Application Of Schmidt Hammer Rebound Test For Weathering Profile Classification Of Granite, Paya Terubong, Penang, Malaysia

Warta Geologi Pub Date : 2022-04-28 DOI:10.7186/wg481202203
Mohamad Anuri Ghazali, M. R. Umor, Mohd Syafiq Hussin, A. G. Md. Rafek
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Abstract

Weathering profile characterization is one of the significant information in the interpretation of the condition of rock. In addition, the tropical climate in Malaysia causes the deep–seated weathering phenomena of granitic rock. The identification of weathering profile of granite can be made using in–situ Schmidt hammer rebound test which is one of the non–destructive tests (NDT) that is widely used. In this study, the test is carried out on granitic rock in Paya Terubong, Pulau Pinang. Based on the study conducted, the value for each of weathering grade of granite can be identified. The value for fresh granite (Grade I) is greater than 55, slightly weathered granite (Grade II) is ranging from 35 – 55, moderately weathered granite (Grade III) is ranging from 17 – 35 and highly weathered granite (Grade IV) is less than 17. Completely weathered granite (Grade V) and residual soil (Grade VI) do not have any Schmidt hammer rebound values. This method can be used as a very useful method in the field to determine the degree of weathering of rock outcrops.
施米特锤回弹试验在马来西亚槟城巴雅特鲁邦花岗岩风化剖面分类中的应用
风化剖面表征是解释岩石状态的重要信息之一。此外,马来西亚的热带气候导致了花岗岩的深层风化现象。现场施密特锤回弹试验是目前应用较为广泛的无损检测方法之一,可用于花岗岩风化剖面的识别。在本研究中,试验是在槟榔屿巴雅特鲁邦的花岗岩上进行的。在此基础上,确定了花岗岩各风化等级的值。新鲜花岗岩(I级)的值大于55,轻度风化花岗岩(II级)的值在35 ~ 55之间,中度风化花岗岩(III级)的值在17 ~ 35之间,高度风化花岗岩(IV级)的值小于17。完全风化的花岗岩(V级)和残积土(VI级)没有任何施密特锤回弹值。该方法可作为野外确定露头岩石风化程度的一种非常有用的方法。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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