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Logan Wash Mine Annual Report <br /> Permit No. M-1977-424 <br /> Historical and 2015 analytical results for mine water(LW-001),retort water(LW-Retort), and <br /> Well LWCW-lA are shown in Tables 5, 6, and 7,respectively. The analytical results for samples <br /> collected during the reporting period do not indicate a significant improvement of retort water <br /> quality compared to past sampling events. <br /> Four additional locations were added to the sampling schedule in 2015.Two of the locations are <br /> considered to be potential source waters of mine water discharge, "Big Seep"and"Research <br /> Mine Tributary". "Big Seep"emanates from the rock wall above the Daylight Portal and was <br /> sampled in May and October of 2015. "Research Mine Tributary"flows through the drainage <br /> above the Research Mine at the head of Logan Wash and was sampled in May of 2015; no flow <br /> was present in October of 2015. In addition, samples were collected in May and October of 2015 <br /> from Well LW-22A, an alluvial well located in Logan Wash approximately 2.25 miles down <br /> Logan Wash from the mine. Samples of the retort water flowing through the Lower Manhole <br /> (LW-LM)were also collected in May and October of 2015. Locations sampled during the spring <br /> 2015 semi-annual sampling event are shown in Figure 5.Analytical data from all of these <br /> samples is shown in Table 8. <br /> 3.4 Research Mine Manometer Monitoring <br /> The manometer installed in the Research Mine Vault is monitored and recorded on a monthly <br /> basis and on a more frequent basis in the spring months of April and May, or until the peak level <br /> begins to subside. If manometer measurements were to indicate a very high(> 36 inches)reading <br /> for more than a week's time,the water in the mine can be released and sampled. The manometer <br /> level was 0 inches throughout the reporting period. <br /> 3.5 Evaporation Pond Leak Detection System <br /> Monitoring of the Evaporation Pond Leak Detection Vault is conducted by continuous <br /> measurement of water pressure(depth)in the vault sump using an installed pressure transducer. <br /> On-site monitoring is conducted monthly as access conditions allow. Figure 6 shows the pressure <br /> transducer water depth results for the period October,2011 to February,2016. During the <br /> reporting period,the pressure transducer log indicated that the Leak Detection Vault slowly <br /> received water beginning in late March,2015 and reached the automated pumping depth of <br /> approximately 1.1 feet in mid-May. The slow flooding sequence repeated itself pumping again in <br /> mid-July. After this, intermittent pumping occurred in August,when late in the month battery <br /> failure apparently occurred. Water level in the vault attained approximately a 4.75 foot depth, <br /> before batteries were replaced in mid-September and again with a new solar controller on <br /> September 21.Another flooding cycle occurred in late October and the pump was replaced on <br /> November 10,which appeared to have fixed the intermittent pumping problem. Based on <br /> observations of suspended buckets under the three collection pipes, it appeared water had entered <br /> the vault through the east drainage pipe. <br /> Periodic inspections of the liner did not reveal any new open holes, cuts or cracks near the water <br /> line. <br /> 3.6 Precipitation <br /> Precipitation was monitored on the Lower Bench and at the Evaporation Pond through the use of <br /> Novalynx Corporation Model 260-2101 SK-P rain gauge instruments. The Lower Bench gauge is <br /> typically operational from April through December, depending on access to the bench.The <br /> Western Water & Land, Inc. 7 <br />