关于LCM方程的李-曹猜想的注记

在研究Hong关于定义在gcd封闭集上的幂LCM矩阵［Se］(e为正整数)的非奇异性的一个猜想时,李和曹研究了如下的不定方程(称为LCM方程)：1lcmy1,y2,y3,y4-4i=11yi+1gcd(y1,y2)+1gcd(y1,y3)+1gcd(y2,y3)[SX)]=0.他们首先证明了当ω(y)＜4时,方程无解,这里y=lcm［y1,y2,y3,y4］,ω(y)表示y的不同素因子的个数;然后他们给出ω(y)=4且y=p21p22p23p2m4时,方程有2次幂整数解的必要条件,这里pi为不同素数,m≥1;根据这些必要条件他们接着验证了方程当y≤1 334 025时没有2次幂整数解;最后他们提出猜想：若n≤9,则定义在gcd封闭集S={x1,…,xn}上的平方LCM矩阵［S2］是非奇异的,即LCM方程没有2次幂整数解.本文作者推广了李-曹关于LCM方程有2次幂整数解的研究：首先给出了当ω(y)=4且y=p2m11p2m22p2m33p2m44时,方程有2次幂整数解的必要条件,并给出了当ω(y)≥4时,方程解的表达式(如果存在的话),这里pi为不同素数,mi≥1;然后根据这些必要条件在计算机上验证了方程当y≤260 620 460 100时没有2次幂整数解,进一步支持了李-曹猜想.     

关于不定方程4x~2-py~2=1

研究了二次不定方程4x2-py2=1(p为奇素数),对于特例p=m2±2(m为正奇数),利用Pell方程x2-py2=1的正整数解公式得到了原方程的所有正整数解.另外还证明了p=1,5(mod8)时方程4x2-py2=1无正整数解.     

关于Tijdeman猜想(Ⅱ)

1989年Tijdeman猜想设a,b,c是互素的正整数,m,n,r是大于1的正整数,则方程ax m+by n=cz r在1/m+1/n+1/r<1时仅有有限多组整数解;本文利用数论方法及Fermat无穷递降法,证明了丢番图方程x 8+my 4=z 2在m=±p,±2p,±4p,±8p及素数p满足一定条件下无正整数解,完善了Mordell等人的结果;并且获得了方程x 4-2py 4=z 2和x 4+8py 4=z 2的无穷多组正整数解的通解公式,从而获得了Tijdeman猜想与广义Fermat猜想的研究进展.     

表方幂为连续的阶乘和

考虑方程a^m=n!＋（n＋1）!＋……＋（n＋k）!,其中a〉1,m〉1,n≥1．我们证明了当a≠0 mod 223092870时,方程所有的解是2^3=2!＋3!,3^2=1!＋2!＋3!,2^5=2!＋3!＋4!,12^2=4!＋5!;当a=0 mod 223092870时,令p是满足p=a的最小素数,如果方程有解,则m≤p．而且,我们猜想上述的四个解是方程仅有的解．     

方程φ(n)=2tw(n)(t∈Z+)的解

利用初等方法研究了方程φ(n)=2tw(n)(t∈Z+)的可解性,给出了两个平凡解和其它一般解必有形式n=2mp1p2…pk(m≥0,k≥1,p1相似文献   

方程xp±y2p=z2与广义费尔马猜想

设p为奇素数,证明了丢番图方程x4 -y4 =zp 与x2p±y2p=z2 均无正整数解;方程xp y2p=z2 仅有整数解 16 2 3 =32 ;方程x2p 2 kyp =z2 (k≥ 1)仅有整数解 12p 2 3 · 1p =32 ;同时还获得了方程x2 ±y4 =zp与x2 ±y4 =±z2p 的深刻结果,从而很大程度地支持广义Fermat猜想.     

关于丢番图方程x3±1=py2

应用因子分解法、简单同余法以及前人的已知结果证明了:(1)设p是1个奇素数,则丢番图方程组x+1=3py21,x2-x+1=3y22,(y1,y2)=1,y1>0,y2>0,无正整数解x,p,y1,y2;(2)丢番图方程x3+1=py2(其中p≡-1(mod 3)为素数)仅有整数解(x,y)=(-1,0);(3)丢番图方程x3-1=py2(其中p≡-1(m od 3)为素数)仅有整数解(x,y)=(1,0).     

关于丢番图方程2py~2=2x~3+3x~2+x的解

本文运用初等数论简单同余法、分解因子法及反证法等,得到丢番图方程2py2=2x3+3x2+x,(p为素数)无正整数解的情况.(1)当p≡1(mod 8),p≡5(mod 8),p≡7(mod 8)时,则方程无正整数解;(2)当p≡3(mod 8)时,Un+Vnp(1/2)=(x0+y0p(1/2))n.其中x0,y0是Pell方程x2-py2=1的基本解,当n≡0(mod 2)时,则方程无整数解;当n≡1(mod 2)时,若2|x0,则方程无整数解.特别是p≡3(mod 8)且p100时,2|x0,则方程无整数解.     

关于不定方程∏nk=1(k2+1)=a·m2的探讨

对于不定方程∏nk=1(k2+1)=a·m2,J. Cilleruelo证明了当a=1时,当且仅当n=3方程有解.证明了当a=5和7时,此方程无解;当a=17时,方程只有唯一解;还证明了一般情形,当a满足(a,17×101×1 297×739 601)=1且a的最大素因子p(a)≤2×738 740时,当n>3,方程无解.     

关于丢番图方程p~2-2q~2=-1

Berger在关于有限群的工作中提出了丢番图方程p~m-2q~n=±,p.q素数,m>1,n>1.(1)Grescenzo在1975年对此进行了研究。并问:是否存在无穷多对素数(p.q)适合p~2-2q~2=±1,p.q素数 (2)对于方程p~2-2q~2=1.模4立刻得到该方程有唯一素数解p=3.q=2。困难的是丢番图方程p~2-2q~2=-1,p.q素数 (3)对于方程(3),目前还没有什么结果。本文通过研究pell数的性质,得到一糸列(2)有解的必要条件     

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.     

Features of Women's language

Language is a means of verbal communication. People use language to communicate with each other. In the society, no two speakers are exactly alike in the way of speaking. Some differences are due to age, gender, statue and personality. Above all, gender is one of the obvious reasons. The writer of this paper tries to describe the features of women＇s language from these perspectives： pronunciation, intonation, diction, subjects, grammar and discourse. From the discussion of the features of women＇s language, more attention should be paid to language use in social context. What＇s more, the linguistic phenomena in a speaking community can be understood more thoroughly.     

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.