首页|粉煤灰资源利用:无机矿物改良剂对CFA源蛋白石/沙粒团聚体形成的影响

粉煤灰资源利用:无机矿物改良剂对CFA源蛋白石/沙粒团聚体形成的影响

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粉煤灰碱法提铝的副产物-蛋白石(SiO2·nH2O,非晶质二氧化硅)具有很强的吸附性,是土壤中的次生/黏土矿物。将蛋白石与沙粒复配形成团聚体应用于沙漠化土壤修复,是一种前景广阔的大规模生态化处置方式。然而,由于无机矿物质的缺乏,该团聚体与自然土壤团聚体仍有差距。本文通过短期土培实验,研究了石灰石(CaCO3)、脱硫石膏(CaSO4·2H2O)、磷酸钙(Ca3(PO4)2)、赤铁矿(Fe2O3)、三水铝石(Al(OH)3)等无机矿物改良剂对团聚体形成、稳定以及孔隙特征的影响,并阐述了其内在的吸附机理。结果表明,五种改良剂中,只有石膏可有效降低团聚体的pH,且石膏对提升团聚体的保水效果最为显著,但石膏会增大电导率。改良剂均能促进团聚体的形成,提高机械稳定性,石膏、CaCO3、Fe2O3有利于提高团聚体的水稳性。XRD/SEM/FT-IR/XPS等分析表明,无机矿物与沙子/蛋白石发生吸附作用,团聚体表面形成了有利于团聚体生成的无机矿物界面层。与CK相比,改良后的大团聚体(>0。25 mm)以孔径<80 μm的孔隙和边界孔隙为主,孔隙率增加、孔隙数量和平均孔隙直径(MPD)减少、孔隙结构更致密、孔隙间的连通性提高以及孔隙网络更复杂。特别是经脱硫石膏改良后,微团聚体(<0。25 μm)的MPD和2~5 nm 中孔的数量增加,总孔隙体积和0~2 nm 微孔的数量降低;而Ca3(PO4)2和Al(OH)3增加了>15 nm介孔的数量。总之,作为土壤"骨架"的无机矿物有效改善了蛋白石/沙粒团聚体的物理结构,加速了团聚体的形成。因此,脱硫石膏优化了大聚集体的形成和稳定性。经脱硫石膏改良的团聚体可作为类土壤基质,加速退化的沙漠化土壤的生态重建。
Coal fly ash resource utilization:Effects of inorganic minerals amendments on CFA-originated opal/sand aggregates formation
Opal(amorphous silica,SiO2·nH2O),a solid waste byproduct of the alkaline extracting alumina from coal fly ash,exhibits strong adsorption properties and is a secondary/clay mineral in the soil.Combining opal with sand to construct opal/sand aggregates for desertification soil remediation holds the potential for large-scale ecological disposal.Unfortunately,the aggregate structure still gaps from natural soil aggregates resulting from inorganic mineral deficiencies.Herein,the effects of five inorganic mineral amendments,limestone(CaCO3),desulphurization gypsum(CaSO4·2H2O),hematite(Fe2O3),tricalcium phosphate(Ca3(PO4)2)and gibbsites(Al(OH)3),on aggregate formation,stabilization,and pore characteristics without the organic matters were investigated in short-term cultivation experiments.Meanwhile,associated adsorption mechanisms were elucidated.Results indicated only gypsum effectively reduced the aggregate's pH,most enhanced water-holding capacity,albeit increased electrical conductivity.All amendments facilitated aggregate formation and mechanical-stability,with gypsum,CaCO3,and Fe2O3 improving water stability.Various analysis techniques,including XRD,SEM,nano-CT,FT-IR,and XPS,provided insights into the physisorption and chemisorption of minerals onto sand/opal,generating interfaces conducive to aggregation.Compared to CK(control check,without amendment addition),amended macroaggregates demonstrated increased porosity,reduced pore quantity and mean pore diameter(MPD),denser pore structure,improved interpore connectivity,and more complex pore networks,dominated by<80 μm diameters and boundary pores.Notably,desulphurization gypsum elicited the most significant variations,increasing MPD of microaggregates and 2-5 nm mesopores,and decreasing total pore volume and 0-2 nm micropores,while Ca3(PO4)2 and Al(OH)3 improved>15 nm mesopores.Overall,inorganic minerals,the"skeleton"of soil,effectively upgraded opal/sand aggregates'physical structure and accelerated aggregate formation quickly.Therein,desulphurization gypsum optimized macroaggregate formation and stability.Desulphurization gypsum-amended aggregates serve as soil-like substrates to accelerate the ecological reconstruction of desertification areas.

inorganic minerals amendmentsopal/sand aggregatesdesulphurization gypsumaggregate stabilitypore characteristicsdesertification soil remediation

李为轮、王一霖、朱锋、周秋生、刘桂华、彭志宏、齐天贵、申雷霆、李小斌

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School of Metallurgy and Environment,Central South University,Changsha 410083,China

无机矿物改良剂 蛋白石/沙粒团聚体 脱硫石膏 团聚体稳定性 孔隙特征 沙漠化土壤修复

湖南省自然科学基金国家重点研发计划

2022JJ406162022YFC2904404

2024

中南大学学报(英文版)
中南大学

中南大学学报(英文版)

CSTPCDEI
影响因子:0.47
ISSN:2095-2899
年,卷(期):2024.31(4)
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