Bis-<4-(hydrazinocarbonyl)-phenyl>-disulfid | 6767-15-3

• 分子结构分类: 有机化合物 - 苯类化合物 - 苯和取代衍生物
• 英文名称: Bis-<4-(hydrazinocarbonyl)-phenyl>-disulfid
• 英文别名: 4,4'-disulfanediyl-di-benzoic acid dihydrazide；4,4'-Disulfandiyl-di-benzoesaeure-dihydrazid；4-[[4-(Hydrazinecarbonyl)phenyl]disulfanyl]benzohydrazide
• CAS: 6767-15-3
• 化学式: C₁₄H₁₄N₄O₂S₂
• 分子量: 334.423
• InChiKey: DICWXDRPGBLLTG-UHFFFAOYSA-N

计算性质

• 辛醇/水分配系数(LogP)：
  1.1
• 重原子数：
  22
• 可旋转键数：
  5
• 环数：
  2.0
• sp3杂化的碳原子比例：
  0.0
• 拓扑面积：
  161
• 氢给体数：
  4
• 氢受体数：
  6

反应信息

• 作为反应物：
  描述：

  Bis-<4-(hydrazinocarbonyl)-phenyl>-disulfid 、 2,4-二氯苯甲醛 在 溶剂黄146 作用下， 生成 4,4'-disulfanediyl-di-benzoic acid bis-(2,4-dichloro-benzylidenehydrazide)
  参考文献：
  名称：

  Hydrazine Derivatives. I. Benzalthio- and Bisbenzaldithio-Salicylhydrazides

  摘要：

  DOI：

  10.1021/jo50016a019
• 作为产物：
  描述：

  对硫氢基苯甲酸甲酯 在 甲醇 、 碘 、 一水合肼 作用下， 反应 2.0h， 生成 Bis-<4-(hydrazinocarbonyl)-phenyl>-disulfid
  参考文献：
  名称：

  Hydrazine Derivatives. I. Benzalthio- and Bisbenzaldithio-Salicylhydrazides

  摘要：

  DOI：

  10.1021/jo50016a019

文献信息

• Gialdi et al., Farmaco, Edizione Scientifica, 1959, vol. 14, p. 216,232
  作者：Gialdi et al.

  DOI：——

  日期：——
• Rock-magnetic investigation of Siberia loess and its implication
  作者：Rixiang Zhu、Kazansky Alexey、Matasova Galina、Bin Guo、Valentina Zykina、Petrovsky Eduard、Jordanova Neli

  DOI：10.1007/bf02886328

  日期：2000.12

  Multiple-rock magnetic investigations conducted on the loess-paleosol sequences at Kurtak in Southwestern Siberia reveal that the mass-normalized low-field magnetic susceptibility profiles reflect changes in lithology between relatively unweathered primary loess of glacial periods and the interglacial paleosols. Maxima in susceptibility values correspond with the least-weathered loess horizons, and minima with the humic horizons of soils. Frequency-dependent susceptibility of the loess-paleosol sequences at Kurtak is very low and practically uniform, indicating the dominance of non-SP ferrimagnetic minerals and negligible pedogenesis. The history of temperature-dependence of susceptibility (TDS) and stepwise acquisition of the isothermal remanent magnetization (SIRM) have confirmed that magnetite is predominant magnetic mineral, and only few maghemite and probably hematite are present within the studied section. Anisotropy of the magnetic susceptibility (AMS) can be used to monitor tilt and disturbance of the sedimentary layers, and also to provide information about the paleo-transport direction for Siberia loess.