排序方式: 共有47条查询结果,搜索用时 46 毫秒
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分别用二次电子扫描线法和垂直抛面法对不同回火制度的30SiMnCrNiMoB钢的冲击断口表面的分维数进行了数量。通过研究发现:平行裂纹扩展方向的分维更适合于描述材料韧性的变化。 相似文献
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对图G的能量ε(G)与K_(1,s)-匹配数μ_s(G)之间的关系进行了研究。证明了对于一般图G有■成立,进一步地,若其子图满足一定的条件,则有■,其中c_1(G)表示G中的奇圈数。还证明了若n阶树T的最大度小于等于3,有ε(T)≥(s+1)μ_s(T)-1成立。 相似文献
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HUANG Qiang SHEN Changxiang FANG Yanxiang 《武汉大学学报:自然科学英文版》2007,12(1):13-16
With analysis of limitations Trusted Computing Group (TCG) has encountered, we argued that virtual machine monitor (VMM) is the appropriate architecture for implementing TCG specification. Putting together the VMM architecture, TCG hardware and application-oriented "thin" virtual machine (VM), Trusted VMM-based security architecture is present in this paper with the character of reduced and distributed trusted computing base (TCB). It provides isolation and integrity guarantees based on which general security requirements can be satisfied. 相似文献
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设G是一个图,G的Tur(a)n数记作ex(n;G),是指阶数为n的不含G作为子图的图的最大边数.根据Erd(o)s在1965年给出的偶圈C2m的Tur(a)n数ex(n;C2m)的上界10mn1+1/m和Wenger在1991年构造的偶图Hm(q),并由这种图得到的ex(n;C2m)(m=2,3,5)的下界cn1+1/m(其中c为一个与n无关的常数),可以知道,当n→+∞时,ex(n;C2m)=O(n1+1/m)(m=2,3,5).n1+1/m就是ex(n;C2m)的准确阶.给出了Wenger图Hm(q)的一些一般性质,并分别构造了Hm(q)中长为8的圈(m≥4)和Hm(q)中长为12的圈(m≥6),
从而证明了不可能由图Hm(q)得到ex(n;C2m)的所有准确阶. 相似文献
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设G是一个图,G的Turan数记作ex(n;G),是指阶数为n的不含G作为子图的图的最大边数.根据Erdos在1965年给出的偶圈C2m的Turan数ex(n;C2m)的上界10mn^1+1/m和Wenger在1991年构造的偶图Hm(q),并由这种图得到的ex(n;C2m)(m=2,3,5)的下界cn^1+1/m(其中c为一个与n无关的常数),可以知道,当n→+∞时,ex(n;C2m)=O(n^1+1/m)(m=2,3,5).n^1+1/m就是ex(n;C2m)的准确阶.给出了Wenger图Hm(q)的一些一般性质,并分别构造了Hm(q)中长为8的圈(m≥4)和Hm(q)中长为12的圈(m≥6),从而证明了不可能由图Hm(q)得到ex(n;C2m)的所有准确阶. 相似文献
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芮昌祥 《云南大学学报(自然科学版)》1993,15(3):275-277
设F是任意域,M_n(x)表示多项式环F〔x〕上n×n矩阵半群。本文决定了全部从M_n(x)到F〔x〕的半群乘法同态,亦即M_n(x)的全部积性函数。 相似文献
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单圈图依次小Q-特征值排序 总被引:1,自引:1,他引:0
n阶图G叫做单圈图,如果G是连通的,并且G的边数也是n.图G的无符号拉普拉斯矩阵定义为Q(G)=D(G)+A(G),其中D(G)是以G所有顶点的度为对角元的对角阵,A(G)是图G的邻接矩阵.Q(G)是一个实对称的半正定矩阵,设它的特征值为q1(G)≥q2(G)≥…≥qn(G)≥0.图G的依次小Q-特征值为qn-1(G),简记为k(G).主要研究单圈图的k(G),记阶数为n的所有连通的单圈图的集合为U(n),给出了当阶数n≥25时,U(n)中依次小Q-特征值为前3大的图. 相似文献
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Evaluation of a 3dVAR system for the South China Sea 总被引:4,自引:0,他引:4
The authors evaluate a three-dimensional variational (3dVAR) system for the South China Sea (SCS) in this study. The assimilation method applied in the system takes into consideration error correlation along each ground track and uses recursive filter for optimiza- tion. Data from three R/V cruises during the spring and summer of 1998 and the summer of 2000 are used to evaluate the system. The root-mean-square error and bias are reduced significantly and when the altimeter data are assimilated, the distribution of the error is much closer to the Gaussian distribution. Precipitation and river discharge in the southwestern SCS are reproduced, and the variability of sea surface height is efficiently transferred to the subsurface. The 3dVAR system performs well for each of the three cruises, suggesting that it is steady for routine usage. 相似文献