Abstract
Buildings and monuments made of carbonate rocks exhibit different rates of erosion. Chemo-mechanical processes are suggested as the main processes, yet quantifying them over long term periods is challenging. To constrain the variety of parameters controlling long-term limestone weathering, we studied the Western Wall, a Herodian-period edifice located in Jerusalem, Israel. The wall represents the outer boundary of the Herodian Temple precinct. Construction of the Herodian Temple precinct is thought to have been completed during the first century CE, and the wall is built entirely of locally quarried limestone. Deterioration of the limestone blocks is mainly associated with human activity and natural disasters, and include the formations of cracks and collapse from the wall. Applying non-invasive, semi-quantitative methods such as portable X-ray fluorescence (XRF) spectrometers, provide chemical information which allows to characterize and map the different materials that lead to the weathering of the limestone blocks. In this work, we find high concentrations of sulfur and chlorine at specific locations along the wall. These elements suggest the presence of salts (e.g., gypsum and soluble chlorides) as one of the promoters of the limestone weathering. Focusing on an ashlar that recently collapsed from the wall to the visitors’ area, our finding indicates the presence of gypsum in the remaining broken half, based on Infrared spectroscopy and XRF analysis. In addition, a survey of other Herodian stones, and later periods joint mortars and plasters that are found adhered to the wall, revealed that gypsum was present only in specific areas on the Wall. This elemental mapping suggests that the salts may originate from several sources (e.g., soil pollution, leakages, and sewage) and is not evenly distributed. The obtained results indicate on the possible use of non-invasive, semi-quantitative methods for detecting potential areas that are more susceptible to weathering in built heritage.
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References
Occhipinti R, Stroscio A, Belfiore CM, Barone G, Mazzoleni P (2021) Chemical and colorimetric analysis for the characterization of degradation forms and surface colour modification of building stone materials. Constr Build Mater 302:124356
Prentice JE (1990) Geology of construction materials, vol 4. Springer Science & Business Media
da Fonseca BS, Pinto AF, Rodrigues A, Piçarra S, Montemor MF (2021) The role of properties on the decay susceptibility and conservation issues of soft limestones: contribution of Ançã stone (Portugal). J Build Eng 44:102997
Benavente D (2011) Why pore size is important in the deterioration of porous stones used in the built heritage
Camuffo D (1998) Microclimate for cultural heritage. Elsevier
Emmanuel S, Levenson Y (2014) Limestone weathering rates accelerated by micron-scale grain detachment. Geol 42(9):751–754
Scherer GW (2004) Stress from crystallization of salt. Cem Concr Res 34(9):1613–1624
Torraca G (1989) Personal communication at the stone conservation course at the summer schools (International Academic Projects) of the University of London
Vallet JM, Gosselin C, Bromblet P, Rolland O, Vergès-Belmin V, Kloppmann W (2006) Origin of salts in stone monument degradation using sulphur and oxygen isotopes: first results of the bourges cathedral (France). J Geochem Explor 88(1–3):358–362
Viles HA, Gorbushina AA (2003) Soiling and microbial colonisation on urban roadside limestone: a three year study in oxford, England. Build Environ 38(9–10):1217–1224
Fitzner B, Heinrichs K, La Bouchardiere D (2002) Damage index for stone monuments
Pozzi F, Rizzo A, Basso E, Angelin EM, de Sá SF, Cucci C, Picollo M (2021) Portable spectroscopy for cultural heritage: applications and practical challenges. In: Portable spectroscopy and spectrometry. pp 499–522
Arnold A (1984) Determination of mineral salts from monuments. Stud Conserv 29(3): 129–138
Arnold A, Zehnder K (1987) Monitoring wall paintings affected by soluble salts. Getty Conservation Institute, Marina Del Rey, pp 103–135
Bläuer Böhm C (2005) Quantitative salt analysis. Conservation of buildings. Restoration of buildings and monuments/Bauinstandsetzen und Baudenkmalpflege 11(6):1–10
Teutonico JM (1988) A laboratory manual for architectural conservators, vol 168. ICCROM, Rome
Borrelli E (1999) Conservation of architectural heritage, historic structures and materials. In: Arc laboratory handbook, vol 3: Salts. International Centre for the Study of the Preservation and Restoration of Cultural Property (ICCROM)
Weiner S (2010) Microarchaeology: beyond the visible archaeological record. Cambridge University Press
Josephus F (1943) Jewish antiquities (books XII−XV). Translated by R. Marcus & A. Wikgern (Loeb Classical Library nos. 365, 489), Michigan, Massachusetts
Warren C (1884) Plans, elevations, sections etc., showing the results of the excavations at Jerusalem. 1867–1870, executed for the committee of the Palestine exploration fund. London
Avi Yona M (1956) The second temple mount. In: Avi-Yonah M Nature, history and development of Jerusalem, from its early days till our time. Bialik Tel Aviv (in Hebrew)
Avi-Yonah M (1968) The facade of herod’s temple–an attempted reconstruction. In: Neusner J (ed) Religions in antiquity essays in memory of E. R. Goodenough, Leiden, pp 327−335
Ben-Dov M (1982) The underground vaults west of the western wall
Ritmeyer L (1992) The architectural development of the temple mount in Jerusalem. PhD dissertation submitted to the university of Manchester
Ritmeyer L (2006) The quest: revealing the temple mount in Jerusalem. The Lamb Foundation, Carta
Netzer E (2009) Palaces and the planning of complexes In Herods realm. In: Herod and Augustus. Brill, pp 171–180
Gill D (1996) The geology of the city of David and its ancient subterranean waterworks. In: Qedem, monographs of the institute of archaeology. The Hebrew University of Jerusalem. Nr. 35
Picard LA (1956) The geological situation in Jerusalem. In: Avi-Yonah M Nature, history and development of Jerusalem, from its early days till our time. Bialik Tel Aviv (in Hebrew)
Mazar B (1976) The archaeological excavations near the temple mount. In: Yadin Y (ed) Jerusalem revealed, archaeology in the holy city 1968–1974. New Haven and London, pp 25–40
Reich R, Billig Y (2000) Excavations near the temple mount and Robinson’s arch, 1994−1996. In: Geva H (ed) Ancient Jerusalem revealed, expanded edition (Israel Exploration Society). Jerusalem
Asscher Y, van Zuiden A, Shor M (2023) Degradation of the stones in the western wall: salts distribution over three decades. In: Bocher E (ed) The southern wall and corners of the temple mount: past present future, ancient Jerusalem publications, Jerusalem Chapter 3: conservation studies
Tzahor Y, Vaknin Y, Kalman Y, Tsipshstein D (2021) Conservation survey of the western wall’s ashlars. In: Zelinger Y, Peleg-Barkat O, Uziel J, Gadot Y (eds) New studies in the archaeology of Jerusalem and its region, collected papers. Tel Aviv University, The Hebrew University and Israel Antiquities Authority (Hebrew)
Baruch Y, Basson U, Nachum O, Reich R (2021) Robinson’s arch: results of a geophysical study. In: Meiron E (ed) City of David, studies of ancient Jerusalem, the 22th conference. Megalim Institute, Israel Antiquitie Authority, National Park Service and Ancient Jerusalem Research Center
Basson U (2021) Ground penetrating radar imaging of the western wall. In: New studies in the archaeology of Jerusalem and its region, collected papers, Tel Aviv University, The Hebrew University and Israel Antiquities Authority
Farmer VC (ed) (1974) In Infra-Red spectra of minerals. Mineralogical Society of Great Britain and Ireland
Melquiades FL, Appoloni C (2004) Application of XRF and field portable XRF for environmental analysis. J Radioanal Nucl Chem 262(2):533–541
Rowe H, Hughes N, Robinson K (2012) The quantification and application of handheld energy-dispersive x-ray fluorescence (ED-XRF) in mudrock chemostratigraphy and geochemistry. Chem Geol 324:122–131
Kokaly RF, Clark RN, Swayze GA, Livo KE, Hoefen TM, Pearson NC, Wise RA, Benzel WM, Lowers HA, Driscoll RL, Klein AJ (2017) Usgs spectral library version 7 data: us geological survey data release. United States Geological Survey (USGS): Reston, VA, USA, 61
Van Zuiden A, Asscher YA (2021) Typology of lime-based plasters from iron age II until the byzantine period in Jerusalem and its vicinity in new studies in the Archaeology of Jerusalem and its Region, vol 14
van Asperen de Boer JRJ, Stambolov T (1976) The deterioration and conservation of porous building materials in monuments. ICCROM, Rome
Shugar AN (2013) Portable X-ray fluorescence and archaeology: limitations of the instrument and suggested methods to achieve desired results. In: Archaeological chemistry VIII. American Chemical Society, pp 173–193
Acknowledgements
The authors wish to thanks Dr.Yuval Baruch, for fruitful discussions, Raanan Kislev, Avi Mashiah, Yoram Saad, and Yossi Vaknin. This research was financially supported by the Israel Antiquity Authority.
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YA, MS and AVZ conceptualized the study; MS, YA and AVZ performed the field and lab work; MS, NW and YA analyzed the data; YA, NW, MS and AVZ wrote the paper.
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Appendix
Appendix
Supplementary Material
Table S1 The result of the analysis of the samples throughout the analytical method of the salts. The table compose of the microscopic observation to groups by the aggregates, the chemical dataset for all the investigated samples in two internal calibrations of the XRF (Geo-Exploration and Mudrock Dual), the ratio between the sulfates to carbonate by the FTIR peak shape analysis and electrical conductivity values. LOD refers to the limit of detection and N.A refers to data which is not available.
pXRF results | FTIR | |||||||||
---|---|---|---|---|---|---|---|---|---|---|
Sample number | Location | Material | Description | Ca | S (Geo-exploration) | S (mudrock) | S:Ca | Cl (Geo- exploration) | SO4:CO3 | EC |
1 | Main prayer plaza (Sect. 5) | M | T4M | 29.5 | 0.1 | <LOD | 0.0 | 0.1 | 0.1 | N.A |
2 | M | T4M | 28.2 | 0.1 | <LOD | 0.0 | 0.1 | 0.5 | N.A | |
3 | M | T4M | 26.4 | 0.1 | 0.0 | 0.0 | 0.1 | 0.0 | N.A | |
4 | M | T4M | 27.7 | 0.3 | 0.0 | 0.0 | 0.1 | 0.2 | N.A | |
5 | M | T4M | 24.0 | 0.0 | <LOD | 0.0 | 0.0 | 0.1 | N.A | |
6 | M | T4M | 31.8 | 0.1 | <LOD | 0.0 | 0.2 | 0.1 | N.A | |
7 | M | T4M | 31.9 | 0.0 | <LOD | 0.0 | 0.1 | 0.0 | N.A | |
8 | M | 24.5 | 0.6 | 0.4 | 0.0 | 0.3 | 0.3 | N.A | ||
9 | M | 28.2 | 0.2 | <LOD | 0.0 | 0.2 | 0.1 | N.A | ||
10 | Ezrat Israel prayer area (Sect. 1) | P | T1P | 37.7 | 0.0 | <LOD | 0.0 | 0.2 | 0.1 | N.A |
11 | P | T1P | <LOD | N.A | <LOD | 0.0 | N.A | N.A | 39.8 | |
12 | P | T2P | 23.4 | 7.2 | 6.6 | 1.0 | 0.7 | 0.1 | 14.4 | |
13 | P | T2P | 26.8 | 1.3 | 0.9 | 0.5 | 1.6 | N.A | 16.3 | |
14 | P | T1P | 21.6 | 1.2 | 1.1 | 0.2 | 2.0 | 0.1 | 8.9 | |
15 | M | T6M | 29.1 | 0.7 | 0.5 | 0.1 | 0.6 | N.A | N.A | |
16 | M | T6M | N.A | N.A | <LOD | N.A | N.A | N.A | 7.1 | |
17 | south to Ezrat Israel (Sect. 4) | M | T4M | 8.0 | 3.7 | 3.7 | 0.2 | 2.5 | 1.0 | N.A |
18 | M | T4M | 30.2 | 4.5 | 4.1 | 0.1 | 0.9 | 0.2 | N.A | |
19 | P | T1P | 19.4 | 0.4 | 0.3 | 0.0 | 0.3 | 0.1 | 11.1 | |
20 | M | T4M | 21.2 | 1.3 | 1.1 | 0.1 | 1.7 | 0.1 | N.A | |
21 | M | T4M | 22.6 | 1.8 | 1.5 | 0.1 | 4.3 | 0.2 | 120.4 | |
22 | M | T4M | 30.3 | 3.7 | 3.3 | 0.1 | 1.0 | 0.3 | 109.7 | |
23 | M | T4M | 23.5 | 3.8 | 3.7 | 0.2 | 1.3 | 0.4 | N.A | |
24 | Robinson arch (section 2) | M | T4M | 22.7 | 0.3 | 0.1 | 0.0 | 0.3 | 0.3 | N.A |
25 | M | T4M | 19.6 | 0.2 | 0.1 | 0.0 | 0.8 | 0.3 | N.A | |
26 | M | T4M | 26.5 | 0.9 | 0.9 | 0.0 | 0.9 | 0.1 | N.A | |
27 | M | T4M | 30.4 | 0.2 | <LOD | 0.0 | 1.3 | 0.0 | N.A | |
28 | P | T3P | 28.2 | 0.2 | <LOD | 0.0 | 0.5 | 0.1 | 12.4 | |
29 | P | T3P | 22.5 | 0.1 | <LOD | 0.0 | 0.5 | 0.1 | 27.4 | |
30 | P | T3P | 14.8 | 0.4 | 0.6 | 0.0 | 1.8 | 0.1 | 121.9 | |
31 | P | T3P | 23.3 | 0.8 | 0.7 | 0.0 | 1.5 | 0.1 | 91.2 | |
32 | M | T4M | 30.4 | 0.2 | <LOD | 0.0 | 0.9 | 0.1 | 21.5 | |
33 | M | T4M | 28.4 | 0.7 | 0.4 | 0.0 | 0.8 | 0.3 | 25.8 | |
34 | M | T4M | 30.4 | 0.1 | <LOD | 0.0 | 0.6 | 0.8 | N.A | |
35 | M | T4M | 26.4 | 0.1 | <LOD | 0.0 | 0.2 | 0.0 | 11.9 | |
36 | M | T4M | 24.2 | 0.2 | 0.1 | 0.0 | 0.7 | 0.1 | N.A | |
37 | M | T4M | 22.1 | 0.2 | 0.0 | 0.0 | 0.1 | 0.0 | N.A | |
38 | M | T4M | 32.9 | 0.1 | <LOD | 0.0 | 0.3 | 0.0 | 13.9 | |
39 | M | T6M | 26.9 | 0.6 | 0.2 | 0.0 | 0.3 | 0.1 | 18.9 | |
40 | M | T6M | 20.4 | 1.1 | 0.9 | 0.1 | 1.6 | 1.4 | 117.3 | |
41 | M | T6M | 16.2 | 0.1 | 0.1 | 0.0 | 2.1 | 0.1 | 144.8 | |
42 | M | T6M | 25.2 | 0.3 | 0.1 | 0.0 | 0.3 | 0.1 | 6.5 | |
43 | South-West (Sect. 3) | M | T4M | 21.8 | 0.1 | <LOD | 0.0 | 0.1 | 0.1 | N.A |
44 | M | T4M | 26.5 | 0.3 | 0.0 | 0.0 | 0.2 | 0.1 | N.A | |
45 | M | T6M | 29.8 | 0.1 | <LOD | 0.0 | 0.3 | 0.0 | 9.3 | |
46 | M | T5M | 29.2 | 0.4 | 0.2 | 0.0 | 0.3 | 0.1 | N.A | |
47 | M | T5M | 27.5 | 0.9 | 0.5 | 0.0 | 0.8 | 0.1 | 8.6 | |
48 | M | T5M | 29.5 | 0.1 | <LOD | 0.0 | 0.2 | 0.0 | 12.6 | |
49 | M | T5M | 33.7 | 0.5 | 0.2 | 0.0 | 0.2 | 0.0 | 3.9 | |
50 | M | T5M | 30.8 | 0.2 | LOD | 0.0 | 0.3 | 0.2 | 10.7 | |
51 | M | T5M | 30.3 | 0.2 | LOD | 0.0 | 0.2 | 0.1 | 5.2 | |
52 | M | T4M | 11.3 | 0.4 | 0.3 | 0.0 | 0.1 | 0.1 | N.A | |
53 | M | T4M | 14.0 | 0.7 | 0.6 | 0.0 | 1.2 | 0.2 | 43.6 | |
54 | Section 4 | S | CS | 23.7 | N.A | 1.0 | 0.0 | N.A | 0.0 | N.A |
55 | S | Control sample | 24.8 | N.A | 0.6 | 0.0 | N.A | 0.2 | N.A | |
56 | S | Control sample | 18.6 | N.A | 10.0 | 0.5 | N.A | 3.0 | N.A | |
57 | S | Control sample | 19.3 | N.A | 10.2 | 0.5 | N.A | 0.2 | N.A | |
58 | S | Control sample | 17.1 | N.A | 0.7 | 0.0 | N.A | 0.1 | N.A | |
59 | S | Control sample | 19.4 | N.A | 0.3 | 0.0 | N.A | 0.0 | N.A | |
60 | S | Control sample | 18.9 | N.A | <LOD | N.A | N.A | 0.1 | N.A | |
61 | S | Control sample | 2.4 | N.A | 2.3 | 0.9 | N.A | 2.7 | N.A | |
62 | S | Control sample | 17.5 | N.A | 18.0 | 1.0 | N.A | 7.1 | N.A | |
63 | Robinson arch | S | Control sample-core | 34.9 | <LOD | N.A | N.A | 0.1 | 0.0 | 0.6 |
64 | Collapsed stone | S | Control sample | 14.3 | N.A | 13.6 | 1.0 | N.A | 0.8 | N.A |
65 | S | Control sample | 14.9 | N.A | 4.0 | 0.3 | N.A | N.A | N.A | |
66 | S | Control sample | 5.4 | N.A | 5.8 | 1.1 | N.A | N.A | N.A | |
67 | Dead Sea | Sa | gypsum control | 20.0 | 25.1 | N.A | 1.3 | < LOD | 10.757 | 15.5 |
68 | Standard | Sa | sea salt | 0.3 | <LOD | N.A | N.A | 33.7 | 0.3 | 200.0 |
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Shor, M., van Zuiden, A., Wieler, N., Asscher, Y. (2024). Stone Deterioration of the Western Wall: Chemical and Mineralogical Characterization of Salts. In: Osman, A., Moropoulou, A., Lampropoulos, K. (eds) Advanced Nondestructive and Structural Techniques for Diagnosis, Redesign and Health Monitoring for the Preservation of Cultural Heritage. TMM 2023. Springer Proceedings in Materials, vol 33. Springer, Cham. https://doi.org/10.1007/978-3-031-42239-3_14
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