Orange County NC Website
24 <br />,�'VATER ti"rAMINATi N <br />GR `, WATER <br />Groundwater protection is a major concern in siting and designing a <br />sanitary landfill in North Carolina. <br />No field testing will be performed to determine the actual hydrogeologic <br />characteristics of the individual candidate sites. Investigations of the candidate <br />sites subsequent to this phase of the project will be performed to obtain site <br />es, depth to <br />specific information pertaining to actual subsurface soil typ of the site specific <br />groundwater, and groundwater quality. Because of the lack <br />h Y drogeologic information, surrogate parameters must be selected to measure the <br />impact to groundwater with readily available information. <br />The soil type influences the rate and extent of migration of a contaminant <br />released from a landfill if a leak in the liner system occurs. For example, clayey <br />soils, which are generally more impervious than other soil types, <br />will tend to restrict the downward migration of contaminants from a site and <br />potentially filter certain contaminants. Also, the deeper the underlying soil strata <br />the greater the protection. <br />Exhibit R -2A presents impact ratings related to groundwater as a function <br />of soil type and depth to groundwater. More impervious and deeper soil strata <br />are assigned a low impact rating. Conversely, highly pervious and shallow soils <br />are assigned a greater impact rating. The soil types are grouped into sands, silts, and clays. This is done to indicate the general permeability characteristics esics of instances, the <br />soils. Rock characteristic categories are also included because, in s o <br />groundwater is located beneath all soils within the bedrock. These rock <br />categories indicate the water now characteristics from relatively pervious rock <br />strata to impervious strata The depth to groundwater e5 give a ter beneath <br />variation of impact ratings based on the projected dept hs to <br />z <br />