• Title/Summary/Keyword: relative travel time

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A Study on the Integrity Assessment of Bare Concrete Bridge Deck based on the Attenuation of Radar Signals (레이더 신호의 감쇠특성을 고려한 일체식 콘크리트 교량 바닥판의 상태평가 방법 고찰)

  • Rhee, Ji-Young;Choi, Jae-Jin;Kim, Hong-Sam;Park, Ko-Eun;Choi, Myeong-Jin
    • Journal of the Korea institute for structural maintenance and inspection
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    • v.20 no.4
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    • pp.84-93
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    • 2016
  • The signal characteristic of radar wave on concrete decks is determined by the attenuation of the radar due to the conversion of EM(Electromagnetic) energy to thermal energy through electrical conduction, dielectric relaxation, scattering, and geometric spreading. In this study, it is found that the attenuation of radar signal received on top rebars in bare deck concrete with 2 way travel time shows a general decreasing linear trend because of its same relative permittivity and conductivity. The radar signal after depth-normalization, can then be interpreted as being principally influenced by the content of chlorides penetrating cover concrete, which caused corrosion of rebars in bridge decks.

Crustal Structure of the Korean Peninsula By Travel Time Inversion of Local Earthquakes

  • Song, Seok-Gu;Lee, Gi-Hwa
    • Journal of the Korean Geophysical Society
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    • v.4 no.1
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    • pp.21-33
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    • 2001
  • Simultaneous inversion of first-arrivals of local earthquakes recorded by the Korea Meteorological Administration(KMA) seismograph network from 1991 to 1998 is made to derive 1D crustal velocity structure of the Korean peninsula. Twenty-nine events with 178 observations are used in the inversion. Average crustal P-wave velocity turns out to be about 6.3 km/sec, and crustal thickness and upper mantle P-wave velocity are estimated as 33 km and 7.9 km/sec, respectively. Results of inversion indicate the possibility of the low velocity layer in the lower crust. Joint inversion is applied to estimate hypocenters, station delays, and velocities simultaneously. Relative station corrections for 11 stations range from zero to about 1.2 sec. Analysis of the synthetic data shows that estimates of hypocenter locations and station corrections as well as averaged crustal structure are reliable for the given data set..

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Teleseismic Travel Time Tomography for the Mantle Velocity Structure Beneath the Melanesian Region (원거리 지진 주시 토모그래피를 이용한 멜라네시아 지역의 맨틀 속도 구조 연구)

  • Jae-Hyung Lee;Sung-Joon Chang
    • Economic and Environmental Geology
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    • v.57 no.1
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    • pp.1-15
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    • 2024
  • The Melanesian region in the western Pacific is dominated by complex plate tectonics, with the largest oceanic plateau, the OntongJava plateau, and a hotspot, the Caroline Islands. To better understand the complex geodynamics of the region, we estimate P- and S-velocity models and 𝛿 (VP/VS) model by using relative teleseismic travel times measured at seismometers on land and the seafloor. Our results show high-velocity anomalies in the subduction zones of the Melanesian region to a depth of about 400 km, which is thought to be subducting Solomon Sea, Bismarck, and Australian plates along plate boundaries. Along subduction zones, positive 𝛿 (VP/VS) anomalies are found, which may be caused by partial melting due to dehydration. A broad high-velocity anomaly is observed at 600 km depth below the Ontong-Java plateau, with a negative 𝛿 (VP/VS) anomaly. This is thought to be a viscous and dry remnant of the Pacific plate that subducted at 45-25 Ma, with a low volume of fluids due to dehydration for a long period in the mantle transition zone. Beneath the Caroline Islands, a strong low-velocity anomaly is obseved to a depth of 800 km and appears to be connected to the underside of the remnant Pacific plate in the mantle transition zone. This suggests that the mantle plume originating in the lower mantle has been redirected due to the interaction with the remnant Pacific plate and has reached its current location. The mantle plume also has a positive 𝛿 (VP/VS) anomaly, which is thought to be due to the influence of embedded fluids or partial melting. A high-velocity anomaly, interpreted as an effect of the thick lithosphere beneath the Ontong-Java plateau, is observed down to 300 km depth with a negative 𝛿 (VP/VS) anomaly, which likely indicate that little fluid remains in the melt residue accumulated in the lithosphere.

The Effect of Rain on Traffic Flows in Urban Freeway Basic Segments (기상조건에 따른 도시고속도로 교통류변화 분석)

  • 최정순;손봉수;최재성
    • Journal of Korean Society of Transportation
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    • v.17 no.1
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    • pp.29-39
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    • 1999
  • An earlier study of the effect of rain found that the capacity of freeway systems was reduced, but did not address the effects of rain on the nature of traffic flows. Indeed, the substantial variation due to the intensity of adverse weather conditions is entirely rational so that its effects must be considered in freeway facility design. However, all of the data in Highway Capacity Manual(HCM) have come from ideal conditions. The primary objective of this study is to investigate the effect of rain on urban freeway traffic flows in Seoul. To do so, the relations between three key traffic variables(flow rates, speed, occupancy), their threshold values between congested and uncontested traffic flow regimes, and speed distribution were investigated. The traffic data from Olympic Expressway in Seoul were obtained from Imagine Detection System (Autoscope) with 30 seconds and 1 minute time periods. The slope of the regression line relating flow to occupancy in the uncongested regime decreases when it is raining. In essence, this result indicates that the average service flow rate (it may be interpreted as a capacity of freeway) is reduced as weather conditions deteriorate. The reduction is in the range between 10 and 20%, which agrees with the range proposed by 1994 US HCM. It is noteworthy that the service flow rates of inner lanes are relatively higher than those of other lanes. The average speed is also reduced in rainy day, but the flow-speed relationship and the threshold values of speed and occupancy (these are called critical speed and critical occupancy) are not very sensitive to the weather conditions.

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Analysis on Leisure ViewPoint of Immigrant Female of Multi-Cultural Families (다문화가정 이주여성의 여가관 분석)

  • Yun, Min-Sook;Lee, Jeng-Heun;Kim, Jeong-Ryeon
    • The Journal of the Korea Contents Association
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    • v.11 no.6
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    • pp.337-349
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    • 2011
  • The purpose of this research is to elucidate the analysis on leisure viewpoint of immigrant female of multi-cultural families. This survey research have been performed with 140 of immigrant females who participate to the program of multi-cultural families support center located in Kyungki-do, Taejeon city, Chungnam-do and Chungbuk-do in 2010 by purposive sampling method. The final analysis was obtained from the survey results of total 89 immigrant females and the credibility of this survey represented Cronbach's ${\alpha}$ value above .613. The apparent results were the follows: First, the major leisure time of immigrant females of multi-cultural families on week days as well as weekend represented to be 1~2 hours. Second, the satisfaction on leisure activity of immigrant females was average level. Third, the best preference as leisure activity was travel. Fourth, their husbands were the favor partner for leisure activity of immigrant females. Fifth, the restriction on leisure activity of immigrant females showed some differences based on age, academic background, nationality and residence period. That is, personal restriction of age was below 25 years old, the highest personal and relative restriction of academic background represented in immigrant females below middle school graduator. Furthemore, the structural restriction and personal restriction on nationality showed the highest in the china and phillippine females, relatively. Personal restriction on residence period was mainly represented in immigrant females residing during 2.1~4 years.