Playing with Fire: The 4th Duke of Hamilton's Jacobite Politics and the Union

James Hamilton, duke of Hamilton and the Scots jacobites are generally linked in analyses of the final years of the Scots polity. Indeed, Hamilton is often presented as the leader of the jacobite party in the Scottish parliament. Yet both contemporaries and historians have been unsure what to make of his on-again, off-again, conduct with respect to the exiled Stuarts and France. This has fuelled an ongoing debate about Hamilton's erratic and highly enigmatic behaviour during the winter of 1706–7, when the Union was passing the Scottish parliament. Was he genuinely opposing the Union? Was he duped by the court? Or was he, ‘bought and sold for English gold ’? This essay takes a fresh look at the duke and his part in the Union crisis in the light of new and previously underused jacobite sources with a view to better understanding Hamilton's aims, objectives, and influence with this crucial group. Only the jacobites and the Cameronians were potentially willing to take their opposition to the Union to God's Acre. But neither party immediately flew to arms in response to passage of a union they both believed was a betrayal of everything they held dear, and Hamilton was a major factor in their failure to do so. This essay thus takes a close look at the duke's part in preventing a major national uprising against the Union in the winter of 1706–7 and advances a new interpretation of his conduct and significance throughout the Union crisis.     

新见三件“叔休”器及相关问题

本文通过研究追缴回来的三件"叔休器"和见于著录的五件"叔休器",判断目前所见所有"叔休器"均属同一器主。叔休可能为春秋早期管理当地盐业贸易的职官,身份地位均较重要。同时结合铭文内容等认为"叔休器"可能来源于淮河流域信阳一带的周代诸侯小国"冠"。冠、番、樊等可能是被淮河以外诸国称"繁"的不同小国,它们位于淮河流域信阳一带,在商周时期盐铜贸易环节发挥了重要作用,逐渐形成盐铜交易枢纽"繁阳"。     

A reexamination of the reasons for the closure of the Dunhuang Library Cave

Abstract

Cave 17 or the cave library is located on the northern wall in the hallway of Cave 16 in Mogao Caves, Dunhuang. The murals on the cover layer of Cave 16 are closely connected with the reason why the cave library was sealed. The transformation tableaux of the thousand Buddhas on the cover layer of Cave 16 seems to reflect the thought of the Final Dharma, which could be dated in the late Guiyijun period when Dunhuang was ruled by the Cao family. In 1052, the trend of the Final-Dharma thought flourished in the Liao Dynasty. With the frequent communications between the Guiyijun regime and the Liao, this trend came to Dunhuang and merged with the original thought of the Final Dharma in this region, which tremendously impacted the Buddhist community in Dunhuang. So the local Buddhist community made the transformation tableaux on the mural of Cave 16 and also transformed Cave 17 for storing Buddhist texts as a response to the coming Final Dharma. These activities seem to have led to the eventual sealing of Cave 17.     

商末黄河中游气候环境的变化与社会变迁

新石器时代到商代黄河流域的气候属于温暖湿润期;商代后期气候出现厂干旱化,导致了古公亶父迁岐,文王迁程迁丰,帝乙帝辛时不断向南方发展;而商末的旱灾和饥荒是周武王克商的直接导火索,导致商周之际的改朝换代。商末气候环境的变迁对其时社会政治的影响极大。     

上海高级服务性公寓经营管理初探

本对酒店公寓行业特点作了较为全面的论述,并结合特定公寓酒店的管理实践,论述了高级服务性公寓经营管理特点,为如何推动酒店公寓行业的发展提供了第一手素材。     

不同添加成分对书画装裱浆糊抑菌效果的评价试验

古代文献中著录的各种书画装裱浆糊添加成分中,有一部分具有防腐防霉的功效。本文利用浆糊药液琼脂培养基,对白矾、花椒、白芨、百部、丁香等添加成分进行抑菌效果评价,结果发现,白矾、百部有明显抑菌效果,花椒、丁香有一定抑菌效果,白芨抑菌效果不明显。     

黄宗智“过密化”理论中的事实判定、逻辑分析与模式建构问题——以《长江三角洲小农家庭与乡村发展》为中心

黄宗智的“过密化”理论自其《长江三角洲小农家庭与乡村发展》于20世纪90年代初出版之后一直在国内外史学界影响广泛,它认为明清以来的人口增长导致了长江三角洲植棉等经济行业的单位工作日劳动报酬的递减。鉴于史学界至今未有人从该书内部详细分析这一理论的实际论证过程,本文以此为切入点,指出它存在：一,植棉经济发韧于明代等诸多事实判定疏误或不当之处;二,抽样数据的数量严重不足等统计数据问题;三,植棉等经济行业的单位工作日劳动报酬因其单位产出价格的巨幅变动而无法简单比较等逻辑分析方面的问题。据此,本文认为该书没能有效证明过密化理论符合明清时期长江三角洲的历史发展事实。     

三年经济困难时期的紧急救灾措施

1959～1961年三年困难时期,党和国家认真总结经验,注意纠正错误,全力领导人民进行了救灾斗争,采取了精简城市人口、降低粮食征购量、紧急调运和进口粮食、节衣缩食"瓜菜代"、提高粮食收购价、大办农业等一系列措施,逐步扭转了局面,保持了社会秩序的相对稳定。     

明末清初文人命运之管窥——侯方域生平考

侯方域是明末清初著名的文人之一,他出生于名门望族,受过良好的教育,很早就名满天下。他早年交游广阔,与当时的一帮名士朝夕对酒作诗,品评当世人物,颇有济世之志。后来,因得罪了小人,自己落得四处飘零,又由于农民战争及清军的蹂躏,他的大部分好友都散去或死去;明清易代,他又成了夹缝中的遗民。他虽然英年早逝,但短暂的一生却历经巨变沧桑。     

Modeling fluid flow in a heterogeneous, fault-controlled hydrothermal system

Previous studies have shown that most hydrothermal systems discharging at the land surface are associated with faulting, and that the location, temperature and rate of discharge of these systems are controlled by the geometry and style of the controlling fault(s). Unfortunately, the transport of heat and fluid in fault-controlled hydrothermal systems is difficult to model realistically; although heterogeneity and anisotropy are assumed to place important controls on flow in faults, few data or observations are available to constrain the distribution of hydraulic properties within active faults. Here, analytical and numerical models are combined with geostatistical models of spatially varying hydraulic properties to model the flow of heat and fluid in the Borax Lake fault of south-east Oregon, USA. A geometric mean permeability within the fault of 7 × 10⁻¹⁴ m² with 2× vertical/horizontal anisotropy in correlation length scale is shown to give the closest match to field observations. Furthermore, the simulations demonstrate that continuity of flow paths is an important factor in reproducing the observed behavior. In addition to providing some insight into possible spatial distributions of hydraulic properties at the Borax Lake site, the study highlights one potential avenue for integrating field observations with simulation results in order to gain greater understanding of fluid flow in faults and fault-controlled hydrothermal and petroleum reservoirs.