3-hydroxy-[2]naphthoic acid hexadecyl ester | 531-84-0

• 分子结构分类: 有机化合物 - 苯类化合物 - 萘
• 英文名称: 3-hydroxy-[2]naphthoic acid hexadecyl ester
• 英文别名: 3-Hydroxy-[2]naphthoesaeure-hexadecylester；3-hydroxy-2-naphthalenecarboxylic acid, hexadecyl ester；Hexadecyl 3-hydroxy-2-naphthoate；hexadecyl 3-hydroxynaphthalene-2-carboxylate
• CAS: 531-84-0
• 化学式: C₂₇H₄₀O₃
• 分子量: 412.613
• InChiKey: RTUSMTGSFGBYEC-UHFFFAOYSA-N

计算性质

• 辛醇/水分配系数(LogP)：
  11
• 重原子数：
  30
• 可旋转键数：
  17
• 环数：
  2.0
• sp3杂化的碳原子比例：
  0.59
• 拓扑面积：
  46.5
• 氢给体数：
  1
• 氢受体数：
  3

反应信息

• 作为产物：
  描述：

  3-羟基-2-萘甲酰氯 、 alkaline earth salt of/the/ methylsulfuric acid 生成 3-hydroxy-[2]naphthoic acid hexadecyl ester
  参考文献：
  名称：

  Isotopic chronology and geological events of Precambrian complex in Taihangshan region

  摘要：

  There are five major geological events in Precambrian complex, Taihangshan region determined by researching into geology and isotopic chronology of the complex. Basaltic magma erupted and quartz-dioritic to tonalitic magma intruded in earlier neo-archaean, which formed horn-blende-plagiogneiss of Fuping gneiss complex and metamorphic mafic rock enclaves in TTG gneiss complex. Granulite facies metamorphism and emplacement of biotite-plagiogneiss occurred in late neo-Archaean. Extension and uplifting from the end of neo-archaean to Paleoproterozoic era formed Chengnanzhuang large extensional deformation zones and metamorphic mafic veins emplaced into the deformation zones. Remobilization of Precambrian complex and tectonic uplifting in late Paleoproterozoic era formed Longquanguan ductile shear zone and emplacement of Nanying gneiss. Occurrence of regional granite pegmatite at the end of Paleoproterozoic era means the end of the Luliang movement.

  DOI：

  10.1007/bf02959449