• 태양에너지
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• 제5권2호
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• pp.20-27
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• 1985

The aims of this study is to examine closely the temperature distribution of the solar pond for conditions of Seoul area climate and to prove capability of the solar pond utilization in Seoul area. In this study the equations for the convecting zone temperature of the solar pond were derived from Rabl and Nielsen's model. As the result of computer simulation, it was found that the average temperature of convecting zone is over $100^{\circ}C$ under conditions which is no output and 120cm depth or over of the insulating layer. Consequently if solar pond is constructed in Seoul area, it is a effective heat storage system.

• Journal of Advanced Marine Engineering and Technology
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• 제40권4호
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• pp.264-269
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• 2016

본 논문은 단열층을 가지는 솔라폰드의 온도특성을 알아보기 위한 기초 연구이다. 또한, 기존의 단열층을 가지지 않는 경우의 솔라폰드의 온도특성과 비교하였다. 수치해석법은 유한차분법(Finite-Difference Method)를 이용하였으며, 2차원 비정상의 상태를 가정하여 계산하였다. 수치해석을 통해 다음과 같은 결과를 얻었다. 1) 솔라 폰드의 깊이가 깊어지면 폰드의 하부까지 도달하는 일사량이 줄어들기 때문에 온도 상승 효과는 발생하지 않는 것을 확인했다. 2) 동절기에는 토양의 온도가 솔라 폰드 내 물의 온도보다 상대적으로 높아 토양에서 폰드 내로 열이 전달되는 것을 확인할 수 있었다. 3) 단열층을 가지는 솔라폰드의 경우, 태양의 의존율은 83.3%, 보일러의 의존율은 16.7%로 자연에너지의 의존도가 높은 것을 확인할 수 있었다.

• 태양에너지
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• 제7권2호
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• pp.22-29
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• 1987

This paper dealed with thickness variation of bottom heat sotrage zone due to salinity and flow rate of extration hot brine in small test solar pond (0.5m wide, 0.5m high, 1.0m long). Testing apparatus and situation were follows: 7.1 cm of height of suction diffuser and 1.8cm of height of discharge diffuser above the test pond respectively, 0.3cm of slot size of suction diffuser, 1.0cm of slot size of discharge diffuser, 47cm of length of the slot; heating of hot water ($75^{\circ}C$) through separated hot water tank, discharge of the brine into storage zone through discharge diffuser, the extration of the brine through suction diffuser, circulation of the extracted brine through a heat exchanger (cooler). Following results were obtained through the experiments. 1. In small test solar pond, the typical three zone which showed up in real solar pond were established. 2. Richardson Number was used more effectively to confirm hydrodynamic stability of the stratified flow. 3. The thickness of non convective layer had a great effect on the heat storage of the bottom convective layer, then the temperature of bottom convective layer had a relation to that of upper convective layer. 4. Optimum operating condition in the test pond was on 10%-15% of salt concentration and $0.05m^3/hr$ of flow rate of extraction hot brine. 5. Following thickness of 3 zones were available to obtain under optimum operation condition: o bottom storage zone: $30%{\pm}10%$ of total pond depth o non-convective zone: $40%{\pm}10%$ of total pond depth o Upper surface zone: $20%{\pm}10%$ of total pond depth.

• 대한기계학회논문집
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• 제11권2호
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• pp.304-313
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• 1987

본 논문에서는 하부가열식 실험용 태양연못을 제작하여 열유속과 초기의 소금 농도구배를 변화시켜 가면서 실험을 수행하였다.실험을 통하여 측정한 각 층안의 온도와 소금농도구배 및 하부혼합층의 성장율 등을 바탕으로 지배방정식과 가정을 세 운뒤 이들 방정식을 풀어 실험테이터와 비교하였다.

• 태양에너지
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• 제9권1호
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• pp.30-35
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• 1989

This paper dealt with an experiments on temperature vairation in the heat storage zone due to change of vertical location (height) of sink diffuser and flow extraction in small saltless solar pond ($0.5{\times}0.5{\times}1.0M$), and the honeycomb device for this experimental purpose consisted of one-tired, sealed, and air filled by honeycomb panels. As results of experiments, 1) The storage zone was formed under lower region below the honeycomb device. 2) The higher vertical location of sink diffuser was placed, the more mixing phenomenon increased in the pond at steady flow extraction. 3) The more flow extraction increased, the more mixing phenomenon decreased at constant heat exchanger and variable flow extraction.

• Journal of Plant Biology
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• 제25권3호
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• pp.123-133
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• 1982

The tropic structure and the function of a small pone ecosystem under the tree stand were studied in terms of energy flow. About 28% of total solar radiation was intercepted by the tree canopy over the pond. Primary producers converted 1.1%(3,382 kcal$\cdot$$m^{-2}$$\cdot$$y^{-1}$) of solar radiation (320,000 kcal$\cdot$$m^{-2}$$\cdot$$y^{-1}$) into gross primary production. The amount of energy availble to the pond snail was 1,683 kcal.m-2.y-1 of the net production by primary producers and 1,033 kcal$\cdot$$m^{-2}$$\cdot$$y^{-1}$ of the litter fallen into the pond. The amount of gross secondary production by the pond snail was 245 kcal$\cdot$$m^{-2}$$\cdot$$y^{-1}$. Judging from these, supply of both net primary production and the litter was indispensable for the maintenance of the pond ecosystem. The total amont of energy as gross primary production plus litter was 4,415 kcal$\cdot$$m^{-2}$$\cdot$$y^{-1}$(100%). Since the total respiration loss was calculated to be 1,917 kcal$\cdot$$m^{-2}$$\cdot$$y^{-1}$(43.4%), the rate of energy accumulation in the pond estimated to 56.6%.

• 태양에너지
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• 제5권2호
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• pp.11-19
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• 1985

In this paper, the interface stability not to occur mixing and entrainment between the adjacent layers has been studied in the case of the selective withdrawal of a stratum and the injection in stratified fluid formed by the density difference in a small solar pond. There are stability parameter, Richardson number, Rayleigh number and Froude number as the parameters governing stability in order to measure the interface stability on the stratified fluid. The model which could measure the interface stability on the stratified fluid was the small solar pond composed by 1 meters wide, 2 meters high, and 5 meters long. In order to measure the interface stability on the stratified fluid at the inlet port, the middle section and the outlet port, Richardson number, Rayleigh number, and Froude number involved in the parameters governing the stability were calculated by means of the data resulted from the test of the study on hydrodynamic stability between the convective and nonconvective layers in that solar pond. Richardson number written by the ratio of inertia force to buoyancy force can be used in order to measure the stability on the stratified fluid related to the buoyancy force generated from the injection of fluid. Rayleigh number written by the product of Grashof number by Prandtl number can be used in order to measure the stability of the fluid related to the heat flux and diffusivity of viscosity. Froude number written by the ratio of gravity force to inertia force can be used in order to measure the stability of the nonhomogeneous fluid related to the density difference. As the result of calculating the parameters governing stability, the interface stability on the stratified fluid couldn't be identified below the 70cm height from the bottom of the solar pond, but it could be identified above the 70cm height from it at the inlet port, the middle section and the outlet port. When compared with such the three parameters as Richardson number, Rayleigh number, Froude number, the calculated result was in accord with them at inlet port, the middle section and the outlet port. Henceforth, it is learned that even though any of the three parameters is used for the purpose of measuring the interface stability on the stratified fluid, the result will be the same with them. It is concluded that all the use of Richardson number, Rayleigh number, and Froude number, is desirable and infallible to measure the interface stability on the stratified fluid in the case of considering the exist of the fluid flow and the heat flux like the model of the solar pond.

• 대한설비공학회지:설비저널
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• 제16권6호
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• pp.606-612
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• 1987

In this study, numerical model was developed to predict behavior of several layers in a solar pond and was solved by finite difference method. The empirical correlation that described heat and salt fluxes across interfacial boundary layer between mixed layer and diffusive layer in a solar pond were obtained from experiments and utilized in developing numerical model. As the results of this study, heat and salt fluxes across the interfacial boundary layer was found to depend on density ratio ${\beta}{\Delta}M_s/{\alpha}{\Delta}T.$ It was also found that the predicted value obtained by using the modified Weinberger's stability criteria showed a good agreement with experiment data.

• 상하수도학회지
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• 제9권2호
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• pp.108-117
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• 1995

연못시스템의 처리정도는 기후조건(氣候條件)과 아주 밀접한 관계가 있다. 기존시스템이 없는 경우 비슷한 기후권의 사례지역을 반드시 비교분석하게 된다. 미국 온대권에 위치한 Corinne과 Eudora 시스템의 기온과 태양복사량을 김포지역과 비교한 결과 아주 유사함이 규명되었다. 특히 태양복사열의 경우, 여름철에 김포지역이 두 시스템보다 조류성장에 유리한 조건이다. 국내 중부지방에 Corinne과 Eudora 시스템과 비슷한 연못시스템을 설치운영(設置運營)하는 데는 문제점이 없음을 알 수 있다. 남부지방은 연중기온이 김포지역보다 높으므로 연못시스템의 이용이 김포지역보다 유리하다. 미국에서는 연못시스템이 2차처리시설(次處理施設)로 합법화되어 있으며, 2차처리 수질기준(水質基準)을 충족시키고 있다. Corinne과 Eudora 연못시스템의 처리수준을 분석한 결과 처리수의 $BOD_5$ 가 30mg/l 이하로 처리되고 있으나, SS 농도가 30mg/l 보다 다소 높은 경우가 있다. Eudora시스템에서 4월에 일어나는 연못하수의 회전기간(回轉期間)을 제외하고는 연못시스템에 적용하는 처리수의 SS기준인 70-100mg/l 이내로 처리되고 있다. 우리나라 중부지방에 Corinne과 Eudora 시스템과 유사한 연못처리시스템을 설치(設置)하면 2차 처리수준으로 하수를 처리할 수 있을 것으로 판단된다. 연못시스템은 양어, 작물생산, 레크레이션이용과 결합시킬 수 있어, 국내의 경우 농촌소도시 지역, 도시경계 생산녹지지역, 내륙 및 하구의 저습지(wetland)에서 소형뿐아니라 대형 시스템으로 활용이 가능하다.

• 한국태양에너지학회:학술대회논문집
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• 한국태양에너지학회 2008년도 추계학술발표대회 논문집
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• pp.85-89
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• 2008

This study carried out field observations of measuring thermal environment, especially evaluating amount of water evaporation at roof Pond by field observations during the summer. Thermal environment measuring was categorized as air temperature, water temperature of roof pond, surface temperature, globe temperature, short and long wave radiation, net radiation, and amount of water evaporation by water level measurement. Results from this study could be used as fundamental for reducing heat Island phenomena.