What soil types are in the Oklahoma City metro?
In short: Soils around Oklahoma City mostly formed from Permian-age red shale, claystone and sandstone. Clay-rich series such as Renfrow and Kirkland shrink and swell strongly with moisture changes, while sandy series such as Dougherty and Lucien move much less. Knowing the mapped soil series is a starting point, but lots are often regraded, so the actual soil under a house has to be checked on site.
How is a soil series description read?
A soil series is a named soil type that the USDA describes in an Official Series Description (OSD): its layers, clay content, drainage and parent material (the rock or sediment it formed from). OSDs don't give a single "shrink-swell rating," but several details point to it:
- Clay content: higher clay usually means more volume change.
- Slickensides: polished, grooved surfaces inside clay layers that form when clay repeatedly swells and shrinks.
- Vertic properties and cracks: deep seasonal cracking, a hallmark of strongly expansive clay.
- Depth to rock: a "paralithic contact" is soft, weathered rock that a shovel can still dig; "densic" material is very dense soil-like material.
What are the major OKC metro soil series?
| Series | Clay (control section) | Drainage | Depth to rock or dense layer | Parent material |
|---|---|---|---|---|
| Renfrow | 35–55% | Well drained, slow water movement | More than 60 in. to noncemented shale | Permian clayey shale 1 |
| Kirkland | 40–60% | Well drained, slow permeability | Weak siltstone at about 82 in. in the typical profile | Clayey sediments over Permian shale 2 |
| Bethany | 35–50% | Well drained | Solum (soil layers) more than 60 in. thick | Loess or alluvium over Permian shale 3 |
| Vernon | 40–60% | Well drained, very slow permeability | Dense bedrock at 20–40 in. | Permian redbed claystone 4 |
| Zaneis | about 18–38% by layer | Well drained | Soft rock at 40–60 in. | Permian sandstone and shale 5 |
| Lucien | loamy | Well drained | Rippable sandstone at 10–20 in. | Permian sandstone with shale 6 |
| Dougherty | 18–35% in subsoil | Well drained | More than 60 in., no rock noted | Sandy terrace sediments 7 |
| Kingfisher | 27–35% (up to 42% in lower subsoil) | Well drained | Soft rock at 20–40 in. | Permian silty shale red beds 15 |
| Chickasha | 18–30% | Well drained | Weakly cemented sandstone at 40–60 in. | Permian sandstone 17 |
| Stephenville | sandy loam to sandy clay loam | Well drained | Sandstone at 20–40 in. | Permian sandstone 9 |
| Darnell | loamy | Well to somewhat excessively drained | Sandstone at 10–20 in. | Permian sandstone 10 |
| Norge | silty clay loam to silty clay subsoil | Well drained | Solum more than 60 in. | Pleistocene loamy alluvium on old terraces 13 |
| Teller | 18–30% in upper subsoil | Well drained | More than 80 in. | Pleistocene loamy sediments on stream terraces 14 |
| Konawa | 18–30% in subsoil | Well drained | More than 80 in. | Pleistocene loamy and sandy alluvium on low terraces 16 |
| Port | silt loam to clay loam | Well drained; occasional or frequent brief flooding | Very deep | Calcareous loamy alluvium on flood plains 11 |
| Pulaski | sandy and loamy | Well drained; occasional or frequent brief flooding | Very deep | Loamy Holocene alluvium on flood plains 12 |
| Dale | silt loam to clay loam | Well drained | Very deep | Loamy alluvium on flood plains of minor streams 18 |
Clay-rich series
Renfrow has vertic properties, with cracks at least 5 mm wide within about 4 feet of the surface for part of most years, and slickensides in the subsoil 1. Kirkland has intersecting slickensides in its subsoil 2. Renfrow's type location is in Kay County and Kirkland's is in Logan County, both in Oklahoma 12.
An Oklahoma State University study of benchmark soils found Kirkland's subsoil liquid limit exceeded 50% with high plasticity indices and described it as highly expansive, with a severe rating for low buildings 8. Bethany, whose type location is in Oklahoma County near Wheatland, had moderate shrink-swell in its subsoil 38.
Shallow-rock and sandy series
Vernon is a red clay over dense claystone at 20–40 inches and is described as very sticky and plastic 4. Zaneis, with a type location north of Edmond, is loamier and reaches soft rock at 40–60 inches 5. Lucien is shallow, with rippable sandstone at 10–20 inches 6. Dougherty formed in sandy, dune-like terrace deposits and is well drained 7.
The same OSU study found that sandy soils with little plasticity had low shrink-swell and good ratings as building sites 8.
Other sandstone soils in the metro follow the same pattern of loamy soil over Permian sandstone. Darnell, with a type location west of Tryon in Lincoln County, reaches sandstone at 10–20 inches on summits and shoulders of low hills 10. Stephenville, with a type location near Spencer in Oklahoma County, reaches sandstone at 20–40 inches 9. Chickasha averages 18–30% clay and sits over weakly cemented sandstone at 40–60 inches 17. Kingfisher formed in Permian silty shale red beds, averages 27–35% clay and reaches soft rock at 20–40 inches 15.
Terrace and flood-plain series
Along streams, some soils formed in water-laid sediment rather than in rock 111213141618:
- Old terraces. Norge (Pleistocene loamy alluvium, silty clay loam to silty clay subsoil), Teller and Konawa (each 18–30% clay in the subsoil, more than 80 inches deep) are well drained terrace soils 131416.
- Flood plains. Port, a calcareous loamy soil with a type location east of Chickasha, and Pulaski, a sandier loamy soil, are both occasionally or frequently flooded for very brief periods from March to October 1112. Dale, with a type location east of Harrah, lies on flood plains of minor streams 18.
What does this mean for foundations?
- Clay-rich series are the ones most associated with perimeter settlement in drought and heave when they rewet.
- Where soft rock is shallow, as in Lucien and Vernon, the depth of soil that can change volume is limited by the rock below.
- The underlying rock units are described on the Hennessey Shale and Garber Sandstone pages.
Soil maps show the dominant soil in an area, but map units include patches of other soils and urban lots are often cut or filled. Hand-auger samples or borings confirm what is actually under a slab; see soil testing and lab values.
Related
- R - OKC Metro
- Bedrock - OKC Metro
- Soil - Renfrow
- Soil - Kirkland
- Soil Series Index
- Shrink-Swell and Active Zone
Common questions
What kind of soil is in Oklahoma City?
Much of the OKC metro has soils formed from Permian red shale and sandstone. Clay-rich series such as Renfrow and Kirkland sit beside sandier series such as Zaneis, Lucien and Dougherty.
Which OKC soils have the most shrink-swell?
Renfrow and Kirkland are clay-rich and show signs of strong shrink-swell, such as slickensides and seasonal cracking. A 1978 Oklahoma State University study found Kirkland highly expansive, with Bethany in the moderate range.
Which OKC-area soils are on flood plains?
Port, Pulaski and Dale formed in loamy stream sediment on flood plains. The official descriptions for Port and Pulaski list occasional or frequent flooding for very brief periods from March to October.
How deep is rock under Oklahoma City soils?
It varies by series. Lucien reaches rippable sandstone in 10 to 20 inches, Vernon has dense claystone at 20 to 40 inches, and Renfrow, Kirkland and Bethany are more than 60 inches deep.
How do I find which soil is under my house?
The USDA soil survey maps soil series by location, but city lots are often graded or filled, so on-site samples or borings are the only way to confirm what is actually under a foundation.
Sources
- Official Series Description - RENFROW Series USDA Natural Resources Conservation Service
- Official Series Description - KIRKLAND Series USDA Natural Resources Conservation Service
- Official Series Description - BETHANY Series USDA Natural Resources Conservation Service
- Official Series Description - VERNON Series USDA Natural Resources Conservation Service
- Official Series Description - ZANEIS Series USDA Natural Resources Conservation Service
- Official Series Description - LUCIEN Series USDA Natural Resources Conservation Service
- Official Series Description - DOUGHERTY Series USDA Natural Resources Conservation Service
- Shrink-Swell and Other Characteristics of Five Benchmark Soils of Western Oklahoma (Technical Bulletin T-150) Oklahoma Agricultural Experiment Station, Oklahoma State University
- Official Series Description - STEPHENVILLE Series USDA Natural Resources Conservation Service
- Official Series Description - DARNELL Series USDA Natural Resources Conservation Service
- Official Series Description - PORT Series USDA Natural Resources Conservation Service
- Official Series Description - PULASKI Series USDA Natural Resources Conservation Service
- Official Series Description - NORGE Series USDA Natural Resources Conservation Service
- Official Series Description - TELLER Series USDA Natural Resources Conservation Service
- Official Series Description - KINGFISHER Series USDA Natural Resources Conservation Service
- Official Series Description - KONAWA Series USDA Natural Resources Conservation Service
- Official Series Description - CHICKASHA Series USDA Natural Resources Conservation Service
- Official Series Description - DALE Series USDA Natural Resources Conservation Service
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