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Soilscapes and Soil Geomorphology

Soilscapes and Soil Geomorphology. Overview and Introduction. Participant Objectives. Know and define fundamental soil geomorphic terms (e.g., landform, landscape). Apply process geomorphology to landform recognition. Interpret landforms via surface form, stratigraphy, and hydrology.

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Soilscapes and Soil Geomorphology

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  1. Soilscapes and Soil Geomorphology Overview and Introduction

  2. Participant Objectives • Know and define fundamental soil geomorphic terms (e.g., landform, landscape). • Apply process geomorphology to landform recognition. • Interpret landforms via surface form, stratigraphy, and hydrology. • Discern soilscape context: Geomorphic stratigraphic, hydrologic, and pedologic setting.

  3. Soil Landscape Context • Geomorphic setting: landscape, landform, hillslope, micro feature. • Stratigraphy: Parent material sequence and composition. • Hydrology: Internal water source, flow direction, flow type, and surface outlets • Pedology: Soil horizons and their relationship to the above components.

  4. Soil Geomorphology • The systematic description, analysis, and understanding of soil landscapes (soilscape) and near-surface materials. This includes constituent landforms, landscapes (landform assemblages), soils, parent materials and the processes that create and change them.

  5. Landscape • A group of spatially associated landforms. • A landform assemblage • A landscape often contains landforms and soils that differ in age and formation process.

  6. Mountain slope Outwash Terrace End Moraine Landscape: Glaciated Mountains Wysocki 2005 CO

  7. Landform Any physical earth-surface feature having an observable shape (form) and internal composition (materials and arrangement) produced by natural forces; a discrete individual. • Surface form • Internal structure -- stratigraphy • Internal hydrology or water flow

  8. Mt Hood Oregon Composite or Strato Volcano Wysocki

  9. Mt Katahdin ME Kettle Lake Wysocki

  10. A field scientist must understand processes that create and change landforms and soils. One can observes features (landforms, soils, sediment bodies), but must infer process.

  11. Soil Survey and Geomorphology lake terraces wave-cut terraces We observe or infer field relationships among landforms, stratigraphy, and soils. Lake Bonn

  12. One must understand the processes that create or control soil, landform, and sediment formation. • Think in terms of process. • How did the landform, soil, and sediment originate? • When did the landform, soil, or sediment originate?

  13. Surface Form Size Shape Orientation Location Stratigraphy Composition What is this landform?

  14. Landform Recognition Surface Form - topography Stratigraphy - internal composition Hydrology - water flow in and through landform and landscapes

  15. Relict Glacial Delta topset-foreset contact marks water plane elevation of former sea or lake level. Foresets Topsets Bottomsets Nova Scotia DNR Five Islands, Nova Scotia

  16. flow water plane

  17. What is this landform? Shape? Composition?

  18. 1.0 mile

  19. Red = Fine loamy till Green = Sandy or coarse loamy outwash or till Blue = Saprists or hemists

  20. 1.0 mile

  21. What is the stratigraphy? What is the sorting? What is the bedding? Delta County MI Wysocki

  22. Red = Fine loamy till Green = Sandy or coarse loamy outwash or till Blue = Saprists or Hemists

  23. Drumlin And Interdrumlin

  24. Soil Survey and Geomorphology Soil Taxonomy and Soil Mapping • Taxonomy classifies soils based upon their properties. You must observe, measure, or infer properties to classify a soil. • Soil Taxonomy is not a predictive tool for soil mapping or a conceptual model for understanding soil-landscape relationships.

  25. Where is it on the landscape? Soil Taxonomy Very-fine, smectitic, thermic Chromic Epiaquert What is the formation process? How does ST help you draw a polygon? Wysocki 1999

  26. Soil Survey and Geomorphology Soil Taxonomy Bias • ST classifies and places focus on the pedon (small, laterally constrained ~ 1 meter soil area), which is not a soil landscape unit. • Uses an artificial soil depth limit (2 meters). • De-emphasizes parent material (stratigraphy)

  27. Sharkey Holocene clayey alluvium Vertical accretion Yazoo Basin Flood Plain Meander Belt Backswamp Rolling Fork, MS Wysocki

  28. Victoria (bowl); (chimney); Sodic Haplusterts Beaumont Formation; Late Pleistocene surface Wysocki

  29. Flood plain clayey deltaic and marine sediments on interstream divide

  30. Landform Recognition Surface Form (topography) Stratigraphy (internal composition) Hydrology (water flow in and through landscapes)

  31. What and where is this soilscape? till closed depressions till plain landscape depression focused recharge TYPIC ENDOAQUOLLS flow direction evaporative discharge TYPIC CALCIAQUOLLS recharge TYPIC HAPLUDOLL

  32. Soil Survey and Geomorphology Soil Survey (Soil Mapping – Landscape Models) • Sediment Distribution - parent materials • Soil-Landform Relationships - geomorphic processes • Age - geomorphic surfaces • Soil Map Unit Design • Soil Map Unit Description

  33. Late Sangamon Pediment Wisconsin age erosion surface Adair Soil Shelby Soil FINE-LOAMY, MIXED, SUPERACTIVE, MESIC TYPIC ARGIUDOLLS FINE, SMECTITIC, MESIC OXYAQUIC VERTIC ARGIUDOLLS

  34. Soil Survey and Geomorphology Soils are mapped largely by what can be seen: Landforms, vegetation, topography, slope inflections, rocks – and the known or inferred relationships that these features have with soil patterns, including parent materials, drainage (hydrology), and land surface age.

  35. Mountain slope End Moraine Outwash Terrace Soil 4 backslope Soil 3 shoulder Soil 5 alluvium Soil 2 outwash Soil 6 outwash Soil 1 till Landscape: Glaciated Mountains Wysocki 2005 CO

  36. Soilscape Context • Geomorphic setting: landscape, landform, hillslope, micro feature. • Stratigraphy: Parent material sequence and composition. • Hydrology: Internal water source, flow direction, flow type, and surface outlets • Pedology: Soil horizons and their relationship to the above components.

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