关于Sauer引理的一个推广

Sauer引理是统计学习理论中的基本结论．在许多实际问题中，需要研究N类模式识别问题．本文将Sauer引理推广到N类分类问题．     

乙醇三维内微肋热管的传热性能

采用实验研究的方法对三维内微肋热管的强化传热特性进行研究，首次报道了以乙醇为工质的三维内微肋热管的传热性能。在实验范围内，与光管相比，竖直放置时，沸腾换热系数可以提高98％—190％，凝结换热系数可以提高76％—178％。三维内微肋结构能够同时明显地强化热管的沸腾换热与凝结换热，可以有效地减小热管的内热阻。     

Comprehensive analysis of the chromatin landscape in Drosophila melanogaster

Chromatin is composed of DNA and a variety of modified histones and non-histone proteins, which have an impact on cell differentiation, gene regulation and other key cellular processes. Here we present a genome-wide chromatin landscape for Drosophila melanogaster based on eighteen histone modifications, summarized by nine prevalent combinatorial patterns. Integrative analysis with other data (non-histone chromatin proteins, DNase I hypersensitivity, GRO-Seq reads produced by engaged polymerase, short/long RNA products) reveals discrete characteristics of chromosomes, genes, regulatory elements and other functional domains. We find that active genes display distinct chromatin signatures that are correlated with disparate gene lengths, exon patterns, regulatory functions and genomic contexts. We also demonstrate a diversity of signatures among Polycomb targets that include a subset with paused polymerase. This systematic profiling and integrative analysis of chromatin signatures provides insights into how genomic elements are regulated, and will serve as a resource for future experimental investigations of genome structure and function.     

基于CVaR的能源互补联合系统优化配置模型研究

由于风电、光电出力具有不确定性,因此会引起电网频率的较大波动,严重影响电能质量.为了保证含有新能源电力系统的稳定运行,特提出风光水储联合调度优化模型.首先,建立含新能源的电力系统优化调度数学模型,该模型追求系统机组耗量最小.在进行含新能源发电的电力系统优化调度中,可被用来调度的出力实际为满足负荷功率后,扣除新能源输出功率的那部分火电机组出力.算例结果表明,本文采取CVaR具有良好的性能;风电与光伏清洁能源机组并入系统中增加了日前调度的不确定性风险,但通过CVaR评估计算系统风险,采取有效的措施会使系统发电成本减少与碳排放量减少.     

重介质旋流器分选机理研究

物料分选过程 ,是整个体系能量降低的过程 ,从这一原理出发 ,不同性质的固体颗粒在重介质旋流器中将位于不同的位置 ,使不同性质的固体颗粒得以分离。固体颗粒在重介质旋流器中的运动轨迹大体呈圆锥螺旋线形状 ,实测出的密度线验证了该结论     

The transition to a sulphidic ocean approximately 1.84 billion years ago

The Proterozoic aeon (2.5 to 0.54 billion years (Gyr) ago) marks the time between the largely anoxic world of the Archean (> 2.5 Gyr ago) and the dominantly oxic world of the Phanerozoic (< 0.54 Gyr ago). The course of ocean chemistry through the Proterozoic has traditionally been explained by progressive oxygenation of the deep ocean in response to an increase in atmospheric oxygen around 2.3 Gyr ago. This postulated rise in the oxygen content of the ocean is in turn thought to have led to the oxidation of dissolved iron, Fe(II), thus ending the deposition of banded iron formations (BIF) around 1.8 Gyr ago. An alternative interpretation suggests that the increasing atmospheric oxygen levels enhanced sulphide weathering on land and the flux of sulphate to the oceans. This increased rates of sulphate reduction, resulting in Fe(II) removal in the form of pyrite as the oceans became sulphidic. Here we investigate sediments from the approximately 1.8-Gyr-old Animikie group, Canada, which were deposited during the final stages of the main global period of BIF deposition. This allows us to evaluate the two competing hypotheses for the termination of BIF deposition. We use iron-sulphur-carbon (Fe-S-C) systematics to demonstrate continued ocean anoxia after the final global deposition of BIF and show that a transition to sulphidic bottom waters was ultimately responsible for the termination of BIF deposition. Sulphidic conditions may have persisted until a second major rise in oxygen between 0.8 to 0.58 Gyr ago, possibly reducing global rates of primary production and arresting the pace of algal evolution.