This paper is prepared to report the result of a discussion made on the effects of moisture, ramming energy, grain size distribution, bentonite and these combined factors upon green permeability of three kinds of base sands described in the previous report. Then the relation between deformability |b| and permeability was discussed. The gist of the discussion is as follows : 1) The moisture content in which the permeability becomes maximum is close to the content in which the variation of specimen height, when rammed, becomes greatest. 2) In general, when the number of blow exceeds two, there exists a proportional relation between permeability and logarithm of ramming number. If the gradient of this line showing the above described relation is culculated by the method of least squares and is named |
β|, then |
β| seems to change with the variation of grain size distribution and bentonite, moisture content, etc. 3) |
β| seems to be maximum at the suitable moisture content for each sand and it increases again as the increasing of moisture content. 4) |
β| increases with a bentonite addition. 5) Changes of permeability due to ramming is most stable in Base Sand Ⅱ.
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