fattdad - one day, I am going to come to the eastern seaboard (I think that is where you are) and we are going to have a nice discussion over many things over many a single malts! - or you can come out to Bali!!
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- sorry - I don't mean to highjack the thread:
I am not a big fan of ASTM. In many ways, I think that they complicate descriptions too much - and when you get down to it, their descriptions rely "heavily" on percentages of the constituent parts too - they just couch the wording in a different way.
In thinking that only the ASTM way "works" one sells out many pioneering geotechnical firms - they didn't use the USCS; used the "percentage" way were involved in building very very many very very important projects. I started work for Geocon in Canada (a long established firm) in 1977 and am familiar with almost all of their early reports (1954 to 1977) from before joining them. They never used "elastic silt", "fat clay" or any of the other terms bandied about by ASTM. Still, their history of major projects in the mining, pulp and paper, steel mill, ports and wharves for the St. Lawrence Seaway, oil refineries (Sarnia, for example) were built with success. Most of Golder's founders were indoctrinated at Geocon before starting Golders and in reports that I saw of theirs when I was with them and subsequently, again, no mention in the logs of their reports the ASTM terminology. Both firms and many others lived with clayey silt, trace sand; silty clay; etc. See attached page from Soderman and Quigley as found in the Canadian Geotechnical Journal (CGS - don't be mad!) - notice that they use clayey silt. This is found, too, in the original USCS charts (as found in Lambe and Whitman among others). See also the Canadian Guide to the Field Description of soils - they also indicate the use of clayey silt (a term not found in ASTM). Review the borehole logs and descriptions form the Canadian Geotechnical Journal articles in the 1960s, 1970s; see the example borehole logs in Fang's Foundation Engineering Handbook. I admit that with the younger set "growing up with ASTM" there is a shift towards the ASTM nomenclature (hell, I never even read an ASTM testing spec for 20 years after I started - we used Lambe's Soil Testing book for our testing). Still, we must give credit to the developers of geotechnical engineering. They did fine without ASTM.
One argues that ASTM is a "behavoural" classification system - if so, then why so much reliance on %ages of constituents as I indicated above. See Fig 1a in D2487 - you need to know 30%, 15%, 50%. Say I have a soil that is fine grained. Less than 15% is "plus #200 sieve". I decide to do two Atterbergs on the same sample. One test gives LL = 51; the also gives LL = 49. The plasticity index of the first is 23, and the second is 21. By ASTM the first is to be called a Fat Clay. The second a Silt. Now, to be honest, these two terms, to me, are diametrically opposite, yet they are the same sample. What is the behavoural difference of the two? I couldn't say. It is similar as what is the "line you draw in the sand" to apply the consistency descriptor - or the relative density descriptor. Anyone venture a guess on that? And how do you classify a varved clay? or is it a varved fat clay? or a varved silt? or a varved ???????
The bottom line, and I think that fattdad, I, and others will agree, is that one must have the experience and "feel" of knowing the material at which you are looking, touching (tactile) and smelling to have the right appreciation of whether a material is one way or the other. A common descriptor system is useful in data-base work but as I pointed out in my little example above, very slight differences in the Atterberg limits may very well slant one's view immensely.