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火山岩利用によるセメントCO₂排出削減技術(Stanford team cuts cement emissions by two-thirds)

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2026-04-0+6 スタンフォード大学

スタンフォード大学の研究では、セメント製造に伴う二酸化炭素排出を大幅に削減する新技術「Phlego」が開発された。従来のセメント製造は高温焼成により大量のCO₂を排出するが、本手法は電気化学プロセスを用いて低温で材料を生成し、排出量を抑えることが可能である。また、副産物として有用なガスも生成できるため、資源効率の向上にも寄与する。建設業は世界のCO₂排出の大きな割合を占めるため、この技術は脱炭素社会の実現に向けた重要なブレークスルーと位置づけられる。持続可能な建材開発と環境負荷低減に貢献する成果である。

火山岩利用によるセメントCO₂排出削減技術(Stanford team cuts cement emissions by two-thirds)
The Phlego manufacturing process is compatible with existing cement production methods. Pictured here are various stages of the process, from raw material (in the bag at left) to a cylindrical Phlego mortar sample that meets industry standards. | Mia Maria Pique

<関連情報>

多段階画像解析、強度および透水性測定:ローマ時代の海洋コンクリートの耐久性を理解する Multi-scale imaging, strength and permeability measurements: Understanding the durability of Roman marine concrete

Jackson MacFarlane, Tiziana Vanorio, Paulo J.M. Monteiro
Construction and Building Materials  Available online: 17 December 2020
DOI:https://doi.org/10.1016/j.conbuildmat.2020.121812

Highlights

  • Roman marine concrete undergoes ductile creep when tri-axially stressed.
  • Creep is identified by coupling triaxial loading and time-lapse tomographic imaging.
  • Pervasive fibrous minerals contribute to the low permeability and high ductility.
  • The matrix is comprised of both calcium-aluminum–silicate-hydrate and geopolymer.
  • Reduced aggregate debonding enhances ductility and preserves matrix permeability.

Abstract

Roman-era concrete is the iconic embodiment of long-term physicochemical resilience. We investigated the basis of this behavior across scales of observations by coupling time-lapse (4-D) tomographic imaging of macroscopic mechanical stressing with structural microscopy and chemical spectroscopy on Roman marine concrete (RMC) from ancient harbors in Italy and Israel. Stress–strain measurements revealed that RMC creeps and exhibits a ductile deformation mode. The low permeability of concrete samples was linked to mortar-dominated microstructures showing no debonding with the aggregates. Structural and chemical imaging shows the presence of well-developed sulfur-rich, fibrous minerals that are intertwined and embedded in a crossbred matrix having the chemical traits of both a calcium-aluminum–silicate-hydrate and a polymerized alkali-alumino-silicate. This latter likely reflects the ultra-alkaline volcanic nature of the primary source materials. We hypothesize that the fine interweave of sulfur-rich fibers within this crossbred matrix enhances aggregate bonding, which altogether contributes to the durability of RMC.

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