| 1054515-93-3

• 分子结构分类: 无机化合物 - 混合金属/非金属化合物 - 碱土金属氧阴离子化合物
• CAS: 1054515-93-3
• 化学式: HNO₃*NO₃
• 分子量: 125.018
• InChiKey: ZIOSHEBZUMXXRC-UHFFFAOYSA-N

计算性质

• 辛醇/水分配系数(LogP)：
  -0.59
• 重原子数：
  8.0
• 可旋转键数：
  0.0
• 环数：
  0.0
• sp3杂化的碳原子比例：
  0.0
• 拓扑面积：
  129.57
• 氢给体数：
  1.0
• 氢受体数：
  5.0

反应信息

• 作为反应物：
  描述：

  在 盐酸 作用下， 以 gas 为溶剂， 生成
  参考文献：
  名称：

  Three‐body ion–molecule association rate coefficients as a function of temperature and cluster size: NO⁻₃(HNO₃)_n+HCl→^MNO⁻₃ (HNO₃)_n(HCl)

  摘要：

  The rate coefficients for the three-body association of NO−3(HNO3)n to HCl have been measured for n=0, 1, and 2. The rates were measured from room temperature to 153 K. The data were taken in three buffers: helium, nitrogen, and hydrogen. The magnitude of the temperature coefficients in the standard power law fits was found to increase with increasing cluster size. Significant variations were found in the different buffers. The association rate coefficient of NO−3(HNO3)(HCl) to HC1 was also measured at 153 K and found to have the same value as that for NO−3(HNO3)2 clustering to HCl. Implications for stratospheric negative ion chemistry are discussed.

  DOI：

  10.1063/1.447972

文献信息

• Viggiano; Henchman; Dale, Journal of the American Chemical Society, 1992, vol. 114, # 11, p. 4299 - 4306
  作者：Viggiano、Henchman、Dale、Deakyne、Paulson

  DOI：——

  日期：——
• Rate Constants for the Reactions of XO₃^-(H₂O)<i>_n</i> (X = C, HC, and N) and NO₃^-(HNO₃)<i>_n</i> with H₂SO₄:  Implications for Atmospheric Detection of H₂SO₄
  作者：A. A. Viggiano、John V. Seeley、Paul L. Mundis、John S. Williamson、Robert A. Morris

  DOI：10.1021/jp971768h

  日期：1997.10.1

  Relative rate constants for the reactions of CO3-(H2O)(n), HCO3-(H2O)(n), NO3-(H2O)(n), and NO3-(HNO3)(n) with H2SO4 have been measured for n = 0-2, 0-2, 0-3, and 0-3, respectively. All rate constants have been found to occur in the ratio expected for the collisional values. This strongly indicates that the reactions proceed at the collision rate, and we assign absolute rate constants on the basis of this assumption. The present results show that all ions previously used for chemical ionization detection of H2SO4 concentrations in the atmosphere react rapidly, as has been previously assumed.