The significant presence of sulfide mineralization within the Sariguney gold deposit raises environmental concerns due to the exposure of waste rock and tailings to atmospheric conditions during mining and ore processing. This exposure leads to a process that poses a threat to local ecosystems and water quality. This study evaluates the potential for Acid Rock Drainage (ARD) from Sariguney's sulfidic rocks using established ARD prediction techniques. These include static methods such as Standard Acid Base Accounting (ABA) and kinetic methods such as Acid Buffering Characteristic Curves (ABCC) and Kinetic Net Acid Generation (NAG) through the monitoring of pH and temperature profiles.
To achieve this, 185 drill core intervals from ore, low-grade (LG), and waste samples were subjected to geochemical and mineralogical analyses. Based on their Net Acid Production Potential (NAPP) and NAG pH values, 31% of waste samples were classified as high acid rock (High-PAF), 13% as acid rock (PAF), and 56% as neutral rock (NAF). The Ore, LG and waste samples have average sulfur values of 2.6, 1.3 and 0.9 (wt.%) and NAPP values of 77, 32 and 18, respectively. The results indicate that ore-grade material has a significant sulfur content, little if any ANC, and a high acid generating potential. Approximately two-thirds of the LG ore samples were classified as High-PAF with low ANC availability would have a relatively short lag prior to acidification. Most of the NAF samples in waste rocks contained < 0.5 %S. (typically ANC <15 kg H2SO4/t) but expected that the higher ANC materials would provide some ARD control if blended with acid generating rock within waste dumps. Overall, approximately more than two-thirds of the samples tested had ANCs<10 kg H2SO4/t, which means most rock will have the capacity to neutralize the acid potential of less than 0.3 %S as pyrite and if blended with acid generating waste, will provide little additional neutralizing capacity and will simply dilute the acid waste.