| Abstract |
With the growing global efforts in advancing geothermal energy development, several technologies are being introduced to capitalize on the full potential of geothermal resources. A critical aspect of these efforts is the understanding of the underlying mechanisms behind challenges encountered during resource utilization. Mineral scaling is one of the persistent challenges in the industry, which can cause significant generation losses and impact the overall performance of geothermal fields. Among the various types of mineral scales, chalcedony—although not commonly observed in production wells—has been identified in certain cases, such as in the Tiwi Geothermal Field in Albay, Bicol, Philippines. Unlike more prevalent scales like calcite and anhydrite, chalcedony typically does not form independently. Its formation is governed by a combination of factors, including reduced flow rate, declining pressure, and changes in wellbore geometry. Chalcedony is often found to crystallize following the initial deposition of primary scale minerals such as calcite or anhydrite. This study seeks to enhance the understanding of the formation mechanism of chalcedony in geothermal production wells. By acquiring clearer insights into its behavior, more effective mitigation strategies can be identified to address this scaling issue and maintain the efficiency of geothermal operations. |