Hilbert空间中K-框架的构造

Hilbert空间中的K-框架是框架理论的一种推广. 在Hilbert空间中,用两个Bessel序列构造K-框架、T₁-框架(T₂-框架),用两个K-框架构造一个P-框架或Q-框架,所得结果推广并改进了已有结论.     

双导堤工程下潮汐汊道与海岸潟湖地貌稳定性

以渤海湾沿岸具有双导堤工程的单一潮汐汊道的华北最大海岸潟湖—七里海潟湖为原型建立理想模型，通过设置包括临界侵蚀应力、临界淤积应力、泥沙沉速、初始床面高程和径流量等影响潟湖地貌演变的相关参数，得到理想模型达到稳定状态后的纳潮量P和潮汐汊道断面最大流量Q_m。分别建立其与潮汐汊道断面面积A的相关关系式以表征潮汐汊道稳定性。比较分析发现在表征潮汐汊道稳定性方面，Q_m?A关系较P?A关系的拟合效果更佳。分别利用Q_m?A关系以及泥沙净冲淤量计算得到潮汐汊道和潟湖稳定所需时长，对比结果表明潟湖明显滞后于潮汐汊道达到稳定状态，临界侵蚀应力对潮汐汊道稳定性影响更大，而临界淤积应力、泥沙沉速和初始床面高程对潟湖稳定性影响尤为显著，径流量对潟湖和潮汐汊道稳定性的影响相当。     

有节点故障的d进制n维方的圈嵌入

互连网络的容错能力是并行计算中的一个关键问题,而d进制n维方（超方的一般形式）在计算机的互连网络中已得到广泛的应用。本文考虑有节点故障的d进制n维方的容错性。F是d进制n维方Q_n（d） 中的错误点集（n≥3）, 且|F|≤n-2,证明了Q_n（d）的每个无故障的边和无故障的点存在于长从4到dⁿ-2|F|的无故障偶圈中。而且,当d是奇数时,Q_n（d）的每个无故障的边和无故障的点存在于长为dⁿ-2|F|的无故障圈中。     

电磁作用常数α值及电子“反常荷”计算

 用Dirac大数D,Planck大数A唯象地计算了电磁相互作用常数α值,结果与惯用值很好相符.在轻子的亚夸克结构动态模型中,因亚夸克运动使轻子发生等体积表面形变产生电磁作用对称破缺,从而产生“反常质量”,“反常电荷”,则α值将不再是常数,是可变的.由Δm_e反>可计算ΔQ_e反反的值,由Δm_e反>和ΔQ_e反反算出的“反常磁矩”,与实验值相近.最后也讨论了Planck尺度的量子条件.     

Hilbert空间中两个K-框架的算子组合

讨论了Hilbert空间中两个K-框架{f_i}^∞_i=1与{g_i}^∞_i=1通过算子作用再求和后得到的序列{T₁ f_i+T₂g_i}^∞_i=1成为K-框架与紧K-框架的一系列等价条件,所得结果推广与修正了已有结果.     

半导体微盘的回音壁模式研究

 采用二维时域有限差分法(FDTD),计算分析了半导体微盘的形状如圆形、椭圆形等对激发其回音壁模式的影响;同时也研究了半导体微盘在不同的增益介质如水、空气、乙醇等中所形成的回音壁模式.研究结果表明:①在同一增益介质中,半导体微盘形状对形成回音壁模式有很大的影响,模式的形成与各点的曲率半径有关,曲率半径越大,越容易形成回音壁模式;②在不同增益介质中,相对折射率n₁₂越大,越容易形成回音壁模式,且有利于提高其Q值.     

具强迫项的中立型差分方程的振动性和渐进性

 使用不等式的某些技巧,获得了如下具强迫项的中立型差分方程Δ(y_n+y_n-τ)+Q_nG(y_n-σ)=f_nn∈N的所有解振动或当n→∞时趋于零的充分条件.还获得了如下的中立型差分方程Δ(y_n-y_n-τ)+Q_nG(y_n-σ)=0 n∈N的所有解振动的充分条件.     

完全图Kn的{P5,C5}分解

图分解问题已在很多邻域中得到了广泛的应用。用P₅表示5个顶点的路，C₅表示5个顶点的圈，本研究讨论了完全图K_n分解成5个顶点的路P₅和圈C₅的存在性，给出完全图K_n存在{P₅,C₅}-强制分解的充分必要条件是n≥7(n≠8)，以及完全图K_n存在{P₅,C₅}-分解的充分必要条件是n≥5(n≠6)。     

地磁太阴日变化L的O1分量的变化特征

 用Winch提出的地磁太阴日变化分析方法确定佘山地磁台的地磁太阴日变化的O₁分量L(O₁).首先把佘山台 196 0～1988年D,H和Z各分量的时均值资料做为整体分析年平均变化,然后按季节和太阳活动性细分后进行计算分析.讨论了L(O₁)的基本特征和季节变化、电离层和海洋发电机效应对L(O₁)的影响以及太阳活动对L(O₁)的贡献,并与国外一些地磁台的结果进行了对比分析.     

最小Q-特征值第二小的给定悬挂点数的非二部单圈图

图的最小Q-特征值常被用来衡量一个图的非二部程度,受到研究者的广泛关注。在路Pn-k-2的一端接出一个圈C3,另一端接出k个悬挂边,所得的n阶图记为Ukn(3)。范益政等人最近证明Ukn(3)是最小Q-特征值达到最小的图。在他们的基础上,证明C13(n-k-1)是最小Q-特征值达到第二小的图,其中C13(n-k-1)是将Ukn(3)的一条悬挂边移至与悬挂邻点相邻的非悬挂点上所得的图。     

Study on estimate method of wave velocity and quality factor to fault seals

Based on ultrasonic test of fault rocks, the responses for wave velocity and quality factor （Q value） to lithology, porosity and permeability of fault rocks and mechanical property of faults are studied. In this paper, a new quantitative estimate method of fault seals is originally offered. The conclusions are as follows： （1） Wave velocity and Q value increase and porosity decreases with the increase in stress perpendicular to joint; （2） In compressive and compresso-shear fault rocks that are obviously anisotropic compared with their original rocks, the wave velocity and Q value are greater in the direction parallel with foliation, and usually less perpendicular to it. In tensile and tenso-shear fault rocks that are not obviously anisotropic, the wave velocity and Q value are under that of original rocks; （3） In foliated fault rocks, the direction with minimal wave velocity and Q value is the best direction for sealing; on the contrary it is the best for flowing; （4） Structural factures develop mainly along foliation, the minimal wave velocity and Q value reflect the flowing capacity in parallel direction to foliation, and the maximal wave velocity as well as Q value reflect the sealing capacity in normal direction to foliation. The new estimate method is based upon contrast of wave velocity and Q value between fault rocks and their original rocks, and is divided into three parts that are respectively to identify rock＇s lithology, to judge mechanic property of faults and to Judge sealing capacity of faults. Although there is vast scale effect between ultrasonic wave and seismic wave, they have similar regularity of response to fabric and porosity of faults. This research offers new application for seismic data and petrophysical basis for seismological estimation of fault seals. The estimate precision will be improved with the enhancement of three-dimensional seismic prospecting work.     

Temperature effects on ethylene and methane production from temperate forest soils

Change in temperature affects the activity of soil microorganisms.However,there is limited knowledge about temperature effects on ethylene(C2H4) and methane(CH4) production from forest soils.Topsoil samples(0―5 cm) collected from different temperate forest stands(e.g.,Pinus sylvestris L.,Cryptomeria japonica,and Quercus serrata) were used to compare C2H4 and CH4 production from soils at temperature from 5 to 35℃ under oxic and anoxic conditions.The rates of C2H4 and CH4 production from soils under oxic cond...     

q - 覆盖及其空间

利用 q - 开集定义了 Q_i( #em/em# = 0, 1, 2, 3, 4) 空间, 讨论了它们的性质及 Q_i 空间同 T_i( i = 0, 1, 2, 3, 4) 空间的关系.给出了, q- 覆盖的定义,即拓扑空间 X 的q- 开集簇{Aα |α∈I } 称为 q- 覆盖, 当且仅当∪_α∈IAα = X .继而定义了一种新的紧致空间--Q- 紧致空间, 讨论它的性质及 Q - 紧空间同 Q_i 空间的关系, 得到一些性质.     

四川盆地二叠系火山岩地震响应特征及分布规律

2018年底,川西南永探1井在二叠系钻遇火山岩储层,日产22. 5×104m3/d工业气流,使四川盆地火山岩成为目前重要的勘探接替领域。但由于钻井较少,研究程度低,火山岩厚度及岩相分布规律不清。充分利用地震信息,精细标定井下火山岩岩相与井旁地震响应特征,结合地震响应特征及层拉平剖面,建立了川西地区火山岩岩相地震识别模式。川西南地区有三种岩相,分别为火山岩喷溢相、火山岩溢流相和火山岩沉积相。通过对二、三维地震资料精细对比解释火山岩顶底界面,预测出川西地区火山岩岩相和厚度分布。综合顶部构造背景、火山岩相分布特征、钻井井下油气显示情况等因素,确定出川西南成都-简阳-三台地区火山岩油气勘探的有利区带,对于四川盆地火山岩油气勘探,提供了重要的支撑。     

Studies on the behaviors of PbSO4/Pb and PbO2/PbSO4 electrodes prepared from lead carbonate by powder microelectrode technique

The behaviors of PbSO₄/Pb and PbO₂/PbSO₄ electrode prepared from PbCO₃ have been examined using powder microelectrode(PME) technique and cyclic voltammetry(CV). Firstly, PMEs packed with PbCO₃ transformed into PbSO₄ PME in 1.0 mol/L H₂SO₄ solution at 30 °C, and then the PbSO₄ in the PMEs were formed to Pb or PbO₂ using an unsymmetrical signal (Q _a/Q _c for PbSO₄/Pb electrode andQ _c/Q _a for PbO₂/PbSO₄ electrode being 0.1–0.3) in 2.5 mol/L H₂SO₄ solution. The results show that the CV characteristic of either PbSO₄/Pb or PbO₂/PhSO₄ PME prepared from PbCO₂ are as good as that of both electrodes made from lead oxide powder produced by ball mill. Foundation item: Supported by the National Natural Science of China(29677013) and Chenguang Foundation of Wuhan Municipal Science and Technology Commission(20005004022) Biography: Dai Zhong-xu(1968-), male, Lecturer, Ph. D. candidate, research direction: electrochemistry.     

SL（2，Qp）中的非初等离散子群的代数收敛性

在Kleinian群中，研究离散群的代数收敛性是一个重要的问题，群列的代数收敛性与流形的形变以及极限集的Hausdorff维数的收敛性有密切关系.随着非阿基米德域上的李群和非阿基米德域上的动力系统的发展，讨论非阿基米德域上的离散群的代数收敛性就是一个重要的问题.这篇文章讨论了PSL（2,Q_p）中由r个元素生成的非初等离散群的代数收敛性，利用PSL（2,Q_p）中关于子群的非阿基米德Jorgensen不等式，以及群双曲Berkovich空间上的双曲等距性，证明了非初等群列代数收敛到非初等群列上.     

Zircon SHRIMP U-Pb dating of meta-diorite from the basement of the Songliao Basin and its geological significance

Located in the east portion of the North Orogenic Belt, the Songliao Basin is bounded by the Da Hinggan Mountains in the west, the Xiao Hinggan Mountains in the north, the Zhangguangcai Range in the east, and the North China Craton (NCC) in the south (Fig…     

Turbidite and bottom-current evolution revealed by anisotropy of magnetic susceptibility of redox sediments in the Ulleung Basin,Sea of Japan

Anisotropy of magnetic susceptibility(AMS) from above and below 7.31 m in a core from the southern Ulleung Basin shows clear differences on an equal area projection of the lower hemisphere.Rather concentrated steep inclination of K 3 and horizontal inclination of K 1 and K 2(K1 ≥K2 ≥K3) are located within the upper part,and the latter two axes lie perpendicular to each other near the bedding plane.In contrast,random distribution of the three axes and extremely high value of shape parameters(Q=(K1-K2)/[(K1+K2)/2-K3]) are evident in the lower part,indicating complete destruction of the original sedimentary structure.This result is consistent with data from X-radiographs,which show numerous conglomerates,distortions and cleavages in the lower part.According to age models by Liu et al.(2010) and Zou et al.(2010),the bottom age at 7.31 m is 48 cal ka BP,and the time domain is discussed below.The degree of AMS(P) is low,1-1.08,and linearly related to the foliation(F)(R2 =0.95,N=176).The relationship between F and linearity(L) implies oblate aligning patterns that are typically sedimentary in origin.At least five redox couplets were found with the aid of S ratios and other rock magnetic parameters,and in most cases,the original signals of climate survived early diagenesis.The paleomagnetically reoriented AMS show corresponding changes with millennial events in the last 48 cal ka.Clearly tilted K 3 directions and reduction of P and F occurred within DO1-BA warm events,when melt water pulse 1A nd the YD cold event took place.The turbulent conditions therein,synchronous with coarsening of sediments,provide evidence of strong bottom currents and possible directional changes,as evidenced by different K3 tilting directions.A NE current direction in the last 4.5 cal ka is consistent with in situ measurements of bottom currents.Responses of AMS,mainly to climatic modulation,show on the one hand,the limited influence of diagenesis on rock magnetic signals and,on the other hand,the dramatic change of hydrodynamic conditions and terrigenous inputs during rapid sea level rise during the last deglaciation.     

Characteristics of magnetocardiography and electrocardiography in the time-frequency domain

As the carriers of electromagnetic information about the cardiac system,both magnetocardiography(MCG) and electrocardiography(ECG) are non-stationary signals(NSS).The essential and crucial features of NSS are the local time-frequency characteristics(LTFCH).Under the constraint of the uncertainty principle in the time-frequency domain(TFD),the LTFCH of those non-stationary signals can be determined by evolutionary spectrum analysis(ESA).In this paper,by analyzing the QRS complexes of both MCG and ECG data from healthy volunteers,we have derived some characteristic parameters(CHPs) in the TFD,such as the quality factor(Q) and center frequency(fz).According to the experiment results,we believe that there are threshold ranges of Q and fz values in the dynamic behavior of the cardiac system for healthy projects.If the CHPs are in the proper ranges,the cardiac system is in a normal condition and homeostasis can be self-correcting.In contrast,if the values of the CHPs are less than the proper ranges,the homeostasis of the cardiac system is lost and some cardiac diseases may result.The assumption of the threshold ranges is verified by sample data from different cardiac diseases,and the results support the assumption.The CHPs are not only a kind of new reference criterion for ECG in clinical diagnosis,but also afford a technological route for the application of MCGs in cardiology.