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9,10-dioxo-octadecanedioic acid monomethyl ester | 115080-95-0

中文名称
——
中文别名
——
英文名称
9,10-dioxo-octadecanedioic acid monomethyl ester
英文别名
9,10-Dioxo-octadecandisaeure-monomethylester
9,10-dioxo-octadecanedioic acid monomethyl ester化学式
CAS
115080-95-0
化学式
C19H32O6
mdl
——
分子量
356.459
InChiKey
HDLYLNRBZOTFOL-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:
    80-83 °C(Solv: ethyl acetate (141-78-6))
  • 沸点:
    476.9±30.0 °C(Predicted)
  • 密度:
    1.065±0.06 g/cm3(Predicted)

计算性质

  • 辛醇/水分配系数(LogP):
    3.84
  • 重原子数:
    25.0
  • 可旋转键数:
    17.0
  • 环数:
    0.0
  • sp3杂化的碳原子比例:
    0.79
  • 拓扑面积:
    97.74
  • 氢给体数:
    1.0
  • 氢受体数:
    5.0

反应信息

  • 作为产物:
    描述:
    alkaline earth salt of/the/ methylsulfuric acid 在 铬酸丙酮 作用下, 生成 壬二酸9,10-dioxo-octadecanedioic acid monomethyl ester
    参考文献:
    名称:
    Using Direct Current Resistivity Sounding and Geostatistics to Aid in Hydrogeological Studies in the Choshuichi Alluvial Fan, Taiwan
    摘要:
    AbstractGround water reservoirs in the Choshuichi alluvial fan, central western Taiwan, were investigated using direct‐current (DC) resistivity soundings at 190 locations, combined with hydrogeological measurements from 37 wells. In addition, attempts were made to calculate aquifer transmissivity from both surface DC resistivity measurements and geostatistically derived predictions of aquifer properties.DC resistivity sounding data are highly correlated to the hydraulic parameters in the Choshuichi alluvial fan. By estimating the spatial distribution of hydraulic conductivity from the kriged well data and the cokriged thickness of the correlative aquifer from both resistivity sounding data and well information, the transmissivity of the aquifer at each location can be obtained from the product of kriged hydraulic conductivity and computed thickness of the geoelectric layer. Thus, the spatial variation of the transmissivities in the study area is obtained.Our work is more comparable to Ahmed et al. (1988) than to the work of Niwas and Singhal (1981). The first “constraint” from Niwas and Singhal's work is a result of their use of linear regression. The geostatistical approach taken here (and by Ahmed et al. [1988]) is a natural improvement on the linear regression approach.
    DOI:
    10.1111/j.1745-6584.2002.tb02501.x
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