Acid Rain and Our Nation's Capital: A Guide to Effects on Buildings and MonumentsMcGee, E. S.
History
Acid Rain and Our Nation's Capital: A Guide to Effects on Buildings and Monuments
McGee, E. S.
Acid rain -- Environmental aspects -- Washington (D.C.); Building stones -- Deterioration -- Washington (D.C.)
We will follow the marble balustrade around the building, noting
differences in deterioration. Some parts of the balustrade have
obviously been replaced, thus enabling us to observe various stages in
the stone deterioration. The edges of the balusters are sharp when new
and become rounded as they age. Blackened alteration crusts have
accumulated on the sheltered sides of the balusters and under the
overhanging top of the balustrade. In some spots under the rail the
blackened crust has spalled off, exposing fresh surfaces and more
vulnerable stone. Some carvings on the balustrade corners are worn,
whereas others have blackened alteration; this difference in weathering
may be due to local effects of wind and rain. Along the steps leading to
the terrace on the west side of the Capitol, gypsum has accumulated on
large areas of the wall. Gypsum can accumulate on any surface that is
not washed by water.
As you walk north along the west side of the Capitol, look at the
central part of the building. The walls here are painted sandstone.
Despite recent restoration of the building, you can see evidence of past
stone deterioration, including the accentuated lines from bedding in the
stone and the pock marks where rounded inclusions have disappeared. We
will see an example of this same sandstone that is not painted in the
buildings near 17th Street.
At the northeast corner of the Capitol building, the marble balustrade
ends in square blocks like the ones we first examined. Here you can see
an example of preferential dissolution where the silicate mineral
inclusions remain and the calcite around them has been dissolved away.
Also, on the north side of this block, examine the blackened grains on
the top surface with a hand lens. Not all of the black material you see
on stone is gypsum; some is of biological origin, probably algae or a
fungus.
[Illustration: A marble block that forms the northeast corner of the
Capitol balustrade shows preferential erosion of the calcite around
a silicate mineral inclusion.]
To continue the tour, follow the pathway that heads west along the
north side of the Capitol, towards First Street. As you approach First
Street you will see a sandstone, diabase (a dark igneous rock), and
granite fence with various carvings. Because these stone types are
resistant to acid attack, the carvings show little damage.
The Peace Monument—Site 2
[Illustration: The Peace Monument, dedicated in 1878, is made of
Italian marble.]
This monument, dedicated in 1878, is made of marble from Carrara, Italy.
The statue does not show much damage, but if you look closely, you can
see alteration crusts (some are light orange) in protected places and
graininess and roughness in places that are exposed to rain. Carved
statues present varied surfaces that direct rain washing and runoff.
[Illustration: MAP OF WASHINGTON]
Public-domain text, read in full here on John Shaqi.
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