Sorption of Nickel(II) on a Calcareous Aridisol Soil, China: Batch, XPS, and EXAFS Spectroscopic Investigations

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作者
Shirong Qiang
Bin Han
Xiaolan Zhao
Yunbo Yang
Dadong Shao
Ping Li
Jianjun Liang
Qiaohui Fan
机构
[1] Key Laboratory of Petroleum Resources,
[2] Gansu Province/CAS Key Laboratory of Petroleum Resources Research,undefined
[3] Institute of Geology and Geophysics,undefined
[4] Chinese Academy of Sciences,undefined
[5] Key Laboratory of Preclinical Study for New Drugs of Gansu Province,undefined
[6] and Institute of Physiology,undefined
[7] School of Basic Medical Sciences,undefined
[8] Lanzhou University,undefined
[9] Graduate University of Chinese Academy of Sciences,undefined
[10] Institute of Plasma Physics,undefined
[11] Chinese Academy of Sciences,undefined
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摘要
The sorption of Ni(II) on a calcareous aridisol (CA) soil, one of the major soil types in northwestern China, was investigated using batch and extended X-ray absorption fine structure (EXAFS) approaches in a 0.01 mol/L NaClO4 solution at different pH values (6.0–10.0), temperatures (25–60 °C) and contact times (2–15 days). Under alkaline conditions, EXAFS analysis showed that the interatomic distances between Ni and O atoms (RNi-O) were approximately 2.04 Å with a typical coordination number (CN) of ~6.0 O atoms in the contact time range from 2 to 15 days. The RNi-Ni (~3.07 Å) suggested that the structure of the Ni(II) adsorbed on the CA soil was basically the same as that of Ni(OH)2(s), while the Ni-Al shell (RNi-Al ~3.16 Å) gradually formed and grew with the increasing contact time. Under weakly acidic conditions, the sorption mechanism of Ni(II) on the CA soil possibly included at least two processes: (i) a fast accumulation dominated by ion exchange and surface complexation and (ii) the formation of a Ni-Al LDH phase over the long term. A high temperature is beneficial to the fixation of Ni(II) on the CA soil and the formation of a Ni-Al LDH.
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