Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/5628
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dc.contributor.authorallJackson, M.; Northern Arizona University, Historyen
dc.contributor.authorallLogan, J. M.en
dc.contributor.authorallScheetz, B. E.en
dc.contributor.authorallDeocampo, D.en
dc.contributor.authorallCawood, C. G.en
dc.contributor.authorallMarra, F.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.authorallVitti, M.en
dc.contributor.authorallUngaro, l.en
dc.date.accessioned2010-01-15T09:11:36Zen
dc.date.available2010-01-15T09:11:36Zen
dc.date.issued2009en
dc.identifier.urihttp://hdl.handle.net/2122/5628en
dc.description.abstractThe Grande Aula, or Great Hall, of the Markets of Trajan is an intact example of the sophisticated, domed, concrete architecture of imperial Rome, which records the expertise of Roman builders in formulating extraordinarily durable pozzolanic concretes between about AD 96 and 115. Petrographic, chemical, X-ray diffraction analyses and SEM images demonstrate that the pozzolanic mortars of the conglomeratic wall concretes contain strätlingite, a complex calcium aluminate cement hydrate (C2 ASH8) that gives modern cements high durability and compressive strength. It has not been previously recognized in ancient pozzolanic mortars. New methods of assessing bulk specific gravity of the porous concretes suggest unit weights of 1495 kg/m³ for the conglomeratic wall cores and 1200-1300 kg/m³ for the pumice-bearing vaulted ceiling mortar.Innovative point load tensile strength testing methods provide a means of evaluating the strengths of small samples of ancient, conglomeratic cementitious materials. Tests of coarse aggregate clasts, pozzolanic mortar, and the adhesive interfacial surfaces of coarse aggregate clasts (caementa) in contact with the mortar, suggest tensile strengths (ft) of 2.7 MPa for brick clasts, 1.2 MPa for Tufo Lionato tuff clasts, and 0.9 MPa for Tufo Giallo della Via Tiberina tuff clasts based on a tentative, approximate correlation with splitting (Brazilian) tests on these materials. The pozzolanic mortar and interfacial zones appear to have lower ft, in the range of 0.8 MPa to 0.5 MPa. The relatively low tensile strengths of the mortar and its somewhat tenuous adhesion to coarse aggregate clasts suggests that the caementa may have had a role in arresting the propagation of tensile microcracks that formed in the mortar, thereby increasing the composite tensile strength of the concrete. Roman builders evidently selected the complex aggregate mixes to optimize the performance and durability of the wall and vault masonry.en
dc.language.isoEnglishen
dc.relation.ispartofJournal of Archaeological Scienceen
dc.relation.ispartofseries11/36 (2009)en
dc.subjectancient Rome, concrete, pozzolanic mortar, strätlingite, tensile strength, expertise of Roman buildersen
dc.titleAssessment of material characteristics of ancient concretes, Grande Aula, Markets of Trajan, Romeen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber2481-2492en
dc.subject.INGV04. Solid Earth::04.01. Earth Interior::04.01.04. Mineral physics and properties of rocksen
dc.identifier.doi10.1016/j.jas.2009.07.011en
dc.description.obiettivoSpecifico3.10. Storia ed archeologia applicate alle Scienze della Terraen
dc.description.journalTypeJCR Journalen
dc.description.fulltextopenen
dc.contributor.authorJackson, M.en
dc.contributor.authorLogan, J. M.en
dc.contributor.authorScheetz, B. E.en
dc.contributor.authorDeocampo, D.en
dc.contributor.authorCawood, C. G.en
dc.contributor.authorMarra, F.en
dc.contributor.authorVitti, M.en
dc.contributor.authorUngaro, l.en
dc.contributor.departmentNorthern Arizona University, Historyen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextopen-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptNorther Arizona University-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia-
crisitem.author.deptNorthern Arizona University, History-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia-
crisitem.author.orcid0000-0002-4881-9563-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent04. Solid Earth-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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