Erik Severson, Research Associate and Interpretive Soil Scientist, - - PowerPoint PPT Presentation

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Erik Severson, Research Associate and Interpretive Soil Scientist, - - PowerPoint PPT Presentation

Erik Severson, Research Associate and Interpretive Soil Scientist, CSES department, Virginia Tech Well Aerobic soil Groundwater Trench Bottom Trench Bottom Trench Bottom Trench Bottom Clayton Site Clayton Site Left Side Lateral 3 Left


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Erik Severson, Research Associate and Interpretive Soil Scientist, CSES department, Virginia Tech

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Groundwater

Well Aerobic soil

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Clayey Horizon Trench Bottom Coarse-Textured

Clayton Site

Left Side – Lateral 3 8/23/1999

Clayey Horizon Trench Bottom Coarse-Textured Clayey Horizon Trench Bottom Coarse-Textured Clayey Horizon Trench Bottom Coarse-Textured

Clayton Site

Left Side – Lateral 3 8/23/1999

Source: Aziz Amoozegar, Lake Wheeler

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Introduction

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F

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Flat Topography + Impermeable Layers = Perched Water Tables

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  • 1. Document morphology and monitor

saturation in the Appomattox and Bentley Soil Series.

  • 2. Calculate % wet season RMFs were

saturated.

  • 3. Confirm or deny epiaquic conditions.
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  • 4. Compare saturation differences of

entirely residual soils versus transported soils.

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Location 1: Bentley Soils Location 2: Residual Soil

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Appomattox Bentley

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Cap and vent hole Annulus Bentonite gravel Restrictive Layer Slotted pipe Solid pipe

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10 20 30 40 50 60 70 80 90 100 1/1 1/8 1/15 1/22 1/29 2/5 2/12 2/19 2/26 3/5 3/12 3/19 3/26 4/2 4/9 4/16 4/23 4/30 Date Depth (cm)

Average 30-day 20-day

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10 20 30 40 50 60 70 80 90 100 1/1 1/8 1/15 1/22 1/29 2/5 2/12 2/19 2/26 3/5 3/12 3/19 3/26 4/2 4/9 4/16 4/23 4/30 Date Depth (cm)

Iron Concentrations: Chroma 3 depleted ped faces 5% 65%

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1) Document Soil Morphology

And

2) Monitor saturation for the Appomattox and Bentley Soils

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Ap Bt1 Bt2 2BCt 3CBt 3Ct

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20 40 60 80 100 120 140 160 180 200

  • 120
  • 100
  • 80
  • 60
  • 40
  • 20

Oct-11 Mar-12 Aug-12 Jan-13 Jun-13 Nov-13 Apr-14

Precipitation (mm) Depth (cm)

5YR 5/8 (c) 10YR 7/8 (d) 10YR 7/4 (d) N/8 (d) Precipitation

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Depleted ped faces n =36

41%

Concentrations n=11

23%

≥3 chroma depletions n=20

41%

≤2 chroma depletions n=12

65%

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  • 350
  • 300
  • 250
  • 200
  • 150
  • 100
  • 50

Sep-11 Apr-12 Oct-12 May-13 Nov-13 Jun-14

Depth (cm)

1.5M 3M Discontinuity

Perching confirmed at 6 out of 8 sites

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Compare hydrology of entirely

residual soils vs. transported soils at same depths (1 m).

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  • 120
  • 100
  • 80
  • 60
  • 40
  • 20

Nov-12 Mar-13 Jul-13 Nov-13 Mar-14 Depth (cm)

Residual Transported

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Soils

  • Avg. Water Table

30-day 20-day

Transported 81 64 91 Residual 95 83

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Conclusions Transported soils perch water for extended periods on impermeable layers.

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Conclusions Redox Features with chroma ≥3 indicate a fluctuating water table.

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Conclusions Residual soils underneath transported soils were not saturated.

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Conclusions Entirely residual soils were “drier” than transported soils.

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 Avoid use of transported soils with

restriction and perched water table

 Avoid 1 M below lithologic discontinuity