Iron speciation of sliding mud in Toyama Prefecture, Japan

被引：18

作者：

Zheng, GD

Lang, YH

Takano, B

Matsuo, M

Kuno, A

Tsushima, H

机构：

[1] Univ Tokyo, Dept Gen Syst Studies, Grad Sch Arts & Sci, Meguro Ku, Tokyo 1538902, Japan

[2] CNK Geotech Inst Inc, Takaoka, Toyama 9330824, Japan

来源：

JOURNAL OF ASIAN EARTH SCIENCES | 2002年 / 20卷 / 08期

关键词：

iron speciation; Mossbauer spectroscopy; sliding mud; Toyama prefecture;

D O I：

10.1016/S1367-9120(01)00088-8

中图分类号：

P [天文学、地球科学];

学科分类号：

07 ;

摘要：

It has been often observed that black mud recently formed and accumulated in slip planes that are closely associated with a progressing landslide in Japan. Mossbauer spectroscopy revealed that the composition of Fe species in the sliding mud is different from those in the debris rock and bedrock. The sliding mud contains more ferrous iron species, which indicates a relatively stronger reducing condition within the sliding zone than within the host rocks. In addition, the composition of Fe species, the total Fe and the volume of sliding mud also change with landslide development. Therefore, detailed Fe speciation in landslide profiles can be a useful approach to understanding the progress of a landslide and may also predict future sliding as well. (C) 2002 Elsevier Science Ltd. All rights reserved.

引用

页码：955 / 963

页数：9

共 24 条

[1] Effect of organic acids on ferric iron removal from iron-stained kaolinite [J].