二氧化碳在转炉炼钢中的应用研究

对炼钢温度下CO2与熔池元素的反应机理进行了研究,并进行了相关热力学和动力学分析.利用30 t转炉进行顶底复吹CO2气体的炼钢工艺试验.试验结果表明:采用顶底复吹CO2试验炉次烟尘量减少了11.15%,烟尘TFe降低了12.98%,炉渣铁损降低了3.10%,试验终点钢液中[N]、[P]含量分别降低了50%和23.33%.转炉顶底复吹CO2气体炼钢工艺是完全可行的,为转炉炼钢节能降耗提供了新方法.     

基于GMM和MRF的自适应阴影检测

运动目标阴影在很大程度上会影响运动目标跟踪、行为识别的正确性和有效性.为此,文中提出了一种基于混合高斯模型和马尔科夫随机场的自适应阴影检测方法.该方法首先对混合高斯模型进行改进,使其可以自适应调整参数学习率以消除浅阴影;然后采用马尔科夫随机场综合邻域的空间依赖性信息进行精确的阴影检测.为了提高基于马尔科夫随机场的阴影检...     

区间删失数据函数的均值估计

运用无偏转换思想构造了区间删失数据函数的均值估计,并在此基础上对所构造的估计量方差进行了研究.针对Ⅰ型区间删失情况和Ⅱ型区间删失情况,找到了估计量方差有限的条件.     

An overview of resistive random access memory devices

With recent progress in material science, resistive random access memory (RRAM) devices have attracted interest for nonvolatile, low-power, nondestructive readout, and high-density memories. Relevant performance parameters of RRAM devices include operating voltage, operation speed, resistance ratio, endurance, retention time, device yield, and multilevel storage. Numerous resistive-switching mechanisms, such as conductive filament, space-charge-limited conduction, trap charging and discharging, Schottky Emission, and Pool-Frenkel emission, have been proposed to explain the resistive switching of RRAM devices. In addition to a discussion of these mechanisms, the effects of electrode materials, doped oxide materials, and different configuration devices on the resistive-switching characteristics in nonvolatile memory applications, are reviewed. Finally, suggestions for future research, as well as the challenges awaiting RRAM devices, are given.     

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.     

海洋有害赤潮调控功能菌的发现与研究

近年来,赤潮的微生物调控研究受到了科学界的高度重视,"以菌治藻"的赤潮调控理念格外引人注目.先从国内外抑/杀藻菌及其作用方式的研究进展进行论述,再结合本课题组近年来筛选获得的海洋抑/杀藻细菌,探讨该类菌质资源的发掘与利用,最后对该领域研究进行了展望.     

京津冀地区耕地变化分析及未来趋势预测

利用京津冀地区耕地面积统计资料为基础,采用耕地资源变化率计算方法和灰色预测法,分析和预测了该地区耕地的变化及趋势.研究结果表明:1985-2007年京津冀地区耕地总面积呈波动下降趋势,总共减少924.3 k hm2,多年平均变化率为-0.59%.耕地的三种类型之中,旱地和水田面积几乎年年减少,多年平均变化率分别为-3.57%和-0.73%,而水浇地的面积在大部分年份都有所增加,多年平均变化率为0.85%.2020年,京津冀地区的耕地总量将从2007年的6 531.61 k hm2减小至6 164.4 k hm2,耕地总面积平均每年减少0.44%,即28.7 k hm2.旱地和水田将继续保持较高的减少率,平均每年分别减少2.57%和0.84%.而水浇地的预测结果为2007年至2020年间每年稍增0.17%.在未来的十几年中,尽管耕地减少的速率减缓,但是京津冀地区耕地保护的压力依然很大.     

低温胁迫对节旋藻质膜的伤害

低温胁迫下,对鄂尔多斯高原碱湖的钝顶节旋藻(A1)、非洲Chad湖的钝顶节旋藻(A2)和墨西哥Texcoco湖的极大节旋藻(A3)的质膜伤害进行比较研究,以了解来自中纬度与低纬度不同节旋藻对低温的反应,探讨其对低温的适应性及与原产地的关系.结果表明,无论直接低温处理还是经低温锻炼后再低温处理,随温度的降低3个样品细胞外渗液中可溶性蛋白和游离氨基酸的含量均增加,且胁迫的温度越低、时间越长,细胞外渗液中两种物质的含量也越高.经低温锻炼可减弱低温胁迫对节旋藻质膜的伤害,相比之下,对A1作用更明显.在相同的处理条件下,外渗液中蛋白质和游离氨基酸的含量均是A1相似文献   

吉林濒危植物天女木兰种群分布格局与生态位研究

以吉林省通化和集安为研究地点,对两地天女木兰种群的分布格局与生态位进行了研究。结果表明：天女木兰多呈聚集分布的特征,种群变小的趋势明显,生态位明显低于分布广的建群树种,在群落中属非建群树种,对群落环境和外貌影响不大,对环境适应能力较低。天女木兰与多数树种的生态位重叠主要集中在0.1以下,相对较低,与其他树种生态位重叠较少,分布范围狭小,在群落中居次要地位;在群落中其他大多数乔木树种天女栏其种间关联均为低度而且不显著。     

A dynamic early East Antarctic Ice Sheet suggested by ice-covered fjord landscapes

The first Cenozoic ice sheets initiated in Antarctica from the Gamburtsev Subglacial Mountains and other highlands as a result of rapid global cooling ～34 million years ago. In the subsequent 20 million years, at a time of declining atmospheric carbon dioxide concentrations and an evolving Antarctic circumpolar current, sedimentary sequence interpretation and numerical modelling suggest that cyclical periods of ice-sheet expansion to the continental margin, followed by retreat to the subglacial highlands, occurred up to thirty times. These fluctuations were paced by orbital changes and were a major influence on global sea levels. Ice-sheet models show that the nature of such oscillations is critically dependent on the pattern and extent of Antarctic topographic lowlands. Here we show that the basal topography of the Aurora Subglacial Basin of East Antarctica, at present overlain by 2-4.5?km of ice, is characterized by a series of well-defined topographic channels within a mountain block landscape. The identification of this fjord landscape, based on new data from ice-penetrating radar, provides an improved understanding of the topography of the Aurora Subglacial Basin and its surroundings, and reveals a complex surface sculpted by a succession of ice-sheet configurations substantially different from today's. At different stages during its fluctuations, the edge of the East Antarctic Ice Sheet lay pinned along the margins of the Aurora Subglacial Basin, the upland boundaries of which are currently above sea level and the deepest parts of which are more than 1?km below sea level. Although the timing of the channel incision remains uncertain, our results suggest that the fjord landscape was carved by at least two iceflow regimes of different scales and directions, each of which would have over-deepened existing topographic depressions, reversing valley floor slopes.