High-Temperature Vacuum Drying Ovens as Key Equipment for Simulating Geologic Mineralization Processes
These ovens enable precise control over temperature, pressure, and fluid environments, providing experimental data to study geologic fluid migration and mineral precipitation mechanisms. Their applications include:
High-temperature vacuum drying ovens replicate mid- to high-temperature hydrothermal conditions (e.g., 300–600°C, 10–100 MPa) found in the deep crust. By maintaining accurate heating rates (5°C/min) and pressurizing with inert gases (e.g., Ar), they help investigate the dissolution-migration behavior of metals (e.g., Cu, Au, Fe) in ore-forming fluids (e.g., NaCl-H₂O-CO₂ systems).
By adjusting temperature gradients, pressure drops, or fluid mixing, these ovens simulate the crystallization of sulfides, oxides, and other minerals. Key findings include:
Integrated with in-situ sensors (temperature/pressure probes, pH/conductivity meters) and post-experiment analyses (SEM, XRD, LA-ICP-MS), experimental data from these ovens validate models like:
Combining synchrotron X-ray imaging and other real-time analytical techniques, these ovens could dynamically capture mineral crystallization, further enhancing simulation accuracy and practical value.
(Adapted from Economic Geology and Geochimica et Cosmochimica Acta standards.)