J K Bates
Biographic Data
| ID | 4053770 |
|---|---|
| NAME | J K Bates |
| GIVEN NAMES | J K |
| FAMILY NAME | Bates |
| SIGNATURE | BATES J K |
| AFFILIATIONS | Argonne National Laboratory |
| VERIFIED | No |
| TOTAL WORKS | 1 |
| TOTAL CITATIONS | 28 |
| AUTHOR COUNT | 1 |
| EDITOR COUNT | 0 |
| FIRST PUBLICATION YEAR | 1991 |
| LATEST PUBLICATION YEAR | 1991 |
| H-INDEX | 1 |
The Experimental Hydration of Obsidian as a Function of Relative Humidity and Temperature
The experimental hydration of obsidian for up to 30 days is described at relative humidities (RH) of 60, 90, 95, and 100 percent and at temperatures of 150, 160, and 175°C. Under isothermal conditions, the rate of hydration increased by as much as 25 percent between 60 and 100 percent RH. The RH dependence is nonlinear, with the majority of the rate increase occurring between 90 and 100 percent RH. The effect of RH can be related to the driving f…
The Experimental Hydration of Obsidian as a Function of Relative Humidity and Temperature
The experimental hydration of obsidian for up to 30 days is described at relative humidities (RH) of 60, 90, 95, and 100 percent and at temperatures of 150, 160, and 175°C. Under isothermal conditions, the rate of hydration increased by as much as 25 percent between 60 and 100 percent RH. The RH dependence is nonlinear, with the majority of the rate increase occurring between 90 and 100 percent RH. The effect of RH can be related to the driving f…
The Experimental Hydration of Obsidian as a Function of Relative Humidity and Temperature
The experimental hydration of obsidian for up to 30 days is described at relative humidities (RH) of 60, 90, 95, and 100 percent and at temperatures of 150, 160, and 175°C. Under isothermal conditions, the rate of hydration increased by as much as 25 percent between 60 and 100 percent RH. The RH dependence is nonlinear, with the majority of the rate increase occurring between 90 and 100 percent RH. The effect of RH can be related to the driving f…
Archaeological and Geological Studies (1 works) · Archaeology and ancient environmental studies (1 works) · Chemistry (1 works) · Diffusion (1 works) · Humidity (1 works) · Isothermal process (1 works) · Mineralogy (1 works) · Pleistocene-Era Hominins and Archaeology (1 works) · Relative humidity (1 works) · Thermodynamics (1 works)