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A Review of CO2 Sequestration Projects and Application in China

Identifieur interne : 000346 ( Ncbi/Merge ); précédent : 000345; suivant : 000347

A Review of CO2 Sequestration Projects and Application in China

Auteurs : Yong Tang [République populaire de Chine] ; Ruizhi Yang [République populaire de Chine] ; Xiaoqiang Bian [République populaire de Chine]

Source :

RBID : PMC:4181513

Abstract

In 2008, the top CO2 emitters were China, United States, and European Union. The rapid growing economy and the heavy reliance on coal in China give rise to the continued growth of CO2 emission, deterioration of anthropogenic climate change, and urgent need of new technologies. Carbon Capture and sequestration is one of the effective ways to provide reduction of CO2 emission and mitigation of pollution. Coal-fired power plants are the focus of CO2 source supply due to their excessive emission and the energy structure in China. And over 80% of the large CO2 sources are located nearby storage reservoirs. In China, the CO2 storage potential capacity is of about 3.6 × 109 t for all onshore oilfields; 30.483 × 109 t for major gas fields between 900 m and 3500 m of depth; 143.505 × 109 t for saline aquifers; and 142.67 × 109 t for coal beds. On the other hand, planation, soil carbon sequestration, and CH4–CO2 reforming also contribute a lot to carbon sequestration. This paper illustrates some main situations about CO2 sequestration applications in China with the demonstration of several projects regarding different ways of storage. It is concluded that China possesses immense potential and promising future of CO2 sequestration.


Url:
DOI: 10.1155/2014/381854
PubMed: 25302323
PubMed Central: 4181513

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<p>In 2008, the top CO
<sub>2</sub>
emitters were China, United States, and European Union. The rapid growing economy and the heavy reliance on coal in China give rise to the continued growth of CO
<sub>2</sub>
emission, deterioration of anthropogenic climate change, and urgent need of new technologies. Carbon Capture and sequestration is one of the effective ways to provide reduction of CO
<sub>2</sub>
emission and mitigation of pollution. Coal-fired power plants are the focus of CO
<sub>2</sub>
source supply due to their excessive emission and the energy structure in China. And over 80% of the large CO
<sub>2</sub>
sources are located nearby storage reservoirs. In China, the CO
<sub>2</sub>
storage potential capacity is of about 3.6 × 10
<sup>9</sup>
 t for all onshore oilfields; 30.483 × 10
<sup>9</sup>
 t for major gas fields between 900 m and 3500 m of depth; 143.505 × 10
<sup>9</sup>
 t for saline aquifers; and 142.67 × 10
<sup>9</sup>
 t for coal beds. On the other hand, planation, soil carbon sequestration, and CH
<sub>4</sub>
–CO
<sub>2</sub>
reforming also contribute a lot to carbon sequestration. This paper illustrates some main situations about CO
<sub>2</sub>
sequestration applications in China with the demonstration of several projects regarding different ways of storage. It is concluded that China possesses immense potential and promising future of CO
<sub>2</sub>
sequestration.</p>
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</TEI>
<pmc article-type="review-article">
<pmc-dir>properties open_access</pmc-dir>
<front>
<journal-meta>
<journal-id journal-id-type="nlm-ta">ScientificWorldJournal</journal-id>
<journal-id journal-id-type="iso-abbrev">ScientificWorldJournal</journal-id>
<journal-id journal-id-type="publisher-id">TSWJ</journal-id>
<journal-title-group>
<journal-title>The Scientific World Journal</journal-title>
</journal-title-group>
<issn pub-type="ppub">2356-6140</issn>
<issn pub-type="epub">1537-744X</issn>
<publisher>
<publisher-name>Hindawi Publishing Corporation</publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="pmid">25302323</article-id>
<article-id pub-id-type="pmc">4181513</article-id>
<article-id pub-id-type="doi">10.1155/2014/381854</article-id>
<article-categories>
<subj-group subj-group-type="heading">
<subject>Review Article</subject>
</subj-group>
</article-categories>
<title-group>
<article-title>A Review of CO
<sub>2</sub>
Sequestration Projects and Application in China</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Tang</surname>
<given-names>Yong</given-names>
</name>
<xref ref-type="aff" rid="I1"></xref>
</contrib>
<contrib contrib-type="author">
<name>
<surname>Yang</surname>
<given-names>Ruizhi</given-names>
</name>
<xref ref-type="aff" rid="I1"></xref>
<xref ref-type="corresp" rid="cor1">*</xref>
</contrib>
<contrib contrib-type="author">
<name>
<surname>Bian</surname>
<given-names>Xiaoqiang</given-names>
</name>
<xref ref-type="aff" rid="I1"></xref>
</contrib>
</contrib-group>
<aff id="I1">The State Key Laboratory of Oil & Gas Reservoir Geology and Exploitation Engineering, Southwest Petroleum University, Chengdu 610500, China</aff>
<author-notes>
<corresp id="cor1">*Ruizhi Yang:
<email>yrz4293@163.com</email>
</corresp>
<fn fn-type="other">
<p>Academic Editor: Arman Siahvashi</p>
</fn>
</author-notes>
<pub-date pub-type="ppub">
<year>2014</year>
</pub-date>
<pub-date pub-type="epub">
<day>1</day>
<month>7</month>
<year>2014</year>
</pub-date>
<volume>2014</volume>
<elocation-id>381854</elocation-id>
<history>
<date date-type="received">
<day>28</day>
<month>4</month>
<year>2014</year>
</date>
<date date-type="accepted">
<day>6</day>
<month>6</month>
<year>2014</year>
</date>
</history>
<permissions>
<copyright-statement>Copyright © 2014 Yong Tang et al.</copyright-statement>
<copyright-year>2014</copyright-year>
<license license-type="open-access">
<license-p>This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.</license-p>
</license>
</permissions>
<abstract>
<p>In 2008, the top CO
<sub>2</sub>
emitters were China, United States, and European Union. The rapid growing economy and the heavy reliance on coal in China give rise to the continued growth of CO
<sub>2</sub>
emission, deterioration of anthropogenic climate change, and urgent need of new technologies. Carbon Capture and sequestration is one of the effective ways to provide reduction of CO
<sub>2</sub>
emission and mitigation of pollution. Coal-fired power plants are the focus of CO
<sub>2</sub>
source supply due to their excessive emission and the energy structure in China. And over 80% of the large CO
<sub>2</sub>
sources are located nearby storage reservoirs. In China, the CO
<sub>2</sub>
storage potential capacity is of about 3.6 × 10
<sup>9</sup>
 t for all onshore oilfields; 30.483 × 10
<sup>9</sup>
 t for major gas fields between 900 m and 3500 m of depth; 143.505 × 10
<sup>9</sup>
 t for saline aquifers; and 142.67 × 10
<sup>9</sup>
 t for coal beds. On the other hand, planation, soil carbon sequestration, and CH
<sub>4</sub>
–CO
<sub>2</sub>
reforming also contribute a lot to carbon sequestration. This paper illustrates some main situations about CO
<sub>2</sub>
sequestration applications in China with the demonstration of several projects regarding different ways of storage. It is concluded that China possesses immense potential and promising future of CO
<sub>2</sub>
sequestration.</p>
</abstract>
</article-meta>
</front>
<floats-group>
<fig id="fig1" orientation="portrait" position="float">
<label>Figure 1</label>
<caption>
<p>Locations of large CO
<sub>2</sub>
point sources and CO
<sub>2</sub>
storage reservoir in China (from Dahowski et al. [
<xref rid="B10" ref-type="bibr">10</xref>
]).</p>
</caption>
<graphic xlink:href="TSWJ2014-381854.001"></graphic>
</fig>
<fig id="fig2" orientation="portrait" position="float">
<label>Figure 2</label>
<caption>
<p>Diagram of well location and surface layout of cross-well seismic lines: yellow dots are CO
<sub>2</sub>
injectors, and the seismic lines are in deep blue color (from Ren et al. [
<xref rid="B45" ref-type="bibr">45</xref>
]).</p>
</caption>
<graphic xlink:href="TSWJ2014-381854.002"></graphic>
</fig>
<fig id="fig3" orientation="portrait" position="float">
<label>Figure 3</label>
<caption>
<p>Measured oil production, water cut, CO
<sub>2</sub>
content and GOR in the CO
<sub>2</sub>
miscible pilot area of Jinlin oilfield (from Ren et al. [
<xref rid="B45" ref-type="bibr">45</xref>
]).</p>
</caption>
<graphic xlink:href="TSWJ2014-381854.003"></graphic>
</fig>
<fig id="fig4" orientation="portrait" position="float">
<label>Figure 4</label>
<caption>
<p>Geotectonic map showing the main depression and uplift regions in the Suibei basin, where the Caoshe oilfield is located (from Zhang [
<xref rid="B52" ref-type="bibr">52</xref>
]).</p>
</caption>
<graphic xlink:href="TSWJ2014-381854.004"></graphic>
</fig>
<fig id="fig5" orientation="portrait" position="float">
<label>Figure 5</label>
<caption>
<p>Simulation result of CO
<sub>2</sub>
miscible flooding of the Taizhou Formation reservoir in the Caoshe oilfield (from Yu et al. [
<xref rid="B51" ref-type="bibr">51</xref>
]).</p>
</caption>
<graphic xlink:href="TSWJ2014-381854.005"></graphic>
</fig>
<fig id="fig6" orientation="portrait" position="float">
<label>Figure 6</label>
<caption>
<p>Distribution of sandbodies in the LT13-1 saline aquifer (from Zhang [
<xref rid="B52" ref-type="bibr">52</xref>
]).</p>
</caption>
<graphic xlink:href="TSWJ2014-381854.006"></graphic>
</fig>
<fig id="fig7" orientation="portrait" position="float">
<label>Figure 7</label>
<caption>
<p>CO
<sub>2</sub>
gas distribution radius in sandbodies A and C during and after injection (from Zhang [
<xref rid="B52" ref-type="bibr">52</xref>
]).</p>
</caption>
<graphic xlink:href="TSWJ2014-381854.007"></graphic>
</fig>
<fig id="fig8" orientation="portrait" position="float">
<label>Figure 8</label>
<caption>
<p>High-pressure CO
<sub>2</sub>
adsorption on the dry Haishiwan coals at 40°C with respect to density (a); CO
<sub>2</sub>
excess sorption isotherms and free CO
<sub>2</sub>
content versus pressure (b);
<italic>P</italic>
<sub>SC</sub>
is the critical pressure of CO
<sub>2</sub>
(from Li et al. [
<xref rid="B75" ref-type="bibr">69</xref>
]).</p>
</caption>
<graphic xlink:href="TSWJ2014-381854.008"></graphic>
</fig>
<table-wrap id="tab1" orientation="portrait" position="float">
<label>Table 1</label>
<caption>
<p>Comparison of different CO
<sub>2</sub>
sequestration projects.</p>
</caption>
<table frame="hsides" rules="groups">
<thead>
<tr>
<th align="left" rowspan="1" colspan="1">Storage media</th>
<th align="center" rowspan="1" colspan="1">Total CO
<sub>2</sub>
storage capacity</th>
<th align="center" rowspan="1" colspan="1">Project</th>
<th align="center" rowspan="1" colspan="1">CO
<sub>2</sub>
storage capacity</th>
<th align="center" rowspan="1" colspan="1">EOR potential</th>
<th align="center" rowspan="1" colspan="1">Cost of storage</th>
</tr>
</thead>
<tbody>
<tr>
<td align="left" rowspan="6" colspan="1">Oilfield</td>
<td align="center" rowspan="6" colspan="1">4.6 × 10
<sup>9</sup>
 t (>800 m)</td>
<td align="center" rowspan="1" colspan="1">Jilin</td>
<td align="center" rowspan="1" colspan="1">0.7 × 10
<sup>6</sup>
 t </td>
<td align="center" rowspan="1" colspan="1">0.5 × 10
<sup>6</sup>
 t </td>
<td align="center" rowspan="1" colspan="1">1 : 1.37
<break></break>
(input : output)</td>
</tr>
<tr>
<td align="center" rowspan="1" colspan="1">Caoshe</td>
<td align="center" rowspan="1" colspan="1">0.309 × 10
<sup>9</sup>
 m
<sup>3</sup>
<break></break>
(by 2009)</td>
<td align="center" rowspan="1" colspan="1">0.03 × 10
<sup>6</sup>
 t
<break></break>
(by 2009)</td>
<td align="center" rowspan="1" colspan="1">$25.78/t</td>
</tr>
<tr>
<td align="center" rowspan="1" colspan="1">Jingbian</td>
<td align="center" rowspan="1" colspan="1">0.04 × 10
<sup>6</sup>
 t/yr</td>
<td align="center" rowspan="1" colspan="1">0.05 × 10
<sup>6</sup>
 t/yr</td>
<td align="center" rowspan="1" colspan="1"></td>
</tr>
<tr>
<td align="center" rowspan="1" colspan="1">Changqing</td>
<td align="center" rowspan="1" colspan="1">0.098 × 10
<sup>9</sup>
 t</td>
<td align="center" rowspan="1" colspan="1">0.239 × 10
<sup>9</sup>
 t </td>
<td align="center" rowspan="1" colspan="1"></td>
</tr>
<tr>
<td align="center" rowspan="1" colspan="1">Shengli</td>
<td align="center" rowspan="1" colspan="1">95.539 × 10
<sup>6</sup>
 t</td>
<td align="center" rowspan="1" colspan="1">9.997 × 10
<sup>6</sup>
 t</td>
<td align="center" rowspan="1" colspan="1"></td>
</tr>
<tr>
<td align="center" rowspan="1" colspan="1">Xinjiang</td>
<td align="center" rowspan="1" colspan="1">0.495 × 10
<sup>9</sup>
 t</td>
<td align="center" rowspan="1" colspan="1"></td>
<td align="center" rowspan="1" colspan="1"></td>
</tr>
<tr>
<td align="center" colspan="6" rowspan="1">
<hr></hr>
</td>
</tr>
<tr>
<td align="left" rowspan="1" colspan="1">Gas field</td>
<td align="center" rowspan="1" colspan="1">30.483 × 10
<sup>9</sup>
 t  
<break></break>
(900–3500 m)</td>
<td align="center" rowspan="1" colspan="1">DF1-1</td>
<td align="center" rowspan="1" colspan="1">0.511 × 10
<sup>9</sup>
 Sm
<sup>3</sup>
</td>
<td align="center" rowspan="1" colspan="1"></td>
<td align="center" rowspan="1" colspan="1">$20/t</td>
</tr>
<tr>
<td align="center" colspan="6" rowspan="1">
<hr></hr>
</td>
</tr>
<tr>
<td align="left" rowspan="3" colspan="1">Saline aquifer</td>
<td align="center" rowspan="3" colspan="1">143.505 × 10
<sup>9</sup>
 t</td>
<td align="center" rowspan="1" colspan="1">LT13-1</td>
<td align="center" rowspan="1" colspan="1">0.1 × 10
<sup>9</sup>
 t</td>
<td align="center" rowspan="1" colspan="1"></td>
<td align="center" rowspan="1" colspan="1">$33–37/t</td>
</tr>
<tr>
<td align="center" rowspan="1" colspan="1">Bohai Bay</td>
<td align="center" rowspan="1" colspan="1">3.9 × 10
<sup>9</sup>
 t</td>
<td align="center" rowspan="1" colspan="1"></td>
<td align="center" rowspan="1" colspan="1"></td>
</tr>
<tr>
<td align="center" rowspan="1" colspan="1">Songliao</td>
<td align="center" rowspan="1" colspan="1">8.96 × 10
<sup>9</sup>
 t</td>
<td align="center" rowspan="1" colspan="1"></td>
<td align="center" rowspan="1" colspan="1"></td>
</tr>
<tr>
<td align="center" colspan="6" rowspan="1">
<hr></hr>
</td>
</tr>
<tr>
<td align="left" rowspan="1" colspan="1">Coal seam</td>
<td align="center" rowspan="1" colspan="1">142.67 × 10
<sup>9</sup>
 t</td>
<td align="center" rowspan="1" colspan="1">Haishiwan</td>
<td align="center" rowspan="1" colspan="1">44.7 m
<sup>3</sup>
/t</td>
<td align="center" rowspan="1" colspan="1"></td>
<td align="center" rowspan="1" colspan="1"></td>
</tr>
<tr>
<td align="center" colspan="6" rowspan="1">
<hr></hr>
</td>
</tr>
<tr>
<td align="left" rowspan="1" colspan="1">Plantation</td>
<td align="center" rowspan="1" colspan="1">3.169 PgC  
<break></break>
(by 2050)</td>
<td align="center" rowspan="1" colspan="1"></td>
<td align="center" rowspan="1" colspan="1"></td>
<td align="center" rowspan="1" colspan="1"></td>
<td align="center" rowspan="1" colspan="1"><$10/t</td>
</tr>
<tr>
<td align="center" colspan="6" rowspan="1">
<hr></hr>
</td>
</tr>
<tr>
<td align="left" rowspan="1" colspan="1">Soil carbon sequestration</td>
<td align="center" rowspan="1" colspan="1">29.2–847.7 TgC  
<break></break>
(by 2050)</td>
<td align="center" rowspan="1" colspan="1"></td>
<td align="center" rowspan="1" colspan="1"></td>
<td align="center" rowspan="1" colspan="1"></td>
<td align="center" rowspan="1" colspan="1"></td>
</tr>
</tbody>
</table>
</table-wrap>
</floats-group>
</pmc>
<affiliations>
<list>
<country>
<li>République populaire de Chine</li>
</country>
</list>
<tree>
<country name="République populaire de Chine">
<noRegion>
<name sortKey="Tang, Yong" sort="Tang, Yong" uniqKey="Tang Y" first="Yong" last="Tang">Yong Tang</name>
</noRegion>
<name sortKey="Bian, Xiaoqiang" sort="Bian, Xiaoqiang" uniqKey="Bian X" first="Xiaoqiang" last="Bian">Xiaoqiang Bian</name>
<name sortKey="Yang, Ruizhi" sort="Yang, Ruizhi" uniqKey="Yang R" first="Ruizhi" last="Yang">Ruizhi Yang</name>
</country>
</tree>
</affiliations>
</record>

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