'Soil development' presentation slideshows

Chapter 6: Soil Formation and Morphology

Chapter 6: Soil Formation and Morphology Homework: 4, 8, 10, 11, 14a. Due 11 October. Soil formation Soils are formed from rock, loose unconsolidated materials (may be transported), or organic residues. See important fact to learn on p. 160. Two processes of soil formation: Weathering

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Designs, Natural Succession, and LTS&M of Disposal Cell Covers for Uranium Mill Tailings WJ Waugh

Designs, Natural Succession, and LTS&M of Disposal Cell Covers for Uranium Mill Tailings WJ Waugh S.M. Stoller Corporation LTS&M Conference November 16-18, 2010. U.S. Department of Energy Office of Legacy Management (LM) Sites.

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Designs, Natural Succession, and LTS&M of Disposal Cell Covers for Uranium Mill Tailings WJ Waugh

Designs, Natural Succession, and LTS&M of Disposal Cell Covers for Uranium Mill Tailings WJ Waugh S.M. Stoller Corporation LTS&M Conference November 16-18, 2010. U.S. Department of Energy Office of Legacy Management (LM) Sites.

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Soil Orders

Soil Orders. Highest level in Soil Taxonomy 12 orders Defined by presence/properties of diagnostic horizons, other specific soil properties Related to state factor model: specific factors influence/determine soil formation. Gelisols (-el). Soils of very cold climates with permafrost

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Monday, Oct. 3

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Assessing the Resilience and Vulnerability of Permafrost Landscapes to Environmental Change

Assessing the Resilience and Vulnerability of Permafrost Landscapes to Environmental Change. Torre Jorgenson, Yuri Shur, Mikhail Kanevskiy, Matt Dillon, and Eva Stephani. Approach to Assessing Permafrost Stability. Define permafrost in relation to climate and ecosystems

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Eolian Environments

Eolian Environments. Texture : super mature, very well sorted, clast sizes of medium sand to silt, clasts typically rounded and etched. Composion: siliciclastic (abundant quartz grains), carbonates (e.g., Bahamas), evaporites (e.g., gypsum in arid regions). SEM image (etched grain).

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Introduction to Soils

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Soils -linking rivers and slopes

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Chapter 2

Chapter 2. Soil Origin and Development. Objectives. Define a soil body List examples of five soil-forming factors Describe how soils develop Describe the horizons of a soil profile. Alluvial fan Alluvial soil Chemical weathering Colluvium Delta Eluviation Eolian deposit Floodplains

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Wetlands, Estuaries and Oceans

Wetlands, Estuaries and Oceans. Unit 4. Wetlands and Estuaries. What is a wetland? lands where saturation with water is the dominant factor determining the nature of soil development and the types of plant and animal communities living in the soil and on its surface What is an estuary?.

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A Lithologic Discontinuity in Brant County Soils August 22, 2014

A Lithologic Discontinuity in Brant County Soils August 22, 2014. Outline. Introduction Study location and sites Observations Where is the lithologic discontinuity? How did it form here?. Introduction. To determine differences in soil development between cultivated and forested sites.

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Movement of iron and aluminum in a series of palesols on a parabolic dune at Cape Kiwanda, Oregon

Movement of iron and aluminum in a series of palesols on a parabolic dune at Cape Kiwanda, Oregon. Karen R. Carroll, Mary Dietrich, and Scott F. Burns Portland State University Department of Geology. Location. Cape Kiwanda. Paleosols in sand dune. 3 rd Paleosol up (from bottom).

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FIELD WATER DISTRIBUTION

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Soil, Water, Vegetation (SFI - 3 08 04)

Soil, Water, Vegetation (SFI - 3 08 04). prof. dr. Nico van Breemen Soil Formation and Ecopedology Group dr. Marcel Hoosbeek Soil Formation and Ecopedology Group dr. Marcel Meinders Soil Formation and Ecopedology Group dr. Wim Braakhekke Nature Conservation and Plant Ecology Group

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