• Title/Summary/Keyword: Metropolitan multi-regional water supply system

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Assessment of the Deterioration of Large-Diameter Pipe Networks (II) : Application to Metropolitan Multi-Regional Water Supply System (1st Phase) (대구경 관로의 노후도 평가 연구(II) : 수도권 광역상수도(1단계) 적용)

  • Lee, Seung-Hyun;Yoon, Ki-Yong;Kim, Eung-Seok
    • Journal of the Korea Academia-Industrial cooperation Society
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    • v.15 no.2
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    • pp.1096-1101
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    • 2014
  • This study (II) has appled the new assessment model of large-diameter pipe deterioration proposed by the study (I) to the metropolitan multi-regional water supply system (1st phase). In the total 30 pipelines, 24 and 27 pipelines were required for improvement as results from the existing evaluation methods 1995 and 2002, respectively. The assessment results were almost similar in the new developed model and the existing methods. It is founded that the new simple model developed in this study can produce reliable results, consistent with those from the existing methods requiring many factors for a pipe deterioration assessment. It is therefore expected that the new model would be helpful in practical applications of a pipe deterioration assessment since it can save both temporal and economic costs for experiments and analysis, as compared with existing assessment methods.

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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