|
Modesto Montoto San Miguel,
Chair Dept. of Geology, Univ. of Oviedo
Rosa Maria Esbert Alemany
(Faculty and Technical Staff)
Jose Ordaz Gargallo
Lope Calleja Escudero
Vincente Gomez Ruiz de Argandona
Luis Miguel Suarez del Rio
Javier Alonso Rey
Carlos de Llanos Gonzalez
Beatriz Perez Garcia
(Graduate Students)
Nicolas Manuel Martinez Alvarez
Carlota Maria Grossi Sampedro
Beatriz Menendez Villar
Antonio Martinez Hernando
Luis Valdeon Menendez
Rosa Maria Marcos Fierro
Mercedes Vazquez Llorens
Angel Martinez Nistal
Period of Activity: 6/87 to 12/89
Project Abstract
Bibliographic retrieval has been carried out, and statistics
on papers presented in the international congresses and symposiums
on the deterioration of monumental stones during the last twelve
years were presented in the first progress report. Future work will
be restricted to sandstone and granite, and will include acoustic
emission/microseismic activity as a new nondestructive procedure.
Authorization has been received to study the Monasterio de Ripoll
and the Monasterio de El Escorial.
Primary and Secondary Publications
Montoto, M., "Evaluation In-Situ of the State of Deterioration
of Monumental Stones by Non-Destructive Sonic Techniques: Monastery
of San Lorenzo El Real De El Escorial (Madrid, Spain)," Final Report,
Department of Geology-Group of Petrophysics, University of Oviedo,
Oviedo, Spain, July 1989.
ABSTRACT-This report summarizes the petrophysical interpretation,
by means of ultrasonic studies, of the deterioration process affecting
the granodiorite rock of the Monastery of El Escorial along the
period of time the rock has been placed in the site.
Aging tests for reproducing the deterioration process and corresponding
ultrasonic monitoring in the laboratory have been designed. Three
types of aging tests have been selected: salt crystallization, thermal
cycling, and freeze-thawing. The ultrasonic parameters used in this
study were: wave amplitude, wave energy, wave duration, number of
counts, and the velocity of longitudinal waves (Vp). From laboratory
tests, an inverse relationship can be found between the ultrasonic
parameters and the degree of artificial deterioration. The acoustic
parameter best displaying this relation is the energy and the most
aggressive aging test is the freeze-thawing one.
In situ tests have been programmed based on the laboratory results.
Measurements were made in different rock masonry at selected stations
representative of all the forms of deterioration in the monument.
A quality index was assigned to each of the measurement stations
according to their deterioration state. The relationship between
this index and the acoustic parameters is statistically analyzed;
three deterioration groups have been obtained. For in situ tests,
an inverse relationship between the rock deterioration degrees and
the acoustic parameters is found. The energy is the best acoustic
variable to define the deterioration groups and classify each of
the measurement stations in one of the groups.
Montoto, M., L. M. Suarez del Rio, and A. Rodriguez Rey, "Métodos
no Destructivos para la Caracterización de los Materiales
Rocosos," 1er Seminario sobre Estudio, Diagnosis y Tratamiento de
la Erosión Lítica en los Monumentos, Granada, Spain,
April 27-30, 1987.
ABSTRACT-By using nondestructive techniques (NDT), rock types used
in the construction of historic monuments can be characterized.
Among NDT's the most notable methods are those that are based in
the analysis of elastic waves, induced or spontaneous, that travel
along their empty spaces, fractures, and/or detached facing slabs.
These ultrasonic procedures have been extensively studied, disseminated,
and commercialized; therefore, many of them, due to their portability,
are more easily applicable in practical professional problem areas.
At the same time, using ultrasonic techniques, the tensile status
of the material can be appraised and possible unstable mechanics
determined. This is carried out by the analysis of the elastic waves
that spontaneously free all solids subjected to stress. This passive
ultrasonic procedure, acoustic emission, or microseismic activity,
AE/MA microseismic activity, can be combined with other active injections
of ultrasound in the materials in order to determine and map fissures
and inhomogeneities.
Calleja, L., M. Montoto, B. Perez-Garcia, L. M. Suarez del Rio,
A. Martinez Hernando, and B. Menendez Villar, "An Ultrasonic Method
to Analyze the Progress of Weathering During Salt Crystallization
Laboratory Cycles," International Symposium, The Conservation of
Monuments in the Mediterranean Basin, Bari, Italy, June 7-10, 1989.
ABSTRACT-A nondestructive ultrasonic procedure to study deterioration
during laboratory aging tests is described. Salt crystallization
aging tests were carried out on a sandstone, similar to that used
in the Santa Maria de Ripoll Monastery (Gerona, Spain). Before,
during, and after tests, steady ultrasonic signals from an ultrasonic
pulse generator were passed through cubic samples of rock and, after
traveling through the samples, the amplitude, duration, energy,
and count number of the elastic waves were received and processed.
Preliminary results show an inverse relationship between the acoustic
variables and the observed degree of deterioration of the rock samples.
Montoto, M., L. Calleja, B. Perez Garcia, L. M. Suarez del Rio,
V. G. Ruiz de Argandona, R. M. Esbert, and C. M. Grossi, "A Non-Destructive
Ultrasonic Procedure to Evaluate In Situ the Relative Deterioration
State of Monumental Stones: Preliminary Results," European Symposium,
Science, Technology, and European Cultural Heritage, Bologna, Italy,
June 13-16, 1989.
ABSTRACT-To evaluate in situ the relative deterioration of monumental
stones, a nondestructive ultrasonic procedure has been in development:
ultrasonic waves are introduced into the rock and processed to evaluate
the ultrasonic parameters of velocity (Vp) velocity, amplitude,
duration, energy, and count number.
The procedure was applied to two Spanish Monasteries, one built
with granodiorite (El Escorial, Madrid, the results of which are
included here) and the other built with sandstone (Sta. Maria de
Ripoll, Gerona).
Laboratory aging tests, involving monitoring of the above-mentioned
ultrasonic parameters, were performed as a basis for interpreting
the in situ measurements. The energy seems to be most sensitive
as an indicator of the state of rock deterioration, so the value
obtained for a masonry block in the monument can be used to classify
the rock into one of preset deterioration groups.
Perez Garcia, B., M. Montoto, L. Calleja, N. Martinez Alvarez,
and J. Ordaz, "An Acousto- ultrasonic Method for Evaluating the
Deterioration Degree of Monumental Stones," Ultrasonics International
89 Conference, Madrid, Spain, July 3-7, 1989.
ABSTRACT-An ultrasonic procedure is being developed for evaluating
the relative deterioration of monumental stones. This method consists
of the injection of ultrasonic signals and the processing and analysis
of the signals after traveling through the rock. The selected ultrasonic
parameters are: velocity of longitudinal waves, amplitude, duration
, energy, and count number. Specimens of sandstone similar to one
of the types used in the building of the Monastery of Santa Maria
de Ripoll (Gerona, Spain) have been subjected to laboratory aging
and monitoring of the variation of the above-mentioned ultrasonic
parameters.
Rodriguez-Rey, A., G. A. D. Briggs, T. A. Field, and M. Montoto,
"Acoustic Microscopy of Rocks," Journal of Microscopy, Vol. 160,
Pt. 1, October 1990, pp. 21-29.
ABSTRACT-Acoustic images of two common rocks, granodiorite and
limestone, are studied to explore the kind of geological information
that they can provide. Rayleigh waves which travel in rock specimens
confined to within a depth of a wavelength or so from the surface
are mainly affected in their propagation by crystal anisotropy and
surface discontinuities. Therefore, acoustic microscopy makes possible
a detailed identification of intragranular structures in the rock-forming
minerals (very fine cracks, grain and subgrain boundaries,etc.);
these features may appear more sharply than in transmitted polarized
light microsopy or in scanning electron microscopy. In particular
the acoustic images are very effective in microfractographic studies
because they can show not only the finest cracks, even those much
less than a wavelength wide, but also their position in relation
to the grain and subgrain structure.
Rodriguez, A., "Applications of Scanning Acoustic Microscopy to
the Study of Rock Materials," Seminar, University of Oxford, Department
of Metallurgy and Science of Materials, December 1, 1987.
ABSTRACT-None available.
Briggs, G. A. D., C. M. W. Daft, A. F. Fagan, T. A. Field, C. W.
Lawrence, M. Montoto, S. D. Peck, A. Rodriguez-Rey, and C. B. Scruby,
"Acoustic Microscopy of Old and New Materials," Acoustical Imaging,
Vol. 17, ed. J. Kushibiki, N. Chubachi and S. Himizu, Plenum Press,
1989, pp. xiii-791.
ABSTRACT-None available.
Montoto, M., L. Calleja, B. Perez, and R. M. Esbert, "Evaluation
In Situ of the State of Deterioration of Monumental Stones by Non-Destructive
Ultrasonic Techniques," Materials Issues in Art and Archaeology,
Vol. 185, 1991, Proccedings of the Materials Research Society, Spring
Meeting, San Francisco, California, April 16-20, 1990, pp. 273-284.
ABSTRACT-A nondestructive ultrasonic procedure is under development
for evaluating in situ the relative deterioration of monumental
stones.Ultrasonic waves are injected into the rock and, after traveling
through the rock, are registered, processed, and petrophysically
interpreted. The procedure is being applied to two Spanish Monasteries,
one built with a granitic rock (El Escorial, Madrid), and the other
built with sandstone (Sta. Maria de Ripoll, Gerona).
The methodology implies: in situ categorization of the observable
deterioration forms, sampling in the quarries, laboratory aging
tests and continuous ultrasonic monitoring, in situ data acquisition,
evaluation of the ultrasonic parameters by signal processing, and
stepwise discriminant analysis. All that information is petrophysically
interpreted for an approximate assignation of the in situ studied
masonry blocks to the categorized deterioration degree.
Final in situ results from the Monastery of El Escorial are presented
here. Among the studied ultrasonic parameters, "energy" is the most
useful of all of them and velocity the least.
Esbert, R. M., M. Montoto, L. M. Suarez del Rio, V. G. R. de Argandona,
and C. Grossi, "Mechanical Stresses Generated by Crystallization
of Salts Inside Treated and Non- Treated Monumental Stones: Monitoring
and Interpretation by Acoustic Emission/ Microseismic Activity,"
Materials Issues in Art and Archaeology II, Vol. 185, 1991, Proceedings
of the Materials Research Society, Spring Meeting, San Francisco,
California, April 16-20, 1990, pp. 285-296,.
ABSTRACT-The crystallization of salts into building stones is one
of the most common and severe deteriorating phenomenon developed
on historic buildings. To evaluate their mechanical effects on treated
and nontreated stones, laboratory aging tests and their corresponding
monitoring of the acoustic emission/microseismic activity, AE/MS,
have been planned.
Therefore, salt crystallization tests have been performed on a
high-porosity, 30%, limestone. limestone.; Each test consisted of
fifteen cycles of immersion of specimens in salt solution (14% Na2SO4.10H2O)
for 4 hours, drying in an oven at 60 C for 14 hours, and final cooling
at room temperature for 6 hours. The treated specimens were consolidated
by total immersion in ethyl silicate-Tegovakon V and protected with
a water repellent, oligomeric polysiloxane- Tegosivin HL-100.
The AE/MS was monitored in the 100-300 KHz range. The preliminary
results show a very different AE/MS behavior between nontreated
and treated specimens; the AE/MS rate peaks of the former being
more frequent and smaller.
Montoto, M., "Acoustic Emission in Stone Conservation," 5th Conference
on Acoustic Emission/Microseismic Activity in Geologic Structures
and Materials, Pennsylvania State University, June 11-13, 1991.
ABSTRACT-The acoustic emission/microseismic activity could represent
a very valuable tool during the relevant stages of diagnosis and
monitoring involved in stone conservation programs. The most relevant
applications in this field are summarized; further research on some
aspects not yet studied is suggested. In general, four main possible
areas of application can be considered regarding AE/MS and stone
conservation: (a) Stability of the rock foundation of the Monument,
(b) Stability of the Monument as an architectural object, (c) State
of the stress and characterization of the rock masonry and, (d)
Evaluation of the treatments applied to the stones after a conservation
program.
|
 |
|