• Explosives and Blasting
• /
• v.21 no.1
• /
• pp.95-101
• /
• 2003

자연 기상현상의 재해는 인간의 힘으로 극복하기 매우 어렵다. 그 중 낙뢰는 기상 재해로 뇌운과 지면사이의 방전 현상을 말한다. 한반도는 기단이 해상을 통과 하면서 많은 에너지를 공급받아 쉽게 뇌운이 형성된다. 기상청의 자동 낙뢰 관측 장비에 의하면, 연간 1,300회 이상의 낙뢰가 발생 되는 것으로 알려져 있다. 낙뢰는 지사응로 방전되면서 인명·전자기기의 파손등 피해를 일으킨다. 특히 발파공법은 주로 지표 지중에서 실시되는 공법으로 낙뢰에 대하여 매우 취약하고, 그 피해 또한 심각하다. 본 연구는 화약발파 기술자들의 참고 자료로써 낙뢰에 대한 주의와 대책을 연구하는 뜻에서 작성한다.

• Proceedings of the Korean Institute of Navigation and Port Research Conference
• /
• 2018.05a
• /
• pp.203-205
• /
• 2018

최근 컨테이너 물동량 증가와 대형컨테이너 선박의 입항으로 부산항 신항내 선박통항안전성 문제가 대두됨에 따라 신항내 해상교통안전성 확보를 위하여 2017년 토도를 제거하는 공사가 추진되었으며 이와 병행하여 주변 해역을 준설 하는데 목적을 둔 부산항 신항 토도 제거 공사의 주요공법 및 착공 후 현재까지의 주요 공정현황을 요약하였다. 국내 최초로 시행되는 통항안전을 위한 현장 섬의 제거과정에 기존 항로를 유지하면서 단계별 투입장비 및 공법, 주변 환경여건을 고려한 육상 및 해상 공정 조정, 장래 비전 등을 제시하였다.

• Journal of the Korean Geotechnical Society
• /
• v.29 no.9
• /
• pp.17-29
• /
• 2013

The geophysical methods have an advantage for investigating the wide area with low cost, and thus the application of these methods has been increased. The objective of this paper estimates the characteristics of alluvium through the geophysical methods including elastic wave, electrical resistivity and ground penetration radar. And the standard penetration test is also carried out for verifying the geophysical data with comparison. The sources of elastic wave method are divided into hammer and sissy and the electrical resistivity method is applied with different sizes, shapes and arrays of electrode for deciding the effective way. The center frequency is determined to be 270 MHz for considering the characteristics of soil. The results of ground penetration radar are also compared with those of standard penetration test. The high resolution shows when the source is a sissy in elastic wave method, however, the water level is not identified. In the electrical resistivity method, the non-polarizable electrode and schlumberger array show highly reliable data and the resolution of ground penetration radar is low. Thus, the results of this study are widely applied for determining the appropriate method when investigating the characteristics of alluvium.

• The Journal of Engineering Geology
• /
• v.4 no.2
• /
• pp.187-206
• /
• 1994

Through a computer model study, optimum system configuration and field parameters were determined for high-resolution marine reflection surveys. Characteristics of far-field signatures were analysed in both time and frequency domains for the six individual R/V Onnuri. The analysis shows that the cluster fired at the depth of 2m below the sea surface generates the most ideal far-field signatures among the above seismic sources. Compared with the 96-channel streamer on the R/V Onnuri, the 12-channel streamer is suitable for shallow reflection profiling due to its high resolution both in the vertical and horizontal directions despite its lower signal-to-noise ratio. Considering factors including target depth, frequency range, airgun volume, number of recording channels, and capacity of compressors, optimum values for record length, sample period, and shot interval are believed to be is, 1ms, and 3.125m or 6.25m, respectively.

• Geophysics and Geophysical Exploration
• /
• v.6 no.3
• /
• pp.126-133
• /
• 2003

High-resolution shallow marine seismic surveys have been carried out for the resources exploration, engineering applications and Quaternary mapping. To improve the resolution of subsurface structure image, multichannel digital technique has been applied. The quality of the image depends on the vertical and horizontal resolution and signal to noise (S/N) ratio which are associated with the data acquisition parameters such as sample interval, common midpoint (CMP) interval and CMP fold. To understand the effect of the acquisition parameters, a test survey was carried out off Yeosu and the acquired data were analyzed. A 30 $in^3$ small air gun was used as a seismic source and 8 channel streamer cable with a 5 m group interval was used as a receiver. The data were digitally recorded with a shot interval of 2 s and sample interval of 0.1 ms. The acquired data were resampled with various sample intervals, CMP intervals and CMP folds. The resampled data were processed, plotted as seismic sections and compared each other. The analysis results show that thin bed structure with ${\~}1m$ thickness and ${\~}6^{\circ}$ slope can be imaged with good resolution and continuity and low noise using the acquisition parameters with a sample interval shorter than 0.2 ms, CMP interval shorter than 2.5 m and CMP fold more than 4. Because seismic resolution is associated with the acquisition parameters, the quality of the subsurface structure can be imaged successfully using suitable and optimum acquisition parameters.

• The Journal of Engineering Geology
• /
• v.3 no.2
• /
• pp.167-176
• /
• 1993

The high resolution studies for shallow seismic reflection are carried out using 24-channel seismograph and the high sensitivity geophone(50-500Hz). In order to study the underground structures such as small faults, fractures, cracks and cavities, it is of great importance to enhance high resolution of the seisrnic records for the targets vertically and laterally. In analysis of high resolution seismic reflection, Nyquist frequency($F_N$) should be lager than the highest frequency in the records and the highest wave number should not be exceed the Nyquist wave number($1/2{\Delta}x$). The highest frequency above the Nyquist will be removed using low pass filter or antialias filter. The trace interval Ax should be taken into account so that the highest wave number(f/v) can be less than $1/2{\Delta}x$. The Fraunhofer diffraction of a hyperbola seismic section above the tunnel appeares on the common offset method, and little first arrivals of direct wave on the single-end shooting, delayed strong impulsive reflections are also shown above the tunnel. Ray Method(Cherveney and Psencik, 1983) also represents the same results that the reflected waves from the tunnel are delayed and single impulsive with little first arrivals, while transrnitted waves through the tunnel are delayed with low frequency.

• Geophysics and Geophysical Exploration
• /
• v.7 no.4
• /
• pp.245-250
• /
• 2004

Horizontal-axes on the seismic section have been represented in a distance unit by applying horizontal-distance correction transformation on a 2-D seismic section of single channel marine seismic data. By drawing horizontal-axes in a distance unit, distortion of horizontal distances shown on the seismic section when the ship speed varies during a survey can be diminished considerably. Position information obtained by GPS and stored in each trace of seismic data as well as data collection windows were used for horizontal distance correction. The minimum window length was decided by considering ship speed and shot interval, and the maximum window length wat determined by reflecting radius of the 1st Fresnel zone. In choosing an optimum window length, horizontal resolution and stacking effect were considered simultaneously. By applying horizontal distance correction we could get a 2-D seismic section which is considered at reflecting the real subsurface structure analogously.