School of Earth Sciences and Engineering, Nanjing University, Nanjing, 210023, China.
School of Earth Sciences and Engineering, Nanjing University, Nanjing, 210023, China; Frontiers Science Center for Critical Earth Material Cycling, Nanjing University, Nanjing, 210023, China.
Chemosphere. 2024 Aug;362:142596. doi: 10.1016/j.chemosphere.2024.142596. Epub 2024 Jun 12.
Biochar has shown promising potential for soil remediation, yet its impact on heavy metals (HMs) immobilization often overlooks soil structure, which could influence soil cracking behavior and HMs transport. To address this gap, this study investigates the role of soil structure (dry density and aggregate size) on the cracking and cadmium (Cd) leaching behavior of biochar-amended fine-grained soils. A series of semi-dynamic leaching tests were conducted on samples with and without wetting-drying (W-D) cycles. Based on the proposed improved method for quantifying the effective diffusion coefficient (D) of Cd in unsaturated soils and microstructural analyses, we found that: (1) Higher dry density and larger aggregate generally resulted in smaller D by decreasing soil pore volume. (2) Biochar could connect isolated pores within large aggregates through its internal pores, yielding greater increases in D (294.8%-469.0%) compared to small aggregates (29.1%-77.4%) with 3% biochar. However, further increases in biochar dosage led to decreased D, primarily due to the dense pore structure. (3) Biochar effectively inhibited soil cracking, achieving the highest reduction of 36.8% in surface crack ratio. (4) After W-D cycles, samples exhibited higher D with increasing dry density, with aggravated cracking being the primary cause, suggesting preferential flow within the cracks, particularly those penetrating the soil. This study highlights the importance of careful consideration of soil structure and cracking potential before in situ field application of biochar as a remediation agent for HMs-contaminated fine-grained soils.
生物炭在土壤修复方面显示出了有前景的潜力,但它对重金属(HMs)固定的影响往往忽略了土壤结构,而土壤结构可能会影响土壤开裂行为和 HMs 的迁移。为了解决这个问题,本研究调查了土壤结构(干密度和团聚体大小)对添加生物炭的细粒土壤的开裂和镉(Cd)淋滤行为的影响。对有和没有干湿(W-D)循环的样品进行了一系列半动态淋滤试验。基于提出的量化非饱和土壤中 Cd 有效扩散系数(D)的改进方法和微结构分析,我们发现:(1)较高的干密度和较大的团聚体通常通过减少土壤孔隙体积导致较小的 D。(2)生物炭可以通过其内部孔隙将大团聚体内部的孤立孔隙连接起来,与小团聚体(29.1%-77.4%)相比,D 的增加幅度更大(294.8%-469.0%),而添加 3%的生物炭。然而,进一步增加生物炭的用量会导致 D 的降低,主要是由于密集的孔隙结构。(3)生物炭有效地抑制了土壤开裂,表面裂缝比达到了最高的 36.8%的降幅。(4)经过 W-D 循环后,随着干密度的增加,样品表现出更高的 D,这主要是由于开裂加剧,这表明裂缝内部存在优先流,特别是穿透土壤的裂缝。本研究强调了在将生物炭作为修复剂原位应用于受 HMs 污染的细粒土壤之前,仔细考虑土壤结构和开裂潜力的重要性。