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Attachment 4 - Geotech Report · MCU23/0030
50 NOOSA PARADE, NOOSA HEADS PROPOSED RESIDENCE 5.3 Groundwater Groundwater seepage and saturated sand indicating the presence of groundwater inflow was encountered during drilling between 1.8 m and 2.0 m BGL (~ RL 0.4 m to RL 0.6 m AHD). Standing groundwater was recorded at a depth of 1.8 m BGL (measured during mid tide) in the borehole BH1 standpipe at completion of drilling works. A groundwater sample was collected (following bore purging) and basic field water quality parameters measured, prior to dispatch to Eurofins MGT for analysis of ASS related water quality parameters. Results of the field and laboratory testing conducted on the groundwater sample from borehole BH1 are given in Table 1. Table 1: Summary of Groundwater Physio-chemical Parameters and Laboratory Testing Parameter Units BH1 SWL* m BGL 1.8 pH pH 6.52 Conductivity mS/cm 0.626 REDOX mV -227 Acidity (as CaCO3) mg/L 310 Sulphate mg/L 55 Chloride mg/L 120 Total Aluminium mg/L 7.6 Aluminium (Soluble) mg/L 0.78 Total Iron mg/L 9.0 Iron mg/L 0.49 (Soluble) Note: SWL denotes standing water level. Test results indicate that the groundwater conditions are fresh (EC >1.5 mS/cm), and neutral (pH 6.5 - 8.5). This is not uncommon for groundwater within such a setting near a tidal river. Levels of chloride and sulphate are typical of estuarine groundwater conditions and do not indicate an added source of sulphate from past oxidation of ASS. Levels of total aluminium and iron are relatively high when compared to guideline levels for recreational surface waters. It is noted that levels of total aluminium and total iron are likely to be mostly present as suspended and colloidal sediment within the groundwater. Where dewatering takes place, appropriate water treatment will be required to adjust pH and reduce total suspended sediment loads, thereby also reducing iron and aluminium levels prior to discharge or release. Groundwater is expected to be generally encountered during excavation of the lower half of the proposed basement excavation, below about RL 1 m AHD. As the site is located directly adjacent to Noosa River, a relatively consistent phreatic groundwater level is likely to be present which will rise and fall in sympathy with tidal surface water movements. Groundwater is expected to be well recharged based on proximity to the river and rates of infiltration into excavations below the water table would likely be high given the sandy nature of the soil profile. 2 February 2023 Report No. 22500-001-Rev0 6
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