• 한국환경과학회지
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• 제9권3호
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• pp.241-252
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• 2000

Twenty-two water samples(fifteen groundwater and seven geothermal water samples) were collected to elucidate chemical characteristics of the ground and geothermal waters in the Haeundae hot spring area and its vicinity. Major and honor elements were analyzed for ground and geothermal water samples. The concentrations of $K^+$, Na+$, $Ca^{2+}$, $SO_4^{2-}$, $Cl^-$, ^F^-$ and $SiO_2$ were higher in the geothermal water samples than the groundwater samples except $HCO_3^- and Mg^{2+}$ ions. Based on the contents of Fe, Zn, Cu, Al, Mn and Pb, some of the ground and geothermal water samples are contaminated by anthropogenic sources. The ground waters shown on the Piper diagram belong to $Ca-HCO_3$ type, while the geothermal waters Na-Cl type. The graphs of $Cl^-$ versus $Na^+$, $Ca^{2+}, Mg^{2+}, K^+, SO_4^{2-} and HCO_3^-$ indicate that the groundwater is related partly with mineral-water reaction and partly with anthropogenic contamination, while the geothermal water is related with saline water. On the phase stability diagram, groundwater and thermal water mostly fall in the field of stability of kaolinite. This indicates that the ground and geothermal waters proceed with forming kaolinite. Factor and correlation analyses were carried out to simplify the physicochemical data into grouping some factors and to find interaction between them. Based on the Na-K, Na-K-Ca and Na-K-Ca-Mg geothermometers and silica geothermometers, the geothermal reservoir is estimated to have equilibrium temperature between 125${$\mid$circ}C$ and 160${$\mid$circ}C$.

• 한국해안해양공학회지
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• 제19권5호
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• pp.408-417
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• 2007

최근, 해수욕장으로서의 기능 창출 뿐만 아니라 해안공간의 이용 및 개발에 따른 자연해변의 소실을 대체할 수 있는 인공해변이 건설되고 있다. 그리고, 파랑작용에 의한 매립토사의 유출로부터 인공해변을 보호하기 위한 구조물이 필요하며, 일반적으로 호안이 주로 건설된다. 해저지반 상부에 건설되는 호안의 안정성을 위하여 필히 검토되어야 할 사항 중의 하나가 호안 배후의 지하수위 거동이다. 그러나, 비선형파랑과 지하수위의 거동특성이 인공해변의 토사유출 및 구조물의 안정성에 중요한 요소로 작용함에도 불구하고 이에 대한 연구는 거의 수행되지 않았다. 본 연구에서는 비선형파랑과 호안 및 지하수위로 인한 흐름간의 동적 상호작용을 살펴보기 위하여 정수위와 지하수위와의 차이를 고려할 수 있는 수치파동수로를 개발하였다. 개발된 수치파동수로를 이용하여, 지하수위 변화가 호안 주변 지반내의 수리학적 특성에 미치는 영향을 살펴보았고, 지하수위의 변화에 따른 파동장 및 간극수 흐름, 간극수압 및 와도를 수치적으로 재현하였다. 결과로부터 지하수위의 변화에 따른 호안 주변 지반내의 수리학적 특성들이 어떻게 영향을 받는지 알 수 있었다.

• 한국환경농학회지
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• 제21권3호
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• pp.165-171
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• 2002

A study was conducted to investigate the seasonal changes in water quality of watershed in the Agricultural Environment Promotion Zone. Samples collected were 12 GW (ground water), 2 IW (irrigation water), 2 SW (stream water) in An-Dong City, 4 GW, 6 IW, 11 SW in Young-Yang Gun, and sampling was conducted separately during dry and rainy season. In the ground water, EC and ionic species, except pH, were higher than those in stream water, and especially $NO_3-N$ concentration exceeded the limitation of drinking water. Concentration of ions decreased as the sampling depth was far from the soil surface. During a rainy season, the concentrations of $NO_3-N$ and K in the stream water were slightly higher than those during season. COD was lower during dry season in Yong-Yang, while the trend was contrasted to An-Dong. These results suggest that ground water was polluted by fertilization and compost while streamwater was polluted by loss of soil and organic during the rainy season. Principal chemical components related with changing water quality were EC, $NO_3^-$, Ca, Mg, Na, $Cl^-$, $Cl^-$, $SO_4^-$ in ground water, whereas $NH_4-N$, K, Mg, $Cl^-$, $SO_4^-$ in stream water.

• 한국지반환경공학회 논문집
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• 제13권12호
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• pp.17-25
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• 2012

본 논문에서는 TDR 장비를 사용하여 지반특성에 따라 변화하는 유전상수를 측정하였으며, 지반의 함수비 및 밀도와의 상관성을 분석하였다. 또한, 유전상수를 이용한 지중 공동탐사기법의 적용성을 평가하기 위하여 공동의 크기에 따른 유전상수의 변화 정도를 측정하였다. 실험결과 지반의 유전상수는 함수비와 밀도가 증가함에 따라 선형적인 증가 경향을 나타내는 것으로 평가 되었으며, 일정한 관계식으로 표현할 수 있었다. 또한, 지반의 유전상수는 공동의 크기에 따라 일정한 경향을 나타내며 변화하는 것으로 평가되었다. TDR 기법을 사용하여 측정된 유전상수값은 지반의 함수비, 밀도와 일정한 상관관계를 나타내고 있음을 확인하였으며, 지중 공동탐사에 관한 기초자료로서 활용할 수 있을 것으로 판단된다.

• 한국의류학회지
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• 제25권3호
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• pp.617-628
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• 2001

Cotton and silk fabrics dyed with brazilein(Caesalpinia Sappan), berberine (Phellodendron Amurense), and shikonin(Lithospermum Erythrorhizon) were stored in the air, in the water, and under the ground for about one year. The change of the color, the flexibility, and the breaking strength were measured at the intervals of few weeks. The results are as follows; 1. The color of the fabrics changed most extensively in the fabrics that were under the ground, then in the order of the ones that were in the water, and in the air. The color of the fabrics changed to the achromatic color over the time. 2. The flexibility change among the dyes was similar. All the fabrics became stiff under the ground and in the water over the storage time. 3. In general, cotton and silk fabrics dyed with berberine showed better strength retention than the fabrics dyed with other substances. 4. The strength retention of cotton fabrics was high in the order of the fabrics which were in the air, in the water, and under the ground. Only minuscule change occurred in the strength of the cotton fabrics. The strength of the fabrics that were in the water and under the ground decreased remarkably after 30 weeks and 20 weeks respectively. 5. The strength retention of silk fabrics was high in the order of the fabrics which were in the air, under the ground, and in the water. In the air, the strength on silk fabrics decreased rapidly after 30 weeks. In the water, the strength of silk fabrics decreased more rapidly than that of the cotton fabrics. Under the ground, the strength retention of silk was higher than that of cotton.

• 한국태양에너지학회 논문집
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• 제32권5호
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• pp.59-67
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• 2012

In this study,the compact type solar thermal and ground coupled heat pump hybrid system for space heating/cooling and hot water supply has been developed. This hybrid system was installed in Zero Energy Solar House(ZeSH) in KIER for the demonstration. The thermal performance and operational characteristics of this hybrid system were analysed especially. The results are as follows. (1) This hybrid system was designed in order to address the existing disadvantages of solar thermal/ground coupled heat pump system. For this design, all parts except solar collector and ground coupled heat pump were integrated into a single product in a factory. The compact type unit includes two buffer tanks, an expansion tank, pumps, valves, a controller, etc. This system has an advantage of easy installation with simple plumbing work even in narrow space. (2) The thermal charging and discharging time of the buffer tanks and its characteristics by ground coupled heat pump, and heat pump COP according to geo-source temperature and buffer storage temperature have been studied. This system was found to meet well to the heat load without any other auxiliary heating equipment. (3) The operating hours of the ground coupled heat pump as a backup device of solar thermal can be reduced significantly by using solar heat. It was also found that the minimum heating water supply setting temperature and maximum cooling water supply setting temperature make an influence on the heat pump COP. The lower heating water and the higher cooling water temperature, the higher COP. In this respect, the hybrid system's performance can be improved in ZeSH than conventional house.

• 한국지하수토양환경학회지:지하수토양환경
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• 제7권3호
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• pp.45-59
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• 2002

본 연구의 목적은 국가 지하수 관측망 자료를 활용하여 우리나라 지하수위 변동 곡선의 유형을 구분하고, 각 유형별 함양률을 평가하여 지하수 함양률의 공간적 변동성을 규명하는 데 있다. 전국 지하수의 수위 변동 곡선을 구분하기 위하여 요인 분석 방법을 사용했으며 그 결과 총 5 개의 유형으로 구분하였다. 유형별 함양률은 95.44%의 신뢰도 수준에서 6.2 %(유형 I), 4.1 %(유형 II), 9.2 %(유형 III), 5.8 %(유형 IV), 15.3 %(유형 V)로 추정되었으며 한 유형에서도 관측 지점별로 약 6 %의 변화폭을 보였다. 지하수위 변동 곡선법을 이용하여 유역별로 지하수 함양률을 평가한 결과 한강과 금강 유역에서는 각각 강수량 대비 10.0 %, 8.3 %의 함양률을 보였고, 낙동강 및 영산강·섬진강 유역에서는 각각 6.1 %, 6.6 %의 함양률을 보였으며 기저유출법에 의해서 유역별로 함양률을 추정한 연구의 결과와 유사하게 나타났다 따라서 본 연구를 통하여 지하수 함양률이 수위 변동 곡선의 유형별 혹은 유역별로 변동성을 가짐을 규명할 수 있었다.

• 한국지하수토양환경학회:학술대회논문집
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• 한국지하수토양환경학회 2003년도 International Symposium
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• pp.70-86
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• 2003

Despite its usability, TCE has been managed as a hazardous material due to the toxicity and many contamination cases were surveyed in some developed countries. U.S.EPA(Kram et al., 2001) suggested DNAPL characterization methods and approaches based on survey experiences at several sites. However, Korea has not the least assessment of contamination and trial of remediation, although there are a lot of doubtable areas where ground water would be contaminated with TCE. In this study, we try to assess the volume and extent of ground water contamination with TCE and delineate the contamination source zones in an industrial area. Ground water in this area flows through fractures and the contaminant TCE has the properties of high volatility, high density and low partitioning to soil material. Thus, we applied a variety of technical approaches to identify the contamination status; documentary, hydrogeochemical, hydrogeological and geological surveys. In addition, additional survey was performed based on the interim findings, which showed that ground water contamination was limited to the relatively small area with high concentrations to the deep place. The contamination source zone is estimated to be the asphalt test institute where a great deal of TCE has been used to analyze the amount of asphalt soluble in TCE since 1984. Based on the contamination characterization and a myriad of documents about ground water remediation, appropriate site remediation management options will be recommended later. This study is now under way and this paper was focused on describing the technical approaches used to achieve the goals of this study.

• 한국환경농학회지
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• 제18권2호
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• pp.148-153
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• 1999

경기도내 농업용 지하수 수질의 현황을 파악하여 영농의 기초자료로 활용하고자 용인시, 평택시, 화성군 및 수원시 등 4개 지역의 시설하우스 53개 지점에서 사용하는 지하수 수질을 1998년에 연 3회에 걸쳐 조사한 결과는 다음과 같다. 1. 지하수중의 EC, COD, $NH_4-N$, $PO_4$ 및 Cl등의 농도는 각 지점 모두 농작물 생육에는 지장이 없는 안전한 수준이었다. 2. 질산성질소의 경우 지역적 차이는 평택>용인>화성>수원 순이었으며, 특히 평택의 경우 연평균 26.89mg/l로 지하수법에서 정하고 있는 농업용수의 수질기준 20mg/l을 상회하는 것으로 나타났고, 조사시기별 농도변화는 큰 차이가 없었다. 평택의 조사대상지처럼 오염된 지하수를 이용하여 작물을 재배할 때는 물관리와 시비 관리에 세심한 주의를 기울여야 할 것으로 판단된다. 3. 중금속의 경우 대부분의 지역에서 미량 검출되어 큰 문제가 없는 것으로 나타났으며, 일부의 조사대상 지점에서는 일시적으로 중금속이 다량 검출되는 경우도 있었다.

• 기술사
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• 제10권2호
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• pp.13-26
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• 1977

The Kum-Ho river basin is one of the densely populated area having more than 35% of the total population and it was also well irrigated since ealier days in the Nackdong River Basin Most of the easily developed source of surface water are fully utilized, and at this moment the basin is at the stage that no more surface water can be made available under the present rapid development of economic condition. Since surface water supplies from the basin have become more difficult to obtain, the ground water resources must be thoroughly investigated and utilized greatly hereafter. In economic ground of the basin what part could ground water play\ulcorner In what quantities and, for what uses could it be put\ulcorner The answer to these questions can be relatively simple; the ground water resources in the basin can be put at almost any desired use and almost anywhere in the basin. The area of the basin is at about 2088km$^2$ in the middle part of Nackdong River Basin and it is located along the Seoul-Pusan Express Highway. The mean annual rainfall is about 974.7m/m, most of which falls from June to September during the monsoon. Accumulated wet period is appeared approximately after every 8 year's accumulated dry-period with the duration of 5 years. The water bearing formations in the basin include unconsolidated alluvial deposits in Age of Quatenary, saprolite derived from weathered crystalline rocks, Kyongsang sedimentary formations of the period from late Jurassic to Cretaceouse, and igneouse rocks ranging of the Age from Mesozoic to Cenozoic. The most productive ground water reservoir in the basin is calcareouse shale and sandstones of Kyongsan system, which occupies about 66% of the total area.