Laserfiche WebLink
Corrective Action Plan Page 20 <br />' water table also introduce oxygen into the vadose zone because air permeates the soil <br /> when groundwater elevations are low and fresh, oxygenated water infuses this zone when <br /> the water nses The fresh supply of oxygen stimulates microbial activity and aids the <br /> process of biodegradation of hydrocarbons <br /> For the above-stated reasons, following an initial period when groundwater will be <br /> continuously pumped at a high rate to remove the most severely contaminated water from <br /> the subsurface, a schedule will be established whereby the pumping rate will be <br /> periodically changed so as to enhance soil flushing and oxygenation <br /> The schedule of periodic changes in pumping rates that will produce the best overall <br /> remediation rate depends on the relative balance between the rate at which groundwater <br /> affected by dissolved contaminants is recovered, the total percentage of contaminant load <br />' that is adsorbed on the soil and the rate at which natural bioremediation progresses This <br /> schedule can not be determined a priori An optimal program must be developed from <br /> observations of the rate of change in contaminant concentrations as the remediation <br /> program progresses However, for planning purposes, but subject to revision as empirical <br /> data from the field become available, the scheme described below is proposed <br /> The groundwater recovery and treatment system will be operated continuously at, or close <br /> to, its design capacity for a period of six months, or until the mean concentration of total <br /> petroleum hydrocarbons in samples recovered from the pumped and monitoring wells falls <br /> to around 25% of its initial levels Pumping will then be stopped for a period not in excess <br /> of one month to allow the water table to rise and flush the soil in the vadose zone After <br /> that delay, a high rate of pumping will be resumed and will be continued for three month <br /> If, as is expected, contaminant concentration in groundwater in the near field of the <br /> recovery wells are observed to rise after pumping is temporally stopped and then fall again <br /> after it is resumed, the cyclical method of operating the groundwater recovery pumps will <br /> be adopted as a standard procedure <br /> As experience is gained and data from regularly scheduled rounds of groundwater <br /> sampling becomes available, the duration of the pump-operating cycles and the pumping <br /> rates will be adjusted to obtain the best possible rate of remediation However, pumping <br /> will not be stopped for such a lengthy period, or the pumping rate so reduced, that there <br /> would be a risk that the original plume of contamination might expand further down <br /> gradient <br /> Contaminant Load in Recovered Groundwater Stream <br /> When groundwater is pumped from recovery wells located in the center of a contaminated <br /> area, the concentrations of contaminants in the stream of recovered water often fluctuate <br />' widely as water from different parts of the affected zone of the subsurface arrives at the <br /> well <br />