Abstract
Cohesive soil, as soil lumps within the sand matrix of the Gangetic alluvial plain, exerts a significant influence on the dynamic properties of sand deposits, as extensively documented in prior research. This study aimed to describe the intricacies of microstructural changes and re-distribution of pore sizes resulting from the effects of loading and wetting. To gain a comprehensive understanding, microstructural characterization of Indo-Gangetic alluvial soil was performed using two advanced analytical techniques, mercury intrusion porosimetry and scanning electron microscopy. The collapse behavior of Sone river sand samples mixed with varying proportions of soil lumps was studied using a series of oedometer test. A decrease in the collapse potential (CP) trend was observed with each increase in the sand percentage. The CPs were estimated as 16.39% and 10.07% for alluvial sand containing 70% and 40% collapsible lumps, respectively. The micrographs and differentiation in pore morphology were used to describe the microstructural evolution of lump-sand mixture due to saturation and loading. This study highlights the pivotal role played by the collapsible soil lumps within the sand matrix. Initially, these lumps possess an open structure, characterized by cementation bonds that interconnect clay-coated silts and sand aggregates. However, these cemented bonds are susceptible to disintegration under the influences of loading and wetting, ultimately triggering collapse in the soil matrix. After the collapse, soil particle re-arrangement occurs, and the initial open structure in soil lumps transforms into a dense structure. Microstructural change is dependent on stress levels. With increasing stress levels, higher inter-aggregate pores or macro-pores evolve into small sized intra-aggregate pores or micro-pores. This study contributes to the literature by providing both qualitative and quantitative insights into soil collapse and valuable guidelines for comprehending the intricate microstructural alterations that occur within alluvial sand containing these unique lumps.
Similar content being viewed by others
Data Availability
All data, models, or codes that support the findings of this study are available from the corresponding author upon request.
Code Availability
No code was generated or used during the study.
Abbreviations
- CL:
-
Low-plasticity clay
- CP:
-
Collapse potential
- d :
-
Entrance pore diameter
- \(d_{macro}\) :
-
Macro-pore diameter
- \(d_{micro}\) :
-
Micro-pore diameter
- \(e\) :
-
Void ratio
- \(e_0\) :
-
Initial void ratio
- \(e_{in}\) :
-
Cumulative intrusion void ratio
- \(e^L\) :
-
Inter aggregate void ratio
- \(e^s\) :
-
Intra aggregate void ratio
- EDS:
-
Energy dispersive spectroscopy
- \(H\) :
-
Initial height of the specimen
- IGP:
-
Indo-Gangetic plain
- MGP:
-
Middle Ganga plain
- MIP:
-
Mercury intrusion porosimetry
- \(m_v\) :
-
Coefficient of volume compressibility
- PSD:
-
Pore size distribution
- p :
-
Penetration pressure
- \(S\) :
-
Sand percentage in lump-sand mixture
- SEM:
-
Scanning electron microscopy
- SP:
-
Poorly graded sand
- SPT:
-
Standard penetration test
- \(t_{90}\) :
-
90% Consolidation time
- USCS:
-
Unified soil classification system
- \(\sigma_{Hg}\) :
-
Surface tension of mercury
- \(\Delta e_0\) :
-
Change in void ratio
- \(\Delta H\) :
-
Change in specimen height
- \(\theta_{nw}\) :
-
Contact angle between the pore wall and mercury
References
Bronick CJ, Lal R (2005) Soil structure and management: a review. Geoderma 124:3–22. https://doi.org/10.1016/j.geoderma.2004.03.005
Li P, Vanapalli S, Li T (2016) Review of collapse triggering mechanism of collapsible soils due to wetting. J Rock Mech Geotech Eng 8:256–274. https://doi.org/10.1016/j.jrmge.2015.12.002
Eberl DD (1984) Clay mineral formation and transformation in rocks and soils. Philos Trans R Soc London Ser A Math Phys Sci. https://doi.org/10.1098/rsta.1984.0026
Singer A (1980) The paleoclimatic interpretation of clay minerals in soils and weathering profiles. Earth-Science Rev 15:303–326. https://doi.org/10.1016/0012-8252(80)90113-0
Peterson CD, Grathoff GH, Reckendorf F et al (2014) Late Pleistocene coastal loess deposits of the central west coast of North America: terrestrial facies indicators for marine low-stand intervals. Aeolian Res 12:47–64. https://doi.org/10.1016/j.aeolia.2013.11.001
Das A, Chakrabortty P, Popescu R (2021) Assessment of lumped particles effect on dynamic behaviour of fine and medium grained sands. Bull Earthq Eng 19:745–766. https://doi.org/10.1007/s10518-020-01012-w
Derbyshire E, Mellors TW (1988) Geological and geotechnical characteristics of some loess and loessic soils from China and Britain: a comparison. Eng Geol 25:135–175. https://doi.org/10.1016/0013-7952(88)90024-5
Jiang M, Zhang F, Hu H et al (2014) Structural characterization of natural loess and remolded loess under triaxial tests. Eng Geol 181:249–260. https://doi.org/10.1016/j.enggeo.2014.07.021
Burton GJ, Pineda JA, Sheng D, Airey D (2015) Microstructural changes of an undisturbed, reconstituted and compacted high plasticity clay subjected to wetting and drying. Eng Geol 193:363–373. https://doi.org/10.1016/j.enggeo.2015.05.010
Li Y, Zhang T, Zhang Y, Xu Q (2018) Geometrical appearance and spatial arrangement of structural blocks of the Malan loess in NW China: implications for the formation of loess columns. J Asian Earth Sci 158:18–28. https://doi.org/10.1016/j.jseaes.2018.02.007
Romero E, Simms PH (2008) Microstructure investigation in unsaturated soils: A review with special attention to contribution of mercury intrusion porosimetry and environmental scanning electron microscopy. Geotech Geol Eng 26:705–727. https://doi.org/10.1007/s10706-008-9204-5
Wang JD, Li P, Ma Y et al (2020) Change in pore-size distribution of collapsible loess due to loading and inundating. Acta Geotech 15:1081–1094. https://doi.org/10.1007/s11440-019-00815-9
Pécsi M (1990) Loess is not just the accumulation of dust. Quat Int 7–8:1–21. https://doi.org/10.1016/1040-6182(90)90034-2
Garcia Giménez R, Vigil de la Villa R, González Martín JA (2012) Characterization of loess in central Spain: a microstructural study. Environ Earth Sci 65:2125–2137. https://doi.org/10.1007/S12665-011-1193-7
Chakrabortty P, Roshan AR, Das A (2020) Evaluation of dynamic properties of partially saturated sands using cyclic triaxial tests. Indian Geotech J 50:948–962. https://doi.org/10.1007/s40098-020-00433-3
Das A, Chakrabortty P (2022) Simple models for predicting cyclic behaviour of sand in quaternary alluvium. Arab J Geosci 15:1–19. https://doi.org/10.1007/S12517-022-09639-6
Nilay N, Chakrabortty P, Popescu R (2022) Liquefaction hazard mapping using various types of field test data. Indian Geotech J 52:280–300. https://doi.org/10.1007/S40098-021-00570-3
Das A, Chakrabortty P (2021) Artificial neural network and regression models for prediction of free-field ground vibration parameters induced from vibroflotation. Soil Dyn Earthq Eng 148:106823. https://doi.org/10.1016/j.soildyn.2021.106823
Beckett CTS, Hall MR, Augarde CE (2013) Macrostructural changes in compacted earthen construction materials under loading. Acta Geotech 8:423–438. https://doi.org/10.1007/s11440-012-0203-6
Saha D, Sahu S (2016) A decade of investigations on groundwater arsenic contamination in Middle Ganga Plain, India. Environ Geochem Health 38:315–337. https://doi.org/10.1007/s10653-015-9730-z
Singh RK, Kar SK, Prasad S (2008) Alluvial soil collapse at Karanda village, Ghazipur district, Uttar Pradesh: a natural hazard of great societal importance. J Eng Geol 32:1–4
Arora S, Singh BP (2020) Status of soil degradation in state of Uttar Pradesh. J Soil Water Conserv 19:119. https://doi.org/10.5958/2455-7145.2020.00016.8
Kushwaha S, Sinha DK, Ahmad N (2020) Dynamics of land degradation in Uttar Pradesh: Zone-wise analysis. Indian J Econ Dev. 16:221–228. https://doi.org/10.35716/ijed/20087
Das A, Chakrabortty P (2021) Large strain dynamic characteristics of quaternary alluvium sand with emphasis on empirical pore water pressure generation model. Eur J Environ Civ Eng 26:5729–5752. https://doi.org/10.1080/19648189.2021.1916605
ASTM D6913/D6913M-17 (2017) Standard test methods for particle-size distribution (gradation) of soils using sieve analysis. ASTM International, West Conshohocken, PA, United States
Indian Standard (1980) IS: 2720 Methods of test for soils, Part 3: Sec-2 Determination of specific gravity. BIS, New Delhi, India
Indian Standard (1983) IS: 2720 Methods of test for soils, Part 14: Determination of density index (relative density) of cohesionless soils. BIS, New Delhi, India
Indian Standard (1985) IS: 2720 Methods of test for soils, Part 4: Grain size analysis. Bur Indian Stand New Delhi, India 1–38
ASTM D6836-16 (2016) Standard test methods for determination of the soil water characteristic curve for desorption using hanging column, pressure extractor, chilled mirror hygrometer, or centrifuge, ASTM International, West Conshohocken, PA, US
Indian Standard (1986) IS: 2720 Methods of test for soils, Part 15: Determination of consolidation properties. BIS, New Delhi, India.
ASTM D4404-10 (2010) Standard test method for determination of pore volume and pore volume distribution of soil and rock by mercury intrusion porosimetry. ASTM International, West Conshohocken, US
Jennings JE, Knight K (1957) The prediction of total heave from the double oedometer test. Trans South Afr Inst Civ Eng 7(9):285–291
Washburm EW (1921) Note on method of determining the distribution of pore size in porous materials. Proc Natl Acad Sci 7:115–116. https://doi.org/10.1073/pnas.7.4.115
Diamond S (1970) Pore size distributions in clays. Clays Clay Miner 18:7–23. https://doi.org/10.1346/ccmn.1970.0180103
Delage P, Audiguier M, Cui YJ, Howat MD (1996) Microstructure of a compacted silt. Can Geotech J 33:150–158. https://doi.org/10.1139/t96-030
Delage P, Lefebvre G (1984) Study of the structure of a sensitive champlain clay and of its evolution during consolidation. Can Geotech J 21:21–35. https://doi.org/10.1139/t84-003
Oualmakran M, Mercatoris BCN, François B (2016) Pore-size distribution of a compacted silty soil after compaction, saturation, and loading. Can Geotech J 53:1902–1909. https://doi.org/10.1139/cgj-2016-0184
Liu Z, Liu F, Ma F et al (2015) Collapsibility, composition, and microstructure of loess in China. Can Geotech J 53:673–686. https://doi.org/10.1139/cgj-2015-0285
Rogers CDF (1995) Types and distribution of collapsible soils. Genes Prop Collapsible Soils Proc Work Loughborough 1994:1–17. https://doi.org/10.1007/978-94-011-0097-7_1
Derbyshire E, Meng X, Wang J et al (1995) Collapsible loess on the Loess Plateau of China. Genes Prop Collapsible Soils Proc Work Loughborough 1994(468):267–293. https://doi.org/10.1007/978-94-011-0097-7_14
Monroy R, Zdravkovic L, Ridley A (2010) Evolution of microstructure in compacted London Clay during wetting and loading. Géotechnique 60:105–119. https://doi.org/10.1680/geot.8.P.125
Muñoz-Castelblanco JA, Pereira JM, Delage P, Cui YJ (2012) The water retention properties of a natural unsaturated loess from northern France. Géotechnique 62:95–106. https://doi.org/10.1680/geot.9.P.084
Wen BP, Yan YJ (2014) Influence of structure on shear characteristics of the unsaturated loess in Lanzhou, China. Eng Geol 168:46–58. https://doi.org/10.1016/j.enggeo.2013.10.023
Romero E, Della Vecchia G, Jommi C (2011) An insight into the water retention properties of compacted clayey soils. Géotechnique 61:313–328. https://doi.org/10.1680/geot.2011.61.4.313
Thom R, Sivakumar R, Sivakumar V et al (2007) Pore size distribution of unsaturated compacted kaolin: the initial states and final states following saturation. Géotechnique 57:469–474. https://doi.org/10.1680/geot.2007.57.5.469
Lloret A, Villar MV, Sànchez M et al (2003) Mechanical behaviour of heavily compacted bentonite under high suction changes. Géotechnique 53:27–40. https://doi.org/10.1680/geot.2003.53.1.27
Ye WM, Cui YJ, Qian LX, Chen B (2009) An experimental study of the water transfer through confined compacted GMZ bentonite. Eng Geol 108:169–176. https://doi.org/10.1016/j.enggeo.2009.08.003
Jefferson IF, Evstatiev D, Karastanev D et al (2003) Engineering geology of loess and loess-like deposits: a commentary on the Russian literature. Eng Geol 68:333–351. https://doi.org/10.1016/S0013-7952(02)00236-3
Paul A, Chakrabortty P (2021) Assessment of collapse potential of lumped soil in alluvial deposit by double consolidation tests. In: Çiner A et al (eds) Recent research on geotechnical engineering, remote sensing, geophysics and earthquake seismology. MedGU 2021. Advances in science, technology & innovation. Springer Nature Switzerland, Cham, pp 39–42. https://doi.org/10.1007/978-3-031-43218-7_10
Li P, Xie W, Pak RYS, Vanapalli SK (2019) Microstructural evolution of loess soils from the Loess Plateau of China. CATENA 173:276–288. https://doi.org/10.1016/j.catena.2018.10.006
Funding
The authors acknowledge the Department of Higher Education (Govt. of India) for providing the funding for the present research work to carry out the doctoral research study for which no specific grant number is allotted. The authors also acknowledge the Department of Atomic Energy, Board of Research in Nuclear Sciences for providing funding (No: 51/14/04/2022-BRNS) for doing research in this area. The authors also express gratitude to the Editor-in-chief, Editors, and anonymous reviewers for their suggestions.
Author information
Authors and Affiliations
Contributions
Dr. Pradipta Chakrabortty contributed to the study's conception and design. Sample preparation, data collection and analysis were performed by Mr. Abhik Paul. The first draft of the manuscript was written by Mr. Abhik Paul and all authors commented on modified versions of the manuscript. All authors read and approved the final manuscript.
Corresponding author
Ethics declarations
Conflict of interest
The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper.
Rights and permissions
Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law.
About this article
Cite this article
Paul, A., Chakrabortty, P. Microstructural Characterization of Alluvial Sand Containing Cohesive Soil Lumps During Loading and Inundating. Int J Civ Eng (2024). https://doi.org/10.1007/s40999-024-00974-1
Received:
Revised:
Accepted:
Published:
DOI: https://doi.org/10.1007/s40999-024-00974-1