Coring
at Brindisi and Egnazia (Italy), May 2008.
In mid-May 2008,
Brandon, Hohlfelder, and Oleson obtained two core samples at Brindisi and
Egnazia. The first core was taken on 14 May from the reproduction pila built by the same team in the harbour basin of Brindisi in
September 2004 (see Hohlfelder et al. 2005)
(BRI.2008.01). [View of coring in progress]
This is the
fourth core sample obtained from the pila; the
others were taken on 19 March 2005 (BRI.2005.01), 17 November 2005 (BRI.2005.02),
and 22 November 2006 (BRI.2006.01). The objective of this repeated coring is
determination of the speed and the degree of curing of the Vitruvian type
concrete used to construct the pila. It seems
that after two years the concrete has cured to a hardness approaching that of
our cores of equivalent ancient concrete, which presumably has cured completely
(Oleson et al. 2006; Gotti et al. 2008).
[View of
BRI.2006.01]
The 2008 core
included both the top and the bottom of the block; foundation sand adhered to bottom
of core. The mortar was very hard, suggesting that curing has continued, but
this particular sample seems very light in aggregate. Perhaps the ancient
builders added the aggregate more frequently than we did in the process of our
reconstruction attempt. Small lime inclusions were observed here and there (D
0.02-0.03), but the mix is very uniform. There was no sign of day joints.
Analysis of the 2008 core, which was 1.70 m in length, is in progress.
On 15 May the
same team, assisted by Dr. Rita Auriemma, Universitˆ di Lecce and several of
her students, took another core from a large concrete pila in the harbour of Egnazia, ancient Egnatia.
[map of area
with indication of core locations].
Due to technical
difficulties, only one of the three cores planned could be recovered (EGN.2008.01).
It was taken from the taller pila near north
side of ancient harbour; no. 2 on plan provided. This structure probably
belongs to the Early Imperial period. Our work was overseen and assisted as
well by Gianfranco Simonini and Ugo Adorante of the Carabinieri Subacquei detachment
in Taranto The archaeological permit was granted by Dr. Giuseppi Andreassi,
Soprintendente of the Soprintendenze per it Beni Archeologici della Puglia,
through the very kind intervention of Dr. Auriemma.
[View of coring
in progress]
The upper
surface of the pila that was sampled lay 3.20 m
below sea level, and the core, which did not quite penetrate the entire
structure, was 2.6 m long. The mortar looks very granular and somewhat porous,
with a wide variety of textures and colours. The aggregate was the local
limestone, which is a pale yellow. It seems placed at irregular intervals, and
it varies greatly in size, some of it being very large: D 0.035 to 0.60. There
are frequent lime inclusions up to D 0.015; most are around D 0.005. Occasional
orange to red potsherd fragments appear in the mortar, D ca. 0.003. These are
probably not an intentional part of the mix. The mortar contains a significant
admixture of hard, porous black lumps, D up to 0.044. The pumice lapilli have
also become black, but they remain soft.
[View of
EGN.2008.01]
We are very
grateful to Dr. Auriemma for her assistance during this campaign, and for her
gracious hospitality. Her enormous enthusiasm inspired us, just as it inspires
her colleagues and students. We thank Angelo Cossa, Melissa Mele, Martina
Lapertosa, Gianpaolo Colucci. and Miranda Carrieri. Fernando Zoccolo provided
us with some excellent photographs of our work underwater.