• Title/Summary/Keyword: Inner vent type

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A Study for the Cooling Performance of a Brake with Heat Pipes (히트 파이프를 장착한 디스크브레이크의 냉각 성능에 관한 연구)

  • Kim, Moo-Geun;Ko, Sung-Kyu;Lee, Moon-Wan
    • Journal of Advanced Marine Engineering and Technology
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    • v.32 no.4
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    • pp.563-569
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    • 2008
  • During braking operation, the surfaces of disk have severe contact conditions and high frictional heat would be generated between disk and pad surfaces. The heat makes high temperature gradient on disk surfaces and results in thermal deformation. To enhance the frictional heat dissipation, heat pipes are embedded in the ventilated type disk along the radial direction. The temperatures of the inner vent type disk and the brake disk with heat pipes are compared at the same operating conditions. By comparison a brake disk with heat pipes has higher cooling performance than the inner vent type disk.

Numerical analysis of solar heat gain on slim-type double-skin window systems - Heat transfer phenomena with opening of windows and vent slot in summer condition - (전산유체 해석을 통한 슬림형 이중외피 창호의 태양열 취득량 분석 - 높은 태양고도 및 하절기 냉방조건에서의 자연환기구 적용 및 창문 조절 방식별 비교 -)

  • Park, Ji-Ho;Oh, Eun-Joo;Cho, Dong-Woo;Cho, Kyung-Joo;Yu, Jung-Yeon
    • KIEAE Journal
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    • v.17 no.1
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    • pp.69-75
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    • 2017
  • Purpose: Heat transfer analysis of recently developed 'slim type double-skin system window' were presented. This window system is designed for curtain wall type façade that main energy loss factor of recent elegant buildings. And the double skin system is the dual window system integrated with inner shading component, enclosed gap space made by two windows when both windows were closed and shading component effectively reflect and terminate solar radiation from outdoor. Usually double-skin system requires much more space than normal window systems but this development has limited by 270mm, facilitated for curtain wall façade buildings. In this study, we estimated thermophysical phenomena of our double-skin curtain wall system window with solar load conditions at the summer season. Method: A fully 3-Dimentional analysis adopted for flow and convective and radiative heat transfer. The commercial CFD package were used to model the surface to surface radiation for opaque solid region of windows' frame, transparent glass, fluid region at inside of double-skin and indoor/outdoor environments. Result: Steep angle of solar incident occur at solar summer conditions. And this steep solar ray cause direct heat absorption from outside of frame surface rather than transmitted through the glass. Moreover, reflection effect of shading unit inside at the double-skin window system was nearly disappeared because of solar incident angle. With this circumstances, double-skin window system effectively cuts the heat transfer from outdoor to indoor due to separation of air space between outdoor and indoor with inner space of double-skin window system.

Volcanisms and igneous processes of the Samrangjin caldera, Korea (삼랑진 칼데라의 화산작용과 화성과정)

  • 황상구;김상욱;이윤종
    • The Journal of the Petrological Society of Korea
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    • v.7 no.3
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    • pp.147-160
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    • 1998
  • The Samrangjin Caldera, a trapdoor-type, formed by the voluminous eruption of the silicic ash-flows of the Samrangjin Tuff which is above 630m thick at the northern inside of the caldera and thinnerly 80m at the southern inside. The caldera volcanism eviscerated the magma chamber by a series of explosive eruptions during which silicic magma was ejected to form the Samrangjin Tuff. The explosive eruptions began with phreatoplinian eruption, progressed through small plinian eruption and transmitted with ash-flow eruption. During the ash-flow eruption, contemporaneous collapse of the roof of the chamber resulted in the formation of the Samrangjin caldera, a subcircular depression subsiding above 550m deep. During postcaldera volcanism after the collapse, flow-banded rhyolite was emplaced as cental plug along the central vent and ring dikes along the caldera margins. Subsequently rhyodacite porphyry and dacite porphyry were emplaced along the inner side of the ring dike. After their emplacement, residual magma was emplaced as a hornblende biotite granite stock into the southwestern caldera margin. In the northeastern part, the eastern dikes were cut final intrusions of granodioritic to granitic composition along the fault zone of $^{\circ}$W trend.

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