On Fri, 2 Aug 2013 06:21:00 -0700 (PDT), "Peter T. Daniels"
<
gram...@verizon.net> wrote:
>On Friday, August 2, 2013 9:06:44 AM UTC-4, PeterWD wrote:
>> On Fri, 2 Aug 2013 05:11:21 -0700 (PDT), "Peter T. Daniels"
>> <
gram...@verizon.net> wrote:
>
>> >Potholes are not caused by the wear and tear of heavy traffic, but by
>> >subsidence of the ground beneath the pavement, which is caused by
>> >freezing and thawing of the subsurface soil. They tend to appear suddenly.
>>
>>
>>
>> That is one mechanism. In my part of the world some potholes appear when
>> there has been no freezing and thawing of subsurface soil.
>
>"Pothole" must have a different sense there, then.
No. Road potholes are overwhelmingly caused by lack of support from
below, yes, but freeze-thaw is only one mechanism for that.
Potholes can form because of ice lenses, but also because expansive
soils expanded; because of pumping of fines from wet soil -this is a
much bigger issue for rigid pavements than flexible ones, of course;
because of poorly tamped fill, sub-base, and base courses; because of
incompatible fill placement; because of crushing of porous aggregate -
early true "Tarmac" and other slag aggregates sometimes saw this, as
have tufas, pumices, sandstones and so on, especially when placed open
graded. Soils whose properties change with moisture or vibration, or
both, can cause them. Local water leaks can cause them, too,
sometimes is a manner that mimics a sinkhole.
There are a lot of ways to make a classic asphalt-surface or
unimproved surface pothole, and many of them can, and do, occur in
places that don't freeze, and so can't thaw. Some of the best -which
is to say worst - potholes I've seen were in Central America.
>Here, they're ragged holes in the road surface with fairly sharp edges --
>clearly not caused by gradual wear.
That looks a bit like a straw man; where did anyone write of "gradual
wear?" For that matter, even a classic ice-lens pothole often comes
on slowly, with several seasons accumulation of damage before actual
breakup of the surface. The edges of the final pothole are sometimes
eased from this. Also, the water entry that causes frost heaving or
fines loss is often a product of surface wear.
>
>There are also "sinkholes," which can be much larger -- last year in
>Florida one swallowed up an entire house -- but are also due to shifts
>in underground water but not relating to freezing.
Umm, no. Changes in water level are only one of the ways that
sinkholes open, and freeze-thaw can cause a plugged sinkhole to open.
ob. Pondian et alia:
Flexible pavement= asphalt surface = tarmac = asphaltic cement
Rigid pavement = portland cement concrete
Others available on request.
Anthony "BA & PE in CE" McCafferty