Rock and Soil Mechanics ›› 2020, Vol. 41 ›› Issue (1): 1-10.doi: 10.16285/j.rsm.2019.6852

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Experimental study on seepage erosion induced by pipeline damage under full pipe flow condition

LIU Cheng-yu1, 2, CHEN Bo-wen1, LUO Hong-lin1, RUAN Jia-chun1   

  1. 1. College of Environment and Resources, Fuzhou University, Fuzhou 350116, China

    2. Fujian Provincial Universities Engineering Research Center of Geological Engineering, Fuzhou 350116, China

  • Online:2020-09-18 Published:2020-09-18
  • About author:born in 1970, PhD, Professor, doctoral supervisor, mainly engaged in the research of engineering geology, tunnel and underground engineering.
  • Supported by:
     the National Natural Science Foundation of China (41272300)

Abstract:

Aiming at the problems of ground settlement induced by the underground pipeline damage in water-rich sand layer, a set of visualization experimental device was designed. For these cases of 11 kinds of sand samples with particle size of soil d90=1.45~8.45mm and 5 kinds of full pipe flow velocity, the behavior of ground settlement induced by seepage erosion was studied. Research showed that:(1)There are three modes of seepage erosion induced by pipeline damage: only water inrush without settlement, soil arching formation with settlement, and sand crushing with settlement;(2)The particle size of soil , damaged mouth size and thick-span ratio are the main factors determining the seepage erosion mode of soil;(3)When the soil arching or sand crushing is formed in the soil above the damaged mouth of pipeline, the relationship between the particle size of soil d90 and the thick-span ratio r is that: when 8.0≥r≥4.2, the d90 decreases parabolically with the increase of r; when 12.5≥r≥8.0, d90 remains unchanged;(4)When the soil arching or sand crushing is formed in the soil above the damaged mouth of pipeline, the initial settlement radius and settlement depth with the flow velocity of 0 are determined by the ratio (D/d50) of the damaged mouth diameter D and the average particle size of soil d50 ; the settlement radius and depth increase linearly with the increase of full pipe flow velocity; when the soil arching is formed, the expansion velocity (VLVH) of settlement radius and settlement depth with the increase of flow velocity is logarithmic to D/d50; When the sand crushing is formed, the expansion velocity VL of settlement radius with the increase of flow velocity is that, when 23.0≥D/d50≥6.0, it increases linearly with the increase of D/d50; when 42.0≥D/d50≥23.0, it decreases logarithmically with the increase of D/d50.

Key words: seepage erosion, settlement, thick-span ratio, flow velocity; particle size