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51#
發(fā)表于 2025-3-30 11:57:08 | 只看該作者
52#
發(fā)表于 2025-3-30 13:07:33 | 只看該作者
53#
發(fā)表于 2025-3-30 17:43:19 | 只看該作者
54#
發(fā)表于 2025-3-31 00:38:00 | 只看該作者
Learning from VLSI Design Experience of unsaturated granular material under plane strain conditions. The required calibration of the new device is presented in detail. Saturated soil samples were tested in the new device under isotropic consolidation conditions. The volume changes of the specimen were measured by two alternative metho
55#
發(fā)表于 2025-3-31 04:21:46 | 只看該作者
56#
發(fā)表于 2025-3-31 06:32:24 | 只看該作者
57#
發(fā)表于 2025-3-31 10:31:09 | 只看該作者
58#
發(fā)表于 2025-3-31 16:12:28 | 只看該作者
Conclusion: Learning from Finland?,n be measured reaches 1500 kPa with no difficulty. The tests were carried out in two boxes of 160× 50× 60 cm under laboratory conditions. The equipment used included a 15 m.c.a. ceramic block pressure sensor, de-aerated water and a special acrylic tube specifically designed for this instrument. The
59#
發(fā)表于 2025-3-31 17:45:17 | 只看該作者
Learning from Imbalanced Data Sets, d, with a number of variables: vertical deformation, stress ratio, η, confining stress, p, plastic work, W., suction, s, and some derived normalized variables. It was found that the common framework of dilatancy being a function of the current stress ratio and the limiting stress ratio is far from
60#
發(fā)表于 2025-3-31 21:43:56 | 只看該作者
Liqiang Nie,Xuemeng Song,Tat-Seng Chuaelocity will control the shear strength due to pore pressure effects in the shear zone. However, the antagonistic effects of overpressure of the pore fluid and compression of grains due to suction tension act on a micro-scale in unsaturated fine grained soils and influence the shear behaviour differ
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