FIELD STABILIZATION OF CHINLE CLAY BY ELECTRO-OSMOSIS AND BASE EXCHANGE OF IONS
A large scale soil stabilization project was initiated in July 1973. A 500-foot section, which is part of a 1300 foot cut on I-40 35 miles east of Holbrook, Arizona, was selected as the test site. The natural soil in the area is Chinle clay, a highly expansive Montmorillonite clay. The stabilization technique used on the Chinle clay was treatment with a 0.4N solution of KCl and electrochemical action. Results show that this method of soil stabilization produced a moderate decrease in the swelling characteristics of the Chinle clay, i.e., about a 50% decrease in expansive pressure and a 36% decrease in percent swell. Moreover, the electron miciographic and x-ray diffraction data have indicated some probable causative factors for the decrease in the swelling characteristics of the Chinle clay.
- Prepared in cooperation with Arizona State Univ., Tempe.
Phoenix, AZ United States 85007
Arizona State University, Tempe206 South 17th Avenue
Tempe, AZ United States 85281
Washington, DC United States 20590
- Mancini, F P
- O'bannon, C E
- Publication Date: 1975-10
- Pagination: 138 p.
- TRT Terms: Clay; Clay soils; Diffraction; Eccentricity; Electroosmosis; Expansive clays; Ion exchange; Ions; Montmorillonite; Soil chemistry; Soil stabilization; Swelling; Swelling soils; X rays
- Uncontrolled Terms: X-ray diffraction
- Geographic Terms: Arizona
- Old TRIS Terms: Base exchange; Chinle clay; Ion exchange reactions; Ion exchanging; Soil swell
- Subject Areas: Geotechnology; Highways;
- Accession Number: 00144026
- Record Type: Publication
- Source Agency: National Technical Information Service
- Report/Paper Numbers: FHWA/AZ/RD-145 Final Rpt.
- Files: NTIS, TRIS, USDOT, STATEDOT
- Created Date: Dec 15 1977 12:00AM