密度及干湿循环影响下的煤系土土-水特征曲线
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杨继凯(1992—),男,硕士研究生,研究方向为滑坡与路基病害防治。

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TU44

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国家自然科学基金项目(51568022);江西省自然科学基金项目(20171BAB206056);江西省高等学校科技落地计划 (KJLD13036)


Effects of Density and Drying-wetting Cycle on Soil Water Characteristic Curve of Coal Soil
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    摘要:

    利用 PF 土壤水分特征曲线仪,测定了不同干密度的重塑非饱和煤系土试样的土-水特征曲线;并对其中一组试样进行 3 次干湿循环试验,并利用 VG 模型对实测数据进行拟合,初步研究了煤系土土-水特征曲线在干湿循环条件下的变化规律。 研究结果表明:干密度对煤系土的土-水特征曲线有较大影响,干密度越大的试样饱和含水率越低,失水速率也越慢,持水能力越好,土-水特征曲线也越平缓;干湿循环作用使得煤系土孔隙相互贯通扩张,孔隙率增大,土体的持水能力减弱,干湿循环对煤系土 SWCC 的影响主要集中在第 1 次干湿循环, 3 次干湿循环后煤系土 SWCC 基本稳定。

    Abstract:

    A series of tests were carried out by means of PF-type SWCC device for SWCCs for remodelled un- saturated coal soil specimens at different initial dry density in this study. Based on test results, the influence of initial dry density on unsaturated coal soil soil water characteristic curve were studied through analyzing the VG curve model. The three times of drying-wetting cycles tests for a specimen at certain initial density were also carried out. The research results show that the dry density has a great influence on the soil-water characteristic curves of coal-bearing soil. Specimens with higher dry density generally have lower saturated content, higher water-losing speed, and better water-holding capacity. The drying-wetting cycles leads to structure change and big pore increase in soil, and water-holding capacity of coal soil can also be reduced. The effect of the 1st dry- ing-wetting cycle on coal soil SWCCs is most obvious. The SWCC of the coal soil is basically stable after the third wet-dry cycle.

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杨继凯,郑明新.密度及干湿循环影响下的煤系土土-水特征曲线[J].华东交通大学学报,2018,35(3):91-96.

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  • 在线发布日期: 2021-05-25
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