{"title":"Investigation of formation mechanism of tufa deposits by chemical breakdown of legacy paper mill sludge","authors":"Md Jahangir Alam, John M. MacDonald","doi":"10.1002/dep2.70054","DOIUrl":null,"url":null,"abstract":"<p>This study investigates the formation mechanisms of anthropogenic tufa deposits resulting from the chemical breakdown of legacy paper mill sludge (PMS) at the former Dalmore Paper Mill site in Auchendinny, Scotland. Tufa, a form of calcium carbonate (CaCO<sub>3</sub>), typically forms in natural freshwater environments; however, this research explores its precipitation through interactions between alkaline industrial waste (PMS) and atmospheric CO<sub>2</sub>. Field and laboratory analyses were carried out to assess the geochemical characteristics of the stream water, as well as the mineralogical and isotopic composition of the associated tufa deposits. X-ray diffraction (XRD) analysis revealed that PMS is composed predominantly of calcite, while tufa samples also contain minor amounts of quartz and kaolinite. Stream water measurements indicated alkaline conditions (pH 8.27–8.98) and elevated calcium concentrations, with calcite saturation indices suggesting conditions favourable for carbonate precipitation. Stable isotope analysis of tufa deposits (δ<sup>13</sup>C −24.62‰ to −13.74‰; δ<sup>18</sup>O −17.50‰ to −7.66‰) revealed a dominant contribution from atmospheric CO<sub>2</sub>, confirming a precipitation mechanism driven by CO<sub>2</sub> ingassing and hydroxylation reactions. The results support a model where rainwater infiltrates PMS heaps, leaching calcium into stream waters. As these calcium-rich waters mix with atmospheric CO<sub>2</sub>, supersaturation occurs, leading to rapid calcite precipitation. The resulting tufa deposits exhibit laminated structures and high porosity, indicating episodic deposition under variable geochemical conditions. This study provides the first detailed evidence of tufa formation from PMS and suggests that such industrial waste materials can act as carbon sinks, capturing and mineralising atmospheric CO<sub>2</sub>. These findings expand the understanding of anthropogenic carbonate systems and highlight the potential of PMS as a low-cost material for environmental remediation and carbon sequestration, supporting sustainable waste management strategies and contributing to climate mitigation goals.</p>","PeriodicalId":54144,"journal":{"name":"Depositional Record","volume":"12 1","pages":""},"PeriodicalIF":2.6000,"publicationDate":"2025-11-12","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://onlinelibrary.wiley.com/doi/epdf/10.1002/dep2.70054","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Depositional Record","FirstCategoryId":"89","ListUrlMain":"https://onlinelibrary.wiley.com/doi/10.1002/dep2.70054","RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"GEOLOGY","Score":null,"Total":0}
引用次数: 0
Abstract
This study investigates the formation mechanisms of anthropogenic tufa deposits resulting from the chemical breakdown of legacy paper mill sludge (PMS) at the former Dalmore Paper Mill site in Auchendinny, Scotland. Tufa, a form of calcium carbonate (CaCO3), typically forms in natural freshwater environments; however, this research explores its precipitation through interactions between alkaline industrial waste (PMS) and atmospheric CO2. Field and laboratory analyses were carried out to assess the geochemical characteristics of the stream water, as well as the mineralogical and isotopic composition of the associated tufa deposits. X-ray diffraction (XRD) analysis revealed that PMS is composed predominantly of calcite, while tufa samples also contain minor amounts of quartz and kaolinite. Stream water measurements indicated alkaline conditions (pH 8.27–8.98) and elevated calcium concentrations, with calcite saturation indices suggesting conditions favourable for carbonate precipitation. Stable isotope analysis of tufa deposits (δ13C −24.62‰ to −13.74‰; δ18O −17.50‰ to −7.66‰) revealed a dominant contribution from atmospheric CO2, confirming a precipitation mechanism driven by CO2 ingassing and hydroxylation reactions. The results support a model where rainwater infiltrates PMS heaps, leaching calcium into stream waters. As these calcium-rich waters mix with atmospheric CO2, supersaturation occurs, leading to rapid calcite precipitation. The resulting tufa deposits exhibit laminated structures and high porosity, indicating episodic deposition under variable geochemical conditions. This study provides the first detailed evidence of tufa formation from PMS and suggests that such industrial waste materials can act as carbon sinks, capturing and mineralising atmospheric CO2. These findings expand the understanding of anthropogenic carbonate systems and highlight the potential of PMS as a low-cost material for environmental remediation and carbon sequestration, supporting sustainable waste management strategies and contributing to climate mitigation goals.