통합 검색 | Korea Science

최희봉;원동호
- 정보보호학회논문지
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- 제11권1호
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- pp.35-42
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- 2001
GF(q)상의 원시다항식은 스크램블러, 에러정정 부호 및 복호기, 난수 발생기 그리고 스트림 암호기 등 여러 분야에 걸쳐 많이 사용되고 있다. GF(q)상의 원시다항식을 생성하는 효율적인 알고리즘이 A.D. Porto에 의하여 제안되었으며, 그 알고리즘은 한 원시다항식을 이용하여 다른 원시다항식을 구하는 방법을 반복 사용하여 원시다항식 수열을 생성하는 방법이다. 이 논문에서는 A.D. Porto가 제안한 알고리즘을 개선한 알고리즘을 제안하였다. A.D. Porto의 알고리즘의 running time은 O($\textrm{km}^2$)이고, 개선된 알고리즘 running time은 O(w(m+k))이다. 여기서 k는 gcd(k,$q^m$-1)이 다. m차 원시다항식을 구하고자 할 때 k, m>>1 조건에서는 개선된 알고리즘을 사용하는 것이 효율적이다.
https://doi.org/10.13089/JKIISC.2001.11.1.35 인용 PDF

김영숙;김성수
- 아동학회지
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- 제22권4호
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- pp.257-269
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- 2001
This study identified and explained the prototypes of teacher's belief about children's play with the use of Stephenson's Q-methodology. The sample consisted of 35 kindergarten teachers. A Q-deck composed of 48 cards, derived in part from a review of related literature and was developed by the researchers and sorted by the subjects. The obtained Q-sort scores were analyzed by factor analysis. The findings revealed that the subjects were divided into 3 belief types : "life-experienced", "developmental-disciplinary", "cultural-environmental". Likely explanations for these results are considered, and implications are discussed.
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김성균
- 한국지진공학회:학술대회논문집
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- 한국지진공학회 1999년도 춘계 학술발표회 논문집 Proceedings of EESK Conference-Spring
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- pp.35-40
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- 1999
In order to know the characteristics of attenuation of coda wave in the Kyungsang Sedimentary Basin quality factor for coda wave or coda Q is estimated from the earthquake data recorded in the KIGAM microearthquake network. The single scattering model for coda wave generation is adopted in estimating coda Q. Coda Q appears to be largely dependent on the normalized time(a) which is the ratio of elapsed time to S-wave travel time. In the present study coda Q(Qc) is estimated in the range of a=1.5-3.Q and expressed in terms of frequency(f). The deduced function in the range of 1 to 25 Hz is Qc=36.8283 f1.15095 to represent the strong dependence of coda Q on frequency. It is found that the difference of Qc between U-D N-S and E-W components is negligible, This face supports the back-scattering theory that coda were originates from scattered waves by randomly distributed heterogeneities in the crust. On the other hand it is observed that the coda Q increases with depth.
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