<?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">IJG</journal-id><journal-title-group><journal-title>International Journal of Geosciences</journal-title></journal-title-group><issn pub-type="epub">2156-8359</issn><publisher><publisher-name>Scientific Research Publishing</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.4236/ijg.2015.612104</article-id><article-id pub-id-type="publisher-id">IJG-62322</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>
 
 
  The Influence of Climate Factors on the Stability of Infrastructures: Case of Forest Ecosystem in Southern Cameroon
 
</article-title></title-group><contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>hilemon</surname><given-names>Zo’o Zame</given-names></name><xref ref-type="aff" rid="aff1"><sup>1</sup></xref></contrib><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Philippe</surname><given-names>Samba Assomo</given-names></name><xref ref-type="aff" rid="aff1"><sup>1</sup></xref><xref ref-type="corresp" rid="cor1"><sup>*</sup></xref></contrib></contrib-group><aff id="aff1"><addr-line>University of Yaounde I, Yaoundé, Cameroon</addr-line></aff><author-notes><corresp id="cor1">* E-mail:<email>sambafilipe@yahoo.fr(PSA)</email>;</corresp></author-notes><pub-date pub-type="epub"><day>16</day><month>12</month><year>2015</year></pub-date><volume>06</volume><issue>12</issue><fpage>1317</fpage><lpage>1322</lpage><history><date date-type="received"><day>30</day>	<month>October</month>	<year>2015</year></date><date date-type="rev-recd"><day>accepted</day>	<month>26</month>	<year>December</year>	</date><date date-type="accepted"><day>29</day>	<month>December</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>
 
 
  The southern forest ecosystem of Cameroon extends from latitude 2
  &#176; to 6
  &#176;N and from 10
  &#176; to 16
  &#176;E. In order to investigate about the influence of climate factors on the infrastructures, the main parameters of local climate of that ecosystem have been evaluated. The results show that, the factors are stable and have a common trend. But, the abundance of precipitations; the important hydrographic network and the presence of dense forest appear as the majors climatic constraints that may be taken in account to ensure the stability of the infrastructures in forest ecosystem.
 
</p></abstract><kwd-group><kwd>Forest Ecosystem</kwd><kwd> Climate Factors</kwd><kwd> Stability</kwd><kwd> Infrastructures</kwd><kwd> Cameroon</kwd></kwd-group></article-meta></front><body><sec id="s1"><title>1. Introduction</title><p>The construction of various infrastructures (roads, buildings, bridges…) are based on technical specifications notably geotechnical parameters and the traffic in road domain. In order to know the cause of the rapid destruction of these infrastructures, it appears necessary to inquiry about the role played by the climate factors on the stability of the infrastructures. The purpose of this paper is to identify the impact of climate factors, on the stability of infrastructures independently, for the good consideration of technical guidance. The forest ecosystem in southern Cameroon is taken as an experimentation site.</p></sec><sec id="s2"><title>2. Situation and Presentation of the Field Studied</title><p>The field studied extends from latitude 2˚ to 6˚N and from 10˚ to 16˚E (<xref ref-type="fig" rid="fig1">Figure 1</xref>). This area is covered by the</p><fig id="fig1"  position="float"><label><xref ref-type="fig" rid="fig1">Figure 1</xref></label><caption><title> Location of studied field</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/5-2801152x7.png"/></fig><p>forest ecosystem and includes three regions: East (Bertoua), Center (Yaound&#233;) and South (Kribi). The coordinates of the localities in with different data have been collected are as follow: Yaound&#233;: LatLng (3.86136, 11.52077); Kribi: LatLng (2.93721, 9.91705) and Batouri: (4.43302, 14.36359). The works of Olivry, 1986 [<xref ref-type="bibr" rid="scirp.62322-ref1">1</xref>] cited by Kamgang Kabeyene, 1987 [<xref ref-type="bibr" rid="scirp.62322-ref2">2</xref>] and Bineli, 2009 [<xref ref-type="bibr" rid="scirp.62322-ref3">3</xref>] show that the area is the domain of equatorial climate that can be divided in three subtypes. In Yaound&#233; there is an equatorial climate with four seasons; in Kribi, the coastal equatorial climate with four seasons and increased humidity; in Batouri, transition tropical and equatorial climate.</p><p>According to many environmental assessments, the forest ecosystem has an important fauna and flora. The climate is characterized by:</p><p>・ presence of dense forest with big and tall trees;</p><p>・ abundance of precipitation;</p><p>・ important and constancy temperature around 25˚C;</p><p>・ important soil coat come from the weathering of original rocks.</p></sec><sec id="s3"><title>3. Methodology</title><p>The methodology of this work is based on the exploitation of many reports of environmental assessment notably the studies of social and economic impact in the construction of the infrastructures that the Ministry of Publics Works is the promoter: “le Competing”, 2011 [<xref ref-type="bibr" rid="scirp.62322-ref4">4</xref>] ; FHEC, 2013 [<xref ref-type="bibr" rid="scirp.62322-ref5">5</xref>] . The use of schematic maps was important to know about pedology and vegetation covers. To determine the climate factors as temperature and average of precipitation, the data was collected into the raining stations of the three localities chosen. The drawing up of specific diagrams permits to identify the four seasons of equatorial climate. The National Laboratory of Civil Engineering of Cameroon and the laboratory of geotechnic of the University of Yaound&#233; I allow us to obtain geotechnical parameters of several authors: Ekodeck, 1984 [<xref ref-type="bibr" rid="scirp.62322-ref6">6</xref>] ; Bitom, 1998 [<xref ref-type="bibr" rid="scirp.62322-ref7">7</xref>] ; Samba, 2008 [<xref ref-type="bibr" rid="scirp.62322-ref8">8</xref>] ; Onana, 2010 [<xref ref-type="bibr" rid="scirp.62322-ref9">9</xref>] ; Zo’o Zame, 2012 [<xref ref-type="bibr" rid="scirp.62322-ref10">10</xref>] ; Ntouala, 2013 [<xref ref-type="bibr" rid="scirp.62322-ref11">11</xref>] .</p></sec><sec id="s4"><title>4. Presentation and Interpretation of Results</title><sec id="s4_1"><title>4.1. Presentation of Results</title><sec id="s4_1_1"><title>4.1.1. Climate Factors</title><p>The components determined concerning the average temperature, the annual average precipitation, hydrographic network, vegetation, soil and the seasons (<xref ref-type="table" rid="table1">Table 1</xref>).</p><p>From the data of raining station of Yaound&#233; (<xref ref-type="table" rid="table2">Table 2</xref>), the Bagnouls and Gaussen, 1996 [<xref ref-type="bibr" rid="scirp.62322-ref12">12</xref>] diagram was built (<xref ref-type="fig" rid="fig2">Figure 2</xref>). This diagram shows in general the period of the different seasons in the forest ecosystem.</p><table-wrap id="table1" ><label><xref ref-type="table" rid="table1">Table 1</xref></label><caption><title> Development of different climate factors in three sites of the ecosystem</title></caption><table><tbody><thead><tr><th align="center" valign="middle" ></th><th align="center" valign="middle" >Precipitation</th><th align="center" valign="middle" >Temperature</th><th align="center" valign="middle" >Hydrography</th><th align="center" valign="middle" >Vegetation</th><th align="center" valign="middle" >Soil</th><th align="center" valign="middle" >Season</th></tr></thead><tr><td align="center" valign="middle" >Batouri</td><td align="center" valign="middle" >1200 to 1600 mm/an</td><td align="center" valign="middle" >24˚C</td><td align="center" valign="middle" >Important network</td><td align="center" valign="middle" >Savanna and forest</td><td align="center" valign="middle" >Ferralitic</td><td align="center" valign="middle" >04 seasons</td></tr><tr><td align="center" valign="middle" >Yaound&#233;</td><td align="center" valign="middle" >1200 to 2000 mm/an</td><td align="center" valign="middle" >24˚C</td><td align="center" valign="middle" >Important network</td><td align="center" valign="middle" >forest</td><td align="center" valign="middle" >Ferralitic</td><td align="center" valign="middle" >04 seasons</td></tr><tr><td align="center" valign="middle" >Kribi</td><td align="center" valign="middle" >2500 to 4000 mm/an</td><td align="center" valign="middle" >22˚C - 29˚C</td><td align="center" valign="middle" >Important network</td><td align="center" valign="middle" >forest</td><td align="center" valign="middle" >Ferralitic</td><td align="center" valign="middle" >04 seasons</td></tr></tbody></table></table-wrap><table-wrap id="table2" ><label><xref ref-type="table" rid="table2">Table 2</xref></label><caption><title> Raining parameters in the station of Yaounde from 1994 to 2014</title></caption><table><tbody><thead><tr><th align="center" valign="middle" >Months</th><th align="center" valign="middle" >Jan</th><th align="center" valign="middle" >Feb</th><th align="center" valign="middle" >Mar</th><th align="center" valign="middle" >Apr</th><th align="center" valign="middle" >May</th><th align="center" valign="middle" >Jun</th><th align="center" valign="middle" >Jul</th><th align="center" valign="middle" >Aug</th><th align="center" valign="middle" >Sept</th><th align="center" valign="middle" >Oct</th><th align="center" valign="middle" >Nov</th><th align="center" valign="middle" >Dec</th><th align="center" valign="middle" >Total</th></tr></thead><tr><td align="center" valign="middle" >Precipitation (mm)</td><td align="center" valign="middle" >24.3</td><td align="center" valign="middle" >49.0</td><td align="center" valign="middle" >98.4</td><td align="center" valign="middle" >157.0</td><td align="center" valign="middle" >82.1</td><td align="center" valign="middle" >129.9</td><td align="center" valign="middle" >51.9</td><td align="center" valign="middle" >78.1</td><td align="center" valign="middle" >224.9</td><td align="center" valign="middle" >259</td><td align="center" valign="middle" >103.1</td><td align="center" valign="middle" >31.2</td><td align="center" valign="middle" >1288.9</td></tr><tr><td align="center" valign="middle" >Temperature (˚C)</td><td align="center" valign="middle" >24.2</td><td align="center" valign="middle" >25.4</td><td align="center" valign="middle" >25.2</td><td align="center" valign="middle" >24.8</td><td align="center" valign="middle" >24.6</td><td align="center" valign="middle" >23.9</td><td align="center" valign="middle" >23.2</td><td align="center" valign="middle" >23.3</td><td align="center" valign="middle" >23.7</td><td align="center" valign="middle" >23.7</td><td align="center" valign="middle" >23.4</td><td align="center" valign="middle" >24.4</td><td align="center" valign="middle" >24.15</td></tr></tbody></table></table-wrap><fig-group id="fig2"><label><xref ref-type="fig" rid="fig2">Figure 2</xref></label><caption><title> Ombrothermic diagram of Bagnouls and Gaussen applied to Yaound&#233; region.</title></caption><fig id ="fig2_1"><label></label><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/5-2801152x8.png"/></fig><fig id ="fig2_2"><label></label><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/5-2801152x9.png"/></fig></fig-group><p>Another important component of climate is the soil. The ferralitic soil of forest ecosystem in equatorial climate has been described by Yongue, 1994 [<xref ref-type="bibr" rid="scirp.62322-ref13">13</xref>] Bekoa, 1994 [<xref ref-type="bibr" rid="scirp.62322-ref14">14</xref>] and 1998, [<xref ref-type="bibr" rid="scirp.62322-ref7">7</xref>] . According to the above authors, the ferralitic soil is acidic. It contains an important pedological cover due to weathering of original rocks of geological substratum. This profile shows three levels upwards (<xref ref-type="fig" rid="fig3">Figure 3</xref>):</p><p>- The inferior level that is characterized by the beginning of the fragmentation of original rocks. This frag- ments are called “alt&#233;rites”;</p><p>- The median level that contains various elements with different size come from broken rocks;</p><p>- The superior level rich in clay and organic matter.</p><p>Also, it is necessary to note that, apart from the general organization of the ferralitic soil, near the sea or important river the soil becomes hydromorphic rich in alluvium with poor mechanic properties.</p><p>According to the important hydrographic network announced above, the case of one locality of Yaound&#233; (Akonolinga) is follow represented (<xref ref-type="fig" rid="fig4">Figure 4</xref>).</p></sec><sec id="s4_1_2"><title>4.1.2. Geotechnical Parameters</title><p>The geotechnical parameters of the sites are constant due to the common organization of the soil through the forest ecosystem. The parameters that have been chosen are volumic weight (γ), porosity (n), Californian Bearing Ratio (CBR), apparent cohesion (Cu) and internal friction angle (φu). The <xref ref-type="table" rid="table3">Table 3</xref> gives the average of these parameters.</p></sec></sec><sec id="s4_2"><title>4.2. Interpretation of Results</title><p>The results obtained are stable not only in climate factors but also in geotechnical parameters. In the first approach, these results may allow the sustainability of infrastructures in southern forest ecosystem in case of civism of population and suitable technical management of works. But it is important to underscore the negative effect that play the combination of three climate factors on the stability of infrastructures in southern ecosystem notably the abundance of precipitation, the important hydrographic network and the dense forest.</p><fig id="fig3"  position="float"><label><xref ref-type="fig" rid="fig3">Figure 3</xref></label><caption><title> Pedological profile of ferralitic soil</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/5-2801152x10.png"/></fig><fig id="fig4"  position="float"><label><xref ref-type="fig" rid="fig4">Figure 4</xref></label><caption><title> Hydrographic network in one locality of Yaound&#233;: Akonolinga</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/5-2801152x11.png"/></fig><table-wrap id="table3" ><label><xref ref-type="table" rid="table3">Table 3</xref></label><caption><title> Geotechnical parameters</title></caption><table><tbody><thead><tr><th align="center" valign="middle" ></th><th align="center" valign="middle" >γ (gf/cm<sup>3</sup>)</th><th align="center" valign="middle" >N (%)</th><th align="center" valign="middle" >CBR (%)</th><th align="center" valign="middle" >Cu (bars)</th><th align="center" valign="middle" >Φu (˚)</th></tr></thead><tr><td align="center" valign="middle" >Superior level</td><td align="center" valign="middle" >2.6</td><td align="center" valign="middle" >55</td><td align="center" valign="middle" >13</td><td align="center" valign="middle" >0.00 - 1.06</td><td align="center" valign="middle" >12 - 52</td></tr><tr><td align="center" valign="middle" >Median level</td><td align="center" valign="middle" >2.8</td><td align="center" valign="middle" >39</td><td align="center" valign="middle" >59</td><td align="center" valign="middle" >0.15 - 1.00</td><td align="center" valign="middle" >31 - 63</td></tr><tr><td align="center" valign="middle" >Inferior level</td><td align="center" valign="middle" >2.6</td><td align="center" valign="middle" >23</td><td align="center" valign="middle" >27</td><td align="center" valign="middle" >0.06 - 2.8</td><td align="center" valign="middle" >16 - 50</td></tr></tbody></table></table-wrap><p>a) the abundance of precipitation and the important hydrographic network facilitate the infiltration of water in infrastructures bodies that creates the loss of resistance; the water overflowing which causes erosion and the obstruction of canalization;</p><p>b) the permanent presence of forest is responsible of the fragmentation of the infrastructures by the phenomena induce by roots growing.</p></sec></sec><sec id="s5"><title>5. Discussion</title><p>The interaction between climate and infrastructures was the great preoccupation of many researches in this last decade. But, among these studies, many of them were related to the climate change and had global signification. The report of USAID, 2014 [<xref ref-type="bibr" rid="scirp.62322-ref15">15</xref>] presented the impacts of climate stressors on building due to climate change; this study also underlined the place of climate variability because any building is typically designed for specific climate. Several others reports show that climate change alter current conditions as temperature, precipitation, sea level or bed river and standard events. The consequence is the damage of various infrastructures: transportation infrastructures, buildings, marine infrastructures, energy infrastructures and roads: IISD, 2013 [<xref ref-type="bibr" rid="scirp.62322-ref16">16</xref>] ; NCA, 2012 [<xref ref-type="bibr" rid="scirp.62322-ref17">17</xref>] . The case study of Southern Australia related to the impact of heat waves on infrastructures and communities conducted by the Queensland university of technology, 2010 [<xref ref-type="bibr" rid="scirp.62322-ref18">18</xref>] is in agreement with others works. The local impact of climate factors on the stability of infrastructures was introduced by Sarrazin et al., 2009 [<xref ref-type="bibr" rid="scirp.62322-ref19">19</xref>] . The results obtained in forest ecosystem in southern Cameroon have the common trend of those showed elsewhere. The peculiarity in southern Cameroon is that the climate factors are local, the study is punctual and the ecological parameters are integrated.</p></sec><sec id="s6"><title>6. Conclusion</title><p>The climate factors that induce negative effect on the stability of infrastructures in southern forest ecosystem of Cameroon are now known. There are the abundance of precipitation, an important hydrographic network and the existence of dense forest that cause the damage and the dysfunctioning of infrastructures. These negative impacts appeal to the strengthening of roadway or foundations and the reinforcement of canalization works. All over the world, the several others factors act negatively on the stability of infrastructures. So that, the attention of the authorities and any expert involved in the construction of infrastructures is called in order to take in account the different impacts linked to the climate factors in additional to the technical specification.</p></sec><sec id="s7"><title>Cite this paper</title><p>PhilemonZo’o Zame,PhilippeSamba Assomo, (2015) The Influence of Climate Factors on the Stability of Infrastructures: Case of Forest Ecosystem in Southern Cameroon. International Journal of Geosciences,06,1317-1322. doi: 10.4236/ijg.2015.612104</p></sec><sec id="s8"><title>NOTES</title></sec></body><back><ref-list><title>References</title><ref id="scirp.62322-ref1"><label>1</label><mixed-citation publication-type="other" xlink:type="simple">Olivry, J. (1986) Fleuves et Rivières du Cameroun. Collection Monographies Hydrologiques ORSTOM n°9, Paris, I Vol. 733 p.</mixed-citation></ref><ref id="scirp.62322-ref2"><label>2</label><mixed-citation publication-type="other" xlink:type="simple">Kamgang Beyala, V. (1987) Altération supergène des roches grenatifères de la région de Yaoundé (Cameroun): Pétrologie-Minéralogie. Th. Doct. 3ème Cycle, Université de Poitiers, Poitiers, 170 p.</mixed-citation></ref><ref id="scirp.62322-ref3"><label>3</label><mixed-citation publication-type="other" xlink:type="simple">Bineli, E. (2009) Impact de la variabilité climatique sur les ressources en eau du bassin du Nyong. Mém. DEA. FAC. Sc. 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