Читать книгу Monument Future - Siegfried Siegesmund - Страница 311

According to the results of the analysis of the material characteristics, the rocks that make up the Stone Standing Buddha and Stone Chamber are pinkish medium-grained biotite granite, milky medium-grained biotite granite, porphyritic granite, and aplite. The host rock is pinkish medium-grained biotite granite that accounts for more than 90 percent of the total, while other types of rocks are used as stones to fill the inside or between the walls (Fig. 2). Particularly, the Urna on the forehead of the Stone Standing Buddha and one Stone Seated Buddha enshrined inside the chamber consist of limestone.

Figure 2: Diagram showing the proportion for constituent rocks of the Stone Chamber in the Mireukri temple site.

The pinkish medium-grained biotite granite, a representative rock, is about 1 to 5 mm in grain size and composed mainly of quartz, alkali feldspar, plagioclase, and biotite. The magnetic susceptibility is measured in the range of 0.08 to 2.04 (× 10^–3 SI unit) in the Stone Standing Buddha and 0.01 to 2065.24 (× 10^–3 SI unit) in Stone Chamber. Generally, it is distributed below 2.00 × 10^–3 SI unit and the mean values are similar.

As a result of on-site investigation, damage types in the Stone Standing Buddha are mainly observed for physical damage such as crack, scaling, scale-off, and break-out, while chemical deterioration is found to be black, brown, white discoloration and believed to be red pigment in the lips. No biological damage is identified as the cleaning treatment was completed. As each damage type of the Stone Standing Buddha occupies below 6 % of the whole, by and large, the Stone Standing Buddha was found to be of good condition in deterioration assessment. In the case of the Stone Chamber, complex cracks in each material are mostly observed and discoloration caused by oxidation of minerals like iron and manganese is partially confirmed.

Infrared thermography analysis showed local exfoliations in the entire of the Stone Standing Buddha, which covered with surface contaminants before cleaning. Exfoliation occupied less than 3 % overall but the frequency of occurrence was high. Relatively large exfoliations were identified in the left arm and the pedestal.

The results of P-XRF measurement on surface contaminants indicated that manganese, iron, calcium 207and lead acted as the main determinants of black, brown, white discoloration and red pigment, respectively. Remarkably, the content of lead on the face of the statue was measured to be 18 times higher than other parts. This allows us to estimate the possibility of using the white pigment, hydrocerussite (2PbCO₃·Pb(OH)₂). It is necessary, however, to carry out further research to investigate a definite cause for this phenomenon (Fig. 3).

Figure 3: Current state of the face on the Stone Standing Buddha and result by P-XRF analysis. (A) Front view of Buddha’s face, (B) Urna and heart-shaped small hole on the face, (C) Measurement points of P-XRF and 2D modeling of Pb contents.

Physical evaluation by ultrasonic velocity was performed at 571 spots on the surface of the Stone Standing Buddha. As a result of ultrasonic measurements, the mean ultrasonic velocities of 2,710 m/s in the Bogae and over 3,000 m/s in the rest of the statue were shown. By applying the absolute coefficient of weathering (K), the weathering indices of the whole were estimated to be in the moderately weathered (MW) stage except for the Bogae which was in the highly weathered stage.

The ultrasonic velocity of the western wall in the Stone Chamber before dismantling was shown to be in the highly weathered (HW) stage with an average ultrasonic wave velocity of 2,291 m/s and coefficient of weathering (K) of 0.55. Therefore, we identified that the degree of weathering on the Stone Chamber is worse than that of the Stone Standing Buddha, which is assumed to be due to the exposure of continuous creep and complex physical damage over long periods (Lee, 1998). Creep that occurs to the west of the lower ground of the western wall causes structural imbalance, resulting in partial load difference that adds to the crack. Consequently, if this phenomenon lasts, the weathering of the masonry becomes more severe and the physical properties become weaker.

To select the substitute stone for damaged parts of the Stone Chamber, the petrographic homogeneity with granite in the surrounding area was examined. Samples used in the analysis were collected in Mungyeong, Danyang, Sangju, and Mireukri in Chungju. Considering the petrographic characteristics, the magnetic susceptibility and geochemical characteristics, the granites around Mireukri in Chungju are the most similar, and the second–most-similar is the quarry in the Mungyeong area (Kim and Shin, 1990). Therefore, it is reasonable to utilize the rocks from these areas as alternative stone in terms of authenticity of the cultural heritage.

Also, the availability of rocks used for the stone cultural heritage around the Mireukdaewonji was investigated. The results of investigating the old cutting traces, petrographic characteristics and the distribution of magnetic susceptibility, showed that there is a similarity between the stone cultural heritage and nearby rocks. It is supposed that there is a possibility to obtain stone from neighboring rocks when constructing stone cultural heritage because a river transportation system has not been developed on a large scale. However, it is necessary to reveal more direct and clear grounds through further quantitative analysis with regards to this.

This study will provide the basic data for making a stable conservation management plan of the Stone Standing Buddha and Stone Chamber, and choosing a substitute stone for masonry repair. It will also be used as an important source of regular monitoring after repair works, helping to determine the progress of damage.