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Design and Performance Test of a Thermal Tuning System for the PEFP DTL
김경렬,Jun Park,Hyung Gyun Kim,Hee Seob Kim,Chong Chul Yoon,Yoon Gyu Son,권혁중,Han Sung Kim,조용섭 한국물리학회 2010 THE JOURNAL OF THE KOREAN PHYSICAL SOCIETY Vol.56 No.61
The resonance control cooling system (RCCS) is the thermal tuning system for controlling the resonance frequency, 350 MHz, of the drift tube linac (DTL) in the Proton Engineering Frontier Project (PEFP). The PEFP uses 12 separate RCCS water pumping skids to control the resonance of the 20-MeV DTL (DTL21-24), 100-MeV DTL (DTL101-107) and the radio frequency quadrupole (RFQ) accelerating structures. The nominal operating inlet water temperature of the RCCS is 27 ℃and should be adjustable depending on the operational RF duty modes (21 to 33 ℃) with a stability of less than 0.1 ℃. In this work, we completed fabrication of the RCCS22-24 and the RCCS101-103. This paper discusses the fabrication, performance test, and analysis of the RCCS water pumping skids. First, the fabrication of the RCCS for the 20-MeV DTL is discussed. Second, the layout of the water pumping skid, including the selection of piping components, instrumentation and controller hardware and software, is presented. Third, the performance test of the RCCS for the 20-MeV DTL, including the continuous driving test, the function test of each components and temperature control test are achieved. Finally, empirical pressure and flow rate data from the RCCS22 water pumping tests are used to verify the design and numerical modeling of the RCCS101-103.
김경렬,이태식 한국해양학회 1991 韓國海洋學會誌 Vol.26 No.3
A synoptic survey of chemical properties was carried out at 21 stations in the Ulleung Basin in May 1988 on board T/V HANBADA. Vertical structures of typical profiles are: surface mixedlayer waters in the upper 30∼40 m with depleted nutrients concentrations, thermocline waters with rapid variations in all physical and chemical properties. and deep Waters below 200 m which are nearly homogeneous. Along the northern section at 37$^{\circ}$12'N. The salinity minimum layer was observed at about 190m. which characterize the East Sea Intermediate Water (ESIW). The dissolved oxygen concentration in this layer was about 230∼ 275uM, lower than 290uM (6.5ml/l) which is the previously known characteristics of the ESIW. However, apparent oxygen utilization (AOU), nitrate, phosphate and silicate show systematically low concentration in the salinity-minimum layer. The low values of AOU and all the nutrients associated with the salinity-minimum, may be useful to identify the ESIW and serve as a new tracer in the East Sea.