Agronomy and Horticulture Department

 

Title

Soil Genesis and Development, Lesson 4 - Soil Profile Development

Date of this Version

2019

Document Type

Article

Citation

Plant and Soil Sciences eLibrary (PASSeL) Lesson

Comments

Copyright © 2019 Plant and Soil Sciences eLibrary. Used by permission.

JNRLSE approved 2009

This lesson was developed by Martha Mamo, Timothy Kettler, and Dennis McCallister at the University of Nebraska–Lincoln; Jim Ippolito, Research Soil Scientist, USDA-ARS-NWISRL, Kimberly, Idaho, formerly at Colorado State University; Ron Reuter at Oregon State University; Christoph Geiss at Trinity College–Connecticut; and William Zanner at the University of Minnesota. Development of this lesson was supported by the National Science Foundation Course, Curriculum, and Laboratory Improvement Program (NSF-CCLI), Award Number DUE-0042603. Any opinions, findings, conclusions, or recommendations expressed in this publication are those of the authors and do not necessarily reflect the view of NSF.

Abstract

This lesson discusses the processes controlling soil formation and how these processes relate to the characteristics of a soil profile.

Goal

Understand the processes controlling soil formation and relate the processes of soil formation to the characteristics of a soil profile through the use of soil horizon designations.

Objectives

  1. Describe the four major soil-forming processes.
  2. Describe how these four processes redistribute soil materials in vertical and horizontal dimensions.
  3. Explain which soil processes are dominant in each soil horizon.
  4. Develop a profile horizon sequence based on given soil properties and a set of soil forming factors.
  5. Describe the general soil-forming processes, based on the soil-forming factors described in Lesson 3, that led to the development of a given soil profile.

From the surface, soil may seem like an innocuous substance. Soil supports our weight; plants and animals live in it. But long after we’ve come and gone, the soil will remain, baking in the sun, hosting plant and animal life, receiving rain and snow. The soil-forming factors—climate, time, organisms, topography, and parent material—affect what is below the surface and, in the long run, how a soil develops: chemically, physically, and biologically.

The vertical dimension of a soil can be variable. What seems homogeneous at the surface can be radically different as you dig in. In conjunction with the soil-forming factors, over the lifespan of a soil (which can be tens to tens of thousands of years) the four general soil-forming processes—additions, losses, transformations, and translocations—are organizing, reorganizing, and altering the soil, creating what are called soil horizons. These horizons also vary laterally throughout the landscape so that soils are truly three dimensional.

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