对称赞语回应之“thank you”的研究

致谢作为一种和谐性的言语行为,本质上是礼貌的,与道歉,命令,祝贺和许诺一样,它与人们的日常生活密切相关。致谢同时又是我们日常生活中发生频率很高的一种言语行为。正确地表达致谢有着重要的社会价值。本研究从理论上增进了我们有关致谢言语行为的知识,从实践上可以帮助我们建立一个良好的人际关系和和谐的社会氛围。     

洪业对顾颉刚的学术影响

洪业对崔述《知非集》、《荍田剩笔》等著作进行研究,系统梳理了崔述著作的版本流传、学术思想和生平事迹,这对顾颉刚整理和编订《崔东壁遗书》是有价值的。洪业主持的哈佛燕京学社引得编纂处支持了顾颉刚的《尚书》研究。在《禹贡》半月刊、禹贡学会的创立和以通俗读物的形式宣传抗日的工作中,洪业作出了自己的贡献,这些都对顾颉刚的学术产生了有意义的影响。     

和谐社会视野下我国企业社会责任机制建设

企业在建设社会主义和谐社会中处于特殊的地位,其健康发展直接决定着社会的和谐程度。企业的社会责任强调再生产过程中对人的价值的关注,强调对消费者、对环境、对社会的贡献。但在我国,企业在创造社会财富的同时,却忽视了对其所造成的“负外部效应”承担本应承担的社会责任。因此,建立和完善企业社会责任机制,具有理论与实践层面的深刻意义。     

我国西部不发达区域自然资源要素转换的若干思考

西部不发达区域是我国自然资源密集地区,极具开发潜力,其经济成长采取自然资源转换模式具有客观必然性。但是传统的自然资源要素转换模式已严重制约着西部地区经济的持续发展。本通过对西部地区自然资源优势、资源开发中的技术结构和利益分配机制以及资源转换模式等问题的系统思考,提出了提升区域自然资源转换模式的构想。     

论江泽民关于社会主义现代化建设规律认识的辩证法

江泽民关于正确处理社会主义现代化建设重大关系的论述,是科学分析国际国内形势、从我国社会主义现代化建设的实践中产生的。它是我国改革开放以来现代化建设经验的概括和总结,是社会主义现代化建设生动实践和客观规律的正确反映,具有全局性、战略性、时代性的特点。     

雅尔塔体制的形成与苏联势力范围的确立

苏德战争之前 ,苏联通过与希特勒德国的合作与争夺 ,在其西北部扩张领土和建立势力范围的努力获得初步成功。第二次世界大战期间 ,苏联以战场上的胜利为基础 ,使盟国逐渐地同意了苏联关于领土和边界、安全保障和势力范围的大部分要求。最后 ,苏联和西方国家以妥协和谅解的方法确立了划分它们势力范围的雅尔塔体制     

The Challenge to ‘Informal’ Empire: Argentina,Chile and British Policy-Makers in the Immediate Aftermath of the First World War

From the late nineteenth century, both Argentina and Chile were integral parts of Britain’s ‘informal’ empire in Latin America. It has been suggested by historians that this ‘informal empire’ came to an end around the mid-twentieth century. By analysing contemporary sources from within the British government and the findings of later economic historians, it is the purpose of this article to contest this viewpoint. It will instead argue that the end of ‘informal’ empire in these countries was a direct consequence of the First World War, and that the decline in British influence in the region was registered by British policy-makers much earlier than has previously been argued.     

保持共产党员先进性长效机制初探

始终保持共产党员的先进性,是保持我们党长期执政的前提和基础。要保持党的先进性,必须建立保持共产党员先进性的长效机制。该从形成党员教育培训机制、健全党员目标管理机制、建立党员激励惩处机制、完善党员队伍吐故纳新机制、完善对党员的党内外监督机制等六个方面,对这一问题进行了探讨。     

An experimental and modeling study of Na-rich hydrothermal alteration

Sodic alteration assemblages including clinoptilolite, mordenite, analcime and Na‐montmorillonite were locally observed in sediments in the eastern part of the Hachimantai geothermal region, northeast Japan. This study investigated the mechanisms of sodic enrichment in the sediments during alteration. Kinetic results for water/rock interaction experiments are reported here. Batch‐type experiments were conducted at 150–250°C under saturated vapor pressure. Pyroclastic rocks dissolved incongruently in these experiments, and the solubility and dissolution rates among elements varied as follows: the apparent steady‐state concentrations of major elements are Si > Na ? K > Ca > Al and the order of the dissolution rates is Si > Al > Na ? K > Ca. Na had the highest steady‐state concentration and fastest dissolution rate of the alkali and alkali earth metal ions. Based on surface analysis of plagioclase, dissolution was effected via a reaction layer of Na‐montmorillonite on the mineral surface. Additionally, a reaction model constructed based on the experimentally observed reaction mechanism quantitatively explains the dissolution behavior. These results show that Na‐montmorillonite can be precipitated by pyroclastic rock/meteoric water interactions without seawater involvement: the Na is derived from the host rocks.