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ID 35654
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title alternative
An experimental study on the swelling properties of soils gathered in the fi eld of the Shobara disaster, Hiroshima Prefecture <Articles>
creator
Uemori, Hiroki
NDC
Earth sciences. Geology
abstract
A lot of slope failures and debris flows occurred at Shobara on July 16, 2010. Some characteristic phenomena were seen by the course that the failure materials flowed down. In many places, surface soils were left without being eroded deeply, though debris materials passed on them. To clarify the cause, we have made some experiments with the soils of Shobara. From the analysis using the X-ray diffraction device, we found out that vermiculite with the swelling characteristic was mainly included. From the swelling check examination between 1000 hours, water more than the volume of initial void before the test was absorbed. Also, from the measuring of the swelling pressure, the maximum value of 9.68 kPa was recorded between 500 hours. These results suggest that the soils of Shobara remained in a kind of unsaturated condition in spite of heavy rainfall during 3 hours, therefore, they were not eroded deeply.
journal title
Bulletin of the Graduate School of Integrated Arts and Sciences, Hiroshima University. II, Studies in environmental sciences
volume
Volume 8
start page
69
end page
75
date of issued
2013-12-31
publisher
広島大学大学院総合科学研究科
issn
1881-7696
ncid
SelfDOI
language
jpn
nii type
Departmental Bulletin Paper
HU type
Departmental Bulletin Papers
DCMI type
text
format
application/pdf
text version
publisher
rights
Copyright (c) 2013 Graduate School of Integrated Arts and Sciences, Hiroshima University. All rights reserved.
department
Graduate School of Integrated Arts and Sciences
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