• 한국자기학회지
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• 제20권5호
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• pp.173-177
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• 2010

이 연구에서는 각분해 광전자 분광법(angle-resolved photoemission spectroscopy: ARPES)을 시용하여 전하밀도파(chargedensity-wave: CDW)를 형성하는 물질인 $CeTe_2$의 전자구조를 연구하였다. $CeTe_2$의 ARPES 데이터에서는 분산적인 띠들이 분명하게 관찰되었다. $CeTe_2$의 일정에너지(constant energy: CE) 맵에서는 4중 대칭성(fourfold symmetry)이 관찰되었으며, 그 형태가 문헌에 있는 $CeTe_2$의 CE 맵과 유사하였다. 이러한 발견은 $CeTe_2$의 CDW 형성이 $2{\times}2$ 형태의 살창 변형에 의한 것임과 4f 전자들이 $CeTe_2$의 CDW 형성에 별다른 기여를 하지 않는다는 것을 나타낸다. 이 연구로부터 $CeTe_2$에서 페르미 준위 근처의 전자들은 주로 Te(1) 5p와 Ce 5d 전자들이며 Te(1) 5p 전자들에 의한 띠가 CDW 형성에 기여하고 Ce 5d 전자들에 의한 띠는 CDW 상태에서도 페르미 준위를 가로지르는 금속성을 나타낸다는 것을 알 수 있었다.

• 한국지진공학회논문집
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• 제26권5호
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• pp.191-202
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• 2022

Markov envelope as a theoretical solution of the parabolic wave equation with Markov approximation for the von Kármán type random medium is studied and approximated with the convolution of two probability density functions (pdf) of normal and gamma distributions considering the previous studies on the applications of Radiative Transfer Theory (RTT) and the analysis results of earthquake records. Through the approximation with gamma pdf, the constant shape parameter of 2 was determined regardless of the source distance r_o. This finding means that the scattering process has the property of an inhomogeneous single-scattering Poisson process, unlike the previous studies, which resulted in a homogeneous multiple-scattering Poisson process. Approximated Markov envelope can be treated as the normalized mean square (MS) envelope for ground acceleration because of the flat source Fourier spectrum. Based on such characteristics, the path duration is estimated from the approximated MS envelope and compared to the empirical formula derived by Boore and Thompson. The results clearly show that the path duration increases proportionately to r_o^1/2-r_o², and the peak value of the RMS envelope is attenuated by exp (-0.0033r_o), excluding the geometrical attenuation. The attenuation slope for r_o≤100 km is quite similar to that of effective attenuation for shallow crustal earthquakes, and it may be difficult to distinguish the contribution of intrinsic attenuation from effective attenuation. Slowly varying dispersive delay, also called the medium effect, represented by regular pdf, governs the path duration for the source distance shorter than 100 km. Moreover, the diffraction term, also called the distance effect because of scattering, fully controls the path duration beyond the source distance of 300 km and has a steep gradient compared to the medium effect. Source distance 100-300 km is a transition range of the path duration governing effect from random medium to distance. This means that the scattering may not be the prime cause of peak attenuation and envelope broadening for the source distance of less than 200 km. Furthermore, it is also shown that normal distribution is appropriate for the probability distribution of phase difference, as asserted in the previous studies.