海南省汉族人头面部测量指标与指数值的年龄变化

 在海南琼海市和万宁市的城市和乡村调查了汉族643例(男为334例,女为309例)成人的22项头面部体质指标,计算了13项头面部体质指数,对海南汉族头面部形态特征的年龄变化进行了初步分析.结果显示:① 眼内角间宽、眼外角间宽、唇高、红唇厚度这4项指标值与年龄呈负相关.上唇皮肤部高度、容貌耳长、容貌耳宽、面颊皮褶这4项指标值与年龄呈正相关.并且上述指标值在不同年龄组中存在有统计学意义的差异.② 随年龄增长,口指数值下降,并且在不同年龄组中存在有统计学意义的差异.海南汉族人头面部测量指标与指数值随年龄增长呈现一定的变化规律.     

Johnson图相关联的一类新的认证码

利用Johnson图J(dm,d)得到了新的认证码,并进一步得到了这类码的参数.在假定编码规则按等概率分布选取时,计算出这类码的模仿攻击成功和替换攻击成功的概率.     

科学发展观与学校体育思想考评

进入21世纪以来,中国学校体育在实践中遇到一系列难以回避的问题,科学发展观科学地回答了当前和今后中国学校体育发展所面临的问题和任务,深刻理解和掌握这一思想,进而实现学校体育现代化的发展.     

体育锻炼对改善大学生身心健康的作用研究

为探讨经常性体育锻炼对大学生身心健康的影响,按照体育人口的标准,将新乡市大学生分为体育人口与非体育人口,进行体质与心理健康状况的对比,得出大学生体育人口在身体形态、机能以及素质三方面均显著优于非体育人口,大学生体育人口的心理健康水平也显著优于非体育人口,体育锻炼对大学生身心健康有着重要的促进作用.     

石膏模-混凝土组合空腹楼盖用磷石膏力学特性研究

对石膏模-混凝土组合楼盖用磷石膏的抗压强度与含水率的关系、抗压强度取值、弹性模量取值、石膏与混凝土之间两类抗剪连接件受力性能进行了试验研究。研究结果表明,磷石膏的抗压强度随含水率的减小而增大,且随着含水率的降低,磷石膏的强度增加幅值越来越大,大致呈对数函数关系;磷石膏具有较好的抗压性能,其抗压强度较高,抗压强度可取4.8MPa,且受力过程中有明显的弹性阶段,根据曲线,其弹性模量取值约550MPa;对混凝土与石膏间的两类剪力连接件进行推出试验,结果表明两类连接件具有相同的抗剪强度,而B类连接件比A类连接件连接效果优越,试验数据比较稳定,最终以石膏破坏而导致构件破坏,连接件较为可靠。     

社会排斥视角下农村学校体育贫困分析及其解决路径

农村学校体育是农村学校教育的重要组成部分,但农村学校体育贫困现象较为突出,由于学校体育资源的缺乏造成学生体育教育机会缺失,而引起这种现象的根源是社会排斥.通过对学校体育贫困概念的界定和学校体育贫困外在表现的分析,从社会排斥的经济、教育、文化3个维度探讨了农村学校体育贫困的原因,并从反社会排斥的视角提出解决农村学校体育贫困的5条路径,以期为农村学校体育发展和促进公平教育提供思考.     

物理化学实验教学改革中的创新教育思路

为提高物理化学实验课程教学效果,更好地培养学生的创新能力,从物理化学实验教学现状入手,探讨了物理化学实验教学改革中一些可行的创新思路和方法,并基于对课程体系、教学内容、教学模式和评价考核体系的分析提出了一些新的措施.     

Simulation of wind gust structure in the atmospheric boundary layer with Lattice Boltzmann Method

Cold fronts occur in northern East Asia during winter and spring.After cold frontal passage,airflow is downward and accompa-nying strong winds fluctuate significantly;this is termed wind gusts.Analysis of observation data shows that wind gust structure has coherent characteristics.This is important for entrainment of spring dust storms into the upper boundary layer,where they are transported great distances.The Lattice Boltzmann Method(LBM) is a computational fluid technique based on the Boltzmann transport equation.The LBM has been used to study complex motion such as turbulence,because it describes motion at the micro level.In this paper,Large eddy simulation is introduced in the LBM,enabling simulation of turbulent flow in the atmospheric boundary layer.The formation and development of wind gusts are simulated,and a coherent structure with a combination of wave and vortex is obtained.This explains the mechanism of soil erosion and sand entrainment by the coherent structure of wind gusts.     

Variable diffusion boundary layer and diffusion flux at sediment-water interface in response to dynamic forcing over an intertidal mudflat

The diffusion boundary layer (DBL) significantly limits the exchange between sediment and overlying water and therefore becomes a bottleneck of diffusive vertical flux at the sediment-water interface (SWI). Variable DBL thickness and diffusion flux in response to dynamic forcing may influence replenishment of nutrients and secondary pollution in coastal waters. In situ measurements of velocity in the bottom boundary layer (BBL) and oxygen concentration in the DBL were made over an intertidal mudflat, using an acoustic Doppler current and mini profiler. A linear distributed zone in the oxygen profile, the profile slope discontinuity and variance of concentration can be used to derive accurate DBL thickness. Diffusion fluxes calculated from the water column and sediment are identical, and their bias is less than 6%. A numerical model PROFILE is used to simulate the in situ dissolved oxygen profile, and layered dissolved oxygen consumption rates in the sediment are calculated. The DBL thickness (0.10-0.35 mm) and diffusion flux (15.4-53.6 mmol m 2 d 1) vary with a factor of 3.5 during a tidal period. Over an intertidal mudflat, DBL thickness is controlled by flow speed U in the BBL, according to δDBL=1686.1DU 1+0.1 (D is the molecular diffusion coefficient). That is, the DBL thickness δDBL increases with decreasing flow speed U. Changes of diffusion flux at the SWI are caused by variations in the water above the sediment and the turbulent mixing intensity. The diffusion flux is positively related to the turbulent dissipation rate, friction velocity and turbulent energy. Under the influence of dynamics in the BBL, DBL thickness and flux vary significantly.     

Propagation of planetary-scale zonal mean wind anomalies and polar oscillations

Global atmospheric variables can be physically decomposed into four components:(1) the zonal time averaged climate symmetric component,(2) the time averaged climate asymmetric,(3) the zonal-mean transient symmetric anomaly,and (4) the transient asymmetric anomaly.This study analyzes the relationships between the intra-seasonal and inter-annual variability of planetary scale decomposed zonal and meridional winds in the tropopause,and oscillations such as those from the El Ni o-Southern Oscillation (ENSO),the Arctic Oscillation (AO) and the Antarctic Oscillation (AAO).The tropical inter-annual zonal mean wind anomalies in the tropopause are linked with the ENSO cycle and can propagate into the subtropics,mid-latitudes,and polar front regions via abnormal meridional vertical cells.Similarly,tropical intra-seasonal (40-60-d) zonal wind anomalies can reach the subtropics and mid-latitudes.The polar intra-seasonal zonal wind anomalies in the tropopause can propagate toward high-latitude areas.Thus,the AO and the AAO are the result of the interaction and propagation of these planetary scale zonal wind anomalies.