含cl -原子和oh -自由基的α-甲基噻吩气相动力学:实验和理论研究

IF 3.7 2区 环境科学与生态学 Q2 ENVIRONMENTAL SCIENCES Atmospheric Environment Pub Date : 2025-04-15 Epub Date: 2025-01-31 DOI:10.1016/j.atmosenv.2025.121078
Prasanna Kumar Bej , B. Rajakumar
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The experimental temperature-dependent rate coefficient was measured to be <span><math><mrow><msup><mrow><mi>k</mi><mrow><mo>(</mo><mi>T</mi><mo>)</mo></mrow></mrow><mrow><mn>258</mn><mo>−</mo><mn>358</mn><mspace></mspace><mi>K</mi></mrow></msup><mo>=</mo><mrow><mo>(</mo><mrow><mn>2.08</mn><mo>±</mo><mspace></mspace><mn>0.10</mn></mrow><mo>)</mo></mrow><mo>×</mo><msup><mn>10</mn><mrow><mo>−</mo><mn>11</mn></mrow></msup><mspace></mspace><mi>exp</mi><mrow><mo>[</mo><mrow><mrow><mo>(</mo><mrow><mn>484.5</mn><mo>±</mo><mspace></mspace><mn>15.4</mn></mrow><mo>)</mo></mrow><mo>/</mo><mi>T</mi></mrow><mo>]</mo></mrow></mrow></math></span> cm<sup>3</sup> molecule<sup>−1</sup> s<sup>−1</sup>. The theoretical rate coefficients for the reaction of MeTp with Cl-atom and OH radical were calculated at BD(T)/VDZ//BHandHLYP/6–31+g∗ and BD(T)/AVDZ//M06-2X/6–311++g∗∗ level of theory respectively. The Arrhenius equation from the theoretically calculated rate coefficients for MeTp + Cl using the MESMER simulation was obtained to be <span><math><mrow><msubsup><mrow><mi>k</mi><mrow><mo>(</mo><mi>T</mi><mo>)</mo></mrow></mrow><mrow><mtext>MeTp</mtext><mo>+</mo><mtext>Cl</mtext></mrow><mrow><mn>200</mn><mo>−</mo><mn>400</mn><mspace></mspace><mi>K</mi></mrow></msubsup><mo>=</mo><mrow><mo>(</mo><mrow><mn>2.44</mn><mspace></mspace><mo>±</mo><mspace></mspace><mn>0.12</mn></mrow><mo>)</mo></mrow><mo>×</mo><msup><mn>10</mn><mrow><mo>−</mo><mn>11</mn></mrow></msup><mspace></mspace><mi>exp</mi><mspace></mspace><mrow><mo>[</mo><mrow><mrow><mo>(</mo><mrow><mn>438.2</mn><mo>±</mo><mn>14.9</mn></mrow><mo>)</mo></mrow><mo>/</mo><mi>T</mi></mrow><mo>]</mo></mrow></mrow></math></span> cm<sup>3</sup> molecule<sup>−1</sup> s<sup>−1</sup>. The experimental and theoretical rate coefficients show a negative temperature dependence behaviour over the studied temperature range. The rate coefficient for MeTP + OH was calculated as <span><math><mrow><msubsup><mrow><mi>k</mi><mrow><mo>(</mo><mi>T</mi><mo>)</mo></mrow></mrow><mrow><mn>200</mn><mo>−</mo><mn>400</mn><mspace></mspace><mi>K</mi></mrow><mrow><mtext>CVT</mtext><mo>/</mo><mtext>SCT</mtext></mrow></msubsup><mo>=</mo><mrow><mo>(</mo><mrow><mn>2.83</mn><mspace></mspace><mo>±</mo><mn>0.20</mn></mrow><mo>)</mo></mrow><mo>×</mo><msup><mn>10</mn><mrow><mo>−</mo><mn>13</mn></mrow></msup><mspace></mspace><mi>exp</mi><mrow><mo>[</mo><mrow><mrow><mo>(</mo><mrow><mn>1641.7</mn><mo>±</mo><mspace></mspace><mn>20.6</mn></mrow><mo>)</mo></mrow><mo>/</mo><mi>T</mi></mrow><mo>]</mo></mrow></mrow></math></span> cm<sup>3</sup> molecule<sup>−1</sup> s<sup>−1</sup> from CVT/SCT methods. Following the MESMER simulation for MeTp + OH reaction, the Arrhenius expression was found to be <span><math><mrow><msubsup><mrow><mi>k</mi><mrow><mo>(</mo><mi>T</mi><mo>)</mo></mrow></mrow><mrow><mtext>MeTp</mtext><mo>+</mo><mtext>OH</mtext></mrow><mrow><mn>200</mn><mo>−</mo><mn>400</mn><mspace></mspace><mi>K</mi></mrow></msubsup><mo>=</mo><mrow><mo>(</mo><mrow><mn>8.31</mn><mspace></mspace><mo>±</mo><mspace></mspace><mn>0.53</mn></mrow><mo>)</mo></mrow><mo>×</mo><msup><mn>10</mn><mrow><mo>−</mo><mn>12</mn></mrow></msup><mspace></mspace><mi>exp</mi><mrow><mo>[</mo><mrow><mrow><mo>(</mo><mrow><mn>588.9</mn><mo>±</mo><mn>19.2</mn></mrow><mo>)</mo></mrow><mo>/</mo><mi>T</mi></mrow><mo>]</mo></mrow></mrow></math></span> cm<sup>3</sup> molecule<sup>−1</sup> s<sup>−1</sup>. At 298 K, the rate coefficient was calculated to be 5.60 × 10<sup>−11</sup> cm<sup>3</sup> molecule<sup>−1</sup> s<sup>−1</sup> and 6.23 × 10<sup>−11</sup> cm<sup>3</sup> molecule<sup>−1</sup> s<sup>−1</sup> for the reaction of MeTp with OH from CVT/SCT method and MESMER simulations. Both calculation methods demonstrated a negative temperature dependency over the temperature range of 200–400 K. No pressure dependency was observed over the 5–760 Torr in the MESMER calculations. The atmospheric lifespan of MeTp was estimated to be ∼100 days in ambient conditions and ∼1 day in polluted or coastal areas.</div></div>","PeriodicalId":250,"journal":{"name":"Atmospheric Environment","volume":"347 ","pages":"Article 121078"},"PeriodicalIF":3.7000,"publicationDate":"2025-04-15","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"A comprehensive gas-phase kinetics of α-methyl thiophene with Cl-atom and OH-radical: Experimental and theoretical studies\",\"authors\":\"Prasanna Kumar Bej ,&nbsp;B. Rajakumar\",\"doi\":\"10.1016/j.atmosenv.2025.121078\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>The rate coefficient for the reaction of methyl thiophene (MeTp) with Cl atom was measured to be (1.09 ± 0.24) × 10<sup>−10</sup> cm<sup>3</sup> molecule<sup>−1</sup>s<sup>−1</sup> at 298K and 760 Torr using the relative rate (RR) method. The experimental temperature-dependent rate coefficient was measured to be <span><math><mrow><msup><mrow><mi>k</mi><mrow><mo>(</mo><mi>T</mi><mo>)</mo></mrow></mrow><mrow><mn>258</mn><mo>−</mo><mn>358</mn><mspace></mspace><mi>K</mi></mrow></msup><mo>=</mo><mrow><mo>(</mo><mrow><mn>2.08</mn><mo>±</mo><mspace></mspace><mn>0.10</mn></mrow><mo>)</mo></mrow><mo>×</mo><msup><mn>10</mn><mrow><mo>−</mo><mn>11</mn></mrow></msup><mspace></mspace><mi>exp</mi><mrow><mo>[</mo><mrow><mrow><mo>(</mo><mrow><mn>484.5</mn><mo>±</mo><mspace></mspace><mn>15.4</mn></mrow><mo>)</mo></mrow><mo>/</mo><mi>T</mi></mrow><mo>]</mo></mrow></mrow></math></span> cm<sup>3</sup> molecule<sup>−1</sup> s<sup>−1</sup>. The theoretical rate coefficients for the reaction of MeTp with Cl-atom and OH radical were calculated at BD(T)/VDZ//BHandHLYP/6–31+g∗ and BD(T)/AVDZ//M06-2X/6–311++g∗∗ level of theory respectively. The Arrhenius equation from the theoretically calculated rate coefficients for MeTp + Cl using the MESMER simulation was obtained to be <span><math><mrow><msubsup><mrow><mi>k</mi><mrow><mo>(</mo><mi>T</mi><mo>)</mo></mrow></mrow><mrow><mtext>MeTp</mtext><mo>+</mo><mtext>Cl</mtext></mrow><mrow><mn>200</mn><mo>−</mo><mn>400</mn><mspace></mspace><mi>K</mi></mrow></msubsup><mo>=</mo><mrow><mo>(</mo><mrow><mn>2.44</mn><mspace></mspace><mo>±</mo><mspace></mspace><mn>0.12</mn></mrow><mo>)</mo></mrow><mo>×</mo><msup><mn>10</mn><mrow><mo>−</mo><mn>11</mn></mrow></msup><mspace></mspace><mi>exp</mi><mspace></mspace><mrow><mo>[</mo><mrow><mrow><mo>(</mo><mrow><mn>438.2</mn><mo>±</mo><mn>14.9</mn></mrow><mo>)</mo></mrow><mo>/</mo><mi>T</mi></mrow><mo>]</mo></mrow></mrow></math></span> cm<sup>3</sup> molecule<sup>−1</sup> s<sup>−1</sup>. The experimental and theoretical rate coefficients show a negative temperature dependence behaviour over the studied temperature range. The rate coefficient for MeTP + OH was calculated as <span><math><mrow><msubsup><mrow><mi>k</mi><mrow><mo>(</mo><mi>T</mi><mo>)</mo></mrow></mrow><mrow><mn>200</mn><mo>−</mo><mn>400</mn><mspace></mspace><mi>K</mi></mrow><mrow><mtext>CVT</mtext><mo>/</mo><mtext>SCT</mtext></mrow></msubsup><mo>=</mo><mrow><mo>(</mo><mrow><mn>2.83</mn><mspace></mspace><mo>±</mo><mn>0.20</mn></mrow><mo>)</mo></mrow><mo>×</mo><msup><mn>10</mn><mrow><mo>−</mo><mn>13</mn></mrow></msup><mspace></mspace><mi>exp</mi><mrow><mo>[</mo><mrow><mrow><mo>(</mo><mrow><mn>1641.7</mn><mo>±</mo><mspace></mspace><mn>20.6</mn></mrow><mo>)</mo></mrow><mo>/</mo><mi>T</mi></mrow><mo>]</mo></mrow></mrow></math></span> cm<sup>3</sup> molecule<sup>−1</sup> s<sup>−1</sup> from CVT/SCT methods. Following the MESMER simulation for MeTp + OH reaction, the Arrhenius expression was found to be <span><math><mrow><msubsup><mrow><mi>k</mi><mrow><mo>(</mo><mi>T</mi><mo>)</mo></mrow></mrow><mrow><mtext>MeTp</mtext><mo>+</mo><mtext>OH</mtext></mrow><mrow><mn>200</mn><mo>−</mo><mn>400</mn><mspace></mspace><mi>K</mi></mrow></msubsup><mo>=</mo><mrow><mo>(</mo><mrow><mn>8.31</mn><mspace></mspace><mo>±</mo><mspace></mspace><mn>0.53</mn></mrow><mo>)</mo></mrow><mo>×</mo><msup><mn>10</mn><mrow><mo>−</mo><mn>12</mn></mrow></msup><mspace></mspace><mi>exp</mi><mrow><mo>[</mo><mrow><mrow><mo>(</mo><mrow><mn>588.9</mn><mo>±</mo><mn>19.2</mn></mrow><mo>)</mo></mrow><mo>/</mo><mi>T</mi></mrow><mo>]</mo></mrow></mrow></math></span> cm<sup>3</sup> molecule<sup>−1</sup> s<sup>−1</sup>. At 298 K, the rate coefficient was calculated to be 5.60 × 10<sup>−11</sup> cm<sup>3</sup> molecule<sup>−1</sup> s<sup>−1</sup> and 6.23 × 10<sup>−11</sup> cm<sup>3</sup> molecule<sup>−1</sup> s<sup>−1</sup> for the reaction of MeTp with OH from CVT/SCT method and MESMER simulations. Both calculation methods demonstrated a negative temperature dependency over the temperature range of 200–400 K. No pressure dependency was observed over the 5–760 Torr in the MESMER calculations. 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引用次数: 0

摘要

用相对速率(RR)法测定了甲基噻吩(MeTp)与Cl原子在298K和760 Torr下的反应速率系数为(1.09±0.24)× 10−10 cm3分子−1s−1。实验测得温度相关速率系数为k(T)258−358K=(2.08±0.10)×10−11exp[(484.5±15.4)/T] cm3分子−1 s−1。分别在BD(T)/VDZ//BHandHLYP/ 6-31 +g∗和BD(T)/AVDZ//M06-2X/ 6-311 ++g∗的理论水平上计算了MeTp与cl -原子和OH自由基反应的理论速率系数。利用MESMER模拟理论计算的MeTp+Cl的速率系数得到的Arrhenius方程为:k(T)MeTp+Cl200−400K=(2.44±0.12)×10−11exp[(438.2±14.9)/T] cm3分子−1 s−1。实验和理论速率系数在研究温度范围内呈负温度依赖关系。MeTP + OH的速率系数计算为k(T)200−400KCVT/SCT=(2.83±0.20)×10−13exp[(1641.7±20.6)/T] cm3分子−1 s−1。通过MESMER模拟MeTp+OH反应,发现Arrhenius表达为k(T)MeTp+OH200−400K=(8.31±0.53)×10−12exp[(588.9±19.2)/T] cm3分子−1 s−1。在298 K时,CVT/SCT方法和MESMER模拟计算得到MeTp与OH反应的速率系数分别为5.60 × 10−11 cm3分子−1 s−1和6.23 × 10−11 cm3分子−1 s−1。两种计算方法在200 - 400k温度范围内均表现出负温度依赖性。在MESMER计算中,没有观察到5-760 Torr的压力依赖性。MeTp的大气寿命在环境条件下估计为~ 100天,在污染或沿海地区估计为~ 1天。
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A comprehensive gas-phase kinetics of α-methyl thiophene with Cl-atom and OH-radical: Experimental and theoretical studies
The rate coefficient for the reaction of methyl thiophene (MeTp) with Cl atom was measured to be (1.09 ± 0.24) × 10−10 cm3 molecule−1s−1 at 298K and 760 Torr using the relative rate (RR) method. The experimental temperature-dependent rate coefficient was measured to be k(T)258358K=(2.08±0.10)×1011exp[(484.5±15.4)/T] cm3 molecule−1 s−1. The theoretical rate coefficients for the reaction of MeTp with Cl-atom and OH radical were calculated at BD(T)/VDZ//BHandHLYP/6–31+g∗ and BD(T)/AVDZ//M06-2X/6–311++g∗∗ level of theory respectively. The Arrhenius equation from the theoretically calculated rate coefficients for MeTp + Cl using the MESMER simulation was obtained to be k(T)MeTp+Cl200400K=(2.44±0.12)×1011exp[(438.2±14.9)/T] cm3 molecule−1 s−1. The experimental and theoretical rate coefficients show a negative temperature dependence behaviour over the studied temperature range. The rate coefficient for MeTP + OH was calculated as k(T)200400KCVT/SCT=(2.83±0.20)×1013exp[(1641.7±20.6)/T] cm3 molecule−1 s−1 from CVT/SCT methods. Following the MESMER simulation for MeTp + OH reaction, the Arrhenius expression was found to be k(T)MeTp+OH200400K=(8.31±0.53)×1012exp[(588.9±19.2)/T] cm3 molecule−1 s−1. At 298 K, the rate coefficient was calculated to be 5.60 × 10−11 cm3 molecule−1 s−1 and 6.23 × 10−11 cm3 molecule−1 s−1 for the reaction of MeTp with OH from CVT/SCT method and MESMER simulations. Both calculation methods demonstrated a negative temperature dependency over the temperature range of 200–400 K. No pressure dependency was observed over the 5–760 Torr in the MESMER calculations. The atmospheric lifespan of MeTp was estimated to be ∼100 days in ambient conditions and ∼1 day in polluted or coastal areas.
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来源期刊
Atmospheric Environment
Atmospheric Environment 环境科学-环境科学
CiteScore
9.40
自引率
8.00%
发文量
458
审稿时长
53 days
期刊介绍: Atmospheric Environment has an open access mirror journal Atmospheric Environment: X, sharing the same aims and scope, editorial team, submission system and rigorous peer review. Atmospheric Environment is the international journal for scientists in different disciplines related to atmospheric composition and its impacts. The journal publishes scientific articles with atmospheric relevance of emissions and depositions of gaseous and particulate compounds, chemical processes and physical effects in the atmosphere, as well as impacts of the changing atmospheric composition on human health, air quality, climate change, and ecosystems.
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