关于某些矩阵行列式的Minkowski型不等式

关于实对称正定矩阵的行列式,有著名的Minkowski不等式(见参考文献)|A+B|~(1/n)≥|A|~(1/n)+|B|~(1/n) 本文将上述不等式推广至某些非对称正定的情况,建立类似的一些不等式。     

关于正定矩阵的一个行列式不等式

本文讨论正定的厄米特(Hermite)矩阵的一个行列式不等式,即定理设■是n阶正定的厄米特矩阵(简称正定阵),n—r>1,则|H|≤|A|·|C|—|A|·|B·A~(-1)B|,(1)且等式成立的充要条件是B=0。     

对称矩阵特征值估计的某些进展

如果λ_1,…,λ_n是对称矩阵A的特征值,P. Tarazaga证明了|tr(A)/n-λ_i|≤[(n-1)/n(‖A‖_F~2-tr(A)~2/n)]~(1/2)对λ_i,i=1,…,n。本文中得到了一个等式成立的充分必要条件,由此给出一类特殊对称矩阵特征值的计算方法,而且证明了下面的定理:如果对称正定矩阵A仅有k个特征值大于或等于αtr(A),0<α<1,则tr(A)/‖A‖_F≥P_k(α)~(1/2),其中P_k(α)~(-1)=[1-(k-1)α]~2+(k-1)α~2,进而得到正定对称矩阵每一个特征值的上界估计。     

球面上k-极值子流形的Pinching定理

令M~n是n维单位球空间S~(n+p)(n≥3)中的紧致k-极值子流形(1≤kn/2),证明当(∫_(M~n)ρ~ndv)2/nC时,|A|~2=nH~2且M~n全脐,其中C依赖于n,p,M~n.记ρ~2=|A|~2-nH~2,H和|A|~2分别表示Mn的平均曲率和第2基本型模长平方.     

广义对角占优矩阵的一些性质

<正>设A=(ajk)（n×n）为n阶复矩阵(本文记为A∈Cn×n,记oj=sum from k=1 k≠j to n |ajk|,j=1,...,n若|ajj|>aj,j=1,…,n,则称a为（按行）严格对角占优矩阵.若（?）=1/2（A+Ax）为严格对角占优矩阵,则称A为共轭（严格）对角占优矩阵.关于各类对角占优矩阵特征值的分布,已在文     

关于矩阵乘积的奇异值的一个不等式及其应用

约定 A(≥0)>0为(半)正定 Hermite 矩阵。如果复矩阵 A=(a_(ij))(∈C~(n×n))的特征值都是实数,规定其特征值满足λ_1(A)≥…≥λ_n(A),用σ_1(A)≥…≥σ_n(A)表示 A 的n 个奇异值,规定{δ_1(A),…,δ_n(A)}与{a_(11),……,a_(nn)}为同一集合且|δ_1(A)≥…≥|δ_n(A)|。当实向量 x=(x_1,…,x_n)与 y=(y_1,…,y_n)的分量按递减顺序排列为 x_[1]≥…≥X_[n]与 y_[1]≥…≥y_[n]时,若(?)X_(i)≤(?)y_[i],k=1,2,…,n,则称 y 弱控制 x,记为 x相似文献   

线性空间的分解与若当标准形

本文证明了下面两点:(1)设A 是n×n 矩阵,那么A 相似于(?)为若当块矩阵,它仅有一个特征值和一个线性无关的特征向量.(2)者|λI-A|=(λ-λ_1)~(r_1)-(λ-λ_2)~(r_2)…(λ-λ_3)~(r_3),其中λ_1,λ_2,…,λ_3两两不同,那么dimN(A-λI)~(r(?))=r_(?)(i=1,2,…,8)其中Ⅳ(A-λ_1I)~(r(?))={α|α∈U~n,(A-λI)~(r(?))·α=0}.U~n 是n 维列向量.     

求矩阵的广义逆

利用行式和列式的性质,给出了两种求矩阵广义逆的方法:1.伴随矩阵法,若m×n矩阵A的行(列)式|A|≠0,则1|A|A*是矩阵A的广义逆.2.如果m×n矩阵A是满秩的,且A的子式Ni1i2…irj1j2…jr(r=min(m,n))的行列式不等于零,则pN-112…mj1j2…jm0或Nii1i2…in12…n0P是矩阵A的一个广义逆.     

积和式变差的几点注

L.Elsner和R.Bhatia给出了n阶方阵A、B的积和式的变差的估计为|per(A)—per(B)|≤n||A—B||,max(||A||_p,||B||_p)~(n-1),p∈{1,2,∞}.L.Elsner猜测上式对任何范数都成立。我们指出对一些||I|_p>1的p—范数也成立。当A、B为长方阵时,我们给出了一些相应的结果。     

k-正则图中第二大特征值和最小特征值的界

运用n阶矩阵B=(b_(ij))≥0的第二大特征值的结果,结合图论的背景,得出了n阶k-正则图G的第二大特征值θ_2(A(G))≤k-(?){|N_i∩N_j|},最小的特征值θ_n(A(G))满足:θ_n(A(G))≥-1-(?){k-|N_i∩N_j|-1,k- |N_i∩N_j| 1}.     

Markedness and its Interpretation in Language Use

Language markedness is a common phenomenon in languages, and is reflected from hearing, vision and sense, i.e. the variation in the three aspects such as phonology, morphology and semantics. This paper focuses on the interpretation of markedness in language use following the three perspectives, i.e. pragmatic interpretation, psychological interpretation and cognitive interpretation, with an aim to define the function of markedness.     

Lower Paleozoic oil relationships within Williston Basin, Canada

The Williston Basin is a significant petroleum province, containing oil production zones that include the Middle Cambrian to Lower Ordovician, Upper Ordovician, Middle Devonian, Upper Devonian and Mississippian and within the Jurassic and Cretaceous. The oils of the Williston Basin exhibit a wide range of geochemical characteristics defined as "oil families", although the geochemical signature of the Cambrian Deadwood Formation and Lower Ordovician Winnipeg reservoired oils does not match any "oil family". Despite their close stratigraphic proximity, it is evident that the oils of the Lower Palaeozoic within the Williston Basin are distinct. This suggests the presence of a new "oil family" within the Williston Basin. Diagnostic geochemical signatures occur in the gasoline range chromatograms, within saturate fraction gas chromatograms and biomarker fingerprints. However, some of the established criteria and cross-plots that are currently used to segregate oils into distinct genetic families within the basin do not always meet with success, particularly when applied to the Lower Palaeozoic oils of the Deadwood and Winnipeg Formation.     

An Analysis of Catherine＇s Character——Wuthering Heights

Wuthering Heights, Emily Bronte＇s only novel, was published in December of 1847 under the pseudonym Ellis Bell. The book did not gain immediate success, but it is now thought one of the finest novels in the English language. Catherine is the key character of this masterpiece, because everybody and everything center on her though she had a short life. We can understand this masterpiece better if we know Catherine well.     

Characterization of Ordovician carbonate reservoirs, southeastern Saskatchewan, Canada

The discovery of the prolific Ordovician Red River reservoirs in 1995 in southeastern Saskatchewan was the catalyst for extensive exploration activity which resulted in the discovery of more than 15 new Red River pools. The best yields of Red River production to date have been from dolomite reservoirs. Understanding the processes of dolomitization is, therefore, crucial for the prediction of the connectivity, spatial distribution and heterogeneity of dolomite reservoirs.The Red River reservoirs in the Midale area consist of 3～4 thin dolomitized zones, with a total thickness of about 20 m, which occur at the top of the Yeoman Formation. Two types of replacement dolomite were recognized in the Red River reservoir: dolomitized burrow infills and dolomitized host matrix. The spatial distribution of dolomite suggests that burrowing organisms played an important role in facilitating the fluid flow in the backfilled sediments. This resulted in penecontemporaneous dolomitization of burrow infills by normal seawater. The dolomite in the host matrix is interpreted as having occurred at shallow burial by evaporitic seawater during precipitation of Lake Almar anhydrite that immediately overlies the Yeoman Formation. However, the low δ18O values of dolomited burrow infills (-5.9‰～ -7.8‰, PDB) and matrix dolomites (-6.6‰～ -8.1‰, avg. -7.4‰ PDB) compared to the estimated values for the late Ordovician marine dolomite could be attributed to modification and alteration of dolomite at higher temperatures during deeper burial, which could also be responsible for its 87Sr/86Sr ratios (0.7084～0.7088) that are higher than suggested for the late Ordovician seawaters (0.7078～0.7080). The trace amounts of saddle dolomite cement in the Red River carbonates are probably related to "cannibalization" of earlier replacement dolomite during the chemical compaction.     

Design and analysis of generic LBS application developing platform

Location based services is promising due to its novel working style and contents.A software platform is proposed to provide application programs of typical location based services and support new applications developing efficiently. The analysis shows that this scheme is easy implemented, low cost and adapt to all kinds of mobile nework system.     

橡胶颗粒沥青混合料低温抗裂性试验研究

以AC-13级配为基础,将橡胶颗粒代替部分集料掺入混合料中,以低温弯曲试验为评价方法对不同橡胶颗粒掺量下沥青混合料的低温抗裂性进行研究,并引入应变能密度值对混合料的低温抗裂性进行综合评价.试验结果表明:橡胶颗粒沥青混合料试件的破坏微应变均超过2 300,满足冬寒区的技术指标;无论是否掺加橡胶颗粒,随着温度的下降,沥青混合料破坏时的最大弯拉强度增大,弯拉应变降低,劲度模量增大;弯曲应变能密度在胶粒掺量为1%左右时具有较大的弯曲应变能密度值,此时橡胶颗粒沥青混合料具有较好的低温抗裂性.     

A computer generator for randomly layered structures

AcomputergeneratorforrandomlylayeredstructuresYUJia shun1,2,HEZhen hua2(1.TheInstituteofGeologicalandNuclearSciences,NewZealand;2.StateKeyLaboratoryofOilandGasReservoirGeologyandExploitation,ChengduUniversityofTechnology,China)Abstract:Analgorithmisintrod…     

低渗透非均质砂岩油藏启动压力梯度研究

理论推导与室内实验相结合,建立了低渗透非均质砂岩油藏启动压力梯度确定方法。首先借助油藏流场与电场相似的原理,推导了非均质砂岩油藏启动压力梯度计算公式。其次基于稳定流实验方法,建立了非均质砂岩油藏启动压力梯度测试方法。结果表明:低渗透非均质砂岩油藏的启动压力梯度确定遵循两个等效原则。平面非均质油藏的启动压力梯度等于各级渗透率段的启动压力梯度关于长度的加权平均;纵向非均质油藏的启动压力梯度等于各渗透率层的启动压力梯度关于渗透率与渗流面积乘积的加权平均。研究成果可用于有效指导低渗透非均质砂岩油藏的合理井距确定,促进该类油藏的高效开发。     

Quantitative trait loci （QTLs） for quality traits related to protein and starch in wheat

Quality traits in wheat （Triticum aestirum L.） were studied by quantitative trait locus （QTL） analysis in a recombinant inbred line （RIL） population, a set of 131 lines derived from Chuan 35050 × Shannong 483 cross （ChSh）. Grains from RILs were assayed for 21 quality traits related to protein and starch. A total of 35 putative QTLs for 19 traits with a single QTL explaining 7.99-40.52% of phenotypic variations were detected on 10 chromosomes, 1D, 2A, 2D, 3B, 3D, 5A, 6A, 6B, 6D, and 7B. The additive effects of 30 QTLs were positive, contributed by Chuan 35050, the remaining 5 QTLs were negative with the additive effect contributed by Shannong 483. For protein traits, 15 QTLs were obtained and most of them were located on chromosomes 1 D, 3B and 6D, while 20 QTLs for starch traits were detected and most of them were located on chromosomes 3D, 6B and 7B. Only 7 QTLs for protein and starch traits were co-located in three regions on chromosomes 1D, 2A and 2D. These protein and starch trait QTLs showed a distinct distribution pattern in certain regions and chromosomes. Twenty-two QTLs were clustered in 6 regions of 5 chromosomes. Two QTL clusters for protein traits were located on chromosomes 1D and 3B, respectively, three clusters for starch traits on chromosomes 3D, 6B and 7B, and one cluster including protein and starch traits on chromosome 1D.     

On Tragic Consciousness In The Works By Ernest Hemingway

As an American modern novelist who were famous in the literary world, Hemingway was not a person who always followed the trend but a sharp observer. At the same time, he was a tragedy maestro, he paid great attention on existence, fate and end-result. The dramatis personae's tragedy of his works was an extreme limit by all means tragedy on the meaning of fearless challenge that failed. The beauty of tragedy was not produced on the destruction of life, but now this kind of value was in the impact activity. They performed for the reader about the tragedy on challenging for the limit and the death.