Module 06 Part 1 Weathering and Soil Lab

.docx

School

Northern Virginia Community College *

*We aren’t endorsed by this school

Course

105

Subject

Geology

Date

Dec 6, 2023

Type

docx

Pages

6

Uploaded by ElderTrout2804

Report
Name: _________________ GOL 105: Weathering and Soil Lab Objective: The objective of this exercise is to help familiarize you with the basic soil profile, the processes responsible for creating each of the horizons within the profile, and the general characteristics of weathering of geologic material . Introduction: This exercise will utilize the information contained in Chapter 6 (Weathering and Soil) in your textbook. All work can either be completed directly on this document (save it to your hard drive with a file name that includes your last name, then complete the exercise, save your copy, and then submit it via Blackboard). Another option is to print it, draw/write on the paper, then scan or photograph it to make digital files capable of being submitted via Blackboard. Note that you will have to draw on several photos, either with pen/pencil or digitally. Directions: 1. Read Chapter 6 (Weathering and Soil) in your textbook. 2. Complete Table 1 . Identify the soil horizons in a typical soil profile. Fill in the name of the soil horizons in the left hand column of the figure, and give a brief description of the content and processes in each of the horizons in the left hand column. (10 pts) 3. Complete Table 2 . Identify the five (5) most important factors affecting the development of a soil at any given location. List each factor separately in the left side column of the table, and then briefly discuss a few specifics on how this may affect the development of a soil profile. Which horizons will be most affected by each factor? (10 pts) 4. Complete Figures 3, 4, and 5 . Try your hand at identifying the various soil horizons in each of these two figures. Draw the boundaries on the photo , and clearly label each horizon with the corresponding letter (O, A, E, B, etc .). Labels may be placed in the white space next to the photo for clarity. (10 pts) Revised: December 2018 Page 1 of 6
Name: _________________ Figure 1: A Typical Soil Profile Name of soil horizon Description ____ O ___ Horizon (Topsoil) Mostly organic material, especially still-recognizable plant litter Lots of microscopic life, which contributes oxygen, carbon dioxide, and organic acids ____ A ___ Horizon (Topsoil) Mostly mineral matter High biological activity Up to 30% humus (partly decomposed organic matter) ____ E ___ Horizon (Zone of Leaching) Light colored Little organic material As water filters down through here, finer particles are carried away Soluble inorganic soil components are carried deeper by the water ____ B ___ Horizon (Subsoil ; Zone of Accumulation) Lots of the material that gets filtered out of E ends up here Enhanced water-holding ability due to the collection of fine clay particles Can form a very compact, impermeable layer called hardpan ____ C ___ Horizon Partially altered parent material Parent material is easily identifiable Has not yet crossed the threshold separating regolith and soil Bedrock Unweathered parent material Revised: December 2018 Page 2 of 6
Name: _________________ Table 2: Factors Affecting Soil Formation Factor Affecting Soil Formation Description Parent Material Different weathering rates of different materials affect the rate of soil formation Chemical makeup of parent material affects soil fertility Climate Variations in climate determine dominant weathering type Varying precipitation determines what material gets removed from the soil Controls the type and numbers of life that is present Plants, Animals, and Microbes Add organic matter to the soil Partially effects soil fertility Decay creates organic acids, which speeds up weathering Increases water retention due to organic matter being able to hold a lot of water Some organisms mix the soil by digging and burrowing Time More time results in thicker layers of soil that bear less resemblance to their parent materials Topography within a Climate Zone Topography affects the amount of erosion that occurs and the water content Slope orientation determines the amount of sunlight exposure, which then determines temperature and moisture Revised: December 2018 Page 3 of 6
Your preview ends here
Eager to read complete document? Join bartleby learn and gain access to the full version
  • Access to all documents
  • Unlimited textbook solutions
  • 24/7 expert homework help