6-methoxy-3-oxo-cyclohepta-1,4,6-trienecarboxylic acid | 855396-95-1

• 分子结构分类: 有机化合物 - 碳氢化合物衍生物 - 环庚三烯酮
• 英文名称: 6-methoxy-3-oxo-cyclohepta-1,4,6-trienecarboxylic acid
• 英文别名: 6-Methoxy-3-oxo-cyclohepta-1,4,6-triencarbonsaeure；6-Methoxy-3-oxocyclohepta-1,4,6-triene-1-carboxylic acid
• CAS: 855396-95-1
• 化学式: C₉H₈O₄
• 分子量: 180.16
• InChiKey: MYKDEQDDMIKKJR-UHFFFAOYSA-N

物化性质

• 熔点：
  190 °C
• 沸点：
  356.4±42.0 °C(Predicted)
• 密度：
  1.31±0.1 g/cm3(Predicted)

计算性质

• 辛醇/水分配系数(LogP)：
  0.5
• 重原子数：
  13
• 可旋转键数：
  2
• 环数：
  1.0
• sp3杂化的碳原子比例：
  0.11
• 拓扑面积：
  63.6
• 氢给体数：
  1
• 氢受体数：
  4

反应信息

• 作为反应物：
  描述：

  6-methoxy-3-oxo-cyclohepta-1,4,6-trienecarboxylic acid 在 氢氧化钾 作用下， 生成 5-羟基间苯二甲酸
  参考文献：
  名称：

  Terrestrial heat flow in Junggar Basin, Northwest China

  摘要：

  Based on temperature logs of 117 boreholes and thermal conductivity of 119 rock samples, the first group of 35 heat flow data in the Junggar Basin are presented. The thermal gradients vary between 11.6 and 26.5 degreesC/km, and the thermal conductivity changes from 0.17 to 3.6 W/mK. Heat flow ranges from 23.4 to 53.7 mW/m(2) with a mean of (42.3+/-7.7) mW/m2. The heat flow pattern shows that heat flow is higher in the uplifts and lower in the depressions. The factors affecting the heat flow and its distribution include basin type, basement structure, sediment thickness, radioactive heat generation, etc. The overall low present-day heat flow in the Junggar Basin reflected its tectonothermal evolution characterized by lithospheric thickening, thrust and fault at shallow crust as well as consequently quick subsidence during the Late Cenozoic.

  DOI：

  10.1007/bf02886273
• 作为产物：
  描述：

  alkaline earth salt of/the/ methylsulfuric acid 在 四氯化碳 、 氯仿 、 溴 作用下， 生成 6-methoxy-3-oxo-cyclohepta-1,4,6-trienecarboxylic acid
  参考文献：
  名称：

  Terrestrial heat flow in Junggar Basin, Northwest China

  摘要：

  Based on temperature logs of 117 boreholes and thermal conductivity of 119 rock samples, the first group of 35 heat flow data in the Junggar Basin are presented. The thermal gradients vary between 11.6 and 26.5 degreesC/km, and the thermal conductivity changes from 0.17 to 3.6 W/mK. Heat flow ranges from 23.4 to 53.7 mW/m(2) with a mean of (42.3+/-7.7) mW/m2. The heat flow pattern shows that heat flow is higher in the uplifts and lower in the depressions. The factors affecting the heat flow and its distribution include basin type, basement structure, sediment thickness, radioactive heat generation, etc. The overall low present-day heat flow in the Junggar Basin reflected its tectonothermal evolution characterized by lithospheric thickening, thrust and fault at shallow crust as well as consequently quick subsidence during the Late Cenozoic.

  DOI：

  10.1007/bf02886273

文献信息

• 358. Synthetic experiments in the cycloheptatrienone series. Part VII
  作者：R. S. Coffey、A. W. Johnson

  DOI：10.1039/jr9580001741

  日期：——
• US5703274A
  申请人：——

  公开号：US5703274A

  公开（公告）日：1997-12-30
• Terrestrial heat flow in Junggar Basin, Northwest China
  作者：Shejiao Wang、Shengbiao Hu、Tiejun Li、Jiyang Wang、Wenzhi Zhao

  DOI：10.1007/bf02886273

  日期：2000.10

  Based on temperature logs of 117 boreholes and thermal conductivity of 119 rock samples, the first group of 35 heat flow data in the Junggar Basin are presented. The thermal gradients vary between 11.6 and 26.5 degreesC/km, and the thermal conductivity changes from 0.17 to 3.6 W/mK. Heat flow ranges from 23.4 to 53.7 mW/m(2) with a mean of (42.3+/-7.7) mW/m2. The heat flow pattern shows that heat flow is higher in the uplifts and lower in the depressions. The factors affecting the heat flow and its distribution include basin type, basement structure, sediment thickness, radioactive heat generation, etc. The overall low present-day heat flow in the Junggar Basin reflected its tectonothermal evolution characterized by lithospheric thickening, thrust and fault at shallow crust as well as consequently quick subsidence during the Late Cenozoic.