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重金属在污水灌溉石灰性土壤中的归宿与分布

Fate and distribution of heavy metals in wastewater irrigated calcareous soils.

作者信息

Stietiya Mohammed Hashem, Duqqah Mohammad, Udeigwe Theophilus, Zubi Ruba, Ammari Tarek

机构信息

Department of Land, Water and Environment, Faculty of Agriculture, The University of Jordan, Amman 11942, Jordan.

School of Plant and Soil Science, Texas Tech University, Lubbock, TX 79409-2122, USA.

出版信息

ScientificWorldJournal. 2014 Mar 2;2014:865934. doi: 10.1155/2014/865934. eCollection 2014.

Abstract

Accumulation of heavy metals in Jordanian soils irrigated with treated wastewater threatens agricultural sustainability. This study was carried out to investigate the environmental fate of Zn, Ni, and Cd in calcareous soils irrigated with treated wastewater and to elucidate the impact of hydrous ferric oxide (HFO) amendment on metal redistribution among soil fractions. Results showed that sorption capacity for Zarqa River (ZR1) soil was higher than Wadi Dhuleil (WD1) soil for all metals. The order of sorption affinity for WD1 was in the decreasing order of Ni > Zn > Cd, consistent with electrostatic attraction and indication of weak association with soil constituents. Following metal addition, Zn and Ni were distributed among the carbonate and Fe/Mn oxide fractions, while Cd was distributed among the exchangeable and carbonate fractions in both soils. Amending soils with 3% HFO did not increase the concentration of metals associated with the Fe/Mn oxide fraction or impact metal redistribution. The study suggests that carbonates control the mobility and bioavailability of Zn, Ni, and Cd in these calcareous soils, even in presence of a strong adsorbent such as HFO. Thus, it can be inferred that in situ heavy metal remediation of these highly calcareous soils using iron oxide compounds could be ineffective.

摘要

用处理后的废水灌溉的约旦土壤中重金属的积累威胁着农业的可持续性。本研究旨在调查用处理后的废水灌溉的石灰性土壤中锌、镍和镉的环境归宿,并阐明水合氧化铁(HFO)改良剂对土壤各组分间金属再分配的影响。结果表明,所有金属在扎尔卡河(ZR1)土壤中的吸附能力均高于瓦迪杜莱伊(WD1)土壤。WD1土壤对金属的吸附亲和力顺序为镍>锌>镉,与静电吸引一致,表明与土壤成分的结合较弱。添加金属后,锌和镍分布在碳酸盐和铁/锰氧化物组分中,而镉则分布在两种土壤的可交换和碳酸盐组分中。用3%的HFO改良土壤并没有增加与铁/锰氧化物组分相关的金属浓度,也没有影响金属的再分配。该研究表明,即使存在HFO这样的强吸附剂,碳酸盐也能控制这些石灰性土壤中锌、镍和镉的迁移率和生物有效性。因此,可以推断,使用铁氧化物化合物对这些高石灰性土壤进行原位重金属修复可能无效。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1225/3958744/a334178a1c36/TSWJ2014-865934.001.jpg

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