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Journal articles on the topic 'Edifices'

Author: Grafiati

Published: 4 June 2021

Last updated: 23 February 2023

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1

Mahajan, Varun. "Dynamic Behaviour Comparison of an Irregular Edifice with Different Locations of Floating Column and Shear Wall." International Journal for Research in Applied Science and Engineering Technology 9, no. 12 (December 31, 2021): 1279–82. http://dx.doi.org/10.22214/ijraset.2021.39507.

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Abstract: Architects nowadays develop attractive edifices, and floating columns are widely employed in this process. Floating columns are used not only to provide a magnificent perspective but also when a vast open area is necessary. Edifices with irregular configurations are more vulnerable to earthquakes and hence, suitable shear wall placement is required to ensure the edifice's stability. Many multi-storey edifices collapsed in seconds after the Bhuj Earthquake (Jan 26, 2001), due to the presence of soft stories, floating columns, and mass anomalies. As a result, knowing the seismic reactions of these buildings are vital for constructing earthquake-resistant assemblies. The relevance of a Floating Column and the existence of a shear wall in an irregular multistorey building is highlighted in this study. Dynamic seismic behaviour of a G+18 irregular edifice with different locations of the floating column and different positions of the shear wall is explored in this research. The edifice is analysed and compared with the model without shear walls and floating columns to examine the alterations. The dynamic analysis is carried out using Response Spectrum Analysis and storey drift, storey displacement and base shear are calculated and finally, software compression is computed for different zones. The analysis is carried out by Indian standardized codes IS 1893:2016 and IS 456:2000 which are the codes specified by the Bureau of Indian Standards for earthquake resistance edifice design and plain and reinforcement concrete design respectively. Keywords: Floating Column, Shear Wall, Irregular Edifice, Seismic behaviour, Response Spectrum Analysis, storey drift, storey displacement, base shear.

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2

Gardner, James V., Brian R. Calder, and Andrew A. Armstrong. "Geomorphometric descriptions of archipelagic aprons off the southern flanks of French Frigate Shoals and Necker Island edifices, Northwest Hawaiian Ridge." GSA Bulletin 133, no. 9-10 (March 1, 2021): 2189–209. http://dx.doi.org/10.1130/b35875.1.

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Abstract This study describes the geomorphometries of archipelagic aprons on the southern flanks of the French Frigate Shoals and Necker Island edifices on the central Northwest Hawaiian Ridge that are hotspot volcanoes that have been dormant for 10–11 m.y. The archipelagic aprons are related to erosional headwall scarps and gullies on landslide surfaces but also include downslope gravitational features that include slides, debris avalanches, bedform fields, and outrunners. Some outrunners are located 85 km out onto the deep seafloor in water depths of 4900 m. The bedforms are interpreted to be the result of slow downslope sediment creep rather than products of turbidity currents. The archipelagic aprons appear to differ in origin from those off the Hawaiian Islands. The landslides off the Hawaiian Islands occurred because of oversteepening and loading during the constructive phase of the islands whereas the landslides off the French Frigate Shoals and Necker Island edifices may have resulted from vertical tectonics due to the uplift and relaxation of a peripheral bulge or isolated earthquakes long after the edifices passed beyond the hotspot. The lack of pelagic drape in water depths above the 4600 m depth of the local carbonate compensation depth suggests that the archipelagic apron off the French Frigate Shoals edifice is much younger, perhaps Quaternary in age, than that off the Necker Island edifice, which has a 50 m pelagic drape. The pelagic drape off the Necker Island edifice suggests that the landslides may be as old as 9 Ma. The lack of pelagic drape off the French Frigate Shoals edifice suggests that the most recent landslides are more recent, perhaps even Quaternary in age. The presence of a chute-like feature on the mid-flank of the French Frigate Shoals edifice appears to be the result of rejuvenated volcanism that occurred long after the initial volcanism ceased to build the edifice.

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3

Bahadur, Gaiutra. "Edifices of Empire." Dissent 65, no. 2 (2018): 169–73. http://dx.doi.org/10.1353/dss.2018.0041.

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4

Kadanoff, Leo P. "Cathedrals and Other Edifices." Physics Today 39, no. 11 (November 1986): 7–9. http://dx.doi.org/10.1063/1.2815195.

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5

Steele, Fiona. "Those old familiar edifices." Nature 332, no. 6161 (March 1988): 216. http://dx.doi.org/10.1038/332216a0.

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6

Babu Rajeswaran. "Visual Perception of Engineering Institutional Campuses’ Entrance Edifices of Tamil Nadu Region, India." Creative Space 7, no. 1 (July 11, 2019): 1–8. http://dx.doi.org/10.15415/cs.2019.71001.

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Institutional Campuses are increasing in numbers but struggling to market themselves in a highly competitive business domain. The entrance edifice of these campuses is an Artifact, presenting a visual representation of their imperial status in society. To empirically analyze how these edifices create meaning in recently established campuses, this paper presents a series of qualitative case studies from the Tamil Nadu region of India. Specifically, it seeks to identify the visual elements of the entrance edifice that influence observers’ perceptions of the Institutional Campus. With this regard, visual elements of the entrance edifice and their physical characters were examined and expand into a questionnaire. Through follow-up interviews with observers on the campus and analyses of the entrance edifice at each Institution, several themes were identified in the observers’ perceptions. The empirical findings suggest that several visual elements can significantly impact the visual perception of an Institutional Campus’s image: Form Identity, Architectural Elements, Scale and Portion, and Color and Material. Integrating these elements into an Institutional Campus entrance edifice design can strengthen its image in urban settings, potentially building up the image for the urban populations around the campus.

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7

Gudmundsson, A. "Strengths and strain energies of volcanic edifices: implications for eruptions, collapse calderas, and landslides." Natural Hazards and Earth System Sciences 12, no. 7 (July 19, 2012): 2241–58. http://dx.doi.org/10.5194/nhess-12-2241-2012.

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Abstract. Natural hazards associated with volcanic edifices depend partly on how fracture resistant the edifices are, i.e. on their strengths. Observations worldwide indicate that large fluid-driven extension fractures (dikes, inclined sheets), shear fractures (landslides), and mixed-mode fractures (ring dikes and ring faults) normally propagate more easily in a basaltic edifice (shield volcano) than in a stratovolcano. For example, dike-fed eruptions occur once every few years in many basaltic edifices but once every 102-3 yr in many stratovolcanoes. Large landslides and caldera collapses also appear to be more common in a typical basaltic edifice/shield volcano than in a typical stratovolcano. In contrast to a basaltic edifice, a stratovolcano is composed of mechanically dissimilar rock layers, i.e. layers with mismatching elastic properties (primarily Young's modulus). Elastic mismatch encourages fracture deflection and arrest at contacts and increases the amount of energy needed for a large-scale edifice failure. Fracture-related hazards depend on the potential energy available to propagate the fractures which, in turn, depends on the boundary conditions during fracture propagation. Here there are two possible scenarios: one in which the outer boundary of the volcanic edifice or rift zone does not move during the fracture propagation (constant displacement); the other in which the boundary moves (constant load). In the former, the total potential energy is the strain energy stored in the volcano before fracture formation; in the latter, the total potential energy is the strain energy plus the work done by the forces moving the boundary. Constant-displacement boundary conditions favor small eruptions, landslides, and caldera collapses, whereas constant-load conditions favor comparatively large eruptions, landslides, and collapses. For a typical magma chamber (sill-like with a diameter of 8 km), the strain energy change due to magma-chamber inflation is estimated at the order of 1014 J (0.1 PJ). For comparison, the surface energy needed to form a typical feeder dike is of the same order of magnitude, or 1014 J. There are several processes besides magma-chamber inflation that may increase the strain energy in a volcano before eruption. Thus, during a typical unrest period with magma-chamber inflation, the added strain energy in the volcano is large enough for a typical feeder dike to form. An injected dike, however, only reaches the surface and becomes a feeder if it is able to propagate through the numerous layers and contacts that tend to deflect or arrest dikes. The strong elastic mismatch between layers that constitute stratovolcanoes not only encourages fracture arrest, but also the storage of more strain energy (than in a typical basaltic edifice/shield volcano) before fracture formation and failure. It is thus through producing materials of widely different mechanical properties that stratovolcanoes become strong and resilient.

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8

Yeongjo Hwangbo. "Modernism in the Francoist Edifices." Journal of Mediterranean Area Studies 10, no. 4 (December 2008): 141–63. http://dx.doi.org/10.18218/jmas.2008.10.4.141.

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9

Bünzli, Jean-Claude G. "Lanthanide-containing luminescent molecular edifices." Journal of Alloys and Compounds 408-412 (February 2006): 934–44. http://dx.doi.org/10.1016/j.jallcom.2004.11.098.

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10

Carrier, Aurore, Jean-Luc Got, Aline Peltier, Valérie Ferrazzini, Thomas Staudacher, Philippe Kowalski, and Patrice Boissier. "A damage model for volcanic edifices: Implications for edifice strength, magma pressure, and eruptive processes." Journal of Geophysical Research: Solid Earth 120, no. 1 (January 2015): 567–83. http://dx.doi.org/10.1002/2014jb011485.

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11

Zhu, Hongtao, Zhiwei Zeng, Hongliu Zeng, and Changgui Xu. "3D seismic data attribute-based characterization of volcanic reservoirs in the BZ34-9 Block, Bohai Bay Basin, eastern China." GEOPHYSICS 85, no. 3 (April 1, 2020): IM1—IM13. http://dx.doi.org/10.1190/geo2019-0049.1.

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Volcanic effusive facies (VEF) and volcanic conduit facies (VCF) are two important facies units that can be found in a volcanic reservoir or edifice. Because VEF and VCF generally exhibit opposing seismic reflection characteristics, few studies have been applied to simultaneous characterization of the two facies in seismic data. We have developed an integrated 3D seismic data attribute-based characterization technique of VEF and VCF in the BZ34-9 Block, Bohai Bay Basin, eastern China. Our method is based mainly on the 3D visualization of a thresholding display so as to separately describe the strong-amplitude reflection of the VEF with its original amplitude attribute and the weak-amplitude chaotic reflection of the VCF with its variance-cube attribute. The detailed workflow comprises four steps, including seismic facies analysis, characterization of the VEF, characterization of the VCF, and merging a display of the two volcanic-facies units. The resulting 3D image of the different volcanic facies described in the BZ34-9 Block should be able to be viewed from any perspective for a better understanding of the related genesis mechanisms of the first and second members of the Shahejie (Es12) and Dongying Formations (Ed). In total, 28 volcanic edifices have been identified on the basis of the proposed method, among which three volcanic edifices exhibited inherited eruptions, in the Es12 and the Ed. Volcanic edifices in the Es12 are distributed locally in the central part of the BZ34-9 Block, showing a central eruption style, whereas those of the Ed are characterized by a widespread distribution in the southern gentle slope of the BZ34-9 Block, revealing a composite, center-fissure eruption style. The approach should be convenient to operate and would be effective in characterizing different volcanic facies simultaneously. This application can serve as a useful reference for other basins or regions with obvious volcanic influence.

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12

Acocella, Valerio, and Giuseppe Puglisi. "Hazard Mitigation of Unstable Volcanic Edifices." Eos, Transactions American Geophysical Union 91, no. 40 (2010): 357. http://dx.doi.org/10.1029/2010eo400002.

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13

Gudmundsson, Agust. "Toughness and failure of volcanic edifices." Tectonophysics 471, no. 1-2 (June 2009): 27–35. http://dx.doi.org/10.1016/j.tecto.2009.03.001.

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14

Head, James W., and Lionel Wilson. "Heat transfer in volcano–ice interactions on Mars: synthesis of environments and implications for processes and landforms." Annals of Glaciology 45 (2007): 1–13. http://dx.doi.org/10.3189/172756407782282570.

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AbstractWe review new advances in volcano–ice interactions on Mars and focus additional attention on (1) recent analyses of the mechanisms of penetration of the cryosphere by dikes and sills; (2) documentation of the glacial origin of huge fan-shaped deposits on the northwest margins of the Tharis Montes and evidence for abundant volcano–ice interactions during the later Amazonian period of volcanic edifice construction and (3) the circumpolar Hesperian-aged Dorsa Argentea Formation, interpreted as an ice sheet and displaying marginal features (channels, lakes and eskers) indicative of significant melting and interior features interpreted to be due to volcano–ice interactions (e.g. subglacial volcanic edifices, pits, basins, channels and eskers). In this context, we describe and analyse several stages and types of volcano–ice interactions: (1) magmatic interactions with ice-rich parts of the cryosphere; (2) subglacial volcanism represented by intrusion under and into the ice and formation of dikes and moberg-like ridges, intrusion of sills at the glacier–volcano substrate interface and their evolution into subglacial lava flows, formation of subglacial edifices, marginal melting and channels; (3) synglacial (ice contact) volcanism represented by flows banking up against glacier margins, chilling and forming remnant ridges and (4) post-glacial volcanism and interactions with ice deposits.

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15

Tuffen, H., D. W. McGarvie, and J. S. Gilbert. "Will subglacial rhyolite eruptions be explosive or intrusive? Some insights from analytical models." Annals of Glaciology 45 (2007): 87–94. http://dx.doi.org/10.3189/172756407782282534.

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AbstractSimple analytical models of subglacial eruptions are presented, which simulate evolving subglacial cavities and volcanic edifices during rhyolitic eruptions beneath temperate glaciers. They show that the relative sizes of cavity and edifice may strongly influence the eruption mechanisms. Intrusive eruptions will occur if the edifice fills the cavity, with rising magma quenched within the edifice and slow melting of ice. Explosive magma–water interaction may occur if a water- or steam-filled gap develops above the edifice. Meltwater is assumed to drain away continuously, but any gap above the edifice will be filled by meltwater or steam. Ductile roof closure will occur if the glacier weight exceeds the cavity pressure and is modelled here using Nye’s law. The results show that the effusion rate is an important control on the eruption style, with explosive eruptions favoured by large effusion rates. The models are used to explain contrasting eruption mechanisms during various Quaternary subglacial rhyolite eruptions at Torfajökull, Iceland. Although the models are simplistic, they are first attempts to unravel the complex feedbacks between subglacial eruption mechanisms and glacier response that can lead to a variety of eruptive scenarios and associated hazards.

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16

Levin, Rona F. "Edifices of Evidence: The Proliferation of Pyramids." Research and Theory for Nursing Practice 25, no. 1 (February 1, 2011): 8–10. http://dx.doi.org/10.1891/1541-6577.25.1.8.

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17

Reid, Mark E., Sarah B. Christian, and Dianne L. Brien. "Gravitational stability of three-dimensional stratovolcano edifices." Journal of Geophysical Research: Solid Earth 105, B3 (March 10, 2000): 6043–56. http://dx.doi.org/10.1029/1999jb900310.

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18

Elhabiri, Mourad, and Anne-Marie Albrecht-Gary. "Supramolecular edifices and switches based on metals." Coordination Chemistry Reviews 252, no. 10-11 (May 2008): 1079–92. http://dx.doi.org/10.1016/j.ccr.2007.09.014.

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19

Andra-Topârceanu, Andreea, Mihaela Verga, Mihaiu Eugen Mafteiu, Marius-Daniel Andra, Marian Marin, Radu-Daniel Pintilii, Giampietro Mazza, and Donatella Carboni. "Vulnerability Analysis of the Cultural Heritage Sites—The Roman Edifice with Mosaic, Constanța, Romania." Land 12, no. 2 (January 31, 2023): 385. http://dx.doi.org/10.3390/land12020385.

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Heritage monuments are religious, historical, strategic, or civil edifices and could be deteriorated or even damaged due to their exposure to natural and anthropogenic hazards. The Roman Edifice with Mosaic (II-IV A.D.), the largest civil edifice (2040 m2) in Eastern Europe, is an ancient civil edifice built on the steep cliff in the western part of the Black Sea, Constanța, Romania, and is exposed to geomorphological and hydrogeological processes, which are affected by degradation. The main objective of this paper is to assess the current state of this ancient historical site in relation to environmental instability and offer scientific support for the rehabilitation process through interdisciplinary and non-destructive methods. Geophysical methods had been applied to comparatively analyze the spatial variations and flows of groundwater around the Roman Edifice with Mosaic in 2008 and 2019. Geomorphological hazards had already been inventoried and mapped. The results emphasize the state of degradation of the Roman mosaic pavement and ancient walls, mainly through high variations in the deposits’ moisture due to poor maintenance, which caused suffosion, and slip processes, bringing the mosaic into a high vulnerability range. The vulnerability map of the Roman Edifice with Mosaic environment is a necessary tool for continuously improving risk management because it clearly emphasizes the sectors that still have hazards.

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20

Mazarovich, A. O. "LANDSLIDE PROCESSES ON VOLCANIC EDIFICES IN THE NORTH-EASTERN PART OF THE ATLANTIC OCEAN." BULLETIN OF KAMCHATKA REGIONAL ASSOCIATION «EDUCATIONAL-SCIENTIFIC CENTER». EARTH SCIENCES 1, no. 53 (2022): 89–103. http://dx.doi.org/10.31431/1816-5524-2022-1-53-89-103.

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In the northeastern Atlantic there are (from south to north) archipelagoes of the volcanic islands of Cape Verde, Canary, Selvagens, Madeira and Azores. They were formed on the oceanic crust in Miocene-Quaternary times. Analysis of the geological structure of the thirty islands leads to the conclusion that half of them were destroyed at different times in the course of their evolution by catastrophic landslide processes. On some of these islands such events have occurred more than once. They caused tsunamis and formed large landslide masses in the adjacent parts of the ocean. Based on the data presented, the assumption is made of volcanic edifices that may have been destroyed by landslide processes. A prerequisite for landslides on a volcanic edifice could be a shift of its center of gravity.

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21

Rajeswaran, Babu, and Thirumaran Kesavaperumal. "Perceived Institutional Campus Image and its Entrance Edifice." Open House International 43, no. 3 (September 1, 2018): 52–58. http://dx.doi.org/10.1108/ohi-03-2018-b0007.

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Entrance edifice of the institutional campus artifice as the visible representation of status in their society. The design shall stand to show the status of the person who develops the setting, it could signify the power of the person or the entire place, and it could sometimes support certain cosmological belief system that prevails in that culture too. This study intended to identify the entrance edifice Physical features that influence observer's perception of the image of the institutional campus. To accomplish this, physical features of the entrance edifice and its characters were identified and developed into questionnaire material. A logistic regression model was adopted to analyze the Physical features of Entrance Edifice. The findings found the followings: (i) Physical features of Entrance Edifice influence the Visual perception of the Institutional Campus. (ii) The Physical features were found to impact the Visual perception of the Institutional campus in the order of Form Identity, Architectural Elements, Scale and Portion, color and material. These variances are based on the observers' perception, which can be integrated into the Institutional Campus Entrance Edifice design to strengthen the Image of the Institutional campus. It is clear that Entrance Edifices have the potential to build the image for a greater content and purpose through its Form Identity, Architectural Elements, Scale and Portion, color and material. Nevertheless, the entrance design could be a powerful element to build up the image of the physical settings it serves.

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22

Braddock, Alexander A., and Emmanuel A. Theodorakis. "Marine Spirotetronates: Biosynthetic Edifices That Inspire Drug Discovery." Marine Drugs 17, no. 4 (April 19, 2019): 232. http://dx.doi.org/10.3390/md17040232.

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Spirotetronates are actinomyces-derived polyketides that possess complex structures and exhibit potent and unexplored bioactivities. Due to their anticancer and antimicrobial properties, they have potential as drug hits and deserve further study. In particular, abyssomicin C and tetrocarcin A have shown significant promise against antibiotic-resistant S. aureus and tuberculosis, as well as for the treatment of various lymphomas and solid tumors. Improved synthetic routes to these compounds, particularly the class II spirotetronates, are needed to access sufficient quantities for structure optimization and clinical applications.

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23

Merle, Olivier, and Franck Donnadieu. "Indentation of volcanic edifices by the ascending magma." Geological Society, London, Special Publications 174, no. 1 (2000): 43–53. http://dx.doi.org/10.1144/gsl.sp.1999.174.01.03.

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24

Bunzli, Jean-Claude G., Frederic Besancon, and Frederic Ihringer. "ChemInform Abstract: Bimetallic Lanthanide Supramolecular Edifices with Calixarenes." ChemInform 31, no. 52 (December 26, 2000): no. http://dx.doi.org/10.1002/chin.200052243.

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25

Falaise, Clément, Anton A. Ivanov, Yann Molard, Maria Amela Cortes, Michael A. Shestopalov, Mohamed Haouas, Emmanuel Cadot, and Stéphane Cordier. "From supramolecular to solid state chemistry: crystal engineering of luminescent materials by trapping molecular clusters in an aluminium-based host matrix." Materials Horizons 7, no. 9 (2020): 2399–406. http://dx.doi.org/10.1039/d0mh00637h.

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26

Takano, Tomoya, Florent Brenguier, Michel Campillo, Aline Peltier, and Takeshi Nishimura. "Noise-based passive ballistic wave seismic monitoring on an active volcano." Geophysical Journal International 220, no. 1 (October 18, 2019): 501–7. http://dx.doi.org/10.1093/gji/ggz466.

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SUMMARY Monitoring temporal changes of volcanic interiors is important to understand magma, fluid pressurization and transport leading to eruptions. Noise-based passive seismic monitoring using coda wave interferometry is a powerful tool to detect and monitor very slight changes in the mechanical properties of volcanic edifices. However, the complexity of coda waves limits our ability to properly image localized changes in seismic properties within volcanic edifices. In this work, we apply a novel passive ballistic wave seismic monitoring approach to examine the active Piton de la Fournaise volcano (La Réunion island). Using noise correlations between two distant dense seismic arrays, we find a 2.4 per cent velocity increase and −0.6 per cent velocity decrease of Rayleigh waves at frequency bands of 0.5–1 and 1–3 Hz, respectively. We also observe a −2.2 per cent velocity decrease of refracted P waves at 550 m depth at the 6–12 Hz band. We interpret the polarity differences of seismic velocity changes at different frequency bands and for different wave types as being due to strain change complexity at depth associated with subtle pressurization of the shallow magma reservoir. Our results show that velocity changes measured using ballistic waves provide complementary information to interpret temporal changes of the seismic properties within volcanic edifices.

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27

Akkerman, Abraham. "MYTHS OF THE NORTH AND ORIGINS OF CITY-FORM: SOME REFLECTIONS ACROSS HISTORY AND PREHISTORY." Journal of Architecture and Urbanism 39, no. 3 (September 29, 2015): 165–75. http://dx.doi.org/10.3846/20297955.2015.1088417.

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Early environmental myths of the body and the sky have been instrumental in the emergence of prehistoric urban environments, and have continued to play an important role in urban design through history to this time. The notions of the body, as the absolutely immediate, and the sky, as the unreachably distant are shown here as precursors to the core proposition of mind-environment transactions, introduced by Walter Benjamin a century ago. Late prehistory and early antiquity manifest the idea of epochal and ongoing progression in mind-city interaction, specifically, as a gender-based configuration of edifice versus space, or volume versus void, in the built environment. The North Star, as a celestial feature representing permanency and solidity, was critical in the formation of masculine myths of the environment upon which the very notion of a designed edifice had been founded, and from which the early city had emerged. The feminine counterpart of the edifice is urban void, often the garden, the street or the city square. Whereas in Neolithic communities the open ritual space seems to have been the most important design element, city-form since antiquity has habitually accentuated the masculinity of edifices over designed voids. More feminine attituted drawing on prehistoric acumen can help refocusing the emphasis on urban volume, onto dynamic urban design of open public spaces for human movement in the city.

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Zaalishvili, V. B., N. I. Nevskaya, L. N. Nevskii, and A. G. Shempelev. "Geophysical fields above volcanic edifices in the North Caucasus." Journal of Volcanology and Seismology 9, no. 5 (September 2015): 333–38. http://dx.doi.org/10.1134/s0742046315050085.

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29

Walter, Thomas R., and Valentin R. Troll. "Experiments on rift zone evolution in unstable volcanic edifices." Journal of Volcanology and Geothermal Research 127, no. 1-2 (September 2003): 107–20. http://dx.doi.org/10.1016/s0377-0273(03)00181-1.

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30

Acocella, V., and M. Neri. "Dike propagation in volcanic edifices: Overview and possible developments." Tectonophysics 471, no. 1-2 (June 2009): 67–77. http://dx.doi.org/10.1016/j.tecto.2008.10.002.

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31

Pedersen, Gro B. M., Pablo Grosse, and Magnús T. Gudmundsson. "Morphometry of glaciovolcanic edifices from Iceland: Types and evolution." Geomorphology 370 (December 2020): 107334. http://dx.doi.org/10.1016/j.geomorph.2020.107334.

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32

Reid, Mark E. "Massive collapse of volcano edifices triggered by hydrothermal pressurization." Geology 32, no. 5 (2004): 373. http://dx.doi.org/10.1130/g20300.1.

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33

Barraud, André. "Engineering supramolecular artificial edifices designed for a specific function." Biosensors and Bioelectronics 9, no. 9-10 (1994): 617–24. http://dx.doi.org/10.1016/0956-5663(94)80057-x.

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34

Saifullah, Muhammad, Jihye Gwak, and Jae Ho Yun. "Comprehensive review on material requirements, present status, and future prospects for building-integrated semitransparent photovoltaics (BISTPV)." Journal of Materials Chemistry A 4, no. 22 (2016): 8512–40. http://dx.doi.org/10.1039/c6ta01016d.

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35

Vougioukalakis, Georges E., Christopher G. Satow, and Timothy H. Druitt. "Volcanism of the South Aegean Volcanic Arc." Elements 15, no. 3 (June 1, 2019): 159–64. http://dx.doi.org/10.2138/gselements.15.3.159.

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Volcanism along the South Aegean volcanic arc began about 4.7 Ma and has lasted until the present day, with eruptions at Methana, Milos, Santorini, Kolumbo and Nisyros volcanoes in historical times. These volcanoes can be grouped into five volcanic fields: three western fields of small, mostly monogenetic edifices, and two central/eastern fields with composite cones and calderas that have produced large explosive eruptions. Crustal tectonics exerts a strong control over the locations of edifices and vents at all five volcanic fields. Tephra and cryptotephra layers in deep-marine sediments preserve a continuous record of arc volcanism in the Aegean as far back as 200,000 years. Hazards from the volcanoes include high ash plumes, pyroclastic flows and tsunamis. Monitoring networks should be improved and expanded.

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36

Diharce, Julien, Jérôme Golebiowski, Sébastien Fiorucci, and Serge Antonczak. "Fine-tuning of microsolvation and hydrogen bond interaction regulates substrate channelling in the course of flavonoid biosynthesis." Physical Chemistry Chemical Physics 18, no. 15 (2016): 10337–45. http://dx.doi.org/10.1039/c5cp05059f.

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37

Shu, Yu-Bo, and Wei-Sheng Liu. "A lanthanide salen “square prism” and a wrapped exo-lanthanide salen “double decker”." Dalton Transactions 44, no. 14 (2015): 6353–57. http://dx.doi.org/10.1039/c4dt03959a.

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We succeeded in building a lanthanide salen “square prism” and in wrapping a labile exo-lanthanide salen “double decker” by cuprous cyanide netting. Both lanthanide edifices show near-infrared (NIR) luminescence.

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Baranov, B. V., R. Werner, V. A. Rashidov, N. V. Tsukanov, and K. A. Dozorova. "MORPHOLOGY OF THE PIIP SUBMARINE VOLCANO IN THE KOMANDORSKY BASIN BASED ON MULTIBEAM ECHOSOUNDER DATA." Bulletin of Kamchatka Regional Association «Educational-Scientific Center». Earth Sciences, no. 2(50) (June 30, 2021): 6–21. http://dx.doi.org/10.31431/1816-5524-2021-2-50-6-21.

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We analyzed the bathymetric data obtained during the cruises on the German research vessel “Sonne” using multibeam echosounders within the framework of the Russian-German projects KALMAR (cruise SO201-2, 2009) and BERING (cruise SO249-2, 2016) in the Komandorsky Basin of the Bering Sea. Detailed bathymetric maps of the Piip submarine volcano were constructed. New morphological features of its summit edifices and their age relations are described, hydrothermal activity confined to the edifices is localized, and all side cones and lava flows are mapped. Based on the flank cones and fissure lava flows alignments we determined the tectonic paleostress that existed at the time of their formation, presumably after the Late Miocene-Early Pliocene. It differs from the recent tectonic stress caused by right-lateral displacements along the Bering fault zone.

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39

Liu, Cui-Lian, Li-Peng Zhou, Debakanta Tripathy, and Qing-Fu Sun. "Self-assembly of stable luminescent lanthanide supramolecular M4L6 cages with sensing properties toward nitroaromatics." Chemical Communications 53, no. 16 (2017): 2459–62. http://dx.doi.org/10.1039/c7cc00189d.

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We report here the first example of concentration-triggered helicate-to-tetrahedron transformation in supramolecular lanthanide edifices, along with their highly efficient and selective luminescence sensing properties toward PA at the ppb level.

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40

O’Hara, Daniel, Leif Karlstrom, and David W. Ramsey. "Time-evolving surface and subsurface signatures of Quaternary volcanism in the Cascades arc." Geology 48, no. 11 (July 13, 2020): 1088–93. http://dx.doi.org/10.1130/g47706.1.

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Abstract Increased resolution of data constraining topography and crustal structures provides new quantitative ways to assess province-scale surface-subsurface connections beneath volcanoes. We used a database of mapped vents to extract edifices with known epoch ages from digital elevation models (DEMs) in the Cascades arc (western North America), deriving volumes that likely represent ∼50% of total Quaternary eruptive output. Edifice volumes and spatial vent density correlate with diverse geophysical data that fingerprint magmatic influence in the upper crust. Variations in subsurface structures consistent with volcanism are common beneath Quaternary vents throughout the arc, but they are more strongly associated with younger vents. Geophysical magmatic signatures increase in the central and southern Cascade Range (Cascades), where eruptive output is largest and vents are closely spaced. Vents and correlated crustal structures, as well as temporal transitions in the degree of spatially localized versus distributed eruptions, define centers with lateral extents of ∼100 km throughout the arc, suggesting a time-evolving spatial focusing of magma ascent.

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41

MÜNN, SEBASTIAN, THOMAS R. WALTER, and ANDREAS KLÜGEL. "Gravitational spreading controls rift zones and flank instability on El Hierro, Canary Islands." Geological Magazine 143, no. 3 (May 2006): 257–68. http://dx.doi.org/10.1017/s0016756806002019.

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Ocean island volcanoes frequently develop local rift zones associated with flank movement and flank collapses. The ocean island El Hierro grew by coalescence and collapse of three volcanic edifices, which are an elongated topographic ridge (the Southern Ridge) and two semi-circular volcanic cones (Tiñor volcano, El Golfo volcano). During edifice growth and volcano coalescence, eruption fissures nucleated into rift zones that developed a complex triangle pattern. In scaled analogue experiments we could successfully reproduce the geometry of rift zones and unstable flanks as observed on El Hierro. The experimental results suggest that the rift configuration on El Hierro is the result of gravitational volcano spreading over deformable basal substrata, rather than of deep-seated magma updoming as thought previously. This paper elucidates the importance of the basal substratum and gravitational spreading, and the relationship to rifting and flank instability on El Hierro Island, and may help in understanding similar volcano architectures elsewhere.

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Brien, John O'. "Clio's "Cabinet": Metaphorical Edifices in Ronsard's "Hymnes" of 1555-1556." Modern Language Review 81, no. 1 (January 1986): 37. http://dx.doi.org/10.2307/3728763.

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43

Scheel, Michael J., Margit Berman, Myrna L. Friedlander, Collie W. Conoley, Changming Duan, and Susan C. Whiston. "Counseling-Related Research in Counseling Psychology: Creating Bricks, Not Edifices." Counseling Psychologist 39, no. 5 (June 14, 2011): 719–34. http://dx.doi.org/10.1177/0011000011410894.

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44

Sheina, S. G., I. Y. Zilberova, and A. O. Vongay. "Energy-saving processes simulation in reconstruction of educational institutions edifices." MATEC Web of Conferences 117 (2017): 00153. http://dx.doi.org/10.1051/matecconf/201711700153.

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45

Mel’nikov, M. E., S. P. Pletnev, V. M. Anokhin, T. E. Sedysheva, and V. V. Ivanov. "Volcanic edifices on guyots of the Magellan Seamounts (Pacific Ocean)." Russian Journal of Pacific Geology 10, no. 6 (November 2016): 435–42. http://dx.doi.org/10.1134/s1819714016060038.

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Guest, John E., Mark H. Bulmer, Jayne Aubele, Kathi Beratan, Ronald Greeley, James W. Head, Gregory Michaels, Catherine Weitz, and Charles Wiles. "Small volcanic edifices and volcanism in the plains of Venus." Journal of Geophysical Research 97, E10 (1992): 15949. http://dx.doi.org/10.1029/92je01438.

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Connor, Patrick E. "Edifices and Ego: An Investor's View of Managerial (In)Effectiveness." Journal of Management Inquiry 3, no. 2 (June 1994): 207–12. http://dx.doi.org/10.1177/105649269432012.

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48

Grosse, Pablo, Benjamin van Wyk de Vries, Pablo A. Euillades, Matthieu Kervyn, and Iván A. Petrinovic. "Systematic morphometric characterization of volcanic edifices using digital elevation models." Geomorphology 136, no. 1 (January 2012): 114–31. http://dx.doi.org/10.1016/j.geomorph.2011.06.001.

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49

MORIYA, Ichio. "Evolution and Classification of Volcanic Edifices on the Philippine Islands." Journal of Geography (Chigaku Zasshi) 123, no. 1 (2014): 89–122. http://dx.doi.org/10.5026/jgeography.123.89.

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50

Wright, Jack, David A. Rothery, Matthew R. Balme, and Susan J. Conway. "Constructional Volcanic Edifices on Mercury: Candidates and Hypotheses of Formation." Journal of Geophysical Research: Planets 123, no. 4 (April 2018): 952–71. http://dx.doi.org/10.1002/2017je005450.

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