• 물과 미래
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• 제29권2호
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• pp.143-151
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• 1996

중간류 유출, 지표표화지역, 흙수분저류량들의 동적 반응을 Richards 방정식을 이용한 수치실험을 통하여 유도하였다. 그리고 수치실험에서 경사면 모양, 토양종류, 경계조건 등을 변화시켜서 지표포화지역-중간류유출 동적 관계 및 지표포화지역-흙수분저류량 동적 관계를 결정하였다. 모의결과에 의하면, 지표포화지역-중간류유출 동적 관계 및 지표포화지역-흙수분 저류량 동적 관계는 각 관계들의 정상류 관계에 의해 근사적으로 설명될 수 있다. 그리고 강우양상이 단순한 펄스입력일지라도 중간류유출 및 지표포화지역의 동적 반응은 중복첨두치에 의해 특징지어지며, 중복첨두치의 발생에 대한 물리적 메케니즘은 "variable source area"의 개념을 이용하여 설명하였다.용하여 설명하였다.

• 한국수자원학회논문집
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• 제31권6호
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• pp.795-806
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• 1998

토양수분은 기후, 토양 및 지표면의 조건 등에 의해 영향을 받는다. 특히, 급격한 도시화 및 산업화의 영향으로 다른 영향인 자들 보다 지표면 조건의 변화가 크게 바뀌고 있다고 할 수 있으며 본 연구에서는 이러한 지표면 조건의 변화가 토양수분에 어떻게 영향을 미칠 수 있는지를 간단한 토양수분 동역학 모형을 이용하여 평가해 보았다. 먼저, 본 논문에서는 토양수분의 시간적 공간적 통계특성을 정량화 해보기 위해 논문의 전반부를 Washita ’92 자료 및 Monsoon ’90 자료의 1차원 및 2차원의 통계적 특성을 정리하는데 할해하였으며, 논문의 후반부에서 지표면 조건의 변화를 모형 매개변수의 통계적인 특성을 변화시킴으로서 고려하고 각각의 경우 토양수분이 어떻게 반응하는가를 살펴보았다. 사용된 모형은 선형저수지의 개념에 토양상층에서의 공간적 거동을 고려하기 위하여 확산의 개념을 도입하여 구성된 모형이다. 모형의 주요 매개변수는 손실률과 확산계수로 나타나고, 이들은 관측자료의 통계특성을 이용하여 추정될 수 있다. 지표면 조건의 변화는 모형의 매개변수에 다양한 통계특성을 적용하고 고려하게 된다. 특히, 본 연구에서는 지표면 조건의 평균적인 변화보다 이의 공간적인 분산도의 변화에 초점을 맞추어 분석하였다. 이는 평균적인 지표면 조건의 변화는 선형저수지의 이론에 근거하여 그 영향을 쉽게 판단할 수 있기 때문이다. 본 연구의 결과를 정리하면 다음과 같다. (1) 지표면 상태의 분산도가 커질 경우 토양수분은 더 쉽게 손실된다, (2) 토양수분의 분산도는 모의 초기에 강우의 영향으로 크게 나타나나 시간이 경과함에 따라 감소하고 점차 지표면 상태의 분산특성를 나타내게 된다, (3) 지표면 유출이나 토양상층에서의 토양수분 이동에 따른 확산의 영향은 지표면 유출이 존재하는 강우기간으로 제한되며 전체적으로 토양수분의 변화에 미미한 영향을 미친다.

• 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.

• 한국방재학회 논문집
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• 제8권2호
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• pp.59-63
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• 2008

지표수 흐름은 육지 물수지 계산에 중요한 요소중에 하나이다. 그러나, 기상변화의 예측과 그로 인한 방재대책수립을 위한 대규모의 기상모형과 연계되는 육지수문모형(Land Surface Model, LSM)들은 지표수 흐름을 토양수분수지로부터 간단하게 산정하고 있다. 침투계산에서 지표수 흐름깊이를 무시하는 것은 지표면 및 지표하 물흐름 모두에 계산상 오류를 초래할 수 있다. 그러므로, 육지수문모형에서 종합적인 물과 에너지 순환 예측을 하기 위해, 지표수 흐름을 위한 1차원 확산모형과 지표하 물흐름을 위한 계산망 체적평균 토양수분이송(Volume Averaged Soil-moisture Transport Model, VAST)모형을 연계하는 대규모 지표면 및 지표하 연계 물흐름 모형이 개발되었다. 이 논문에서는, 최첨단 육지수문모형중 하나인 CLM(Common Land Model)내의 지표수리수문 모의를 위한 주요부분을 비롯하여, 지형특성에 따른 지표수 흐름과 공간적 토양수분 분포의 예측개선을 위한 새로운 지표면 및 지표하 연계 물흐름 모형에 대해 기술하였다.

• 한국지하수토양환경학회:학술대회논문집
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• 한국지하수토양환경학회 2003년도 추계학술발표회
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• pp.360-362
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• 2003

The adhesion of hydrocarbon degrading bacteria(HDB) differing in surface hydrophobicity was investigated. Cell wall hydrophobicity was modified chemically and physiologically. Modified adhesion deficient mutant of HDB was selected in a soil column assay Physiologically and chemical modification increased cell surface hydrophobicity. Cell surface charcteristis including BATH and zeta potential were measured. Physiological modification using ampicillin was not stable, but chemical modification was stabel. Hydrocarbon degrading potential was measured for modified and unmodifed HDB.

• 한국지하수토양환경학회:학술대회논문집
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• 한국지하수토양환경학회 2004년도 임시총회 및 추계학술발표회
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• pp.273-276
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• 2004

The adhesion of hydrocarbon degrading bacteria(HDB) differing in surface hydrophobicity was investigated. Cell wall hydrophobicity was modified chemically and physiologically. Modified adhesion deficient mutant of HDB was selected in a soil column assay. Physiologically and chemical modification increased cell surface hydrophobicity. Cell surface characteristics including BATH and FTIR were measured. Physiological modification using ampicillin was not stable, but chemical modification was stable. Hydrocarbon degrading efficiency was measured of TPH modified and unmodifed HDB.

• 조명전기설비학회논문지
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• 제25권6호
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• pp.68-74
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• 2011

The touch or step voltages which exist in the vicinity of a grounding electrode are closely related to the earth structure and resistivity and the ground current. The grounding design approach is required to determine the grounding electrode location where the hazardous voltages are minimized. In this paper, in order to propose a method of mitigating the electric shock hazards caused by the ground surface potential rise in the vicinity of a counterpoise, the hazards relevant to touch voltage were evaluated as a function of the soil resistivity ratio $\rho_2/\rho_1$ for several practical values of two-layer earth structures. The touch voltage and current on the ground surface just above the test electrode are calculated with CDEGS program. As a consequence, it was found that burying a grounding electrode in the soil with low resistivity is effective to reduce the electric shock hazards. In the case that the bottom layer soil where a counterpoise is buried has lower resistivity than the upper layer soil, when the upper layer soil resistivity is increased, the surface potential is slightly raised, but the current through the human body is reduced with increasing the upper layer soil resistivity because of the greater contact resistance between the earth surface and the feet. The electric shock hazard in the vicinity of grounding electrodes is closely related to soil structure and resistivity and are reduced with increasing the ration of the upper layer resistivity to the bottom layer resistivity in two-layer soil.

• 한국환경과학회지
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• 제17권5호
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• pp.573-580
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• 2008

This study aims to measure and to analyze the characteristics of thermal environment of the various permeable pavement materials such as a break stone pavement (Green block cubic), soil protection pavement (Soil tector), soil cement pavement and ceramic brick pavement under the summer outdoor environment. The thermal environment characteristics measured in the study includes the changes of surface temperature during the day, and long and short wave radiation of each pavement surface. The experimental condition is based on the data on the hottest temperature (August 9, 2006, $37.1^{\circ}C$) of the year. The albedo was the highest on the break stone pavement(0.8) from 12:00 to 14:00. The albedo of the ceramic brick pavement, a soil tector pavement and soil cement pavement were 0.35, 0.29 and 0.27 from 12:00 to 14:00, respectively. The peak surface temperature and long wave radiation was the highest on the soil protection pavements($56.6^{\circ}C$/627 W/$m^2$). The peak surface temperatures and long wave radiation on the ceramic brick pavement, a stone brick pavement and soil cement pavement were $51.7^{\circ}C$/627 W/$m^2$, $48.8^{\circ}C$/607 W/$m^2$ and $45.9^{\circ}C$/582 W/$m^2$, respectively. The heat environment was better on the break stone pavement than on the other pavements. This is mainly due to the high albedo of the break stone pavement(0.8) while the albedo value of a ceramic brick pavement, a soil tactor pavement and soil cement pavement were 0.35. 0.29 and 0.27. Large heat capacity($2,629kJ/m^3{\cdot}K$) of the stone brick pavements also contributes to this difference. The heat environment was better on the soil cement pavement than the soil tector pavement. This is mainly due to the evaporation of the soil cement pavement while the active evaporation of the soil tactor pavement was not continued after two days from the rainfall event. To improve the thermal environments in the urban area, it is recommended to raise the albedo of the pavements by brightening the surface color of the pavement materials. Further studies on the pavement materials and the construction methods which can enhance the continuous evapotranspiration from the pavements surface are needed.

• 한국습지학회지
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• 제3권1호
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• pp.61-73
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• 2001

This study was performed to survey the characteristics of surface water and soil in Wangdungjae wetland located at Chiri-Mountain. The results of survey summarized as follows; 1. The physico-chemical characteristics of surface water such as pH, temperature, and DO were in the range of 6.02-6.39, $13.5-24.3^{\circ}C$ and 3.81-9.97 mg/L, respectively. Also, the organic concentrations such as BOD and COD were in the range of 1.3-1.61 mg/L and 3.55-9.97 mg/L, respectively. The water quality of five different sampling sites showed the similar characteristics. 2. The physico- chemical characteristics of soil showed the different properties with the soil sampling depth. According to increasing sampling depth, cation exchange capacity (CEC) and electric conductivity (EC) increased but pH decreased. 3. The future survey and researches on surface water and soil environments are needed to preserve the Wangdungjae wetland at Chiri-mountain marsh.

• 한국환경과학회지
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• 제4권5호
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• pp.41-41
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• 1995

In order to discuss the differences among the SMP(Surface Moisture Availability Parameter), by previous researchers on the basis of their own theoretical and empirical background, we assessed the SMP according to the soil types and volumetric soil water contents. The results are as follows. There are differences among all the five SMAPs. There''s a tendency that the larger grain size, the higher value of parameters. And they divided into two groups for their value: one group has parameters with exponential function and the other with cosine and linear function. The maximum difference between the two groups appears when the volumetric soil water contents are 0.07$m^3m^{-3}$ for sand, 0.l1$m^3m^{-3}$ for loam, 0.12 for clay, and 0.13$m^3m^{-3}$ for silt loam. So, these differences must be considered when we estimate the surface evaporation rate. From field data, the paddy field soil around Junam reservoir is classified as a silt has high wetness, 0.56. So, the parameter obtained from the field measurement is much higher than that of Clapp and Hornberger(1978)''s Table. This study treated the SMP for a certain point of time in winter season. But if we measured the soil water contents continuously, we could obtain better time-dependent parameter.