参与性收藏的理论探析与思考

参与性收藏是近些年来西方一些博物馆基于"记录今天"理念而新兴的收藏。从收藏的角度,参与性收藏是博物馆通过主题策划与活动设计,组织社会公众携相关物件加入博物馆收藏,并成为馆藏的一部分,以参与的方式将公众与博物馆物品、内容、语境联系起来,其主题多与当下社会发展、生产生活方式变迁等相关,方式上突破传统收藏相对单一、封闭的模式,具有流动、共享、多元、充满活力的特点。从藏品内涵上,具有"记录今天""关注日常""突出藏品与人的关联"等特点,丰富了博物馆藏品的内涵与外延,这是对传统收藏的丰富与推进。在参与性收藏的视野下,航海类博物馆收藏具有更深广的创新空间。     

Agricultural Bank of China Debuts Facial Recognition Withdrawal in Tibet

正The Agricultural Bank of China has introduced facial recognition technology at its automatic teller machines(ATM)in Tibet.By the end of 2017,20 ATMs with facial recognition technology has been installed and 100 new ATMs will be in operation in Feb.2018.The machines can be used in Tibetan language,making them more convenient for use among local Tibetans.     

RELATIVES COMING TOGETHER

正The sun shines upon the earth in spring.The Paltang Xuanzi is a well-known dance from Paltang County,Garze Tibetan Autonomous Prefecture.In the village committee of Yarigon's Daxu Village,there are over 100 villagers gathered together,discussing something of great importance."Today,I have a bit of good news!"said Sonam Drakpa,party secretary of the town of Yarigong,while surrounded by locals."Lu Guangrong,the party secretary of Chengdu's Xihanggang Street in     

Tracing the origin of Chinese early white porcelain in the late sixth century—evidence from Xing kiln

As the criterion used by archaeologists for determining early white porcelain is quite ambiguous, the origin of Chinese white porcelain remains a point of disagreement. In this study, we systematically investigate 61 typical Xing porcelains of the late Northern dynasties to the early Sui dynasty (550–600 CE) using spectrophotometer, X-ray fluorescence (XRF), scanning electron microscopy (SEM), and X-ray powder diffraction (XRD), and analyze the differences between early white porcelain and celadon of Xing kiln in terms of their whiteness and raw materials characteristic. The results show that early white porcelain is a new type of ware that differs from celadon, which can be distinguished by whiteness, with a whiteness greater than 8% being early white porcelain and a whiteness less than 8% being celadon. It is assumed that the ancient potters created the whiter wares based on celadon by improving the glaze and selecting new raw materials for the body, but the production of this type of ware was short lived and subsequently refined in the Sui dynasty (581–618 CE) owing to the limited improvement in whiteness.     

天堑与通途:清末民初铁路与天津城市空间探析

清末民初在天津城市空间从传统的城厢向四乡拓展时,铁路的引入使该过程变得更为复杂剧烈。对于城市空间而言,铁路带来的变化并不能完全用商贸繁荣程度来衡量。东站在带来巨大的商贸利益的同时也阻断了沈王郭旺诸村居民的市内交通,使铁路两侧迥然不同,形成一块特殊的隔离区。西站的建立并没有使当地传统的商业中转中心复兴,反而因联运使得当地商业利益受到冲击。而不同城区居民也通过各自方式应对铁路带来的变化。沈王郭旺诸村居民通过呼吁政府修筑地道的方式将铁路带来的隔离效果略为降低。而西站附近居民通过疏通西站的方式使其没有彻底贯彻联运,保障了本地的商业垄断利益。     

“新历史学家”对以色列传统史学的挑战

20世纪八九十年代,一批受西方影响的以色列历史学家通过对大量解密文献的研判与调查,率先对犹太复国主义提出种种质疑,从而引发了以色列社会对主流意识形态的反思,形成了一种新的社会文化思潮——"后犹太复国主义",这些历史学家被称为"新历史学家"。他们的观点主要集中在对以色列国家合法性与官方历史阐释的修正、对犹太复国主义的重新解读、对以色列国家属性及其未来走向的质疑等方面,从而对以色列传统史学提出了挑战。"新历史学家"拓宽了历史研究的视域,推进了学术自由,有益于促进国家的世俗化与民主化进程,但他们的批判性大于建设性,有些主张过于激进且不切实际,并且在某种程度上加剧了以色列社会的动荡性。     

释荣仲方鼎“■”字

本文通过对"序"和"宫"的时代考察和字形分析,认为《荣仲方鼎》中的"■"不应释为"序",而应释为"宫",是居住之所,非宗庙。"王作荣仲宫"中的"宫"应是王对荣仲的赏赐。     

Experimental investigation of carbon dioxide trapping due to capillary retention in saline aquifers

Capillary trapping is a physical mechanism by which carbon dioxide (CO₂) is naturally immobilized in the pore spaces of aquifer rocks during geologic carbon sequestration operations, and thus a key aspect of estimating geologic storage potential. Here, we studied capillary trapping of supercritical carbon dioxide (scCO₂), and the effect of initial scCO₂ saturation and flow rate on the storage/trapping potential of Berea sandstone. We performed two‐phase, scCO₂‐brine displacements in two samples, each subject to four sequential drainage–imbibition core‐flooding cycles to quantify end‐point saturations of scCO₂ with the aid of micro‐ and macro‐computed tomography imaging. From these experiments, we found that between 51% and 75% of the initial CO₂ injected can be left behind after the brine injection. We also observed that the initial scCO₂ saturation influenced the residual scCO₂ saturation to a greater extent than the rate of brine injection under the experimental conditions examined. In spite of differences in the experimental conditions tested, as well as those reported in the literature, initial and residual saturations were found to follow a consistent relationship.     

Fluid mixing induced by hydrothermal activity in the ordovician carbonates in Tarim Basin,China

Permian hydrothermal activity in the Tarim Basin may have been responsible for the invasion of hot brines into Ordovician carbonate reservoirs. Studies have been undertaken to explain the origin and geochemical characteristics of the diagenetic fluid present during this hydrothermal event although there is no consensus on it. We present a genetic model resulting from the study of δ¹³C, δ¹⁸O, δ³⁴S, and ⁸⁷Sr/⁸⁶Sr isotope values and fluid inclusions (FIs) from fracture‐ and vug‐filling calcite, saddle dolomite, fluorite, barite, quartz, and anhydrite from Ordovician outcrops in northwest (NW) Tarim Basin and subsurface cores in Central Tarim Basin. The presence of hydrothermal fluid was confirmed by minerals with fluid inclusion homogenization temperatures being >10°C higher than the paleo‐formation burial temperatures both in the NW Tarim and in the Central Tarim areas. The mixing of hot (>200°C), high‐salinity (>24 wt% NaCl), ⁸⁷Sr‐rich (up to 0.7104) hydrothermal fluid with cool (60–100°C), low‐salinity (0 to 3.5 wt% NaCl), also ⁸⁷Sr‐rich (up to 0.7010) meteoric water in the Ordovician unit was supported by the salinity of fluid inclusions, and δ¹³C, δ¹⁸O, and ⁸⁷Sr/⁸⁶Sr isotopic values of the diagenetic minerals. Up‐migrated hydrothermal fluids from the deeper Cambrian strata may have contributed to the hot brine with high sulfate concentrations which promoted thermochemical sulfate reduction (TSR) in the Ordovician, resulting in the formation of ¹²C‐rich (δ¹³C as low as ?13.8‰) calcite and ³⁴S‐rich (δ³⁴S values from 21.4‰ to 29.7‰) H₂S, pyrite, and elemental sulfur. Hydrothermal fluid mixing with fresh water in Ordovician strata in Tarim Basin was facilitated by deep‐seated faults and up‐reaching faults due to the pervasive Permian magmatic activity. Collectively, fluid mixing, hydrothermal dolomitization, TSR, and faulting may have locally dissolved the host carbonates and increased the reservoir porosity and permeability, which has significant implications for hydrocarbon exploration.     

从孔庙看民国时期历史建筑保护现象

历代传承的寺观坛庙是我国建筑遗产的重要一类。本文以此观察民国时期的历史建筑保护现象,孔庙建筑的维护是具体案例。民国时期,这些历史建筑成为文物法规的保护对象,也形成了新的公共空间。社会以之为精神文化象征而关注其物质保存,并通过保护和使用方式发挥了教育功能。"不改变原状"原则在20世纪30年代的修复实例中有所体现。