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31.
Flavia De Luca Gerardo M. Verderame Fernando Gómez-Martínez Agustín Pérez-García 《Bulletin of Earthquake Engineering》2014,12(5):1999-2026
On May 11, 2011 an earthquake of magnitude 5.1 ( \(M_{w}\) ) struck Murcia region causing nine casualties and damage to buildings and infrastructures. Even if the main characteristics of the event would classify it as a moderate earthquake, the maximum Peak Ground Acceleration (PGA) registered (equal to 0.37 g) exceeded significantly local code provisions in terms of hazard at the site. This high PGA was a result of directivity effects in the near source region. An overview of earthquake characteristics and damage observed is provided. Notwithstanding the lack of proper structural design characterizing building stock in the area, most of the losses were caused by non-structural damage. According to in field observations, it emerges that masonry infills provided additional, “not designed”, strength to reinforced concrete (RC) buildings. Observed damage data, collected after the earthquake, are shown and compared to the results of a simplified approach for nonstructural damage assessment of RC infilled structures (FAST vulnerability approach). The latter comparison provided a fair accordance between observed data and analytical results. 相似文献
32.
Paolo Ricci Flavia De Luca Gerardo Mario Verderame 《Bulletin of Earthquake Engineering》2011,9(1):285-305
On 6th April 2009 an earthquake of magnitude M
w
= 6.3 occurred in the Abruzzo region; the epicentre was very close to the city of L’Aquila (about 6 km away). The event
produced casualties and damage to buildings, lifelines and other infrastructures. An analysis of the main damage that reinforced
concrete (RC) structures showed after the event is presented in this study. In order to isolate the main causes of structural
and non-structural damage, the seismological characteristics of the event are examined, followed by an analysis of the existing
RC building stock in the area. The latter issue came under scrutiny after the release of official data about structural types
and times of construction, combined with a detailed review of the most important seismic codes in force in the last 100 years
in Italy. Comparison of the current design provisions of the Italian and European codes with previous standards allows the
main weaknesses of the existing building stock to be determined. Damage to structural and non-structural elements is finally
analyzed thanks to photographic material collected in the first week after the event; the main causes of damage are then inferred. 相似文献
33.
Flavia Cristaldi 《GeoJournal》2002,58(2-3):81-90
This research examines the presence of foreign national residents in Rome, through an examination of their distribution and localisation in different administrative districts. Since there is a close relationship between localisation and access to services, job opportunities, linguistic integration, and education, the residential patterns of migrant communities need to be explored in order to foster the process of ethnic integration. The 1998 census is used to analyze the presence of foreign nationals both in the districts and in the different urban zones of the Capital. For this reason it is possible to apply the index of segregation to 7 foreign national groups and then produce maps which detail where these groups are concentrated. The study also discusses public policy issues in order to improve the process of integration of different ethnic groups in Rome. 相似文献
34.
Digiacomo Flavia Tobler Dominique J. Held Thomas Neumann Thomas 《Geochemical transactions》2020,21(1):1-22
The study presented in this work emerged as a result of a multiyear regional geochemical survey based on low-density topsoil sampling and the ensuing geochemical atlas of Croatia. This study focuses on the Dinaric part of Croatia to expound the underlying mechanisms controlling the mobilities and variations in distribution of potentially harmful elements as observed from different environmental angles. Although serious environmental degradation of the vulnerable karst soil landscapes was expected to occur chiefly through the accumulation of various heavy metals, the most acute threat materialized through the soil acidification (Al-toxicity) affecting the entire Dinaric karst area. This picture surfaced from the analysis of all three investigated discriminant function models employing the abovementioned environmental criteria selected autonomously with respect to the evaluated soil geochemistry, namely, geologic setting, regional placement and land use. These models are presented by not only the characteristic discriminant-function diagrams but also a set of appropriate mathematically derived geochemical maps disclosing the allocations of potential threats to the karst soil landscapes posed by soil acidity. 相似文献
35.
Near-fault ground motions can impose particularly high seismic demands on the structures due to the pulses that are typically observed in the velocity time-histories. The velocity pulses can be further categorized into either a distinct acceleration pulse (acc-pulse) or a succession of high-frequency, one-sided acceleration spikes (non-acc-pulse). The different characteristics of velocity pulses imply different frequency content of the ground motions, potentially causing different seismic effects on the structures. This study aims to investigate the characteristics of the two types of velocity pulses and their impacts on the inelastic displacement ratio (CR) of single-degree-of-freedom systems. First, a new method that enables an automated classification of velocity pulses is used to compile a ground motion dataset which consists of 74 acc-pulses and 45 non-acc-pulses. Several intensity measures characterizing different seismological features are then compared using the two groups of records. Finally, the influences of acc-pulses and non-acc-pulses on the CR spectra are studied; the effects of pulse period and hysteretic behavior are also considered. Results indicate that the characteristics of the two types of velocity pulses differ significantly, resulting in clearly distinct CR spectral properties between acc-pulses and non-acc-pulses. Interestingly, mixing acc-pulses and non-acc-pulses can lead to local “bumps” that were found in the CR spectral shape by previous studies. The findings of this study highlight the importance of distinguishing velocity pulses of different types when selecting near-fault ground motions for assessing the nonlinear dynamic response of structures. 相似文献
36.
Alessandra Smedile Flavia Molisso Catherine Chagué Marina Iorio Paolo Marco De Martini Stefania Pinzi Philip E. F. Collins Leonardo Sagnotti Daniela Pantosti 《Sedimentology》2020,67(3):1553-1576
Tsunami deposits present an important archive for understanding tsunami histories and dynamics. Most research in this field has focused on onshore preserved remains, while the offshore deposits have received less attention. In 2009, during a coring campaign with the Italian Navy Magnaghi, four 1 m long gravity cores (MG cores) were sampled from the northern part of Augusta Bay, along a transect in 60 to 110 m water depth. These cores were taken in the same area where a core (MS06) was collected in 2007 about 2·3 km offshore Augusta at a water depth of 72 m below sea level. Core MS06 consisted of a 6·7 m long sequence that included 12 anomalous intervals interpreted as the primary effect of tsunami backwash waves in the last 4500 years. In this study, tsunami deposits were identified, based on sedimentology and displaced benthic foraminifera (as for core MS06) reinforced by X-ray fluorescence data. Two erosional surfaces (L1 and L2) were recognized coupled with grain-size increase, abundant Posidonia oceanica seagrass remains and a significant amount of Nubecularia lucifuga, an epiphytic sessile benthic foraminifera considered to be transported from the inner shelf. The occurrence of Ti/Ca and Ti/Sr increments, coinciding with peaks in organic matter (Mo incoherent/coherent) suggests terrestrial run-off coupled with an input of organic matter. The L1 and L2 horizons were attributed to two distinct historical tsunamis (ad 1542 and ad 1693) by indirect age-estimation methods using 210Pb profiles and the comparison of Volume Magnetic Susceptibility data between MG cores and MS06 cores. One most recent bioturbated horizon (Bh), despite not matching the above listed interpretative features, recorded an important palaeoenvironmental change that may correspond to the ad 1908 tsunami. These findings reinforce the value of offshore sediment records as an underutilized resource for the identification of past tsunamis. 相似文献