Incorporate hydraulic conductivity estimates for layered soils Sample Clauses

Incorporate hydraulic conductivity estimates for layered soils. In many cases, estimated saturated hydraulic conductivity values are derived from discrete soil samples collected from several depths at several different horizontal locations beneath each of the infiltration ponds. The goal should be to collect at least one sample from each discrete layer at each horizontal location. Table 4 gives an example of how the data from these multiple samples can be combined to obtain a single “effective” or “equivalent” hydraulic conductivity estimate for an infiltration facility. Soil samples were collected at four different horizontal locations at the example site. At three of these horizontal locations, samples were collected from three different layers. At the fourth location, samples were collected from only two different layers. Hydraulic conductivity values were estimated for each soil sample using the Xxxxx equation. Hydraulic conductivity estimates from different layers at a single horizontal location can be combined using the harmonic mean: ∑ d d Kequiv = Ki
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