4.5 Article

Weathering Processes and Mechanisms Caused by Capillary Waters and Pigeon Droppings on Porous Limestones

Journal

MINERALS
Volume 11, Issue 1, Pages -

Publisher

MDPI
DOI: 10.3390/min11010018

Keywords

salt crystallisation; pigeon droppings; rising damp; stone conservation; calcarenite

Funding

  1. Asociacion de Amigos de la Basilica de Nuestra Senora del Socorro
  2. Aspe City Council
  3. Regional Government of Madrid (Spain) [S2018/NMT-4372]
  4. EU
  5. MINECO
  6. Generalitat Valenciana

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This study investigates the physical and chemical effects of salt weathering on biocalcarenites and biocalcrudites in the Basilica of Our Lady of Succour in Aspe, Spain. The formation of various salts and crystals is associated with rising capillary water and pigeon droppings, with single salts showing non-equilibrium shapes and double salts having crystals corresponding to near-equilibrium form. The dissolution of limestone driven by acidic water lixiviated from pigeon droppings is a critical weathering process affecting the architectural elements of the facades.
This investigation studies the physical and chemical effect of salt weathering on biocalcarenites and biocalcrudites in the Basilica of Our Lady of Succour (Aspe, Spain). Weathering patterns are the result of salty rising capillary water and water lixiviated from pigeon droppings. Surface modifications and features induced by material loss are observable in the monument. Formation of gypsum, hexahydrite, halite, aphthitalite and arcanite is associated with rising capillary water, and niter, hydroxyapatite, brushite, struvite, weddellite, oxammite and halite with pigeon droppings. Humberstonite is related to the interaction of both types of waters. Analysis of crystal shapes reveals different saturation degree conditions. Single salts show non-equilibrium shapes, implying higher crystallisation pressures. Single salts have undergone dissolution and/or dehydration processes enhancing the deterioration process, particularly in the presence of magnesium sulphate. Double salts (humberstonite) have crystals corresponding to near-equilibrium form, implying lower crystallisation pressures. This geochemical study suggests salts precipitate via incongruent reactions rather than congruent precipitation, where hexahydrite is the precursor and limiting reactant of humberstonite. Chemical dissolution of limestone is driven mainly by the presence of acidic water lixiviated from pigeon droppings and is a critical weathering process affecting the most valuable architectural elements present in the facades.

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