Investigation of formation mechanism of tufa deposits by chemical breakdown of legacy paper mill sludge

IF 2.6 3区 地球科学 Q1 GEOLOGY
Md Jahangir Alam, John M. MacDonald
{"title":"Investigation of formation mechanism of tufa deposits by chemical breakdown of legacy paper mill sludge","authors":"Md Jahangir Alam,&nbsp;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.

Abstract Image

纸厂遗留污泥化学分解凝灰岩沉积形成机理的研究
本研究探讨了苏格兰奥昌迪尼前达尔莫尔造纸厂遗址遗留造纸厂污泥(PMS)化学分解所导致的人为凝灰岩沉积物的形成机制。凝灰岩是碳酸钙(CaCO3)的一种形式,通常在天然淡水环境中形成;然而,本研究通过碱性工业废物(PMS)与大气CO2的相互作用来探索其沉淀。通过实地和实验室分析,评估了水流的地球化学特征,以及相关凝灰岩矿床的矿物学和同位素组成。x射线衍射(XRD)分析表明,PMS主要由方解石组成,而凝灰岩样品中也含有少量的石英和高岭石。水流测量结果表明,水体呈碱性(pH值8.27-8.98),钙浓度升高,方解石饱和度指数表明,水体条件有利于碳酸盐沉淀。稳定同位素分析(δ13C−24.62‰~−13.74‰;δ18O−17.50‰~−7.66‰)表明,大气CO2对凝灰岩沉积的贡献占主导地位,证实了CO2吸入和羟基化反应驱动的沉淀机制。结果支持了一个模型,即雨水渗入PMS堆,将钙浸入溪流中。当这些富含钙的水与大气中的二氧化碳混合时,会发生过饱和,导致方解石快速沉淀。由此形成的凝灰岩矿床具有层状结构和高孔隙度,表明在可变地球化学条件下的幕式沉积。这项研究提供了PMS凝灰岩形成的第一个详细证据,并表明这种工业废料可以作为碳汇,捕获和矿化大气中的二氧化碳。这些发现扩大了对人为碳酸盐系统的理解,并突出了PMS作为环境修复和碳封存的低成本材料的潜力,支持可持续废物管理战略,并有助于实现气候减缓目标。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
求助全文
约1分钟内获得全文 求助全文
来源期刊
CiteScore
4.10
自引率
16.70%
发文量
42
审稿时长
16 weeks
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
联系我们:info@booksci.cn Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。 Copyright © 2023 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:604180095
Book学术官方微信
小红书