Iron oxide precipitate in seepage of groundwater from a landslide slip zone

被引:22
作者
Zheng, Guodong [1 ]
Lang, Yuhua
Miyahara, M.
Nozaki, T.
Haruaki, T.
机构
[1] Chinese Acad Sci, Lanzhou Ctr Oil & Gas Resources, Inst Geol & Geophys, Lanzhou 730000, Peoples R China
[2] Hiroshima Univ, Dept Earth & Planetary Syst, Grad Sch Sci, Higashihiroshima 7398526, Japan
[3] CNK GeoTech Inst Inc, Toyama 9330824, Japan
[4] Tohoku Univ, Grad Sch Sci, Aoba Ku, Sendai, Miyagi 9808578, Japan
来源
ENVIRONMENTAL GEOLOGY | 2007年 / 51卷 / 08期
基金
日本学术振兴会;
关键词
hydrous ferric oxide; redox condition; slip zone; Kumanashi Landslide; Japan;
D O I
10.1007/s00254-006-0442-7
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Orange precipitate was collected at the mouth of groundwater drainage tubes from the Kumanashi Landslide slip zone in Toyama prefecture, Northwest Japan. Data from XRF, X-ray diffraction, and Mossbauer spectroscopy determined the precipitate as hydrous ferric oxide (HFO) bearing multi-elements such as phosphorous, silica, calcium, etc. The occurrence of HFO may indicate an oxidation of ferrous iron in the percolated groundwater from the slip zone. Moreover, the precipitate iron should be mobilized with groundwater circulation from the slip zone, whose reducing condition was determined by the iron speciation on the same type of landslide profiles within the study area in previous studies. The HFO precipitate may be considered as a secondary reliable indicator to locate the seepage of a slip zone on surface, especially for a landslide newly investigated under wet-warm climate.
引用
收藏
页码:1455 / 1464
页数:10
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