19
University of Nebraska Carbon Sequestration Program

University of Nebraska Carbon Sequestration Program

  • View
    223

  • Download
    2

Embed Size (px)

Citation preview

  • Slide 1
  • 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