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Investigation of the collapse potential of Malan loess from different regions on the Loess Plateau in terms of pore size distribution and clay distribution form

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Abstract

Loess microstructure and collapsibility show regional differences on the Loess Plateau. Characterization and comparison of loess microstructure and its evolution during collapse in different loess regions help to better interpret the intrinsic mechanism of loess collapse, while related research is still limited. In this study, the microstructures of loess from Lanzhou (LZ), Qingyang (QY), Hengshan (HS) and Jingyang (JY) were characterized, and pores changes in response to loading and wetting were quantitatively analyzed using micro-computed tomography (μ-CT) scanning and mercury intrusion porosimetry (MIP). The results indicate that inter-particle (aggregate) pores with a size ranging from tens of microns to a few microns are favorable for collapse deformation at a low pressure, the small pores of a few microns provide space for collapse under high pressures. The pore size distribution and clay distribution form within loess considerably influence its collapse potential. Loess with skeleton particles connected by clay bridges, forming concentrated inter-particle pores (i.e., LZ loess), are more likely to collapse at a low pressure. Loess with more clays distributed among particles or as buttresses (i.e., JY loess) usually shows great collapse potential at a high pressure, with the precondition of enough small pores for compaction. The limited pore space in loess (i.e., QY loess with a relatively low void ratio) constrains the collapse potential with pressure. Clay coatings adhering to skeleton particles predominant in loess (i.e., HS loess) have little influence on inducing particle movement and collapse deformation.

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References

  1. Assallay AM, Rogers CDF, Smalley IJ (1997) Formation and collapse of metastable particle packings and open structures in loess deposits. Eng Geol 48(1–2):101–115

    Article  Google Scholar 

  2. Barden L, Mcgown A, Collins K (1973) The collapse mechanism in partly saturated soil. Eng Geol 7(1):49–60

    Article  Google Scholar 

  3. Deng LS, Fan W, Chang YP, Yu B, Wei YN, Wei TT (2021) Microstructure quantification, characterization, and regional variation in the Ma Lan Loess on the Loess Plateau in China. Int J Geomech 21(8):04021143

    Article  Google Scholar 

  4. Deng LS, Fan W, Liu SP, Chang YP, Dai Y, Li YB (2020) Quantitative research and characterization of the loess microstructure in the Bailu Tableland, Shaanxi Province, China. Adv Civ Eng 2020:3681382

    Google Scholar 

  5. Derbyshire E, Mellors TW (1988) Geological and geotechnical characteristics of some loess and loessic soils from China and Britain: a comparison. Eng Geol 25(2–4):135–175

    Article  Google Scholar 

  6. Fan W, Deng LS, Yu B, Wei YN, Wei TT, Yu NY, Yuan WN (2022) Three-dimensional microstructure of loess. Science Press, Beijing (In Chinese)

    Google Scholar 

  7. Gao GR (1981) Classification of microstructures of loess in China and their collapsibility. Sci Sinica 7:962–970

    Google Scholar 

  8. Gao GR (1988) Formation and development of the structure of collapsing loess in China. Eng Geol 25:235–245

    Article  Google Scholar 

  9. Ge MM, Pineda JA, Sheng DC, Burton GJ, Li N (2021) Microstructural effects on the wetting-induced collapse in compacted loess. Comput Geotech 138:104359

    Article  Google Scholar 

  10. Gibbs HJ, Holland WY (1960) Petrographic and engineering properties of loess. Technical Information Branch, Denver Federal Center

  11. Lei XY (1985) Characteristics of loess pore distribution in North Shaanxi and East Gansu. Chin Sci Bull 30(5):656–661

    Google Scholar 

  12. Lei XY (1989) The relationship between microtexture types and indices of physicomechanical properties of loess in China. Acta Geol Sin 2(4):433–443

    Article  Google Scholar 

  13. Li P, Pan ZH, Xiao T, Wang JD (2022) Effects of modeling water content and compaction degree on the microstructure and permeability of compacted loess. Acta Geotech. https://doi.org/10.1007/s11440-022-01592-8

    Article  Google Scholar 

  14. Li P, Vanapalli S, Li TL (2016) Review of collapse triggering mechanism of collapsible soils due to wetting. J Rock Mech Geotech Eng 8(2):256–274

    Article  Google Scholar 

  15. Li P, Xie WL, Pak RS, Vanapalli S (2019) Microstructural evolution of loess soils from the Loess Plateau of China. CATENA 173:276–288

    Article  Google Scholar 

  16. Li TL, Zhang H, Li P, Kang HW, Ge SL (2020) Mode analysis of pore distribution and soil-water characteristic curve of Malan loess under different depositional environments. Hydrogeol Eng Geol 47(3):107–114 ((in Chinese))

    Google Scholar 

  17. Li XA, Li LC (2017) Quantification of the pore structures of Malan loess and the effects on loess permeability and environmental significance, Shaanxi Province, China: an experimental study. Environ Earth Sci 76:523

    Article  Google Scholar 

  18. Li XA, Li LC, Song YX, Hong B, Wang L, Sun JQ (2019) Characterization of the mechanisms underlying loess collapsibility for land creation project in Shaanxi Province, China—A study from a micro perspective. Eng Geol 249:77–88

    Article  Google Scholar 

  19. Liu DS (1965) Chinese Loess deposits. Science Press, Beijing (In Chinese)

    Google Scholar 

  20. Liu DS, An ZS, Yuan BY (1985) Eolian process and dust mantle(loess) in China. Quat Sci 6(1):113–125 ((in Chinese))

    Google Scholar 

  21. Liu Z, Liu FY, Ma FL, Wang M, Bai XH, Zheng YL, Yin H, Zhang GP (2016) Collapsibility, composition, and microstructure of loess in China. Can Geotech J 53(4):673–686

    Article  Google Scholar 

  22. Mellors TW (1995) The influence of the clay component in loess on collapse of the soil structure. In: Derbyshire E, Dijkstra T, Smalley IJ (eds) Genesis and properties of collapsible soils. Springer, Dordrecht, pp 207–216

    Chapter  Google Scholar 

  23. MWRPRC (1999) Specification of Soil Test, SL 237–1999. Ministry of Water Resources of the People’s Republic of China, China Water Resources and Hydropower Press, Beijing (In Chinese)

    Google Scholar 

  24. Ng CWW, Sadeghi H, Hossen SKB, Chiu CF, Alonso EE, Baghbanrezvan S (2016) Water retention and volumetric characteristics of intact and re-compacted loess. Can Geotech J 53(8):1258–1269

    Article  Google Scholar 

  25. Osipov VI, Sokolov VN (1995) Factors and mechanism of loess collapsibility. In: Derbyshire E, Dijkstra T, Smalley IJ (eds) Genesis and properties of collapsible soils. Springer, Dordrecht, pp 49–63

    Chapter  Google Scholar 

  26. Peng JB, Duan Z (2018) Landslides in the words of little loess-grain. Chin J Nat 40(4):285–289 ((in Chinese))

    Google Scholar 

  27. Rogers CDF (1995) Types and distribution of collapsible soils. In: Derbyshire E, Dijkstra T, Smalley IJ (eds) Genesis and Properties of Collapsible Soils. Springer, Dordrecht, pp 1–17

    Google Scholar 

  28. Shao XX, Zhang HY, Tan Y (2018) Collapse behavior and microstructural alteration of remolded loess under graded wetting tests. Eng Geol 233:11–22

    Article  Google Scholar 

  29. Smalley I, O’Hara-Dhand K, Kwong J (2014) China: Materials for a loess landscape. CATENA 117:100–107

    Article  Google Scholar 

  30. Sun JZ (2005) Loessology (Volume I). Hong Kong Archaeological Society, Hong Kong (In Chinese)

    Google Scholar 

  31. Wang HK, Qian H, Gao YY, Li YB (2020) Classification and physical characteristics of bound water in loess and its main clay minerals. Eng Geol 265:105394

    Article  Google Scholar 

  32. Wang JD, Li P, Ma Y, Vanapalli S, Wang XG (2020) Change in pore-size distribution of collapsible loess due to loading and inundating. Acta Geotech 15:1081–1094

    Article  Google Scholar 

  33. Wang JD, Zhang DF, Zhang YS, Chen H, Ma WQ (2022) Variations in hydraulic properties of collapsible loess exposed to wetting and shearing. Acta Geotech 17:2995–3015

    Article  Google Scholar 

  34. Wang M (2010) Study on structure of collapsible loess in China. Doctoral dissertation of Taiyuan University of Technology, Taiyuan (In Chinese)

  35. Wei TT, Fan W, Yu NY, Wei YN (2019) Three-dimensional microstructure characterization of loess based on a serial sectioning technique. Eng Geol 261:105265

    Article  Google Scholar 

  36. Wei TT, Fan W, Yuan WN, Wei YN, Yu B (2019) Three-dimensional pore network characterization of loess and paleosol stratigraphy from South Jingyang Plateau, China. Environ Earth Sci 78:333

    Article  Google Scholar 

  37. Wei YN, Fan W, Fu CB, Yu B (2023) Experimental investigation of the hydration swelling effect of clay minerals on loess collapsibility. Int J Geomech 23(1):06022036

    Article  Google Scholar 

  38. Wei YN, Fan W, Ma GL (2022) Characteristics of microstructure and collapsible mechanism of Malan loess in Loess Plateau, China. J Earth Sci Environ 44(4):581–592 (In Chinese)

    Google Scholar 

  39. Wei YN, Fan W, Yu B, Deng LS, Wei TT (2020) Characterization and evolution of three-dimensional microstructure of Malan loess. CATENA 192:104585

    Article  Google Scholar 

  40. Wei YN, Fan W, Yu NY, Deng LS, Wei TT (2020) Permeability of loess from the South Jingyang Plateau under different consolidation pressures in terms of the three-dimensional microstructure. Bull Eng Geol Environ 79(9):4841–4857

    Article  Google Scholar 

  41. Xie WL, Li P, Zhang MS, Cheng TE, Wang Y (2018) Collapse behavior and microstructural evolution of loess soils from the Loess Plateau of China. J Mt Sci 15(8):1642–1657

    Article  Google Scholar 

  42. Xu PP, Zhang QY, Qian H, Qu WG, Li MN (2021) Microstructure and permeability evolution of remolded loess with different dry densities under saturated seepage. Eng Geol 282:105875

    Article  Google Scholar 

  43. Yang H, Xie WL, Liu QQ, Zhu RS, Liu YY (2022) Three-stage collapsibility evolution of Malan loess in the Loess Plateau. CATENA 217:106482

    Article  Google Scholar 

  44. Yu B, Fan W, Dijkstra TA, Wei YN, Deng LS (2021) Heterogeneous evolution of pore structure during loess collapse: insights from X-ray micro-computed tomography. CATENA 201:105206

    Article  Google Scholar 

  45. Yu B, Fan W, Dijkstra TA, Wei YN, Deng LS (2022) Pore structure evolution due to loess collapse: a comparative study using MIP and X-ray micro-CT. Geoderma 424:115955

    Article  Google Scholar 

  46. Yu B, Fan W, Fan JH, Dijkstra TA (2020) X-ray micro-computed tomography (μ-CT) for 3D characterization of particle kinematics representing water-induced loess micro-fabric collapse. Eng Geol 279:105895

    Article  Google Scholar 

  47. Yuan WN, Fan W (2022) Quantitative study on the microstructure of loess soils at micrometer scale via X-ray computed tomography. Powder Technol 408:117712

    Article  Google Scholar 

  48. Zhang DF, Wang JD, Chen CL, Wang SH (2020) The compaction and collapse behavior of intact loess in suction-monitored triaxial apparatus. Acta Geotech 15:529–548

    Article  Google Scholar 

  49. Zhang WP, Sun YF, Chen WW, Song YP, Zhang JK (2019) Collapsibility, composition, and microfabric of the coastal zone loess around the Bohai Sea. China Eng Geol 257:105142

    Article  Google Scholar 

Download references

Acknowledgements

The authors sincerely acknowledge the financial support from the National Natural Science Foundation of China (Grant Nos. 42002285, 42220104005 and 42072286) and the National Key R&D Program of China (Grant No. 2022 YFC3003400).

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Correspondence to Wen Fan.

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Wei, Yn., Fan, W., Yu, B. et al. Investigation of the collapse potential of Malan loess from different regions on the Loess Plateau in terms of pore size distribution and clay distribution form. Acta Geotech. 18, 6595–6613 (2023). https://doi.org/10.1007/s11440-023-02084-z

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