Enrichment of trace elements in ferromanganese concretions from terra rossa and their potential desorption
Enrichment of trace elements in ferromanganese concretions from terra rossa and their potential desorption
复制标题
红土铁锰结核中微量元素的富集及其潜在的解吸
DOI:
10.2343/geochemj.1.0156
复制
发表时间:
2012-04
影响因子:
0.8
通讯作者:
Ji-Feng Zhang
中科院分区:
文献类型:
--
作者:
Jin-Liang Feng;Yong-Chong Lin;Shao-Peng Gao;Ji-Feng Zhang
The distributions of trace elements in ferromanganese concretions (FMCs) and the surrounding terra rossa (TR) matrix overlying dolomite have been examined to extend our understanding of their mobilization, redistribution and fractionation during karst weathering and pedogenesis. This study demonstrates that the characteristics of trace elements in TR have been severely overprinted by weathering and pedogenetic processes. The composition of trace elements in FMCs within TR soil profiles varies greatly with depth. The concentrations of Be, Ni, Cu, Zn, As and Bi in FMCs fluctuate and tend to increase with depth; other trace element concentrations fluctuate in the profile but show no clear trend. The toxic elements Cr, As, Cd, Tl and Pb, as well as Co, are significantly enriched in FMCs relative to the surrounding TR matrix: arsenic exhibits strong affinity with Fe, but Cr and Cd contents are not significantly correlated with either Mn or Fe. Correspondingly, Co, Tl and Pb are related to the Mn in FMCs rather than the Fe. In FMCs, trace element distribution and partitioning in the Mn‐Fe phases are governed by the location-specific formational pedoenvironment, with the weathering front etching downwards. Experiments with simulated acid rain indicate that desorption of elements from FMCs is generally pH-dependent regardless of the variation of the released amounts and their desorbability. Moreover, it seems that toxic elements bonded to Mn-phase were easily desorbed from FMCs. As a result, the bioavailability, mobility and activity of some toxic elements in FMCs and TR are potentially increased in field areas experiencing severe soil erosion and acid rain.
登录
查看更多内容
影响因子:
3.9
作者:
A. Mee;E. Bestland;Nigel A. Spooner
通讯作者:
A. Mee;E. Bestland;Nigel A. Spooner
影响因子:
2.2
作者:
N. Whitehead;J. Hunt;D. Leslie;P. Rankin
通讯作者:
N. Whitehead;J. Hunt;D. Leslie;P. Rankin
影响因子:
6.1
作者:
J. Marques;Darrell G Schulze;Nilton Curi;S. Mertzman
通讯作者:
J. Marques;Darrell G Schulze;Nilton Curi;S. Mertzman
影响因子:
2.2
作者:
P. Rankin;C. W. Childs
通讯作者:
P. Rankin;C. W. Childs
影响因子:
6.1
作者:
B. Dawson;J. Fergusson;A. Campbell;E. Cutler
通讯作者:
B. Dawson;J. Fergusson;A. Campbell;E. Cutler