Grain size distribution of collapsed scraps of argillaceous rock and its relationship with expansibility: An experimental study
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Grain size distribution of collapsed scraps of argillaceous rock and its relationship with expansibility: An experimental study
Vol. 34, Issue 1, (2013)
作者机构:
1. 中国科学院地质与地球物理研究所 工程地质力学重点试验室,北京,100029
2. 中国科学院研究生院,北京,100049
3. 铁道第三勘察设计院集团有限公司,天津,300142
4. 西南交通大学 土木工程学院,成都,610031
作者简介:
基金信息:
DOI:
CLC:TU452
Online First:10 January 2013,
Published:2013
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ZHANG Wei1, 2, SHANG Yan-jun, et al. Grain size distribution of collapsed scraps of argillaceous rock and its relationship with expansibility: An experimental study[J]. 2013, 34(1).
DOI:
ZHANG Wei1, 2, SHANG Yan-jun, et al. Grain size distribution of collapsed scraps of argillaceous rock and its relationship with expansibility: An experimental study[J]. 2013, 34(1).DOI:
Grain size distribution of collapsed scraps of argillaceous rock and its relationship with expansibility: An experimental study
Slaking is one of the most basic characteristics of swelling rocks. However
criteria refer to slaking and characteristics of collapsed scraps are rare among rapid identification and classification criteria available. Thus
it is necessary to explore into slaking and grain size distribution (GSD) of the dry collapsed scraps of swelling rock and their relationships with the level of expansibility
which can complete the rapid identification and classification criteria with respect to slaking. With argillaceous rock samples collected from Daban Tunnel in Xinjiang Uygur Autonomous Region
and Heidong Cavern of Taizhou and Shepan Island in Zhejiang province
laboratory tests of saturated water absorptivity of dry rock block and slaking test are conducted; and GSD of the dry collapsed scraps
slake durability index and their relationship with expansibility derived from saturated water absorptivity of the swelling rock are analyzed. Results show that the effective grain size
grain sizes of the particle group with the maximum content and slake durability index are inversely correlated with the level of expansibility of the swelling rock. It is concluded that GSD of dry collapsed scraps of swelling rock can approximately act as an indicator for the level of expansibility.