期刊
CONSTRUCTION AND BUILDING MATERIALS
卷 208, 期 -, 页码 1-12出版社
ELSEVIER SCI LTD
DOI: 10.1016/j.conbuildmat.2019.02.173
关键词
Lacustrine sludge; Reactive MgO-fly ash; Durability; Carbonation; Mechanisms
资金
- National Natural Science Foundation of China [51879202, 51609180]
- Program for Science and Technology Development of Henan Province [182102310800]
- Key Basic Research Foundation of the Higher Education Institutions of Henan Province [18B560006]
The reactive MgO-fly ash blends are employed for stabilizing lacustrine sludge through absorbing gaseous CO2, which is a prospective and sustainable technique combined of carbonation and solidification. The mechanical and microstructural variation of carbonated MgO-fly ash solidified sludge subjected to three durability tests (i.e. water immersion, cyclic dry-wet, cyclic freeze-thaw) is investigated through unconfined compressive strength (UCS), X-ray diffraction (XRD), mercury intrusion porosimetry (MIP) and scanning electron microscopy (SEM) tests. The obtained results demonstrate that the CO2 carbonation reaction can greatly enhance the resistance of MgO-fly ash solidified sludge to environmental changes, and the stress-strain behaviour depends mainly on types of durability tests, damage period and carbonation mode. The main carbonation products detected in CO2-MgO-fly ash-sludge system are the elongated prismatic hydromagnesite (skeleton constructing), flower-/bone-like and flaky dypingite and nesquehonite (pore filling and particle cementing). The coupled action of skeleton constructing-filling-cementing enables the CO2 carbonated specimens to be qualified with higher strength, better water stability, and stronger resistance to dry-wet and freeze-thaw cycles. Especially, the continuous immersion in water leads to transition of some interparticle pores into intra-aggregate pores and phase transformation of dypingite and nesquehonite to hydromagnesite. The cyclic dry-wet exposure causes partial transition of intra-aggregate pores into interparticle pores and phase transformation from dypingite and nesquehonite to hydromagnesite. However, no visible transformation between carbonation products can be recognized for specimens under freeze-thaw cycles, except an increased amount of large pores with radius around 10 mu m. (C) 2019 Elsevier Ltd. All rights reserved.
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