4.5 Article

Effect of basic oxygen furnace slag particle size on sequestration of carbon dioxide from landfill gas

期刊

WASTE MANAGEMENT & RESEARCH
卷 37, 期 5, 页码 469-477

出版社

SAGE PUBLICATIONS LTD
DOI: 10.1177/0734242X18823948

关键词

Basic oxygen furnace slag; carbon dioxide sequestration; landfill gas; landfill cover; particle size

资金

  1. U.S. National Science Foundation [grant CMMI] [1724773]
  2. Div Of Civil, Mechanical, & Manufact Inn
  3. Directorate For Engineering [1724773] Funding Source: National Science Foundation

向作者/读者索取更多资源

The mineral carbon sequestration capacity of basic oxygen furnace (BOF) slag offers great potential to absorb carbon dioxide (CO2) from landfill emissions. The BOF slag is highly alkaline and rich in calcium (Ca) containing minerals that can react with the CO2 to form stable carbonates. This property of BOF slag makes it appealing for use in CO2 sequestration from landfill gas. In a previous study, CO2 and CH4 removal from the landfill gas was investigated by performing batch and column experiments with BOF slag under different moisture and synthetic landfill gas exposure conditions. The study showed two stage CO2 removal mechanism: (1) initial rapid CO2 removal, which was attributed to the carbonation of free lime (CaO) and portlandite [(Ca(OH)(2))], and (2) long-term relatively slower CO2 removal, which was attributed to be the gradual leaching of Ca2+ from minerals (calcium-silicates) present in the BOF slag. Realising that the particle size could be an important factor affecting total CO2 sequestration capacity, this study investigates the effect of gradation on the CO2 sequestration capacity of the BOF slag under simulated landfill gas conditions. Batch and column experiments were performed with BOF slag using three gradations: (1) coarse (D-50 = 3.05 mm), (2) original (D-50 = 0.47 mm), and (3) fine (D-50 = 0.094 mm). The respective CO2 sequestration potentials attained were 255 mg g(-1), 155 mg g(-1), and 66 mg g(-1). The highest CO2 sequestration capacity of fine BOF slag was attributed to the availability of calcium containing minerals on the slag particle surface owing to the highest surface area and shortest leaching path for the Ca2+ from the inner core of the slag particles.

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