• Title/Summary/Keyword: conveyance increasement

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A Study of the Conveyance Increasement for Urban River using 1, 2-Dimensional Numerical Model (1, 2차원 수치모형에 의한 도시하천의 통수능 확보 방안에 관한 연구)

  • Baek, Chun-Woo;Park, Moo-Jong;Kim, Seok-Woo;Jo, Deok-Jun;Kim, Joong-Hoon
    • Journal of the Korean Society of Hazard Mitigation
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    • v.5 no.3 s.18
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    • pp.73-82
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    • 2005
  • The scheme for the conveyance increasement of urban river is presented in this study. For the use of the lower part of the road paralleled to urban river as a conveyance, the 2-dimensional flood flow between main channel and added conveyance section is analyzed by mathematical model SMS(2-D simulation model). The result of the HEC-RAS(1-D simulation model) is used to calibrate the parameters of SMS. New scheme is applied to the Cheonggeyecheon Restoration Project. The capacity of flood flow between main channel and added conveyance is simulated for 50, 80, 200 year frequency flood and suitable size of pathway is proposed.

Geothermal Effects on the Underground Water Conveyance Pipe System from Han River (한강수계 광역상수도 원수관의 지열 영향 조사)

  • Cho, Yong;Park, Jin-Hoon;Park, Tae Jin;Kim, Youngjoon
    • 한국신재생에너지학회:학술대회논문집
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    • 2010.06a
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    • pp.171.2-171.2
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    • 2010
  • Geothermal effects on the underground water conveyance pipe system have been investigated through the multiregional water supply system from Paldang water intake station. To make an investigation of raw water thermal energy, temperature sensors are installed the surface of the pipes of metropolitan area water supply system. In 2009 winter and early spring seasons, the monthly averaged temperatures at Paldang 2 intake stations are $1.94^{\circ}C$ in February, $4.96^{\circ}C$ in March, and $10.56^{\circ}C$ in April. After the transfer in 26.0 km distance of tunnel and buried pipe, the raw water temperatures are raised to $3.13^{\circ}C$, $6.04^{\circ}C$, and $11.39^{\circ}C$ respectively. As the temperature difference between the raw water and the air reduces, the temperature increasement is reduced by $1.19^{\circ}C$ in Feb., $1.08^{\circ}C$ in Mar., and $0.83^{\circ}C$ in Apr. Since the flowrate is over 1,150,000 $m^3$/day, it is estimated that the water exchanges a huge amount of heat over 1.0 Tcal a day with the ground.

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