管材超声检测中导波模式及频厚积的选择

用轴向功率流分布来选择检测自由管状结构的最佳导波模式及其最佳频厚积 ,并将混合边界元法应用于管状结构 ,对其结果的有效性进行了验证 .结果表明 :对于自由管材 ,用超声纵向L(0 ,1)模式检测时 ,频厚积在 0 .15MHz·mm以下时较为灵敏 ;用L(0 ,2 )模式检测时 ,在 1.4～ 1.8MHz·mm之间对检测管壁中央的缺陷较灵敏 ;用L(0 ,3)模式检测时 ,在 2 .0MHz·mm以下对管内外表面上的缺陷都较灵敏 .轴向功率流分布能有效地选择检测的最佳导波模式及其频厚积 .     

肌肉自发振动过程中结合几率与化学反应速率的变化

定量分析肌球蛋白与肌动蛋白丝的结合几率及相关化学反应的速率常数,对于准确掌握肌肉收缩的内在机制具有非常重要的意义.以肌肉自发振动的实验结果为依据,从振动过程所满足的动力学方程出发,推导出结合几率与肌丝滑行速度及肌节长度之间的定量关系,并求得化学反应速率随肌肉收缩的速度变化而改变的数学规律.结果显示,结合几率的基准值由溶液中主要化学成分的浓度决定;结合几率的变化值与肌肉收缩的速度成正比,与肌节长度成反比;而化学反应速率随收缩速度按指数规律变化.上述结果与实验值基本一致.     

A current filamentation mechanism for breaking magnetic field lines during reconnection

During magnetic reconnection, the field lines must break and reconnect to release the energy that drives solar and stellar flares and other explosive events in space and in the laboratory. Exactly how this happens has been unclear, because dissipation is needed to break magnetic field lines and classical collisions are typically weak. Ion-electron drag arising from turbulence, dubbed 'anomalous resistivity', and thermal momentum transport are two mechanisms that have been widely invoked. Measurements of enhanced turbulence near reconnection sites in space and in the laboratory support the anomalous resistivity idea but there has been no demonstration from measurements that this turbulence produces the necessary enhanced drag. Here we report computer simulations that show that neither of the two previously favoured mechanisms controls how magnetic field lines reconnect in the plasmas of greatest interest, those in which the magnetic field dominates the energy budget. Rather, we find that when the current layers that form during magnetic reconnection become too intense, they disintegrate and spread into a complex web of filaments that causes the rate of reconnection to increase abruptly. This filamentary web can be explored in the laboratory or in space with satellites that can measure the resulting electromagnetic turbulence.     

Observed increase in local cooling effect of deforestation at higher latitudes

Deforestation in mid- to high latitudes is hypothesized to have the potential to cool the Earth's surface by altering biophysical processes. In climate models of continental-scale land clearing, the cooling is triggered by increases in surface albedo and is reinforced by a land albedo-sea ice feedback. This feedback is crucial in the model predictions; without it other biophysical processes may overwhelm the albedo effect to generate warming instead. Ongoing land-use activities, such as land management for climate mitigation, are occurring at local scales (hectares) presumably too small to generate the feedback, and it is not known whether the intrinsic biophysical mechanism on its own can change the surface temperature in a consistent manner. Nor has the effect of deforestation on climate been demonstrated over large areas from direct observations. Here we show that surface air temperature is lower in open land than in nearby forested land. The effect is 0.85 ± 0.44 K (mean ± one standard deviation) northwards of 45° N and 0.21 ± 0.53 K southwards. Below 35° N there is weak evidence that deforestation leads to warming. Results are based on comparisons of temperature at forested eddy covariance towers in the USA and Canada and, as a proxy for small areas of cleared land, nearby surface weather stations. Night-time temperature changes unrelated to changes in surface albedo are an important contributor to the overall cooling effect. The observed latitudinal dependence is consistent with theoretical expectation of changes in energy loss from convection and radiation across latitudes in both the daytime and night-time phase of the diurnal cycle, the latter of which remains uncertain in climate models.     

直觉模糊集所诱导的软集语义及其三支决策

借助于阴影集,利用直觉模糊参数,将直觉模糊集转化为悲观阴影集和乐观阴影集,提出直觉模糊集悲观三支决策和乐观三支决策,给出直觉模糊集诱导软集的方法。利用三支决策理论,提出软集三支决策定性模型。结合直觉模糊集悲观三支决策和乐观三支决策,利用直觉模糊参数,给出软集三支决策定量模型。