 값도 높아지며, 공간적 분포로 볼 때. 상대적으로 건조한 캔자스 서부로부터 증가하여 시간에 따라 점차 그 분포도 변화하였다. 연구결과는 또한 가뭄의 진행단계에 따라 가뭄에 대한 각 토양 변수의 영향도 달라짐을 보여주었다.