Soil Temperature Protocol
Site Selection and Set-up
Make measurements adjacent to your Soil Moisture Study Site, or if this is not
possible, within 10 m of your Atmosphere Study Site. Study the figures of the star or
transect sampling patterns described in the Sampling Strategies and Site Layout
sections which illustrate acceptable sampling locations. If you are making these
measurements at your Atmosphere Study Site, follow the sampling pattern and site layout
for the Star Pattern.
- Select a relatively flat sunny area.
- Try to find an area with uniform characteristics across an area having a diameter of 5m.
- The ground should not be compacted but can be covered with litter or grass.
- Check the box on the Data Work Sheet if it has rained in the past 24 hours or if the
soil is frozen.
When making measurements on consecutive days, try to make your readings on days with
similar weather conditions and for soil conditions that are typical for the week you are
making them. Try to make diurnal readings around the middle of March, June, September, and
December.
Instrument Construction
Your thermometer should be most sensitive to temperature changes about 2 cm from the
tip because of the length of the temperature sensor inside the probe. To take measurements
at 5 and 10 cm depths, the thermometer will have to be pushed 7 and 12 cm into the ground.
Drill a hole in a wooden block so that when the soil thermometer is pushed all the way
into this hole, 7 cm of your probe extends beyond the bottom of the block. This will help
students maintain a uniform depth for each measurement.
Get a nail that is the same length and diameter as your thermometer probe or cut a nail
to this length. Many hardware stores carry "gutter spikes" that work for this
purpose .
Purpose
- To measure near-surface soil temperature
- To detect diurnal changes in soil temperature
- To learn about the insulating capabilities of the soil
Overview
Soil Temperatures at 5 and 10 cm depths will be measured using a probe thermometer.
Soil temperature is a function of climate, soil, soil moisture, depth and geographic
setting. This protocol collects data to explore these interactions.
Time
20-30 minutes per measurement set (6 probe measurements)
Level
All
Frequency
- Weekly: three measurements each at 5 and 10 cm depths
- Seasonally: one measurement each at 5 and 10 cm depths every 2 to 3 hours during
the daytime on two consecutive days
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Teacher Support
Key Concepts
- Soil is an insulating layer.
- Soil temperature varies with depth, soil moisture, and air temperature.
- Soil temperature varies less than air temperature.
Skills
- Reading dial scales
- Field sampling
- Observing related phenomena
- Graphing temperature cycles
Processes
Additional Materials
- Soil Temperature Data Worksheet
Prerequisites
Select a site
Teacher Preparation
Consider using the learning activities: Land, Water and Air; A Field View of Soil -
Digging Around
Student Preparation
Do the activity, Introducing Soil Temperature.
Helpful Hints
- Depth Jig: Use a wooden block to help maintain proper probe depth. See Instrument
Construction.
- Pilot Holes: Make a pilot hole if you can not easily push the temperature probe into the
ground. Hammer the pilot nail in 7 or 12 cm. Remove the nail using a slight twisting
motion. Try to minimize the amount you disturb the soil. If the hole caves in, offset
about 25 cm and try again.
- If the soil is dry and sandy/rocky, it will be very difficult to keep your pilot hole
open. You might have to wait for a natural ground wetting event to begin measurements
again.
- The temperature probe is delicate and will bend if forced. Easy does it.
Key Definitions
- Diurnal: Occuring each day; daily; Used here to indicate daily temperature cycles.
- Insulator: A material that insulates - to slow or prevent the transfer of heat.
Student Support
Scientific Justification
Animals burrow into the ground to escape extremes of hot and cold. Many seeds will not
germinate until the soil has warmed sufficiently. A warming soil can also trigger
metamorphosis in insect larvae buried in the soil. Scientists are interested in the
surface temperature in order to understand the Earth's surface energy balance - or how
much heat is radiated to space.
Synthesis Questions
- When is the soil at depth warmest?
- When would you expect deeper soil temperatures to be warmer than shallow soil
temperatures?
- Why is there a difference between the daily maximum air and soil temperatures?
Calibration and Instrument Maintenance
Task:
Monthly calibration check of field and standard thermometers
What you need:
- Dial or Digital probe thermometer
- Calibration thermometer
How to Make Monthly Calibration Checks:
Check the accuracy of your probe every month. This is particularly important if you are
using more than one thermometer, as differences or biases between two thermometers will
make your data impossible to interpret. Follow this calibration procedure:
- Use the calibration thermometer from the Atmosphere Investigation as a calibration
standard.
- Place your thermometers in water at room temperature; record their temperature readings
after 2 minutes.
- There should be less than 2° C difference between your thermometer readings and the
calibration thermometer.
- Follow the manufacturer's directions to reset dial-type thermometers, if your
differences are greater than this.
Protocol
Task:
Weekly soil temperature observations at 5 and 10 cm depth.
What you need:
- Dial or Digital probe thermometer
- Guide block, 12 cm spike and hammer
How to Measure Weekly Soil Temperature
Take three sets of soil temperature measurements adjacent to your current soil moisture
star pattern sampling location or within 10 m of your Atmospheric weather shelter at 5 and
10 cm depths. Complete these measurements within 1 hour of local solar noon and within a
period of 20 minutes.
- Expose a soil surface. Brush away grass and litter until you see the soil
surface.
- Make a pilot hole to 5-7 cm. If needed.
- Insert the thermometer to 7 cm. Insert the thermometer through your block. Gently
push in the thermometer until the tip is 7 cm below the soil surface.
- Read the soil temperature at 5 cm. Wait at least 2 minutes; then read the
thermometer every minute until consecutive readings are within 0.5-1.0° C of each other.
Record this value and the current time on the Soil Temperature Data Worksheet.
- Remove the thermometer.
- Repeat steps 1-4 in the same hole. Instead of depths of 5 and 7 cm, use depths of
10 and 12 cm, respectively.
- Report your measurements to the GLOBE Student Data Server on the Soil Temperature
Data Entry Sheet.
How to Measure Diurnal Soil Temperature
Take diurnal temperature measurements every three months, preferably during March,
June, September, and December (if the soil is not frozen). Use the procedure given for
Weekly Soil Temperature Observations but:
- Repeat the measurements every 2 to 3 hours for two consecutive days.
- Do not collect triplicate observations. Try to take at least 5 sets of readings per day.
Offset each new reading by at least 10 cm. See Figure SOIL-P-18.
- Read the current temperature at your Atmosphere Investigation Instrument Shelter and
record it on the Soil Temperature Worksheet each time you measure soil temperature.
Figure SOIL-P-18: Soil Temperature: Layout of Diurnal Observations

Data Analysis and Presentation
Construct a table in your GLOBE Student Notebook similar to the one below for recording
your results or use the Soil Temperature Data Work Sheet. Plot the data using Figure
SOIL-P-20 as a guide.
Diurnal Soil Temperature
Figure SOIL-P-19: Table of Diurnal Soil Temperatures Tucson, AZ, USA
| 2/12/97 |
2/13/97 |
ND=no data |
| Local Time |
5 cm |
10 cm |
Local Time |
5 cm |
10 cm |
Air Temp |
| 8:00 |
5.0 |
7.2 |
8:30 |
5.1 |
7.7 |
ND |
| 10:00 |
9.5 |
9.1 |
10:30 |
12.0 |
9.4 |
ND |
| 12:00 |
17.8 |
13.0 |
12:30 |
19.4 |
13.8 |
26.2 |
| 14:30 |
20.6 |
16.5 |
14:30 |
21.1 |
16.3 |
ND |
| 17:00 |
16.8 |
16.3 |
17:00 |
16.7 |
16.3 |
ND |
| 20:30 |
13.0 |
13.9 |
20:00 |
12.5 |
13.6 |
ND |
Figure SOIL-P-20: Plot of Diurnal Soil Temperatures
