Abstract

As a national development plan, ecological protection of the Yellow River Basin has attracted extensive social attention in recent years. Considering the influence of acid rain on the engineering characteristics of loess in this area, we investigated changes in the physical and mechanical characteristics of remolded loess under the combined action of acid rain and dry-wet cycles by means of triaxial tests, nuclear magnetic resonance spectroscopy, and scanning electron microscopy. The results are as follows: in the acidic environment, the stress-strain relationship of remolded loess undergoes stress hardening after dry-wet cycling. The cohesion and internal friction angle of remolded loess are negatively correlated with the number of cycles. From the multiscale analysis of the dry-wet cycle process under acid rain condition, the T2 spectrum of the test soil has three peaks at the micropore level. With the increasing number of cycles, the spectral area increases gradually, and the sample transitions from small pores to large- and medium-size pores. At the microscopic level, the clay mineral particles among soil particles decrease in size, the contact mode between soil particles develops from stable to unstable, the particles are gradually rounded, and the fractal dimension decreases. Chemical erosion and physical erosion are special features of this experiment. Physical erosion causes particle erosion and pore growth, while chemical erosion includes reactions by feldspar. Together, physical and chemical reactions aggravate the soil deterioration process. These research results have laid a good experimental foundation for the ecological protection of the Yellow River Basin.

Highlights

  • An important means to study the interactions between acid rain and soil is the study of the leaching characteristics and release rules of phosphorus, calcium, magnesium, boron, and other major elements from samples [23, 24]

  • In view of this gap in the literature, this paper takes the environmental and geotechnical problems of the Yellow River Basin as background, studies the physical and mechanical changes in remolded loess for an acid rain environment and dry-wet cycles, and uses results obtained at the macro, meso, and microscale levels to explore damage laws of experimental rocks and soil. e research results are expected to provide a reference for ecological protection and prevention of soil erosion in the Yellow River Basin

  • This paper focuses on the analysis of the changes in soil particle abundance and fractal dimension as a result of the effects of dry and wet cycles

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Summary

Introduction

An important means to study the interactions between acid rain and soil is the study of the leaching characteristics and release rules of phosphorus, calcium, magnesium, boron, and other major elements from samples [23, 24]. Solution properties, an important index of the test results, are not considered, especially as they relate to the macro- and microscale characteristics of soil under the combined action of acid rain erosion and drywet cycles. In view of this gap in the literature, this paper takes the environmental and geotechnical problems of the Yellow River Basin as background, studies the physical and mechanical changes in remolded loess for an acid rain environment and dry-wet cycles, and uses results obtained at the macro-, meso-, and microscale levels to explore damage laws of experimental rocks and soil. To ensure the success of sample preparation, a static pressure sample preparation method was adopted

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