• ISSN 0258-2724
  • CN 51-1277/U
  • EI Compendex
  • Scopus
  • Indexed by Core Journals of China, Chinese S&T Journal Citation Reports
  • Chinese S&T Journal Citation Reports
  • Chinese Science Citation Database
Volume 30 Issue 4
Jul.  2017
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Article Contents
ZENG Qiang, XU Zemin, ZHANG Youwei, ZHANG Huining, MEI Xuefeng, REN Zhe. Research on Macropores Flow in Unsaturated Zone Soil of Slopes under Different Vegetation Community[J]. Journal of Southwest Jiaotong University, 2017, 30(4): 694-704. doi: 10.3969/j.issn.0258-2724.2017.04.007
Citation: ZENG Qiang, XU Zemin, ZHANG Youwei, ZHANG Huining, MEI Xuefeng, REN Zhe. Research on Macropores Flow in Unsaturated Zone Soil of Slopes under Different Vegetation Community[J]. Journal of Southwest Jiaotong University, 2017, 30(4): 694-704. doi: 10.3969/j.issn.0258-2724.2017.04.007

Research on Macropores Flow in Unsaturated Zone Soil of Slopes under Different Vegetation Community

doi: 10.3969/j.issn.0258-2724.2017.04.007
  • Received Date: 14 Jun 2015
  • Publish Date: 25 Aug 2017
  • To evaluate Macropores Flow in unsaturated zone Soil of natural Slopes under rainfall conditions, A dyeing tracing test with methylene blue was carried out based on retaining the original state of the slopes and simulating rainfall process. Combined with water breakthrough method and high-precision dyeing profile image, based on image processing, differential and regression analysis, distribution and influence factors of macropore flow in high coverage(90%) slope during the rainfall process were studied. The results show that: comparing with herbaceous vegetation community soil, the distribution range(dyeing coverage is at 46.18%-63.55%) of macropores flow in the profile of woody vegetation community soil is larger, the continuous degree is lower, the differentiation degree(dyeing route number is at 203-8 599) is higher, the staining patterns are more complex. Macropores flow patterns of 2D can reflect that of 3D. In the rainfall distribution process, competing with the interception effect of macropore in soils, slope orientation effect is tend to infiltrate vertically along the slopes(max dyeing coverage are at 63.55% and 59.67%). Roots size is not the only factor to control macropores scale(the mean pore sizes are at 1.23-2.03 mm and 1.34-2.23 mm). Aggregate particles themselves can also have root channels.

     

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  • 徐则民. 植被与斜坡非饱和带大空隙[J]. 地学前缘,2007,14(6): 134-142. XU Zemin. Vegetation and macropores in vadose zones of hill slopes[J]. Earth Science Frontiers, 2007, 14(6): 134-142.
    ALAOUI A, HELBLING A. Evaluation of soil compaction vsing hydro-dynamic water content variation:comparison between compacted and noncompacted soil[J]. Geoderma, 2006, 134: 97-108.
    LIN H S, MCINNES K J, WILDING L P, et al. Effective porosity and flow rate with infiltration at low tensions into a well-structured subsoil[J]. American Society of Agricultural Engineers, 1996, 39: 131-135.
    TSUKAMOTO Y, OHTA T, NOGUCHI H. Hydrological and geomorphological studies of debris slides on forested hillslopes in Japan[C]//Recent developments in the explanation and prediction of erosion and sediment yield. Rennes:Internation Association of Hydrological Sciences Publication, 1982: 89-98.
    FAN P, LIU Q Q, LI J C, et al. Numerical analysis of rainfall infiltration in the slope with a fracture[J]. Science in China: Series E: Engineering and Materials Science, 2005, 48(Sup.1): 107-120.
    GATTINONI P, FRANCANI V. A tool for modeling slope instability triggered by piping[J]. World Academy of Science, Engineering and Technology, 2009, 56: 471-478.
    CAPOWIZE Y, PIERRET A, DANIEL O, et al. 3D skeleton reconstructions of natural earthworm burrow systems using CAT scan images of soil cores[J]. Biol Fertil Soils, 1998, 27(1): 51-59.
    PIERRET A, CAPOWIZE Y, BELZUNCES L, et al. 3D reconstruction and quantification of macropores using X-ray computed tomography and image analysis[J]. Geoderma, 2002, 106(3): 247-271.
    冯杰,郝振纯. CT扫描确定土壤大孔隙分布[J]. 水科学进展,2002,13(5): 611-617. FENG Jie, HAO Zhenchun. Distribution of soil macropores characterized by CT[J]. Advances in Water Science, 2002, 13(5): 611-617.
    朱宝龙,巫锡勇,李晓宁,等. 合肥地区重塑黏性土细观结构演化三轴CT试验[J]. 西南交通大学学报,2015,50(1): 144-149. ZHU Baolong, WU Xiyong, LI Xiaoning, et al. Triaxial CT tests of meso-structure evolution of remodeled cohesive soil in Hefei[J]. Journal of Southwest Jiaotong University, 2015, 50(1): 144-149.
    HILLEL D. Intriduction to soil physics[M]. London: Academic Press, 1982: 92-100.
    MOSLEY M P. Streamflow generation in a forested watershed, New Zealand[J]. Water Resource Research, 1979, 15(4): 795-806.
    HOLDEN J.Flow through macropores of different size classes in Blanket Peat[J]. Journal of Hydrology, 2008, 364(3): 342-348.
    BEVEN K,GERMANN P. Macropores and water flow in soils[J]. Water Resources Research, 1982, 18(5): 1311-1325.
    PASSIOURA J B. Soil conditions and plant growth[J]. Plant, Cell and Environment, 2002, 25(2): 311-318.
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