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Dames & Moore, 1999 - USDA Forest Service

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The portal drainage was sampled at the 1500-level main portal (P-I) and directly prior to the portal drainage<br />

confluence with Railroad Creek (P-5). Dissolved aluminum. cadmium, copper, iron, and zinc decreased<br />

from spring to fall. Manganese decreased slightly at P-l and increased slightly at P-5. The pH was acidic in<br />

the spring and neutral in the fall. During the same sampling evenf concentrations of dissolved aluminum,<br />

cadmium, copper, iron, manganese, and zinc generally decreased from P-l to P-5 in the spring, remained<br />

constant in the summer, and were constant or decreased in the fall. The data from P-5 indicate that the<br />

portal drainage introduces concentrations of aluminum, cadmium, copper, iron, lead, manganese, and zinc<br />

into Railroad Creek that are above background with the actual concentration dependent upon season and<br />

stream flow. The data for P-1 and P-5 were compared to surface water quality criteria (WQC and MTCA<br />

Method B cleanup levels). P- 1 was compared to groundwater quality criteria (WAC 173-200 and MTCA<br />

Method B cleanup levels) as well. PCOCs identified based on surface water comparison included<br />

cadmium, copper, lead, zinc and pH. PCOCs identified at P-1 based on groundwater quality criteria<br />

included arsenic, beryllium, cadmium, copper, iron, lead. zinc, sulfate, total dissolved solids. and pH.<br />

The PCOCs are summarized by sampling event in Section 5.3.4. The fate and transport of metals in and<br />

from the portal drainage are further discussed in Section 6.0.<br />

A grab sample (VP-I) was collected from water discharging from the 1500-level ventilator portal.<br />

Generally, the concentrations of dissolved metals were orders of magnitude lower than the corresponding<br />

portal drainage samples. The pH was neutral (6.4 SU). The data appeared to indicate that the sample<br />

collected was more indicative of meteoric water possibly resulting from snowmelt.<br />

Water quality in the Copper Creek diversion was assessed. The Copper Creek diversion is the outflow from<br />

the hydroelectric plant and is used as a source of water for a dipping pond associated with a sauna utilized<br />

intermittently by residents and guests of Holden Village. Concentrations of cadmium, copper, iron,<br />

manganese, and zinc during the spring were above upstream Copper Creek concentrations. The data were<br />

compared to WQC. Cadmium, copper and zinc were identified as PCOCs in May (spring). Water quality at<br />

the diversion is included in the human health risk discussion in Section 7.0.<br />

Water quality in Copper Creek upstream of apparent Holden Mine influences and adjacent to the tailings<br />

piles was assessed. The data from the upstream location was compiled with other data,in the background<br />

surface water quality assessment. The data collected from CC-2 (adjacent to the tailings piles) was<br />

compared to WQC and background values. Metals detected at CC-2 were not above WQC or background.<br />

Additionally, concentrations between upstream and downstream stations on Copper Creek do not indicate<br />

seasonal variations. PCOCs were not identified in Copper Creek.<br />

5.4 GROUNDWATER<br />

Groundwater samples were collected from groundwater monitoring wells located in Holden Village, west<br />

of Holden Village near the baseball field, on the Site downgradient of the maintenance yard, in tailings<br />

piles 1,2, and 3, downgradient of tailings pile 3, and from a single well located at Lucerne. Samples were<br />

also collected from lysimeters located in tailings piles 1 and 3. The samples were collected during two<br />

sampling events conducted in May 1997 and September 1997. Sample locations are shown on Figure<br />

5.4-1.<br />

As part of the groundwater quality assessment, samples were also collected from seeps located on the Site<br />

and along Railroad Creek upgradient, adjacent to, and downgradient of the Holden Mine. The seeps were<br />

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