• Title/Summary/Keyword: Soil Water

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Calculation of Thermal Conductivity and Heat Capacity from Physical Data for Some Representative Soils of Korea

  • Aydin, Mehmet;Jung, Yeong-Sang;Lee, Hyun-Il;Kim, Kyung-Dae;Yang, Jae-E.
    • 한국토양비료학회지
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    • 제45권1호
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    • pp.1-8
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    • 2012
  • The thermal properties including volumetric heat capacity, thermal conductivity, thermal diffusivity, and diurnal and annual damping depths of 10 representative soil series of Korea were calculated using some measurable soil parameters based on the Taxonomical Classification of Korean Soils. The heat capacity of soils demonstrated a linear function of water content and ranged from 0.2 to $0.8cal\;cm^{-3}^{\circ}C^{-1}$ for dry and saturated medium-textured soil, respectively. A small increase in water content of the dry soils caused a sharp increase in thermal conductivity. Upon further increases in water content, the conductivity increased ever more gradually and reached to a maximum value at saturation. The transition from low to high thermal conductivity occurred at low water content in the soils with coarse texture, and at high water content in the other textures. Thermal conductivity ranged between $0.37{\times}10^{-3}cal\;cm^{-1}s^{-1}^{\circ}C^{-1}$ for dry (medium-textured) soil and $4.01{\times}10^{-3}cal\;cm^{-1}s^{-1}^{\circ}C^{-1}$ for saturated (medium/coarse-textured) soil. The thermal diffusivity initially increased rapidly with small increases in water content of the soils, and then decreased upon further increases in the soil-water content. Even in an extreme soil with the highest diffusivity value ($1.1{\times}10^{-2}cm^2s^{-1}$), the daily temperature variation did not penetrate below 70 cm soil depth and the yearly variation not below 13.4 m as four times of damping depths.

SATEEC ArcView GIS 시스템을 이용한 홍천군 자운리 유역 무허가경작지의 산림 환원에 따른 토양유실 및 유사저감 분석 (Soil Erosion and Sediment Yield Reduction Analysis with Land Use Conversion from Illegal Agricultural Farming to Forest in Jawoon-ri, Kangwon using the SATEEC ArcView GIS System)

  • 장원석;박윤식;김종건;최중대;임경재
    • 한국수자원학회:학술대회논문집
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    • 한국수자원학회 2008년도 학술발표회 논문집
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    • pp.1300-1304
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    • 2008
  • The fact that soil loss causing to increase muddy water and devastate an ecosystem has been appearing upon a hot social and environmental issues which should be solved. Soil losses are occurring in most agricultural areas with rainfall-induced runoff. It makes hydraulic structure unstable, causing environmental and economical problems because muddy water destroys ecosystem and causes intake water deterioration. One of three severe muddy water source areas in Soyanggang-dam watershed is Jawoon-ri region, located in Hongcheon county. In this area, many cash-crops are planted at illegally cultivated agricultural fields, which were virgin forest areas. The purpose of this study is to estimate soil loss with current land uses (including illegal cash-crop cultivation) and soil loss reduction with land use conversion from illegal cultivation back to forest. In this study, the Sediment Assessment Tool for Effective Erosion Control (SATEEC) ArcView GIS system was utilized to assess soil erosion. If the illegally cultivated agricultural areas are converted back to forest, it is expected to 17.42% reduction in soil loss. At the Jawoon-ri region, illegally cultivated agricultural areas located at over 30% and 15% slopes take 47.48 ha (30.83%) and 103.64 ha (67.29%) of illegally cultivated agricultural fields respectively. If all illegally cultivated agricultural fields are converted back to forest, it is expected that 17.41% of soil erosion and sediment reduction, 10.86% reduction with forest conversion from 30% sloping illegally agricultural fields, and 16.15% reduction with forest conversion from 15% sloping illegally agricultural fields. Therefore, illegally cultivated agricultural fields located at these sloping areas need to be first converted back to forest to maximize reductions in soil loss reduction and muddy water outflow from the Jawoon-ri regions.

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다단토양층을 이용한 하수처리에 관한 연구 (Study of Sewage Treatment using Multi-soil-layering System)

  • 손대희;정윤철;신정훈;정진영;안대희
    • 한국물환경학회지
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    • 제20권3호
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    • pp.215-222
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    • 2004
  • The sewages produced from small villages, rural community, drinking water reservation area and park which doesn't have sewage piping system can be caused a serious water pollution at the restricted areas. The objective of this research was to suggest an economical and effective sewage treatment method by investigating the removal of the organics, nitrogen, and phosphorus in the multi-soil-layering reactor. Soil, natural zeolite, and iron slag were used as a supporting media of multi-soil-layering in this research. The purpose of natural zeolite addition was to maintain the consistent ammonium exchange capacity by providing a sequential environment, and that of iron slag addition was to remove phosphorus by adsorption. Continuous experiment of lab-scale single-soil-layering (S-1), multi-soil-layering (S-2), and mixed-soil-layering (S-3) methods were studied to compare and optimize three different types of the reactors. The organic removal efficiencies showed more than 90% in all three reactors. While S-1 and S-3 reactors showed about T-N removal of 31%, 45%, respectively, the average T-N removal efficiency of the S-2 reactor represented an 87%. In conclusion, that results suggest that the multi-soil-layering reactor could be effectively utilized as a plant for treatment of small village sewage.

요소(尿素)를 시용(施用)한 삼림토양(森林土壤)과 토양수중(土壤水中) 양분함량(養分含量)의 계절적(季節的) 변화(變化) (Seasonal Changes in the Nutrient Content of Soil and Soil Water Affected by Urea Application in Forest)

  • 진현오;주영특;손요환;오종민;정덕영
    • 한국토양비료학회지
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    • 제32권2호
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    • pp.115-122
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    • 1999
  • 본 연구는 인공조림된 잣나무임분과 일본잎갈나무임분을 대상으로 1997년 6월에 요소 (N: $150kg\;ha^{-1}$)를 시용하고 1년간의 토양 및 토양수중 양분함량 변화를 조사하였다. 토양 pH는 시용 후 잣나무임분에서는 급격한 감소경향을, 일본잎갈나무임분에서는 완만한 증가경향을 보였으나 시간이 경과함에 따라 시용 전 농도수준으로 회복되고 있었으며, 전탄소, 전질소는 시용 후 증가 경향을 보이다. 일정한 값을 나타내고 있었다. 치환성 Ca, Mg는 시용 후 감소하는 경향을 보였으나 치환성 K는 증가하는 경향을 보였다. 일본잎갈나무의 토양수의 pH를 제외하고는 양임분 모두 토양수의 pH와 시용 후 감소하는 양이온중 Ca, $NH_4-N$, 음이온중 $NO_3-N$, $SO_4-S$, Cl 농도는 초기간계에서 증가하였으나, K, Mg, 농도는 시용 후 1~2개월 후부터 증가하기 시작하여 4개월 후에 최고 농도치를 나타내고 있었다. 시용 후 급격히 증가한 토양수중 각 용존원소 농도가시용 전과 같은 수준의 농도로 회복되는데에는 Ca, $NH_4-N$, $SO_4-S$, Cl에서 약 1개월, $NO_3-N$, K, Mg에서는 6~12개월로 용존원소에 따라 그 경향을 달리하고 있다.

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전답용 유기질 세립토의 슬레이킹 내구성 및 분쇄 특성 (Slaking and Particle-Separation Characteristics of the Organic Fine Soil in Paddy Fields)

  • 조성민
    • 한국환경복원기술학회지
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    • 제5권3호
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    • pp.1-8
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    • 2002
  • Clayey paddy soils should be mixed with other good coarse soils to be used as a material for the lining, or, embankment. However, it has been difficult to separate soil particles from each other because of the internal cohesion in the soil gradation(separation) characteristics of the fine soil were investigated by various laboratory tests including the slaking durability test. Degradation rate of the soil were dependent upon the clay content and the initial water content before the submergence. The amount of degradations decreased as initial water content increased with exponential functions. The dried specimens separated into the particles after 24 hours of the submergence and specimens which water contents were less than 10% also separated into the particles after 2, or 3 days of the submergence. Compaction curves and the unconfined strength were not varied before and after the submergence. However, unconfined strength decreased as water content increased.

풍화화강토 사면에서 강우로 인한 모관흡수력 변화에 대한 실험 연구 (In-situ Monitoring of Matric Suctions in a Weathered Granite Soil Slope)

  • 이인모;조우성;김영욱;성상규
    • 한국지반공학회:학술대회논문집
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    • 한국지반공학회 2002년도 봄 학술발표회 논문집
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    • pp.509-516
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    • 2002
  • Rainfall-induced landslides in a weathered granite soil slope have mostly relative shallow slip surfaces above the groundwater table The pore-water pressure of soil above the groundwater table is usually negative. This negative pore-water pressure(or matric suction) has been found to make a large contribution to the slope stability. Therefore, the variation of in-situ matric suction profiles with time in a soil slope should be understood. In this study, a field measurement program was carried out from June to August, 2001 to monitor in-situ matric suctions and volumetric water contents in a weathered granite soil slope. The influence of climatic conditions on the variation of in-situ matric suctions could be found to decrease rapidly with depth. It could be found that decrement of matric suction induced by precipitation is affected not only by the amount and duration of rainfalls but also by the initial matric suction just prior to rainstorms. The soil-water characteristic from the field monitoring tends toward the wetting path of SWCC obtained from the laboratory test.

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농업용수 수요량 산정 시스템 개발 (Development of the Estimation System for Agricultural Water Demand)

  • 이광야;김선주
    • 한국농공학회지
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    • 제43권1호
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    • pp.53-65
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    • 2001
  • To estimate agricultural water demand, many factors such as weather, crops, soil, cultivation method, crop coefficient and cultivation area, etc. must be considered. But it is not easy to estimate water demand in consideration of these factors, which are variable according to growth stage and regional environment. This study provides estimation system for agricultural water demand(ESAD) in order to estimate water demand easily and accurately, and arranges all factors needed for water demand estimation. This study identifies the application of estimation system for agricultural water demand with the data observed in the other studies, and analyzes nationwide agricultural water demand. The results are as follows. 1) The practice of different rice cultivation in the paddy field resulted in different water demands. Water depth and infiltration ratio in paddy are the most important factors to estimate water demand. The water depths in paddy simulated by ESAD is very similar to the observed ones. 2) Water demand of upland crops varies with the crops, soil, etc.. Effective rainfall estimated by daily routing of soil moisture varies according to the crops, soil, and effective soil zone(root depth). As crop root become grown, effective rainfall and an amount of irrigation water has been increased. 3) The current unit water demand of upland crops applied as 500mm or 550mm to estimate water demand does not reflect the differences caused by the crops, regional surrounding, weather condition, etc. Results from ESAD for the estimation of water demand of upland crops show that ESAD can simulate the actual field conditions reasonably because it simulates the actual irrigation practices with the daily routing of soil moisture.

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Environmental Conditions and Resource Management in Smallholder Dairy Farms in Thailand. II. Effects of Dairy Wastes on Water and Soil

  • Chantalakhana, C.;Korpraditsakul, R.;Skunmun, P.;Poondusit, T.
    • Asian-Australasian Journal of Animal Sciences
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    • 제12권2호
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    • pp.220-225
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    • 1999
  • The environmental conditions in smallholder dairy farms especially the effects of dairy wastes on waters and soil were the main objectives of this investigation. Forty-three dairy farms from an older dairy cooperative (Nongpho Dairy Cooperative, NP) were compared with four dairy fauns from relatively new dairy cooperative (Kamphaengsaen Dairy Cooperative, KS) for the quality parameters of water and soil samples during a 12-month period. Forty-three farms at NP were from three geographical areas and three levels farm crowdedness. The results from this study clearly showed that the waste waters from older dairy barns contained much higher levels of organic and inorganic substances which could create environmental pollution if not properly managed. The differences in waste water qualities due to areas and seasons were not significant, while waste water samples from crowded farms tended to contain higher averages of waste water parameters such as COD and BOD. Highly significant correlations between pairs of waste water parameters indicated that certain parameters can be used without the need for chemical analysis of some other parameters. The qualities of well water on dairy farms as well as water samples from public waterways nearby indicated some contamination of dairy wastes such as manure. Storage and sun-drying of dairy manure on bare soil surface could result in the contamination of underground water and nearby water sources. Some recommendations from this study if implemented can prevent environmental pollution in smallholder dairy farms.

정수슬러지 혼합토의 함수특성곡선과 불포화 투수 특성 (Characteristics of Soil-Water Characteristic Curve and Unsaturated Permeability of Sludge Mixture)

  • 임병권;김윤태
    • 한국지반공학회논문집
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    • 제29권2호
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    • pp.57-64
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    • 2013
  • 본 논문에서는 정수슬러지의 고함수비 문제를 해결하고 재활용을 촉진하기 위해 정수슬러지와 화강풍화토를 다양한 배합비로 혼합하여 슬러지혼합토(sludge mixture)를 제작하고, 다양한 실내 시험을 통해 슬러지혼합토의 물리적 특성과 불포화 특성을 분석하였다. 시험 결과, 정수슬러지 함량이 증가함에 따라 동일한 모관흡수력에 대응하는 체적 함수비는 증가하였다. 또한 정수슬러지 함량 또는 세립분 함량이 증가함에 따라 공기함입치는 0.9kPa에서 2.4kPa로 증가하였다. 슬러지혼합토의 포화투수계수 값과 함수특성곡선의 결과를 활용하여 강우 시 침투해석을 수행하는데 있어서 중요한 인자인 불포화 투수함수를 산정하였다.

시설재배 토양의 수분 조절을 위한 자동 수분제어시스템 개발 (Development of an Automatic Water Control System for Greenhouse Soil Water Content Management)

  • 이동훈;이규승;장영창
    • Journal of Biosystems Engineering
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    • 제33권2호
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    • pp.115-123
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    • 2008
  • This study was conducted to develop an automatic soil water content control system for greenhouse, which consisted of drip irrigation nozzles, soil water content sensors, an on/off valve, a servo-motor assembly and a control program. The control logic adopted in the system was Ziegler-Nichols algorithm and rising time, time constant and over/undershoot ratio as control variables in the system was selected and determined by various control experiments to maintain small delay time and low overshoot. Based on the experimental results, it was concluded that the control system developed in the study could replace the unreliable conventional greenhouse soil water management.