• Title/Summary/Keyword: 금정산

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시추자료와 순간충격시험의 관련성에 의한 금정산 화강암지역의 수리적 특성

  • 정재열;함세영;이병대;류상민;김광성;우윤정
    • Proceedings of the Korean Society of Soil and Groundwater Environment Conference
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    • 2002.09a
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    • pp.378-381
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    • 2002
  • 금정산지역의 수리적인 특성을 파악하기 위하여 27개 지하수 공을 대상으로 순간충격시험(주입, 인양시험)을 실시하였다. 순간충격시험자료는 C-B-P법, Hvorslev법, Bouwer & Rice법을 이용하여 분석하였으며, 분석을 위해서는 AQTESOLV(Version 3.01) 소프트웨어를 이용하였다. 또한, 자료의 해석을 위해서 시추자료와 연관하여 해석하였으며, 이때 시추시 용출심도와 수리전도도와의 관련성 분석으로 dummy의 충격과 심도의 관련성을 고찰해 보았다. 순간충격시험 분석결과 얻어진 수리전도도는 7.69E-8 ~ 2.30E-5m/sec를 보인다.

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Rb-Sr Whole-rock Isochron Age and Petrology of the Mt. Geumjeong Granite, Busan (부산 금정산화강암체의 암석학 및 Rb-Sr 전암 등시선 연대)

  • Yun Sung-Hyo;Koh Jeong-Seon;Park Kwang-Sun;Ahn Hyo-Chan;Kim Young-Il;Yoo Sung-Hyeon;Lee Dong-Han;Yun Gi-Young
    • The Journal of the Petrological Society of Korea
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    • v.14 no.1
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    • pp.61-72
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    • 2005
  • The granitoids in the Mt. Geumjeong, Busan can be divided into granodiorite, hornblende granite, adamellite, tonalite, biotite granite and micrographic granite. The geochemical characteristics of the Mt. Geumjeong granites indicate that they were crystallized from a calc-alkaline series and that they belong to Ⅰ-type granitic rocks which evolved from granodioritic magma into hornblende granite, adamellite, biotitie granite, and finally micrographic granite through fractional crystallization of plagioclase. The crystallization pressures and temperatures of the minimum melt compositions of the granitic rocks were estimated to about 1∼5 kbar and 720∼700℃. The trace element composition and REE patterns, characterized by a high LILE/HFSE ratio and enrichments in LREE, indicate typical continental margin arc calc-alkaline rocks produced in the subduction environment. The Rb-Sr isotopic data for the Mt. Geumjeong granites define a well-defined isochron yielding as age of 69.6±1.9 Ma with an initial Sr isotopic ratio of 0.70503.

A Study on Inter-agency Fare Allocation Methods under the Integrated Distance-based Fare System in Seoul (서울시의 대중교통 통합거리비례요금제 하에서 운영기관 간 요금정산방안에 관한 연구)

  • Yun, Ji-Hyeon;Kim, Seong-Su
    • Journal of Korean Society of Transportation
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    • v.25 no.1 s.94
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    • pp.37-47
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    • 2007
  • The Integrated Public Transport Reforms of the Seoul Metropolitan Government, which were implemented on the $1^{st}$ of July. 2004, launched a new fare allocation method. However, when a Private transit operator or a new transport system is introduced into the existing system, it will cause an allocation problem. Therefore, this study aims to Propose a rational fare allocation method which can be applicable regardless of the number of Public transportation modes or operators. To create alternatives, this study has adopted a fundamental principle of revenue allocation methods for the transit or communications sectors, and has applied it to the current transit system of Seoul. This study kas analyzed results of the cost recovery ratios and characteristics of each alternative through case studies. This study kas Presented an assessment criterion Z in order to select an optimal alternative. The criterion consists of the sum of the cost recovery ratio of each operator and the difference of the cost recovery ratio for each agency in inter-agency transit. Using the assessment criterion. the results showed that Alternative 1 is superior to the others : Alternative 1 is considering passenger-km of each operator and unit cost of passenger-km for each operator.

Study on Spatial Characteristics of Physicochemical Components of Spring Water in Mts. Geumjeong and Baekyang Area Using Kriging (크리깅 기법을 이용한 금정산-백양산 일대 용천수의 물리화학적 성분의 공간적 분포 특성 연구)

  • 함세영;정재열;류상민;강래수
    • The Journal of Engineering Geology
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    • v.12 no.4
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    • pp.439-457
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    • 2002
  • Sping waters at 60 sites and groundwaters at 6 wells in Mts. Geumjeong and Baekyang area were investigated for measuring nine physicochemical components (temperature, pH, Eh, EC, TDS, DO, salinity, alkalinity and discharge rate). The pH of spring waters ranges from 5.06 to 8.38, alkalinity from 7.93 to 102.21 mg/ㅣ, electrical conductance from 9.5 to $270{\;}\mu\textrm{s}/cm$, Eh from 64.2 to 685.9 mV, DO from 4.57 to 12.13 mg/l, and the discharge rate from 4.26 to 182.2 ml/s. General statistics was carried out to analyze statistical characteristics of those components. To compare the components with one another, regression analyses were carried out. And the components of spring waters were compared to those of groundwaters. Kriging was used to estimate the spatial variation of DO, pH, Eh, EC, alkalinity and discharge rate in the study area. The kriged isopleth maps were made using normalized kriged values to find anomalies of the physicochemical components and to compare anomalies of different components.

Crystal Morphology of Zircon in Granitoids from the Mt. Keumjeong District, Pusan, Korea (부산 금정산 지역 화강암류의 저어콘에 대한 형태학적 연구)

  • 이윤종;윤성효;김상욱;고인석;황상구;정원우;김중욱;이철락;하야시마사오
    • The Journal of the Petrological Society of Korea
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    • v.8 no.2
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    • pp.71-80
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    • 1999
  • We report zircon morphology of granitoids in the Mt. Keumjeong district, Pusan. There are a series of granitoids in the study area of the late Cretaceous: granodiorite, hornblende granite, adamellite, tonalite, biotite granite, and micrographic granite. Generally, the shapes of zircon crystals are short prismatic to middle prismatic and are dominant in {loo) prism and {101) pyramid in total average morphological data of the granitoids. The crystal forms of zircon in the granitoids can be distinguished by the PPEF diagram and the prism index (PI). The prism index values of zircon crystal forms in granodoirite and hornblende granite are higher than those of tonalite and micrographic granite. The finishing temperature range ($820~800^{\circ}C$) for crystallization of zircon crystals in granodoirite and hornblende granite is higher than the temperature ($790~770^{\circ}C$) at which the zircon crystals are created in tonalite and micrographic granite. The last differentiates (biotite granite and micrographic granite) have mainly intermediate zircon ({110)={100)) crystals, respectively. As differentiation proceeds, the zircons of granitoids become from short prismatic to middle prismatic in the each granitoid types.

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