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배영(Young Bae),박소라(So Ra Park),박찬웅(Chan Ung Park) 이화여자대학교 이화사회과학원 2008 사회과학연구논총 Vol.20 No.-
본 연구는 현재 중요한 삶의 환경으로 작용하고 있는 정보화 환경과 개인들의 인터넷 이용에 있어서 한국과 일본의 유사성과 상이함의 측면들을 살펴보고 인터넷에 기반한 커뮤니케이션이 개인들의 일상에서 중요한 역할을 하고 있는 사회적 관계에 미치는 영향에 대해 파악해보고자 했다. 연구결과를 요약하면 다음과 같다. 한국과 일본의 미디어 이용행태에 있어서 두드러지게 나타나는 것은 TV 와 인터넷 이용에 있어서의 차이였고, 인터넷 이용에 있어서는 한국의 응답자들이 일본의 응답자들에 비해 보다 적극적인 이용자로 분류될 수 있음을 알 수 있었다. 관계 유지를 위해 필요한 커뮤니케이션 수단들의 중요성은 양국 모두에서 직접 대면이 가장 중요한 수단이라는 점을 보여주었고 전반적으로 매체의 이용빈도와 중요도에 대한 인식은 커다란 상관관계를 가지고 있는 것으로 파악할 수 있었다. 인터넷을 이용하여 새로운 관계의 형성이 활발하게 이루어지고 있는 상황에서도 여전히 오프라인에서의 대면적인 활동이 가장 중요하다는 것은 아직까지는 온라인에서의 커뮤니케이션이 가지고 있는 편의적인 측면보다는 대면적 관계에서의 확실성이 더욱 중요하게 여겨지고 있다는 점을 의미한다. 또한 인터넷의 도입으로 인해 관계의 유지에 있어서 오프라인에서의 대면적 접촉이나 전화의 빈도가 줄어드는 것이 아니라 더 늘어나고 있는 양상을 발견할 수 있었는데, 한국과 일본은 인터넷 이용의 정도나 선호매체의 질적인 차이는 존재하고 있었지만 사회적 관계를 기반으로 하는 사회자본의 형성과 유지에 인터넷이 긍정적인 요소로 작용할 수 있다는 점은 양국 모두에서 공통적으로 보여주고 있었다. The goal of this study is two-folds: first, this study examines similarities and differences in informatization circumstance and internet use between South Korea and Japan and, second, examines how internet-based communication influences social relations in everyday life. The findings go as follows. First, results show distinct activities that South Korean internet users enjoy on the web. South Korean internet users spent more time and cost than those Japanese internet users spent on the web. Second, both South Korean and Japanese people considered face-to-face interaction the most important way of communication to maintain a relational closeness. It is also worth noting that frequency of each specific media use and perceived importance of the media are highly correlated. Even if internet-based communication started the development of a new personal interaction, this finding gives an implication that people prefer face-to-face interaction (offline interaction) to online interaction. Third, in both South Korea and Japan, results reveal increasing use of internet in communication. However, this change does not lead to decrease in face-to-face interaction (offline interaction) and decrease in telephone use; rather telephone use is increasing. In conclusion, in spite of qualitative difference in degree of internet use and preferred media, South Korean society and Japanese society have commonality in that internet use contributes to generating and maintaining social capital that originates from social relations.
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배영(Young Bae),박소라(Sora Park),이동형(Dong Hyeung Lee) 사이버커뮤니케이션학회 2009 사이버 커뮤니케이션 학보 Vol.26 No.1
본 연구에서는 어린이들에게 매우 중요한 일상의 요소인 인터넷을 하나의 미디어로 보고 인터넷의 소비가 어린이들의 사회적 관계와 어떠한 관련성이 있는지를 탐색하고자 하였다. 사회적 관계를 맺는 방식이 인터넷을 이용하는 패턴에 영향을 주는지를 알아보기 위해서는 한 시점의 횡적 조사를 통해서 알아내기란 불가능하다. 따라서 본 연구에서는 2년에 걸쳐 동일한 집단을 대상으로 텔레비전과 인터넷 등 미디어 이용에 따라 사회적 관계를 맺는 방식이 달라지는가를 실증적으로 분석하였다. 이를 위해 서울시내 1개 초등학교에서 2학년, 5학년 학생들을 대상으로 2004년에 조사한 후 다시 동일한 집단을 대상으로 이들이 3학년, 6학년이 되었을 때 반복 조사하여 그 변화 추이를 분석하였다. 분석결과 어린이들의 친구관계에 텔레비전보다는 인터넷이 더 유의미하게 작용하고 있었고, 부모와의 대화에는 오히려 텔레비전이 부정적 영향을 주었다. 텔레비전에 비해 인터넷은 커뮤니케이션의 주요 도구로 직접 활용이 가능하다. 텔레비전의 이용정도는 학생들의 연결망의 특성에 별다른 영향을 주고 있지 못하지만 인터넷은 그 이용정도에 따라 차별적으로 영향을 미치고 있는 것이다. 또한 인터넷을 많이 이용하는 학생들의 경우 그렇지 않은 학생들에 비해 상대적으로 관계망의 중심에 근접하는 특성을 보여주고 있다. 인터넷 이용정도가 높다는 것은 인터넷 이용을 통해 얻게 되는 정보의 양이 많다는 것을 의미한다는 측면에서 텔레비전을 통해 얻게 되는 정보보다는 인터넷에서 얻게 되는 정보가 관계의 형성과 유지에 도움이 되는 것이다. This study views the mass media as important aspects of children's everyday lives and that they have significant effects on how they relate to others socially. The mechanism of how media use affect the social relationships and networks cannot be studied cross-sectionally. We need to pursue a longitudinal panel study in order to see the actual changes that occur across time. This study is a two year consecutive panel study that surveyed children of various ages. We adopted the network effects as an important factor in explaining the media use of children. The survey was conducted in an elementary school in Seoul. Children in the second and fifth grade were surveyed the first year and in the second year, the same students were surveyed with similar questionnaires. The results show that internet, more than television, influences the social relationships children engage in. However, the communication with parents were less affected by the internet but more so by the time spent on television. This can be explained by the fact that the internet is a communication device as well as a means to entertain ment or information. Various forms of internet use influence the social networks differently. Also, those who use the internet are relatively situated in the center of the social networks of the children.
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박효진,배영인,최준균,Park, Hyo-Jin,Bae, Young-In,Choi, Jun-Kyun 대한임베디드공학회 2008 대한임베디드공학회논문지 Vol.3 No.4
Internet protocol television (IPTV), one of the most emerging services, offers multimedia streaming services with security, reliability, and relevant quality of service (QoS)/quality of experience (QoE). It provides added values to all the involving players and also brings technical and business challenges to them. For IPTV services, we expect to adopt the next generation network (NGN) environment for high quality and the Web technologies for personalization to meet the customer's necessity. Web can provide an open, flexible, and agile platform. Therefore, in this paper, we propose personalized IPTV services based on Web-based open platform in NGN environment and present functional architecture for Web-based personalized IPTV services. Technical issues for deploying the proposed IPTV services using Web are also provided. The objective of this paper is to analyze the critical architectural issues for developing viable and feasible networking platform models for personalized IPTV services.
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전남(全南)과 하동지역(河東地域)에서 산출(産出)하는 요업(窯業) 및 점토(粘土) 광물자원(鑛物資源)과 성인(成因)에 관(關)한 연구(硏究)
박홍봉,박배영,신상은,허민,Park, Hong Bong,Park, Bae Young,Shin, Sang Eun,Huh, Min 대한자원환경지질학회 1988 자원환경지질 Vol.21 No.1
This is a study on the mineral compositions, SK numbers of refractoriness and the genesis of the clay mineral deposits in Cheonnam Province and Handong area. 1. Jindo kaolin deposits: Chief clay minerals of the deposits are kaolinite, quartz and alunite. The SK number of the ore is from $34^+$(the highest) to 27(the lowest). On the genesis of the deposits some geologists believe that the deposits were formed by the alteration of the siliceous tuff. But the deposits seems to be formed by the hydrothermal alteration of the rhyolite lava beds. This area is formed by alternative beds of tuff; and kaoline deposits. 2. Hadong area: Chief mineralogy of Hadong kaolin area is $10{\AA}$ halloysite and kaolinite. The SK number of some of the ore is up to $36^+$. The theoretic SK number of kaolinitic composition is 35. So one of the highest alumina minerals of gibbsite is formed in the ores of $36^+$ SK numbers. 3. Hampyong kaolin deposits: Most of kaolin has black color. The chief minerals are kaolinite, quartz and muscovite. Some of the kaoline contains rutile crystals. SK number ranges from 30 to 17. The kaolin deposit is formed by the transported sedimentation in lower part of the seashore. 4. Jangsan kaoline deposits: Chief minerals of the kaolin is kaolinite, quartz and muscovite. Some kaoline contains small crystals of pyrite. This area consists almost of the tuffs. Kaolin deposits also would be formed by the alteration of the tuffs. 5. Nohwado pyrophyllite deposits: Quartz and pyrophyllite are chief minerals. SK number of the ore ranges from 32 to 30. The pyrophyllite deposits would be formed by the hydrothermal alteration of the rhyolitic lava beds. This area consists of alterative beds of tuffs and rhyolitic lavas. 6. Songsuk pyrophyllite deposits: Chief minerals are quartz, kaolinite, pyrophyllite and iron oxides. In the pyrophyllite deposits egg-like inclusions of diaspore and kaolinite in composition. This area almost consists of tuffs. Several faults are developed and along the fault the tuff would begin to alter to pyrophyllite and some parts to diaspore and kaolinite nodules by the acts of hydrothermal solution.
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고내화도(高耐火度) 광석광물(鑛石鑛物)의 분포(分布)와 성인(成因)에 관(關)한 연구(硏究) -전남지역(全南地域)을 중심(中心)으로-
박홍봉,권숙문,박배영,신상은,Park, Hong Bong,Kwon, Sook Moon,Park, Bae Young,Sin, Sang Eun 대한자원환경지질학회 1982 자원환경지질 Vol.15 No.2
Several mines in Jeonnam produce the ores of having high SK number of refractoriness. Among those for 5 mines, this paper deals with the relationahip between SK number and mineral composition of the ore, and with the genesis of the deposits. 1. Byok-Song and Chon-Un Mine: Mineral compositions of the ores are chiastolite, chloritoid(monoclinic), kaolinite, sericite, diaspore, corundum, and quartz. The ores having SK number of 36 or 37, consist chiefly of chiastolite and diaspore and a little amount of kaolinite, sericite, corundum, chloritoid, and quartz. The ores having SK number of 33 or 34 consist of chloritoid, sericite, kaolinite, chiastolite, and diaspore. With increasing the amount of chloritoid and sericite, and decreasing the amount of diaspore and chiastolite, the SK number of the ores decreases. The deposit, originally high alumina-bearing shale of Chon-Un San formation, seems to be formed by contact metamorphism(forming of chiastolite), regional metamorphism(forming of monoclinic chloritoid), and hydrothermal replacement(forming of large crystal of diaspore veinlets). 2. Song-Sauk Mine: Mineral compositions of the ores are chiefly pyrophyllite and quartz and a little amount of kaolinite, dickite, diaspore, and pyrite. Many spherical inclusions containing in pyrophyllite deposits, consist chiefly of diaspore and kaolinite, The inclusions have the high SK number of 38. Amount of spherical inclusions is about 5 % to the whole pyrophyllite ores. The SK number of other pyrophyllite ore is less than 32. Quartz and pyrite are chief minerals lowering the SK number of the ore. The deposits have been formed by hydrothermal processes by replacing the siliceous tuff of Mesozoic age. Spherical inclusions consisting of diaspore and kaolinite, show the selective replacement of hydrothermal solutions to the materials of feldspar in tuff. 3. Seung-San Mine: Mineral compositions of the ores are chiefly kaolinite, dickite, diaspore, and quartz. But some part of the mine consists of alunite deposits. The ores having SK number of 35 or higher consist chiefly of kaolinite and diaspore and a little amount of quartz. With increasing the amount of quartz and decresing the amount of diaspore, the SK number of the ore decreases. The deposits have been formed by hydrothermal processes by replacing the siliceous tuff and quartz porphyry. 4. Wan-Do Mine: Mineral compositions of the ores are chiefly pyrophyllite and quartz. But some ore contains a little amount of diaspore, kaolinite, pyrite, and chloritoid. The ores having high SK number of 36 consist chiefly of diaspore and pyrophyllite. Pyrophyllite ore has a SK number of 32 or lower. Amount of quartz and pyrite decreases the SK number of ores in this mine. Rhyolite was replaced by the action of hydrothermal solutions forming the pyrophyllite deposits.
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