Thermal expansion on volcanic tuff rocks used as building stones: examples from Mexico

  • Rubén López-DoncelEmail author
  • Wanja Wedekind
  • Alfredo Aguillón-Robles
  • Reiner Dohrmann
  • Sergio Molina-Maldonado
  • Theresa Leiser
  • Anna Wittenborn
  • Siegfried Siegesmund
Thematic Issue
Part of the following topical collections:
  1. Stone in the Architectural Heritage: from quarry to monuments—environment, exploitation, properties and durability


Three cities in the center of Mexico, declared as cultural heritage, were erected mainly of volcanic tuffs as main construction element. Many of the historic buildings of these cities show significant damage and deterioration. One of the causes of these damages can be attributed to a phenomenon poorly studied in volcanic tuffs, the thermal expansion. To understand the response of volcanic tuffs to thermal expansion, as well as to know their thermal expansion coefficient, thermal expansion test was performed on 12 representative tuffs of these localities. In the same way and to know which of their petrographic, petrophysical, mineralogical, and geochemical properties influence this phenomenon, several laboratory studies were carried out to determine which of these plays an important role in the expansion. The results of our tests showed that volcanic tuffs rocks have very varied thermal expansion values, ranging from 0.7 mm/m at their maximum expansion to even contraction in the order of − 0.5 mm/m. Equally varied were the thermal expansion coefficient values ranging from 10.1 to − 7.2 10−6/K. The most dominant behavior type is the “anisotropic no residual strain behavior”. In general, the behavior of the tuffs in practically all the tests carried out showed a very important heterogeneity in the rocks; however, in spite of the non-homogeneous behavior of the tuffs, three main factors could be identified that play an important role in the thermal expansion of the studied rocks, the chemical composition, e.g., acid volcanic tuff rocks (rhyolitic composition) had greater expansions, while the more basic rocks (basaltic composition) expanded less, the textural and fabrics homogeneity, e.g., the most homogeneous rocks texturally have higher expansion values and the degree of crystallinity, and, e.g., the tuff rocks with the largest amount of glass showed smaller thermal expansions than the tuffs composed of microcrystals.


Volcanic tuff rocks Thermal expansion Crystallinity Anisotropy 



The authors thank the financial support of the National Council of Science and Technology, Mexico (CONACyT) through projects CB-130282 and Coop. Bil. 191044 and to the German Science Foundation (DFG Si-438 / 44-1). For the technical, editing and laboratory support, we thank Erasmo Mata, Nohemi Cardona, Eneida Maldonado, Ana Rocio Hernández and Karla Guadalupe González.


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Copyright information

© Springer-Verlag GmbH Germany, part of Springer Nature 2018

Authors and Affiliations

  • Rubén López-Doncel
    • 1
    Email author
  • Wanja Wedekind
    • 2
  • Alfredo Aguillón-Robles
    • 1
  • Reiner Dohrmann
    • 3
  • Sergio Molina-Maldonado
    • 4
  • Theresa Leiser
    • 2
  • Anna Wittenborn
    • 2
  • Siegfried Siegesmund
    • 2
  1. 1.Instituto de GeologíaUniversidad Autónoma de San Luis PotosíSan Luis PotosíMexico
  2. 2.Geowissenschaftliches Zentrum der Universität GöttingenGöttingenGermany
  3. 3.Bundesanstalt für Geowissenschaften und RohstoffeHannoverGermany
  4. 4.Posgrado en Geología AplicadaUniversidad Autónoma de San Luis PotosíSan Luis PotosíMexico

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