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포스트 코로나 시대의 교회 활성화를 위한 청중의 설교 참여 방안 : 루돌프 보렌을 중심으로
최광희 한국복음주의실천신학회 2022 복음과 실천신학 Vol.65 No.-
한국교회는 2020년에 코로나 19의 직격탄을 맞아 예배와 소모임을 제한당하면서 신앙 공동체 기능이 상실될 위기에 처하였다. 다행히 2022년 봄부터 사회적 거리 두기는 완화되었지만, 한동안 중단되었던 소모임이 원활해지고 이를 통해 신앙 공동체를 활성화하기 위해서는 특별한 방안 마련이 필요하다. 그 방안 가운데 하나는 청중이 소그룹 활동을 통해 설교에 참여하도록 하는 것인데 적절한 대안으로 설교 비 평을 제안한다. 한국교회에 설교 비평이 필요한 또 한 가지 이유가 있는데 그것은 한 국교회 강단에 정당성과 적실성을 상실한 설교가 난무한 실정이라는 것이다. 한국교회 강단은 성역화되어 있어서 오랫동안 제대로 된 평가 를 받지 않았다. 그러므로 한국교회의 강단은 해석과 전달에 있어 설교 학적 기준 마련이 절실한 상황이다. 설교자의 발전과 청중의 설교 참여라는 두 가지 목적을 위해 설교 비 평은 꼭 필요하다. 하지만‘비평’이라는 부정적 이미지를 보완하고 건 설적 설교 비평을 하기 위해서는 먼저 올바른 기준을 마련해야 한다. 설교 비평은 먼저 설교자 그룹과 청중 그룹으로 구분하여 이중 노선으 로 운영할 필요가 있다. The Korean church is in danger of losing its function as a community of faith as worship and small gatherings are restricted in the face of a direct hit from Corona 19 in 2020. Fortunately, social distancing has been relaxed from the spring of 2022, but special measures are needed to facilitate small groups that have been suspended for a while and to revitalize the faith community. One of the ways is to engage the audience in the sermon through small group activities. As an appropriate alternative, sermon critique is suggested. Another reason why Korean churches need sermon critique is that there are a lot of sermons that have lost their validity and relevancy in the pulpit of Korean churches. The pulpit of the Korean church has not been properly evaluated for a long time because it is sanctuary. Therefore, the pulpit of the Korean church is in dire need of sermon standards for interpretation and delivery. Preaching critique is essential for two purposes: the development of the preacher and the participation of the audience in the sermon. However, in order to supplement the negative image of‘critique’and to give constructive sermon critique, it is necessary to first prepare the right standards. Sermon critique needs to be divided into a preacher group and an audience group first, and it needs to be operated in a double line.
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최광희,정연수,이재일 한국정보보호학회 2012 情報保護學會誌 Vol.22 No.6
최근 해킹 등으로 인한 대량 개인정보 유출 사고로 인한 계속됨에 따라 개인정보보호 법제도 측면에서 변화가 시작되고 있다. 지금까지는 사고원인을 분석하여 기술적, 관리적으로 미흡한 부분을 보완하는 기업의 보호조치의무를 강화하는 방식이었으나, 최근에는 보다 근본적으로 개인정보 수집을 최소화하고 사고를 적극적으로 예방하려는 다양한 신규 제도가 만들어지고 있다. 따라서 새롭게 도입되는 개인정보보호제도의 의미와 주요 내용을 살펴보고 기업이 새로운 제도에 대응하는 전략을 고찰하고자 한다.
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최광희 한국지형학회 2020 한국지형학회지 Vol.27 No.2
Grain size analysis is the most basic procedure for identifying the origin, transport and sedimentation processes of sediments, and is widely used in geomorphology and sedimentology. Traditionally, grain size was determined by a sieve-pippette method, but the use of automated analyzers is increasing in recent years. These analyzers have many advantages over traditional techniques, but the measurement results are not always the same. It is still difficult to solve the pretreatment problem such as incomplete diffusion and residual organic matter, and inappropriate results may be obtained. This study compared image-based grain size analysis and sieve analysis to verify its statistical reliability, and conducted experiments to enhance the measurement accuracy using shape parameters. The results showed that the image-based analysis overestimated the grain size of sand dunes by about 7% compared to the sieve analysis, but the two measurements were not statistically different. In addition, by using shape parameters, such as aspect ratio, sphericity, and convexity, improved statistics were obtained compared to the original data. Using the morphological properties of the individual grains is a complementary method to the incomplete pretreatment of the grain size analysis process, and at the same time, it will contribute to improving the accuracy and reliability of the results.
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최광희,공학양 한국지형학회 2017 한국지형학회지 Vol.24 No.4
The Okjukdong dune in Daecheong Island attracts national attention because of its unique landscape that is not covered by vegetation. However, there has been little knowledge on the timing of the dune formation, associated wind regime, and conservational strategies. In this study, we used OSL dating and grain size analyses to reveal the history of the dune development. In addition, we analyzed the wind regime in the dunefield which is surrounded by artificial coastal forest. The fine sand at Okjukdong underlain by a colluvial gravel layer indicates that the dune has been developed since at least 5 ka. Aeolian sands were found to be deposited around 700 years ago. The dunefield appears to have been severely eroded 30~60 years ago. The dune landscape has been destroyed after constructing a windbreak forest around the dunefield. The sand seems to be moving south and north with the season.
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최광희,성영배 한국지질과학협의회 2021 Geosciences Journal Vol.25 No.3
The occurrence of global warming and concomitant rises in sea level means it is important to assess the vertical lowering rates and evolution of shore platforms. Most previous studies, however, were based on empirical measurements and limited to the decadal scale, implying there is great necessity to learn about long-term rates of change on rocky coasts. In particular, because it is relatively easy to monitor soft rocks such as chalk, there is little information about hard rocky coasts that consist of volcanic, igneous, and metamorphic rocks. In this study, we used cosmogenic 36Cl exposure dating to overcome the spatial and temporal limitations of previous studies that have restricted progress in rocky coast research. Results show that the exposure ages of samples collected from the shore platforms along volcanic islands in the middle of the East Sea (Sea of Japan) range from the mid-Holocene (ca. 4 ka) to the last century (ca. 0.1 ka). The large range in ages along the outer platform edges may be related to stochastic, differential, and mechanical wave erosion. We also calculated the rates of vertical lowering from the 36Cl concentrations of the platform surfaces, yielding a maximum rate, excluding outliers, of 0.68 mm/yr. The rates of vertical lowering inferred from the cosmogenic 36Cl abundances are comparable with previous empirical values, and will improve our understanding of the long-term evolution of rocky coasts.
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최광희 한국지도학회 2020 한국지도학회지 Vol.20 No.3
강원도 고성군에 있는 운봉산은 화강암 산지 사이에 단독으로 떨어져 있는 화산체로 경관이 매우 독특하다. 현무암 거력으로 구성된 애추와 암괴류가 일부 사면을 덮고 있다. 지질학적 측면에서 이 산의 특징은 비교적 상세히 조사되었다. 하지만, 암괴 지형의 전반적인 분포 패턴이나 발달과정은 잘 알려지지 않았다. 이 연구는 암괴 지형에 대한 지도화, 사면의 형태적 특성 분석, 암괴에 대한 야외조사를 통해 운봉산의 암괴 지형을 분류하고자 하였다. 노출 암괴는 산의 서사면에 집중적으로 분포하고 동사면에 는 거의 분포하지 않는 특징이 있다. 야외조사 결과, 암괴는 모두 주상절리가 발달한 현무암이었으며, 해발고도 및 경사에 따라서 장축방향성이 나타났다. 수치고도모형에 대한 지형위치지수(TPI) 및 사면분석 결과는 암괴류가 주로 계곡을 따라 분포하고 애추는 가파른 능선이나 현무암 단애 하부에 분포함을 보여주었다. 사면 지형을 분류한 결과, 산의 중심으로부터의 거리에 따라, 평탄한 산정부, 현무암 단애, 애추, 암괴류가 차례로 나타난다는 것을 확인하였다. 운봉산의 암괴 지형은 화산체의 사면 후퇴로 발생하는 사면발달과정을 잘 보여준다. Unbongsan Mountain is a volcanic edifice with a unique landscape, which is located alone between granite mountains in Goseong-gun, Gangwon-do. The slopes of the mountain are partially covered with talus and block streams consisting of large basalt bouders. The geological features of this mountain have been investigated in detail. However, their overall distribution patterns and development processes are not well known. This study aims to classify these bouldery landforms through mapping the location of basalt blocks, the analysis of the morphological characteristics of the slope, and field surveys on the large boulders. The exposed boulders are concentrated in the western valleys of the mountains and are rarely found in the eastern slopes. Field data show that all the boulders are composed of basalt rocks with columnar joints, and that there is a long-axis isotropy related to the elevation and gradient of slope. In addition, the result of TPI and slope analysis for DEM indicate that block stream was mainly distributed along the valley, and the talus appeared in the steep ridge and the lower part of the cliffs. The slope classification indicates that flat mountain tops, basalt cliffs, talus, and block streams develop in sequence, as the distance from the center of the mountain increases. The bouldery landforms of Unbongsan Mountain illustrate the process of slope change that appears as a slope retreat in a volcanic edifice.
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