Spatiotemporal evolution characteristics of leaching solution dispersion and mineral dissolution in acid ISL of uranium
摘要
This study investigated the spatiotemporal evolution of acid in-situ leaching (ISL) in the Bayan Ula uranium deposit’s C12 mining area. Tracer tests and anorthite dissolution analysis revealed progressive ore-layer clogging, reducing dispersion, most notably along the KZ15262 → KC15060 pathway. Anorthite dissolution generally decreased due to passivation but increased downstream owing to prolonged contact time. A dynamic "dissolution–precipitation–clogging–dispersion weakening" coupling mechanism was identified, with dissolution dominating near injection wells and precipitation-induced clogging prevailing farther away. These processes impaired leaching solution migration, ultimately lowering uranium recovery. The findings highlight the critical role of spatiotemporal dynamics in optimizing ISL efficiency.