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7-hexyl-tridec-6-ene | 66359-59-9

中文名称
——
中文别名
——
英文名称
7-hexyl-tridec-6-ene
英文别名
7-Hexyl-tridec-6-en;7-Hexyl-tridecen-(6);7-hexyltridec-6-ene
7-hexyl-tridec-6-ene化学式
CAS
66359-59-9
化学式
C19H38
mdl
——
分子量
266.511
InChiKey
FSALSQDLMRPABV-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

物化性质

  • 沸点:
    149-150 °C(Press: 5.5 Torr)
  • 密度:
    0.7957 g/cm3

计算性质

  • 辛醇/水分配系数(LogP):
    9.5
  • 重原子数:
    19
  • 可旋转键数:
    14
  • 环数:
    0.0
  • sp3杂化的碳原子比例:
    0.89
  • 拓扑面积:
    0
  • 氢给体数:
    0
  • 氢受体数:
    0

反应信息

  • 作为反应物:
    描述:
    7-hexyl-tridec-6-ene 在 palladium on activated charcoal 、 溶剂黄146 作用下, 生成 7-己基十三烷
    参考文献:
    名称:
    Mineralogy of Tagish Lake: An ungrouped type 2 carbonaceous chondrite
    摘要:
    Abstract— In this paper we describe the recovery, handling and preliminary mineralogical investigation of the Tagish Lake meteorite. Tagish Lake is a type 2 carbonaceous chondrite which bears similarities to CI1 and CM chondrite groups, but is distinct from both. Abundant phyllosilicates as well as chondrules (however sparse) and common olivine grains in the matrix preclude any other classification. The bulk density of Tagish Lake (1.67 g/cc) is far lower than CI or CM chondrites (2.2‐2.3 and 2.6‐2.9 g/cc, respectively), or any other meteorite for that matter. We have identified two lithologies: a dominant carbonate‐poor lithology and a less‐abundant carbonate‐rich lithology. The meteorite is a breccia at all scales.We have noted similarities between Tagish Lake and some clasts within the enigmatic meteorite Kaidun; possibly there are genetic relationships here worth exploring. In the paper we describe a clast of CM1 material within Tagish Lake which is very similar to a major lithology in Kaidun.
    DOI:
    10.1111/j.1945-5100.2002.tb00852.x
  • 作为产物:
    描述:
    tri-n-hexyl-carbinol硫酸 作用下, 以 溶剂黄146 为溶剂, 生成 7-hexyl-tridec-6-ene
    参考文献:
    名称:
    Catalytic synthesis of high-density C20-C38 isoparaffins
    摘要:
    DOI:
    10.1007/bf01182955
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文献信息

  • Petrow; Tschernyschew, Izvestiya Akademii Nauk SSSR, Seriya Khimicheskaya, 1952, p. 1082,1083
    作者:Petrow、Tschernyschew
    DOI:——
    日期:——
  • Catalytic synthesis of high-density C20-C38 isoparaffins
    作者:A. P. Meshcheryakov、E. I. Erzyutova、Go Chun'-i
    DOI:10.1007/bf01182955
    日期:——
  • Mineralogy of Tagish Lake: An ungrouped type 2 carbonaceous chondrite
    作者:M. E. Zolensky、K. Nakamura、M. Gounelle、T. Mikouchi、T. Kasama、O. Tachikawa、E. Tonui
    DOI:10.1111/j.1945-5100.2002.tb00852.x
    日期:2002.5
    Abstract— In this paper we describe the recovery, handling and preliminary mineralogical investigation of the Tagish Lake meteorite. Tagish Lake is a type 2 carbonaceous chondrite which bears similarities to CI1 and CM chondrite groups, but is distinct from both. Abundant phyllosilicates as well as chondrules (however sparse) and common olivine grains in the matrix preclude any other classification. The bulk density of Tagish Lake (1.67 g/cc) is far lower than CI or CM chondrites (2.2‐2.3 and 2.6‐2.9 g/cc, respectively), or any other meteorite for that matter. We have identified two lithologies: a dominant carbonate‐poor lithology and a less‐abundant carbonate‐rich lithology. The meteorite is a breccia at all scales.We have noted similarities between Tagish Lake and some clasts within the enigmatic meteorite Kaidun; possibly there are genetic relationships here worth exploring. In the paper we describe a clast of CM1 material within Tagish Lake which is very similar to a major lithology in Kaidun.
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