昆明理工大学电力工程学院,昆明,650500
纸质出版:2018
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范本贤, 黄 英, 孙书君, 等. 云南红土的循环胀缩特性研究[J]. 水土保持学报, 2018,32(2):120-127.
FAN Benxian, HUANG Ying, SUN Shujun, et al. Study on Cyclic Swell-Shrink Characteristics of Yunnan Laterite[J]. 2018, 32(2): 120-127.
范本贤, 黄 英, 孙书君, 等. 云南红土的循环胀缩特性研究[J]. 水土保持学报, 2018,32(2):120-127. DOI: 10.13870/j.cnki.stbcxb.2018.02.018.
FAN Benxian, HUANG Ying, SUN Shujun, et al. Study on Cyclic Swell-Shrink Characteristics of Yunnan Laterite[J]. 2018, 32(2): 120-127. DOI: 10.13870/j.cnki.stbcxb.2018.02.018.
以云南红土为研究对象,考虑干湿循环时间、干湿循环次数、初始干密度等影响因素,通过膨胀、收缩试验与图像处理相结合的方法,研究不同影响因素对云南红土胀缩特性的影响。结果表明:干湿循环过程中,红土的膨胀过程可以分为快速膨胀、缓慢膨胀和稳定膨胀3个阶段,收缩过程可以分为缓慢收缩、快速收缩和稳定收缩3个阶段。随增湿时间延长,红土的竖向膨胀率、含水率、孔隙率等膨胀参数呈“厂”形增大变化;随脱湿时间延长,竖向收缩率、横向收缩率、体积收缩率等收缩参数呈“S”形增大变化,含水率、孔隙率逐渐减小。随增湿次数增加,稳定竖向膨胀率、横向膨胀率、体积膨胀率呈先急剧增大后缓慢减小的变化;随脱湿次数增加,稳定竖向收缩率、横向收缩率、体积收缩率呈先增大后缓慢波动变化。随初始干密度增大,稳定竖向膨胀率、竖向收缩率、体积膨胀率增大,横向膨胀率、横向收缩率、体积收缩率呈减小变化。竖向膨胀大于竖向收缩,体积膨胀大于体积收缩,横向收缩大于竖向收缩。
Taking Yunnan laterite as the research object
this paper studied the effects of different factors on the swell-shrink characteristics of Yunnan laterite and the influencing factors such as wetting-drying cycle time
wetting-drying cycle times and initial dry density were taken into account through the method of expansion and shrinkage test combined with image processing. The results showed that the expansion process of laterite can be divided into 3 stages: rapid expansion
slow expansion
and stable expansion. The contraction process could also be divided into 3 stages: slow contraction
rapid contraction
and stable contraction. With the increase of wetting time
the vertical expansion rate
moisture content
porosity and other expansive parameters of laterite increased as the “厂” type. The shrinkage parameters such as vertical shrinkage
transverse shrinkage
volume shrinkage and so on increased with the time of dewetting
showing the change of “S” type
and the moisture content and porosity decrease gradually. With the increase of humidification times
the stability of vertical expansion rate
the transverse expansion rate
and the volume expansion rate increased sharply first and then decreased slowly. With the increase of dehumidifying times
the vertical shrinkage
the transverse shrinkage
and the volume shrinkage increased firstly and then fluctuated slowly. With the increase of initial dry density
the vertical expansion rate
the vertical shrinkage rate
and the volume expansion rate increased
while the transverse expansion rate
transverse shrinkage rate
and volume shrinkage rate decreased.
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