Rim Guanhe, Roy Noyonika, Zhao Diandian, Kawashima Shiho, Stallworth Phillip, Greenbaum Steven G, Park Ah-Hyung Alissa
Department of Earth and Environmental Engineering, USA and Lenfest Center for Sustainable Energy, The Earth Institute, Columbia University, NY 10027, USA.
Lenfest Center for Sustainable Energy, The Earth Institute, Columbia University, NY 10027, USA.
Faraday Discuss. 2021 Jul 16;230(0):187-212. doi: 10.1039/d1fd00022e.
Carbon mineralization to solid carbonates is one of the reaction pathways that can not only utilize captured CO2 but also potentially store it in the long term. In this study, the dissolution and carbonation behaviors of alkaline solid wastes (i.e., waste concrete) was investigated. Concrete is one of the main contributors to a large carbon emission in the built environment. Thus, the upcycling of waste concrete via CO2 utilization has multifaceted environmental benefits including CO2 emission reduction, waste management and reduced mining. Unlike natural silicate minerals such as olivine and serpentine, alkaline solid wastes including waste concrete are highly reactive, and thus, their dissolution and carbonation behaviors vary significantly. Here, both conventional acid (e.g., hydrochloric acid) and less studied carbonic acid (i.e., CO2 saturated water) solvent systems were explored to extract Ca from concrete. Non-stoichiometric dissolution behaviors between Ca and Si were confirmed under far-from-equilibrium conditions (0.1 wt% slurry density), and the re-precipitation of the extracted Si was observed at near-equilibrium conditions (5 wt% slurry density), when the Ca extraction was performed at a controlled pH of 3. These experiments, with a wide range of slurry densities, provided valuable insight into Si re-precipitation phenomena and its effect on the mass transfer limitation during concrete dissolution. Next, the use of the partial pressure of CO2 for the pH swing carbon mineralization process was investigated for concrete, and the results were compared to those of Mg-bearing silicate minerals. In the PCO2 swing process, the extraction of Ca was significantly limited by the precipitation of the carbonate phase (i.e., calcite), since CO2 bubbling could not provide a low enough pH condition for concrete-water-CO2 systems. Thus, this study showed that the two-step carbon mineralization via PCO2 swing, that has been developed for Mg-bearing silicate minerals, may not be viable for highly reactive Ca-bearing silicate materials (e.g., concrete). The precipitated calcium carbonate (PCC) derived from waste concrete via a pH swing process showed very promising results with a high CO2 utilization potential as an upcycled construction material.
碳矿化形成固体碳酸盐是一种反应途径,它不仅可以利用捕获的二氧化碳,还具有长期储存二氧化碳的潜力。在本研究中,对碱性固体废物(即废弃混凝土)的溶解和碳酸化行为进行了研究。混凝土是建筑环境中碳排放的主要来源之一。因此,通过利用二氧化碳对废弃混凝土进行升级再造具有多方面的环境效益,包括减少二氧化碳排放、废物管理和减少采矿。与天然硅酸盐矿物如橄榄石和蛇纹石不同,包括废弃混凝土在内的碱性固体废物具有高反应活性,因此它们的溶解和碳酸化行为差异显著。在此,研究了传统酸(如盐酸)和研究较少的碳酸(即二氧化碳饱和水)溶剂体系从混凝土中提取钙的情况。在远离平衡条件(0.1 wt%浆料密度)下证实了钙和硅之间的非化学计量溶解行为,当在pH值为3的条件下进行钙提取时,在接近平衡条件(5 wt%浆料密度)下观察到了提取的硅的再沉淀。这些在广泛浆料密度范围内进行的实验,为硅再沉淀现象及其对混凝土溶解过程中传质限制的影响提供了有价值的见解。接下来,研究了在混凝土的pH值摆动碳矿化过程中使用二氧化碳分压的情况,并将结果与含镁硅酸盐矿物的结果进行了比较。在二氧化碳分压摆动过程中,由于二氧化碳鼓泡无法为混凝土 - 水 - 二氧化碳体系提供足够低的pH条件,钙的提取受到碳酸盐相(即方解石)沉淀的显著限制。因此,本研究表明,为含镁硅酸盐矿物开发的通过二氧化碳分压摆动的两步碳矿化法,对于高反应活性的含钙硅酸盐材料(如混凝土)可能不可行。通过pH值摆动过程从废弃混凝土中获得的沉淀碳酸钙(PCC)作为一种升级再造的建筑材料,显示出非常有前景的结果,具有很高的二氧化碳利用潜力。