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Pulacayo Project Feasibility Study - Apogee Silver

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<strong>Pulacayo</strong> 1 000 t/d Phase I <strong>Feasibility</strong> <strong>Study</strong> - NI 43-101 Technical Report<br />

090644-3-0000-20-IFI-100<br />

18.9.5 Foundation Preparation<br />

The site is overlain by a very thin layer of topsoil, which will be removed from the dike foundations<br />

as the first step in construction (topsoil within the impoundment and outside of the dike<br />

foundations may be either removed or left in place at the owner’s election. The stripped topsoil<br />

will be stockpiled for use in closure and reclamation. The topsoil layer is underlain by alluvial soil<br />

in and near the bottom of the valley, and residual soils up slope. There are a few areas where<br />

moraine deposits remain, but these are limited in area and generally thin. The entire site is<br />

underlain by a sandstone basement rock.<br />

The alluvial soils have been placed by the seasonal flow within the tailings valley, and (more<br />

importantly) the seasonal flow of the adjacent Rio Negro, which has its confluence with the<br />

tailings valley just downstream of the facility. Since the tailings valley is very near the top of the<br />

watershed, with a very small catchment area (about 45 ha), the extent and depth of the alluvium<br />

is very limited within the TSF area.<br />

The alluvium consists of well-graded gravels and sands, generally dense. The residual soils are<br />

those that have weathered in situ from the basement rock and are dense to very dense. These<br />

soils are poorly graded silty gravels and sands with cobbles. The glacial moraines are generally<br />

composed of silty gravels with some cobbles, and are very dense. The basement rock consists of<br />

principally of competent, medium grained sandstone. The surface of the basement rock is lightly<br />

weathered and fractured to a shallow depth, and it gains competency with increasing depth.<br />

Except for the thin layer of topsoil, the site soils are considered suitable for use as structural fill<br />

(Dikes 1 & 2), random or mass fill (Dikes 3 & 4) and as foundations for all of the dikes. Some<br />

removal (less than 3,000 m 3 ) of inadequate soils will be required beneath the first dike,<br />

emergency pond and subdrain monitoring ports area. This soil will be stockpiled with the topsoil.<br />

18.9.6 Foundation Underdrains<br />

A system of underdrains or subdrains will be installed to capture shallow subsurface water and<br />

seepage from the tailings. This system will drain the entire TSF basin and will also act to monitor<br />

and provide an early indication if there is detrimental impacts to water quality from the TSF. This<br />

subdrainage system will consist of a network of perforated double wall polyethylene pipes<br />

(generally 100 mm and 300 mm diameter), which will be installed in trapezoidal ditches nominally<br />

700 mm deep and filled with drainage gravel (conventionally called French drains). These French<br />

drains will slope at a minimum of 2% and the flow will be collected in the small monitoring ports<br />

located below the emergency pond.<br />

The preliminary location of the drainage network is shown on the design drawings (by Anddes),<br />

but the final locations will be determined and fit in the field based on the observed ground<br />

conditions at the time of construction. That is, the network may be adjusted or expanded to<br />

accommodate actual as-built conditions. The discharge from the subdrains is expected to range<br />

from negligible to a peak of between 1.0 and 2.2 m3/h (based on the peak storm event).<br />

18.9.7 Containment System<br />

The facility is located in a tight, closed basin underlain by shallow, tight sandstone. This basin<br />

drains to a single outlet just below the TSF. The tailings will be discharged at high solids contents<br />

TWP Sudamérica S.A. Av. Encalada 1257 Of. 801, Santiago de Surco Lima 33, Perú (51-1) 4377473<br />

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