Laserfiche WebLink
DocuSign Envelope ID: EBE28081-13782-41342-BAD13-D8C9313687131B <br />TOXICITY REDUCTION EVALUATION — LINES OF INVESTIGATION <br />Design Basis <br />construction, or in the event of inerting (coating), additional powered iron could be fluidized and added to <br />the reactor periodically during operation through the upper cell lateral pipes that are discussed later. <br />However, iron as Fe3+ is present in many ores, and iron reducing bacteria (IRB) can reduce and dissolve <br />it as Fez+. In addition to testing of the seep water for total and dissolved iron, locally available sources of <br />rock fill will also be investigated. The more promising local site materials will be bench and field tested, <br />possibly reducing or eliminating the need for supplemental iron. This could reduce both the construction <br />and operating cost. <br />Sizing <br />At neutral pH and at 33°C (91 °F), an average of 0.17 grams (170 mg) per liter per hour of sulfate to <br />sulfide conversion is possible based on prior studies (Table 8, Brahmacharimayum 2018). This means <br />under warm water conditions, as little as 9 hours of hydraulic retention time may be required to convert <br />1,000 mg/L of sulfate to sulfide. The effect of lower temperatures on this rate are significant and will be <br />evaluated during bench and site testing. On average, reaction rates halve (required treatment time <br />doubles) for every 10°C decrease. For the purposes of this estimate, it is assumed a 30°C temperature <br />decrease to a worst case water temperature of 3°C (37°F) will occur, resulting in a required retention time <br />of 72 hours or 3 days. Including safety factors, up to 6 days of retention time was assumed for the <br />purposes of this preliminary estimate. Assuming a maximum 364 gpm flow and 25% rock porosity, a <br />bioreactor (and rock) volume of nearly 70,000 cubic yards (cy) would be required. Collecting data on <br />actual temperatures and BSR rates will be used to optimize the final system size. <br />Configuration <br />The outfall from the East Taylor Pond flows through a graded creek channel that will be lined with an <br />impermeable geomembrane to design elevations, several feet below the access road. (All <br />geomembranes mentioned in this section would be sandwiched between geotextile for protection). This <br />will create a liner bioreactor nearly 1,000 feet long, which enhances mixing. Cells are included to maintain <br />fluid levels under variable flows, to promote mixing of the water, and to allow for more precise monitoring <br />and carbon dosing. <br />Cells: Rock fill placement would likely begin on the downgradient end, gradually sloping from the existing <br />creek grade up to the bioreactor height, estimated to be between 10 to 15 feet. After the first section has <br />been filled, a geomembrane will be placed across the creek channel against the rock angle of repose. <br />The sides may be welded or tape -sealed to the adjacent geomembrane - some leakage between cells <br />(i.e. several gallons a minute) would be acceptable given the anticipated high system flows. This fill and <br />geomembrane installation process would be repeated up the channel creating a series of cells (assumed <br />to be 6). <br />Laterals: Lateral water conveyance piping would be placed across the bottom (influent) and near the top <br />(effluent) of the rock in each cell. This pipe may be similar to leach -field piping for septic systems. Laterals <br />would run parallel to the channel alignment, with several laterals in each cell as sizing and flow rates <br />require. No pumping would be required, flow would be driven by gravity head differences between each <br />dpg \\us0321-ppfss011shared_projectsV33001407\reports\4_tre lines of investigationitre lines of investigation_20200320_ifra.docx 2.9 <br />