| 1 | The IR spectrum shows one or more bands with an asymmetric shape, with the slope of the high-wavenumber side less than the slope of the low-wavenumber side. |
| 2 | Formation of the amorphous ice is favoured by gas-phase condensation at low temperatures. |
| 3 | Formation of the amorphous ice is favoured by short deposition times for gas-phase condensation. |
| 4 | Formation of the amorphous ice is favoured by low rates of gas-phase condensation. |
| 5 | An irreversible crystallization is initiated by warming the ice sample. |
| 6 | Crystallization occurs as the thickness of the sample increases on continued deposition. |
| 7 | The spectrum resulting from crystallization by warming is close, but not necessarily identical, to that found on condensation at higher temperatures. |
| 8 | An isosbestic point accompanies the amorphous-to-crystalline change. |
| 9 | The spectrum's appearance resembles that of the corresponding liquid in the sense of broader bands than in IR spectra of crystalline solids and the presence of nominally forbidden features. |
| 10 | The IR spectrum agrees with theoretical expectations for amorphous solids. See, for example, the work of Ovchinnikov & Wight (1993; 1995) or that of Firanescu & Signorell (2009). |
| 1 | The IR spectrum shows one or more bands with an asymmetric shape, with the slope of the high-wavenumber side less than the slope of the low-wavenumber side. |
| 2 | Formation of the amorphous ice is favoured by gas-phase condensation at low temperatures. |
| 3 | Formation of the amorphous ice is favoured by short deposition times for gas-phase condensation. |
| 4 | Formation of the amorphous ice is favoured by low rates of gas-phase condensation. |
| 5 | An irreversible crystallization is initiated by warming the ice sample. |
| 6 | Crystallization occurs as the thickness of the sample increases on continued deposition. |
| 7 | The spectrum resulting from crystallization by warming is close, but not necessarily identical, to that found on condensation at higher temperatures. |
| 8 | An isosbestic point accompanies the amorphous-to-crystalline change. |
| 9 | The spectrum's appearance resembles that of the corresponding liquid in the sense of broader bands than in IR spectra of crystalline solids and the presence of nominally forbidden features. |
| 10 | The IR spectrum agrees with theoretical expectations for amorphous solids. See, for example, the work of Ovchinnikov & Wight (1993; 1995) or that of Firanescu & Signorell (2009). |
| 1 | The IR spectrum shows one or more bands with an asymmetric shape, with the slope of the high-wavenumber side less than the slope of the low-wavenumber side. |
| 2 | Formation of the amorphous ice is favoured by gas-phase condensation at low temperatures. |
| 3 | Formation of the amorphous ice is favoured by short deposition times for gas-phase condensation. |
| 4 | Formation of the amorphous ice is favoured by low rates of gas-phase condensation. |
| 5 | An irreversible crystallization is initiated by warming the ice sample. |
| 6 | Crystallization occurs as the thickness of the sample increases on continued deposition. |
| 7 | The spectrum resulting from crystallization by warming is close, but not necessarily identical, to that found on condensation at higher temperatures. |
| 8 | An isosbestic point accompanies the amorphous-to-crystalline change. |
| 9 | The spectrum's appearance resembles that of the corresponding liquid in the sense of broader bands than in IR spectra of crystalline solids and the presence of nominally forbidden features. |
| 10 | The IR spectrum agrees with theoretical expectations for amorphous solids. See, for example, the work of Ovchinnikov & Wight (1993; 1995) or that of Firanescu & Signorell (2009). |
| 1 | The IR spectrum shows one or more bands with an asymmetric shape, with the slope of the high-wavenumber side less than the slope of the low-wavenumber side. |
| 2 | Formation of the amorphous ice is favoured by gas-phase condensation at low temperatures. |
| 3 | Formation of the amorphous ice is favoured by short deposition times for gas-phase condensation. |
| 4 | Formation of the amorphous ice is favoured by low rates of gas-phase condensation. |
| 5 | An irreversible crystallization is initiated by warming the ice sample. |
| 6 | Crystallization occurs as the thickness of the sample increases on continued deposition. |
| 7 | The spectrum resulting from crystallization by warming is close, but not necessarily identical, to that found on condensation at higher temperatures. |
| 8 | An isosbestic point accompanies the amorphous-to-crystalline change. |
| 9 | The spectrum's appearance resembles that of the corresponding liquid in the sense of broader bands than in IR spectra of crystalline solids and the presence of nominally forbidden features. |
| 10 | The IR spectrum agrees with theoretical expectations for amorphous solids. See, for example, the work of Ovchinnikov & Wight (1993; 1995) or that of Firanescu & Signorell (2009). |
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