Lu Lin, Yan Li-Ling, Liang Mei-Na, Cheng Guan-Wen, Zhu Zong-Qiang, Zhu Yi-Nian, Wang Dun-Qiu
School of Environmental Science and Engineering, Guilin University of Technology, Guilin 541004, China.
Guangxi Key Laboratory of Environmental Pollution Control Theory and Technology, Guilin 541004, China.
Huan Jing Ke Xue. 2022 Nov 8;43(11):5214-5223. doi: 10.13227/j.hjkx.202112162.
In this study, original mulberry-biochar (M-BC) and magnetic iron oxide/mulberry stem biochar (Fe-BC) materials were prepared and characterized using mulberry stems as the raw material. The effects of carbonized temperature of Fe-BC and M-BC on dissolved organic carbon (DOC) and arsenic(As) speciation in soil leaching solutions were studied using soil incubation experiments. The results showed that:① Fe-BC was mainly composed of FeO and was magnetic, and the main functional groups were a C=O double bond, O-H bond, C-O bond, and Fe-O bond. The point of zero charge values (pH) of Fe-BC-400, Fe-BC-500, and Fe-BC-600 were 8.92, 8.74, and 9.19, respectively, and the specific surface areas of Fe-BC-400, Fe-BC-500, and Fe-BC-600 were 447.412, 482.697, and 525.708 m·g, respectively. ② With the increase in the carbonization temperature of M-BC and Fe-BC, the (DOC) of soil leaching solution decreased 11.6-315.6 mg·L and 78-365.6 mg·L, respectively. The DOC concentration of soil leaching solution was negatively correlated with soil EC. On day 35 of the incubation experiments, compared with that in soil after incubation without biochar (control), the As concentration of the soil leaching solution with Fe-BC-600 decreased by 55.96%, and there was no significant correlation between the As concentration of the soil leaching solution and the DOC concentration of the soil. ③ The available As concentration on day 35 in soil after incubation with Fe-BC was lower than that of the control group; the available As concentration on day 35 in soil incubated with Fe-BC-600 was reduced by 39.21%. ④ The residue As concentration on day 35 in soil incubated with M-BC decreased by 17.76%-49.11%. The residue As content on day 35 in soil incubated with Fe-BC-600 increased by 80%. Fe-BC-600 was most beneficial to reduce the DOC concentration and the available As content in soil leaching solution and increased the residue As content, thus reducing the bioavailability of soil arsenic. Therefore, this study can provide a theoretical basis for magnetic iron oxide/biochar remediation in arsenic-contaminated soil.
在本研究中,以桑树枝条为原料制备了原始桑木炭(M-BC)和磁性氧化铁/桑树枝条生物炭(Fe-BC)材料,并对其进行了表征。通过土壤培养实验研究了Fe-BC和M-BC的碳化温度对土壤淋溶液中溶解有机碳(DOC)和砷(As)形态的影响。结果表明:①Fe-BC主要由FeO组成且具有磁性,主要官能团为C=O双键、O-H键、C-O键和Fe-O键。Fe-BC-400、Fe-BC-500和Fe-BC-600的零电荷点值(pH)分别为8.92、8.74和9.19,Fe-BC-400、Fe-BC-500和Fe-BC-600的比表面积分别为447.412、482.697和525.708 m·g。②随着M-BC和Fe-BC碳化温度的升高,土壤淋溶液的(DOC)分别降低了11.6 - 315.6 mg·L和78 - 365.6 mg·L。土壤淋溶液的DOC浓度与土壤电导率呈负相关。在培养实验的第35天,与未添加生物炭培养后的土壤(对照)相比,添加Fe-BC-600的土壤淋溶液中As浓度降低了55.96%,土壤淋溶液中As浓度与土壤DOC浓度之间无显著相关性。③用Fe-BC培养后第35天土壤中有效As浓度低于对照组;用Fe-BC-600培养后第35天土壤中有效As浓度降低了39.21%。④用M-BC培养后第35天土壤中残留As浓度降低了17.76% - 49.11%。用Fe-BC-600培养后第35天土壤中残留As含量增加了80%。Fe-BC-600最有利于降低土壤淋溶液中的DOC浓度和有效As含量,并增加残留As含量,从而降低土壤砷的生物有效性。因此,本研究可为磁性氧化铁/生物炭修复砷污染土壤提供理论依据。