• 콘크리트학회논문집
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• 제13권2호
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• pp.175-183
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• 2001

국내에서 생산되는 5종류 시멘트로 제조한 시멘트 경화체의 해수침식에 대한 저항성을 알아보기 위한 목적으로 2배농도 인공 해수에 각각 400일 및 800일동안 침지시켜 모르타르의 압축강도 및 길이변화를 측정한 결과, 혼합시멘트계 모르타르가 광물질혼 화재의 영향으로 포틀랜드시멘트계 모르타르와 비교하여 좋은 결과를 나타내었다. 또한 시멘트 페이스트의 XRD분석에 의한 수 화 및 반응생성물의 피크강도비를 살펴보면, 포틀랜드시멘트계 페이스트 중 저열포틀랜드시멘트의 피크강도비가 가장 작았으며, 혼합시멘트계 페이스트의 경우 portlandite 및 brucite의 피크강도비가 포틀랜드시멘트계 페이스트보다 작았다. 인공해수 침식으 로 인한 시멘트 페이스트의 공극량을 수은압입법으로 측정한 결과에 의하면 보통포틀랜드시멘트 페이스트의 총공극량이 가장 크게 나타났으나, 포틀랜드시멘트에 고로슬래그미분말 및 플라이애시를 혼합한 혼합시멘트계 페이스트의 경우 총공극량이 각각 약 56% 및 약 32 % 정도 저감되는 효과가 있었다.

• 한국터널지하공간학회 논문집
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• 제23권6호
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• pp.451-468
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• 2021

터널 굴진면 전방 위험 지반 예측은 TBM (Tunnel Boring Machine) 굴진 성능 및 안정성 확보에 필수적이다. 국내·외에서 굴진면 전방 예측을 위한 전기비저항 탐사법에 대한 연구가 다수 이루어졌으나, TBM 터널 굴진을 고려한 전기비저항 탐사의 실내 실험 모사가 어렵기에 이와 관련된 실험 연구가 매우 부족한 실정이다. 따라서 본 연구에서는 전기비저항 탐사법의 터널 전방 위험 지반 예측 적용성을 분석하기 위한 TBM 굴진을 모사한 실내 축소 모형 실험을 수행하였다. 터널 굴진면 전방의 단층 파쇄대, 해수 침수대, 토사-암반 변화구간, 암반-토사 변화구간을 축소 모사하여, 굴진 중 전기비저항의 변화를 측정하였다. 본 연구에서는 실제 시공 조건을 재현하기 위해 화강암 블록을 사용하여 모형 지반을 모사하였다. 실험 결과, 터널이 굴진하면서 단층 파쇄대에 근접할수록 전기비저항이 감소하였으며, 해수 침수대도 동일한 경향을 보였으나, 단층 파쇄대와 비교하여 측정된 전기비저항이 크게 감소하였다. 토사-암반 변화구간의 경우, 전기비저항이 상대적으로 높은 암반에 터널 굴진면이 다가갈수록 전기비저항이 증가하는 양상을 보였다. 이와 반대로 암반-토사 변화구간의 경우, 전기비저항이 낮은 토사 지반에 굴진면이 근접할수록 전기비저항이 감소하였다. 실험 결과를 통해 전기비저항 탐사 굴진면 전방 위험 지반(단층 파쇄대, 해수 침수대, 토사-암반 변화구간, 암반-토사 변화구간)의 예측이 가능하다고 판단된다.

• 한국지구물리탐사학회:학술대회논문집
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• 한국지구물리탐사학회 2011년도 학술대회 및 정기총회
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• pp.103-104
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• 2011

• 한국지구물리탐사학회:학술대회논문집
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• 한국지구물리탐사학회 2003년도 Proceedings of the international symposium on the fusion technology
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• pp.455-458
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• 2003

A combination of drilling, hydrogeochemical survey, geophysical survey and the numerical modelling for the flow and transport of groundwater was performed to evaluate the seawater intrusion in Baeksu-eup, Yeonggwang-gun, Korea. The survey area extends to over 24 $km^2$. Twelve wells were also drilled for the collection of geologic, geochemical, hydrologic, and geophysical logging data to delineate the degree and vertical extent of seawater intrusion. To evaluate and map the salinity in a coastal aquifer, geophysical data and hydrogeochemical results were used. Layer parameters derived from VES data, various in situ physical properties from geophysical well loggings, and the estimated equivalent NaCl concentration were used as the useful input parameters for the numerical simulation with density-dependent flow. Our multidisciplinary approach for evaluating the seawater intrusion can be considered as a valuable attempt to enhancing the utilization of various data and the reliability of numerical ground modelling.

• 대한지하수환경학회지
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• 제4권1호
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• pp.5-13
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• 1997

제주도는 예상되는 물 부족분을 충당하기 위하여 대규모 지하수 개발을 계획하고 있다. 효율적인 지하수 자원의 관리를 위해서는 개발에 대한 영향평가가 선행되어야 하는데 제주도에서는 지역의 특성상 해수의 영향을 고려해야 한다. 본 연구에서는 가상의 지하수 개발에 대한 중-동제주 수역의 해수쐐기의반응을 해석하였다. 해석 방법으로는 담수와 해수의 동수역학을 동시에 고려하는 비확산 전산모형(sharp interface numerical model)을 이용하였다. 모델링에서 사용된 단계적 지하수 개발 일정은 제주도 광역상수도개발 계획과 동일한 비율과 시간 간격에 따라 설정되었다. 모델링 결과 해수쐐기(saltwater wedge)는 지역에 따라 1km이상 침투하는 것으로 예측되었다. 이러한 결과는 해수쐐기를 고정된 것으로 가정하여 담수의 흐름만을 고려한 모델링을 바탕으로 한 영향평가의 신뢰성에 의문을 가지게 한다.

• 한국지반환경공학회 논문집
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• 제21권11호
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• pp.11-20
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• 2020

연약지반 차수 및 보강용 그라우트에 대하여 다양한 양생조건에서 초기 및 장기재령에 걸쳐 내구성에 대한 검토를 수행하였다. 그라우트는 물유리계, 급결광물계 및 아크릴고분자계를 대상으로 하였으며, 양생조건은 수도수(청수) 양생, 인공해수 양생 및 대기 양생으로 하고, 시험은 재령별 일축압축강도와 길이변화량 및 중량변화량에 대하여 수행하였다. 인공해수는 MgCl₂와 MgSO₄ 수용액을 각각 제조하여 사용하였다. 급결광물계와 아크릴고분자계는 수도수와 인공해수에서는 내구성에 큰 변화가 없이 안정적으로 양생되는 반면 물유리의 경우 수도수에 비해 인공해수조건에서 매우 급격한 내구성 저하가 발생되었다. 대기 양생조건에서는 모든 경우에서 수도수 양생에 비해 내구성이 저하되는데, 특히 급결광물계와 물유리계에서 중량감소가 각각 약 62% 및 60%로 큰 내구성 저하가 발생되었다.

• 한국지하수토양환경학회:학술대회논문집
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• 한국지하수토양환경학회 2000년도 추계학술대회
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• pp.232-236
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• 2000

Multi-regression statistical analyses were applied for the water quality data of shallow alluvial ground water (n = 47) collected from the Youngdeok area, in order to quantitatively generalize the natural (non-anthropogenic) causes of regional water quality variation. Seven samples having the high contamination index ( $C_{a}$ > 3) reflect the striong effects by anthropogenic activity. Most of the alluvial groundwaters have acquired their quality primarily due to the dissolution of carbonate minerals. The results of multi-regression analysis show that chlorine is mainly derived from seawater effect. Sulfur isotopic compositions of dissolved sulfur and the S $O_4$/Cl ratio also enable us to discriminate the samples (n = 18) which are affected by atmospheric input of marine aerosol (sea-spray) and also by mixing between freshwater and seawater. Hydrogen and oxygen isotope data of the samples collected lie close to the local meteoric water line obtained from nearby Pohang city but has lower slope (5.45) on the $\delta$D-$^{18}$ O plot, indicating that alluvial groundwater was recharged from infiltrated meteoric water which has undergone some degree of kinetic evaporation. The estimated initial isotopic composition of the recharged water ($\delta$D = -74.8$^{0}$ /$_{00}$, $\delta$$^{18}$ O = -10.8$^{[-1000]}$ /$_{[-1000]}$ ) suggests that the alluvial ground water recharge largely occurs during summer storm events.s.s.

• 한국농공학회지
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• 제8권1호
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• pp.1055-1063
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• 1966

Ground water hydrology may be defined as the science of the occnrrence, distribution, and movement of water below the surface of the earth. Geohydrology has an identical connotation, and hydrogeology differs only by its greater emphasis on geology. Ground water referred to with out further specification is commonly understood to mean water occupying all the voids with in a geologic stratum. This saturated zone is tobe distinguished from an unsaturated, or aeration zone where voids are filled \yith water and air. Water contained in saturate:! zones is important for engineering works, geologic studies, and water supply developements Conseqently, the occurrence of water in these zones will be emphasized here. Un-saturated zones are usualiy found above saturated zones and extending upward to the ground surface. Because this water includes soil moisture with in the root zone, it is a major concern of agricultlre, botmy and soil science. No rigid demarcation of waters, between the two zones is possible, for they possess an iriterdependent boundary and water can move from zone to zone in either science, including eology, hydrology, meteorology, and oceanography are concerned with earths water, but ground water hydrology may be regarded as a specialized science combining elements of geology, hydrology, and fluid mechanics. Geology governs the occurrence and distribution of ground water, hydrology determines the supply of water to the ground, and fluid mechanics explains its movement. To provide maximum development of grofnd water resources. for benefical use requires thinking in terms of an entire ground water basin. In order to inorease the natural supply of ground water, man has attempted to artifially recharge ground water basins. Coastal aquifers come in contact with the ocean at seawater of the coastline. Fresh ground water is discharged in to the ocean. the seaward flow of ground water has been decreased or even reversed, Sea water penettating in land in aquifer.

• Fisheries and Aquatic Sciences
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• 제21권1호
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• pp.1.1-1.12
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• 2018

Pacific bluefin tuna (Thunnus orientalis) is one of the commercially important species in Korea as well as other countries of the North Pacific. Korean offshore large purse seine fisheries targeting small pelagic fishes such as chub mackerel have caught T. orientalis temporarily in the east of Jeju Island. The catch of T. orientalis in March through June occupied approximately 60% of the total. The monthly catch around Jeju Island from 2004 to 2013 showed a negative correlation (r = - 0.755, p < 0.01) with the seawater temperature at 50 m and had a significant positive correlation (r = 0.856, p < 0.01) with the Pacific Decadal Oscillation Index (PDOI). The highest catch and catch per unit effort (CPUE) of T. orientalis around Jeju Island occurred either when the seawater temperature ranged between 15 and $16^{\circ}C$ at 50 m or when the catch was taken near the frontal area where two water masses from offshore and coastal areas collide. The length of T. orientalis caught around Jeju Island from 2004 to 2013 ranged from 19 to 193 cm in fork length (FL). The time series of the monthly mean FL of T. orientalis had a negative correlation (r = - 0.592, p < 0.01) with the seawater temperature at 50 m and had a significant positive correlation (r = 0.668, p < 0.05) with PDOI.

• 한국수산과학회지
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• 제45권3호
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• pp.262-270
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• 2012

Seaweeds provide habitats in which marine animals can spawn and develop, and serve as a food supply for algaegrazing species such as sea urchins and abalone. Recently, seaweed species have disappeared from coastal ecosystems, leaving barren ground, defined as habitats that have lost their algae forests and where coralline algae containing calcium carbonate components have become encrusted on rocks. The biological causes of barren ground include grazing by herbivores and excessive seaweed harvest. The environmental harm caused by the spread of barren ground includes accelerated eutrophication following the reduction in seaweed, which plays an important role in oceanic purification. In the present study, we identified the relationships between various seaweed species and the occurrence of barren ground. Subtidal benthic macroalgal flora and community structure were observed seasonally on barren ground along vertical transects of rocky shores of Bihwa, Samchuck, and the east coast of Korea from February to November 2006. Fifty-eight seaweed species were identified, including 7 green, 15 brown, and 36 red algae species. There were between 6 and 28 species among seasons. Over the whole study period, average seaweed biomass (g wet wt $m^{-2}$) was 241.90 g, with a seasonal range of 25.26 to 760.34 g. Seaweed biomass declined with increasing seawater depth and ranged between 91.26 and 422.08 g. The vertical distribution of algae was characterized by Undaria pinnatifida and Sargassum honeri at 5 m, S. honeri and U. pinnatifida at 10 m, and U. pinnatifida and Agarum clathratum at 15 m depth. Seasonal patterns in community indices were not found. Community indices showed different patterns along vertical shoreline gradients; the dominance index increased but the richness, evenness, and diversity indices decreased with seawater depth. Sea urchin density was 8 to 24 individ. $m^{-2}$ in Bihwa. These urchin populations had significantly aggregated spatial patterns and recurrent destructive grazing appeared to be occurring.