H₂O Ice at 186 K
| Sample Type | Ice |
|---|---|
| Components | H₂O |
| Ratio | 1 |
| Substrate | Si |
| Phase / State | Polycrystalline hexagonal |
| Reference Temperature | 186 K |
| Wavenumber (cm⁻¹) | 3721.015 - 6981.188 |
| Wavelength (µm) | 0.002 - 2.687 |
Polycrystalline hexagonal water (H₂O) ice deposited at 186 K onto a silicon (Si) substrate, and held at 186 K during spectroscopic measurements.
The real (n) and imaginary (k) parts of the complex index of refraction were determined using optical measurements done at a temperature of 186 K, by infrared transmission spectroscopy from 6981 to 3721 cm⁻¹ with a resolution of 4 cm⁻¹.
More information can be found in the publication and on the OCdb contributor's page.
Any use of this data should recognize the parent publication(s):
Rajaram, B., Glandorf, D. L., Curtis, D. B., Tolbert, M. A., Toon, O. B. and Ockman, N. (2001) 'Temperature-dependent optical constants of water ice in the near-infrared: new results and critical review of the available measurements', Applied Optics, 40:25, pp. 4449-4462.
n/k Values
Compatible Datasets (i.e., same molecule, phase, and temperature) are marked with *
| Select | Chemical | Ratio | Phase / State | T (K) | Wavelength Min (µm) |
Wavelength Max (µm) |
Compatible | n | k | Reference |
|---|---|---|---|---|---|---|---|---|---|---|
|
|
H₂O | 1 | 10 | 2.501 | 199.39 | ✓ | ✓ | Hudgins et al. (1993) | ||
|
|
H₂O | 1 | 100 | 2.501 | 199.39 | ✓ | ✓ | Hudgins et al. (1993) | ||
|
|
H₂O | 1 | 105 | 0.25 | 19.995 | ✓ | ✓ | He et al. (2022) | ||
|
|
H₂O | 1 | 120 | 2.501 | 19.997 | ✓ | ✓ | Hudgins et al. (1993) | ||
|
|
H₂O | 1 | 135 | 0.25 | 19.995 | ✓ | ✓ | He et al. (2022) | ||
|
|
H₂O | 1 | 140 | 2.501 | 199.39 | ✓ | ✓ | Hudgins et al. (1993) | ||
|
|
H₂O | 1 | Polycrystalline hexagonal | 166 | 0.002 | 2.687 | ✓ | ✓ | Rajaram et al. (2001) | |
|
|
H₂O | 1 | Polycrystalline hexagonal | 176 | 0.002 | 2.687 | ✓ | ✓ | Rajaram et al. (2001) | |
|
|
H₂O | 1 | Polycrystalline hexagonal | 196 | 0.002 | 2.687 | ✓ | ✓ | Rajaram et al. (2001) | |
|
|
H₂O | 1 | 30 | 0.25 | 19.941 | ✓ | ✓ | He et al. (2022) | ||
|
|
H₂O | 1 | 4.2 | 0.546 | 0.546 | ✓ | - | Kruger and Ambs (1959) | ||
|
|
H₂O | 1 | 40 | 2.501 | 19.997 | ✓ | ✓ | Hudgins et al. (1993) | ||
|
|
H₂O | 1 | 75 | 0.25 | 19.992 | ✓ | ✓ | He et al. (2022) | ||
|
|
H₂O | 1 | 77 | 0.546 | 0.546 | ✓ | - | Kruger and Ambs (1959) | ||
|
|
H₂O | 1 | 80 | 2.501 | 19.997 | ✓ | ✓ | Hudgins et al. (1993) |