摩熵化学
数据库官网
小程序
打开微信扫一扫
首页 分子通 化学资讯 化学百科 反应查询 关于我们
请输入关键词

8-heptyl pentadecane | 71005-15-7

中文名称
——
中文别名
——
英文名称
8-heptyl pentadecane
英文别名
8-Heptyl-pentadecan;8-Heptylpentadecane
8-heptyl pentadecane化学式
CAS
71005-15-7
化学式
C22H46
mdl
——
分子量
310.607
InChiKey
SGOHLOFHILWVPA-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

  • 熔点:
    29°C (estimate)
  • 沸点:
    349.19°C (estimate)
  • 密度:
    0.7719 (estimate)

计算性质

  • 辛醇/水分配系数(LogP):
    11.8
  • 重原子数:
    22
  • 可旋转键数:
    18
  • 环数:
    0.0
  • sp3杂化的碳原子比例:
    1.0
  • 拓扑面积:
    0
  • 氢给体数:
    0
  • 氢受体数:
    0

反应信息

  • 作为产物:
    描述:
    HEPTYLMAGNESIUM BROMIDE 在 乙醚溶剂黄146 作用下, 生成 8-heptyl pentadecane
    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
点击查看最新优质反应信息

文献信息

  • Petrow; Kaplan, Izvestiya Akademii Nauk SSSR, Seriya Khimicheskaya, 1949, p. 539,544
    作者:Petrow、Kaplan
    DOI:——
    日期:——
查看更多