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Evaluation of Septic Tank and Subsurface Wetland for

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Since evapotranspiration decreases fluid content without removing salts, there was<br />

concern regarding excessive increase in the concentration <strong>of</strong> total dissolved solids (TDS)<br />

over time. Water samples collected in the wetl<strong>and</strong> after a year <strong>and</strong> a half <strong>of</strong> service had<br />

conductance ranging from 438 – 447 μmho (see Appendix 4). This range is comparable<br />

to the conductance measurements <strong>for</strong> the Retrieve wetl<strong>and</strong> <strong>and</strong> below the regularly<br />

measured levels found in the effluent from oxidation ditches <strong>and</strong> stabilization ponds in<br />

Western Jamaica (NWC, 2004). Insufficient data was collected to make a conclusive<br />

determination regarding TDS buildup, but there was no indication that TDS accumulation<br />

was excessive.<br />

Retrieve Sanitation System Hydraulics<br />

The volumetric flowrate <strong>of</strong> water to the toilets <strong>and</strong> urinal ranged from 10,540 liter/wk to<br />

49,090 liter/wk. Average water use <strong>for</strong> toilets <strong>and</strong> urinal was 22,680 liter/wk or 3,240<br />

L/d (857 USgal/day). Averaged over the seven day week this is 48.3 L/p-d. Hydraulic<br />

retention time in the septic tank averaged 1.2 days. The constant urinal wash water <strong>and</strong><br />

occasional malfunction <strong>of</strong> toilet flappers contributed to the high water use <strong>and</strong> resultant<br />

low septic tank HRT. This school pays a flat rate water bill.<br />

Hydraulic loading on the wetl<strong>and</strong> from sewage ranged from 1.1 – 5.3 USgal/ft 2 -d<br />

(45 - 216 L/m 2 -d). The heaviest weekly precipitation accumulation at this site was 3.2<br />

inches (81 mm). Hydraulic loading on the wetl<strong>and</strong> from sewage <strong>and</strong> rainfall combined<br />

ranged from 1.4 – 5.3 USgal/ft 2 -d (57 – 216 L/m 2 -d) with an average <strong>of</strong> 2.6 USgal/ft 2 -d<br />

(105 L/m 2 -d). Average HRT <strong>for</strong> the single wetl<strong>and</strong> bed used during the evaluation was<br />

2.2 days.<br />

On two occasions, high influent flow rate caused surface flooding (i. e. water over the<br />

rock surface) at the inlet <strong>of</strong> the wetl<strong>and</strong> <strong>and</strong> near overflow water level at the inlet<br />

manhole. This was observed when average influent flow <strong>and</strong> precipitation exceeded<br />

5,055 L/d (1,335 USgal/d) <strong>and</strong> 7,010 L/d (1,852 USgal/d) corresponding to hydraulic<br />

34

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