• 암석학회지
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• 제7권2호
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• pp.77-97
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• 1998

경상분지 북부에 위치한 온정리 화강암의 암석화학적, 동위원소 지구화학적 특징으로부터 암체의 성인과 기원물질의 특징 등을 고찰하였다. 온정리 화강암의 연대에 대해 선백악기, 또는 백악기라는 상반된 견해가 있었으나 야외지질학적인 특징과 K-Ar 자료로 볼 때 백악기 말(87 Ma 내외)로 판단된다. 각섬석 지압계를 적용시켜 보았을 때 온정리 화강암의 정치 압력은 2 kbar 이하로 계산된다. 온정리 화강암의 암석화학적, 동위원소적 특징은 비교적 미 성숙된 호 환경에서 생성되었음을 지시한다. 온정리 화강암의 $SiO_2$ 함량과 $^{87}Sr/^{86}Sr$ 초기치는 부(-)의 직선관계를 잘 보이며 $^{207}Pb/^{204}Pb$ 초기치는 정(+)의 상관관계를 보여 두 단성분 사이의 불완전한 혼합, 또는 동화작용의 가능성을 지시한다. 그러나 현재 노출되어 있는 암체 중 오염체로 고려할 만한 단성분을 찾기는 어려우며 따라서 혼합이나 동화 작용을 일으킨 오염체가 하부지각에 위치할 가능성이 높다. 경상분지 내에 분포하는 백악기-제 3기 화강암의 연대와 지화학적, 동위원소적 특징을 정리하고 온정리 화강암의 특징과 비교해 보면 다음과 같은 결론이 얻어진다. 1) 화강암류의 연대는 특정 시기에 집중되는 경향성을 보여 경상 분지에서의 백악기 이후 화성 활동이 불연속적인 사건에 의해 일어났을 가능성이 높다. 2) 화강암류는 젊은(9억년 이내) 하부지각에서 유래되었으며 그 동위원소적 특징은 기원물질의 불균질성을 반영한다고 보아진다. 전반적으로 경상분지 화강암류의 동위원소적 특징과 화학조성은 상부지각 혼염에 의해 조화적으로 설명되지 않는다. 3) 경상분지 화강암류의 암상과 연대, 그리고 동위원소적 특징은 서남 일본 산인 벨트에 분포하는 화강암의 특징과 잘 일치한다. 4) 온정리 화강암의 Sr-Nd 동위원소비는 경상분지와 서남일본 내대에 분포하는 백악기 이후 암체 중 비교적 초생적인 영역에 해당된다.

• 한국환경과학회지
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• 제7권6호
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• pp.793-801
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• 1998

In this study, the Dilution Method is used to measure river discharge through the hydraulic model test. the dilution method is divided into Constant-Rate-Infection Method and Slug-Injection Method in the river discharge measurement techniques. When the dilution method is applied in the hydraulic model flume, it is analyzed that the estimated error of constant-rate-injection method is less than that of the slug-in-jection method, and the result shows that floodflow analysis is more efficient than lowflow analysis as compared observed discharge with calculated discharge. The result of statistical error analysis shows that the constant-rate-injection method is appropriate technique for the measurement of the river discharge. Therefore, the dilution method among the river discharge measurement techniques can be applied for the river basin which can't be measured with current meter or unsteady-flow regime in the urban-small drainage or hydraulic structure equipment area and can be obtained more exact results than any other discharge measurement techniques.

• 상하수도학회지
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• 제26권3호
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• pp.423-430
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• 2012

This study was conducted to qualify the equality of the flow distribution from open channel between rapid mixing basin and flocculation basins in a domestic S_ water treatment plant, and to suggest a remedy for improving the equality. In order to evaluate the feasibility of the suggested remedy, computational fluid dynamics (CFD) technique are used, and for verifying the CFD simulation results tracer tests were carried out. From the results of CFD simulation and tracer tests, it was investigated that the modification of hydraulic structure in the distribution channel, which is to install the longitudinal orifice baffle in flow direction, could improve the equality of the flow distribution over 75%.

• 한국환경과학회지
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• 제18권4호
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• pp.473-478
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• 2009

The removal characteristics of total petroleum hydrocarbons (TPHs) and heavy metals in contaminated soils with ultrasonic washing have been studied. The ultrasonic washing was evaluated on a laboratory scale. In this investigation, the effects of factors such as ultrasonic frequency, power intensity, duration of irradiation, contents of the TPHs and heavy metals and mixing ratios between the contaminated soils and water, were considered. Experimental results suggested that the rates for contaminant extraction of the TPHs and heavy metals in the contaminated soil increased considerably with the ultrasonic washing. Therefore, the ultrasonic washing has previously been to be an effective method to remediate the contaminated soils with the TPHs and heavy metals.

• 유체기계공업학회:학술대회논문집
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• 유체기계공업학회 2005년도 연구개발 발표회 논문집
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• pp.273-277
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• 2005

The large particles of suspended matter in raw water can be removed by allowing them to settle out in a presedimentation basin. But there are smaller particles in almost all surface water and some groundwater that will not settle out within a reasonable time without some help to accelerate the process, In the coagulation and flocculation processes, nonsettleable solids are converted into large and heavier settleable solids by physical-chemical changes broght about by adding and mixing coagulant chemicals into the raw water. The object of this research was to improve corrective injection method for low dissolution liquid in the water treatment plant. A sort of chemical feed equipment are diaphram pump, flow control in combined magnetic flowmeter md control valve, roto dipper wheel system and tube pump. Particularly low dissolution liquid (Calcium Hydroxide) put in a bit by feed equipment, tube pump is very useful method for corrective injection method in the water treatment plant.

• 한국해양학회지:바다
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• 제3권4호
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• pp.175-182
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• 1998

동해의 울릉분지 표층에서 1996년 9월 초부터 11월 사이에 염분$^*$ 32 이하의 저염 해수가 출현했음이 최근 학계에 보고되었으며, 이 해수의 기원으로 여름철에 제주도 부근까지 세력을 확장하는 장강 유출수가 지목되었다. 대한해협의 서수로를 통과하는 해수가 두 단성분(장강 회석수와 쿠로시오 해수) 간의 단순한 혼합에 의한다는 가정하에 $^{228}Ra/^{226}Ra$ 방사능 비를 보존적 추적자로 활용하여, 두 수괴가 대한해협 서수로를 통과하는 표층수를 형성하는데 얼마나 기여하는가를 산정하였다. 알려진 두 단성분의 $^{228}Ra$, $^{226}Ra$ 방사능 측정값과 대한해협 서수로에서 측정한 $^{228}Ra/^{226}Ra$ 방사능 비로써 계산한 결과, 장강 희석수는 평균 염분이 32.17이었던 1996년 9월에 대한해협 서수로 표층수의 $58{\pm}3%$ 그리고 평균 염분이 34.53이었던 1997년 2월에는 $10{\pm}3%$ 기여하였던 것으로 나타났다. 이것은 제한된 자료와 매우 단순한 모델로부터 얻은 결과이지만 장강 유출수가 동해 내부에까지 영향을 주고 있음을 지시하며, 현재 장강 수계에 건설중인 삼협댐이 완공되면 장강 희석수 자체의 변화로 인해 북부 동중국해와 울릉분지 부근에 걸쳐 수십년 시간 규모의 해양 환경 변화가 일어날 것으로 판단된다.

• 자원환경지질
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• 제30권1호
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• pp.1-14
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• 1997

The shales from the Euiseong area are interbedded along the bedding in Cretaceous Gyeongsang Supergroup, which are composed mainly of quartz, plagioclase, K-feldspar and associated with trace amount of biotite, muscovite, chlorite, pyrite, hematite, carbonate and clay minerals. The ratio of $Al_2O_3/Na_2O$ and $K_2O/Na_2O$ in shales from the Shindong Group are ranged from 9.16 to 24.32 and from 1.70 to 5.97, and the Hayang Group ranged from 2.76 to 8.89 and from 0.42 to 2.74, which are negative correlated between $K_2O/Na_2O$ and $Al_2O_3/Na_2O$ against $SiO_2/Al_2O_3$ respectively. Those are suggested that controlled of mineral compositions in shales due to substitution and migration of elements by sedimentation and diagenesis. These shale formation were deposited in basin of terrestrial environments originated from the igneous rocks, and the REE of these rocks are not influenced with diagenesis and hydrothermal alterations on the basis of $Al_2O_3$ versus La, La against Ce, Zr versus Yb, the ratios of La/Ce (0.43 to 0.62) and Th/U (1.11 to 10.71). The narrow range in trace and REE element characteristics as Co/Th (0.63 to 1.92), La/Sc (1.98 to 5.90), Sc/Th (0.58 to 1.30), V/Ni (0.90 to 3.25), Cr/V (0.45 to 1.78), Ni/Co (1.88 to 6.67) and Zr/Hf (30.04~60.87) of these shales argues for inefficient mixing of the simple source lithologies during sedimentation. These rocks also show much variation in $La_N/Yb_N$ (6.90 to 17.02), Th/Yb (4.17 to 13.68) and La/Th (1.98 to 5.90), and their origin is explained by derivation from a mixture of intermediate to acidic igneous rocks.

• 한국물환경학회지
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• 제23권6호
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• pp.889-896
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• 2007

From the direct outflow of Chungju Dam to the junction of water body and watershed in Paldang lake is the scope of this research. This study performed to investigate the main cause of water quality deterioration and the influenced region in the middle field range of the Namhan river Basin with the onsite measurement of water quality and flow rate simultaneously during spring dry season. The purpose of this study is to find out the time-spatial variation characteristics of water quality and flow rate. Following the flow direction $BOD_5$ and $COD_{Mn}$ concentration increased to the highest value of 3.7 mg/L, 5.9 mg/L at Wolgesa respectively. Chl.a concentration increased to $50mg/m^3$ or so at Kangsang, after that it decreased to $37mg/m^3$ at the junction of Paldang lake. Organic matter concentration variation trend showed similar than that of Chl.a. Also $BOD_5$ concentration tendency was similar to Chl.a in every measuring sites except Paldang lake mixing zone. The major factors of water quality deterioration in Namhan river and Paldang lake during dry season were algal bloom and followed internal production. High phosphorus load from Dalcheon and Seom river caused dry season algal bloom and internal production in transitional zone which was stagnant area in downstream of Namhan river.

• 상하수도학회지
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• 제21권3호
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• pp.341-348
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• 2007

The efficiency of powdered activated carbon (PAC) for removing taste and odor (T&O) in drinking water supplies is dependent on the contact time, quality of mixing, and the presence of competing compounds. All of these are strongly influenced by the stage in the treatment process at which the PAC is added. In conventional water treatment plants (WTPs), PAC is commonly added into the rapid mixing basin where chemicals such as coagulants, alkaline chemicals, and chlorine, are simultaneously applied. In order to prevent interference between PAC and other water treatment chemicals, alternative locations for addition of PAC, such as at transmission pipe in the water intake tower or into a separated PAC contactor, were investigated. Whatever the location, addition of PAC apart from other water treatment chemicals was more effective for geosmin removal than simultaneous addition. Among several combinations, the sequence 'chlorine-PAC-coagulant' produced the best result with respect to geosmin removal efficiency. Consequently, when PAC has to be applied to cope with T&O problems in conventional WTPs, it is very important to prevent interference with other water treatment chemicals, such as chlorine and coagulant. Adequate contact time should also be given for adsorption of the T&O compounds onto the PAC. To satisfy these conditions, installation of a separated PAC contactor would be the superior alternative if there is space available in the WTP. If necessary, PAC could be added at transmission pipe in the water intake tower and still provide some benefit for T&O treatment.

• 대한토목학회논문집
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• 제36권2호
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• pp.219-229
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• 2016

본 연구에서는 저수지의 붕괴로 인한 하류부 하천의 하상변동에 대한 해석을 수행하였다. 저수지 붕괴에 따른 1차원 비평형, 비균일 유사의 이송과 하상 변동을 연구를 위해 CCHE1D 모형을 이용하였다. CCHE1D 모형은 비평형 및 비균일 유사해석을 위해 조정거리와 분류된 입자의 입경을 사용하며, 하상 물질의 교환을 위한 혼합층의 개념이 사용된다. CCHE1D 모형을 1996년 저수지 붕괴가 발생한 Ha!Ha!강 유역에 적용하여 저수지 붕괴로 인한 하류부의 비평형, 비균일 유사이송을 해석하고, 계산 결과를 저수지 붕괴전 후에 하류부 실측 하상과 비교하였다. 또한, 조정계수($L_{s,b}$), 비평형 계수(${\alpha}_s$), 혼합층 두께(${\delta}_m$), 공극률(p')을 포함하는 주요 매개변수에 대한 민감도를 분석하였으며, 대상유역에서는 비평형 계수가 하상변동에 가장 큰 영향을 주는 것으로 나타났다.