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<front>
<journal-meta>
<journal-id journal-id-type="publisher-id">Front. Earth Sci.</journal-id>
<journal-title>Frontiers in Earth Science</journal-title>
<abbrev-journal-title abbrev-type="pubmed">Front. Earth Sci.</abbrev-journal-title>
<issn pub-type="epub">2296-6463</issn>
<publisher>
<publisher-name>Frontiers Media S.A.</publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="publisher-id">1362776</article-id>
<article-id pub-id-type="doi">10.3389/feart.2024.1362776</article-id>
<article-categories>
<subj-group subj-group-type="heading">
<subject>Earth Science</subject>
<subj-group>
<subject>Original Research</subject>
</subj-group>
</subj-group>
</article-categories>
<title-group>
<article-title>Study of the effect of salt deposition on production capacity and storage capacity in underground gas storage</article-title>
<alt-title alt-title-type="left-running-head">Zhongxin et al.</alt-title>
<alt-title alt-title-type="right-running-head">
<ext-link ext-link-type="uri" xlink:href="https://doi.org/10.3389/feart.2024.1362776">10.3389/feart.2024.1362776</ext-link>
</alt-title>
</title-group>
<contrib-group>
<contrib contrib-type="author" corresp="yes">
<name>
<surname>Zhongxin</surname>
<given-names>Ren</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="corresp" rid="c001">&#x2a;</xref>
<uri xlink:href="https://loop.frontiersin.org/people/994541/overview"/>
<role content-type="https://credit.niso.org/contributor-roles/Writing - review &#x26; editing/"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname>Xiaoping</surname>
<given-names>Yang</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author">
<name>
<surname>Dawei</surname>
<given-names>Chang</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author">
<name>
<surname>Ning</surname>
<given-names>Wang</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author">
<name>
<surname>Da</surname>
<given-names>Meng</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group>
<aff id="aff1">
<sup>1</sup>
<institution>National Oil and Gas Pipeline Network Group</institution>, <addr-line>Shanghai</addr-line>, <country>China</country>
</aff>
<aff id="aff2">
<sup>2</sup>
<institution>Petroleum Engineering School</institution>, <institution>Southwest Petroleum University</institution>, <addr-line>Chendu</addr-line>, <country>China</country>
</aff>
<author-notes>
<fn fn-type="edited-by">
<p>
<bold>Edited by:</bold> <ext-link ext-link-type="uri" xlink:href="https://loop.frontiersin.org/people/1423308/overview">Paolo Capuano</ext-link>, University of Salerno, Italy</p>
</fn>
<fn fn-type="edited-by">
<p>
<bold>Reviewed by:</bold> <ext-link ext-link-type="uri" xlink:href="https://loop.frontiersin.org/people/2623722/overview">Behnam Sedaee</ext-link>, University of Tehran, Iran</p>
<p>
<ext-link ext-link-type="uri" xlink:href="https://loop.frontiersin.org/people/1716395/overview">Zhongwei Wu</ext-link>, Yangtze University, China</p>
</fn>
<corresp id="c001">&#x2a;Correspondence: Ren Zhongxin, <email>765802228@qq.com</email>
</corresp>
</author-notes>
<pub-date pub-type="epub">
<day>07</day>
<month>03</month>
<year>2024</year>
</pub-date>
<pub-date pub-type="collection">
<year>2024</year>
</pub-date>
<volume>12</volume>
<elocation-id>1362776</elocation-id>
<history>
<date date-type="received">
<day>29</day>
<month>12</month>
<year>2023</year>
</date>
<date date-type="accepted">
<day>27</day>
<month>02</month>
<year>2024</year>
</date>
</history>
<permissions>
<copyright-statement>Copyright &#xa9; 2024 Zhongxin, Xiaoping, Dawei, Ning and Da.</copyright-statement>
<copyright-year>2024</copyright-year>
<copyright-holder>Zhongxin, Xiaoping, Dawei, Ning and Da</copyright-holder>
<license xlink:href="http://creativecommons.org/licenses/by/4.0/">
<p>This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) and the copyright owner(s) are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.</p>
</license>
</permissions>
<abstract>
<p>Underground gas storage (UGS) is the most economical and effective means to guarantee stable gas supply. During gas production process, the evaporation of formation water leads to the increase of water content in the gas, and the salinity of the remaining formation water increases. This work applied numerical simulation to analyze the effect of salt deposition on flowing bottomhole pressure, production capacity and storage capacity. The simulation results show that the minimum and maximum pressure of UGS is more likely to be reached during multi-cycle production under the conditions of salt deposition. Under the initial water condition, reservoir drying can improve the gas storage capacity. At the end of the tenth cycle, the storage capacity increases by 1.4%. It is concluded that the study on the impact of formation water evaporation on storage capacity is helpful for the prevention and control of salt formation water in UGS with high salinity.</p>
</abstract>
<kwd-group>
<kwd>underground gas storage</kwd>
<kwd>salt deposition</kwd>
<kwd>high salinity</kwd>
<kwd>storage capacity</kwd>
<kwd>production capacity</kwd>
</kwd-group>
<custom-meta-wrap>
<custom-meta>
<meta-name>section-at-acceptance</meta-name>
<meta-value>Solid Earth Geophysics</meta-value>
</custom-meta>
</custom-meta-wrap>
</article-meta>
</front>
<body>
<sec id="s1">
<title>1 Introduction</title>
<p>The use of fossil energy is a key factor in environmental change and pollution (<xref ref-type="bibr" rid="B37">Wu et al., 2016</xref>; <xref ref-type="bibr" rid="B19">Liu et al., 2018</xref>; <xref ref-type="bibr" rid="B24">Pachiannan et al., 2019</xref>; <xref ref-type="bibr" rid="B31">Tang et al., 2022</xref>). The large amount of fossil energy consumption causes greenhouse gas emissions, which increase the concentration of greenhouse gases in the atmosphere (<xref ref-type="bibr" rid="B28">Tang et al., 2015</xref>; <xref ref-type="bibr" rid="B10">Han et al., 2017</xref>; <xref ref-type="bibr" rid="B20">Mac Kinnon et al., 2018</xref>; <xref ref-type="bibr" rid="B33">Tong et al., 2020</xref>). Low carbon energy has been recognized as a key means to achieve sustainable development (<xref ref-type="bibr" rid="B7">Dost&#xe1;l and Lad&#xe1;nyi, 2018</xref>). Natural gas is known as a clean energy source that produces less carbon dioxide pollution than other fossil fuels such as coal and oil (<xref ref-type="bibr" rid="B30">Tang et al., 2021a</xref>; <xref ref-type="bibr" rid="B12">Hu et al., 2021</xref>; <xref ref-type="bibr" rid="B11">He et al., 2022</xref>; <xref ref-type="bibr" rid="B44">Zhu et al., 2022</xref>). Compared to conventional energy sources, natural gas has relatively low carbon emissions and is considered an important energy source for the transition to renewable energy (<xref ref-type="bibr" rid="B34">Ullah Khan et al., 2017</xref>; <xref ref-type="bibr" rid="B36">Whiting et al., 2017</xref>; <xref ref-type="bibr" rid="B9">Gillessen et al., 2019</xref>; <xref ref-type="bibr" rid="B40">Zeren and Akku&#x15f;, 2020</xref>). The peak shaving are a challenge for the efficient use of natural gas. UGS peak shaving has the advantages of large storage capacity, good safety, and low storage costs. It is the main and economic way of gas supply peaking method (<xref ref-type="bibr" rid="B5">Chen et al., 2018</xref>; <xref ref-type="bibr" rid="B8">Firme et al., 2019</xref>; <xref ref-type="bibr" rid="B14">Jelu&#x161;i&#x10d; et al., 2019</xref>; <xref ref-type="bibr" rid="B26">Sedaee et al., 2019</xref>; <xref ref-type="bibr" rid="B2">Animah and Shafiee, 2020</xref>).</p>
<p>According to the experience of countries around the world, the use of underground gas storage for regulation is the most effective way to ensure the safe and stable supply of natural gas (<xref ref-type="bibr" rid="B42">Zhang et al., 2020</xref>; <xref ref-type="bibr" rid="B23">Mol&#xed;kov&#xe1; et al., 2022</xref>; <xref ref-type="bibr" rid="B17">Li et al., 2023</xref>). In 2021, China&#x2019;s natural gas consumption reaches 354.2 billion m<sup>3</sup>, up 8.6% compared with 2020. China&#x2019;s natural gas consumption is expected to reach 430 billion m<sup>3</sup> by 2025, with an average annual increment of 21 billion m<sup>3</sup> (<xref ref-type="bibr" rid="B4">Braungardt et al., 2019</xref>; <xref ref-type="bibr" rid="B16">Kvamme and Saeidi, 2021</xref>; <xref ref-type="bibr" rid="B35">Wei et al., 2021</xref>; <xref ref-type="bibr" rid="B44">Zhu et al., 2022</xref>). The construction of UGS has accelerated with the increase in natural gas consumption. Hence, achieving efficient development of UGS has become one of the difficulties faced by the natural gas industry (<xref ref-type="bibr" rid="B38">Xiao et al., 2020</xref>).</p>
<p>Chinese UGS industry started late compared to developed western countries (<xref ref-type="bibr" rid="B41">Zhang et al., 2017</xref>; <xref ref-type="bibr" rid="B3">Bian et al., 2020</xref>). Depleted reservoir UGS is the most common and economical form of UGS. At present, there are more than 400 such reservoirs in the world, covering more than 75% of the total number of UGS. Salt deposition occurs when the initial salinity of formation water is high (<xref ref-type="bibr" rid="B39">Zeidouni et al., 2009</xref>; <xref ref-type="bibr" rid="B27">Spycher and Pruess, 2010</xref>; <xref ref-type="bibr" rid="B1">Andr&#xe9; et al., 2014</xref>; <xref ref-type="bibr" rid="B21">Miri et al., 2014</xref>; <xref ref-type="bibr" rid="B25">Peysson et al., 2014</xref>; <xref ref-type="bibr" rid="B32">Tang et al., 2015</xref>; <xref ref-type="bibr" rid="B22">Miri et al., 2015</xref>; <xref ref-type="bibr" rid="B13">Jeddizahed and Rostami, 2016</xref>; <xref ref-type="bibr" rid="B29">Tang et al., 2021b</xref>). However, the study of salt deposition mainly focuses on the process of CO<sub>2</sub> geological sequestration (<xref ref-type="bibr" rid="B15">Kim et al., 2013</xref>; <xref ref-type="bibr" rid="B6">Cui et al., 2018</xref>; <xref ref-type="bibr" rid="B18">Li et al., 2021</xref>; <xref ref-type="bibr" rid="B43">Zhao et al., 2021</xref>). However, there are few studies on the changes of production capacity and storage capacity due to formation water evaporation after multi-cycle production of UGS. Water evaporation in the reservoir can enhance formation permeability and porosity without formation water supply. The porosity and permeability of the cores after evaporation are elevated compared with the porosity and permeability under initial water saturation conditions, with an average increase of 42% in porosity and 39% in permeability (<xref ref-type="bibr" rid="B31">Tang et al., 2022</xref>). The improved storage volume can be calculated based on the drying radius of the gas well during the production of the gas storage. The drying radius of gas storage is increasing with the increase of production cycle.</p>
<p>This paper analyzes the effect of reservoir salt deposition on bottomhole flow pressure, production capacity and storage capacity based on a numerical model. Taken the Wen23 UGS as an example, the changes in production capacity and storage capacity after multiple-cycle production are studied.</p>
</sec>
<sec id="s2">
<title>2 Building model of salt deposition in reservoir</title>
<p>During the development of the gas reservoir, the pressure drop in the near-wellbore causes the gas to flow towards the well and the water vapor content in the gas phase increases. Salt deposition occurs when the salinity of the formation water reaches its maximum solubility. Evaporation of formation water and salt formation have a major impact on the gas-liquid phase balance and solid phase precipitation in the system, and they also have an impact on gas flow capacity and reservoir storage capacity during gas production.</p>
<sec id="s2-1">
<title>2.1 The water saturation model near-wellbore</title>
<p>
<xref ref-type="fig" rid="F1">Figure 1</xref> shows the schematic diagram of the volume element of the single well model.</p>
<fig id="F1" position="float">
<label>FIGURE 1</label>
<caption>
<p>The schematic diagram of the volume element of the single well model.</p>
</caption>
<graphic xlink:href="feart-12-1362776-g001.tif"/>
</fig>
<p>Pore volume of volume elements within the formation:<disp-formula id="e1">
<mml:math id="m1">
<mml:mrow>
<mml:mo>&#x394;</mml:mo>
<mml:mi>V</mml:mi>
<mml:mo>&#x3d;</mml:mo>
<mml:mn>2</mml:mn>
<mml:mi>&#x3c0;</mml:mi>
<mml:mi>r</mml:mi>
<mml:mi>h</mml:mi>
<mml:mi>&#x3c6;</mml:mi>
<mml:mi mathvariant="normal">d</mml:mi>
<mml:mi>r</mml:mi>
</mml:mrow>
</mml:math>
<label>(1)</label>
</disp-formula>Where &#x25b3;<italic>V</italic> is the pore volume of volume element, cm<sup>3</sup>; <italic>r</italic> is the reservoir radius, cm; <italic>h</italic> is the thickness of reservoir, cm; <italic>&#x3d5;</italic> is the porosity, %.</p>
<p>The amount of change in the volume of the water phase is as follows due to the decrease of water saturation in the system caused by the evaporation of the water phase:<disp-formula id="e2">
<mml:math id="m2">
<mml:mrow>
<mml:mi mathvariant="normal">d</mml:mi>
<mml:msub>
<mml:mi>V</mml:mi>
<mml:mi mathvariant="normal">w</mml:mi>
</mml:msub>
<mml:mo>&#x3d;</mml:mo>
<mml:mn>2</mml:mn>
<mml:mi>&#x3c0;</mml:mi>
<mml:mi>r</mml:mi>
<mml:mi>h</mml:mi>
<mml:mi>&#x3c6;</mml:mi>
<mml:msub>
<mml:mtext>dS</mml:mtext>
<mml:mi mathvariant="normal">w</mml:mi>
</mml:msub>
<mml:mi mathvariant="normal">d</mml:mi>
<mml:mi>r</mml:mi>
</mml:mrow>
</mml:math>
<label>(2)</label>
</disp-formula>Where <italic>V</italic>
<sub>w</sub> is the amount of change in the volume of the water phase, cm<sup>3</sup>; S<sub>w</sub> is the water content saturation, %.</p>
<p>The pressure in the near-well zone decreases, causing evaporation of the aqueous phase and an increase in water saturation as the gas flows through. The water phase change within the volume element can also be expressed as follows:<disp-formula id="e3">
<mml:math id="m3">
<mml:mrow>
<mml:mi mathvariant="normal">d</mml:mi>
<mml:msub>
<mml:mi>V</mml:mi>
<mml:mi mathvariant="normal">w</mml:mi>
</mml:msub>
<mml:mo>&#x3d;</mml:mo>
<mml:mtext>qdtd</mml:mtext>
<mml:mi>&#x3c9;</mml:mi>
</mml:mrow>
</mml:math>
<label>(3)</label>
</disp-formula>Where q is the gas production volume, cm<sup>3</sup>/s; t is the production time, s; &#x3c9; is the saturated content of water vapor in natural gas, cm<sup>3</sup>/cm<sup>3</sup>.</p>
<p>And the content of water vapor in natural gas is as follows:<disp-formula id="e4">
<mml:math id="m4">
<mml:mrow>
<mml:mi>&#x3c9;</mml:mi>
<mml:mo>&#x3d;</mml:mo>
<mml:mi>A</mml:mi>
<mml:msup>
<mml:mi>p</mml:mi>
<mml:mi mathvariant="normal">B</mml:mi>
</mml:msup>
</mml:mrow>
</mml:math>
<label>(4)</label>
</disp-formula>Where <italic>p</italic> is the pressure, MPa; <italic>A</italic> and <italic>B</italic> are the correlation factor.</p>
<p>In steady seepage, the radial pressure drop in a gas well based on Darcy&#x2019;s law is as follows;<disp-formula id="e5">
<mml:math id="m5">
<mml:mrow>
<mml:mfrac>
<mml:mrow>
<mml:mi mathvariant="normal">d</mml:mi>
<mml:mi>p</mml:mi>
</mml:mrow>
<mml:mrow>
<mml:mi mathvariant="normal">d</mml:mi>
<mml:mi>r</mml:mi>
</mml:mrow>
</mml:mfrac>
<mml:mo>&#x3d;</mml:mo>
<mml:mfrac>
<mml:mrow>
<mml:msub>
<mml:mi>&#x3bc;</mml:mi>
<mml:mi mathvariant="normal">g</mml:mi>
</mml:msub>
<mml:msub>
<mml:mi>B</mml:mi>
<mml:mi mathvariant="normal">g</mml:mi>
</mml:msub>
</mml:mrow>
<mml:mrow>
<mml:mn>2</mml:mn>
<mml:mi>&#x3c0;</mml:mi>
<mml:mi>r</mml:mi>
<mml:mi>h</mml:mi>
<mml:mi>K</mml:mi>
<mml:msub>
<mml:mi>K</mml:mi>
<mml:mtext>rg</mml:mtext>
</mml:msub>
</mml:mrow>
</mml:mfrac>
<mml:mi mathvariant="normal">q</mml:mi>
</mml:mrow>
</mml:math>
<label>(5)</label>
</disp-formula>Where <italic>&#x3bc;</italic>
<sub>g</sub> is the viscosity of gas, mPa&#xb7;s; <italic>B</italic>
<sub>g</sub> is the volume factor; <italic>K</italic> is the reservoir permeability, mD; <italic>K</italic>
<sub>rg</sub> is the gas phase relative permeability.</p>
<p>Combining Eqs <xref ref-type="disp-formula" rid="e3">3</xref>&#x2013;<xref ref-type="disp-formula" rid="e5">5</xref>, the following equations are obtained:<disp-formula id="e6">
<mml:math id="m6">
<mml:mrow>
<mml:mfrac>
<mml:mrow>
<mml:mi mathvariant="normal">d</mml:mi>
<mml:msub>
<mml:mi>S</mml:mi>
<mml:mi mathvariant="normal">w</mml:mi>
</mml:msub>
</mml:mrow>
<mml:mtext>dt</mml:mtext>
</mml:mfrac>
<mml:mo>&#x3d;</mml:mo>
<mml:mfrac>
<mml:mrow>
<mml:mi>A</mml:mi>
<mml:mi>B</mml:mi>
<mml:msub>
<mml:mi>&#x3bc;</mml:mi>
<mml:mi mathvariant="normal">g</mml:mi>
</mml:msub>
<mml:msub>
<mml:mi>B</mml:mi>
<mml:mi mathvariant="normal">g</mml:mi>
</mml:msub>
<mml:msup>
<mml:mi mathvariant="normal">q</mml:mi>
<mml:mn>2</mml:mn>
</mml:msup>
<mml:msup>
<mml:mi>p</mml:mi>
<mml:mrow>
<mml:mi mathvariant="normal">B</mml:mi>
<mml:mo>&#x2212;</mml:mo>
<mml:mn>1</mml:mn>
</mml:mrow>
</mml:msup>
</mml:mrow>
<mml:mrow>
<mml:mn>4</mml:mn>
<mml:msup>
<mml:mi>&#x3c0;</mml:mi>
<mml:mn>2</mml:mn>
</mml:msup>
<mml:msup>
<mml:mi>r</mml:mi>
<mml:mn>2</mml:mn>
</mml:msup>
<mml:msup>
<mml:mi>h</mml:mi>
<mml:mn>2</mml:mn>
</mml:msup>
<mml:mi>&#x3c6;</mml:mi>
<mml:mi>K</mml:mi>
<mml:msub>
<mml:mi>K</mml:mi>
<mml:mtext>rg</mml:mtext>
</mml:msub>
</mml:mrow>
</mml:mfrac>
</mml:mrow>
</mml:math>
<label>(6)</label>
</disp-formula>
</p>
<p>The expression of the volume factor is as follows:<disp-formula id="e7">
<mml:math id="m7">
<mml:mrow>
<mml:msub>
<mml:mi>B</mml:mi>
<mml:mi mathvariant="normal">g</mml:mi>
</mml:msub>
<mml:mo>&#x3d;</mml:mo>
<mml:mfrac>
<mml:mrow>
<mml:mi>T</mml:mi>
<mml:msub>
<mml:mi>p</mml:mi>
<mml:mtext>sc</mml:mtext>
</mml:msub>
<mml:mi>Z</mml:mi>
</mml:mrow>
<mml:mrow>
<mml:msub>
<mml:mi>T</mml:mi>
<mml:mtext>sc</mml:mtext>
</mml:msub>
<mml:mi>p</mml:mi>
</mml:mrow>
</mml:mfrac>
</mml:mrow>
</mml:math>
<label>(7)</label>
</disp-formula>
</p>
<p>Combining Eqs <xref ref-type="disp-formula" rid="e6">6</xref>, <xref ref-type="disp-formula" rid="e7">7</xref>, the following equation is obtained:<disp-formula id="e8">
<mml:math id="m8">
<mml:mrow>
<mml:mfrac>
<mml:mrow>
<mml:mi mathvariant="normal">d</mml:mi>
<mml:msub>
<mml:mi>S</mml:mi>
<mml:mi mathvariant="normal">w</mml:mi>
</mml:msub>
</mml:mrow>
<mml:mtext>dt</mml:mtext>
</mml:mfrac>
<mml:mo>&#x3d;</mml:mo>
<mml:mfrac>
<mml:mrow>
<mml:mi>A</mml:mi>
<mml:mi>B</mml:mi>
<mml:msub>
<mml:mi>&#x3bc;</mml:mi>
<mml:mi mathvariant="normal">g</mml:mi>
</mml:msub>
<mml:mi>T</mml:mi>
<mml:msub>
<mml:mi>p</mml:mi>
<mml:mtext>sc</mml:mtext>
</mml:msub>
<mml:msup>
<mml:mtext>Zq</mml:mtext>
<mml:mn>2</mml:mn>
</mml:msup>
<mml:msup>
<mml:mi>p</mml:mi>
<mml:mrow>
<mml:mi mathvariant="normal">B</mml:mi>
<mml:mo>&#x2212;</mml:mo>
<mml:mn>2</mml:mn>
</mml:mrow>
</mml:msup>
</mml:mrow>
<mml:mrow>
<mml:mn>4</mml:mn>
<mml:msup>
<mml:mi>&#x3c0;</mml:mi>
<mml:mn>2</mml:mn>
</mml:msup>
<mml:msup>
<mml:mi>r</mml:mi>
<mml:mn>2</mml:mn>
</mml:msup>
<mml:msup>
<mml:mi>h</mml:mi>
<mml:mn>2</mml:mn>
</mml:msup>
<mml:mi>&#x3c6;</mml:mi>
<mml:msub>
<mml:mi>T</mml:mi>
<mml:mtext>sc</mml:mtext>
</mml:msub>
<mml:mi>K</mml:mi>
<mml:msub>
<mml:mi>K</mml:mi>
<mml:mtext>rg</mml:mtext>
</mml:msub>
</mml:mrow>
</mml:mfrac>
</mml:mrow>
</mml:math>
<label>(8)</label>
</disp-formula>
</p>
<p>The formation water has a certain salinity, the presence of salt inhibits the evaporation of the water phase, reducing the water vapor content in the gas phase, according to Morin&#x2019;s theory, certain modifications to Eq <xref ref-type="disp-formula" rid="e8">8</xref>:<disp-formula id="e9">
<mml:math id="m9">
<mml:mrow>
<mml:mfrac>
<mml:mrow>
<mml:mi mathvariant="normal">d</mml:mi>
<mml:msub>
<mml:mi>S</mml:mi>
<mml:mi mathvariant="normal">w</mml:mi>
</mml:msub>
</mml:mrow>
<mml:mtext>dt</mml:mtext>
</mml:mfrac>
<mml:mo>&#x3d;</mml:mo>
<mml:mfrac>
<mml:mrow>
<mml:mi>A</mml:mi>
<mml:mi>B</mml:mi>
<mml:msub>
<mml:mi>&#x3bc;</mml:mi>
<mml:mi mathvariant="normal">g</mml:mi>
</mml:msub>
<mml:mi>T</mml:mi>
<mml:msub>
<mml:mi>p</mml:mi>
<mml:mtext>sc</mml:mtext>
</mml:msub>
<mml:msup>
<mml:mtext>Zq</mml:mtext>
<mml:mn>2</mml:mn>
</mml:msup>
<mml:msup>
<mml:mi>p</mml:mi>
<mml:mrow>
<mml:mi mathvariant="normal">B</mml:mi>
<mml:mo>&#x2212;</mml:mo>
<mml:mn>2</mml:mn>
</mml:mrow>
</mml:msup>
</mml:mrow>
<mml:mrow>
<mml:mn>4</mml:mn>
<mml:msup>
<mml:mi>&#x3c0;</mml:mi>
<mml:mn>2</mml:mn>
</mml:msup>
<mml:msup>
<mml:mi>r</mml:mi>
<mml:mn>2</mml:mn>
</mml:msup>
<mml:msup>
<mml:mi>h</mml:mi>
<mml:mn>2</mml:mn>
</mml:msup>
<mml:mi>&#x3c6;</mml:mi>
<mml:msub>
<mml:mi>T</mml:mi>
<mml:mtext>sc</mml:mtext>
</mml:msub>
<mml:mi>K</mml:mi>
<mml:msub>
<mml:mi>K</mml:mi>
<mml:mtext>rg</mml:mtext>
</mml:msub>
<mml:mrow>
<mml:mfenced open="(" close=")" separators="|">
<mml:mrow>
<mml:mn>1</mml:mn>
<mml:mo>&#x2212;</mml:mo>
<mml:mn>0.02865</mml:mn>
<mml:msup>
<mml:mi mathvariant="normal">c</mml:mi>
<mml:mn>1.44</mml:mn>
</mml:msup>
</mml:mrow>
</mml:mfenced>
</mml:mrow>
</mml:mrow>
</mml:mfrac>
</mml:mrow>
</mml:math>
<label>(9)</label>
</disp-formula>Where c is the molar concentration of salt in formation water, mol/L.</p>
<p>The value of c is mainly based on whether the formation water is in a saturated state during salt deposition, and c is expressed as follows:<disp-formula id="e10">
<mml:math id="m10">
<mml:mrow>
<mml:mi mathvariant="normal">c</mml:mi>
<mml:mo>&#x3d;</mml:mo>
<mml:mrow>
<mml:mfenced open="{" close="" separators="|">
<mml:mrow>
<mml:mtable columnalign="left">
<mml:mtr>
<mml:mtd>
<mml:mrow>
<mml:mfrac>
<mml:mrow>
<mml:msub>
<mml:mi>S</mml:mi>
<mml:mtext>wi</mml:mtext>
</mml:msub>
</mml:mrow>
<mml:mrow>
<mml:msub>
<mml:mi>S</mml:mi>
<mml:mi mathvariant="normal">w</mml:mi>
</mml:msub>
</mml:mrow>
</mml:mfrac>
<mml:msub>
<mml:mi>c</mml:mi>
<mml:mi mathvariant="normal">i</mml:mi>
</mml:msub>
</mml:mrow>
</mml:mtd>
</mml:mtr>
<mml:mtr>
<mml:mtd>
<mml:msub>
<mml:mi>c</mml:mi>
<mml:mi mathvariant="normal">c</mml:mi>
</mml:msub>
</mml:mtd>
</mml:mtr>
</mml:mtable>
</mml:mrow>
</mml:mfenced>
</mml:mrow>
<mml:mtable columnalign="left">
<mml:mtr>
<mml:mtd>
<mml:mrow>
<mml:msub>
<mml:mi>c</mml:mi>
<mml:mi mathvariant="normal">i</mml:mi>
</mml:msub>
<mml:mo>&#x3c;</mml:mo>
<mml:msub>
<mml:mi>c</mml:mi>
<mml:mi mathvariant="normal">c</mml:mi>
</mml:msub>
</mml:mrow>
</mml:mtd>
</mml:mtr>
<mml:mtr>
<mml:mtd>
<mml:mrow>
<mml:msub>
<mml:mi>c</mml:mi>
<mml:mi mathvariant="normal">i</mml:mi>
</mml:msub>
<mml:mo>&#x2265;</mml:mo>
<mml:msub>
<mml:mi>c</mml:mi>
<mml:mi mathvariant="normal">c</mml:mi>
</mml:msub>
</mml:mrow>
</mml:mtd>
</mml:mtr>
</mml:mtable>
</mml:mrow>
</mml:math>
<label>(10)</label>
</disp-formula>Where <italic>c</italic>
<sub>i</sub> is the molar concentration of salt in formation water under initial conditions, mol/L; <italic>c</italic>
<sub>c</sub> is the molar concentration of salt when the formation is saturated with water, mol/L; <italic>S</italic>
<sub>wi</sub> is the initial water content saturation, %.</p>
</sec>
<sec id="s2-2">
<title>2.2 Water saturation model in the near-wellbore considering evaporation of formation water</title>
<p>Water vapor content in the gas phase is related to temperature, pressure and salinity. During the flow of gas to the wellbore, the pressure gradually decreases and the water vapor content in the gas phase increases. The salinity of the formation water around the wellbore increases, and even salt deposition occurs. Assume that no transport of formation water occurs in the reservoir, so the salt ion content remains constant at any point in the formation:<disp-formula id="e11">
<mml:math id="m11">
<mml:mrow>
<mml:msub>
<mml:mi>S</mml:mi>
<mml:mtext>wi</mml:mtext>
</mml:msub>
<mml:mo>&#xd7;</mml:mo>
<mml:msub>
<mml:mi>C</mml:mi>
<mml:mi mathvariant="normal">i</mml:mi>
</mml:msub>
<mml:mo>&#x3d;</mml:mo>
<mml:mi>C</mml:mi>
<mml:mi>o</mml:mi>
<mml:mi>n</mml:mi>
<mml:mi>s</mml:mi>
<mml:mi>t</mml:mi>
</mml:mrow>
</mml:math>
<label>(11)</label>
</disp-formula>
</p>
<p>As the pressure decreases, evaporation of formation water accelerates and the salinity of formation water will change<disp-formula id="e12">
<mml:math id="m12">
<mml:mrow>
<mml:msub>
<mml:mi>S</mml:mi>
<mml:mtext>wi</mml:mtext>
</mml:msub>
<mml:mo>&#xd7;</mml:mo>
<mml:msub>
<mml:mi>C</mml:mi>
<mml:mi mathvariant="normal">i</mml:mi>
</mml:msub>
<mml:mo>&#x3d;</mml:mo>
<mml:msub>
<mml:mi>S</mml:mi>
<mml:mrow>
<mml:mtext>wi</mml:mtext>
<mml:mo>&#x2b;</mml:mo>
<mml:mn>1</mml:mn>
</mml:mrow>
</mml:msub>
<mml:mo>&#xd7;</mml:mo>
<mml:msub>
<mml:mi>C</mml:mi>
<mml:mrow>
<mml:mi mathvariant="normal">i</mml:mi>
<mml:mo>&#x2b;</mml:mo>
<mml:mn>1</mml:mn>
</mml:mrow>
</mml:msub>
</mml:mrow>
</mml:math>
<label>(12)</label>
</disp-formula>
</p>
<p>Therefore, the salinity of the formation water under a certain moment is as follows:<disp-formula id="e13">
<mml:math id="m13">
<mml:mrow>
<mml:msub>
<mml:mi>C</mml:mi>
<mml:mrow>
<mml:mi mathvariant="normal">i</mml:mi>
<mml:mo>&#x2b;</mml:mo>
<mml:mn>1</mml:mn>
</mml:mrow>
</mml:msub>
<mml:mo>&#x3d;</mml:mo>
<mml:mfrac>
<mml:mrow>
<mml:msub>
<mml:mi>S</mml:mi>
<mml:mtext>wi</mml:mtext>
</mml:msub>
<mml:mo>&#xd7;</mml:mo>
<mml:msub>
<mml:mi>C</mml:mi>
<mml:mi mathvariant="normal">i</mml:mi>
</mml:msub>
</mml:mrow>
<mml:msub>
<mml:mi>S</mml:mi>
<mml:mrow>
<mml:mtext>wi</mml:mtext>
<mml:mo>&#x2b;</mml:mo>
<mml:mn>1</mml:mn>
</mml:mrow>
</mml:msub>
</mml:mfrac>
</mml:mrow>
</mml:math>
<label>(13)</label>
</disp-formula>
</p>
<p>Salt deposition occurs in the formation when <italic>C</italic> &#x3e; <italic>C</italic>
<sub>critical</sub>.</p>
<p>Where <italic>S</italic>
<sub>wi</sub> is the water content saturation at moment i, %; <italic>S</italic>
<sub>wi&#x2b;1</sub> is the water content saturation at moment i&#x2b;1, %; <italic>C</italic>
<sub>i</sub> is the salinity of formation water at moment i, mol/L; <italic>C</italic>
<sub>i&#x2b;1</sub> is the salinity of formation water at moment i&#x2b;1, mol/L; <italic>Const</italic> is the constant.</p>
<p>The p, <italic>C</italic>
<sub>i</sub>, <italic>S</italic>
<sub>wi</sub> at time i is brought into the Eq <xref ref-type="disp-formula" rid="e13">13</xref> to obtain the salinity of the formation water at time i&#x2b;1. The phase software is used to calculate the solubility of NaCl at different pressure and salinity, and when the salinity of the formation water exceeds the solubility of NaCl, which is used to determine the values <italic>C</italic>
<sub>i</sub> in Eq <xref ref-type="disp-formula" rid="e13">13</xref> at different times:<disp-formula id="e14">
<mml:math id="m14">
<mml:mrow>
<mml:msub>
<mml:mi>C</mml:mi>
<mml:mrow>
<mml:mi mathvariant="normal">i</mml:mi>
<mml:mo>&#x2b;</mml:mo>
<mml:mn>1</mml:mn>
</mml:mrow>
</mml:msub>
<mml:mo>&#x3d;</mml:mo>
<mml:mfrac>
<mml:mrow>
<mml:msub>
<mml:mi>S</mml:mi>
<mml:mtext>wi</mml:mtext>
</mml:msub>
<mml:mo>&#xd7;</mml:mo>
<mml:msub>
<mml:mi>C</mml:mi>
<mml:mi mathvariant="normal">i</mml:mi>
</mml:msub>
</mml:mrow>
<mml:mrow>
<mml:mfrac>
<mml:mn>1</mml:mn>
<mml:mrow>
<mml:mo>&#x2212;</mml:mo>
<mml:mn>0.53</mml:mn>
</mml:mrow>
</mml:mfrac>
<mml:mrow>
<mml:mfenced open="[" close="]" separators="|">
<mml:mrow>
<mml:mi>ln</mml:mi>
<mml:mrow>
<mml:mfenced open="(" close=")" separators="|">
<mml:mrow>
<mml:mfrac>
<mml:mrow>
<mml:mn>0.53</mml:mn>
<mml:mi>A</mml:mi>
<mml:mi>B</mml:mi>
<mml:msub>
<mml:mi mathvariant="normal">&#x3bc;</mml:mi>
<mml:mi mathvariant="normal">g</mml:mi>
</mml:msub>
<mml:mi>T</mml:mi>
<mml:msub>
<mml:mi>p</mml:mi>
<mml:mtext>sc</mml:mtext>
</mml:msub>
<mml:msup>
<mml:mtext>Zq</mml:mtext>
<mml:mn>2</mml:mn>
</mml:msup>
<mml:msup>
<mml:mi>p</mml:mi>
<mml:mrow>
<mml:mi>B</mml:mi>
<mml:mo>&#x2212;</mml:mo>
<mml:mn>2</mml:mn>
</mml:mrow>
</mml:msup>
</mml:mrow>
<mml:mrow>
<mml:mn>4</mml:mn>
<mml:msup>
<mml:mi>&#x3c0;</mml:mi>
<mml:mn>2</mml:mn>
</mml:msup>
<mml:msup>
<mml:mi>r</mml:mi>
<mml:mn>2</mml:mn>
</mml:msup>
<mml:msup>
<mml:mi>h</mml:mi>
<mml:mn>2</mml:mn>
</mml:msup>
<mml:mi mathvariant="normal">&#x3c6;</mml:mi>
<mml:msub>
<mml:mi>T</mml:mi>
<mml:mtext>sc</mml:mtext>
</mml:msub>
<mml:mi>K</mml:mi>
<mml:mrow>
<mml:mfenced open="(" close=")" separators="|">
<mml:mrow>
<mml:mn>1</mml:mn>
<mml:mo>&#x2212;</mml:mo>
<mml:mn>0.02865</mml:mn>
<mml:msup>
<mml:msub>
<mml:mi>C</mml:mi>
<mml:mi mathvariant="normal">i</mml:mi>
</mml:msub>
<mml:mn>1.44</mml:mn>
</mml:msup>
</mml:mrow>
</mml:mfenced>
</mml:mrow>
</mml:mrow>
</mml:mfrac>
<mml:msub>
<mml:mi mathvariant="normal">t</mml:mi>
<mml:mrow>
<mml:mi mathvariant="normal">i</mml:mi>
<mml:mo>&#x2b;</mml:mo>
<mml:mn>1</mml:mn>
</mml:mrow>
</mml:msub>
<mml:mo>&#x2b;</mml:mo>
<mml:mn>4.65</mml:mn>
</mml:mrow>
</mml:mfenced>
</mml:mrow>
<mml:mo>&#x2212;</mml:mo>
<mml:mn>1.75</mml:mn>
</mml:mrow>
</mml:mfenced>
</mml:mrow>
</mml:mrow>
</mml:mfrac>
</mml:mrow>
</mml:math>
<label>(14)</label>
</disp-formula>
</p>
<p>The formation salt deposition model is more complex, and the solution needs to rely on numerical simulation software before it can be calculated. The idea of solving the near-well water content saturation distribution model is shown in <xref ref-type="fig" rid="F2">Figure 2</xref>.</p>
<fig id="F2" position="float">
<label>FIGURE 2</label>
<caption>
<p>The idea of solving the near-well water content saturation distribution model.</p>
</caption>
<graphic xlink:href="feart-12-1362776-g002.tif"/>
</fig>
</sec>
</sec>
<sec id="s3">
<title>3 Numerical simulation model of single well</title>
<p>The numerical simulation software CMG is used to model the radial mechanism of a single well with multi-cycle production UGS. This model can be used to study the effect of water evaporation and salt deposition on production capacity and reservoir capacity in UGS.</p>
<sec id="s3-1">
<title>3.1 Rock physical properties, fluid properties and phase parameters</title>
<p>To simplify the simulation, pure CH<sub>4</sub> is used for both the formation fluid and injection gas composition for the simulation. The model mainly considers the effect of salt deposition on the production capacity and storage capacity of UGS. Na<sup>&#x2b;</sup> and Cl<sup>&#x2212;</sup> in the formation water are supersaturated to precipitate NaCl crystals. NaCl crystals affect the reservoir properties by depositing in the pore space. The main chemical reaction equation is shown in Eq <xref ref-type="disp-formula" rid="e15">15</xref>.<disp-formula id="e15">
<mml:math id="m15">
<mml:mrow>
<mml:msup>
<mml:mtext>Na</mml:mtext>
<mml:mo>&#x2b;</mml:mo>
</mml:msup>
<mml:mo>&#x2b;</mml:mo>
<mml:msup>
<mml:mtext>Cl</mml:mtext>
<mml:mo>&#x2212;</mml:mo>
</mml:msup>
<mml:mo>&#x21d4;</mml:mo>
<mml:mtext>NaCl</mml:mtext>
</mml:mrow>
</mml:math>
<label>(15)</label>
</disp-formula>
</p>
<p>Salt deposition and evaporation of formation water can lead to changes in reservoir porosity and permeability. The pore-permeability relationship is given by the experimental data.<disp-formula id="e16">
<mml:math id="m16">
<mml:mrow>
<mml:mi mathvariant="normal">K</mml:mi>
<mml:mo>&#x3d;</mml:mo>
<mml:mn>0.0016</mml:mn>
<mml:msup>
<mml:mi mathvariant="normal">e</mml:mi>
<mml:mrow>
<mml:mn>55.281</mml:mn>
<mml:mi>&#x3d5;</mml:mi>
</mml:mrow>
</mml:msup>
</mml:mrow>
</mml:math>
<label>(16)</label>
</disp-formula>
</p>
<p>The relative permeability curve is taken from laboratory long core experiments. The relative permeability is shown as in <xref ref-type="fig" rid="F3">Figure 3</xref>.</p>
<fig id="F3" position="float">
<label>FIGURE 3</label>
<caption>
<p>Gas-water relative permeability curve.</p>
</caption>
<graphic xlink:href="feart-12-1362776-g003.tif"/>
</fig>
</sec>
<sec id="s3-2">
<title>3.2 Basic program setting</title>
<p>In order to study the effect of formation salt formation caused by formation water evaporation on the production and storage capacity of gas storage, the radial mechanism model of multi-cycle injection and production single well of gas storage was established by using numerical simulation software CMG. The model grid was divided into 10&#xd7;1&#xd7;5, and the radial mesh size was 1m, 2m, 3m, 5m, 8m, 13m, 21m, 34m, 40 m and 47 m, respectively. The layer is 40 m thick and 200 m longitudinally. The grid plane distribution and three-dimensional distribution are shown in <xref ref-type="fig" rid="F4">Figure 4</xref>. The reservoir parameters are set according to the field data of the gas reservoir. The average permeability is 10.66mD, the average porosity is 11.16%, the bound water saturation is 0.35, and the formation water salinity is 300000ppm. <xref ref-type="table" rid="T1">Table 1</xref> shows the parameters used in modeling and their values.</p>
<fig id="F4" position="float">
<label>FIGURE 4</label>
<caption>
<p>Numerical model grid division diagram.</p>
</caption>
<graphic xlink:href="feart-12-1362776-g004.tif"/>
</fig>
<table-wrap id="T1" position="float">
<label>TABLE 1</label>
<caption>
<p>Model setting parameters.</p>
</caption>
<table>
<thead valign="top">
<tr>
<th align="center">Parameter</th>
<th align="center">Value</th>
</tr>
</thead>
<tbody valign="top">
<tr>
<td align="center">Permeability (mD)</td>
<td align="center">10.66</td>
</tr>
<tr>
<td align="center">Porosity (%)</td>
<td align="center">11.16</td>
</tr>
<tr>
<td align="center">Bound water saturation</td>
<td align="center">0.35</td>
</tr>
<tr>
<td align="center">Thickness (m)</td>
<td align="center">200</td>
</tr>
<tr>
<td align="center">Radius(m)</td>
<td align="center">120</td>
</tr>
<tr>
<td align="center">Current formation pressure (MPa)</td>
<td align="center">4</td>
</tr>
<tr>
<td align="center">Upper operating pressure (MPa)</td>
<td align="center">38.6</td>
</tr>
<tr>
<td align="center">Lower operating pressure (MPa)</td>
<td align="center">20</td>
</tr>
<tr>
<td align="center">Gas reservoir temperature (&#xb0;C)</td>
<td align="center">120</td>
</tr>
<tr>
<td align="center">Formation water salinity (mg/L)</td>
<td align="center">300000</td>
</tr>
</tbody>
</table>
</table-wrap>
<p>A well of UGS is set up in the middle of the model, and all layers are shot open. The basic program is set up in 2 phases, including cushion gas stage and UGS multi-cycle production stage.<list list-type="simple">
<list-item>
<p>(1) Cushion gas stage: The gas injection volume of single well is about 400,000 m<sup>3</sup>/d.</p>
</list-item>
<list-item>
<p>(2) UGS multi-cycle production stage: In this stage, UGS is injected to the maximum pressure of 38 MPa, then gas is exploited to the minimum pressure of 20 MPa. The maximum injection volume and maximum gas extraction volume are both 600,000 m<sup>3</sup>/d in a single cycle. The natural gas is injected in the UGS from July to December and extracted from January to June every year. This work can predict the changes in production capacity and storage capacity after multiple-cycle production by simulating salt deposition in the near-wellbore.</p>
</list-item>
</list>
</p>
</sec>
</sec>
<sec id="s4">
<title>4 Analysis of salt deposition</title>
<p>The model is calculated separately for two sets of schemes, including considering salt deposition and not considering salt deposition. The rest of the model conditions are the same. The results of the two schemes are compared to analyze the gas production capacity.</p>
<sec id="s4-1">
<title>4.1 Effect of salt deposition on bottomhole pressure</title>
<p>The bottomhole pressures in injection wells and production wells are shown in <xref ref-type="fig" rid="F5">Figures 5</xref>, <xref ref-type="fig" rid="F6">6</xref>. There is no significant change in bottom flow pressures in injection wells and production wells without considering salt deposition. In the condition of considering salt deposition, the bottom flow pressures of injection well rise to the maximum pressure as the production cycle increases. The reason for this phenomenon is that salt deposition is more severe in the near-well zone and a larger pressure is required to inject the same amount of gas. Similarly, the bottom flow pressure of injection well reaches the minimum pressure earlier without considering salt deposition.</p>
<fig id="F5" position="float">
<label>FIGURE 5</label>
<caption>
<p>Comparison of bottomhole flow pressure in considering salt deposition conditions and without considering salt deposition conditions of injection well.</p>
</caption>
<graphic xlink:href="feart-12-1362776-g005.tif"/>
</fig>
<fig id="F6" position="float">
<label>FIGURE 6</label>
<caption>
<p>Comparison of bottomhole flow pressure in considering salt deposition conditions and without considering salt deposition conditions of production well.</p>
</caption>
<graphic xlink:href="feart-12-1362776-g006.tif"/>
</fig>
</sec>
<sec id="s4-2">
<title>4.2 Effect of salt deposition on production capacity</title>
<p>The impact of salt deposition on production capacity of gas well can be divided into two parts. Firstly, the evaporation of formation water increases the flow space and the flow capacity of gas, thus increasing the production capacity. In addition, salt crystals can block the pores in the formation and reduce the production capacity of the gas well. These two mechanisms affect the production capacity of gas well.</p>
<p>Two scenarios with different conditions are calculated in this work. The first is a comparison of the effect of salt deposition on gas well production capacity under considering water evaporation conditions and without considering water evaporation conditions. Then this work investigates the effect of salt deposition on gas well production capacity with formation water supplement. The results are shown in <xref ref-type="fig" rid="F7">Figure 7</xref>. The evaporation of formation water increases the gas phase flow capacity without formation water supply.</p>
<fig id="F7" position="float">
<label>FIGURE 7</label>
<caption>
<p>Comparison of cumulative gas production under different water production conditions without considering movable water.</p>
</caption>
<graphic xlink:href="feart-12-1362776-g007.tif"/>
</fig>
<p>The comparison of cumulative gas production under different water production conditions with considering movable water is shown in <xref ref-type="fig" rid="F8">Figure 8</xref>. The damage of salt deposition gradually increases and the production capacity of gas wells is severely reduced under the conditions of formation water supplement.</p>
<fig id="F8" position="float">
<label>FIGURE 8</label>
<caption>
<p>Comparison of cumulative gas production under different water production conditions with considering movable water.</p>
</caption>
<graphic xlink:href="feart-12-1362776-g008.tif"/>
</fig>
</sec>
<sec id="s4-3">
<title>4.3 Effect of salt deposition on storage capacity</title>
<p>A pressure drop funnel is formed in the near-wellbore during production of a gas well. The natural gas in the reservoir evaporates the formation water causing ion oversaturation during the gas from the far-end to the bottom of the well, resulting in salt deposition., The dry gas flows from the bottom of the well to the far-end and evaporates formation water during the gas injection process. More space can be used to store natural gas, enhancing the storage capacity of the UGS.</p>
<p>The drying volume is the volume of evaporation of formation water under reservoir conditions. The proportion of increase in geological reserves is the percentage of increased reserves to the control reserves of a single well. The calculation methods of the drying volume and the proportion of increase in geological reserves are as follows.<disp-formula id="e17">
<mml:math id="m17">
<mml:mrow>
<mml:msub>
<mml:mi>V</mml:mi>
<mml:mi mathvariant="normal">m</mml:mi>
</mml:msub>
<mml:mo>&#x3d;</mml:mo>
<mml:mi>&#x3c0;</mml:mi>
<mml:msup>
<mml:mi>r</mml:mi>
<mml:mn>2</mml:mn>
</mml:msup>
<mml:mi>h</mml:mi>
<mml:msub>
<mml:mi>S</mml:mi>
<mml:mi mathvariant="normal">w</mml:mi>
</mml:msub>
</mml:mrow>
</mml:math>
<label>(17)</label>
</disp-formula>where <italic>V</italic>
<sub>m</sub> is the drying volume, &#x201c;<italic>r</italic>&#x201d; is the drying radius, &#x201c;<italic>h</italic>&#x201d; is the thickness of reservoir and <italic>S</italic>
<sub>w</sub> is the initial water saturation.<disp-formula id="e18">
<mml:math id="m18">
<mml:mrow>
<mml:msub>
<mml:mi>V</mml:mi>
<mml:mi mathvariant="normal">p</mml:mi>
</mml:msub>
<mml:mo>&#x3d;</mml:mo>
<mml:mfrac>
<mml:mrow>
<mml:msub>
<mml:mi>V</mml:mi>
<mml:mi mathvariant="normal">m</mml:mi>
</mml:msub>
</mml:mrow>
<mml:mrow>
<mml:msub>
<mml:mi>B</mml:mi>
<mml:mi mathvariant="normal">g</mml:mi>
</mml:msub>
</mml:mrow>
</mml:mfrac>
</mml:mrow>
</mml:math>
<label>(18)</label>
</disp-formula>where <italic>V</italic>
<sub>p</sub> is the volume of natural gas underground conditions and &#x201c;<italic>B</italic>
<sub>g</sub>&#x201d; is the volume factor of natural gas.<disp-formula id="e19">
<mml:math id="m19">
<mml:mrow>
<mml:mi>K</mml:mi>
<mml:mo>&#x3d;</mml:mo>
<mml:mfrac>
<mml:mrow>
<mml:msub>
<mml:mi>V</mml:mi>
<mml:mi mathvariant="normal">p</mml:mi>
</mml:msub>
</mml:mrow>
<mml:mrow>
<mml:mi>G</mml:mi>
</mml:mrow>
</mml:mfrac>
</mml:mrow>
</mml:math>
<label>(19)</label>
</disp-formula>where <italic>K</italic> is the proportion of increase in geological reserves and &#x201c;<italic>G</italic>&#x201d; is geological reserves of natural gas.</p>
<p>
<xref ref-type="table" rid="T2">Table 2</xref> shows the calculation results of the drying volume, working gas volume and geological reserves with the various production cycle. The drying radius of reservoir is expanding with the increase of production cycle under initial water saturation conditions. The working gas volume increased by 5.4&#xd7;10<sup>6</sup> m<sup>3</sup> by the tenth cycle. The geological reserves increased by 1.4% compared to the control reserves of single well.</p>
<table-wrap id="T2" position="float">
<label>TABLE 2</label>
<caption>
<p>The calculation results of the drying volume, working gas volume and the proportion of increase in geological reserves with the various production cycle.</p>
</caption>
<table>
<thead valign="top">
<tr>
<th align="center">Production cycle</th>
<th align="center">The drying volume (10<sup>4</sup>m<sup>3</sup>)</th>
<th align="center">The increase of working gas volume (10<sup>6</sup>m<sup>3</sup>)</th>
<th align="center">The proportion of increase in geological reserves (%)</th>
</tr>
</thead>
<tbody valign="top">
<tr>
<td align="center">Cushion gas stage</td>
<td align="center">0.31</td>
<td align="center">0.84</td>
<td align="center">0.22</td>
</tr>
<tr>
<td align="center">The first cycle</td>
<td align="center">0.52</td>
<td align="center">1.41</td>
<td align="center">0.37</td>
</tr>
<tr>
<td align="center">The second cycle</td>
<td align="center">0.68</td>
<td align="center">1.87</td>
<td align="center">0.50</td>
</tr>
<tr>
<td align="center">The third cycle</td>
<td align="center">0.85</td>
<td align="center">2.32</td>
<td align="center">0.61</td>
</tr>
<tr>
<td align="center">The fourth cycle</td>
<td align="center">1.06</td>
<td align="center">2.90</td>
<td align="center">0.77</td>
</tr>
<tr>
<td align="center">The fifth cycle</td>
<td align="center">1.21</td>
<td align="center">3.30</td>
<td align="center">0.88</td>
</tr>
<tr>
<td align="center">The sixth cycle</td>
<td align="center">1.35</td>
<td align="center">3.70</td>
<td align="center">0.98</td>
</tr>
<tr>
<td align="center">The seventh cycle</td>
<td align="center">1.48</td>
<td align="center">4.06</td>
<td align="center">1.08</td>
</tr>
<tr>
<td align="center">The eighth cycle</td>
<td align="center">1.65</td>
<td align="center">4.50</td>
<td align="center">1.19</td>
</tr>
<tr>
<td align="center">The ninth cycle</td>
<td align="center">1.81</td>
<td align="center">4.96</td>
<td align="center">1.32</td>
</tr>
<tr>
<td align="center">The tenth cycle</td>
<td align="center">1.99</td>
<td align="center">5.44</td>
<td align="center">1.44</td>
</tr>
</tbody>
</table>
</table-wrap>
</sec>
<sec id="s4-4">
<title>4.4 Effect of production rates</title>
<p>Four groups of schemes were set, and salt formation damage under different production rates was studied by comparing the daily production rates (20, 40, 60 and 80&#xd7;10<sup>4</sup> m<sup>3</sup>/d), the salinity was 300000ppm, the lower limit of bottom-hole flow pressure in production Wells was 20MPa, and the upper limit of gas injection Wells was 38.6 MPa.</p>
<p>The cumulative gas production curves under different production rates are shown in <xref ref-type="fig" rid="F9">Figures 9</xref>&#x2013;<xref ref-type="fig" rid="F12">12</xref>. When the production rate is 40&#xd7;10<sup>4</sup> m<sup>3</sup>/d, there is no significant change in cumulative gas production. When the output is 60&#xd7;10<sup>4</sup> m<sup>3</sup>/d, there is a significant decrease in daily gas production in the 7th cycle. When the yield was 80&#xd7;10<sup>4</sup> m<sup>3</sup>/d, the salt formation damage was aggravated in the 5th cycle. As shown in <xref ref-type="fig" rid="F12">Figure 12</xref>, the cumulative gas production capacity decline rate histogram shows that when the production is 60&#xd7;10<sup>4</sup> m<sup>3</sup>/d, the gas production capacity decline rate rises to 22.89% after ten cycles, and the salt formation damage is serious. The conclusions are as follows: the higher the production, the greater the salt formation risk and the more serious the formation salt formation. When the production is greater than 60&#xd7;10<sup>4</sup> m<sup>3</sup>/d, the daily gas capacity decreases significantly and the salt formation is serious. Low gas production is conducive to controlling the risk of salt formation, and it is recommended to produce less than 60&#xd7;10<sup>4</sup> m<sup>3</sup>/d.</p>
<fig id="F9" position="float">
<label>FIGURE 9</label>
<caption>
<p>Cumulative gas production curve at a production rate of 80&#xd7;10<sup>4</sup> m<sup>3</sup>/d.</p>
</caption>
<graphic xlink:href="feart-12-1362776-g009.tif"/>
</fig>
<fig id="F10" position="float">
<label>FIGURE 10</label>
<caption>
<p>Cumulative gas production curve at a production rate of 60&#xd7;10<sup>4</sup> m<sup>3</sup>/d.</p>
</caption>
<graphic xlink:href="feart-12-1362776-g010.tif"/>
</fig>
<fig id="F11" position="float">
<label>FIGURE 11</label>
<caption>
<p>Cumulative gas production curve at a production rate of 40&#xd7;10<sup>4</sup> m<sup>3</sup>/d.</p>
</caption>
<graphic xlink:href="feart-12-1362776-g011.tif"/>
</fig>
<fig id="F12" position="float">
<label>FIGURE 12</label>
<caption>
<p>Histogram of gas production capacity decline rate.</p>
</caption>
<graphic xlink:href="feart-12-1362776-g012.tif"/>
</fig>
</sec>
</sec>
<sec sec-type="conclusion" id="s5">
<title>5 Conclusion</title>
<p>In this work, numerical simulation is performed to analyze the effect of salt deposition on flowing bottomhole pressure, production capacity and storage capacity in UGS.<list list-type="simple">
<list-item>
<p>(1) Salt deposition makes the buttonhole pressure of the well more dramatic, and the minimum and maximum pressure of UGS is more likely to be reached during multi-cycle production under the conditions of salt deposition.</p>
</list-item>
<list-item>
<p>(2) The evaporation of formation water increases the gas phase flow capacity without formation water supply. The damage of salt deposition gradually increases and the production capacity of gas wells is severely reduced under the conditions of formation water supplement.</p>
</list-item>
<list-item>
<p>(3) The working gas volume increased by 5.4&#xd7;10<sup>6</sup> m<sup>3</sup> by the tenth cycle. The geological reserves increased by 1.4% compared to the control reserves of single well.</p>
</list-item>
</list>
</p>
</sec>
</body>
<back>
<sec sec-type="data-availability" id="s6">
<title>Data availability statement</title>
<p>The raw data supporting the conclusion of this article will be made available by the authors, without undue reservation.</p>
</sec>
<sec id="s7">
<title>Author contributions</title>
<p>ZR: Writing&#x2013;review and editing.</p>
</sec>
<sec sec-type="funding-information" id="s8">
<title>Funding</title>
<p>The author(s) declare that no financial support was received for the research, authorship, and/or publication of this article.</p>
</sec>
<sec sec-type="COI-statement" id="s9">
<title>Conflict of interest</title>
<p>Authors RZ, YX, CD, and MD were employed by National Oil and Gas Pipeline Network Group.</p>
<p>The remaining author declares that the research was conducted in the absence of any commercial or financial relationships that could be construed as a potential conflict of interest.</p>
</sec>
<sec sec-type="disclaimer" id="s10">
<title>Publisher&#x2019;s note</title>
<p>All claims expressed in this article are solely those of the authors and do not necessarily represent those of their affiliated organizations, or those of the publisher, the editors and the reviewers. Any product that may be evaluated in this article, or claim that may be made by its manufacturer, is not guaranteed or endorsed by the publisher.</p>
</sec>
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