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(+/-)-erythro-2.3.4-triphenyl-butyric acid amide | 110664-07-8

中文名称
——
中文别名
——
英文名称
(+/-)-erythro-2.3.4-triphenyl-butyric acid amide
英文别名
(+/-)-erythro-2.3.4-Triphenyl-buttersaeure-amid;(2R,3S)-2,3,4-triphenylbutanamide
(+/-)-<i>erythro</i>-2.3.4-triphenyl-butyric acid amide化学式
CAS
110664-07-8
化学式
C22H21NO
mdl
——
分子量
315.415
InChiKey
CQNVIGGYUXKNSD-RTWAWAEBSA-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):
    4.5
  • 重原子数:
    24
  • 可旋转键数:
    6
  • 环数:
    3.0
  • sp3杂化的碳原子比例:
    0.14
  • 拓扑面积:
    43.1
  • 氢给体数:
    1
  • 氢受体数:
    1

反应信息

  • 作为反应物:
    描述:
    五氯化磷(+/-)-erythro-2.3.4-triphenyl-butyric acid amide三氯氧磷 生成 alkaline earth salt of/the/ methylsulfuric acid
    参考文献:
    名称:
    Recent sediments from a coastal pond, eastern margin of the Dead Sea, Jordan
    摘要:
    A marginal pond on the eastern coast of the southern part of the Dead Sea in Jordan receives fresh and thermal waters from adjacent areas. The pool has a narrow "intertidal" zone in which halite-encrusted stromatolites flourish. The muddy sediments of the pond consist of a mixture of detrital clay minerals and calcite with authigenic halite and dolomite. The association of halite with dolomite supports the assertion that dolomite is an evaporitic mineral. The absence of gypsum in these sediments is attributed to bacterial reduction of sulfates.
    DOI:
    10.1007/bf03175659
  • 作为产物:
    描述:
    苄基溴化镁 在 乙醚硫酸溶剂黄146 作用下, 生成 (+/-)-erythro-2.3.4-triphenyl-butyric acid amide
    参考文献:
    名称:
    Recent sediments from a coastal pond, eastern margin of the Dead Sea, Jordan
    摘要:
    A marginal pond on the eastern coast of the southern part of the Dead Sea in Jordan receives fresh and thermal waters from adjacent areas. The pool has a narrow "intertidal" zone in which halite-encrusted stromatolites flourish. The muddy sediments of the pond consist of a mixture of detrital clay minerals and calcite with authigenic halite and dolomite. The association of halite with dolomite supports the assertion that dolomite is an evaporitic mineral. The absence of gypsum in these sediments is attributed to bacterial reduction of sulfates.
    DOI:
    10.1007/bf03175659
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文献信息

  • Polyphenylnaphthalenes. II. 1,2,3-Triphenylnaphthalene
    作者:Felix Bergmann、David Schapiro、H. Emile Eschinazi
    DOI:10.1021/ja01255a027
    日期:1942.3
  • Recent sediments from a coastal pond, eastern margin of the Dead Sea, Jordan
    作者:Fadhil N. Sadooni、Walid Saqqa、Ghada Abrahim
    DOI:10.1007/bf03175659
    日期:2002.3
    A marginal pond on the eastern coast of the southern part of the Dead Sea in Jordan receives fresh and thermal waters from adjacent areas. The pool has a narrow "intertidal" zone in which halite-encrusted stromatolites flourish. The muddy sediments of the pond consist of a mixture of detrital clay minerals and calcite with authigenic halite and dolomite. The association of halite with dolomite supports the assertion that dolomite is an evaporitic mineral. The absence of gypsum in these sediments is attributed to bacterial reduction of sulfates.
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