Land Judging in OklahomaJames H. Stiegler, Extension Soils Specialist |
| For contest, the subsoil texture sample in the box will be used to determine the permeability. |
Slowly permeable --- Soils that have moderately fine-textured subsoils with angular and subangular blocky structure are slowly permeable. The subsoils are firm when moist and hard when dry. Roots are common. Length differences of vertical and horizontal cracks are negligible. Soil peds often have thin, discontinuous, clay films on surfaces and tend to break more easily along the vertical axis than in the very slowly permeable soils. Soils frequently have thick surface and transitional horizons from the surface to the most clayey horizon in the profile.
Very slowly permeable --- Soils that have dense, fine-textured subsoils and claypan soils are very slowly permeable. Their structure is coarse, angular blocky or massive with very few visible pores. Roots are few and generally follow ped faces and cracks. These subsoils are very firm when moist and very hard when dry. Soil peds have thick, continuous, clay films on surfaces. Horizontal cracks are longer than vertical ones. (Moddling and grayish subsoil colors are not required for a soil to have a very slow permeability in Oklahoma.)
Surface Runoff
Surface runoff is the relative rate water is removed by flowing over the soil surface. This includes rainfall, as well as water from adjacent slopes. It is the combined effect of soil slope, position in the landscape, permeability, and infiltration rate on runoff. Four classes of runoff are recognized in Oklahoma land judging.
Rapid --- Water is removed from the surface at a rapid rate. A large amount of rainfall is lost and only a small portion moves into the soil increasing the erosion hazard. This is a result of compaction, clayey textures and/or slopes greater than 3% (except when the soils are rapidly permeable).
Moderate --- Water drains away readily but yet slow enough that a large amount of the water enters the soil. This condition causes little erosion hazard and is considered a normal amount of runoff. This condition occurs on slopes of 1% to 3% (except when the soils are rapidly permeable).
Slow --- Water flows away so slowly that free water covers the soil for moderate periods. This increases the moisture supply but may interfere with farming operation. This condition occurs on slopes of 0 to 1% and includes soils with moderate, slow, or very slowly permeable subsoils.
| Soil Factor | Best Land Class | |
| Texture (1): | Coarse textured Moderately coarse, medium Moderately line and fine | III I I |
| Depth (2): | Deep or moderately deep Shallow Very shallow | I III VII |
| Slope (3): | Nearly level (0 to 1%) Gently sloping (1% to 3%) Moderately sloping (3% to 5%) Strongly sloping (5% to 8%) Steep and very steep (8% to 15%+) | I II III IV VI |
| Erosion (4): | None to slight erosion Moderate Severe or very severe | I II VI |
| Permeability (5): | Rapid Moderate and slow Very slow | III I II |
| Runoff (6): | Rapid Moderate and slow Very slow | III I II |
Class III --- Soils in Class III are good for cultivated crops, but have severe limitations that reduce the choice of plants and/or require special conservation practices that are more difficult to apply. Terracing and other water control measures will be needed.
Class IV --- Soils in Class IV can be cultivated, but they have very severe limitations that restrict the choice of plants, require very careful management, special conservation, or both. They are sloping, moderately eroded soils with poor characteristics. Cultivated areas should be strip tilled, terraced, and farmed on the contour. They are best suited for pasture and hay meadows.
Non-Cultivated
Class V --- Soils in Class V have little or no erosion hazards, but have other limitations that make them unsuitable for cultivation. Limitations are impractical and very expensive to remove and limits their use to pasture, range, woodland, or wildlife food and cover. Limitations include very poor surface and internal drainage or frequent flooding. (Frequent flooding will be shown with "other factors" when it occurs.)
Class VI --- Soils in Class VI have severe limitations such as steep slopes, severe erosion, shallowness, and rockiness that make them generally unsuited for cultivation and limits their use to pasture or range, woodland, or wildlife food and cover.
Class VII --- Soils in Class VII have many very severe limitations similar to Class VI that make them unsuited for cultivation and that restrict their use to grazing, woodland, or wildlife.