康熙朝理学与理学名臣

从康熙朝开始,理学成为清朝统治者治国安邦的重要指导思想。在康熙帝的表率和众多理学名臣的推动下,理学在缓和满汉民族矛盾、重建社会伦理秩序中发挥了独特的作用。     

Fp上不可约多项式的周期与次数的关系

有限域Fp上的不可约多项式在密码和编码的领域研究中起着重要作用,近年来,人们对Fp上的不可约多项式周期、次数等问题进行了大量研究.文中主要研究了Fp上不可约多项式有关周期及次数的若干性质,讨论了周期和次数的关系.     

陕西省“十一五”时期发明专利文献分析

专利数据是衡量区域创新能力的指标之一,可以反映出一个地区的技术水平和竞争力。以2006—2010年的陕西省发明专利为例,对发明专利申请量的时间、地区分布及IPC重点技术领域进行了统计分析,为陕西省的科技管理和专利战略制定提供基础资料和决策依据。     

论民国文献的史料价值与保护利用

简要介绍了民国文献的收藏与保护现状,阐述了民国文献的史料价值与现实意义,探讨了加强民国文献保护与开发利用的对策。     

先秦汉语反义连用结构研究——以《荀子》为例简

反义连用结构是汉语复音化进程中的一种重要现象,但是目前研究较为薄弱。《荀子》一书提供了大量的反义连用结构,展现了反义连用结构的意义结构类型,比较全面地体现出先秦时期反义连用结构的稳定性和成熟性,而这一特性又是由反义连用结构独特的结构特点决定的。     

传播辩证论：先秦辩证传播思想及其现代理论转化

传播具有两大基本问题：一是符号能否指代意义,意义能否共享,这是符号学传统;二是交流如何进行,交流障碍能否解决,这是哲学和伦理学传统。中国先秦思想家对这两大问题的思考带有强烈的辩证色彩,深远地影响了后世。前者表现为“名实”和“言意”之辩,后者表现为“是非”与“辩讷”之争,肇始于《老子》,发展于《庄子》,经各学派争论,《荀子》集大成。学术寻根意在理论建构,需要进行“创造性转化”：将古代传播思想看成一个整体,提炼核心概念和命题,重新组成具有逻辑关联的命题系统,从而建构“传播辩证论”。     

Spatiotemporal characteristics of freezing and thawing of the active layer in the source areas of the Yellow River （SAYR）

Based on the analysis of data on temperatures and moisture of soils in the active layer at four different permafrost sites in the source areas of the Yellow River(SAYR)in 2010–2012,the freeze–thaw processes of soils in the active layer were compared and contrasted for understanding the spatiotemporal variations.At the four studied sites,the thickness and mean annual temperature of permafrost are different.The temperatures at the top of permafrost(TTOP),i.e.,the maximum depth(s)of seasonal frost and/or thaw penetration,are-1.9°C at the Chalaping site(CLP),-0.9°C at the site on the southern bank of the Zhaling Lake(ZLH),-0.4°C at the Maduo Town site(MDX),and 1.1°C at the site on the northern bank of the Eling Lake(ELH).Differences in the mean annual ground temperature of permafrost and TTOPs may be responsible for the differentiations in the freeze–thaw processes of soils in the active layer.With rising TTOPs,the ground thawing started earlier:CLP in early June,ZLH in late May,MDX in early May,and ELH in mid-April,while the freezing began later:CLP in early October,ZLH in early to midOctober,MDX in mid-October,and ELH in the mid-to late October.With increasing TTOPs,the freeze-up periods for permafrost sites were shortened:202 days at CLP,130 days at ZLH,100 days at MDX,and the period of complete thaw was 89 days at ELH.At the CLP and ZLH sites,the two-directional ground freezing(downwards from ground surfaces and upwards from the permafrost table)and thawing finished in the same year,but the ground freezing at the MDX continued to the end of the nextJanuary,with very slow freezing rates in the end.At the ELH site,ground freezing kept on until early May when thawing began on the surface,and upward and downward thawing became increasingly stable in late June to early July.At each site,with rising TTOPs,the downward freezing accelerated in comparison with the upward freezing,and with an increasing proportion of downward frozen depth,and with the larger ratios of freezing to thawing duration.In summary,the patterns of thawing and freezing processes in the active layer in the SAYR differ from those in other parts of the Qinghai–Tibet Plateau to a noticeable extent.     

Impact of the closure of Indonesian seaway on climate: A numerical modeling study

Using a global OGCM and its relevant coupled ocean-atmosphere GCM with the contemporary, 6 MaBP and 14 MaBP oceanic topography, respectively, a series of numerical experiments are implemented in order to investigate the effect of the north shift of Australian continent on the tropical oceanic circulation, especially the formation of the western Pacific warm pool. The numerical experiments of the individual OGCM forced by the modern atmospheric circulation indicate that the closure of Indonesian passage results in warming in the tropical Pacific Ocean and cooling in the tropical Indian Ocean; furthermore, it also results in change in source of the Indonesian Through Flow (ITF) water, e.g. ITF mainly originates from the south Pacific at 14 MaBP, but it mainly originates from the north Pacific now. The coupled model shows similar results as the individual OGCM qualitatively.     

川西北二叠纪栖霞期沉积相及其与油气的关系

通过对川西北地区众多下二叠统野外剖面和钻井剖面的分析,结合前人的研究成果,提出该地区在早二叠世栖霞期兼具碳酸盐台地和碳酸盐缓坡沉积特征,称为均斜台地环境。综合研究认为,均斜台地边缘浅水高能型生物滩为储层发展演化的最有利相带,主要分布于栖二时的天井山—广元西北乡一带,厚度大、分布较广,也是区内最好的勘探相带;而深缓坡和盆地环境则较有利于油气的生成与演化,主要分布于区内西北部的栖一时和栖二时。     

“十二五”时期我国投资规模合理空间分析

本文基于灰色理论以及增量资本产出率和经济增长目标,确定了“十二五”时期我国投资规模的合理空间。,结果表明,当投资率不小于23．7％时,我国投资与GDP构成的灰色系统才会保持稳定增长的状态;在既定经济增长目标和增量资本产出率波动空间的约束下,“十二五”时期我国投资率的合理空间为[27．91％,41．86％];目前我国实际投资率已经突破了合理投资率的上限,我国投资率急需进行向下调整