New Mexico Geological Society Annual Spring Meeting — Abstracts


MINERALOGY OF THE CLAY-SIZE FRACTION OF ADOBE SOILS IN NEW MEXICO: IMPLICATIONS FOR USE IN BUILDING MATERIALS

George S. Austin

New Mexico Bureau of Mines and Mineral Resources, Socorro, NM, 87801

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In 1988, 33 commercial adobe brick producers, 28 pressed-earth-block, and two rammed-earth contractors were located in New Mexico. Extensive analyses of the materials used in earth-block production indicated that sand-and-larger grain-size materials make up from 27 to 89% of earth construction materials, whereas clay-size material varies from 1 to 15% with silt making up the remainder. The clat mineralogy of adobe soils quite variable, but commonly consists of about equal portions of expandable clay minerals (smectite and mixed-layered illite-smectite or I/S) and nonexpandable clay minerals (kaolinite, illite, and chlorite). Calcite (CaCO3) is nearly ubiquitous, particularly in the
smaller-size fractions of adobe soils, and appears to play a far more active role in binding particles together in earth construction materials than previously considered possible.

pp. 31

1989 New Mexico Geological Society Annual Spring Meeting
April 7, 1989, Macey Center
Online ISSN: 2834-5800