玉龍雪山西麓原狀冰磧土CT掃描試驗(yàn)研究
[Abstract]:Moraine soil is a kind of special geotechnical material, which is formed by the rapid mixed accumulation of drift stone, gravel, silty soil and clay in the process of glacier melting. The engineering problems caused by it have been paid more and more attention in geotechnical engineering field. The micro-fabric of gravel particles is a reflection of the unique depositional history of moraine soil, which directly affects the geotechnical mechanical properties of soil. However, it is very difficult to obtain the original moraine soil samples. So far, there have been few studies in geotechnical engineering field. In view of this, the undisturbed moraine samples at the western foot of Yulong Xueshan Mountain were successfully obtained by means of artificial fine cutting, and the original samples of 6 moraine soils were scanned by CT, and the true meso-fabric images of the moraine soil were obtained for the first time. After binarization and de-noising of CT images by Matlab, the profile fabric indexes of gravel particles in moraine soil, such as surface content of gravel, grain orientation and particle shape, were described by using conventional statistical methods. The results show that the statistical difference between the vertical section and the horizontal section is small, but the difference between the vertical section and the horizontal section is large.
【作者單位】: 中國(guó)科學(xué)院武漢巖土力學(xué)研究所巖土力學(xué)與工程國(guó)家重點(diǎn)實(shí)驗(yàn)室;
【基金】:國(guó)家自然科學(xué)基金資助項(xiàng)目(No.41172286) 廣西巖土力學(xué)與工程重點(diǎn)實(shí)驗(yàn)室資助課題(No.11-KF-03)
【分類(lèi)號(hào)】:TU445
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