Abstract

The experience needed to carry out engineering and construction in diatomaceous earth areas is currently lacking. This project studies the new Hang Shaotai high-speed railway passing through a diatomaceous earth area in Shengzhou, Zhejiang Province, and analyzes the hydrological and mechanical properties of diatomaceous earth on the basis of a field survey and laboratory. Moreover, a new antidrainage subgrade structure was proposed to address the rainy local environment, and field excitation tests were performed to verify the antidrainage performance and stability of the new subgrade structure. Finally, the dynamic characteristics and deformation of the diatomaceous earth roadbed were examined. The hydrophysical properties of diatomaceous earth in the area are extremely poor, and the disintegration resistance index ranges from 3.1% to 9.0%. The antidrainage subgrade structure has good water resistance and stability under dynamic loading while submerged in water. After 700,000 loading cycles, the dynamic stress and vibration acceleration of the surface of the subgrade bed stabilized at approximately 6.37 kPa and 0.94 m/s2, respectively. When the number of excitations reached 2 million, the settlement of the diatomaceous earth foundation was 0.08 mm, and there was basically negligible postwork settlement of the diatomaceous earth foundation. These results provide new insights for engineering construction in diatomaceous earth areas.

Highlights

  • IntroductionPublisher’s Note: MDPI stays neutral with regard to jurisdictional claims in published maps and institutional affiliations

  • The soil moisture variation and the dynamic response of the antidrainage subgrade structure were detervariation the dynamic response ofeffect the antidrainage subgrade structure werethe determined mined toand evaluate the antidrainage of the new antidrainage layer, and propagato evaluate the antidrainage effect of the new antidrainage layer, and the propagation law tion law of the dynamic response within the subgrade was studied

  • The disintegration resistance index of the diatomaceous earth specimens ranged from 3.1% to 9.0%, with an average value of 6.05%, which means that they were weakly resistant to disintegration; When diatomaceous earth was exposed to the natural environment, it was susceptible to disintegration and deterioration with frequent cycling between wet and dry, which led to problems such as softening and strength reduction, disintegration damage, penetration cracks, and other issues

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Summary

Introduction

Publisher’s Note: MDPI stays neutral with regard to jurisdictional claims in published maps and institutional affiliations. Diatomite (diatomaceous earth) is a rock (soil) made of diatom shells deposited over a long period. Diatom shells are the cell walls of the decayed internal material of diatoms, and the main component is hydrated silica, which has a hard texture. The presence of diatoms makes the internal porosity of diatomite (soil) high [1]; in addition, diatomite (soil) exhibits low density, a low permeability coefficient, a strong structure, good adsorption, and easy disintegration in the presence of water [2,3,4]

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