水文频率曲线绘制的Matlab程序设计

基于目估适线法,选用皮尔逊Ⅲ型频率曲线作为水文频率分布线型,在Matlab平台上编写三个M文件,分别实现海森频率格纸的绘制、频率曲线参数x軃、Cv的求解以及水文频率曲线的绘制。通过多次的适配,找到与实测水文资料配合较好的理想曲线的参数作为设计值并估算指定的水文特征值。并以某一水文测站24年的年径流实测资料为基础,检验了方法的正确性。为水文学中相关计算以及水文频率曲线的绘制提供了一种新的实现方法。     

递推法求一元n次实系数多项式函数的完全等价n次Bezier参数曲线

用递推方法论证了至少存在一条n次Bezier参数曲线与一元n次实数多项式函数完全等价。同时给出了将一元n次实纱多项式转换为完全等价的n次Bezier参数曲线的方法。     

两个极限命题的证明

用归纳法证明了两个极限命题。(1)设m>1,pi(x)(i=1,2,…,m)是[1, ∞)上的连续正函数,在满足一定条件下成立li mx→ ∞∫1xtm-1p1(t)p2(t)…pm(t)dtxmp1(x)p2(x)…pm(x)=α2α3…αm α1α3α…1αα2m… αm… α1α2…αm-1(2)设pjn,an(j=1,2,…,m;n=1,2,…;m>1)均为正数,在满足一定条件下成立li mn→∞∑nk=1akm-1p1kp2k…pmkanmp1np2n…pmn=α2α3…αm α1α3α…1αα2m… αm… α1α2…αm-1     

二水固态草酸镁脱水的热分析动力学

经以下步骤求算二水固态草酸镁脱水的动力学三因子 :( 1)迭代法或 KAS法求出可靠的 Ea;( 2 )积分法Coats- Redfern方程和微分法 Achar方程相结合判定出可能的机理函数 ,并计算 A.得出 Ea 为 113.0 8k J· m ol- 1 ;A为 4 .35× 10 8～ 8.5 8× 10 1 2 s- 1 ;机理函数微分形式和积分形式分别为 f( α) - 2 ( 1- α) [- ln( 1- α) ]1 / 2、g( α) =[- ln( 1-α) ]1 / 2 ,其脱水反应的动力学方程为 :dα/dt=Ae- Ea/ RT· 2 ( 1-α) [- ln( 1-α) ]1 / 2 .     

无穷等比级数求和公式∑n=0^∞αx^n=α/1-x在级数中的应用

利用无穷等比级数的求和公式∑n=0^∞αx^n=α/1-x求幂级数和函数的两大类级数的通式，给出了四种函数在展开成幂级数及泰勒级数过程中，应用求和公式的间接展开法。     

一类具有零因子的环的结构

设R为有限环，其左零因子集为D，D≠R，D^2=0，则R的特征为素数或素数的平方．进一步，当charR=p为素数且任意d∈D-l(R)有dR=Rd时，则存在非负整数r，非负整数n≥r及自然数s，使得R≌Ar,n,s.其中Ar,n,s={(αo，α1，…，αr，αr 1，…，αn)|αi∈K}，K=GF(p^s)(α0，α1，…，αr，αr 1，…，αn) (b0，b1，…，br，br 1，…，bn)△(α0 b0，α1 b1，…，αr br，αr 1 br 1，…，αn bn)(α0，α1，…，αr，αr 1，…，αn)(b0，b1，…，br，br 1，…，bn)△(α0b0，α0b1，…，α0br，α0br 1 αr 1b0^pnr 1,…，α0bn αnb0^prn)ti∈{0，1，2，…，s-1}，r 1≤i≤n。     

代数双曲混合H-Bezier函数及其性质

目的精确表示一类超越曲线，如双曲线弧、悬链线、指数曲线等。方法在代数双曲混合函数空间Гn=span{1，t，t^2，…，t^n-2，sinh t，cosh t}（n≥2）中构造一组规范基，基于该规范基函数定义曲线。结果给出了空间Гn的一组规范基函数{Ui,n（t）}i=0^n，得到了H-Bezier曲线，并分析得出了该基函数及所生成曲线的性质。结论所得曲线可精确表示一类超越曲线，它既继承了多项式曲线的优点，又具有双曲函数的优点。     

关于Iyengar不等式

利用函数f(x)在积分区间[n,b]端点的函数值及各阶导数值,对函数f(x)在[α,b]上的定积分进行估计,进而得到若干积分不等式．主要结果如下：若函数f(x)是[α,b]上n 1次可微函数,且│f^(n 1)(x)│≤M(M＞0),则│∫^b α(x)dx-n∑k=0 (b-α)^k 1/2^k 1(k 1)! [f^(k) (α) (-1)^k f^(k)(b)]│≤1/2^n 1(n 2)! M(b-α)^n 2.     

水电站日调节计算中的一个数学问题

对电站上下游的明渠不恒定流动用微幅波理论来处理,日调节问题就将被归结为下述数学问题; {α~2q/αt~2+2U_0(α~2q/αtαs)-(gH_0-U_0~2)α~2q/αs~2+2I_0g/U_0 αq/αt+3I_0g αq/αs=0, {q=0=q_0(s), {qt=0=q_1(s), {(q(0,t)+Q_0){integral from n=0 to t αq/αs(0+,η)-αq/αs(0_-η)dη+f(0)q_0(0)+Q_0}-f(t)。其中U_0,H_0,I_0,g,Q_0均为确定的常数,而q_0(s),q_1(s),f(t)均为充分光滑的函数。我们用双曲型方程混合问题的处理方法,结合了中间的非线性连结条件,得到了结论;当条件 [q_0(g)+Q_0-1/2gH_0~(1/2)(1-F_τ~2)△H_0]~2≥α>0被满足时,那末在一定的时间段内,问题是适定的。其中△H_0=(f(0)/q_0(0)+Q_0)是电站上下游的初始水位差,而F_τ=U_0/gH_0~(1/2)是弗劳德数。     

两类广义Fibonacci数列的关系

本文将研究广义Fibonacci数列｛un=un-1 un-2｝和数列｛αn=αn-1 αn-3 αn-4｝的内在关系，得到：设αn=1，α2=(m↑∑↑i=1ui s)^2,α4=(m 1↑∑↑i=2ui s)^2,α6=(m 2↑∑、i=3ui s)^2且αn=αn-1 αn-3 αn-4，则（1）α2n=(m n-1↑∑↑i=nui s)^2,α2n 1 α2n-2 α2n-3=2(m n-2↑∑↑i=n-1ui s)(m n-1↑∑↑i=nui s)(2)α2n 1=(m n-1↑∑↑i=nui s)(m n↑∑↑i=n 1ui s) (-1)^n 1X(m,s)，其中X（m,s)=(um s 1-us 1)(um s 2-us 2)-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.     

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.