University of Nebraska Carbon Sequestration Program
Slide 2
Soil Moisture Monitoring and Modeling in the Nebraska Carbon
Sequestration Project Kenneth G. Hubbard Todd T. Schimelfenig and
Cynthia J. Hays University of Nebraska Carbon Sequestration
Program
Slide 3
University of Nebraska Carbon Sequestration Program Objective
To provide continuous measurements of rainfall, irrigation and
root-zone soil water for the overall study on carbon sequestration
and real-time data for use in irrigation management
Slide 4
University of Nebraska Agricultural Research Development Center
Ithaca NE 1.Continuous irrigated maize 2.Irrigated maize/soybean
rotation 3.Rain fed maize/soybean rotation
Slide 5
University of Nebraska Carbon Sequestration Program
Slide 6
University of Nebraska Carbon Sequestration Program SYSTEM
COMPONENTS Free Wave spread spectrum wireless data transceiver
Campbell Scientific datalogger Theta-probe soil moisture sensor
Tipping bucket rain gauge
Slide 7
University of Nebraska Carbon Sequestration Program
Slide 8
University of Nebraska Carbon Sequestration Program
Slide 9
University of Nebraska Carbon Sequestration Program
Slide 10
University of Nebraska Carbon Sequestration Program
www.hprcc.unl.edu/soilm/home.html
Slide 11
University of Nebraska Carbon Sequestration Program
Slide 12
University of Nebraska Carbon Sequestration Program
Slide 13
University of Nebraska Carbon Sequestration Program
Slide 14
University of Nebraska Carbon Sequestration Program
Slide 15
(Mahmood and Hubbard, 2003) University of Nebraska Carbon
Sequestration Program S/t = p + I - ET - R o - D r S = v z, the
equivalent depth of water in the soil z = layer depth v =
volumetric water content t = time p = precipitation I = irrigation
ET = evapotranspiration R o = runoff D r = drainage
Slide 16
University of Nebraska Carbon Sequestration Program
Slide 17
University of Nebraska Carbon Sequestration Program Conclusions
Theta probes should be calibrated for each soil type It is
important to include calibration set-points that are near the end
of the range (wilting point & field capacity) Clay soils
present considerable challenge because of swelling, shrinking, and
cracking Quick disconnects and buried tubes ensure that sensors in
agricultural fields are undisturbed from year-to-year
Slide 18
THE END
Slide 19
University of Nebraska Carbon Sequestration Program