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Water quality in the alluvium was monitored in each of the three sectors at Stations W82-17A, W82- <br />' 18A and W82-19A. Stations W82-17A and W82-18A are in the Maitland alluvium, while W82-19A is in <br />the Gordon alluvium. Water quality of Stations W82-17A and W82-I8A compare closely. The water is a <br />sodium/calcium bicarbonate-type water with a moderate mineralization. The water also has a low SAR, high <br />' concentrations of iron, and low concentrations of trace metals. Conversely, Station W82-19A in Gordon <br />Arroyo is highly mineralized sodium bicarbonate-type water with TDS and conductivity being measured at <br />over 3000. The station exhibits high SAR and low concentrations of trace metals. Comparison of this water <br />chemistry with the Lennox Seam water chemistry confirm the alluvial/deep aqui[er communication. <br />1 <br /> <br /> <br /> <br />t <br />