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HG-11 | 188690-77-9

中文名称
——
中文别名
——
英文名称
HG-11
英文别名
Ethane, 1-(difluoromethoxy)-2-((difluoromethoxy)difluoromethoxy)-1,1,2,2-tetrafluoro-;1-(difluoromethoxy)-2-[difluoromethoxy(difluoro)methoxy]-1,1,2,2-tetrafluoroethane
HG-11化学式
CAS
188690-77-9
化学式
C5H2F10O3
mdl
——
分子量
300.053
InChiKey
ICIZOWVAGSOWBZ-UHFFFAOYSA-N
BEILSTEIN
——
EINECS
——
  • 物化性质
  • 计算性质
  • ADMET
  • 安全信息
  • SDS
  • 制备方法与用途
  • 上下游信息
  • 反应信息
  • 文献信息
  • 表征谱图
  • 同类化合物
  • 相关功能分类
  • 相关结构分类

计算性质

  • 辛醇/水分配系数(LogP):
    4.1
  • 重原子数:
    18
  • 可旋转键数:
    7
  • 环数:
    0.0
  • sp3杂化的碳原子比例:
    1.0
  • 拓扑面积:
    27.7
  • 氢给体数:
    0
  • 氢受体数:
    13

反应信息

  • 作为反应物:
    描述:
    HG-11五氟乙烷氧气 作用下, 22.84 ℃ 、93.33 kPa 条件下, 生成 氟光气
    参考文献:
    名称:
    氯原子引发 HCF2OCF2OCF2CF2OCF2H 和 HCF2O(CF2O)n-(CF2CF2O)mCF2H 氧化的动力学和产物
    摘要:
    烟雾室/FTIR 技术用于测量 k(Cl + HCF2OCF2OCF2-CF2OCF2H) = k(Cl + HCF2O(CF2O)n(CF2CF2O)mCF2H) = (5.0 ± 1.4) × 10−17 cm3 分子−1 s−1 in 700 Torr 的 N2/O2 稀释剂,温度为 296 ± 1 K。Cl 引发的 HCF2OCF2OCF2CF2OCF2H 的大气氧化和本工作中使用的 HCF2O(CF2O)n(CF2CF2O)mCF2H 样品产生的 COF2 摩尔产率为 (476 ± 36)%和 (859 ± 63)%,没有其他可观察到的含碳产物(即,两种氢氟聚醚基本完全转化为 COF2)。讨论了通式为 HCF2O(CF2O)n(CF2CF2O)mCF2H 的氢氟聚醚的大气化学和环境影响的结果。© 2008 Wiley Periodicals, Inc. Int J Chem Kinet
    DOI:
    10.1002/kin.20349
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文献信息

  • Tropospheric Degradation Products of Novel Hydrofluoropolyethers
    作者:Ernesto C. Tuazon
    DOI:10.1021/es961010w
    日期:1997.6.1
    The Cl atom-initiated photooxidations of the hydrofluoropolyethers (HFPEs) HCF2OCF2OCF2CF2OCF2H, HCF2OCF2CF2OCF2H, and HCF2OCF2OCF2H in air produced C(O)F-2 as the only carbon-containing product, with observed average C(O)F-2 molar formation yields of 4.73, 3.77, and 2.82, respectively. The C(O)F-2 molar formation yields during the early stages of the reactions were observed to be closer to the number of C atoms in each parent HFPE. On the basis of current knowledge concerning the degradation pathways of hydrofluorocarbons and hydrochlorofluorocarbons, it is expected that C(O)F-2 will also be produced with near unit yield per C atom from the above HFPEs in the troposphere, where loss processes would be initiated primarily by reaction with OH radicals. The rate constants for reaction with the Cl atom at 298 +/- 2 K were determined for the HFPEs by a relative rate method that employed CF3CF2H as the reference compound [k(Cl + CF2CF2H) = (2.4 +/- 0.5) x 10(-16) cm(3) molecule(-1) s(-1)], with measured values of (in units of 10(-17) cm(3) molecule(-1) s(-1)) HCF2OCF2OCF2CF2OCF2H, 3.6 +/- 0.8; HCF2OCF2CF2OCF2H, 4.5 +/- 1.0; and HCF2OCF2OCF2H, 5.0 +/- 1.1.
  • Kinetics and products of chlorine atom initiated oxidation of HCF<sub>2</sub>OCF<sub>2</sub>OCF<sub>2</sub>CF<sub>2</sub>OCF<sub>2</sub>H and HCF<sub>2</sub>O(CF<sub>2</sub>O)<sub><i>n</i></sub>-(CF<sub>2</sub>CF<sub>2</sub>O)<sub><i>m</i></sub>CF<sub>2</sub>H
    作者:T. J. Wallington、M. D. Hurley、M. S. Javadi、O. J. Nielsen
    DOI:10.1002/kin.20349
    日期:2008.12
    HCF2OCF2OCF2-CF2OCF2H) = k(Cl + HCF2O(CF2O)n(CF2CF2O)mCF2H) = (5.0 ± 1.4) × 10−17 cm3 molecule−1 s−1 in 700 Torr of N2/O2 diluent at 296 ± 1 K. The Cl-initiated atmospheric oxidation of HCF2OCF2OCF2CF2OCF2H and the sample of HCF2O(CF2O)n(CF2CF2O)mCF2H used in this work gave COF2 in molar yields of (476 ± 36)% and (859 ± 63)%, respectively, with no other observable carbon containing products (i.e., essentially complete
    烟雾室/FTIR 技术用于测量 k(Cl + HCF2OCF2OCF2-CF2OCF2H) = k(Cl + HCF2O(CF2O)n(CF2CF2O)mCF2H) = (5.0 ± 1.4) × 10−17 cm3 分子−1 s−1 in 700 Torr 的 N2/O2 稀释剂,温度为 296 ± 1 K。Cl 引发的 HCF2OCF2OCF2CF2OCF2H 的大气氧化和本工作中使用的 HCF2O(CF2O)n(CF2CF2O)mCF2H 样品产生的 COF2 摩尔产率为 (476 ± 36)%和 (859 ± 63)%,没有其他可观察到的含碳产物(即,两种氢氟聚醚基本完全转化为 COF2)。讨论了通式为 HCF2O(CF2O)n(CF2CF2O)mCF2H 的氢氟聚醚的大气化学和环境影响的结果。© 2008 Wiley Periodicals, Inc. Int J Chem Kinet
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