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Department of Forestry and Wildland Resources at Humboldt State University

Department of Forestry and Wildland Resources at Humboldt State University

Department of Forestry and Wildland Resources at Humboldt State University. Our Forestry Program Is Known For:. Being student-centered Providing hands-on instruction Having a field orientation where almost all courses have outdoor labs Focusing on Forest Management

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726 views • 64 slides
Department of Forestry and Wildland Resources at Humboldt State University

Department of Forestry and Wildland Resources at Humboldt State University

Department of Forestry and Wildland Resources at Humboldt State University. Our Forestry Program Is Known For:. Being student-centered Providing hands-on instruction Having a field orientation where almost all courses have outdoor labs Focusing on Forest Management

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765 views • 64 slides
Introduction to Vadose Zone Hydrology

Introduction to Vadose Zone Hydrology

1. Introduction to Vadose Zone Hydrology. Course objectives. CE/ENVE 320-03 provides theoretical and experimental foundation for understanding and quantifying physical and hydrological properties of soils and other porous media.

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904 views • 36 slides
Lecture 3b Writing Soil Profile Descriptions and Forest Soils

Lecture 3b Writing Soil Profile Descriptions and Forest Soils

Lecture 3b Writing Soil Profile Descriptions and Forest Soils. Writing Soil Profile Descriptions. First step- prepare suitable pedon for describing Stand back and view the horizons from a distance Determine approximately how many distinct horizons are present.

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504 views • 28 slides
Soils, Mass movements, and soil conservation

Soils, Mass movements, and soil conservation

Soils, Mass movements, and soil conservation. From a half-sick Mr. Lewis. Soils. Soils are a result of weathering Without soil there could be no life on land Soil is made of loose, weathered rock, and organic material with which plants can grow

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458 views • 16 slides
P transport and accumulation along preferential flow pathways in forest soils

P transport and accumulation along preferential flow pathways in forest soils

Roots > 2mm. Tracer stained area. Macropores. C. B. A. Soil depth [cm]. P transport and accumulation along preferential flow pathways in forest soils Dorit Julich, Jianhong Liang, Karl-Heinz Feger. Dye coverage [%].

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101 views • 1 slides

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