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Characterization
& Analysis of Surface Finishes
Material
characterization and analysis in the context of the Cliff Palace conservation
program were undertaken to describe the microstructure and chemical composition
of the earthen finishes in order to better understand their original appearance
and basic properties, especially as the latter relates to decay processes
and remedial and preventive treatments. Not addressed during this study
were archaeometric issues of raw material sourcing (provenience) or age.
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| Treatment
supervisor collecting samples for analysis, 2001. |
The eighteen
priority spaces at Cliff Palace were studied and analyzed with the main
focus of the analyses on Kiva Q, Kiva K, Room 121 and Room 64. These were
chosen as representative spaces to further explore the relationship between
space type and surface finishes. Microstructure and chemical composition
were studied through a comparison of successive layer sequencing (i.e.,
stratigraphic analysis). Polarized light microscopy, reflected light microscopy,
quantitative image analysis, and x-ray diffraction were also performed
to analyze selected samples from the above spaces in advance of treatment.
According
to the Architectural Finishes Treatment Priority Assessment, Mesa Verde
National Park, 1998-1999, the following high priority areas in Cliff Palace
(5MVO625) were selected for treatment. Mortar and surface finishes samples
were taken from the 18 selected spaces:
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| Graduate
student prepares samples in field for laboratory testing, 2001. |
Sample locations
were selected according to representative architectural elements, visible
schemes, and condition (i.e., protected areas displaying existing damage
were preferred sample locations in order to reduce damage). Samples were
extracted with a scalpel and varied in size from 0.2g to 100g depending
on the situation. The sample location and number were recorded on field
photographs and in schedule form. Given the fragile nature of many of
the multi-layer samples, specimens were carefully packed in individual
glass and plastic sample vials in cotton and clean sand and labeled. Samples
taken in previous years were merged and renumbered according to the final
sample list. Sample locations were then indicated on the treatment photomontage
elevations for each space.
All bulk samples from the 18-priority spaces were examined under a Nikon
SMZ stereomicroscope in normal reflected light. Physical properties such
as texture, hardness, color, size, shape and weight were noted. The samples
were then compared and grouped per space by location, and sample type
(e.g., modern repairs versus historical repairs). Selected representative
samples for each space were embedded in a polyester-acrylic mounting medium
(Bioplast®) and cross-sectioned with an Isomet® micro saw. Samples
from Kiva Q, Kiva K, Room 121, and Room 64 were further analyzed in greater
detail through thin section analysis. The thin-sections were vacuum imbedded
with blue dye and stained with alizarin crimson to indicate pore space
distribution (blue) and the presence of calcite (red).
Microscopical
Analysis
All
analytical techniques have limitations and hence several methods are needed
to complement and confirm results. Through gross visual examination and
low magnification reflected light microscopy, the color, texture and initial
description of the finishes were recorded. Further examination of whole
sample thin sections with polarized light microscopy (PLM) revealed both
the microstructure and fabric of the mortars including stratigraphy, determined
the relative ratio of matrix and aggregates, and identified the morphology
and mineralogy of the aggregates. X-ray diffraction was utilized to identify
the mineralogy of the fine clay and silt fractions comprising the paste.
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| Treatment
supervisor working on sample analysis using Bio-Quant software at
the Architectural Conservation Laboratory, University of Pennsylvania,
2001. |
Image
Analysis and Micromorphology
Image
analysis [Bioquant Nova® for Windows, 98 BQ Nova Version 5.00.8 MR
(R&M Biometrics, Inc.)] was used to better characterize the geo-physical
properties of the samples. Since gravimetric analysis is not possible
on these small-layered samples, image analysis provides a non-destructive
method to study and describe the various components such as the ratio
of matrix (paste) to aggregate. A micro-morphological description of each
layer per sample was prepared to support numerical and visual results
from the image analysis software and allow quantitative comparison of
layers within a sample, samples within a space, and samples across spaces
and sites.
Micro-morphology
is a unique technique for the study of multi-phase composite materials:
soils, mineral formations and transformations, and man-made composites
such as mortars and plasters. The microstructure of a plaster or wash
is the spatial distribution and total organization of the plaster/wash
system as expressed by the degree and type of aggregation and the nature
and distribution of the pores and pore space. The matrix or paste of the
plaster and washes forms a more or less continuous phase, which encloses
coarse material concretions, etc., and has been quantified for every plaster
finish layer. Basic micro-morphological concepts recorded included fabric,
matrix and structures.
The Bioquant ® Basic toolkit provides morphometric measurements and
topographic maps of hand traced areas, distances and object counts. It
can be used with or without a video camera. Customizable data structure
allows the addition of an unlimited number of user-defined calculation
arrays, as well as multiple measurement arrays of the same type. Array
names are customized to reflect the features measured.
Instrumental Analysis
X-Ray
diffraction analysis (XRD) was performed as the method of choice for identification
of the mineralogical species of the clay/silt fraction. Previously, representative
finish samples from Kiva Q and Kiva K, Cliff Palace were analyzed by George
Austin of the New Mexico Bureau of Mines and Mineral Resources in April
1999. The current analysis was performed with a Rigaku D-MAX diffractometer
at the Laboratory for Research on the Structure of Matter at the University
of Pennsylvania. The divergent slit and the scatter slit was 0.3mm, the
receiving slit and the detector was 1 degree. A copper tube mono-chronometer
was used. Bulk samples were crushed in an agate mortar and pestle and
dry sieved. For matrix analysis, particles less than 2mm were sedimented
on glass slides. For aggregate analysis, unoriented grains were mounted
on an adhesive taped "sticky" glass slide.
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