Eleventh Annual V. M. Goldschmidt Conference (2001) 3212.pdf DAMAGE TO MONUMENTS FROM THE CRYSTALLIZATION OF MIRABILITE, THENARDITE AND HALITE: MECHANISMS, ENVIRONMENT, AND PREVENTIVE POSSIBILITIES. E. Doehne1, C. Selwitz2, D. Carson1, and A. de Tagle1, 1The Getty Conservation Institute, 1200 Getty Center Drive, Suite 700, Los Angeles, CA 90049, USA, TEL: (310) 440 6237, FAX: 310 440 7711, Email:
[email protected], 23631 Surfwood road, Malibu, CA, 90265, USA. Introduction: "In time, and with water, everything sulfate through columns of limestone. The limestones changes." ---Leonardo da Vinci were oolitic Monks Park stone where 90% of its pores The crystallization of soluble salts in porous building measured between 0.05-0.80 microns and Texas materials is a widespread weathering process that re- Creme, a fossilferous stone with 90% of its pore size sults in damage to important monuments and archaeo- distribution measuring between 0.5 and 3.0 microns. logical sites [1]. Salt weathering by thenardite (sodium In the absence of modifiers, sodium chloride passage sulfate) and mirabilite (sodium sulfate decahydrate) is through Monks Park limestone gave predominantly especially destructive, yet is still not fully understood subflorescence with mild edge erosion while sodium [2]. Halite (sodium chloride) in contrast, is one of the sulfate mainly effloresced and severely damaged the least damaging salts [3]. Previous work has also dem- stone column. With Texas Creme limestone, essen- onstrated the importance of airflow in salt weathering tially only efflorescence occurred with either salt and [4]. Here we present new data that help explain why there was little or no stone damage. sodium sulfate is so damaging and also show how Most crystallization inhibitors--used in industry to crystallization modifiers and changes in airflow can prevent scaling by promoting high supersaturation reduce salt damage in laboratory experiments.