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101.
The sources which offer insights into the life of Duke William IX of Aquitaine, the ‘first troubadour’, are few and disparate in nature. This study focuses on the conclusions which have been drawn from Anglo-Norman chroniclers' accounts of his clashes with the Church, reportedly over the issue of his adultery, and on Latin poems in praise of the bishop who excommunicated William and whom the duke persecuted.While it is generally believed that the duke married twice, close investigation shows this to be based largely on an error in a nineteenth-century secondary source: it is probable that Philippa of Toulouse was William's only wife. A new reading is proposed of the major Latin verse-compositions referring to the duke's excommunication (1114-17) and it is suggested that the historical evidence concerning the Poitevin claim to the country of Toulouse does not match well with the notion that William attempted to repudiate his wife Philippa, on whom this claim depended.  相似文献   
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The purpose of this two-part symposium of the Policy Studies Journal is to broaden theconcept of disability policy from one that has relevance onlyforpeople interested in that substantive area to that of a major field of social policy having ramifications for the study and teaching of public policy broadly construed. The goal is for experiences in disability policy to be regarded in the same way that experiences in Other substantive areas, such as environmental policy, other social services, and civil rights, illustrate broader themes in areas such as public management, policy analysis, or ethics.  相似文献   
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Book reviews     
Tsuyoshi Kato. Matriliny and migration: evolving Minangkabau traditions in Indonesia. 267 pp. Ithaca and London: Cornell University Press, 1982. $28.10.

E. M. Beekman (tr.). The poison tree. Selected writings of Rimphius on the natural history of the Indies. Amherst: University of Massachusetts Press, 1981. (Library of the Indies.) $20.

Nigel Phillips. Sijobang: sung narrative poetry of West Sumatra, xi, 255 pp. Cambridge, etc: Cambridge University Press, 1981. (Cambridge Studies in Oral and Literate Culture, I.) £22.50.

Bernd Nothofer. Dialektatlas von Zentral‐Java. vi, 32 pp., 337 maps. Wiesbaden: Otto Harrassowitz, 1981. DM 64.

Marlene van Doom and cthers (ed.). Improving access to Indonesian collections in the Netherlands: contributions to a survey of Dutch library and documentation activities in the field of Indonesian studies. Edited by Mavlene van Doorn, Irene Farjon, Ciska Pattipilohy, Gerard J Telkamp. [iv], 78 pp. Leiden: Centre for the History of European Expansion (University of Leiden) in cooperation with the Koninklijk Instituut voor de Tropen for the Contactgroep Documentatie Indonesie, 1981. (Intercon‐tinenta, No. 2.)

Leo Suryadinata. Eminent Indonesian Chinese: biographical sketches. Revised edition. 218 pp. Singapore: Gunung Agung, 1981.

A. Ed. Schmidgall‐Tellings and Alan M Stevens. Contemporary Indonesian‐English dictionary: a supplement to the standard Indonesian dictionaries with particular concentration on new words3 expressions, and meanings, xv, 388 pp. Athens, Ohio, etc: Ohio University Press, [C1981].

Peter B R Carey (tr.). Babad Dipanagara. An account of the outbreak of the Java War (1825–30). “ The Surdkarta court version of the Babad Dipanagara with translations into English and Indonesian Malay, lxxiii, 344 pp., front., 4 plates, map. Kuala Lumpur: printed for the Council of the M.B.R.A.S. by Art Printing Works Sdn. Bhd., 1981. (Malaysian Branch of the Royal Asiatic Society. Monograph No. 9.) M$55.  相似文献   

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To investigate the kinetics of interfacial energy‐driven fluid infiltration, experiments were carried out in a quartzite–water system at 621–925°C and 0.8 GPa. Infiltration couples were made by juxtaposing presynthesized dry quartzite cylinders and fluid reservoirs. The infiltration process was confirmed by the presence of pores at the quartzite grain edges. As predicted from theoretical considerations and previous experiments, wetting fluids such as pure water and NaCl aqueous solution infiltrated into quartzite, whereas nonwetting CO2‐rich fluids did not. Newly precipitated quartz layers at the surfaces of the infiltrated sample proved that infiltration took place by a dissolution–precipitation mechanism. The enhancement of grain growth by fluid infiltration was observed over the entire range of experimental temperatures. The fluid fraction, gauged by the porosity of the run products, increases at the infiltration front and then decreases towards the fluid reservoir to form a high‐porosity zone with a maximum porosity of 2.3–2.9%. As infiltration proceeds, the high‐porosity zone advances like a travelling wave. This porosity wave is probably caused by a grain curvature gradient resulting from preferential grain growth in the infiltrated part of the quartzite, perhaps combined with other factors. The infiltration kinetics were modelled with a steady‐state diffusion model over the high‐porosity zone. The solubility difference between dissolving and precipitating grains was deduced to be 2 × 10?2?3 × 10?1 wt %. The experimentally obtained infiltration rate of aqueous fluid in the steady‐state diffusion regime (2 ± 0.5 × 10?8 m sec?1 at 823°C) is much faster than the estimated metamorphic fluid flux rates, so that interfacial energy‐driven fluid redistribution in quartz‐rich layers could significantly contribute to the fluid flux in high‐grade metamorphism, at least over a short distance. Cathodoluminescence observations of the run products revealed that the grain growth of quartzite in the presence of fluid proceeds extensively, which would promote the chemical equilibration between fluid and rock more effectively than would volume diffusion in quartz crystals.  相似文献   
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