360R-06 Design of Slabs-on-Ground



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Design of Slabs-on-Ground

9.2—Definitions
Selected terms and expressions that appear in 
Chapter 9
are defined and explained.
allowable differential deflection—the amount of slab
deflection that can be tolerated by the type of superstructure
supported by the slab or equipment operating on the slab.
differential deflection distance—the total slab length
may not be the proper distance over which to evaluate the
acceptability of the expected differential deflection. Analysis of
the locations of maximum and minimum deflections shows
that several such locations may occur in longer (or wider)
slabs; that is, the slabs experience multimodal bending
(Thompson and Anderson 1968). All such bending, however,
occurred within a distance of 6
β from the edge of the slab.
Using a length of L or 6
β, whichever is smaller, when deter-
mining the allowable differential deflection, will limit the
deflection to an acceptable amount, and this length is called
the differential deflection distance.
differential soil movement y
m
—this is the expected
vertical movement of the perimeter soil due to type and
amount of clay mineral, its initial wetness, the depth of the
zone within which the moisture varies, and other factors (PTI
2004). The differential soil movement will often be greater
than the allowable deflection.
edge moisture variation distance e
m
—also known as the
edge moisture penetration distance, e
m
is the distance
measured inward from the edge of the slab over which the
moisture content of the soil varies. An increasing moisture
content at increasing distances inside the slab perimeter is
indicative of a center lift condition, whereas a decreasing
moisture content indicates an edge lift condition.
lift conditions—several terms refer to the shape of a slab
or the stresses generated within a slab during the transition
period from the as-cast shape to the intermediate or long-
term shape. If the moisture content of the soil beneath the
slab changes after construction of the slab, it will distort into
either a center lift condition (also termed “center heave” and
“doming”) or an edge lift condition (also called “edge
heave” and “dishing”). The center lift condition is a long-
term condition and occurs either when the soil beneath the
interior of the slab becomes wetter and expands, when the
soil around the perimeter of the slab dries and shrinks, or a



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