青海盐湖水化学特征的因子分析研究

采用最大方差正交旋转因子分析方法研究青海盐湖水化学特征，结果表明，青海盐湖水化学类型主要为硫酸镁盐型，盐湖卤水发育程度较深，没有碳酸盐型，K、Na、Mg//Cl、SO4-H2O是青海盐湖卤水的主要化学平衡体系等，这与青海盐湖的实际情况完全相符。     

论影响科技传播效果的障碍因素

传播的最终归宿是传播效果的实现,科技传播承载着知识传播和文化传通的双重使命,尤其注重传播效果的实现和传播者主观意图的完成.但是在实际操作过程中,由于种种因素造成传播效果实现困难,本文着重分析这些影响科技传播的障碍因素,由此试图解决科技传播实践中所遭遇的种种尴尬和问题.     

论休闲活动在弱势群体中的开展

当弱势群体开始不断受到社会关注的时候,人们更多的是从教育培训、就业、医疗保险等方面去考虑如何帮助他们,而很少从他们日常的休闲活动中去考虑.所以,全社会都需要重新认识休闲活动、弱势群体及它们之间的关系,分析休闲活动在弱势群体中的开展现状,进而就如何开展提出若干设想.     

垃圾填埋场中水泥土屏障对Cu2+的阻滞性能

通过室内模型试验,研究了不同水泥掺量的水泥土防渗屏障和上海老港填埋场的膨润土砂水泥(塑性混凝土)防渗屏障对Cu~(2+)的阻滞效果,并应用数值模拟的方法对Cu~(2+)在防渗屏障中的有效扩散系数进行求解.研究结果表明,随着水泥掺量和屏障厚度的增加,水泥土屏障对金属离子的阻滞效果会逐步提升;Cu~(2+)在水泥土中的有效扩散系数(1×10~(-7)~2.5×10~(-7) cm~2·s~(-1))是在土中的有效扩散系数(9.53×10~(-6)~1.14×10~(-5) cm~2·s~(-1))的1/35~1/100;上海老港填埋场中的塑性混凝土防渗屏障对Cu~(2+)有较好的阻滞效果.     

Damage evolution and failure mechanism of thermal barrier coatings under Vickers indentation by using acoustic emission technique

Acoustic emission(AE) technique was adopted to monitor the damage evolution of air plasma-sprayed(APS) yttria-partially-stabilized zirconia(YSZ) thermal barrier coatings(TBCs) during instrumented indentation testing, and then the failure mechanisms were investigated by cluster analysis and wavelet transform methods.The results of cluster analysis showed that there were three classes associated with distinct failure types for the 8YSZ coatings under Vickers indentation. Based on wavelet transform, these three clusters could be clearly distinguished from their dominant frequency bands, which were concentrated on levels A5(0–156.25 kHz), D5(156.25–312.5 kHz) and D4(312.5–625 kHz), respectively. Thus, the failure mechanism of 8YSZ coatings under Vickers indentation could be clarified by the distribution of different failure types in indentation depth. To sum up, as indentation load increases, the 8YSZ coatings can accommodate the indenter by elastic or little plastic deformation, microcracks propagation and then debonding at the splat boundaries. By comparing the distribution of AE signals induced by different failure types in indentation depth for samples with different thermal exposure time, it can be inferred that thermal exposure treatment can accelerate the degradation of APS 8YSZ TBCs.     

辽西早白垩世义县组大康堡层纹泥的古环境意义

辽西地区义县组湖泊沉积层中产出著名的“热河生物群”化石,对于此时期古环境的研究一直是诸多学者关注的焦点.本文对大康堡层湖相纹泥展开研究,重建此时期古环境.通过野外及室内对纹泥组成、类型、厚度等方面的观测,对此时期古气候有了新的认识.纹泥厚度特征变化表明沉积期降水量和沉积速率逐渐减小,统计洪水沉积间纹层数量可指示沉积期洪水事件的频率和规模.结合近现代纹泥形成和保存条件,可知该地区沉积期湖泊水体较深,湖水分层,存在一个缺氧环境,具有较小的表面积/深度比,湖盆形态适合,未受到风的侵扰.     

利用ETC技术的小区内无线车位锁设计

针对居住小区内的专用车位被随意占用现象,提出了基于ETC技术的自动控制车位锁系统。该系统通过无线自动控制装置,免去了每次都需要车主手动开锁车位或者利用无线控制器的情况。经过实验,该设计可以智能化地解决专属车位的随意占用现象。     

有限时期障碍期权的三项式期权定价模型

本文研究了有限时期障碍期权的三项式定价模型,对具有三种变化的股票价格模型进行了讨论,推广了CRR二项式定价模型,推出了某一假定证券市场中有限时期障碍期权的三项式期权定价公式。     

基于扩散模型的ZnO/p-Si异质结伏安特性研究

为了揭示ZnO/p-Si异质结的导电机理,基于p-n结扩散模型和Anderson扩散模型推导了ZnO/p-Si异质结在理想情况下的伏安特性,并分析了掺杂浓度、工作温度以及能带补偿的影响.结果表明:当正向偏压超过势垒高度时,界面两边多数载流子由耗尽变为堆积,形成反向势垒,对异质结的正向电流起阻碍作用;当外加正向电压等于内...     

A high-resolution environmental change record since 19 cal ka BP in Pumoyum Co,southern Tibet

A 380-cm-long sediment core was acquired from the deep water area of Pumoyum Co, southern Tibet. Twenty-five plant residue samples were selected, and organic carbon stable isotopes were obtained using the AMS ¹⁴C chronological method. The ¹⁴C age and carbon reservoir effect were calibrated with surface sedimentation rate measurements using ²¹⁰Pb dating. Results showed that the core sediment deposited over 19 cal ka BP. Based on a multi-proxy analysis of TOC and IC contents, grain size and pollen assemblage data, the palaeoclimatic evolution of Pumoyum Co was reconstructed since the last glacial. Pumoyum Co was a shallow lake prior to 16.2 cal ka BP; although the glacier around the lake began to melt due to increasing temperatures, climate was still cold and dry. In the interval of 16.2–11.8 cal ka BP, the sedimentary environment fluctuated drastically and frequently. Two cold-events occurred at 14.2 and 11.8 cal ka BP, and these may correspond to the Older Dryas and the Younger Dryas events, respectively. After 11.8 cal ka BP, Pumoyun Co developed into the deep lake as it is now. The lake water temperature was relatively lower at that time because of influx of cold water from glacial meltwater entering the lake. As a result, the multi-proxy indicators showed no sign of warm conditions. Comparisons between the sedimentary record of Pumoyum Co with that of other lakes of the same age in southern Tibet indicate a warmer climate following the last deglaciation influenced the southeastern Tibetan Plateau. These results imply that the southwest Asian monsoon gradually became stronger since the deglaciation during its expansion to the inner plateau. The glacial-supplied water of the lake responded sensitively to cold-events. The entire southern Tibet region was dominantly influenced climatically by the southwest Asian monsoon during the Holocene.