首页> 外文期刊>Journal of soil & sediments >Dissipation and sorption processes of polycyclic aromatic hydrocarbons (PAHs) to organic matter in soils amended by exogenous rich-carbon material
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Dissipation and sorption processes of polycyclic aromatic hydrocarbons (PAHs) to organic matter in soils amended by exogenous rich-carbon material

机译:外源富碳物质改良土壤中多环芳烃(PAHs)对有机质的耗散和吸附过程

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Purpose The aim of the research was to assess the effect of biochar addition on aging, degradation, and sorption processes of polycyclic aromatic hydrocarbons (PAHs) to soil organic matter. The study was carried out as a sorption experiment in strictly controlled water and air conditions, which allowed for the accurate observation and prediction of PAH behavior in soils. Materials and methods Four soils were fortified with a PAH mixture (Fluorene-Flu, Anthracene-Ant, Phenanthrene-Phe, Pyrene-Pyr, Chrysene-Chry) at 20 mg kg(-1) of single-compound concentration level. The experiment was carried out in two trials: soils + 5PAHs amended with biochar and soil + 5PAHs without biochar addition with incubation times of 0, 1, 3, 6, and 9 months. After each interval time, the extractable (E-SOM) and stable organic matter (S-SOM) were measured as well as PAHs determined in two forms: total concentration (PAH-tot) and residual concentration (PAH-rest) after E-SOM extraction. The PAH loss and half-life times were estimated according to pseudo first-order kinetics equation. Results and discussion The amounts of PAH-tot in the soils without biochar decreased by an average of 92%, while in soil with biochar, this was 41% after 9 months of aging. The amount of PAHs-rest bounded with S-SOM after 9 months of incubation varied from 0.9 to 3.5% and 0.2 to 1.3% of the initial PAH concentration, respectively, for soils non-induced and induced by biochar. In soils without biochar, Flu, Ant, Phe, and Pyr exhibited similar T-1/2 (43-59 days), but Chry was characterized by a much higher and broader T-1/2 than other hydrocarbons (67-280 days). Biochar addition to the soils significantly influenced the half-life changes for all PAHs. The highest changes were noted for Phe (14-fold increase), and the lowest was for Flu (7-fold increase). Conclusions The addition of exogenous-rich carbon material such as biochar to the soil significantly changes the behavior and sorption potential of PAHs in the soil. Soils enriched with biochar are characterized by a higher persistence of PAHs, longer aging time, and lower affinity for sorption by native organic matter structures. Soils freshly polluted by PAH are mainly sorbed by E-SOM, which significantly increases their accessibility and reduces formation of bound-residues in the soil.
机译:目的研究目的是评估生物炭添加对多环芳烃(PAHs)对土壤有机质的老化,降解和吸附过程的影响。该研究是在严格控制的水和空气条件下进行的吸附实验,可以准确观察和预测土壤中的PAH行为。材料和方法用20 mg kg(-1)的单一化合物浓度水平的PAH混合物(氟-氟,蒽-蚂蚁,菲-苯,P-吡,Ch-Chry)强化了四种土壤。该实验在两项试验中进行:土壤+ 5PAHs进行生物炭改良,土壤+ 5PAHs不添加生物炭,孵育时间分别为0、1、3、6和9个月。在每个间隔时间后,测量可萃取物(E-SOM)和稳定有机物(S-SOM)以及以两种形式测定的PAH:E-后的总浓度(PAH-tot)和残留浓度(PAH-rest) SOM提取。根据伪一级动力学方程估算了PAH损失和半衰期。结果与讨论在没有生物炭的土壤中,PAH-tot含量平均下降了92%,而在有生物炭的土壤中,老化9个月后的PAH-tot含量为41%。温育9个月后,与S-SOM结合的PAHs剩余量,对于非生物炭和非生物炭诱发的土壤,分别为初始PAH浓度的0.9%至3.5%和0.2%至1.3%。在没有生物炭的土壤中,Flu,Ant,Phe和Pyr表现出相似的T-1 / 2(43-59天),但是Chry的特征是T-1 / 2比其他碳氢化合物(67-280天)高得多且宽得多)。土壤中添加生物碳显着影响所有多环芳烃的半衰期变化。 Phe的变化最大(增加了14倍),而Flu的变化最小(增加了7倍)。结论向土壤中添加生物炭等外源性富碳材料会显着改变土壤中PAHs的行为和吸附潜力。富含生物炭的土壤的特征是PAHs的持久性更高,老化时间更长,对天然有机物结构吸附的亲和力较低。多环芳烃新鲜污染的土壤主要被E-SOM吸附,这大大增加了土壤的可及性并减少了土壤中结合残留物的形成。

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