THERMAL ACTIVITY OF BASE COURSE MATERIAL RELATED TO PAVEMENT CRACKING

An initial computer study using a heat transfer program showed that freeze-thaw activity during a winter, for Perryton, Texas, was centered mainly in the base course for a typical pavement. Comprehensive freeze-thaw testing showed the base course to be more active, thermally, than asphaltic concrete. The thermal activity is composed of a freeze deformation and a residual deformation. Both quantities are related to the soil moisture suction of the material. The soil moisture suction which develops in a sample is a function of the grain size, moisture, pore structure and clay mineralogy. Clay mineralogy determinations were done using x-ray diffraction to obtain the relative percentages of the clay minerals present. A direct relationship is established between the freeze deformation and clay mineralogy of the material tested. The data also demonstrate the validity of using clay mineralogy properties as a design quantity for base course material.

Media Info

  • Media Type: Digital/other
  • Pagination: 128 p.

Subject/Index Terms

Filing Info

  • Accession Number: 00137323
  • Record Type: Publication
  • Source Agency: National Technical Information Service
  • Report/Paper Numbers: TTI-2-8-73-18-2 Res. Rpt., FHWA/RD-S0478
  • Files: NTL, TRIS, USDOT, STATEDOT
  • Created Date: Sep 16 1977 12:00AM