GLOBE Protocol eLearning Title

GLOBE Protocol eTraining

This module will provide you an overview of the protocols of the GLOBE Pedosphere Investigation. It also explains how to define soil study sites for both Soil Moisture and Temperature and for Soil Characterization. After completing it you will be prepared to proceed to learn any and all of the soil measurement protocols.
 

Pedosphere (Soil) eTraining Preview

Pedosphere (Soil) eTraining

Welcome to the Pedosphere eTraining. Students and scientists investigate the pedosphere – the global layers of soil – through collection of data that are generally unavailable from any other sources and address the significant local variations in soils.

The training in this section will introduce you to the investigation of soil and the seven GLOBE Program measurement protocols. You will also learn how to select and define a soil site.

Finally, you will see how to report your data to GLOBE and visualize data using the GLOBE visualization system.

GLOBE Protocol eTraining Activities

Equipment

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Activities

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PROTOCOLS

Click a protocol name to view the training and assessment for that topic.

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Soil Characterization

 

Soil Moisture (Gravimetric)

 

Soil Temperature

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Soil Moisture (SMAP)

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Soil Infiltration

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Soil Bulk Density

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Frost Tube

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Soil Characterization

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eTraining: Soil Characterization

This module provides step-by-step instructions in how to characterize soil by its structure, color, consistence, texture, and abundance of roots, rocks, and carbonates. First, learn how to select, expose and define a Soil Characterization protocol study site. Then, review how field samples of soil are collected and characterized.

Time Requirement 1.5 hours

eTraining: Soil Moisture (Gravimetric)

Learn how to collect soil samples from the field, then determine the soil water content by calculating the difference between the wet sample mass and the dry sample mass. You will be able to relate soil moisture measurement to the physical and chemical properties of the soil. In this instance, gravimetric means determining the amount of moisture in the soil by weight.

Time Requirement 1.5 hours

Before you begin

Before you begin

Safety first!

Make sure the site is safe for digging. Coordinate with local utility companies and school maintenance staff to make sure you do not dig into utility cables, gas pipes, water, sewer, or sprinkler systems.

Select your site


Image courtesy, Izolda Trakhtenberg

 

Ideal

Acceptable

Unacceptable

Site is representative of the local landscape

   

Ground cover is natural vegetation

Lawns, agricultural sites, or other managed landscapes 

Ground cover is very different than the surroundings

Relatively undisturbed

Some disturbance

Broken or packed ground

At least three meters from buildings, roads, paths, and playing fields

 

Immediately adjacent to human activity

Near an atmospheric measuring station

   

Oriented so that the sun shines on the soil profile at the time students carry out the soil characterization measurements

Existing exposed profiles that are in shadow or pits dug under tree canopies

 
  View Site Characterization eTraining →
Selecting, Exposing, and Defining a Soil Characterization Site (pdf) >

Initial Measurements Landing Page

Initial Measurements

Describe Your Site

  1. Observe and describe your site before you conduct your soil investigation.
  2. Record the site characteristics. At a minimum, these include the following. (See the Soil Characterization eTraining to learn about additional measurements.)
    • Surface state
    • Surface cover
    • Canopy cover
  3. Take landscape photographs of the site to the North, East, South, and West of the profile.

View Site Characterization eTraining →
Soil Characterization protocol Field Guide (pdf) >

Why is it important?

Handling Data

View resources on GLOBE data entry

Soil Moisture Is Important Because It Affects:

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Plant Nutrient Uptake
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Water for Plant Use
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Water Storage
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Atmospheric Humidity
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Weathering
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Flooding

Soil acts like a sponge spread across the land surface. It absorbs rain and snowmelt, slows run-off and helps to control flooding. The absorbed water is held on soil particle surfaces and in pore spaces between particles. This water is available for use by plants. Some of this water evaporates back into the air; some of this water is transpired by plants; some drains through the soil into groundwater.

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Why is it important?

By studying the soil in your area and reporting these data to GLOBE, you will make an invaluable contribution to our knowledge of planet Earth.

As you take your soil measurements, remember that you are likely the only ones who will study your specific soil. For much of this critical information, there exists no other way to study the soil in your community. Your contribution to science will be important and unique.


 

Explore Connections to Other Spheres

Why is defining soil characteristics important?

Soil characterization is a fundamental step in describing and analyzing soil as part of the Earth system. The characteristics you identify will help to explain the role of the soil in exchanging matter and transferring energy with the atmosphere, biosphere and hydrosphere.

Soil characterization measurements are taken for many reasons, including:

  • supporting the interpretation of soil moisture and temperature, land cover, and atmosphere measurements;
  • complementing and extending land cover mapping;
  • developing soil maps of a region; and
  • providing information for computer modeling.

Image: Jenn Glaser and Russanne Low

Explore further: Earth as a system: Soils Bundle

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Frequently Asked Questions (FAQs)

It depends on which soil property you are examining. Soil properties change over time on different timescales. Properties such as temperature, moisture content, and local composition of air change over a period of minutes or hours. Other properties change over months or years, including soil pH, soil color, soil structure, bulk density, soil organic matter, soil fertility, and the microorganisms, animals and plants in the soil. Over much longer timescales, that is, tens to hundreds and thousands of years, changes in mineral content, particle size distribution, horizons and particle density take place. These last measurements you need to do only once.

Landing Page Feedback

Feedback

Please provide us with feedback about this module. This is a community project and we welcome your comments, suggestions and edits! Comment here: eTraining Feedback

Do you have questions after reviewing this module? Please contact us at globehelp@ucar.edu.

Landing Page Credits

Credits

Content: Izolda Trachtenberg, Dixon Butler, Russanne Low

Photographs: Izolda Trachtenberg

Soil Profile Photos: r. John Kimble and Sharon Waltman, USDA Natural Resources Conservation Service, National Soil Survey Center, Lincoln, Nebraska,

Illustrations: Rich Potter

Cover Art: Jenn Glaser, ScribeArts