<?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">JEP</journal-id><journal-title-group><journal-title>Journal of Environmental Protection</journal-title></journal-title-group><issn pub-type="epub">2152-2197</issn><publisher><publisher-name>Scientific Research Publishing</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.4236/jep.2016.78101</article-id><article-id pub-id-type="publisher-id">JEP-69066</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>
 
 
  Effect of Fertilization on the Dynamics and Activity of Iron-Reducing Bacterial Populations in a West African Rice Paddy Soil Planted with Two Rice Varieties: Case Study of Kou Valley in Burkina Faso
 
</article-title></title-group><contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>C&amp;egrave;cile</surname><given-names>Harmonie Otoidobiga</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>Adama</surname><given-names>Sawadogo</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>Yapi</surname><given-names>Sinar&amp;egrave;</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>Ibrahima</surname><given-names>Ou&amp;egrave;draogo</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>Prosper</surname><given-names>Zombr&amp;egrave;</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>Susumu</surname><given-names>Asakawa</given-names></name><xref ref-type="aff" rid="aff4"><sup>4</sup></xref><xref ref-type="corresp" rid="cor1"><sup>*</sup></xref></contrib><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Alfred</surname><given-names>S. Traore</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>Day&amp;egrave;ri</surname><given-names>Dianou</given-names></name><xref ref-type="aff" rid="aff5"><sup>5</sup></xref><xref ref-type="corresp" rid="cor1"><sup>*</sup></xref></contrib></contrib-group><aff id="aff4"><addr-line>Soil Biology and Chemistry, Graduate School of Bio-Agricultural Sciences, Nagoya University, Chikusa, Nagoya, Japan</addr-line></aff><aff id="aff2"><addr-line>Institute of Environment and Agricultural Research, Bobo Dioulasso, Burkina Faso</addr-line></aff><aff id="aff1"><addr-line>Research Center for Biological, Alimentary and Nutritional Sciences, Research and Training Unit, Life and Earth Sciences, University of Ouagadougou, Ouagadougou, Burkina Faso</addr-line></aff><aff id="aff5"><addr-line>National Center for Sciences and Technology Research, Ouagadougou, Burkina Faso</addr-line></aff><aff id="aff3"><addr-line>Laboratory of Soil-Materials and Environment, Research and Training Unit, Life and Earth Sciences, University of Ouagadougou, Ouagadougou, Burkina Faso</addr-line></aff><author-notes><corresp id="cor1">* E-mail:<email>otoidobiga@univ-ouaga.bf(CHO)</email>;<email>otoidobiga@univ-ouaga.bf(AS)</email>;<email>otoidobiga@univ-ouaga.bf(YS)</email>;<email>otoidobiga@univ-ouaga.bf(IO)</email>;<email>otoidobiga@univ-ouaga.bf(PZ)</email>;<email>otoidobiga@univ-ouaga.bf(SA)</email>;<email>otoidobiga@univ-ouaga.bf(AST)</email>;<email>otoidobiga@univ-ouaga.bf(DD)</email>;</corresp></author-notes><pub-date pub-type="epub"><day>30</day><month>06</month><year>2016</year></pub-date><volume>07</volume><issue>08</issue><fpage>1119</fpage><lpage>1131</lpage><history><date date-type="received"><day>7</day>	<month>June</month>	<year>2016</year></date><date date-type="rev-recd"><day>accepted</day>	<month>22</month>	<year>July</year>	</date><date date-type="accepted"><day>26</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>
 
 
  Iron toxicity is a major stress to rice caused by a high concentration of reduced iron, in the soil in many lowlands worldwide. To reduce iron toxicity in the West African lowlands, an investigation was performed at the site of the University of Ouagadougou, in pots containing an iron toxic soil from the Kou Valley (West of Burkina Faso). The experiment objective was to study the effect of mineral fertilizer on Iron Reducing Bacteria (IRB) dynamics and activity during rice cultivation, iron accumulation in rice plant and rice biomass yield under iron toxicity conditions. BOUAKE-189 and ROK-5 rice varieties, sensitive and tolerant to iron toxicity, respectively, were used for the experiment. The pots were amended with chemical fertilizers (NPK + Urea and NPK + Urea + Ca + Mg + Zn complex). Control pots without fertilization were prepared similarly. The kinetics of IRB and ferrous iron content in soil near rice roots were monitored throughout the cultural cycle using MPN and colorimetric methods, respectively. The total iron content was evaluated in rice plant using spectrometric method. Data obtained were analyzed in relation to fertilization mode, rice growth stage and rice yield using the student’s t-test and XLSTAT 2014 statistical software. The experiment revealed that NPK + Urea and NPK + Urea + Ca + Mg + Zn fertilization, decreased significantly (p &lt; 0.0001) the number of IRB in the soil for BOUAKE-189 rice varieties. In most pots, highest IRB densities and ferrous iron content in soil were recorded from rice tillering and flowering to maturity stages, indicating that rice plants promoted microbial processes and iron reduction in soil. From the study, the NPK + Urea amendment decreased significantly ferrous iron content (p &lt; 0.0001) in soil near BOUAKE-189 and ROK-5 rice varieties roots relatively to control pots. However, NPK + Urea + Ca + Zn + Mg amendment increased significantly ferrous iron content (p &lt; 0.0001) in the soil near roots, Fe accumulation in plant biomass and rice yield for the two rice varieties. 
   
  
 
</p></abstract><kwd-group><kwd>Iron-Reducing Bacteria</kwd><kwd> Rice</kwd><kwd> Iron Toxicity</kwd><kwd> Fertilization</kwd></kwd-group></article-meta></front><body><sec id="s1"><title>1. Introduction</title><p>Iron is the fourth-most abundant element in the Earth’s crust and the most prevalent redox-active metal [<xref ref-type="bibr" rid="scirp.69066-ref1">1</xref>] [<xref ref-type="bibr" rid="scirp.69066-ref2">2</xref>] . Iron is a first row transition metal which mainly exists in one of the two readily inter-convertible redox states under physiological conditions: the reduced Fe<sup>2+</sup> ferrous form and the oxidised Fe<sup>3+</sup> ferric form. Iron can also adopt different spin states (high or low) in both the ferric and ferrous form, depending on its ligand [<xref ref-type="bibr" rid="scirp.69066-ref3">3</xref>] [<xref ref-type="bibr" rid="scirp.69066-ref4">4</xref>] . These properties permit to the iron to participate in many major biological processes, such as photosynthesis, N<sub>2</sub> fixation, methanogenesis, production and consumption of H<sub>2</sub>, respiration, the trichloroacetic acid (TCA) cycle, oxygen transport, gene regulation and the biosynthesis of DNA [<xref ref-type="bibr" rid="scirp.69066-ref5">5</xref>] - [<xref ref-type="bibr" rid="scirp.69066-ref7">7</xref>] . Iron is absolutely required for all forms of life; however, a large concentration of reduced iron (Fe<sup>2+</sup>) in the soil solution can cause high production of oxygen radicals which can damage cell structural components and impair physiological processes of plants [<xref ref-type="bibr" rid="scirp.69066-ref3">3</xref>] [<xref ref-type="bibr" rid="scirp.69066-ref8">8</xref>] [<xref ref-type="bibr" rid="scirp.69066-ref9">9</xref>] .</p><p>Rice (Oryza sativa L.) is cultivated on approximately 213.7 million hectares of irrigated and rained lowlands in the world [<xref ref-type="bibr" rid="scirp.69066-ref10">10</xref>] - [<xref ref-type="bibr" rid="scirp.69066-ref12">12</xref>] . Since the first report of its occurrence [<xref ref-type="bibr" rid="scirp.69066-ref13">13</xref>] , the iron toxicity for rice in lowland has been largely reported in several countries, especially in the humid tropical regions in Asia, South America and West and Central Africa [<xref ref-type="bibr" rid="scirp.69066-ref14">14</xref>] - [<xref ref-type="bibr" rid="scirp.69066-ref17">17</xref>] . By overlaying the soil map with the rice distribution map [<xref ref-type="bibr" rid="scirp.69066-ref12">12</xref>] , it is roughly estimated that 19% of the total rice area in Africa has a potential risk of Fe toxicity. Ch&#233;rif et al. [<xref ref-type="bibr" rid="scirp.69066-ref18">18</xref>] have reported that about 55% of the rice area is affected by iron toxicity in three West African countries (Guinea, Ivory Coast and Ghana), and about 10% of the area of rice cultivation is abandoned due to severe iron toxicity [<xref ref-type="bibr" rid="scirp.69066-ref19">19</xref>] [<xref ref-type="bibr" rid="scirp.69066-ref20">20</xref>] . In Burkina Faso, many lowland crop fields were even abandoned due to iron toxicity [<xref ref-type="bibr" rid="scirp.69066-ref21">21</xref>] . The Kou Valley is recognized as an excellent agricultural plain, because of its great hydraulic potential and the soils fertility [<xref ref-type="bibr" rid="scirp.69066-ref22">22</xref>] . With an area of 1200 hectares, the Kou valley belongs to the first irrigated perimeters (1960) of Burkina Faso [<xref ref-type="bibr" rid="scirp.69066-ref22">22</xref>] . However, in 1986, 300 ha of fields were abandoned, in Kou Valley because of ferrous intoxication [<xref ref-type="bibr" rid="scirp.69066-ref21">21</xref>] ; and most among these intoxicated fields remained uncultivated up to date [<xref ref-type="bibr" rid="scirp.69066-ref23">23</xref>] .</p><p>Iron toxicity is one of the most important edaphic constraints to rice production on acid soils [<xref ref-type="bibr" rid="scirp.69066-ref9">9</xref>] [<xref ref-type="bibr" rid="scirp.69066-ref24">24</xref>] . The iron toxicity conditions are most frequently reported from inland valley, swamps and coastal or tidal wetlands [<xref ref-type="bibr" rid="scirp.69066-ref25">25</xref>] . Many studies show that the occurrence of Fe toxicity is associated with a high concentration of Fe (II) in soil solution [<xref ref-type="bibr" rid="scirp.69066-ref11">11</xref>] [<xref ref-type="bibr" rid="scirp.69066-ref15">15</xref>] [<xref ref-type="bibr" rid="scirp.69066-ref26">26</xref>] . Thus, large concentrations of ferrous Fe in soil solution may occur either when Fe is mobilized in situ by microbial reduction of ferric iron [<xref ref-type="bibr" rid="scirp.69066-ref27">27</xref>] or when reduced Fe is translocated into valley bottoms by interflow or subsurface flow from adjacent slopes [<xref ref-type="bibr" rid="scirp.69066-ref19">19</xref>] [<xref ref-type="bibr" rid="scirp.69066-ref28">28</xref>] [<xref ref-type="bibr" rid="scirp.69066-ref29">29</xref>] .</p><p>The microbial reduction of iron is considered to be an ubiquitous and important redox process, in which IRB can gain energy for growth by coupling the oxidation of organic compounds or hydrogen with the reduction of Fe (III) [<xref ref-type="bibr" rid="scirp.69066-ref30">30</xref>] - [<xref ref-type="bibr" rid="scirp.69066-ref33">33</xref>] . The soils of rice fields are intermediate between upland systems and the true aquatic systems, and the alternation between anoxic and oxic conditions causes periodically the occurrence of redox reactions [<xref ref-type="bibr" rid="scirp.69066-ref32">32</xref>] . The IRB populations are abundant in paddy soils, because of the unique characteristics of these soils to provide abundant electron acceptors and substrates for their growth [<xref ref-type="bibr" rid="scirp.69066-ref32">32</xref>] .</p><p>After the soil flooding by stagnant water, reductive processes start immediately; the dissolved oxygen is consumed by aerobic bacteria and chemical oxidation reactions [<xref ref-type="bibr" rid="scirp.69066-ref34">34</xref>] - [<xref ref-type="bibr" rid="scirp.69066-ref36">36</xref>] . Oxygen is depleted fast in most regions of the soil and alternative electron acceptors are used [<xref ref-type="bibr" rid="scirp.69066-ref37">37</xref>] . Therefore, within a few days, aerobic and facultative anaerobic microorganisms use the free oxygen and reduce the oxidized compounds of the soil such as nitrates, Mn (IV)-oxides, oxides of Fe (III) as well as sulfates [<xref ref-type="bibr" rid="scirp.69066-ref35">35</xref>] [<xref ref-type="bibr" rid="scirp.69066-ref38">38</xref>] [<xref ref-type="bibr" rid="scirp.69066-ref39">39</xref>] . In anoxic conditions, the Fe (III)-comp- ounds are reduced and it results in ferrous ions production.</p><p>The appearance of iron toxicity symptoms in rice involves an excessive uptake of Fe<sup>2+</sup> and H<sub>2</sub>S<sup>−</sup> by the rice roots and its acropetal translocation into the leaves. The typical visual symptom associated with these processes is the “bronzing” of the rice leaves and substantial yield losses [<xref ref-type="bibr" rid="scirp.69066-ref11">11</xref>] [<xref ref-type="bibr" rid="scirp.69066-ref17">17</xref>] [<xref ref-type="bibr" rid="scirp.69066-ref18">18</xref>] .</p><p>Many studies showed that Iron-induced yield is frequently associated with a poor nutrient status of the soil [<xref ref-type="bibr" rid="scirp.69066-ref40">40</xref>] . Indeed, the iron toxicity was described as a multiple nutritional disorder hastened by, but also increased by the deficiency of mineral (P, K, and Zn) and H<sub>2</sub>S<sup>−</sup> toxicity [<xref ref-type="bibr" rid="scirp.69066-ref25">25</xref>] .</p><p>In order to determine the effect of chemical fertilization on microbiological and chemical parameters sustaining iron toxicity in paddy fields and on rice yield, the present study was conducted. Plastics pots were filled with a sensitive soil from Kou valley and amended by chemicals fertilizers. The iron-reducing bacterial populations’ density, Fe<sup>2+</sup> content in the paddy soil and iron accumulation in rice plant, were recorded during the cultural cycle of BOUAKE-189 and ROK-5 rice varieties (sensitive and tolerant to iron toxicity, respectively).</p></sec><sec id="s2"><title>2. Material and Methods</title><sec id="s2_1"><title>2.1. Sampling Site</title><p>The soil used for the experiments was collected at Kou Valley, a site located at the West of Burkina Faso (11˚23'12&quot;N and 4˚23'25&quot;W) and carried out to the experimental site of the University of Ouagadougou. The experiments were performed from June to November 2014. The physical and chemical proprieties of the soil studied are presented in <xref ref-type="table" rid="table1">Table 1</xref>. The soil studied had a sandy-silt texture, a high iron content and a low organic matter.</p></sec><sec id="s2_2"><title>2.2. Pots Experiments</title><p>Seventy two plastics pots with 25 cm<sup>3</sup> of bulk were used in 3 replications throughout the study. At the bottom of each pot, an external tap was installed to sub-drain the soil. After 2 weeks of flooding, 15 day-old rice plants were transplanted. Two rice varieties, BOUAKE-189 [<xref ref-type="bibr" rid="scirp.69066-ref41">41</xref>] and ROK-5 [<xref ref-type="bibr" rid="scirp.69066-ref42">42</xref>] , sensitive and resistant to iron toxicity, respectively were used. The soil was continuously flooded until rice maturity and harvest (120 days after flooding). Three replications and three modes of fertilization were performed throughout the study: without fertilization (control), NPK + Urea and NPK + Urea + Zn + Ca + Mg, respectively. The doses of N-P-K (14-23-14), Urea, CaCO<sub>3</sub>, ZnO and MgCl<sub>2</sub> application in pots were in the ratio of 720:240:50:22.4:20 mg/Kg of dry soil according to the recommended doses of 300 kg/ha for N-P-K, 100 kg/ha for urea, 10 kg/ha for ZnO, 250 kg/ha for CaCO<sub>3</sub> and 8.92 Kg/ha of MgCl<sub>2</sub> [<xref ref-type="bibr" rid="scirp.69066-ref40">40</xref>] [<xref ref-type="bibr" rid="scirp.69066-ref41">41</xref>] [<xref ref-type="bibr" rid="scirp.69066-ref43">43</xref>] - [<xref ref-type="bibr" rid="scirp.69066-ref46">46</xref>] .</p></sec><sec id="s2_3"><title>2.3. Enumeration of Iron-Reducing Bacterial Populations</title><p>The numbers of Iron-Reducing Bacteria (IRB) were determined by the most-probable-number (MPN) method, using the basal medium adapted from Hammann and Ottow [<xref ref-type="bibr" rid="scirp.69066-ref35">35</xref>] as described by Otoidobiga et al. [<xref ref-type="bibr" rid="scirp.69066-ref36">36</xref>] . The enumeration of bacteria was performed before flooding when the soil was dried, on transplanting day (two weeks after flooding) and during the rice growth stages until harvest near rice hills.</p><table-wrap id="table1" ><label><xref ref-type="table" rid="table1">Table 1</xref></label><caption><title> Physico-chemical characteristics of the Kou Valley soil</title></caption><table><tbody><thead><tr><th align="center" valign="middle" >Depth (cm)</th><th align="center" valign="middle" >Clay (%)</th><th align="center" valign="middle" >Silt (%)</th><th align="center" valign="middle" >Sand (%)</th><th align="center" valign="middle" >MO (%)</th><th align="center" valign="middle" >Total C (%)</th><th align="center" valign="middle" >Total N (%)</th><th align="center" valign="middle" >C/N</th><th align="center" valign="middle" >Fe<sub>t</sub><sub> </sub> ppm</th><th align="center" valign="middle" >Fe<sub>o</sub> ppm</th><th align="center" valign="middle" >pH<sub>H2O</sub></th></tr></thead><tr><td align="center" valign="middle" >0 - 10</td><td align="center" valign="middle" >23.53</td><td align="center" valign="middle" >33.33</td><td align="center" valign="middle" >43.14</td><td align="center" valign="middle" >1.829</td><td align="center" valign="middle" >1.061</td><td align="center" valign="middle" >0.089</td><td align="center" valign="middle" >12</td><td align="center" valign="middle" >29.23</td><td align="center" valign="middle" >0.08</td><td align="center" valign="middle" >3.73 - 4.52</td></tr><tr><td align="center" valign="middle" >10 - 20</td><td align="center" valign="middle" >27.45</td><td align="center" valign="middle" >33.33</td><td align="center" valign="middle" >39.22</td><td align="center" valign="middle" >1.484</td><td align="center" valign="middle" >0.861</td><td align="center" valign="middle" >0.077</td><td align="center" valign="middle" >11</td><td align="center" valign="middle" >41.98</td><td align="center" valign="middle" >0.53</td><td align="center" valign="middle" >3.71 - 4.43</td></tr><tr><td align="center" valign="middle" >20 - 40</td><td align="center" valign="middle" >45.10</td><td align="center" valign="middle" >23.53</td><td align="center" valign="middle" >31.37</td><td align="center" valign="middle" >0.688</td><td align="center" valign="middle" >0.399</td><td align="center" valign="middle" >0.035</td><td align="center" valign="middle" >11</td><td align="center" valign="middle" >56.65</td><td align="center" valign="middle" >0.84</td><td align="center" valign="middle" >3.75 - 4.52</td></tr></tbody></table></table-wrap><p>MO, Organic matter; C, Carbon; N, Nitrogen; C/N, Carbon to Nitrogen ratio; Fet, total amount of Fe; Fe<sub>o</sub><sub>, </sub>active Fe.</p></sec><sec id="s2_4"><title>2.4. Determination of Ferrous Iron in Soil</title><p>From the soil sampled for bacterial enumeration and at the same periods during the rice cultural cycle, the method of Vizier and Blanch [<xref ref-type="bibr" rid="scirp.69066-ref47">47</xref>] was used to measure the content of ferrous iron in the soil solution, using 0.2% ortho-phenantroline and 10% acetic acid reagents.</p></sec><sec id="s2_5"><title>2.5. Plant analysis</title><p>The Total Fe was analysed in the leaves and roots of the two rice varieties. Young leaves were taken from each pot during the cultural cycle of rice. At harvest, the aerial biomass and the roots of each plant were also collected. The dried leaves and roots were digested with a mixture of concentrated HNO<sub>3</sub> and HClO<sub>4</sub> [<xref ref-type="bibr" rid="scirp.69066-ref48">48</xref>] and the total Fe content was determined by Atomic Absorption Spectrometry [<xref ref-type="bibr" rid="scirp.69066-ref49">49</xref>] .</p></sec><sec id="s2_6"><title>2.6. Statistical Analysis</title><p>Data obtained were analysed with regard to the IRB populations’ development and activity, fertilization mode, rice growth stage and rice yield variations using the Student’s t-test and XLSTAT 2014 statistical software. Mean parameters were compared according to the Fishers’ test at 5% probability level.</p></sec></sec><sec id="s3"><title>3. Results and Discussion</title><sec id="s3_1"><title>3.1. Effect of Fertilization on IRB Populations Dynamics in Soil near BOUAKE-189 and ROK-5 Rice Roots</title><p>The variance of the numbers of IRB in soil near rice roots, in relation to fertilization mode and rice growth stage is presented in <xref ref-type="table" rid="table2">Table 2</xref>. The Fishers’ test revealed that the variance of the number of bacteria in the soil near BOUAKE-189 roots (sensitive to iron toxicity) was significantly related to fertilization (p &lt; 0.0001), stage of rice growth (p &lt; 0.0001) and combined both factors (p = 0.001, <xref ref-type="table" rid="table2">Table 2</xref>). Throughout the study, the average number of IRB population in the soil decreased significantly in NPK + Urea + Ca + Zn + Mg amended pots (p &lt; 0.0001), relatively to the control (T) and NPK + Urea pots ones (<xref ref-type="table" rid="table3">Table 3</xref>).</p><p>It appeared also that no significant difference was observed for fertilization on IRB populations (p = 0.24) in the soil near rice roots of the tolerant rice variety (ROK-5) (<xref ref-type="table" rid="table2">Table 2</xref>). However, the mean density of IRB population in the soil decreased for NPK + Urea + Ca + Zn + Mg amended pots, relatively to the control (T) and</p><table-wrap id="table2" ><label><xref ref-type="table" rid="table2">Table 2</xref></label><caption><title> Variance of IRB number in soil near rice roots in relation to fertilization and plant growth stage, during the cultural cycle of BOUAKE-189 and ROK-5 rice varieties</title></caption><table><tbody><thead><tr><th align="center" valign="middle"  colspan="2"  ></th><th align="center" valign="middle"  colspan="4"  >log (IRB number/g dry soil)</th></tr></thead><tr><td align="center" valign="middle" >Source of variation</td><td align="center" valign="middle" >df</td><td align="center" valign="middle"  colspan="2"  >BOUAKE-189</td><td align="center" valign="middle"  colspan="2"  >ROK-5</td></tr><tr><td align="center" valign="middle" ></td><td align="center" valign="middle" ></td><td align="center" valign="middle" >F</td><td align="center" valign="middle" >p</td><td align="center" valign="middle" >F</td><td align="center" valign="middle" >p</td></tr><tr><td align="center" valign="middle" >Fertilization</td><td align="center" valign="middle" >2</td><td align="center" valign="middle" >10.190</td><td align="center" valign="middle" >&lt;0.0001*</td><td align="center" valign="middle" >1.432</td><td align="center" valign="middle" >0.240<sup>ns</sup></td></tr><tr><td align="center" valign="middle" >Stage of plant growth</td><td align="center" valign="middle" >11</td><td align="center" valign="middle" >293.465</td><td align="center" valign="middle" >&lt;0.0001*</td><td align="center" valign="middle" >303.055</td><td align="center" valign="middle" >&lt;0.0001**</td></tr><tr><td align="center" valign="middle" >Fertilization* Stage of growth</td><td align="center" valign="middle" >22</td><td align="center" valign="middle" >2.296</td><td align="center" valign="middle" >0.001**</td><td align="center" valign="middle" >3.568</td><td align="center" valign="middle" >&lt;0.0001**</td></tr></tbody></table></table-wrap><p>df = degree of freedom; F = Fishers’ F; *significant p &lt; 0.05; **significant p &lt; 0.01; <sup>ns</sup>not significant p &lt; 0.05.</p><table-wrap id="table3" ><label><xref ref-type="table" rid="table3">Table 3</xref></label><caption><title> Effect of fertilization on IRB population number in soil near rice roots during the cultural cycle of BOUAKE-189 and ROK-5 rice varieties in pots not fertilized (T), and in pots fertilized with NPK + Urea and NPK + Urea + Ca + Zn + Mg (means of 3 replicates)</title></caption><table><tbody><thead><tr><th align="center" valign="middle" >Fertilization</th><th align="center" valign="middle"  colspan="2"  >log (IRB number/g dry soil)</th></tr></thead><tr><td align="center" valign="middle" ></td><td align="center" valign="middle" >BOUAKE-189</td><td align="center" valign="middle" >ROK-5</td></tr><tr><td align="center" valign="middle" >NPK + Urea</td><td align="center" valign="middle" >8.210<sup>a</sup></td><td align="center" valign="middle" >8.110<sup>a</sup></td></tr><tr><td align="center" valign="middle" >No Fertilization</td><td align="center" valign="middle" >8.136<sup>a</sup></td><td align="center" valign="middle" >8.045<sup>a</sup></td></tr><tr><td align="center" valign="middle" >NPK + Urea + Ca + Zn + Mg</td><td align="center" valign="middle" >7.602<sup>b</sup></td><td align="center" valign="middle" >7.873<sup>a</sup></td></tr></tbody></table></table-wrap><p>Means with a same letter within a column are not significantly different according to Fishers’ test p &lt; 0.05.</p><fig id="fig1"  position="float"><label><xref ref-type="fig" rid="fig1">Figure 1</xref></label><caption><title> Densities of Iron-Reducing Bacteria in soil before flooding, at transplanting day, and in soil near rice roots during the cultural cycle of BOUAKE-189 rice variety in pots without fertilization (T), and in NPK + Urea and NPK + Urea + Ca + Zn + Mg fertilized pots, respectively (means of 3 replicates)</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/5-6703035x7.png"/></fig><fig id="fig2"  position="float"><label><xref ref-type="fig" rid="fig2">Figure 2</xref></label><caption><title> Densities of Iron-Reducing Bacteria in soil before flooding, at transplanting day, and in soil near rice roots during the cultural cycle of ROK-5 rice variety in pots without fertilization (T), and in NPK + Urea and NPK + Urea + Ca + Zn + Mg fertilized pots, respectively (means of 3 replicates)</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/5-6703035x8.png"/></fig><p>NPK + Urea pots ones (<xref ref-type="table" rid="table3">Table 3</xref>). Study reported also that the number of IRB in the soil near rice roots was significantly related to the growth stage and combined effects of fertilization and growth stage (p &lt; 0.0001) of ROK-5.</p><p>These results are in agreement with those found by Benckiser et al. [<xref ref-type="bibr" rid="scirp.69066-ref40">40</xref>] which showed that the number of iron-reducing bacteria decreased with increased supply of K, Ca, and Mg for IR22 and IR42 rice varieties (susceptible and tolerant to iron toxicity, respectively). Thus, Trolldenier [<xref ref-type="bibr" rid="scirp.69066-ref50">50</xref>] found that a sufficient mineral nutrition of potassium, was important in maintaining the oxidising power of rice roots and in the reducing of IRB populations in rice fields.</p><p>The experiment showed also that the number of IRB in the soil near rice roots increased after two weeks of flooding in all pots for BOUAKE-189 and ROK-5 rice varieties (<xref ref-type="fig" rid="fig1">Figure 1</xref>, <xref ref-type="fig" rid="fig2">Figure 2</xref>). As reported by Hammann and Ottow [<xref ref-type="bibr" rid="scirp.69066-ref35">35</xref>] , soon as a soil is flooded, oxygen is consumed by soil respiration (bacteria and fungi mainly) and a large amounts of mineral elements as Fe III and nutriments were released in the soil solution [<xref ref-type="bibr" rid="scirp.69066-ref51">51</xref>] . In these conditions, Fe III was used as electron acceptor by IRB for anaerobic respiration, coupled to the biodegradation of organic compounds [<xref ref-type="bibr" rid="scirp.69066-ref33">33</xref>] [<xref ref-type="bibr" rid="scirp.69066-ref37">37</xref>] .</p><p><xref ref-type="fig" rid="fig1">Figure 1</xref> and <xref ref-type="fig" rid="fig2">Figure 2</xref>, showed that the number of IRB in soil near rice roots increased gradually with fluctuations from transplanting day to rice flowering and maturity stages in all the paddy pots. In most pots, the highest densities of IRB were recorded from rice tillering and flowering to maturity stages (10<sup>8</sup> to 10<sup>18</sup> cells/g dry soil). These results indicate that the presence of rice plants in the soils, influence and promote microbial processes, especially iron reduction [<xref ref-type="bibr" rid="scirp.69066-ref36">36</xref>] [<xref ref-type="bibr" rid="scirp.69066-ref52">52</xref>] [<xref ref-type="bibr" rid="scirp.69066-ref53">53</xref>] .</p><p>These results are in agreement with those of Berthelin et al. [<xref ref-type="bibr" rid="scirp.69066-ref52">52</xref>] who also recorded a same evolution of IRB population during rice cultural cycle in a Senegal paddy soil. Our previous results [<xref ref-type="bibr" rid="scirp.69066-ref36">36</xref>] obtained on Kamboinse paddy soil, reported the same pattern. Indeed, as reported by many studies, tillering, flowering and maturity stages which correspond to the highest level of reduced soil condition may enhance the exudation of carbohydrates and other metabolites sustaining IRB population growth in soil [<xref ref-type="bibr" rid="scirp.69066-ref33">33</xref>] [<xref ref-type="bibr" rid="scirp.69066-ref36">36</xref>] [<xref ref-type="bibr" rid="scirp.69066-ref52">52</xref>] .</p></sec><sec id="s3_2"><title>3.2. Effect of Mineral Fertilization on IRB Populations’ Activity in Soil near the Roots of BOUAKE-189 and ROK-5 Rice Plants</title><p>The variance of ferrous iron content in soil near rice roots in relation to fertilization and rice growth stage for both varieties is presented in <xref ref-type="table" rid="table4">Table 4</xref>. The Fishers’ test revealed that ferrous iron content in soil near rice roots was significantly related to fertilization (p = 0.009 and p = 0.049, for BOUAKE-189 and ROK-5 rice varieties, respectively), rice growth stage (p &lt; 0.0001) and combined both factors (p &lt; 0.0001, <xref ref-type="table" rid="table4">Table 4</xref>), for iron sensitive (BOUAKE-189) and tolerant (ROK-5) rice varieties, respectively. The study, also revealed that ferrous iron content in soil decreased significantly (p = 0.009 and p = 0.049, for BOUAKE-189 and ROK-5 rice varieties, respectively) in the NPK + Urea amended pots relatively to the control pots (<xref ref-type="table" rid="table5">Table 5</xref>). Trolldenier [<xref ref-type="bibr" rid="scirp.69066-ref50">50</xref>] showed that the nutritional status of rice plant essentially influences bacterial activity and oxidation-reduction conditions around the roots. Thus, Trolldenier [<xref ref-type="bibr" rid="scirp.69066-ref50">50</xref>] and Prade et al. [<xref ref-type="bibr" rid="scirp.69066-ref53">53</xref>] found that potassium and phosphorus nutrition, separately or in combination, reduced ferrous iron content in soil by maintaining the oxidising power of rice roots and decreased the uptake of Fe (II), which seemed to be governed by soil pH or redox potential, respectively.</p><p>The experiment reported also that the average of the ferrous iron content in the soil near rice roots increased significantly (p = 0.009 and p = 0.049) for the two rice varieties in the pots amended with NPK + Urea + Ca + Zn + Mg (<xref ref-type="table" rid="table5">Table 5</xref>), relatively to the control pots. Many studies reported that the role of Ca, Mg, and Zn fertilizers is the regulation of ferrous iron absorption in the rice plant, both as competing ion and by increasing the plant tolerance to iron toxicity [<xref ref-type="bibr" rid="scirp.69066-ref11">11</xref>] [<xref ref-type="bibr" rid="scirp.69066-ref17">17</xref>] . Therefore, NPK + Urea + Ca + Zn + Mg application doesn’t reduce ferrous iron production in rice fields but permit to rice plant to resist to the high content of toxic iron in soil.</p><p>In all pots, two peaks of intensive formation of Fe (II) occurred, one during two weeks after transplanting (primary iron toxicity) and the second between heading and flowering (<xref ref-type="fig" rid="fig3">Figure 3</xref>, <xref ref-type="fig" rid="fig4">Figure 4</xref>). In fact, in most pots, the highest content of ferrous iron in soil near rice roots was recorded from rice tillering and flowering to maturity stages at which it could reach 2.10<sup>3</sup> to 6.10<sup>3</sup> &#181;g/g dry soil. These results can be explained by an increased root permeability (K deficiency) and enhanced iron microbial reduction in the rizosphere due to intensive exudation during the physiological active phase between heading and flowering [<xref ref-type="bibr" rid="scirp.69066-ref33">33</xref>] [<xref ref-type="bibr" rid="scirp.69066-ref36">36</xref>] [<xref ref-type="bibr" rid="scirp.69066-ref53">53</xref>] . Thus, an improved energy supply (root debris and/or exudation of carbohydrates) stimulate microbial activity in general and anaerobic respiration (denitrification and/or ferric iron reduction) in particular [<xref ref-type="bibr" rid="scirp.69066-ref53">53</xref>] .</p></sec><sec id="s3_3"><title>3.3. Impact of Fertilization on BOUAKE-189 and ROK-5 Rice Plants Total Iron Content</title><p>The effect of fertilization on iron content in the BOUAKE-189 and ROK-5 rice varieties was measured during the study. Experiment showed that the total iron accumulation in BOUAKE-189 and ROK-5 rice plant was</p><table-wrap id="table4" ><label><xref ref-type="table" rid="table4">Table 4</xref></label><caption><title> Variance of ferrous iron content in soil near rice roots in relation to fertilization and rice growth stage during the cultural cycle of BOUAKE-189 and ROK-5 rice varieties in pots not fertilized (T), and in NPK + Urea and NPK + Urea + Ca + Zn + Mg fertilized pots</title></caption><table><tbody><thead><tr><th align="center" valign="middle"  colspan="2"  ></th><th align="center" valign="middle"  colspan="4"  >Ferrous iron content (&#181;g/g dry soil)</th></tr></thead><tr><td align="center" valign="middle" >Source of variation</td><td align="center" valign="middle" >df</td><td align="center" valign="middle"  colspan="2"  >BOUAKE-189</td><td align="center" valign="middle"  colspan="2"  >ROK-5</td></tr><tr><td align="center" valign="middle" ></td><td align="center" valign="middle" ></td><td align="center" valign="middle" >F</td><td align="center" valign="middle" >p</td><td align="center" valign="middle" >F</td><td align="center" valign="middle" >p</td></tr><tr><td align="center" valign="middle" >Fertilization</td><td align="center" valign="middle" >2</td><td align="center" valign="middle" >4.731</td><td align="center" valign="middle" >0.009*</td><td align="center" valign="middle" >3.040</td><td align="center" valign="middle" >0.049*</td></tr><tr><td align="center" valign="middle" >Stage of growth</td><td align="center" valign="middle" >12</td><td align="center" valign="middle" >60.562</td><td align="center" valign="middle" >&lt;0.0001**</td><td align="center" valign="middle" >41.174</td><td align="center" valign="middle" >&lt;0.0001**</td></tr><tr><td align="center" valign="middle" >Fertilization* Stage of growth</td><td align="center" valign="middle" >24</td><td align="center" valign="middle" >2.902</td><td align="center" valign="middle" >&lt;0.0001**</td><td align="center" valign="middle" >4.588</td><td align="center" valign="middle" >&lt;0.0001**</td></tr></tbody></table></table-wrap><p>df = degree of freedom; F = Fishers’ F; *significant p &lt; 0.05; **significant p &lt; 0.01.</p><table-wrap id="table5" ><label><xref ref-type="table" rid="table5">Table 5</xref></label><caption><title> Mean concentration of ferrous iron in soil near rice roots during the cultural cycle of BOUAKE-189 and ROK-5, rice varieties, in pots not fertilized (T), NPK + Urea and NPK + Urea + Ca + Zn + Mg fertilized pots (means of 3 replicates)</title></caption><table><tbody><thead><tr><th align="center" valign="middle" >Fertilization</th><th align="center" valign="middle"  colspan="2"  >Ferrous iron content (&#181;g/g dry soil)</th></tr></thead><tr><td align="center" valign="middle" ></td><td align="center" valign="middle" >BOUAKE-189</td><td align="center" valign="middle" >ROK-5</td></tr><tr><td align="center" valign="middle" >NPK + Urea + Ca + Zn + Mg</td><td align="center" valign="middle" >0.0015<sup>a </sup></td><td align="center" valign="middle" >0.0016<sup>a </sup></td></tr><tr><td align="center" valign="middle" >No fertilized</td><td align="center" valign="middle" >0.00149<sup>a </sup></td><td align="center" valign="middle" >0.00143<sup>b</sup></td></tr><tr><td align="center" valign="middle" >NPK + Urea</td><td align="center" valign="middle" >0.0013<sup>b </sup></td><td align="center" valign="middle" >0.00142<sup>b</sup></td></tr></tbody></table></table-wrap><p>Means with a same letter within a column are not significantly different according to Fishers’ test p &lt; 0.05.</p><fig id="fig3"  position="float"><label><xref ref-type="fig" rid="fig3">Figure 3</xref></label><caption><title> Evolution of the soil Ferrous iron content during the cultural cycle of BOUAKE-189 rice in pots not fertilized (T), fertilized with NPK + Urea and NPK + Urea + Ca + Zn + Mg, respectively (means of 3 replicates)</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/5-6703035x9.png"/></fig><p>significantly related to fertilization (p &lt; 0.0001). From the results obtained the content of iron in the leaves increased from rice tillering to flowering and maturity stages (1.299<sup> </sup>to 5.899 mg/g dry leaf, <xref ref-type="table" rid="table6">Table 6</xref>) during the cultural cycle of the two rice varieties. Iron mobilization in leaves increased critically according to Jones et al. [<xref ref-type="bibr" rid="scirp.69066-ref54">54</xref>] , who reported that iron content in rice leaves become toxic when the content exceed 300 ppm (Fe &gt; 0.3 mg/g dry leaf). The values recorded from our study, were largely over this critical value. However, only the control pots of BOUAKE-189 rice variety showed symptoms, according to the IRRI standard evaluation systems for rice [<xref ref-type="bibr" rid="scirp.69066-ref37">37</xref>] . One reason of this result could be due to the susceptibility and tolerance of BOUAKE-189 and ROK-5 varieties to iron toxicity, respectively as reported [<xref ref-type="bibr" rid="scirp.69066-ref41">41</xref>] [<xref ref-type="bibr" rid="scirp.69066-ref42">42</xref>] . Some studies also reported that yield losses</p><fig id="fig4"  position="float"><label><xref ref-type="fig" rid="fig4">Figure 4</xref></label><caption><title> Evolution of the soil Fe<sup>2+</sup> content during the cultural cycle of ROK-5 rice in pots not fertilized (T), fertilized with NPK + Urea and NPK + Urea + Ca + Zn + Mg, respectively (means of 3 replicates)</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/5-6703035x10.png"/></fig><table-wrap id="table6" ><label><xref ref-type="table" rid="table6">Table 6</xref></label><caption><title> Effect of fertilization on iron content in the parts of BOUAKE-189 and ROK-5 rice plants in pots not fertilized (T), fertilized with NPK + Urea and NPK + Urea + Ca + Zn + Mg (means of 3 replicates)</title></caption><table><tbody><thead><tr><th align="center" valign="middle" ></th><th align="center" valign="middle"  colspan="2"  >Leaf-30d</th><th align="center" valign="middle"  colspan="2"  >Leaf-60d</th><th align="center" valign="middle"  colspan="2"  >Leaf-90d</th><th align="center" valign="middle"  colspan="2"  >Biomass Aerial-120d</th><th align="center" valign="middle"  colspan="2"  >Root-120d</th></tr></thead><tr><td align="center" valign="middle" >Treatments (mg/g of dry leaf)</td><td align="center" valign="middle" >BOUAKE-189</td><td align="center" valign="middle" >ROK-5</td><td align="center" valign="middle" >BOUAKE-189</td><td align="center" valign="middle" >ROK-5</td><td align="center" valign="middle" >BOUAKE-189</td><td align="center" valign="middle" >ROK-5</td><td align="center" valign="middle" >BOUAKE-189</td><td align="center" valign="middle" >ROK-5</td><td align="center" valign="middle" >BOUAKE-189</td><td align="center" valign="middle" >ROK-5</td></tr><tr><td align="center" valign="middle" >NPK + Urea</td><td align="center" valign="middle" >2.188<sup>a </sup></td><td align="center" valign="middle" >3.188<sup>a</sup></td><td align="center" valign="middle" >2.266<sup>a</sup></td><td align="center" valign="middle" >3.266<sup>a</sup></td><td align="center" valign="middle" >1.854<sup>c</sup></td><td align="center" valign="middle" >2.854<sup>c</sup></td><td align="center" valign="middle" >3.248<sup>ab</sup></td><td align="center" valign="middle" >4.248<sup>ab</sup></td><td align="center" valign="middle" >4.899<sup>a</sup></td><td align="center" valign="middle" >5.899<sup>a</sup></td></tr><tr><td align="center" valign="middle" >NPK + Urea + Ca + Zn + Mg</td><td align="center" valign="middle" >1.846<sup>b </sup></td><td align="center" valign="middle" >2.846<sup>b</sup></td><td align="center" valign="middle" >2.163<sup>b</sup></td><td align="center" valign="middle" >3.163<sup>b</sup></td><td align="center" valign="middle" >2.215<sup>b</sup></td><td align="center" valign="middle" >3.215<sup>b</sup></td><td align="center" valign="middle" >3.865<sup>a</sup></td><td align="center" valign="middle" >4.865<sup>a</sup></td><td align="center" valign="middle" >2.495<sup>b</sup></td><td align="center" valign="middle" >3.495<sup>b</sup></td></tr><tr><td align="center" valign="middle" >No Fertilized</td><td align="center" valign="middle" >1.911<sup>b</sup></td><td align="center" valign="middle" >2.911<sup>b</sup></td><td align="center" valign="middle" >1.299<sup>c</sup></td><td align="center" valign="middle" >2.299<sup>c</sup></td><td align="center" valign="middle" >2.611<sup>a</sup></td><td align="center" valign="middle" >3.611<sup>a</sup></td><td align="center" valign="middle" >2.345<sup>b</sup></td><td align="center" valign="middle" >3.345<sup>b</sup></td><td align="center" valign="middle" >2.947<sup>b</sup></td><td align="center" valign="middle" >3.947<sup>b</sup></td></tr></tbody></table></table-wrap><p>Means with a same letter within a column are not significantly different according to Fishers’ test p &lt; 0.05.</p><p>and the symptoms of leaf bronzing due to iron toxicity, were more pronounced in the dry-season as compared to the wet-season [<xref ref-type="bibr" rid="scirp.69066-ref28">28</xref>] [<xref ref-type="bibr" rid="scirp.69066-ref55">55</xref>] . Thus, in the present study, the period of experiment (wet season) may have reduced the appearance of the symptoms of iron toxicity.</p><p>The study revealed also that NPK + Urea + Ca + Zn + Mg amended pots, had the greatest Fe content in aerial biomass at harvest, followed by NPK + Urea and control pots (no fertilization), respectively, for both varieties.</p><p>These results are in agreement with those of Panda et al. [<xref ref-type="bibr" rid="scirp.69066-ref56">56</xref>] who showed that the leaf iron content increased with the increases of N, P, and K application for Sharbati, IR-64 and Lalat rice varieties. Panda et al. [<xref ref-type="bibr" rid="scirp.69066-ref56">56</xref>] found also that among the nutrients, N was most effective in increasing leaf Fe concentration, followed by P and K for the three rice cultivars tested.</p><p>Panda et al. [<xref ref-type="bibr" rid="scirp.69066-ref56">56</xref>] explained the physiological and biochemical mechanisms that improve Fe uptake under a favourable N, P or K nutrition. Therefore, rice plants release the siderophores into the rhizosphere, which bind to Fe<sup>3+</sup> in the form of a ligand. The ligand complex enters into the cell, and Fe<sup>3+</sup> is reduced into Fe<sup>2+</sup> inside the cytoplasm. Thus, NPK applications might contributed to Fe acquisition by enabling the plant to synthesize more photosynthetic assimilates and more reducing power (NADPH+H+), which might helped in the synthesis and release of more siderophores in the rice rhizosphere and subsequent reduction of Fe<sup>3+</sup> to a soluble ferrous form. Thus, the mineral amendment (Ca, Mg, Mn P, K and Zn) in iron toxicity conditions seems to promote leaf tissue tolerance to excess amounts of Fe [<xref ref-type="bibr" rid="scirp.69066-ref57">57</xref>] and to optimize Fe<sup>3+</sup> absorption in the rice plant for a better growth and better yield [<xref ref-type="bibr" rid="scirp.69066-ref17">17</xref>] .</p><p>The NPK + Urea amended pots showed also the highest content of total Fe in roots at harvest followed by NPK + Urea + Ca + Zn + Mg and the control pots, respectively, for the two rice varieties. Therefore, NPK + Urea and NPK + Urea + Ca + Zn + Mg applications seem to promote also the capacity of BOUAKE-189 and ROK-5 rice varieties to survive into an iron toxicity condition by oxidizing Fe II into their Fe<sup>3+</sup> forms at the root surface (Fe-excluding power) [<xref ref-type="bibr" rid="scirp.69066-ref58">58</xref>] [<xref ref-type="bibr" rid="scirp.69066-ref59">59</xref>] .</p><p>The experiment reported also that the iron tolerant rice variety (ROK-5), showed the highest accumulation of iron than the sensitive rice variety (BOUAKE-189) and the content of iron in the roots was significantly higher than in the aerial biomass. These results can be explained by the physiological mechanisms of iron (II) avoidance and/or tolerance of rice plants in order to survive under Fe-toxic condition [<xref ref-type="bibr" rid="scirp.69066-ref60">60</xref>] [<xref ref-type="bibr" rid="scirp.69066-ref61">61</xref>] . Therefore, ROK-5 rice variety can survive to iron toxicity by oxidation of ferrous iron at the root surface (Fe-oxidizing power) [<xref ref-type="bibr" rid="scirp.69066-ref52">52</xref>] , exclusion of Fe at the root surface (Fe-excluding power), retention of Fe in the root tissue (Fe-retaining power) [<xref ref-type="bibr" rid="scirp.69066-ref58">58</xref>] [<xref ref-type="bibr" rid="scirp.69066-ref59">59</xref>] or by leaf tissue tolerance to excess amounts of Fe [<xref ref-type="bibr" rid="scirp.69066-ref57">57</xref>] .</p></sec><sec id="s3_4"><title>3.4. Impact of Fertilization on BOUAKE-189 and ROK-5 Rice Varieties Yield</title><p>From our results, a significant difference (p &lt; 0.0001) was found for the rice biomass yield among treatments for both varieties (BOUAKE-189 and ROK-5). Our study reported also that ROK-5 rice variety (tolerant to iron toxicity) recorded the highest biomass yield among treatments. Thus, as reported by Mahato et al. [<xref ref-type="bibr" rid="scirp.69066-ref62">62</xref>] , the yield parameters of the rice plant in iron toxicity conditions, is related to genetic variation of cultivars.</p><p>The pots which received NPK + Urea + Ca + Zn + Mg application, recorded also the highest yield followed by NPK + Urea and the control pots (<xref ref-type="fig" rid="fig5">Figure 5</xref>). These results are in agreement with those obtained by Panda et al. [<xref ref-type="bibr" rid="scirp.69066-ref56">56</xref>] which reported that plant biomass and grain yield of all cultivars were improved by the applications of Nitrogen, Potassium and Phosphorus. Also, depending on the soil and the season, application of P, K, Ca, Mg, and Zn, solely or in combinations, can reduce bronzing symptoms and increase rice yield [<xref ref-type="bibr" rid="scirp.69066-ref3">3</xref>] [<xref ref-type="bibr" rid="scirp.69066-ref29">29</xref>] [<xref ref-type="bibr" rid="scirp.69066-ref41">41</xref>] [<xref ref-type="bibr" rid="scirp.69066-ref56">56</xref>] . Shu and Chung [<xref ref-type="bibr" rid="scirp.69066-ref63">63</xref>] reported also that it is possible that absorption of N, P, and K by the plant increases biomass and grain yield in rice because the nutrients play positive roles directly or indirectly on leaf photosynthesis to improve primary production. The application of essential plant nutrients can also counteract negative effects of excess amounts of iron, by competing with Fe<sup>2+</sup> uptake at the sites of ion adsorption of the root or by enhancing plants’ defence or tolerance mechanisms [<xref ref-type="bibr" rid="scirp.69066-ref25">25</xref>] . Fageria et al. [<xref ref-type="bibr" rid="scirp.69066-ref17">17</xref>] and Sahrawat [<xref ref-type="bibr" rid="scirp.69066-ref11">11</xref>] also revealed that Zinc application increased the tolerance of rice to an elevated content of reduced iron in the soil. Therefore, a chemical amendment (Ca, Mg, Mn P, K and Zn) can play an important role in the regulation of Fe up-take in the rice plant by optimizing the Fe<sup>3+</sup> absorption in the rice plant for a better growth and yield [<xref ref-type="bibr" rid="scirp.69066-ref17">17</xref>] .</p><fig id="fig5"  position="float"><label><xref ref-type="fig" rid="fig5">Figure 5</xref></label><caption><title> Yield of total biomass of BOUAKE-189 and ROK-5 rice varieties in pots not fertilized, fertilized with NPK + Urea and NPK + Urea + Ca + Zn + Mg, respectively (means of 3 replicates).Yields sharing the same letter are not significantly different according to Fishers’ test p &lt; 0.05</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/5-6703035x11.png"/></fig></sec></sec><sec id="s4"><title>4. Conclusions</title><p>The experiment revealed that mineral fertilization (NPK, Urea, Ca, Zn, Mg) decreased significantly the number of IRB in the soil near the roots of ROK-5 and BOUAKE-189 rice varieties (iron tolerant and iron susceptible rice varieties, respectively). However, in all pots, the highest densities of IRB and ferrous iron content in soil near rice roots were recorded from rice tillering and flowering to maturity stages. This result indicates that the presence of rice plants in the soils, influences and favours microbial processes and iron reduction by an intensive exudation during the physiological active phase between heading and flowering.</p><p>The study reported also that NPK + Urea amendment decreased significantly ferrous iron content in soil near rice roots relatively to control pots. However, amendment of rice fields with NPK + Urea + Ca + Zn + Mg fertilizers increased significantly the ferrous iron content in the soil near rice roots and accumulated the greatest Fe content for iron sensitive and tolerant rice varieties. In fact, Potassium and Phosphorus nutrition, separately or in combination, reduce ferrous iron content in soil by maintaining the oxidising power of rice roots and decrease Fe (II) uptake. However, NPK + Urea + Ca + Zn + Mg application didn’t reduce ferrous iron production in rice fields but permitted a high resistance to rice plant to survive in condition of iron toxicity in soil. Application of P, K, Ca, Mg, and Zn, solely or in combinations has been also reported to reduce bronzing symptoms and to increase rice yield depending on the soil and the season. The study showed also that the pots which received NPK + Urea + Ca + Zn + Mg application, recorded the highest yield followed by NPK + Urea and the control for the two rice varieties.</p></sec><sec id="s5"><title>Acknowledgements</title><p>The authors would like to express profound gratitude to CNRST/IRSS, International Foundation for Science, CIOSPB, PACER-UEMOA/RABIOTECH, FCN/WAAPP and CNS-FL/WAAPP, for financial and technical supports.</p></sec><sec id="s6"><title>Cite this paper</title><p>C&#232;cile Harmonie Otoidobiga,Adama Sawadogo,Yapi Sinar&#232;,Ibrahima Ou&#232;draogo,Prosper Zombr&#232;,Susumu Asakawa,Alfred S. Traore,Day&#232;ri Dianou, (2016) Effect of Fertilization on the Dynamics and Activity of Iron-Reducing Bacterial Populations in a West African Rice Paddy Soil Planted with Two Rice Varieties: Case Study of Kou Valley in Burkina Faso. 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