<?xml version="1.0" encoding="UTF-8"?><!DOCTYPE article  PUBLIC "-//NLM//DTD Journal Publishing DTD v3.0 20080202//EN" "http://dtd.nlm.nih.gov/publishing/3.0/journalpublishing3.dtd"><article xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" dtd-version="3.0" xml:lang="en" article-type="research article"><front><journal-meta><journal-id journal-id-type="publisher-id">OJMS</journal-id><journal-title-group><journal-title>Open Journal of Marine Science</journal-title></journal-title-group><issn pub-type="epub">2161-7384</issn><publisher><publisher-name>Scientific Research Publishing</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.4236/ojms.2016.63030</article-id><article-id pub-id-type="publisher-id">OJMS-67924</article-id><article-categories><subj-group subj-group-type="heading"><subject>Articles</subject></subj-group><subj-group subj-group-type="Discipline-v2"><subject>Earth&amp;Environmental Sciences</subject></subj-group></article-categories><title-group><article-title>
 
 
  Frequency and Surface Slope’s Effects on the Surface Displacement by Drilling Shallow and Deep Tunnels under Dynamic Loads
 
</article-title></title-group><contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Arash</surname><given-names>Rostami</given-names></name><xref ref-type="aff" rid="aff1"><sup>1</sup></xref><xref ref-type="corresp" rid="cor1"><sup>*</sup></xref></contrib><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Hamid</surname><given-names>Alielahi</given-names></name><xref ref-type="aff" rid="aff2"><sup>2</sup></xref><xref ref-type="corresp" rid="cor1"><sup>*</sup></xref></contrib><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Mehdi</surname><given-names>Zare</given-names></name><xref ref-type="aff" rid="aff3"><sup>3</sup></xref><xref ref-type="corresp" rid="cor1"><sup>*</sup></xref></contrib><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Kaveh</surname><given-names>Haghighi</given-names></name><xref ref-type="aff" rid="aff4"><sup>4</sup></xref><xref ref-type="corresp" rid="cor1"><sup>*</sup></xref></contrib></contrib-group><aff id="aff3"><addr-line>International Institute of Earthquake Engineering and Seismology, Tehran, Iran</addr-line></aff><aff id="aff1"><addr-line>Department of Civil Engineering, Islamic Azad University, Central Tehran Branch, Tehran, Iran</addr-line></aff><aff id="aff4"><addr-line>Research Institute of Shakhes Pajouh, Isfahan, Iran</addr-line></aff><aff id="aff2"><addr-line>Department of Civil Engineering, Islamic Azad University of Zanjan Branch, Zanjan, Iran</addr-line></aff><author-notes><corresp id="cor1">* E-mail:<email>dr.arash.rostami@gmail.com,H.AliElahi@iauz.ac.ir,Mzare@iiees.ac.ir,Kaveh.Haghighi@gmail.com(AR)</email>;<email>dr.arash.rostami@gmail.com,H.AliElahi@iauz.ac.ir,Mzare@iiees.ac.ir,Kaveh.Haghighi@gmail.com(HA)</email>;<email>dr.arash.rostami@gmail.com,H.AliElahi@iauz.ac.ir,Mzare@iiees.ac.ir,Kaveh.Haghighi@gmail.com(MZ)</email>;<email>dr.arash.rostami@gmail.com,H.AliElahi@iauz.ac.ir,Mzare@iiees.ac.ir,Kaveh.Haghighi@gmail.com(KH)</email>;</corresp></author-notes><pub-date pub-type="epub"><day>02</day><month>06</month><year>2016</year></pub-date><volume>06</volume><issue>03</issue><fpage>353</fpage><lpage>370</lpage><history><date date-type="received"><day>2</day>	<month>April</month>	<year>2016</year></date><date date-type="rev-recd"><day>accepted</day>	<month>27</month>	<year>June</year>	</date><date date-type="accepted"><day>1</day>	<month>July</month>	<year>2016</year></date></history><permissions><copyright-statement>&#169; Copyright  2014 by authors and Scientific Research Publishing Inc. </copyright-statement><copyright-year>2014</copyright-year><license><license-p>This work is licensed under the Creative Commons Attribution International License (CC BY). http://creativecommons.org/licenses/by/4.0/</license-p></license></permissions><abstract><p>
 
 
  Development and expansion of cities in one hand and increasing transport needs on the other hand have been causing underground constructions. So understanding the behavior of these structures is essential. Ground displacement around the tunneling area is one of the most important issues which have been studied by many researchers, while the effects of the slope behavior of the ground on the tunnel is paid less attention. This study will have analyzed the effects of frequency and surface slope on the surface subsidence caused by tunneling under dynamic loads (without structure). The results show that the frequency and surface slope have significant effects on the land displacements and the area surrounded by a tunnel.
 
</p></abstract><kwd-group><kwd>Tunnel</kwd><kwd> Settlement</kwd><kwd> Slope</kwd><kwd> Depth</kwd><kwd> Dynamic Loads</kwd><kwd> Abaqus</kwd></kwd-group></article-meta></front><body><sec id="s1"><title>1. Introduction</title><p>Due to the importance of the land displacement caused by shallow tunnels’ drillings in urban areas, many studies have been done on this subject by different researchers, since some decades ago. Pack (1969) did field studies on some excavated tunnels in different soils and showed that ground-level profiles’ subsidence statistical distribution is a normal curve (Gaussian) [<xref ref-type="bibr" rid="scirp.67924-ref1">1</xref>] . Then Atkinson and Potts [<xref ref-type="bibr" rid="scirp.67924-ref2">2</xref>] (1977), Clough and Schmidt [<xref ref-type="bibr" rid="scirp.67924-ref3">3</xref>] (1981), Mill and colleagues (1983) [<xref ref-type="bibr" rid="scirp.67924-ref4">4</xref>] and Leach (1985) [<xref ref-type="bibr" rid="scirp.67924-ref5">5</xref>] offered different relationships to estimate subsidence caused by tunneling operations. Pitilakis and colleagues in 2014 studied the seismic behavior of circular tunnels due to the interaction of ground structures; their main focus was on the tunnel responses, and their priority was tunnel’s behaviors. The results of this study show that in all analyzed cases, increased dynamic response of the tunnel in terms of deformation and lining in shallow tunnels is more significant [<xref ref-type="bibr" rid="scirp.67924-ref6">6</xref>] .</p><p>Alielahi and colleagues (2014) studied the use of boundary element method on time-domain for seismic response of buried cylindrical holes in soil. As a result of this research; the numerical results suggested that in a random SV wave with buried hole, horizontal component at the top of the cavity is reduced in comparison with displacement of the empty earth [<xref ref-type="bibr" rid="scirp.67924-ref7">7</xref>] .</p><p>Sika and partners examined the surface ground-domain under affections of buried and underground cavities and the ground-level domain was their main effort and activity. The results showed that the numerical methods suggest that the presence of buried craters on the earth has influence on the vacant land’s reinforce and this effect is not negligible [<xref ref-type="bibr" rid="scirp.67924-ref8">8</xref>] . Liu and colleagues in 2013 focused on the seismic behavior of buried tunnels with treating P and SV relay waves. The numerical results show that due to the effects of lined tunnels buried in the ground, linear shear modulus ratio of the average thickness is linear and has significant amounts [<xref ref-type="bibr" rid="scirp.67924-ref9">9</xref>] .</p><p>But most studies have been stated on the horizontal surface and few studies have done about the effects of the earth’s tilt on the subsidence which has been caused by tunneling operations. Heydari and his colleagues (2003) expressed that the land slope in the tunnel subsidence is negligible [<xref ref-type="bibr" rid="scirp.67924-ref10">10</xref>] . Ghazavi and Karimpour (2006) examined the slope of the surface subsidence caused by tunneling operations an announced that the land slope is not affected by this issue [<xref ref-type="bibr" rid="scirp.67924-ref11">11</xref>] .</p><p>Hasanloo Rad and colleagues in 2014 analyzed the surface slope effects on vertical displacement of tunnel’s crown and floor by ABAQUS 3D Tunnel software help, and mentioned that with increase in surface slope, displacement of tunnel’s crown and floor would have increase and the displacement of the tunnel’s walls at the bottom and top of the slope would encounter decrease [<xref ref-type="bibr" rid="scirp.67924-ref12">12</xref>] . Moosiv and Bayat in 2015 used software ABAQUS 3D Tunnel, and examined the surface slope on the surface subsidence and horizontal displacement of tunnel surrounding and they announced that any increase in ground-level slope will cause subsidence in surface level at the top of the tunnel and horizontal relocation with 6 m from the center of the tunnel at the bottom and top of the slope will be decreased or increased, respectively [<xref ref-type="bibr" rid="scirp.67924-ref13">13</xref>] . Rostami et al. [<xref ref-type="bibr" rid="scirp.67924-ref14">14</xref>] (2016) focus on investigating Effect of Tunnel Gate Shapes on ground settlements and acceleration they concluded that the rectangular tunnels had more effect in case of other tunnel shapes on ground responses. Rostami et al. [<xref ref-type="bibr" rid="scirp.67924-ref15">15</xref>] (2016) evaluated the effect of tunnel maintenances on surface and concluded that an umbrella method had significant effect on surface. Rostami et al. [<xref ref-type="bibr" rid="scirp.67924-ref16">16</xref>] (2016) evaluated effect of tunnels with different shapes on ground acceleration. Mousivan and Askari Ziarati [<xref ref-type="bibr" rid="scirp.67924-ref17">17</xref>] (2014) focused on depth of tunnel in different conditions with plaxis software. Also Alielahi et al. [<xref ref-type="bibr" rid="scirp.67924-ref18">18</xref>] (2015) worked on seismic ground amplification by unlined tunnels and concluded that The effect of the tunnel on the seismic ground surface response is gradually decreased or becomes insignificant with increasing the buried depth of the tunnel. Rostami et al. (2016) investigated Effect of Tunnel Gate Shapes with Similar Cross Section on Inserted Forces on Its Coverage and Soil Surface Settlement and conclude that the forces and settlements on rectangular tunnel shapes more than other tunnel shapes [<xref ref-type="bibr" rid="scirp.67924-ref19">19</xref>] . All the above issues are conducted in static loading state, and despite the expanded studies, evaluating the effects of dynamic loading is less considered. In this study, the effects of frequency and surface slopes on the displacements caused by tunneling under dynamic load will be discussed, using the software ABAQUS.</p></sec><sec id="s2"><title>2. Geometric Features of the Model</title><p>Earth has a dust layer according to the specifications set in <xref ref-type="table" rid="table1">Table 1</xref> [<xref ref-type="bibr" rid="scirp.67924-ref1">1</xref>] . Underground water level is lower than 50 meters from the ground.</p><p>In modeling with finite element method, choosing the model’s behavior is very important, because the stress-strain analysis is highly dependent on the behavioral model. To explain the soil behavior, the Hardening Soil Model has been used. The hardening model is a dough model which merges the shear hardening and volume hardening by using the united law to cap submission and using the in-united issue to non-diversion submission [<xref ref-type="bibr" rid="scirp.67924-ref13">13</xref>] (<xref ref-type="fig" rid="fig1">Figure 1</xref>).</p><p>Main features of this model can be summarized as follows:</p><p>・ Stress is dependent to stiffness according to the 3<sup>rd</sup> power (hard-tension power dependency)</p><p>・ The relationship between the strain and stress contribute to the deviant stress in the tri-axial tests</p><p>・ Segregation of initial loading in contrast with of reloading process</p><p>・ Failure according to Mohr-Coulomb criteria</p><p>・ Material parameters</p><p>There is a tunnel in the above land with a diameter of 8.85 m at a distance from the surface and the specifications are mentioned in <xref ref-type="table" rid="table2">Table 2</xref> and <xref ref-type="table" rid="table3">Table 3</xref>. Also the thickness of the tunnel in the form of Lining has been defined in <xref ref-type="table" rid="table4">Table 4</xref>.</p><table-wrap id="table1" ><label><xref ref-type="table" rid="table1">Table 1</xref></label><caption><title> Soil properties</title></caption><table><tbody><thead><tr><th align="center" valign="middle" >Soil Depth</th><th align="center" valign="middle" >Soil Length</th><th align="center" valign="middle" ><sub>sat</sub>γ</th><th align="center" valign="middle" >γ<sub>d</sub></th><th align="center" valign="middle" ><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/2-1470276x6.png" xlink:type="simple"/></inline-formula></th><th align="center" valign="middle" ><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/2-1470276x7.png" xlink:type="simple"/></inline-formula></th><th align="center" valign="middle" ><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/2-1470276x8.png" xlink:type="simple"/></inline-formula></th><th align="center" valign="middle" >ψ</th><th align="center" valign="middle" >φ</th><th align="center" valign="middle" >C</th><th align="center" valign="middle"  rowspan="2"  >R<sub>inter</sub></th><th align="center" valign="middle"  rowspan="2"  >υ</th></tr></thead><tr><td align="center" valign="middle" >m</td><td align="center" valign="middle" >m</td><td align="center" valign="middle" >KN/m<sup>2</sup></td><td align="center" valign="middle" >KN/m<sup>2</sup></td><td align="center" valign="middle" >KN/m<sup>2</sup></td><td align="center" valign="middle" >KN/m<sup>2</sup></td><td align="center" valign="middle" >KN/m<sup>2</sup></td><td align="center" valign="middle" >Degree</td><td align="center" valign="middle" >Degree</td><td align="center" valign="middle" >KN/m<sup>2</sup></td></tr><tr><td align="center" valign="middle" >50</td><td align="center" valign="middle" >200</td><td align="center" valign="middle" >19.2</td><td align="center" valign="middle" >19.2</td><td align="center" valign="middle" >5.67e4</td><td align="center" valign="middle" >5.67e4</td><td align="center" valign="middle" >1.7e5</td><td align="center" valign="middle" >10</td><td align="center" valign="middle" >40</td><td align="center" valign="middle" >25</td><td align="center" valign="middle" >0.7</td><td align="center" valign="middle" >0.2</td></tr></tbody></table></table-wrap><table-wrap id="table2" ><label><xref ref-type="table" rid="table2">Table 2</xref></label><caption><title> Tunnel specifications</title></caption><table><tbody><thead><tr><th align="center" valign="middle" >Kind of Tunnel</th><th align="center" valign="middle" >Tunnel Diameter</th><th align="center" valign="middle" >Thickness of Tunnel Covering</th><th align="center" valign="middle" >Tunnel Depth from the Ground</th></tr></thead><tr><td align="center" valign="middle" >Bored Tunnel</td><td align="center" valign="middle" >8.85 m</td><td align="center" valign="middle" >0.35 m</td><td align="center" valign="middle" >32 m</td></tr></tbody></table></table-wrap><table-wrap id="table3" ><label><xref ref-type="table" rid="table3">Table 3</xref></label><caption><title> Tunnels specification</title></caption><table><tbody><thead><tr><th align="center" valign="middle" >Kind of Tunnel</th><th align="center" valign="middle" >Tunnels Diameter</th><th align="center" valign="middle" >Thickness of Tunnel Covering</th><th align="center" valign="middle" >Tunnel Depth from the Ground</th></tr></thead><tr><td align="center" valign="middle" >Bored Tunnel</td><td align="center" valign="middle" >8.85 m</td><td align="center" valign="middle" >0.35 m</td><td align="center" valign="middle" >18 m</td></tr></tbody></table></table-wrap><table-wrap id="table4" ><label><xref ref-type="table" rid="table4">Table 4</xref></label><caption><title> Lining specification</title></caption><table><tbody><thead><tr><th align="center" valign="middle" >d (m)</th><th align="center" valign="middle" >υ</th><th align="center" valign="middle" >EA (KN/m<sup>2</sup>)</th><th align="center" valign="middle" >EI (KN∙m<sup>2</sup>/m)</th></tr></thead><tr><td align="center" valign="middle" >0.35</td><td align="center" valign="middle" >0.25</td><td align="center" valign="middle" >8.05e6</td><td align="center" valign="middle" >8.218e4</td></tr></tbody></table></table-wrap><fig id="fig1"  position="float"><label><xref ref-type="fig" rid="fig1">Figure 1</xref></label><caption><title> Submission level of hardening soil model [<xref ref-type="bibr" rid="scirp.67924-ref13">13</xref>] </title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/2-1470276x9.png"/></fig></sec><sec id="s3"><title>3. Modeling</title><p>In this research, modeling has been done by using finite element software ABAQUS. Meshing is in average kind with 15-points, and in sensitive areas like the tunnel’s walls finer mesh has been considered (<xref ref-type="fig" rid="fig2">Figure 2</xref> and <xref ref-type="fig" rid="fig3">Figure 3</xref>). Dynamic loads applied to the soil mass, are sinusoidal harmonic in range of 100 KN with different frequencies of 2, 4, 8 and 16 Hz and are applied to the bottom of the mass (<xref ref-type="fig" rid="fig4">Figure 4</xref>).</p><fig id="fig2"  position="float"><label><xref ref-type="fig" rid="fig2">Figure 2</xref></label><caption><title> Soil meshing of shallow tunnel</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/2-1470276x10.png"/></fig><fig id="fig3"  position="float"><label><xref ref-type="fig" rid="fig3">Figure 3</xref></label><caption><title> Soil meshing of deep tunnel</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/2-1470276x11.png"/></fig><fig id="fig4"  position="float"><label><xref ref-type="fig" rid="fig4">Figure 4</xref></label><caption><title> Dynamic load applied to soil</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/2-1470276x12.png"/></fig><disp-formula id="scirp.67924-formula1097"><label>(1)</label><graphic position="anchor" xlink:href="http://html.scirp.org/file/2-1470276x13.png"  xlink:type="simple"/></disp-formula><disp-formula id="scirp.67924-formula1098"><label>(2)</label><graphic position="anchor" xlink:href="http://html.scirp.org/file/2-1470276x14.png"  xlink:type="simple"/></disp-formula><p>In the amplitude above, A is domain, w is angular velocity and f is frequency. The amount of the initial phase (Φ) is considered as zero. Standard boundaries and energy-absorbing barriers have been used in this model. <xref ref-type="table" rid="table5">Table 5</xref> shows studies’ programs; in order to analyze the effects of frequency and slopes, 20 models have been considered.</p></sec><sec id="s4"><title>4. Vertical Displacements of the Surface in Deep Tunnels</title><p>By analyzing the models, land surface subsidence curves changes are as forms 5 to 9 (Figures 5-9).</p><table-wrap id="table5" ><label><xref ref-type="table" rid="table5">Table 5</xref></label><caption><title> Model’s specifications</title></caption><table><tbody><thead><tr><th align="center" valign="middle"  colspan="4"  >Frequency</th><th align="center" valign="middle" >Ground Slope</th><th align="center" valign="middle" ></th></tr></thead><tr><td align="center" valign="middle"  colspan="4"  >Hz</td><td align="center" valign="middle" >Degree</td><td align="center" valign="middle" >Model Number</td></tr><tr><td align="center" valign="middle" >16</td><td align="center" valign="middle" >8</td><td align="center" valign="middle" >4</td><td align="center" valign="middle" >2</td><td align="center" valign="middle" >0</td><td align="center" valign="middle" >1</td></tr><tr><td align="center" valign="middle" >16</td><td align="center" valign="middle" >8</td><td align="center" valign="middle" >4</td><td align="center" valign="middle" >2</td><td align="center" valign="middle" >2</td><td align="center" valign="middle" >2</td></tr><tr><td align="center" valign="middle" >16</td><td align="center" valign="middle" >8</td><td align="center" valign="middle" >4</td><td align="center" valign="middle" >2</td><td align="center" valign="middle" >5</td><td align="center" valign="middle" >3</td></tr><tr><td align="center" valign="middle" >16</td><td align="center" valign="middle" >8</td><td align="center" valign="middle" >4</td><td align="center" valign="middle" >2</td><td align="center" valign="middle" >10</td><td align="center" valign="middle" >4</td></tr><tr><td align="center" valign="middle" >16</td><td align="center" valign="middle" >8</td><td align="center" valign="middle" >4</td><td align="center" valign="middle" >2</td><td align="center" valign="middle" >15</td><td align="center" valign="middle" >5</td></tr></tbody></table></table-wrap><fig id="fig5"  position="float"><label><xref ref-type="fig" rid="fig5">Figure 5</xref></label><caption><title> Surface subsidence-surface slope with 0 degree</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/2-1470276x15.png"/></fig><fig id="fig6"  position="float"><label><xref ref-type="fig" rid="fig6">Figure 6</xref></label><caption><title> Surface subsidence-surface slope with 2 degrees</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/2-1470276x16.png"/></fig><fig id="fig7"  position="float"><label><xref ref-type="fig" rid="fig7">Figure 7</xref></label><caption><title> Surface subsidence-surface slope with 5 degrees</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/2-1470276x17.png"/></fig><fig id="fig8"  position="float"><label><xref ref-type="fig" rid="fig8">Figure 8</xref></label><caption><title> Surface subsidence-surface slope with 10 degrees</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/2-1470276x18.png"/></fig><fig id="fig9"  position="float"><label><xref ref-type="fig" rid="fig9">Figure 9</xref></label><caption><title> Surface subsidence-surface slope with 15 degrees</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/2-1470276x19.png"/></fig><p>In static mode with increasing slope, vertical subsidence on top of the tunnel will have increase too, and this subsidence would decrease in the left side of the tunnel and would increase for the right side. In dynamic modes, with slope increase in equal frequencies, vertical subsidence in tunnel’s summit part will increase too, this subsidence would encounter decrease in left side of the tunnel and increase in right side; these changes are due to the decrease or increase of the overloads because of the transformations in surface slopes. In general we can say that the general view of vertical displacement changes in static mode and in dynamic mode is equal. According to the above charts f = 2 in all cases the maximum amount of subsidence is in summit and around the tunnel, this amount of frequency can be considered as dominant frequency and surface slope changes has no effect on the amount of dominant frequency.</p><sec id="s4_1"><title>4.1. Horizontal Displacements of the Left Side of the Deep Tunnel</title><p>The following charts are plotted for horizontal displacements, 6 m from left side of the tunnel center (Figures 10-14).</p><fig id="fig10"  position="float"><label><xref ref-type="fig" rid="fig1">Figure 1</xref>0</label><caption><title> Surface horizontal displacement-surface slope is 0 degree</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/2-1470276x20.png"/></fig><fig id="fig11"  position="float"><label><xref ref-type="fig" rid="fig1">Figure 1</xref>1</label><caption><title> Surface horizontal displacement-surface slope is 2 degrees</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/2-1470276x21.png"/></fig><fig id="fig12"  position="float"><label><xref ref-type="fig" rid="fig1">Figure 1</xref>2</label><caption><title> Surface horizontal displacement-surface slope is 5 degrees</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/2-1470276x22.png"/></fig><fig id="fig13"  position="float"><label><xref ref-type="fig" rid="fig1">Figure 1</xref>3</label><caption><title> Surface horizontal displacement-surface slope is 10 degrees</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/2-1470276x23.png"/></fig><p>Assessing the forms 10 to 14, it can be concluded that in static mode with increasing slopes up to 5˚, the horizontal displacement of the surface due to the lower overhead, decreases and in slopes greater than 5˚ the horizontal displacement enhances. In dynamic mode on the same frequency, the horizontal displacement of the surface would decrease with increasing slopes up to 5˚, and horizontal displacement would increase for angles greater than 5˚. According to the above graphs, in the f = 2 all cases of the maximum amount of horizontal displacement of the surface can be considered (except in the case that surface slope is 5˚). This frequency can be expressed as the dominant frequency.</p></sec><sec id="s4_2"><title>4.2. Horizontal Displacements in Right Side of the Deep Tunnel</title><p>The following charts are plotted for horizontal displacement in 6 m from the right side of the tunnel center (Figures 15-19).</p><p>By examining the forms 15 and 19 we see that in a statically state by increasing the surface slope, the horizontal displacement of the surface increases, due to the increased overhead. In dynamic states with same frequencies, increasing the surface slope up to 5˚, causes decrease in the horizontal displacement and in angles</p><fig id="fig14"  position="float"><label><xref ref-type="fig" rid="fig1">Figure 1</xref>4</label><caption><title> Surface horizontal displacement-surface slope is 15 degrees</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/2-1470276x24.png"/></fig><fig id="fig15"  position="float"><label><xref ref-type="fig" rid="fig1">Figure 1</xref>5</label><caption><title> Horizontal displacement of surface-surface slope is 0 degree</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/2-1470276x25.png"/></fig><fig id="fig16"  position="float"><label><xref ref-type="fig" rid="fig1">Figure 1</xref>6</label><caption><title> Horizontal displacement of surface-surface slope is 2 degrees</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/2-1470276x26.png"/></fig><fig id="fig17"  position="float"><label><xref ref-type="fig" rid="fig1">Figure 1</xref>7</label><caption><title> Horizontal displacement of surface-surface slope is 5 degrees</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/2-1470276x27.png"/></fig><fig id="fig18"  position="float"><label><xref ref-type="fig" rid="fig1">Figure 1</xref>8</label><caption><title> Horizontal displacement of surface-surface slope is 10 degrees</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/2-1470276x28.png"/></fig><fig id="fig19"  position="float"><label><xref ref-type="fig" rid="fig1">Figure 1</xref>9</label><caption><title> Horizontal displacement of surface-surface slope is 15 degrees</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/2-1470276x29.png"/></fig><p>greater than 5˚, causes increases. According to the above graphs of f = 2, in all cases the maximum amount of horizontal displacement of the surface can be observed (except in the case in that slope is 5˚). This frequency can be expressed as the dominant frequency.</p></sec></sec><sec id="s5"><title>5. Vertical Displacements of Surface in Shallow Tunnels</title><p>By analyzing models, land surface subsidence curves’ changes can be seen as Figures 20-24.</p><p>In static mode with increasing slopes, upright subsidence will increase on top of the tunnel and decrease on the left and again increase in the right side of the tunnel. In dynamic state in same frequencies, with increase in the surface slope, subsidence will increase on top of the tunnel and also this subsidence will decrease on the left and increase on the right side of the tunnel; these changes are due to the increase or decrease of the overhead because of the slope changes. In general we can say that the general state of changes of vertical subsidence of surface in both static and dynamic states is equal. According to the above graphs f = 2, in all cases the maximum amount of subsidence is in the top and around the tunnel and this value of frequency can be expressed as the dominant frequency, and changes of surface slope have no effect on the dominant frequency.</p><fig id="fig20"  position="float"><label><xref ref-type="fig" rid="fig2">Figure 2</xref>0</label><caption><title> Surface subsidence-surface slope is 0 degree</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/2-1470276x30.png"/></fig><fig id="fig21"  position="float"><label><xref ref-type="fig" rid="fig2">Figure 2</xref>1</label><caption><title> Surface subsidence-surface slope is 2 degrees</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/2-1470276x31.png"/></fig><fig id="fig22"  position="float"><label><xref ref-type="fig" rid="fig2">Figure 2</xref>2</label><caption><title> Surface subsidence-surface slope is 5 degrees</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/2-1470276x32.png"/></fig><fig id="fig23"  position="float"><label><xref ref-type="fig" rid="fig2">Figure 2</xref>3</label><caption><title> Surface subsidence-surface slope is 10 degrees</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/2-1470276x33.png"/></fig><fig id="fig24"  position="float"><label><xref ref-type="fig" rid="fig2">Figure 2</xref>4</label><caption><title> Surface subsidence-surface slope is 15 degrees</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/2-1470276x34.png"/></fig><sec id="s5_1"><title>5.1. Horizontal Displacement of Left Side in the Shallow Tunnel</title><p>The following charts are plotted for horizontal displacement with 6 m from the left side of the tunnel center (Figures 25-29).</p><fig id="fig25"  position="float"><label><xref ref-type="fig" rid="fig2">Figure 2</xref>5</label><caption><title> Horizontal displacement-surface slope is 0 degree</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/2-1470276x35.png"/></fig><fig id="fig26"  position="float"><label><xref ref-type="fig" rid="fig2">Figure 2</xref>6</label><caption><title> Horizontal displacement-surface slope is 2 degrees</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/2-1470276x36.png"/></fig><fig id="fig27"  position="float"><label><xref ref-type="fig" rid="fig2">Figure 2</xref>7</label><caption><title> Horizontal displacement-surface slope is 5 degrees</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/2-1470276x37.png"/></fig><fig id="fig28"  position="float"><label><xref ref-type="fig" rid="fig2">Figure 2</xref>8</label><caption><title> Horizontal displacement-surface slope is 10 degrees</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/2-1470276x38.png"/></fig><fig id="fig29"  position="float"><label><xref ref-type="fig" rid="fig2">Figure 2</xref>9</label><caption><title> Horizontal displacement-surface slope is 15 degrees</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/2-1470276x39.png"/></fig><p>Studying forms 25 and 29 show that in the static state by increasing the surface slope, horizontal displacement of the ground on the left side of the tunnel will reduce due to the overhead. In dynamic states with same frequencies, horizontal displacement of the surface will decrease with increasing surface slopes up to 5˚, and will increases for angles greater than 5˚. According to the above graphs, f = 2 in all cases is the maximum amount of horizontal displacement of the surface (except in the case that the slope is 5˚). This frequency can be expressed as the dominant frequency.</p></sec><sec id="s5_2"><title>5.2. Horizontal Displacements of the Right Side of the Shallow Tunnel</title><p>The following charts are plotted for horizontal displacement with 6 m distance of the right side from center of the tunnel (Figures 30-34).</p><p>By examining the forms 30 and 34 we can see that in a static state by increasing the surface slope, horizontal displacement of the surface would increase due to the rise in the overhead. In dynamic states with same frequencies,</p><fig id="fig30"  position="float"><label><xref ref-type="fig" rid="fig3">Figure 3</xref>0</label><caption><title> Horizontal displacement-surface slope is 0 degree</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/2-1470276x40.png"/></fig><fig id="fig31"  position="float"><label><xref ref-type="fig" rid="fig3">Figure 3</xref>1</label><caption><title> Horizontal displacement-surface slope is 2 degrees</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/2-1470276x41.png"/></fig><fig id="fig32"  position="float"><label><xref ref-type="fig" rid="fig3">Figure 3</xref>2</label><caption><title> Horizontal displacement-surface slope is 5 degrees</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/2-1470276x42.png"/></fig><fig id="fig33"  position="float"><label><xref ref-type="fig" rid="fig3">Figure 3</xref>3</label><caption><title> Horizontal displacement-surface slope is 10 degrees</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/2-1470276x43.png"/></fig><fig id="fig34"  position="float"><label><xref ref-type="fig" rid="fig3">Figure 3</xref>4</label><caption><title> Horizontal displacement-surface slope is 15 degrees</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/2-1470276x44.png"/></fig><p>horizontal displacement of the surface will decrease by increasing the surface slope up to 5˚, and increases for angles greater than 5˚. According to the above graphs f = 2 in all cases is the maximum amount of the horizontal movement of the surface (except in the case with slope of 5˚). This frequency can be expressed as the dominant frequency.</p></sec></sec><sec id="s6"><title>6. Conclusions</title><p>In this study, the effects of frequency and slopes on the surface subsidence and horizontal displacement (a distance of 6 km of tunnel X) caused by tunneling under dynamic loads have been considered and summaries of the results are as follows</p><p>1) In the static mode vertical subsidence on top of the tunnel will increase with increase in surface slope, and this subsidence would decrease in the left side of the tunnel and increase in the right side.</p><p>2) Horizontal displacement of the surface beside tunnel is under affection of surface slope and this surface slope would cause decrease and increase of horizontal displacement for down side of the slope and up side of that, respectively.</p><p>3) In dynamic state with increase in the surface slope at same frequency, vertical subsidence on top of the tunnels would increase, and also this subsidence will decrease on the left side and increase on the right side of the tunnel. Horizontal displacement of the ground on the left and right side of the tunnel would decrease in the surface slope up to 5˚ and would increase in angles greater than 5˚.</p><p>4) Only one frequency in all cases (except when the slope surface is 5˚) causes the maximum displacement (f = 2) which is called dominant frequency. In the case where the surface slope is 5˚C, the dominant frequency is (f = 4), in other words it can be said that the dominant frequency change is effective on slopes. It is suggested to do complementary studies on the dominant frequency studies.</p><p>5) With increasing the depth, the amount of subsidence because of the tunnel excavations would reduce, it can be concluded that the depth is inversely related to the subsidence.</p></sec><sec id="s7"><title>Cite this paper</title><p>Arash Rostami,Hamid Alielahi,Mehdi Zare,Kaveh Haghighi, (2016) Frequency and Surface Slope’s Effects on the Surface Displacement by Drilling Shallow and Deep Tunnels under Dynamic Loads. 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