Silty Clay Soil
Silty clay is at least 40% clay and 40% silt: smooth, sticky and slow to drain. Below: how it differs from silty clay loam and clay, why its shrink-swell matters, and where USDA maps it.[1][2][3]
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Silty clay
What makes a soil silty clay
Silty clay needs two floors at once. The Soil Survey Manual defines it as 40% or more clay and 40% or more silt, so there is never more than 20% sand in it.[1] On the triangle: clay ≥ 40 and silt ≥ 40.
Moist, it ribbons two inches or more and feels very smooth.[2]
You may see it called “clay silt” or “silt clay.” Neither is a USDA name: the manual has twelve texture classes, and silty clay is the one for soil that is high in both clay and silt.[1]
Silty clay vs silty clay loam and clay
The clay floor separates it from silty clay loam, and the silt floor separates it from clay. In our classifier, 15/45/40 sand/silt/clay is silty clay; shift one point from clay to silt (15/46/39) and it is silty clay loam; drop silt to 35% (20/35/45) and it is clay. Pure silt sits far off at the other end, with 80% or more silt.[1]
Shrink-swell: the trait to plan around
Silty clay topsoils have a median linear extensibility of 7.5%, in USDA’s high shrink-swell class, second only to clay (9.2%).[4] Linear extensibility measures how much the soil swells as it wets and shrinks as it dries. Before you build or pour, run the address through the expansive soil checker, which reads every layer, not just the surface.
In a trench, OSHA lists silty clay as an example of cohesive Type A soil, its most stable excavation class, once a competent person has confirmed the deposit’s strength and that it is not fissured or disturbed.[5] The soil types hub covers the OSHA and engineering systems.
How silty clay handles water
Slowly. Saturated topsoil passes water at a median 0.92 µm/s, about 0.13 inches an hour, which USDA’s classes call moderately low.[6] 70.5% of silty clay acres are in hydrologic group D, the group where water soaks in slowly and runoff is high when the soil is wet, a share topped only by clay.[7]
| Property | Median | Components |
|---|---|---|
| Water it holds | 1.8 in per foot of soil | n = 14,214 |
| How fast water moves | 0.92 µm/s · Moderately low | n = 14,214 |
| Bulk density | 1.32 g/cm³ | n = 14,214 |
| Organic matter | 2.5% | n = 14,214 |
| Shrink-swell (LEP) | 7.5% · high | n = 14,213 |
It holds a median 1.8 inches of plant-available water per foot, and 28.6% of its acres are poorly or very poorly drained, against 53.6% well drained.[8] Drainage changes its farm value: 12.5% is mapped prime farmland, and a larger 19.6% counts as prime only if drained, protected from flooding or irrigated.[3][9]
Is silty clay fertile?
It holds nutrients well. Purdue’s typical cation exchange capacity for dark-colored silty clays and silty clay loams in Indiana is 30 to 40 meq/100 g, at the top of its mineral-soil ranges;[10] the clay page has the full CEC ladder.
On USDA’s capability scale, 58% of rated silty clay acres are cultivable (Classes I–IV), and the limits it records split between erosion (subclass e, 41%) and wetness (w, 38%).[11] pH leans alkaline: 45.1% of its acres are alkaline, 31.5% neutral and 23.5% acid.
For a garden, the clay rules apply. Utah State advises against tilling clay when it is wet, because it compacts, and names organic matter as the best amendment;[12] the full method is on how to amend clay soil, and plants that tolerate it are on plants for clay soil.
Where silty clay is found
- 1. Texas: 4.9M
- 2. South Dakota: 3.1M
- 3. Montana: 2.9M
- 4. Kansas: 1.9M
- 5. North Dakota: 1.7M
- 6. Arkansas: 1.5M
As a share of each state’s own classified soil, silty clay peaks in Hawaii (17.5%), followed by South Dakota (6.5%) and Arkansas (4.9%).[3]
Most widespread silty clay soil series
| Series | Acres | Most in | Survey areas |
|---|---|---|---|
| Eckrant | 1,365,750 | Texas | 17 |
| Fargo | 862,332 | North Dakota | 38 |
| Sharkey | 760,031 | Arkansas | 24 |
| Clime | 751,344 | Kansas | 31 |
| Eden | 725,076 | Kentucky | 19 |
Eckrant (Texas) has the most silty clay acres, ahead of Fargo (North Dakota). Sharkey also ranks among the top clay series, because a series can carry more than one surface texture across its map units.[3]
Frequently asked questions
- What is silty clay?
- A USDA texture class with at least 40% clay and at least 40% silt: smooth, sticky, slow to drain and prone to shrink and swell.[1][2][3][4]
- Is clay silt a soil type?
- Not in USDA’s system. A soil high in both clay and silt is silty clay; with less than 40% clay it is silty clay loam.[1]
- What is the difference between silty clay and clay?
- Silt. Both have 40% or more clay, but silty clay also has 40% or more silt, while clay has less than 40%.[1]
- Does silty clay drain well?
- Not quickly. Water moves through it at about 0.13 inches an hour, and 70.5% of its acres are in the slow-infiltrating hydrologic group D.[3][7]
- Where is silty clay found?
- Texas, South Dakota and Montana have the most acres; as a share of a state’s soil it is highest in Hawaii.[3]
How we calculate this
Each soil component in USDA's detailed soil surveys gets the texture class of its surface horizon, the first horizon below any organic (O) layer, using the sand, silt and clay limits of the Soil Survey Manual. Miscellaneous areas such as Urban land, rock outcrop and water are counted separately and not classified, and so are organic soils (Histosols), even where a mineral layer lies under their organic surface. A component whose surface horizon has no sand, silt and clay values also stays unclassified.
- Acres are weighted by each soil component's share of its map unit (USDA's representative percent) and summed across 3,386 detailed USDA soil surveys.
- A class's share is of the 1,915.5 million acres that carry a texture class; states are the 50 states plus DC.
- Data generated 2026-10-30.
- More in our methodology.
Sources
- USDA NRCS, Soil Survey Manual (Agriculture Handbook 18), Ch. 3 “Examination and Description of Soil Profiles” (Soil Science Division Staff; eds. Ditzler, Scheffe, Monger; 2017)
- Colorado State University Extension, Estimating Soil Texture (GardenNotes #214)
- USDA NRCS, Soil Survey Geographic Database (SSURGO), via Soil Data Access
- USDA NRCS, National Soil Survey Handbook, Part 618, section 618.42: Linear extensibility percent (shrink-swell classes)
- OSHA, 29 CFR 1926 Subpart P, Appendix A “Soil Classification” (U.S. Department of Labor)
- USDA NRCS, Soil Survey Manual (Agriculture Handbook 18), Ch. 3: saturated hydraulic conductivity classes
- USDA NRCS, National Engineering Handbook, Part 630, Chapter 7: Hydrologic Soil Groups (January 2009)
- USDA NRCS, Soil Survey Manual (Agriculture Handbook 18), Ch. 3: drainage classes
- USDA NRCS, Farmland Protection Policy Act (7 U.S.C. 4201): definitions of prime, unique and statewide or local farmland
- Purdue Extension AY-238, Fundamentals of Soil Cation Exchange Capacity (CEC) (D. B. Mengel; c. 1993)
- USDA Soil Conservation Service, Land-Capability Classification (Agriculture Handbook 210; Klingebiel and Montgomery, 1961)
- Utah State University Extension, Gardening in Clay Soils (Wagner, Kuhns, Cardon; 2015)
Marko Visic · MPharm, BSc Physics · Last reviewed November 13, 2026