<?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">OJAppS</journal-id><journal-title-group><journal-title>Open Journal of Applied Sciences</journal-title></journal-title-group><issn pub-type="epub">2165-3917</issn><publisher><publisher-name>Scientific Research Publishing</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.4236/ojapps.2015.55023</article-id><article-id pub-id-type="publisher-id">OJAppS-56552</article-id><article-categories><subj-group subj-group-type="heading"><subject>Articles</subject></subj-group><subj-group subj-group-type="Discipline-v2"><subject>Biomedical&amp;Life Sciences</subject><subject> Chemistry&amp;Materials Science</subject><subject> Computer Science&amp;Communications</subject><subject> Engineering</subject><subject> Physics&amp;Mathematics</subject></subj-group></article-categories><title-group><article-title>
 
 
  Design of Underground Pipelines under Arbitrary Seismic Loading
 
</article-title></title-group><contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>iyorbek</surname><given-names>Bekmirzaev</given-names></name><xref ref-type="aff" rid="aff1"><sub>1</sub></xref><xref ref-type="corresp" rid="cor1"><sup>*</sup></xref></contrib></contrib-group><aff id="aff1"><label>1</label><addr-line>Institute of Seismic Stability of Structures, Academy of Sciences of the Republic of Uzbekistan, Tashkent, 
Republic of Uzbekistan</addr-line></aff><author-notes><corresp id="cor1">* E-mail:<email>diyorbek_84@mail.ru</email></corresp></author-notes><pub-date pub-type="epub"><day>12</day><month>05</month><year>2015</year></pub-date><volume>05</volume><issue>05</issue><fpage>226</fpage><lpage>232</lpage><history><date date-type="received"><day>8</day>	<month>April</month>	<year>2015</year></date><date date-type="rev-recd"><day>accepted</day>	<month>18</month>	<year>May</year>	</date><date date-type="accepted"><day>22</day>	<month>May</month>	<year>2015</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>
 
 
  On the basis of Hamilton-Ostrogradskiy variation principle a system of equations of linear pipeline vibrations interacting with surrounding soil is derived with appropriate boundary and initial conditions under arbitrary direction of seismic effect. Dynamic problem of underground pipeline is solved by finite difference method of the second order of accuracy with different combinations of boundary conditions under the effect of seismic load on a given law with arbitrary direction. Numerical implementation of the problem is realized.
 
</p></abstract><kwd-group><kwd>Underground Pipeline</kwd><kwd> Seismo-Dynamics</kwd><kwd> Boundary Conditions</kwd><kwd> Seismic Effect</kwd><kwd> “Pipeline-Soil” System Interaction</kwd><kwd> Finite Difference Method</kwd></kwd-group></article-meta></front><body><sec id="s1"><title>1. Introduction</title><p>Current state of computing resources allows considering more closely numerous factors and determining more reliably the actual stress-strain state of underground pipeline.</p><p>In this regard, republican and foreign works have been analyzed, in particular, proceedings of XIV (Beijing, 2008) and XV (Lisbon, 2012) World Conferences on Earthquake Engineering and International Conference on Design in Geotechnical Engineering (Tokyo, 2009), associated with the study of seismic systems of pipelines, such as underground gas-, water- and oil-pipelines, to improve developed theory by new data, to evaluate its effectiveness and to establish the level of this work [<xref ref-type="bibr" rid="scirp.56552-ref1">1</xref>] - [<xref ref-type="bibr" rid="scirp.56552-ref3">3</xref>] .</p><p>At present, industrial enterprises and life support systems play a crucial role in human life and in economic development of the country: for this reason, their structural safety under extreme conditions, such as strong earthquakes, should be provided, especially when a large number of toxic and combustible materials are transported by these facilities. After the earthquake event, accident rate in pipelines is often increasing. In underground structures, the failure of one part affects the performance of the whole system, while in ground structures it is local. Therefore, diversified study of seismic vulnerability assessment was carried out for a number of industrial facilities and life support systems, such as pipelines, underground storage tanks and reservoirs.</p><p>Modern cities are growing not only in breadth, in height, but also in depth, using underground space. Pipelines of hot and cold water supply, sewage system, electric, telephone cable lines, along with subway lines, garages, etc. all create a new environment, which differs from the traditional soil medium. All located under modern megalopolis is likely to be regarded as a soil medium with disturbed structure. The key problem is, on one hand, design feature of the structures, and on the other, evaluation of interaction nature in “structure-soil” system [<xref ref-type="bibr" rid="scirp.56552-ref4">4</xref>] .</p><p>Fundamental analysis of the effects of earthquakes on underground pipes has been conducted; main types of damage have been stated; the effect of impact depth, soil conditions, geometrical sizes, types of joining and the quality of construction on seismic stability of underground pipelines for various purposes has been revealed [<xref ref-type="bibr" rid="scirp.56552-ref5">5</xref>] - [<xref ref-type="bibr" rid="scirp.56552-ref7">7</xref>] .</p><p>Practical significance of the problem consists in the following. Many large metropolitan areas are located in seismically active areas. Therefore, the design of underground structures becomes more difficult. Analysis of many earthquakes all over the world shows that the majority of destructions of underground pipelines occur on the border and close to it [<xref ref-type="bibr" rid="scirp.56552-ref8">8</xref>] . In this paper the solution of the problem of underground pipeline is studied under seismic load of arbitrary direction with different boundary conditions.</p></sec><sec id="s2"><title>2. Statement of the Problem</title><p>To study combined longitudinal, transverse vibrations of underground structures such as pipelines under arbitrary direction of seismic load we will consider applied theory of bar oscillations. This paper investigates a seismo-dynamics of underground pipelines based on the theory of seismo-dynamics of underground structures, with mathematical model of bar theory discussed by Bekmirzaev D.A. and Rashidov T.R. for the case of bar points displacements under combined action of longitudinal and transversal forces [<xref ref-type="bibr" rid="scirp.56552-ref9">9</xref>] .</p><p>Based on the assumptions given in [<xref ref-type="bibr" rid="scirp.56552-ref9">9</xref>] , the pipeline is modeled in the form of a bar (<xref ref-type="fig" rid="fig1">Figure 1</xref>), α―is an angle of incidence of seismic wave, and displacements are selected as follows:</p><disp-formula id="scirp.56552-formula1625"><label>(1)</label><graphic position="anchor" xlink:href="http://html.scirp.org/file/6-2310412x5.png"  xlink:type="simple"/></disp-formula><p>where<inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x6.png" xlink:type="simple"/></inline-formula>―are displacements of the points of a pipeline, u―longitudinal displacements, v―transversal displacements,<inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x7.png" xlink:type="simple"/></inline-formula>―an angle of rotation of pipe section.</p><p>When δ―is a thickness, D<sub>H</sub>―external diameter, and l―a length of cylinder shell, then at relative dimensions, expressed through order values,</p><disp-formula id="scirp.56552-formula1626"><label>(2)</label><graphic position="anchor" xlink:href="http://html.scirp.org/file/6-2310412x8.png"  xlink:type="simple"/></disp-formula><p>the discussed structure may be referred to a category of long cylinder shells. Such shells, independent on form and geometrical sizes of the profile, may be called thin-walled bars [<xref ref-type="bibr" rid="scirp.56552-ref10">10</xref>] . The pipeline under discussion always meets the condition (2).</p><fig id="fig1"  position="float"><label><xref ref-type="fig" rid="fig1">Figure 1</xref></label><caption><title> Scheme of underground pipeline under arbitrary directed seismic effect on horizontal plane</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/6-2310412x9.png"/></fig><p>Assume that pipeline is strained elastically; so Hooke’s law is considered for pipe material:</p><disp-formula id="scirp.56552-formula1627"><label>(3)</label><graphic position="anchor" xlink:href="http://html.scirp.org/file/6-2310412x10.png"  xlink:type="simple"/></disp-formula><p>To derive differential equations with boundary and initial conditions we will use Hamilton-Ostrogradskiy variation principle:</p><disp-formula id="scirp.56552-formula1628"><label>(4)</label><graphic position="anchor" xlink:href="http://html.scirp.org/file/6-2310412x11.png"  xlink:type="simple"/></disp-formula><p>where Т―is kinetic, П―potential energy, А―work of external forces, t―time. On the basis of Hamilton-Ostro- gradskiy variation principle (4), considering relationships (1) and (3) the following system of differential equations is derived:</p><disp-formula id="scirp.56552-formula1629"><label>(5)</label><graphic position="anchor" xlink:href="http://html.scirp.org/file/6-2310412x12.png"  xlink:type="simple"/></disp-formula><p>natural boundary conditions</p><disp-formula id="scirp.56552-formula1630"><label>(6)</label><graphic position="anchor" xlink:href="http://html.scirp.org/file/6-2310412x13.png"  xlink:type="simple"/></disp-formula><p>and initial conditions</p><disp-formula id="scirp.56552-formula1631"><label>(7)</label><graphic position="anchor" xlink:href="http://html.scirp.org/file/6-2310412x14.png"  xlink:type="simple"/></disp-formula><p>where<inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x15.png" xlink:type="simple"/></inline-formula>―is a density of pipeline material, F―an area of its cross section, E―modulus of elasticity of pipeline material, G―modulus of elasticity under shear,<inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x16.png" xlink:type="simple"/></inline-formula>―inertia moment of cross-section,<inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x17.png" xlink:type="simple"/></inline-formula>―pipeline coordinates <inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x18.png" xlink:type="simple"/></inline-formula> [<xref ref-type="bibr" rid="scirp.56552-ref6">6</xref>] .</p><disp-formula id="scirp.56552-formula1632"><label>(8)</label><graphic position="anchor" xlink:href="http://html.scirp.org/file/6-2310412x19.png"  xlink:type="simple"/></disp-formula><p>where<inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x20.png" xlink:type="simple"/></inline-formula>―is Poisson ratio of soil,<inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x20.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x21.png" xlink:type="simple"/></inline-formula>―coefficient of uniform shear of the pipeline in soil, l―a length,<inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x20.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x21.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x22.png" xlink:type="simple"/></inline-formula>―external pipe size,<inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x20.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x21.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x22.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x23.png" xlink:type="simple"/></inline-formula>―internal pipe size,<inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x20.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x21.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x22.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x23.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x24.png" xlink:type="simple"/></inline-formula>―external radius of a pipe, <inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x20.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x21.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x22.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x23.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x24.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x25.png" xlink:type="simple"/></inline-formula>and<inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x20.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x21.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x22.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x23.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x24.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x25.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x26.png" xlink:type="simple"/></inline-formula>―projections on coordinate axes of the law of soil movement,<inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x20.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x21.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x22.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x23.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x24.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x25.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x26.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x27.png" xlink:type="simple"/></inline-formula>―coefficients which depend on soil conditions,<inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x20.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x21.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x22.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x23.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x24.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x25.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x26.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x27.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x28.png" xlink:type="simple"/></inline-formula>―ver- tical soil pressure per linear length of a pipe, B―trench width at trench laying of the pipeline [<xref ref-type="bibr" rid="scirp.56552-ref11">11</xref>] .</p><p>Intensity of normal and tangential stresses</p><disp-formula id="scirp.56552-formula1633"><label>(9)</label><graphic position="anchor" xlink:href="http://html.scirp.org/file/6-2310412x29.png"  xlink:type="simple"/></disp-formula><disp-formula id="scirp.56552-formula1634"><label>(10)</label><graphic position="anchor" xlink:href="http://html.scirp.org/file/6-2310412x30.png"  xlink:type="simple"/></disp-formula><p>except intensity of tangential stresses<inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x31.png" xlink:type="simple"/></inline-formula>, often implies the concept of intensity of normal stresses <inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x31.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x32.png" xlink:type="simple"/></inline-formula> [<xref ref-type="bibr" rid="scirp.56552-ref12">12</xref>] .</p><p>From natural boundary conditions (6) we may obtain their different combinations. The system of Equations (5) with boundary (6) and initial conditions (7) is solved by finite difference method of the second order of accuracy. Based on computer algorithm, a program for problem-oriented Borland Delphi 7 language was developed and numerical results were obtained.</p></sec><sec id="s3"><title>3. Analysis of the Results of Numerical Studies</title><p>The algorithm and design program for underground pipelines in case of incidence of seismic wave at an angle to the pipe axis have been worked out; this corresponds to arbitrary seismic loading in the form of accelerograms or seismograms. As an example we will consider the following problems:</p><p>Problem. Consider a steel underground pipeline. Stated problem is solved on the basis of computer implementation of the algorithm. The mechanical and geometrical parameters of underground pipeline and soil are selected as follows:</p><p>Modulus of elasticity<inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x33.png" xlink:type="simple"/></inline-formula>, density<inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x33.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x34.png" xlink:type="simple"/></inline-formula>, external and internal diameter</p><p><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x35.png" xlink:type="simple"/></inline-formula>, <inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x35.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x36.png" xlink:type="simple"/></inline-formula>, area of cross-section<inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x35.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x36.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x37.png" xlink:type="simple"/></inline-formula>, pipeline length<inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x35.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x36.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x37.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x38.png" xlink:type="simple"/></inline-formula>, moment of inertia<inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x35.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x36.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x37.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x38.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x39.png" xlink:type="simple"/></inline-formula>, coefficient of uniform shear of the pipeline in soil<inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x35.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x36.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x37.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x38.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x39.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x40.png" xlink:type="simple"/></inline-formula>, projection of seismic load on coordinate axes<inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x35.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x36.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x37.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x38.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x39.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x40.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x41.png" xlink:type="simple"/></inline-formula>, <inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x35.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x36.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x37.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x38.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x39.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x40.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x41.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x42.png" xlink:type="simple"/></inline-formula>, amplitude of vibrations<inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x35.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x36.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x37.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x38.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x39.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x40.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x41.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x42.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x43.png" xlink:type="simple"/></inline-formula>, frequency of vibrations<inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x35.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x36.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x37.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x38.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x39.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x40.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x41.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x42.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x43.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x44.png" xlink:type="simple"/></inline-formula>, period of vibrations of the pipeline<inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x35.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x36.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x37.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x38.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x39.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x40.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x41.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x42.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x43.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x44.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x45.png" xlink:type="simple"/></inline-formula>, Poisson’s</p><p>ratio of soil<inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x46.png" xlink:type="simple"/></inline-formula>, Poisson’s ratio of a pipe<inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x46.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x47.png" xlink:type="simple"/></inline-formula>.</p><p>From the nature of an earthquake it is known that it has a complex character and effects on the structure and underground pipelines in arbitrary direction. Such effects of seismic loads on underground pipes complicate an assessment of stress-strain state of underground structures.</p><p>In this problem underground pipeline under seismic load works on tension, compression and bending. In the process of vibration of underground pipeline phases of displacements and stresses are changing. Results of problem solution are given in the form of graphs.</p><p>Vibration time is chosen in such a way that under all three boundary conditions the pipeline is either in tensile state <xref ref-type="fig" rid="fig2">Figure 2</xref>(a) or in compressed one―<xref ref-type="fig" rid="fig2">Figure 2</xref>(b) at α = 0, and normal stress at a given time along the length of a pipeline is changing as in <xref ref-type="fig" rid="fig2">Figure 2</xref>(c) in tensile state and <xref ref-type="fig" rid="fig2">Figure 2</xref>(d)―in compressed one at α = 0.</p><fig-group id="fig2"><label><xref ref-type="fig" rid="fig2">Figure 2</xref></label><caption><title> Changes of longitudinal displacement and normal stress along the axis of the pipeline at given time: 1) both ends of the pipeline are jammed, 2) the left end of the pipeline is jammed, the right one is free, 3) both ends are elastically fixed.</title></caption><fig id ="fig2_1"><label> (b)</label><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/6-2310412x48.png"/></fig><fig id ="fig2_2"><label>(c)</label><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/6-2310412x49.png"/></fig></fig-group><p>The effect of seismic load along the axis of underground pipeline under different boundary conditions and different times of changes of longitudinal displacement and normal stress along pipeline axis are shown in <xref ref-type="fig" rid="fig2">Figure 2</xref> (α = 0). Time is chosen so that the pipeline is in tensile or compressed state.</p><p>Three boundary conditions are examined:</p><p>1. Both ends of the pipeline are jammed,</p><disp-formula id="scirp.56552-formula1635"><graphic  xlink:href="http://html.scirp.org/file/6-2310412x50.png"  xlink:type="simple"/></disp-formula><p>2. The left end is jammed, the right one is free,</p><disp-formula id="scirp.56552-formula1636"><graphic  xlink:href="http://html.scirp.org/file/6-2310412x51.png"  xlink:type="simple"/></disp-formula><p>3. Both ends of the pipeline are elastically fixed,</p><disp-formula id="scirp.56552-formula1637"><graphic  xlink:href="http://html.scirp.org/file/6-2310412x52.png"  xlink:type="simple"/></disp-formula><p>where<inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x53.png" xlink:type="simple"/></inline-formula>, <inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x53.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x54.png" xlink:type="simple"/></inline-formula>,<inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x53.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x54.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x55.png" xlink:type="simple"/></inline-formula>―are rigidity coefficients of joints under corresponding loading (longitudinal forces, bending moment, transversal forces).</p><p>Analysis of results in <xref ref-type="fig" rid="fig2">Figure 2</xref> shows that maximum values of longitudinal displacement at boundary conditions 1 and 3 are within the span of the pipeline, and boundary conditions 2―at free end of the pipeline. Longitudinal stress has its maximum value at jammed ends or elastically fixed ends of the pipeline. It should be noted that the value of normal stress at jammed end of the pipeline is greater than the one at elastically fixed end of the pipeline (see <xref ref-type="fig" rid="fig2">Figure 2</xref>).</p><p>The changes of transversal displacement and tangential stress under seismic loads transversal to the axis of the pipeline at different boundary conditions and at different times are shown in <xref ref-type="fig" rid="fig3">Figure 3</xref>.</p><fig-group id="fig3"><label><xref ref-type="fig" rid="fig3">Figure 3</xref></label><caption><title> Changes of transversal displacement and tangential stress along the axis of the pipeline at given time: 1) both ends of the pipeline are jammed, 2) the left end of the pipeline is jammed, the right one is free, 3) both ends are elastically fixed.</title></caption><fig id ="fig3_1"><label> (b)</label><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/6-2310412x56.png"/></fig><fig id ="fig3_2"><label>(c)</label><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/6-2310412x57.png"/></fig></fig-group><p>Here, as in <xref ref-type="fig" rid="fig2">Figure 2</xref>, transverse displacement reaches its maximum value at boundary conditions 1 and 3 in pipeline range, and at boundary conditions 2-at the free end of the pipeline (<xref ref-type="fig" rid="fig3">Figure 3</xref>). Shear stress has its maximum values at jammed and elastically fixed ends of the pipeline (<xref ref-type="fig" rid="fig3">Figure 3</xref>). This corresponds to a change in the value of normal stress (<xref ref-type="fig" rid="fig2">Figure 2</xref>).</p><p>At each boundary condition the time is chosen so that transverse displacement has either positive value <xref ref-type="fig" rid="fig3">Figure 3</xref>(a) or negative one―<xref ref-type="fig" rid="fig3">Figure 3</xref>(b) at α = 90, and tangential stress at a given time along the length of the pipeline is changing as in <xref ref-type="fig" rid="fig3">Figure 3</xref>(c) in tensile state and <xref ref-type="fig" rid="fig3">Figure 3</xref>(d)―in compressed one at α = 90.</p><p>The law of soil motion is considered in the form<inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x58.png" xlink:type="simple"/></inline-formula>. Then the projections on coordinate axes x and y have the form:<inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x58.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x59.png" xlink:type="simple"/></inline-formula>, <inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x58.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x59.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x60.png" xlink:type="simple"/></inline-formula>,<inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x58.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x59.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x60.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/6-2310412x61.png" xlink:type="simple"/></inline-formula>. Equation system (4) with stated</p><p>boundary conditions and at the change of incidence angle of seismic load on pipeline axis is solved with these data.</p><p><xref ref-type="fig" rid="fig4">Figure 4</xref> shows the changes of maximum values of longitudinal and transversal displacements, and normal and tangential stresses when the direction of the effect of seismic loads is changing. If consider the figures with increasing angle of seismic load effect, maximum values of transversal displacements and tangential stresses are also increasing (<xref ref-type="fig" rid="fig4">Figure 4</xref>(b) and <xref ref-type="fig" rid="fig4">Figure 4</xref>(d)). When an angle of the effect of seismic load is increasing, the values of maximal longitudinal displacement and normal stress are decreasing (<xref ref-type="fig" rid="fig4">Figure 4</xref>(a) and <xref ref-type="fig" rid="fig4">Figure 4</xref>(c)).</p><p>To determine strength characteristics of the pipeline it is necessary to determine the intensity of normal and tangential stresses. This operation is performed by formulas (9) and (10).</p><p>The results are shown in <xref ref-type="fig" rid="fig5">Figure 5</xref>. Here it should be noted that, in general with increasing angle of incidence of seismic load, intensity values of normal and tangential stresses are also increasing (<xref ref-type="fig" rid="fig5">Figure 5</xref>). It should be also noted that elastically fixed pipelines (relative to other boundary conditions (1, 2)) have lower intensity values of normal and tangential stresses (<xref ref-type="fig" rid="fig5">Figure 5</xref>).</p></sec><sec id="s4"><title>4. Conclusions</title><p>An algorithm for solution of obtained equations and the design program are worked out. The solution is built on the</p><fig-group id="fig4"><label><xref ref-type="fig" rid="fig4">Figure 4</xref></label><caption><title> Change of longitudinal and transversal displacements and normal and tangential stresses at alteration of incidence angle of seismic loads: 1) both ends of the pipeline are jammed, 2) the left end of the pipeline is jammed, the right one is free, 3) both ends are elastically fixed.</title></caption><fig id ="fig4_1"><label> (b)</label><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/6-2310412x62.png"/></fig><fig id ="fig4_2"><label>(c)</label><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/6-2310412x63.png"/></fig><fig id ="fig4_3"><label> (d)</label><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/6-2310412x64.png"/></fig><fig id ="fig4_4"><label></label><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/6-2310412x65.png"/></fig></fig-group><fig-group id="fig5"><label><xref ref-type="fig" rid="fig5">Figure 5</xref></label><caption><title> Changes of intensity of normal and tangential stresses at alteration of incidence angle of seismic load: 1) both ends of the pipeline are jammed, 2) the left end of the pipeline is jammed, the right one is free, 3) both ends are elastically fixed.</title></caption><fig id ="fig5_1"><label> (b)</label><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/6-2310412x66.png"/></fig><fig id ="fig5_2"><label></label><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/6-2310412x67.png"/></fig></fig-group><p>basis of finite difference method; that allows simultaneously specifying the initial and boundary conditions, soil response and the decision itself. The results are obtained under different boundary conditions. From analysis of the results, it is evident that stress-strain state of the pipeline with elastically fixed ends is lower than with other combination of boundary conditions. It can be concluded that in design of underground pipeline, joining parts must be close to elastically fixed conditions. Thus stress-strain state of the pipeline decreases by 20% - 40% relative to the rigidly fixed boundary conditions. Maximal normal stresses occur under longitudinal seismic loading, and tangential stress reaches its maximum value at transversal seismic loading of the pipeline.</p><p>Results of the intensity of normal and tangential stresses of the pipeline are given. This makes it possible to evaluate strength characteristics of underground pipelines during strong earthquakes in seismically active areas. Presented methods and software tools provide a comprehensive analysis of the strength of underground pipeline under seismic actions and implement a systematic approach to determining the effects of the earthquake on stress-strain state of the pipeline and to planning engineering measures to ensure safe and reliable operation of underground pipeline in zones of high seismic risk. Developed algorithms and design programs allow us to consider pipeline vibrations under different types of loading, types of ends fixing and soil parameters. All these procedures allow us to determine actual loading and displacements occurring in sections of the pipeline under different seismic loadings. This makes it possible to improve regulatory documents on earthquake-resistant engineering of underground networks of supply pipelines [<xref ref-type="bibr" rid="scirp.56552-ref11">11</xref>] and to develop universal applied programs of design and construction.</p></sec><sec id="s5"><title>Cite this paper</title><p>Diyorbek Bekmirzaev, (2015) Design of Underground Pipelines under Arbitrary Seismic Loading. Open Journal of Applied Sciences,05,226-232. doi: 10.4236/ojapps.2015.55023</p></sec></body><back><ref-list><title>References</title><ref id="scirp.56552-ref1"><label>1</label><mixed-citation publication-type="other" xlink:type="simple">The 14th World Conference on Earthquake Engineering, Beijing (2008).</mixed-citation></ref><ref id="scirp.56552-ref2"><label>2</label><mixed-citation publication-type="other" xlink:type="simple">The 15th World Conference on Earthquake Engineering, Lisbon (2012).</mixed-citation></ref><ref id="scirp.56552-ref3"><label>3</label><mixed-citation publication-type="other" xlink:type="simple">Proceeding of International Conference on Performance-Based Design in Earthquake Geotechnical Engineering, Tokyo (2009).</mixed-citation></ref><ref id="scirp.56552-ref4"><label>4</label><mixed-citation publication-type="other" xlink:type="simple">Rashidov, T.R. and An, E.V. (2013) Seismo-Dynamics of Structures, Interacting with Soil. Uzbek Journal “Problems of Mechanics”, 3-4, 40-45.</mixed-citation></ref><ref id="scirp.56552-ref5"><label>5</label><mixed-citation publication-type="other" xlink:type="simple">Rashidov, T.R. (1973) Dynamic Theory of Seismic Stability of Complex Systems of Underground Structures. FAN, Tashkent, 180 p.</mixed-citation></ref><ref id="scirp.56552-ref6"><label>6</label><mixed-citation publication-type="other" xlink:type="simple">Rashidov, T.R. and Khojmetov, G.Kh. (1985) Seismic Stability of Underground Pipelines. FAN, Tashkent, 153 p.</mixed-citation></ref><ref id="scirp.56552-ref7"><label>7</label><mixed-citation publication-type="other" xlink:type="simple">Tashkent Earthquake on 26th of April, 1966 (1971) FAN, Tashkent, 672 p.</mixed-citation></ref><ref id="scirp.56552-ref8"><label>8</label><mixed-citation publication-type="other" xlink:type="simple">Ghekhman, A.S. and Zainetdinov, Kh. (1988) Design, Construction and Operation of Pipelines in Seismic Regions. Stroyizdat, Moscow, 184 p.</mixed-citation></ref><ref id="scirp.56552-ref9"><label>9</label><mixed-citation publication-type="other" xlink:type="simple">Bekmirzaev, D.A. and Rashidov, T.R. (2014) Solution of the Problem of Seismo-Dynamics of Underground Pipelines under Loading of Arbitrary Direction. Uzbek Journal “Problems of Mechanics”, 3-4, 8-13.</mixed-citation></ref><ref id="scirp.56552-ref10"><label>10</label><mixed-citation publication-type="other" xlink:type="simple">Vlasov, V.Z. (1963) Selected Works. Volume II. USSR Academy of Sciences, Moscow, 508 p.</mixed-citation></ref><ref id="scirp.56552-ref11"><label>11</label><mixed-citation publication-type="other" xlink:type="simple">Building Code (1996) Engineering in Seismic Regions. КМК 2.01.03-96, Tashkent, 88 p.</mixed-citation></ref><ref id="scirp.56552-ref12"><label>12</label><mixed-citation publication-type="other" xlink:type="simple">Aleksandrov, А.V. and Potapov, V.D. (1990) Bases of the Theory of Elasticity and Plasticity: Text-Book for Engineering Colleges. High School, Moscow, 400 p.</mixed-citation></ref></ref-list></back></article>