Philipp Ingold , Gisela Weibel , Patrick Kämpfer , Sergey V. Churakov
{"title":"湿提和干提城市生活垃圾底灰的风化和微量元素的迁移","authors":"Philipp Ingold , Gisela Weibel , Patrick Kämpfer , Sergey V. Churakov","doi":"10.1016/j.jconhyd.2025.104566","DOIUrl":null,"url":null,"abstract":"<div><div>This study aims on the characteristics of occurring weathering processes of dry and wet extracted bottom ash materials and its effects on element emissions. To examine the role of initial water contact, dry bottom ash was experimentally moistened. Titration experiments were performed to elaborate buffer capacities and dissolution processes of the waste residues as a function of <em>pH</em>, and thermodynamic calculations were used to identify the solubility-controlling phases. Dry bottom ash showed highly alkaline in-situ <em>pH</em> conditions (<em>pH</em> 12.6). Continuous acid addition revealed a multi-stage process, which was characterised by the formation and dissolution of different phases across four different buffer systems, including portlandite dissolution and formation of ettringite and CSH phases in the first stage (<em>pH</em> > 12.1), dissolution of ettringite and CSH phases in the second stage (<em>pH</em> 9.7–12.1), carbonate dissolution during the third stage (<em>pH</em> 5.5–9.7), and dissolution of Al- and Fe-hydroxides in the fourth stage (<em>pH</em> < 5.5). Prior weathering processes in the moistened dry bottom ash and wet bottom ash resulted in a reduction of the in-situ <em>pH</em> (<em>pH</em> 12.1 and 10.3, respectively). Thermodynamic calculations suggested that phases containing Ca, S, Al, and Si were mainly responsible for the <em>pH</em> stabilisation. Emission trends as a function of <em>pH</em> generally aligned with calculated solubility curves, with dry bottom ash showing higher concentrations than wet bottom ash. Discrepancies, especially found in the dry bottom ash system, may be associated with elevated the presence of ligands (i.e., DIC, DOC), enhancing the mobility of selected elements (Al, Cu, Zn).</div></div><div><h3>Environmental implications</h3><div>Bottom ashes investigated in this study are subject to environmental contaminants and potential hazards. Their characterisation and behaviour investigated during this work provides further insight into their behaviour and highlights the enhanced leaching of dry extracted bottom ash under naturally and environmentally relevant conditions.</div></div>","PeriodicalId":15530,"journal":{"name":"Journal of contaminant hydrology","volume":"272 ","pages":"Article 104566"},"PeriodicalIF":3.5000,"publicationDate":"2025-04-08","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Weathering and trace element mobilisation of MSWI bottom ash from wet and dry extraction\",\"authors\":\"Philipp Ingold , Gisela Weibel , Patrick Kämpfer , Sergey V. Churakov\",\"doi\":\"10.1016/j.jconhyd.2025.104566\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>This study aims on the characteristics of occurring weathering processes of dry and wet extracted bottom ash materials and its effects on element emissions. To examine the role of initial water contact, dry bottom ash was experimentally moistened. Titration experiments were performed to elaborate buffer capacities and dissolution processes of the waste residues as a function of <em>pH</em>, and thermodynamic calculations were used to identify the solubility-controlling phases. Dry bottom ash showed highly alkaline in-situ <em>pH</em> conditions (<em>pH</em> 12.6). Continuous acid addition revealed a multi-stage process, which was characterised by the formation and dissolution of different phases across four different buffer systems, including portlandite dissolution and formation of ettringite and CSH phases in the first stage (<em>pH</em> > 12.1), dissolution of ettringite and CSH phases in the second stage (<em>pH</em> 9.7–12.1), carbonate dissolution during the third stage (<em>pH</em> 5.5–9.7), and dissolution of Al- and Fe-hydroxides in the fourth stage (<em>pH</em> < 5.5). Prior weathering processes in the moistened dry bottom ash and wet bottom ash resulted in a reduction of the in-situ <em>pH</em> (<em>pH</em> 12.1 and 10.3, respectively). Thermodynamic calculations suggested that phases containing Ca, S, Al, and Si were mainly responsible for the <em>pH</em> stabilisation. Emission trends as a function of <em>pH</em> generally aligned with calculated solubility curves, with dry bottom ash showing higher concentrations than wet bottom ash. Discrepancies, especially found in the dry bottom ash system, may be associated with elevated the presence of ligands (i.e., DIC, DOC), enhancing the mobility of selected elements (Al, Cu, Zn).</div></div><div><h3>Environmental implications</h3><div>Bottom ashes investigated in this study are subject to environmental contaminants and potential hazards. Their characterisation and behaviour investigated during this work provides further insight into their behaviour and highlights the enhanced leaching of dry extracted bottom ash under naturally and environmentally relevant conditions.</div></div>\",\"PeriodicalId\":15530,\"journal\":{\"name\":\"Journal of contaminant hydrology\",\"volume\":\"272 \",\"pages\":\"Article 104566\"},\"PeriodicalIF\":3.5000,\"publicationDate\":\"2025-04-08\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Journal of contaminant hydrology\",\"FirstCategoryId\":\"93\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S0169772225000713\",\"RegionNum\":3,\"RegionCategory\":\"环境科学与生态学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q2\",\"JCRName\":\"ENVIRONMENTAL SCIENCES\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of contaminant hydrology","FirstCategoryId":"93","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0169772225000713","RegionNum":3,"RegionCategory":"环境科学与生态学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"ENVIRONMENTAL SCIENCES","Score":null,"Total":0}
Weathering and trace element mobilisation of MSWI bottom ash from wet and dry extraction
This study aims on the characteristics of occurring weathering processes of dry and wet extracted bottom ash materials and its effects on element emissions. To examine the role of initial water contact, dry bottom ash was experimentally moistened. Titration experiments were performed to elaborate buffer capacities and dissolution processes of the waste residues as a function of pH, and thermodynamic calculations were used to identify the solubility-controlling phases. Dry bottom ash showed highly alkaline in-situ pH conditions (pH 12.6). Continuous acid addition revealed a multi-stage process, which was characterised by the formation and dissolution of different phases across four different buffer systems, including portlandite dissolution and formation of ettringite and CSH phases in the first stage (pH > 12.1), dissolution of ettringite and CSH phases in the second stage (pH 9.7–12.1), carbonate dissolution during the third stage (pH 5.5–9.7), and dissolution of Al- and Fe-hydroxides in the fourth stage (pH < 5.5). Prior weathering processes in the moistened dry bottom ash and wet bottom ash resulted in a reduction of the in-situ pH (pH 12.1 and 10.3, respectively). Thermodynamic calculations suggested that phases containing Ca, S, Al, and Si were mainly responsible for the pH stabilisation. Emission trends as a function of pH generally aligned with calculated solubility curves, with dry bottom ash showing higher concentrations than wet bottom ash. Discrepancies, especially found in the dry bottom ash system, may be associated with elevated the presence of ligands (i.e., DIC, DOC), enhancing the mobility of selected elements (Al, Cu, Zn).
Environmental implications
Bottom ashes investigated in this study are subject to environmental contaminants and potential hazards. Their characterisation and behaviour investigated during this work provides further insight into their behaviour and highlights the enhanced leaching of dry extracted bottom ash under naturally and environmentally relevant conditions.
期刊介绍:
The Journal of Contaminant Hydrology is an international journal publishing scientific articles pertaining to the contamination of subsurface water resources. Emphasis is placed on investigations of the physical, chemical, and biological processes influencing the behavior and fate of organic and inorganic contaminants in the unsaturated (vadose) and saturated (groundwater) zones, as well as at groundwater-surface water interfaces. The ecological impacts of contaminants transported both from and to aquifers are of interest. Articles on contamination of surface water only, without a link to groundwater, are out of the scope. Broad latitude is allowed in identifying contaminants of interest, and include legacy and emerging pollutants, nutrients, nanoparticles, pathogenic microorganisms (e.g., bacteria, viruses, protozoa), microplastics, and various constituents associated with energy production (e.g., methane, carbon dioxide, hydrogen sulfide).
The journal''s scope embraces a wide range of topics including: experimental investigations of contaminant sorption, diffusion, transformation, volatilization and transport in the surface and subsurface; characterization of soil and aquifer properties only as they influence contaminant behavior; development and testing of mathematical models of contaminant behaviour; innovative techniques for restoration of contaminated sites; development of new tools or techniques for monitoring the extent of soil and groundwater contamination; transformation of contaminants in the hyporheic zone; effects of contaminants traversing the hyporheic zone on surface water and groundwater ecosystems; subsurface carbon sequestration and/or turnover; and migration of fluids associated with energy production into groundwater.