Page 274 - Geotechnical Engineering Soil and Foundation Principles and Practice
P. 274

Soil Consistency and Engineering Classification
                                                                   Soil Consistency and Engineering Classification  269

                  Color and Odor
                  Dark or drab shades of gray or brown to nearly black indicate fine-grained soils
                  containing organic colloidal matter (OL or OH), whereas brighter colors,
                  including medium and light gray, olive green, brown, red, yellow, and white, are
                  generally associated with inorganic soils.

                  An organic soil (OL or OH) usually has a distinctive odor that can be helpful for
                  field identification. This odor is most obvious in a fresh sample and diminishes on
                  exposure to air, but can be revived by heating a wet sample.

                  The details of field identification are less imposing and more easily remembered if
                  they are reviewed in relation to each particular requirement. For example, if a
                  specification is for SC, the criteria for an SC soil should be reviewed and
                  understood and compared with those for closely related soils, SM and SP and
                  respective borderline classifications.


                  12.12    THE AASHTO SYSTEM OF SOIL CLASSIFICATION



                  12.12.1   History
                  A system of soil classification was devised by Terzaghi and Hogentogler for the
                  U.S. Bureau of Public Roads in the late 1920s, predating the Unified Classification
                  system by about 20 years. The Public Roads system was subsequently modified
                  and adopted by the American Association of State Highway Officials (now
                  Highway and Transportation Officials) and is known as the AASHTO system
                  (AASHTO Method M14S; ASTM Designation D-3282).

                  As in the Unified Classification system, the number of physical properties of a soil
                  upon which the classification is based is reduced to three—gradation, liquid limit,
                  and plasticity index. Soil groups are identified as A-1 through A-8 for soils
                  ranging from gravel to peat. Generally, the higher the number, the less desirable
                  the soil for highway uses.


                  12.12.2   Using the AASHTO Chart

                  The process of determining the group or subgroup to which a soil belongs is
                  simplified by use of the tabular chart shown in Table 12.3. The procedure is as
                  follows. Begin at the left-hand column of the chart and see if all these known
                  properties of the soil comply with the limiting values specified in the column. If
                  they do not, move to the next column to the right, and continue across the chart
                  until the proper column is reached. The first column in which the soil properties fit
                  the specified limits indicates the group or subgroup to which the soil belongs.
                  Group A-3 is placed before group A-2 in the table to permit its use in this manner
                  even though A-3 soils normally are considered less desirable than A-2 soils.

                          Downloaded from Digital Engineering Library @ McGraw-Hill (www.digitalengineeringlibrary.com)
                                             Copyright © 2007 The McGraw-Hill Companies. All rights reserved.
                                                Any use is subject to the Terms of Use as given at the website.
   269   270   271   272   273   274   275   276   277   278   279