Clays and Shales of Minnesota
By Frank F. Grout
With Contributions by E. K. Soper
United States Geological Survey, Bulletin 678
Washington, Government Printing Office, 1919
[Shakopee] Page 230
At Shakopee the river alluvium is known to extend over 20 acres to the unusual depth of 30 feet. A dark clay some distance from the river is more plastic than that closer by, and the two are mixed to produce material proper for soft-mud red bricks. Some re-pressed brick are made at the same plant. The [unfired] clay slakes [quality by which a dry lump of clay tends to absorb water and fall to pieces when immersed] in three minutes and has a rather low plasticity [capability of being molded]. It requires 23 per cent of water for molding and shrinks 4 per cent on drying. Its tensile strength [maximum stress it can withstand before breaking] is about 150 pounds to the square inch and is not much reduced if the clay is rapidly dried. Burning tests resulted as follows:
Page 231
Cone No. | Color. | Shrinkage. | Absorption. |
Per cent | Percent | ||
02 | Salmon | 0 | 22 |
2 | Brown | 3 | 15 |
3 | …do | 5 | 13 |
5 | …do | … | … |
The clay becomes hard at cone 01 (2,066° F.) and reaches viscosity [change in form] at cone 4 (2,210° F.). The plant has a capacity of about 3,000,000 brick a season. Burning is conducted in a patent 30-arch kiln by what is known as the John G. Boss system.