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<title> International Journal of Civil Engineering </title>
<link>http://ijce.iust.ac.ir</link>
<description>International Journal of Civil Engineering - Journal articles for year 2010, Volume 8, Number 2</description>
<generator>Yektaweb Collection - https://yektaweb.com</generator>
<language>en</language>
<pubDate>2010/6/11</pubDate>

					<item>
						<title>Experimental Investigation of Reverse Fault Rupture – Rigid Shallow Foundation Interaction</title>
						<link>http://www.iust.ac.ir/ijce/browse.php?a_id=364&amp;sid=1&amp;slc_lang=en</link>
						<description>&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;Ground differential movements due to faulting have been observed to cause damage to engineered structures&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;and facilities. Although surface fault rupture is not a new problem, there are only a few building codes in the world&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;containing some type of provisions for reducing the risks. Fault setbacks or avoidance of construction in the proximity&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;to seismically active faults, are usually supposed as the first priority. In this paper, based on some 1-g physical&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;modelling tests, clear perspectives of surface fault rupture propagation and its interaction with shallow rigid&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;foundations are presented. It is observed that the surface fault rupture could be diverted by massive structures seated&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;on thick soil deposits. Where possible the fault has been deviated by the presence of the rigid foundation, which&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;remained undisturbed on the footwall. It is shown that the setback provision does not give generally enough assurance&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;that future faulting would not threaten the existing structures.&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;
</description>
						<author>M.K. Jafari </author>
						<category></category>
					</item>
					
					<item>
						<title>Cyclic Behavior of Mixed Clayey Soils</title>
						<link>http://www.iust.ac.ir/ijce/browse.php?a_id=452&amp;sid=1&amp;slc_lang=en</link>
						<description>&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;Mixed clayey soils occur as mixtures of sand (or gravel) and clay in widely varying proportions. Their&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;engineering behavior has not been comprehensively studied yet. An experimental program, comprising monotonic,&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;cyclic, and post-cyclic triaxial tests was undertaken on compacted clay-granular material mixtures, having different&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;proportions of clay and sand or gravel. This paper presents the results of cyclic triaxial tests and explains the behavior&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;of the mixtures based on number of loading cycles, cyclic strain amplitude, granular material content, grain size, and&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;effective confining pressure. The results indicate an increase in degree of degradation and cyclic loading-induced pore&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;water pressure as the number of loading cycles, cyclic strain and granular material content increase. Also the results&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;show that the grain size has no significant effect on the degree of degradation and cyclic loading-induced pore water&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;pressure in the specimens. The effect of granular material content on pore water pressure during cyclic loading in&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;equal-stress-level was also examined. The pore water pressure increases with the increase of granular material&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;content.&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;
</description>
						<author>A. Soroush</author>
						<category></category>
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					<item>
						<title>Investigating Dynamic Response of a Buried Pipeline in Sandy Soil Layer by 1G Shaking Table Test</title>
						<link>http://www.iust.ac.ir/ijce/browse.php?a_id=453&amp;sid=1&amp;slc_lang=en</link>
						<description>&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;Investigating the parameters influencing the behavior of buried pipelines under dynamic loading is of great&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;importance. In this study the soil structure interaction of the pipelines with the surrounding soil was addressed using&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;shaking table tests. Wave propagation along the soil layers was also included in the study. The semi infinite nature of&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;the field was simulated using a laminar shear box. The soil used in the experiments was Babolsar coastal sand (Iran).&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;PVC pipes were used due to their analogy with the field. Eight models were constructed with the first four models&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;having uniform base. In the next models, the non-uniformities of real ground were simulated using a concrete pedestal&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;installed at the very bottom of the shear box. Pipe deformations under dynamic loading, acceleration distribution in&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;height, soil settlement and horizontal displacements were measured by strain gauges, acceleratometers and&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;displacement meters. Analyzing the obtained data, influence of different parameters of dynamic loading such as&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;acceleration, frequency, soil density, base conditions and shaking direction to pipe axis on the acceleration&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;amplification ratio and pipe deformation were investigated. Also in order to study the effect of dynamic loading on two&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;different materials, soil and pipe, the horizontal strains were compared&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;
</description>
						<author>F. Jafarzadeh</author>
						<category></category>
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					<item>
						<title>Simulating the Effects of Projectile Explosion on a Jointed Rock Mass Using 2D DEM: A Case Study of Ardebil-Mianeh Railway Tunnel</title>
						<link>http://www.iust.ac.ir/ijce/browse.php?a_id=454&amp;sid=1&amp;slc_lang=en</link>
						<description>&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;Considerations on the explosion resistant design of special infrastructures have increased in the recent&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;years. Amongst the various types of infrastructures, road and railway tunnels have a unique importance due to their&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;vital role in connection routes in emergency conditions. In this study, the explosion effects of a projectile impacting on&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;a railway tunnel located in a jointed rock medium has been simulated using 2D DEM code. Primarily, a GP2000&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;projectile has been considered as a usual projectile and its penetration depth plus its crater diameter were calculated&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;in rock mass. The blast pressure was, then, calculated via empirical formula and applied on the boundary of crater as&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;input load. Finally, the wave pressure propagation through the jointed rock medium was investigated. In part of the&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;study a sensitivity analysis has been carried out on jointed rock parameters such as joint orientation, dynamic modulus&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;and damping ratio. Their effects on tunnel lining axial force as well as bending moment have also been investigated.&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;
</description>
						<author>H. Shahnazari</author>
						<category></category>
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						<title>The Validity Assesment of Laboratory Shear Modolus Using In-Situ Seismic Piezocone Test Results</title>
						<link>http://www.iust.ac.ir/ijce/browse.php?a_id=455&amp;sid=1&amp;slc_lang=en</link>
						<description>&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;Seismic piezocone device (SCPTu) together with Resonant Column and Cyclic Triaxial test apparatus are&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;employed to measure small strain shear modulus (G0) of carbonate sandy and clayey soils of southern coasts of Iran.&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;A large area of southern regions of Iran is formed from clay, silt and sand. In this study, maximum shear modulus that&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;is derived from both field (by seismic piezocone) and laboratory (by Resonant Column and Cyclic Triaxial) tests on&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;soil samples from the southern region, indicated a meaningful effect of sample disturbance. Results show that in&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;laboratory tests, loose samples tend to become denser and therefore exhibit greater stiffness whereas dense samples&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;tend to become looser, showing a reduction in stiffness. According to the results of the present study, there are narrow&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;limits of soils shear moduli for which the laboratory tests and the field measurements yield approximately the same&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;amounts. This limit of shear moduli is about 30-50(MPa) for clay deposits and 70-100 (MPa) for sandy deposits. Since&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;the shear moduli of soils in small strains can also be computed from the shear wave velocity, also correlations based&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;on parameters derived from SCPTu test for shear wave velocity determination of sandy and clayey soils of the studied&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;area are presented. This study shows that shear wave velocity can be related to both corrected tip resistance and total&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;normal stress. The measurements of the damping ratio and shear module, because of a great disturbance of stiff&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;deposits during the sampling process and also due to considerable differences between the laboratory and field&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;results, by the laboratory approaches are not reliable and advised.&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;
</description>
						<author>S.M. Mir Mohammad Hosseini</author>
						<category></category>
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						<title>A Simple Unconventional Plasticity Model Within the Multilaminate Framework</title>
						<link>http://www.iust.ac.ir/ijce/browse.php?a_id=456&amp;sid=1&amp;slc_lang=en</link>
						<description>&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;A semi-micromechanical multilaminate model is introduced here to predict the mechanical behavior of soils.&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;This model is like a bridge between micro and macro scale upon the satisfaction of minimum potential energy level&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;during any applied stress/strain increments. The concept of this model is based on a certain number of sampling planes&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;which constitute the elastic-plastic behavior of the soil. The soil behavior presents as the summation of behavior on&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;these planes. A simple unconventional constitutive equations are used in each of the planes to describe the behavior&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;of these planes separately. An unconventional plasticity can predict the soil behavior as a smooth curve with&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;considering plastic deformation due to change of stress state inside the yield surface. The model is capable of&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;predicting softening behavior of the soil in a reasonable manner due to using unconventional plasticity. The influences&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;of induced anisotropy are included in a rational way without any additional hypotheses owing to in-nature properties&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;of the multilaminate framework. Results of this model are compared with test data and reasonable agreement is found.&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;
</description>
						<author>S. A. Sadrnejad</author>
						<category></category>
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						<title>Active Earth Pressure on Inclined Retaining Walls in Static and Pseudo-Static Conditions</title>
						<link>http://www.iust.ac.ir/ijce/browse.php?a_id=210&amp;sid=1&amp;slc_lang=en</link>
						<description>&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;Inclined retaining walls with slopes less than perpendicular are appropriate candidates in several&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;engineering problems. Yet, to the knowledge of authors, only a few analytical solution for calculation of active earth&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;pressure on such walls, which will be usually smaller than the same pressure on vertical ones, has been presented&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;neither in research papers nor in design codes. Considering limit equilibrium concept in current research, a new&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;formulation is proposed for determination of active earth pressure, angle of failure wedge and application point of&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;resultant force for inclined walls. Necessary parameters are extracted assuming the pseudo-static seismic coefficient&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;to be valid in earthquake conditions. Moreover, based on Horizontal Slices Method (HSM) a new formulation is&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;obtained for determining the characteristics of inclined walls in granular and or frictional cohesive soils. Findings of&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;present analysis are then compared with results from other available methods in similar conditions and this way, the&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;validity of proposed methods has been proved. Finally according to the results of this research, a simplified relation&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;for considering the effect of slope in reduction of active earth pressure and change in failure wedge in inclined&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;retaining walls has been proposed.&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;
</description>
						<author>A. Ghanbari</author>
						<category></category>
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						<title>Analysis of Help Model Application in Smi-Arid Areas, Study on Tehran Test Cells</title>
						<link>http://www.iust.ac.ir/ijce/browse.php?a_id=458&amp;sid=1&amp;slc_lang=en</link>
						<description>&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;Hydrologic Evaluation of Landfill Performance (HELP) model is one of the most accepted tools to simulate&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;the hydrological attributes of landfills. Although some major deviations from real values has been reported about the&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;calculated results for leachate generation by HELP model but other researchers and/or engineers in practice have&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;used it in some places to estimate amount of leachate produced in the landfills. On the Other hand this model is&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;elaborated and mainly used in developed countries with the waste having low moisture content and also in climatic&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;conditions with high precipitation. This research investigated the applicability of the model in arid areas, by&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;construction of two 30m× 50m (effective horizontal length) test cells in Kahrizak landfill (longitude=51°, 20&amp;#39,&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;latitude= 35° 27&amp;#39 degrees), and monitoring the real leachate generation from each one. A set of field capacity and&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;saturated water conductivity tests were also performed to determine basic hydrologic properties of municipal waste&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;landfilled. A comparison was made between values calculated by HELP model and recorded values, shows that a&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;prediction of leachate on annual basis can be done by HELP model with acceptable accuracy but when the infiltration&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p align=&quot;LEFT&quot;&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;of water to waste body increases due to leachate production, the model intents to underestimate water storage capacity&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;

&lt;p&gt;&lt;i&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;&lt;font face=&quot;TimesNewRomanPS-ItalicMT&quot; size=&quot;1&quot;&gt;of the landfill, which lead to deviation of calculated values from real ones.&lt;/font&gt;&lt;/font&gt;&lt;/i&gt;&lt;/p&gt;
</description>
						<author>N. Shariatmadari</author>
						<category></category>
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