• 한국농공학회지
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• 제34권4호
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• pp.69-79
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• 1992

To estimate soil behavior and structural characteristics under the conditions of cyclic loading, freezing & thawing and initial state, several testing was performed and obtained following results. 1.After repeated freezing and thawing processes, original soil structure was destroyed and changed to globular structure from honeycomb or tube in its structure types. Also above processes resulted increasing the soil compression strain while decreasing the failure stress in stress-strain relationship and reached the soil structure into the mode of brittle fracture. Under cyclic loading conditions, soil cluster which was originally dispersed structure colloided with each other, seperated, and finally the soil failed due to the effect of overcompaction. 2.Through the stabilization processes seperated by four steps, the structure of soil skeleton was changed to quite different globular type. The degree of compressibility of soil was decreased in the normally consolidated zone, while the strength against external load increased due to soil particle stabilization. 3.Soil stress-strain chracteristics were largely influenced by repeated up and down processes of temperature. The maximum deformation was obtained in the case of temperature between 0 10˚C by the reseon of particle cluster reformation. 4.Soil compressibility was largely influenced by the optimum moisture content. Under freezing process, swelling could be found and its magnitude was proportional to the density of soil. 5.Density of soil was decreased as increasing the number or repeated freezing and thawing processes and the largest decreasing rate was found at the first turning point from freezing to thawing cycle.

• 대기
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• 제15권1호
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• pp.1-16
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• 2005

Land-surface and soil processes significantly affect mesoscale local weather systems as well as global/regional climate. In this study, characteristics of land-surface models (LSMs) and soil models (SMs) that are frequently coupled into mesoscale meteorological models are investigated. In addition, detailed analyses on three LSMs, employed by the PSU/NCAR MM5, are provided. Some impacts of LSMs on heavy rainfall prediction are also discussed.

• 한국토양비료학회지
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• 제6권1호
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• pp.67-73
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• 1973

Soil humic substances are defined as a humified part of the soil organic matters and regarded to play beneficial roles for colloid chemical properties and the fertility of the soils. This paper is referred to review the present trend of the studies on the forming processes of humic substances and on the effect on plant metabolism by some organic compounds that are directly absorbed by plants. It is generally considered that the humic substances are formed organic matters in soil or plant materials through numerous organic or biochemical processes. However, the nature of the constituting "core" and of attachment of carbohydrate, nitrogen containing compounds like protein, phenolic compounds and metals to the core are unclear though various models are suggested. It is reviewed that some organic compounds, phenclic acids, derived from humic substances are effective on plant metablism in many cases, although the mechanisms are remained to be clarified.

• 한국토양비료학회지
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• 제47권5호
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• pp.362-367
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• 2014

This study was performed to test the applicability of the ozone/hydroxy radical reaction system, which applied advanced oxidation processes, to remove total petroleum hydrocarbon (TPH) from the fine soil in washing water of the soil washing process. Removal efficiency was tested on 40 L of washing water in a pilot reaction tank. Fine soil contaminated with $800mg\;kg^{-1}$ TPH was prepared at 5% and 10% suspended solids. Testing conditions included ozone/hydroxy radical flow rates of 40, 80, and $120L\;min^{-1}$, and processing time of 2 to 12 hours. The removal efficiency of petroleum hydrocarbon from water waster by ozone/hydroxy radical was increased with higher flow rates and lower percentages of suspended solids. Optimal efficiency was achieved at $80L\;min^{-1}$ flow rate for 4 hours for the 5% suspended solids, and $120L\;min^{-1}$ for 6 hours for the 10% suspended solids. These results verified the efficiency of hydroxy radical in removing TPH and the applicability of the ozone/hydroxy radical reaction system in the field.

• Journal of Microbiology
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• 제42권4호
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• pp.267-277
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• 2004

Effects of elevated $CO_2$ on soil microorganisms are known to be mediated by various interactions with plants, for which such effects are relatively poorly documented. In this review, we summarize and syn­thesize results from studies assessing impacts of elevated $CO_2$ on soil ecosystems, focusing primarily on plants and a variety the of microbial processes. The processes considered include changes in microbial biomass of C and N, microbial number, respiration rates, organic matter decomposition, soil enzyme activities, microbial community composition, and functional groups of bacteria mediating trace gas emission such as methane and nitrous oxide. Elevated $CO_2$ in atmosphere may enhance certain micro­bial processes such as $CH_4$ emission from wetlands due to enhanced carbon supply from plants. How­ever, responses of extracellular enzyme activities and microbial community structure are still controversy, because interferences with other factors such as the types of plants, nutrient availabilitial in soil, soil types, analysis methods, and types of $CO_2$ fumigation systems are not fully understood.

• 한국환경과학회지
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• 제22권4호
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• pp.415-424
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• 2013

In this paper, time series of soil moisture were measured for a steep forest hillslope to model and understand distinct hydrological behaviours along two different transects. The transfer function analysis was presented to characterize temporal response patterns of soil moisture for rainfall events. The rainfall is a main driver of soil moisture variation, and its stochastic characteristic was properly treated prior to the transfer function delineation between rainfall and soil moisture measurements. Using field measurements for two transects during the rainy season in 2007 obtained from the Bumrunsa hillslope located in the Sulmachun watershed, a systematic transfer functional modeling was performed to configure the relationships between rainfall and soil moisture responses. The analysis indicated the spatial variation pattern of hillslope hydrological processes, which can be explained by the relative contribution of vertical, lateral and return flows and the impact of transect topography.

• 자원환경지질
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• 제53권4호
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• pp.441-477
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• 2020

매년 다량 발생되고 있는 정화토가 적절하게 재이용 또는 재활용되지 못하고 반출 처리장에 적치되어 또 다른 환경적 이슈가 되고 있다. 이에 본 논문에서는 이러한 정화토의 재이용 및 재활용을 활성화하기 위하여 필요한 정화토의 토양 질 회복 기술에 대한 연구 및 개발 동향을 조사하였다. 이를 위해 먼저 정화기술별 토양 특성의 변화 양상을 살펴보고, 정화공정에 따른 토양 질의 열화 특성을 파악하였다. 뿐만 아니라 정화토 재이용 및 재활용을 위한 정책적 관련 사항들을 정리하고, 향후 필요한 연구들에 대하여 제안하였다. 본 논문은 국내외 관련 문헌들을 검색하여 작성하였다. 키워드 검색을 통하여 정화기술별 토양 특성의 변화와 토양 개량 및 회복 기술과 연관된 문헌을 조사하였으며, 본문에서는 주로 최근에 발표된 문헌들을 바탕으로 논의하였다. 뿐만 아니라, 제 1, 2차 토양보전기본계획을 참고하여 정화토 재이용 및 재활용과 관련된 정책적 사항들을 정리하였다. 현재까지 국내에서 가장 많이 적용된 토양경작, 토양세척, 열탈착 등을 대상으로 정화공정에 따른 토양의 특성 변화를 정리한 결과, 적용하는 정화기술에 따라서 매우 상이하게 나타나는 것으로 조사되었다. 특히 정화공정을 거치면서 토양 질이 열화되는 양상이 정화기술에 따라서 다르게 나타났다. 토양 개량 및 회복 기술은 크게 무기 개량제, 유기 개량제, 생물학적 개량제 등의 제제를 이용한 방법들로 구분할 수 있으며, 각 개량제에는 다양한 물질들이 활용되고 있고, 각 물질에 따라 개선 또는 향상되는 토양의 특성이 달랐다. 하지만, 각 정화기술별 열화되는 토양 질 회복을 위한 연구들은 현재까지 활발하게 수행되지 않은 것으로 조사되었다. 제 2차 토양보전기본계획에서는 정화토의 품질인증제, 목표관리제 등과 같은 정책적 방안이 명시되어 있음으로써 향후 정화토의 재이용 및 재활용이 촉진될 수 있을 것으로 예상된다. 정화토의 재이용 및 재활용을 위해서는 적용된 정화기술과 미래 용도를 고려한 공공활용성을 담보한 회복 기술들이 개발되어야 할 것으로 판단된다. 이와 더불어 제 2차 토양보전기본계획에서 제시한 정화토의 적극적 활용을 위해서는 이를 뒷받침할 수 있는 구체적이고 세부적인 정책 추진 방안이 마련되어야 할 것이다.

• 한국환경과학회지
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• 제15권2호
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• pp.133-139
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• 2006

Soil biofiltration is an environmentally-sound technology for elimination of VOCs, odorous and NOx compounds from a low concentration, high volume waste gas streams because of its simplicity and cost-effectiveness. This study was performed to evaluate effect of removal of gaseous NOx using a soil and a yellow soil. Over $60\%\;and\;48\%$ of NOx from a soil and a yellow soil was removed at the inlet NO concentrations of $423\~451$ppb, respectively. The bio-filter using a soil media was capable of purifying NOx with a different natural processes. Although some of the processes are quite complex, they can broadly be summarized as adsorption into soil pore water, and biochemical transformations by soil bacteria. When the filteration bio-reactor was applied to a soil and a yellow soil, effective NOx removal was obtained for several times and months. These results show that a soil biofilter can be of use as an alternative advanced NOx treatment system.

• 한국수자원학회:학술대회논문집
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• 한국수자원학회 2009년도 학술발표회 초록집
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• pp.529-534
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• 2009

Climate models, both global and regional, have increased in sophistication and are being run at increasingly higher resolutions. The Land Surface Models (LSMs) coupled to these climate models have evolved from simple bucket models to sophisticated Soil-Vegetation-Atmosphere Transfer (SVAT) schemes needed to support complex linkages and processes. However, some underpinnings of terrestrial hydrologic parameterizations so crucial in the predictions of surface water and energy fluxes cause model errors that often manifest as non-linear drifts in the dynamic response of land surface processes. This requires the improved parameterizations of key processes for the terrestrial hydrologic scheme to improve the model predictability in surface water and energy fluxes. The Common Land Model (CLM), one of state-of-the-art LSMs, is the land component of the Community Climate System Model (CCSM). However, CLM also has energy and water biases resulting from deficiencies in some parameterizations related to hydrological processes. This research presents the implementation of a selected set of parameterizations and their effects on the runoff prediction. The modifications consist of new parameterizations for soil hydraulic conductivity, water table depth, frozen soil, soil water availability, and topographically controlled baseflow. The results from a set of offline simulations are compared with observed data to assess the performance of the new model. It is expected that the advanced terrestrial hydrologic scheme coupled to the current CLM can improve model predictability for better prediction of runoff that has a large impact on the surface water and energy balance crucial to climate variability and change studies.

• 한국수자원학회논문집
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• 제47권10호
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• pp.945-958
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• 2014

토양온도는 비점오염과 관련된 수문학적 및 생지화학적 과정에 영향을 주는 중요한 물리적 환경인자 중 하나이다. 이 연구에서는 분포형 유역모델인 CAMEL(Chemicals, Agricultural Management and Erosion Losses)의 겨울철 토양온도 모의성능을 개선하기 위해서 융설과 토양 동결-융해 모델을 개발하였으며, 경기도 여주에 위치한 시험유역의 4개 지점에서 3개월 동안 관측한 토양온도 자료를 사용하여 모델을 보 검정하였다. 모의 결과, 표층 토양온도에 대해서는 모델이 토양온도의 시계열 변화를 비교적 잘 재현하는 반면($R^2$ 0.71~0.95, RMSE $0.89{\sim}1.49^{\circ}C$), 하부토양층 온도에 대해서는 경우에 따라 모델의 예측오차가 다소 크게 나타났는데($R^2$ 0.51~0.97, RMSE $0.51{\sim}5.08^{\circ}C$), 이것은 모델에서 토양 깊이별 토성을 동일한 것으로 가정한 것이 주요 원인인 것으로 판단된다. 한편, 개발된 모델은 융설에 의한 단열효과와 토양 동결-융해 과정에서 유입 또는 방출되는 잠열흐름의 영향으로 토양온도의 진폭이 감소하는 현상을 잘 모의하고 있다. 비록 모델 구조의 한계와 자료의 부족으로 토양온도에 대한 다소의 예측오차가 발생하였지만, 개발된 토양온도 모델은 시험유역의 토지이용 및 지형에 따른 토양온도와 적설상당수량의 시공간적 분포를 합리적으로 잘 모의하는 것으로 사료된다.