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Use of stainless reinforcing steel (SRS) in reinforced concrete (RC) structures is a promising solution to corrosion issues.
However, for SRS to be used in seismic applications, several mechanical properties need to be investigated. These include
specified and actual yield strengths, tensile strengths, uniform elongations and low-cycle fatigue behavior. Three types of
SRSs (Talley S24100, Talley 316LN and Talley 2205) were tested and the results are reported in this paper. They were compared
with the properties of A706 carbon reinforcing steel (RS), which is typical for seismic applications, and MMFX II, which is
a high strength, corrosion resistant RS. Low-cycle fatigue tests of the RS coupons were conducted under strain control with
constant amplitude to obtain strain life models of the steels. Test results show that the SRSs have slightly lower moduli
of elasticity, higher uniform elongations before necking, and better low-cycle fatigue performance than A706 and MMFX II.
All five types of RSs tested satisfy the requirements of the ACI 318 code on the lower limit of the tensile to yield strength
ratio. Except Talley 2205, the other four types of RSs investigated meet the ACI 318 requirement that the actual yield strength
does not exceed the specified yield strength by more than 18 ksi (124 MPa). Among the three types of SRSs tested, Talley S24100
possesses the highest uniform elongation before necking, and the best low-cycle fatigue performance. 相似文献
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Nisha Kurian Matthieu Lengaigne Gopalakrishna Venkata Vissa Jerome Vialard Stephane Pous Anne-Charlotte Peter Fabien Durand Shweta Naik 《Ocean Dynamics》2013,63(4):329-346
Active and break phases of the Indian summer monsoon are associated with sea surface temperature (SST) fluctuations at 30–90 days timescale in the Arabian Sea and Bay of Bengal. Mechanisms responsible for basin-scale intraseasonal SST variations have previously been discussed, but the maxima of SST variability are actually located in three specific offshore regions: the South-Eastern Arabian Sea (SEAS), the Southern Tip of India (STI) and the North-Western Bay of Bengal (NWBoB). In the present study, we use an eddy-permitting 0.25° regional ocean model to investigate mechanisms of this offshore intraseasonal SST variability. Modelled climatological mixed layer and upper thermocline depth are in very good agreement with estimates from three repeated expendable bathythermograph transects perpendicular to the Indian Coast. The model intraseasonal forcing and SST variability agree well with observed estimates, although modelled intraseasonal offshore SST amplitude is undere-stimated by 20–30 %. Our analysis reveals that surface heat flux variations drive a large part of the intraseasonal SST variations along the Indian coastline while oceanic processes have contrasted contributions depending of the region considered. In the SEAS, this contribution is very small because intraseasonal wind variations are essentially cross-shore, and thus not associated with significant upwelling intraseasonal fluctuations. In the STI, vertical advection associated with Ekman pumping contributes to ~30 % of the SST fluctuations. In the NWBoB, vertical mixing diminishes the SST variations driven by the atmospheric heat flux perturbations by 40 %. Simple slab ocean model integrations show that the amplitude of these intraseasonal SST signals is not very sensitive to the heat flux dataset used, but more sensitive to mixed layer depth. 相似文献
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GIS-based impact assessment of land-use changes on groundwater quality: study from a rapidly urbanizing region of South India 总被引:4,自引:0,他引:4
Haris H. Khan Arina Khan Shakeel Ahmed Jerome Perrin 《Environmental Earth Sciences》2011,63(6):1289-1302
This study attempts to assess the influence of changing land-use patterns on the groundwater quality of the hard rock aquifer
system in the Maheshwaram watershed, near Hyderabad, India. The study area is a rapidly urbanizing region with land development
progressing at a fast pace. To study the impact of this rapid urbanization and overall land-use transition, a groundwater
quality index (GQI) was prepared within a geographical information system (GIS). The GQI integrates the different water quality
parameters to give a final index value that can be used for spatio-temporal comparisons. The land-use transitions were closely
monitored from 2003 to 2008 using multispectral satellite images. The land-use pattern has changed drastically with an increase
in the built-up area at the expense of other land uses. The analysis reveals a rapid deterioration of groundwater quality
related mainly to the increase in built-up land with unsewered sanitation and poultry farms. Seasonal variability of the groundwater
quality was also assessed. Mean GQI decreased from 84.16 to 83.26 over a period of 5 years from 2003 to 2008, while seasonal
variability of water quality increased. GQI and Seasonal Variability of water quality were integrated in GIS to yield a groundwater
sustainability map, in terms of water quality. Zones of sustainable and unsustainable groundwater use were demarcated for
better decision making related to municipal land allotment in this rapidly urbanizing region. 相似文献
36.
阿尔金断裂带对青藏高原北部生长、隆升的制约 总被引:62,自引:3,他引:59
大量的同位素年代学证据表明(古)阿尔金断裂带可能形成于三叠纪,后又经历了侏罗纪、白垩纪的强烈左旋走滑活动,自印度板块与欧亚大陆碰撞后阿尔金断裂再次活动。主要的走滑活动发生在:(1)245~220Ma;(2)180~140Ma;(3)120~100Ma;(4)90~80Ma;(5)60~45Ma;(6)渐新世至中新世;(7)上新世至更新世以及(8)全新世。沿阿尔金断裂带,伴随左旋走滑活动形成一系列的逆冲断裂和正断裂,反映走滑过程中伴随隆升作用的存在,并且形成自北向南包括祁连山、大雪山、党河南山、柴北缘山、祁漫塔格山和昆仑山,表明阿尔金断裂带制约着青藏高原北部的生长和隆升。阿尔金断裂带东、西两端的白垩纪和新生代火山活动是断裂走滑活动的响应。 相似文献
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Genetic structure of the reef grouper Epinephelus merra in the West Indian Ocean appears congruent with biogeographic and oceanographic boundaries
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The reef fauna connectivity of the West Indian Ocean (WIO) is one of the least studied globally. Here we use genetic analyses of the grouper Epinephelus merra (Bloch 1793) to determine patterns of connectivity and to identify barriers to dispersal in this WIO marine area. Phylogeographic and population‐level analyses were conducted on cytochrome b sequences and microsatellites (13 loci) from 557 individuals sampled in 15 localities distributed across the West Indian Ocean. Additional samples from the Pacific Ocean were used to benchmark the WIO population structure. The high level of divergence revealed between Indian and Pacific localities (of about 4.5% in sequences) might be the signature of the major tectonic and climatic changes operating at the Plio‐Pleistocene transition, congruently with numerous examples of Indo‐Pacific speciation. In comparison, the E. merra sequences from the Indian Ocean constitute a monophyletic clade with a low average genetic distance (d < 0.5%). However both genetic markers indicated some structure within this ocean. The main structure revealed was the isolation of the Maldives from the WIO localities (a different group signature identified by clustering analysis, great values of differentiation). Both marker types reveal further significant structure within the WIO, mainly the isolation of the Mascarene Islands (significant AMOVA and isolation‐by‐distance patterns) and some patchy structure between the northernmost localities and within the Mozambique Channel. The WIO genetic structure of E. merra appeared congruent with main biogeographic boundaries and oceanographic currents. 相似文献
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