Department of Soil&Crop Sciences

  • Print
  • Email
  • Decrease text size
  • Increase text size

Quantifying Spatial and Temporal Heterogeneity of Soil Cracking to Model Watershed Surface Hydrology

NameTitle Email
Dr. Cristine Morgan Project Leader cmorgan@ag.tamu.edu
Dr. Kevin McInnes Co-PI KMcInnes@ag.tamu.edu
Dr. Andrea Kishne Post Doc. AKishne@ag.tamu.edu
Takele Dinka PhD Student takele_72@tamu.edu
Leo Rivera MS Student LRivera@ag.tamu.edu

Overall Objective:hydrology

Shrink-swell properties Vertisols have an impact on a watershed hydrology, which influences the flow rate of water and pollutants into a soil and/or surface water. Therefore the goal is to characterize, quantify and model, both temporally and spatially (across catena and depth), shrink-swell behavior Vertisols. This contributes to the study and better understanding of a watershed hydrology and to a sustainable water management.

Specific Objectives:

  1. Quantify cracking behavior across a Houston Black catena
  2. Compare estimates of crack volume in two Texas Vertisols
  3. Quantify and model, both temporally and spatially (across catena and depth), shrink-swell behavior of a Vertisol under different vegetations
  4. Develop a smart sampling strategy for quantifying hydraulic conductivity of benchmark soil series under different management and landscape conditions

Results:

  • Rivera, L. and C.L.S. Morgan. Comparing Methods of Estimating Crack Volume in Shrink-Swell Soils. Undergraduate Research Thesis, TAMU. 2008

Funding:

  • Texas NRCS Soil Survey

Presentations

  • Rivera, L., C.L.S. Morgan A. Kishne, C.T. Hallmark. 2008. Estimating Crack Volume in Two Texas Vertisols. Southern Regional Cooperative Soil Survey Conference. Gainsville, FL.
  • Rivera, L., C.L.S. Morgan A. Kishne, C.T. Hallmark. 2008. Estimating Crack Volume in Two Shrink-Swell Soils. Soil Survey and Land Resources Workshop. College Station, TX.

For more Information on this project contact: Dr. Cristine Morgan cmorgan@ag.tamu.edu