Japan suffers from landslide hazards, especially in the granitic rock areas. In 2014, many slope failures occurred in western and central Japan and more than 70 people were killed. Granite weathering produces grus and core stones, which often cause severe landslides under intense rainfall. This phenomenon has been recognised for a long time; however, the weathering condition of these granitic areas has not been investigated. This study explored the chemical and mineralogical properties of samples from bedrock and soils in granite landslide areas. Granitic rocks taken from several areas of central to southwestern Japan were analysed. All of these areas have suffered from landslides in recent decades. A series of samples of bedrock, slip surface and surface soil samples were collected from these landslide-prone areas. For mineralogical and chemical properties, X-ray powder diffraction analysis (XRD) and SEM-EDS analysis were carried out. Quartz, k-feldspar, plagioclase and biotite were mainly found in bedrock samples, whereas clay minerals such as kaolin minerals, mica clay minerals and vermiculite or 14Å intergrade minerals were found in the soil samples. Based on the chemistry data, chemical weathering indices were calculated, including: Si–Al ratio, product index (PI), Si–Ti index, chemical index of alteration (CIA), chemical index of weathering (CIW), Vogt. ratio (V), plagioclase index of alteration (PIA), modified weathering potential index (MWPI), parker index (WIP) and Al–Ti index. These index values showed weathering progress in the order from bedrock, slip surface and upper surface soil. To consider climatic influence, the relationships between mean annual air temperature and chemical indices of CIA and Si–Al ratio were investigated. The CIA values for soil samples increased with temperature, whereas the Si–Al ratio decreased with temperature. Those values for bedrock had no correlation, which means that original bedrock condition is almost the same across these areas. On the other hand, there seemed to be no relationship between mean annual precipitation (1981-2010) and weathering indices. The results clearly show the effects of temperature on chemical weathering of granite landslide areas in central-southwest Japan.
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