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This paper reviews the literature on the religion–technology nexus, drawing up a research agenda and offering preliminary empirical insights. First, I stress the need to explore the new politics of space as a consequence of technological development, emphasizing questions about the role of religion in effecting a form of religious (neo)imperialism, and uneven access to techno-religious spaces. Second, I highlight the need to examine the politics of identity and community, since cyberspace is not an isotropic surface. Third, I underscore the need to engage with questions about the poetics of religious community as social relations become mediated by technology. Finally, I focus on questions about the poetics of place, particularly the technological mediation of rituals. 相似文献
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正The 2017 Geoscience Frontiers Annual Convention was held in Beijing,China during October 19-21,2017 hosted by China University of Geosciences,Beijing(Fig.1).This convention assembled earth scientists from seven countries,including Australia(Dr.Christopher Spencer and Dr.Stijn Glorie),Korea(Dr.S.Kwon),India(Dr.Shaji Erath),Japan(Dr.Toshiaki Tsunogae and Dr.Masaki Yoshida),Russia(Dr.Inna Safonova),UK(Dr.Nick Roberts),China,and also 相似文献
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Michael D. Lee Lily Sehayek Brent E. Sleep Terry D. Vandell 《Ground Water Monitoring & Remediation》1999,19(3):82-88
A release of 1,2-dichloroethane. also known as ethylene dichloride (EDC), resulted in shallow subsurface freephase contamination of a Gulf Coast site in the southern United States. The site stratigraphy consists primarily of a low permeability, surficial peat. silt, and clay zone underlain by fractured clay; a confined 12 in deep sand ground water flow zone; a confined 21 m deep fine sand zone of limited ground water flow, followed by a deep aquitard. The Gumbo clay and sandy clay aquitard below the release area overlies and protects the 61 m deep Upper Chicot Aquifer, which is a confined regional aquifer. An ongoing recovery and hydraulic containment program from the primary impacted and laterally and vertically restricted shallow 40-foot sand zone has effectively recovered dense nonaqueous phase liquid (DNAPL) and contained dissolved phase EDC.
Natural attenuation of EDC was demonstrated through (1) a laboratory microcosm study substantiating the ability of the native microbial population in the deeper aquifer lo degrade EDC under anaerobic environmental conditions found at the site. (2) field investigations showing reductions in EDC concentrations over time in many of the wells on site, and (3) an evaluation of the ground water for EDC and its degradation products and oilier geo-chemical parameters such as dissolved oxygen, redox potential, and pH. Degradation products of EDC found in the field investigations included 2-chloroeihanol, ethanol. ethene, and ethane. Dissolved EDC concentrations in selected wells between the first recorded samples and the fourth quarter of 1997 ranged from greater than 4% to 99% reductions. First-order exponential decay half-lives ranged from 0.21 to 4.2 years for wells showing decreases in FDC concentrations over time. Elevated methane concentrations indicated carbon dioxide to be the major terminal electron acceptor. 相似文献
Natural attenuation of EDC was demonstrated through (1) a laboratory microcosm study substantiating the ability of the native microbial population in the deeper aquifer lo degrade EDC under anaerobic environmental conditions found at the site. (2) field investigations showing reductions in EDC concentrations over time in many of the wells on site, and (3) an evaluation of the ground water for EDC and its degradation products and oilier geo-chemical parameters such as dissolved oxygen, redox potential, and pH. Degradation products of EDC found in the field investigations included 2-chloroeihanol, ethanol. ethene, and ethane. Dissolved EDC concentrations in selected wells between the first recorded samples and the fourth quarter of 1997 ranged from greater than 4% to 99% reductions. First-order exponential decay half-lives ranged from 0.21 to 4.2 years for wells showing decreases in FDC concentrations over time. Elevated methane concentrations indicated carbon dioxide to be the major terminal electron acceptor. 相似文献
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Lily Kong 《Geoforum》2000,31(4)
In this paper, I examine the role of cultural policy in a newly industrialised economy, which is at the same time a state with a short history and only nascent beginnings in nation-building and efforts to construct a distinctive cultural identity. Using Singapore as the site of analyses, develop an understanding of the intersection between the economic and socio-cultural agendas behind cultural development policies. I illustrate the hegemony of the economic, supported by the ideology and language of pragmatism and globalisation. At the same time, I explore the reception of and attempts to negotiate (and at times, contest) state policies by “cultural practitioners” – artists, dancers, playwrights, actors, directors and so forth, illustrating the disjuncture between state policies and practitioners' ideals. This may be cast as a conflict between social and cultural development priorities as envisaged by the practitioners as opposed to economic development priorities as embodied in the state’s cultural economic policies. 相似文献
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Lily L. Claiborne Calvin F. Miller Joseph L. Wooden 《Contributions to Mineralogy and Petrology》2010,160(4):511-531
Hafnium, U, Th, and REE content of zircons from the Spirit Mountain batholith in southern Nevada correlate with calculated
temperatures from the Ti-in-zircon thermometer to support field and petrologic evidence of rejuvenation of crystal mush and
melt extraction events during the 2-million year accumulation of the granitoid batholith. Marked variation in zircon composition
from sample to sample, from grain to grain within individual samples, and from zone to zone within individual grains documents
in detail a history of fluctuating conditions with repeated episodes of replenishment, reheating, crystal mush rejuvenation,
fractional crystallization, and melt segregation. The zircons exhibit compositional and thermal variability indicative of
variations in host melt composition due to (1) melt rejuvenation, mixing, and fractionation (2) coeval growth of other REE-rich
accessory minerals, and possibly (3) fluctuation in fO2. 相似文献
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The 1920S Drought Recorded by Tree Rings and Historical Documents in the Semi-Arid and Arid Areas of Northern China 总被引:7,自引:0,他引:7
Eryuan Liang Xiaohong Liu Yujiang Yuan Ningsheng Qin Xiuqi Fang Lei Huang Haifeng Zhu Lily Wang Xuemei Shao 《Climatic change》2006,79(3-4):403-432
Using a network of tree-ring data, we show that there had been significant growth decline in the 1920s and early 1930s throughout
a wide area of northern China. This growth depression is indicative of a severe and sustained drought in the 1920s and early
1930s, which was then confirmed with a variety of historical and instrumental records including hydrological, meteorological,
and documentary evidence. The 1920s drought had a devastating effect not only on agricultural productivity, hydrological resources
and society in the affected areas, but also on natural vegetation, as inferred from the tree-ring network and historical records.
This research offers a picture of the drought calamity during the 1920s and early 1930s in northern China, and demonstrates
the potential to identify spatial anomalies of large-scale drought using tree-ring networks in the semi-arid and arid areas
of northern China. 相似文献
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<正>Geoscience Frontiers 2014 Annual Convention was held in Beijing,China during September 19e21,2014 hosted by China University of Geosciences,Beijing(CUGB),together with 2014 IAGR Convention and 11th International Conference on Gondwana to Asia.This grand event assembled more than 100 earth scientists from 17 countries and regions,including 相似文献
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Having analyzed the tree ring width and maximum latewood density of Pinus den-sata from west Sichuan, we obtained different climate information from tree-ring width and maximum latewood density chronology. The growth of tree ring width was responded princi-pally to the precipitation in current May, which might be influenced by the activity of southwest monsoon, whereas the maximum latewood density reflected summer temperature (June–September). According to the correlation relationship, a transfer function had been used to reconstruct summer temperature for the study area. The explained variance of re-construction is 51% (F=52.099, p<0.0001). In the reconstruction series: before the 1930s, the climate was relatively cold, and relatively warm from 1930 to 1960, this trend was in accor-dance with the cold-warm period of the last 100 years, west Sichuan. Compared with Chengdu, the warming break point in west Sichuan is 3 years ahead of time, indicating that the Tibetan Plateau was more sensitive to temperature change. There was an evident sum-mer warming signal after 1983. Although the last 100-year running average of summer tem-perature in the 1990s was the maximum, the running average of the early 1990s was below the average line and it was cold summer, but summer drought occurred in the late 1990s. 相似文献