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首页> 外文期刊>European Journal of Soil Science >Short-term effects of biochar on soil heavy metal mobility are controlled by intra-particle diffusion and soil pH increase.
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Short-term effects of biochar on soil heavy metal mobility are controlled by intra-particle diffusion and soil pH increase.

机译:生物炭对土壤重金属迁移率的短期影响是通过颗粒内扩散和土壤pH升高来控制的。

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摘要

Biochar, the solid product of biomass pyrolysis, can be used as a soil amendment to stabilize metals in contaminated soils. The effects of biochar on the mobility of metals in soils are, however, poorly understood. To identify the predominant processes, we focused on (i) a possible kinetic limitation by transport in biochar particles, (ii) the evolution of biochar mineral phases and (iii) the effect of biochar on soil pH. Batch experiments were conducted to measure the sorption kinetics of copper (Cu), cadmium (Cd) and nickel (Ni) and the sorption-desorption isotherms for lead (Pb), Cu, Cd, zinc (Zn) and Ni in a wood-derived biochar. Sorption data were then compared with extraction test results using biochar with one acidic and one basic soil contaminated by Zn, Cd and Pb. Kinetic results showed that biochar particle sizes controlled metal sorption rate despite a similar specific surface area, which indicated a limitation by intra-particle diffusion. Isotherms showed a partially reversible sorption to biochar following the order Pb > Cu > Cd >= Zn > Ni, which we explained primarily by the (co)precipitation of metals or their adsorption on specific biochar mineral phases. Effective metal immobilization was observed with biochar in both contaminated soils but could not be predicted from the sorption isotherms. This immobilization appeared to be governed by the soil pH increase, which induced a greater retention of metals on soil particles. Short-term effects of biochar on contaminated soils may therefore be controlled by diffusion in biochar particles and by soil alkalinization processes.
机译:生物炭是生物质热解的固体产物,可以用作土壤改良剂,以稳定污染土壤中的金属。然而,人们对生物炭对土壤中金属迁移率的影响知之甚少。为了确定主要过程,我们集中于(i)生物炭颗粒中的运输可能引起的动力学限制,(ii)生物炭矿物质相的演化,以及(iii)生物炭对土壤pH的影响。进行了分批实验,测量了木材中铜(Cu),镉(Cd)和镍(Ni)的吸附动力学以及铅(Pb),Cu,Cd,锌(Zn)和Ni的吸附-解吸等温线。衍生生物炭。然后将吸附数据与使用一种具有Zn,Cd和Pb污染的酸性和一种碱性土壤的生物炭的提取测试结果进行比较。动力学结果表明,尽管具有相似的比表面积,生物炭的粒径仍控制着金属的吸附速率,这表明了颗粒内扩散的限制。等温线显示出对生物炭的部分可逆吸附,顺序为Pb> Cu> Cd> = Zn> Ni,我们主要通过金属的(共)沉淀或它们在特定生物炭矿物相上的吸附来解释。在两种被污染的土壤中均观察到了有效的金属炭固定化,但无法通过吸附等温线预测。这种固定化似乎是由土壤pH升高控制的,土壤pH升高导致金属在土壤颗粒上的保留更大。因此,可通过在生物炭颗粒中扩散和通过土壤碱化过程来控制生物炭对受污染土壤的短期影响。

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