“…Regarding trace element abundances, the mean concentration values of these in groundwater of the studied area (with the exception of Pb) were lower than the mean concentrations of trace elements in groundwater supplied to other megacities such as Tokyo (Mn 82 μg/L, Cu 3.7 μg/L, Se 4.7 μg/L, Cr 1.8 μg/L, As 1.8 μg/L, and Cd 0.1 μg/L), mainly because groundwater in that region is in contact with volcanic ash soils (which can be rich in trace elements) and unconsolidated layers of silt, sand, and gravel (Thuyet et al 2016 ). However, the mean trace element contents in groundwater supplied to MMA were higher than those found in groundwater supplied to heavily urbanized areas of Hong Kong (Mn 2.72 μg/L, Cu 1.16 μg/L, Zn 40.8 μg/L, Se 0.38 μg/L, Cr 0.71 μg/L, Co 0.02 μg/L, As 0.42 μg/L, Mo 0.29 μg/L, and Cd 0.07 μg/L), a region in which the geology is dominated by acidic volcanic rocks and granite bedrocks (Leung and Jiao 2006 ).…”