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生物炭在土壤中直接固定镉的能力随老化而发生显著变化:对镉污染土壤生物炭修复的启示。

Marked changes in biochar's ability to directly immobilize Cd in soil with aging: implication for biochar remediation of Cd-contaminated soil.

作者信息

Ren Xinhao, He Jiayi, Chen Qiao, He Fei, Wei Ting, Jia Honglei, Guo Junkang

机构信息

School of Environmental Science and Engineering, Shaanxi University of Science & Technology, Xi'an, 710021, People's Republic of China.

Shaanxi Huadi Survey and Design Consulting Co. LTD, Xi'an, 710020, People's Republic of China.

出版信息

Environ Sci Pollut Res Int. 2022 Oct;29(49):73856-73864. doi: 10.1007/s11356-022-21000-8. Epub 2022 May 27.

Abstract

To investigate the change in biochar's ability to directly immobilize Cd in soil, a successive wheat cultivation experiment was conducted. Three biochars with different Cd adsorption mechanisms were added to the soils, and a mesh bag was used to separate the soil particles (> 1 μm) from the biochar. The results showed that the ash contents and anionic contents (CO and PO) of the biochar decreased with the cultivation time, while the oxygen-containing functional group content and CEC of the biochar increased. As a result, the Cd concentration on biochar decreased, by 68.9% for WBC300, while unstable Cd species (acid soluble and reducible fraction of Cd) on biochar increased with successive cultivation, increasing from 3 to 17% for WBC300 in FS. Correspondingly, the ability of biochar to inhibit Cd accumulation in wheat decreased. The results of this study illustrated that the ability of biochar to directly immobilize Cd in soil is not permanent; it gradually decreases with aging in soil. The adsorption mechanism of Cd on biochar changed from precipitation to complexation, and ion exchange processes could be the main reason.

摘要

为研究生物炭在土壤中直接固定镉能力的变化,开展了连续小麦种植试验。将具有不同镉吸附机制的三种生物炭添加到土壤中,并用网袋将土壤颗粒(> 1μm)与生物炭分离。结果表明,生物炭的灰分含量和阴离子含量(CO和PO)随种植时间降低,而生物炭的含氧官能团含量和阳离子交换量增加。结果,生物炭上的镉浓度降低,WBC300降低了68.9%,而生物炭上不稳定的镉形态(酸溶态和可还原态镉)随连续种植增加,在FS中WBC300从3%增加到17%。相应地,生物炭抑制小麦中镉积累的能力降低。本研究结果表明,生物炭在土壤中直接固定镉的能力不是永久性的;它会随着在土壤中的老化而逐渐降低。镉在生物炭上的吸附机制从沉淀转变为络合,离子交换过程可能是主要原因。

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