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(1R)-2,2-dimethyl-3-methylene-norbornane-1-carboxylic acid | 10309-19-0

中文名称
——
中文别名
——
英文名称
(1R)-2,2-dimethyl-3-methylene-norbornane-1-carboxylic acid
英文别名
(1R)-2,2-Dimethyl-3-methylen-norbornan-1-carbonsaeure;(1R)-3.3-Dimethyl-2-methylen-norbornan-carbonsaeure-(4);(1R,4R)-2,2-dimethyl-3-methylidenebicyclo[2.2.1]heptane-1-carboxylic acid
(1<i>R</i>)-2,2-dimethyl-3-methylene-norbornane-1-carboxylic acid化学式
CAS
10309-19-0
化学式
C11H16O2
mdl
——
分子量
180.247
InChiKey
ZZGALJOLYVMECF-KCJUWKMLSA-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):
    2
  • 重原子数:
    13
  • 可旋转键数:
    1
  • 环数:
    2.0
  • sp3杂化的碳原子比例:
    0.73
  • 拓扑面积:
    37.3
  • 氢给体数:
    1
  • 氢受体数:
    2

上下游信息

  • 上游原料
    中文名称 英文名称 CAS号 化学式 分子量

反应信息

点击查看最新优质反应信息

文献信息

  • Asahina; Kawahata, Chemische Berichte, 1939, vol. 72, p. 1540,1543
    作者:Asahina、Kawahata
    DOI:——
    日期:——
  • Houben; Pfankuch, Justus Liebigs Annalen der Chemie, 1930, vol. 483, p. 271,273, 281
    作者:Houben、Pfankuch
    DOI:——
    日期:——
  • The Skien lavas, Oslo Rift: petrological disequilibrium and geochemical evolution
    作者:E. Dunworth、E.-R. Neumann、J. Rosenbaum
    DOI:10.1007/s004100000215
    日期:2001.3
    The Skien lavas, which form the earliest phase of basaltic magmatism within the Permo-Carboniferous Oslo Rift, contain multiple generations of clinopyroxene which exhibit strong petrological and geochemical disequilibrium. Three principal core compositions have been identified: (1) low-jadeite, high-Mg, Cr-diopside cores (CrMgDi) with strongly depleted trace-element signatures, which are believed to be xenocrystic in origin; (2) Mg-rich, Cr-poor diopside cores (MgDi) with moderately depleted trace-element signatures which probably represent early cognate growth; and (3) more dominant, low-Mg, phenocrystic diopside cores (Phen-Di). Several samples contain CrMgDi or MgDi cores which have been subjected to resorption and partial reequilibration with their host melts, indicative of extensive disequilibrium and magma mixing. These three core types are overgrown by trace-element-enriched Ti-augite, which also forms megacrysts and late-stage lava groundmass. Calculated Ti-augite/melt partition coefficients show clinopyroxene compatibility of the M-HREE, Zr, Hf and Y. The LILE, Sr, and Nb remain incompatible. epsilon Sr-300 and epsilon Nd-300 Of Ti-augite overgrowths, phenocrystic diopside, and MgDi diopside cores show that intrasample isotopic disequilibrium existed when the host basalts were erupted. All epsilon values lie within the range of data previously published for the Skien lavas. Detailed examination of the chemical, isotopic and textural disequilibrium features seen in these lavas has enabled us to place constraints upon the magmatic evolution of this basalt suite, ranging from xenocryst incorporation to cognate multistage pyroxene growth, as well as identifying clear evidence of magma mixing and possible crustal contamination.
  • Antkowiak,W.Z., Bulletin de l'Academie Polonaise des Sciences, Serie des Sciences Chimiques, 1966, vol. 14, p. 437 - 441
    作者:Antkowiak,W.Z.
    DOI:——
    日期:——
  • Tamminen, Annales Academiae Scientiarum Fennicae, Series A2: Chemica, 1966, # 132, p. 12,28
    作者:Tamminen
    DOI:——
    日期:——
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同类化合物

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