Geotechnical Behaviour of Bauxite Residue (Red Mud): A Review of Global Parameter Variability and Chemical–Mechanical Interactions

Abstract

Bauxite residue (red mud) is a highly alkaline byproduct of the alumina refining process generated in large volumes worldwide. Most alumina operations currently rely on long-term storage facilities due to the high costs and technical constraints of residue reuse technologies. Therefore, understanding the mechanical behaviour of bauxite residue is critical to minimising environmental contamination risks, preventing structural failures, and ensuring the long-term stability of storage facilities. However, obtaining reliable geotechnical parameters is challenging due to the residue’s complex composition and chemical characteristics, particularly given the current fragmented state of the literature. This review compiles an extensive database of bauxite residue parameters across alumina operations worldwide, synthesising existing knowledge and research needs. The database encompasses 940 data points extracted from 63 studies across 25 countries. The findings reveal considerable variability in parameter values across countries, potentially exacerbated by inconsistencies in experimental methodologies. Few studies have integrated geochemical conditions, such as pH and salinity, with geomechanical behaviour, thereby limiting understanding of the mechanisms that govern key parameters, including strength and deformability. Enhancing the predictability of bauxite residue behaviour requires the development of standardised experimental protocols that explicitly account for the coupled effects of chemistry and mechanics to support reliable risk assessments of storage facilities.

1. Introduction

Bauxite residue, also known as red mud, is a fine-grained, highly alkaline waste generated during the alumina refining process. Over 90% of alumina production is utilised for aluminium manufacturing, with approximately 95% derived from the Bayer Process [1]. This refining process, schematically depicted in Figure 1, involves adding caustic soda (NaOH) to the orebody under high-temperature, high-pressure conditions, leading to the formation of bauxite residue—a waste characterised by extreme pH and salinity.

As the global demand for aluminium continues to increase and requires higher alumina production, as illustrated in Figure 2, mining operations are extending into lower-grade ore bodies, resulting in larger annual waste volumes. It is estimated that the Bayer process generates between 0.3 and 2.5 tonnes of red mud per tonne of alumina refined [1,2,3,4,5].

Extensive research has been conducted on strategies to neutralise or reuse bauxite residue to mitigate the environmental risks associated with its management, including the use of the residue as an additive or aggregate for producing construction material [5,6,7,8,9,10,11,12,13,14,15] or road base material [16,17], recovery of rare and valuable metals [2,18,19,20], and the neutralisation of the residue [21,22,23,24,25,26,27,28,29,30]. Despite this, long-term storage facilities remain the standard practice for bauxite residue deposition and management [31], due to the considerable volume of residue produced each year and the high costs associated with refining processes, making the large-scale implementation of reuse technologies economically infeasible.

Additionally, bauxite residue deposits pose environmental risks associated with dust release, and soil and groundwater contamination. Several incidents have been documented in recent years, including the catastrophic failures at the Ajka Alumina Plant in Hungary in 2010 [32,33], at the Xiangjiang Wanji Aluminium Plant in China in August 2016 and at the HINDALCO Plant in India in 2019 [34,35]. Most recently, in September 2024, another failure was reported at a storage facility in Lajigarh, India [36]. Such failures typically result in the uncontrolled release of hazardous bauxite residue into surrounding areas, leading to severe environmental repercussions owing to the material’s alkalinity and raising concerns about the existing uncertainty in the design of these facilities. Therefore, maintaining the physical stability of bauxite residue storage facilities is essential to ensuring sustainable aluminium production and preventing environmental catastrophes.

However, despite decades of research, the geotechnical parameters reported for bauxite residue remain highly variable and often inconsistent. The variability arises from a range of causes, including differences in ore composition, refining process conditions, and inherent characteristics of the material, such as structural and cementation effects, and pore fluid chemistry [31,34,37,38,39,40,41]. Additionally, lack of standardised procedures for sample preparation and testing adds to the variability documented in this review. As a result, the existing state of research on red mud remains fragmented, and no standardised database allows systematic comparisons across refineries to enhance predictability in facility design.

Considering the recurrent failures of bauxite residue storage facilities and the complexity of this material’s behaviour, there is a clear need for an integrated assessment of the reported geotechnical properties of bauxite residue. This review addresses this gap by compiling a comprehensive database of published bauxite residue properties to facilitate cross-operation comparisons and evaluate current limitations in understanding red mud behaviour, particularly regarding chemical–mechanical interactions. The analysis consolidates existing knowledge on key geotechnical parameters, with particular emphasis on physical, chemical, and mineralogical characteristics and their influence on classification, strength and deformability. Furthermore, this work identifies knowledge gaps and proposes research directions to improve the operational safety and long-term stability of bauxite residue storage facilities.

2. Methodology and Database Framework

This review synthesises existing knowledge on bauxite residue geotechnical parameters and behaviour, and chemical composition. The aim was to compile a database of globally reported properties and to explore current limitations in understanding material behaviour that can lead to parameter variability, uncertainty and ultimately long-term environmental risk.

2.1. Review Methodology

A systematic literature search was conducted for peer-reviewed journal articles and academic theses published between 1974 and 2025. Primary searches were performed using Scopus and Google Scholar, using combinations of keywords such as (“bauxite residue” OR “red mud”) AND (“geotechnical properties” OR “mechanical behaviour” OR “shear strength”). Following the primary search, a “snowballing” technique was applied to capture relevant historical data not indexed in primary databases. Studies were included if they reported geotechnical laboratory or field data, specified the geographic source of the bauxite residue, and described sample preparation (e.g., drying methods and pore fluid). Conversely, studies were excluded if they focused exclusively on chemical processing or mineralogical characterisation without geotechnical testing. To address data quality, sources that failed to specify critical testing conditions (e.g., consolidation or drainage conditions in triaxial tests) were omitted to ensure the dataset’s reliability.

2.2. Database Summary

The review compiled a global dataset consisting of 940 data points from 25 countries.

Table 1. Geographic distribution and parameter matrix of the global bauxite residue database.

Region	Number of Studies	Geotechnical Parameters Available	Chemical Parameters Available	Total Data Points
Africa	1	Atterberg Limits	-	3
Asia	20	Atterberg Limits, Particle Size Distribution, Specific Gravity, Compressibility, Compaction	pH and XRF	233
Australia	11	Atterberg Limits, Particle Size Distribution, Specific Gravity, Compressibility, Compaction, Shear Strength	pH and XRF	93
Europe	11	Atterberg Limits, Particle Size Distribution, Specific Gravity, Compressibility, Compaction, Shear Strength	pH and XRF	123
North America	8	Atterberg Limits, Particle Size Distribution, Specific Gravity, Compressibility, Compaction, Shear Strength	pH and XRF	136
South America	12	Atterberg Limits, Particle Size Distribution, Specific Gravity, Compressibility, Compaction, Shear Strength	pH and XRF	352

provides a summary of the compiled database, categorising the data by geographic origin, the number of independent studies, and the specific geotechnical and chemical parameters available.

To preserve the conciseness of the review while ensuring maximum transparency and reproducibility, a breakdown of the dataset is provided in the Supplementary Materials. The Supplementary Materials detail every study considered, including the geographic origin of the residue and the ranges of all evaluated geotechnical and chemical parameters. Furthermore, it encompasses descriptions of sampling protocols, material characteristics (e.g., storage deposit type, sampling method, and whether the residue was filtered or otherwise treated), and the specific laboratory sample preparation procedures utilised across the different testing programs.

3. Bauxite Residue Composition, Alkalinity and Morphology

Most observations on the geotechnical behaviour of bauxite residue have been correlated with the material’s mineralogical and chemical characteristics. This subsection establishes the features of bauxite residue composition, regional characteristics, and external factors that may affect these properties.

3.1. Mineralogy and Alkalinity

The bauxite residue mineralogy reflects the mineral composition of the ore (bauxite) and modifications induced by the refining process. Bauxites are classified as fine-grained residual soil derived from the weathering of felspathoids, igneous, volcanic, and metamorphic rocks through a process known as “bauxitization”. Because alumina in bauxite can occur as a monohydrate (boehmite or diaspore) or a trihydrate (gibbsite), the conditions in the digestion tanks vary. Trihydrate, being more soluble, can be extracted at temperatures up to 150 °C with weaker caustic solutions, while monohydrate requires temperatures over 160 °C and stronger solutions [4,42]. Aside from the predominant alumina trihydrate and monohydrate minerals (i.e., gibbsite, boehmite, and diaspore), other residual minerals can be found in bauxite, such as kaolinite—the dominant siliceous mineral in the matrix, especially in older bauxites [43]—halloysite, goethite, hematite, magnetite, anatase, and quartz.

When bauxite ore undergoes the Bayer process, new mineral phases form [44]. The mineral composition of the residue can include hematite, goethite, gibbsite, silica, quartz, titanium dioxide, boehmite, anatase, rutile, calcite, and desilication products (DSP). Other compounds, such as muscovite, perovskite, calcium aluminate, and magnetite, can also be found [8,34,40,45,46,47].

Published results of elemental composition, presented in

Table 2. The most abundant elements present in bauxite residue and their reported concentration ranges based on elemental composition test results.

Oxides	Concentration (%) 1
Hematite (Fe2O3)	4.9–71.9
Aluminium oxide (Al2O3)	2.12–33
Quartz (SiO2)	0.6–36.3
Rutile (TiO2)	0.8–22.6
Calcium oxide (CaO)	0.11–47.2
Sodium oxide (Na2O)	0.1–16

¹ [12,15,21,45,46,47,48,49,50,51,52,53,54,55,56,57,58,59,60,61].

, indicate the most abundant elements in BR to be iron oxide or hematite (Fe₂O₃), aluminium oxide or alumina (Al₂O₃), silicon dioxide or quartz (SiO₂), titanium dioxide or rutile (TiO₂), calcium oxide or quicklime (CaO) and sodium oxide (Na₂O).

Desilication products are formed during the pre-desilication and desilication phases of the Bayer process, which convert reactive silica species into insoluble sodium aluminosilicates to prevent contamination of the pregnant liquor [25,45,62,63].

The most common DSPs are sodalite (Na₈(Al₆Si₆O₂₄)X₂, X is OH⁻, Cl⁻, ${\mathrm{C}\mathrm{O}}_3^{2-}$, or ${\mathrm{S}\mathrm{O}}_4^{2-}$) and cancrinite (Na₆Al₆Si₆O₂₄⋅2CaCO₃). Because of the Bayer process conditions, they exhibit a zeolite-type structure. These zeolite structures can have properties similar to those of clay minerals, including high ion-exchange and adsorption capacities [64,65,66]. Bayer’s sodalite (Figure 3) structure resembles a honeycomb or cage, with relatively large cavities that can accommodate loosely bound water molecules and exchangeable ions. Cancrinite has a similar formation, exhibiting channels in addition to structural cages [67]. The presence of DSPs, particularly sodalite, is inherently linked to the high salinity of the residue, as sodium is incorporated within the sodalite “cages”, releasing sodium ions (Na⁺) into the pore fluid when dissolved [45,47,68].

Pre-desilication and digestion also contribute to the formation of alkaline substances in bauxite residue. Approximately one-quarter of the alkalis present in BR is in soluble form, while the remainder exists as structural alkaline minerals such as sodalite and cancrinite, as well as calcite (CaCO₃), sodium hydroxide (NaOH), sodium carbonates (Na₂CO₃), sodium aluminates (NaAl(OH)₄), and sodium silicates (Na₂SiO₃), among others [21,25,29].

It is important to note, however, that the chemical composition of bauxite residue is not stable, as the material’s physicochemical properties can change in response to external conditions [69]. Over time, both the alkaline agents and mineral structures evolve: while fresh bauxite residue contains abundant free hydroxides, aluminates, and carbonates, the alkalinity of weathered red mud becomes largely governed by carbonates, as hydroxides and aluminates precipitate over time [25]. Aged samples may also exhibit changes in the concentrations of other essential oxides, in microstructure, aggregate stability, and in pH over time. These processes result from the transformation of soluble forms (such as sodium and calcium), leaching of dissolved solids due to weathering, and an increase in mineral crystallisation over time [58,68,70,71,72].

3.2. Morphology

Bauxite residue is described to exhibit scattered fine particles, containing grains with sharp edges, slightly rounded forms, and spongelike porous surfaces [34,69,73] with notable angularity, especially in the coarse fraction [6]. The residue matrix is heterogeneous, comprising individual grains and particle aggregates that form a loose, porous structure. The formation of aggregates is commonly attributed to the presence of DSP sodalite, which can act as a cementing agent at alkaline conditions [5,40,50,74,75].

The microstructure of bauxite residue appears to be affected by time, as schematically illustrated in Figure 4. Freshly deposited red mud typically contains a higher proportion of amorphous minerals and has a more disordered microstructure. In comparison, samples collected from areas where the residue had been stored for over a decade showed increased crystallisation of some mineral phases, a decrease in the total dissolved solids, pH and sodium ion concentrations, an increase in calcium ion concentration, and the development of larger macroaggregates due to particle agglomeration [70,72].

4. A Global Database—Bauxite Residue Geotechnical Properties and Mechanical Behaviour

4.1. Characterisation

The characterisation of geomaterials, including index properties, influences the engineering team’s perception of the storage facility operation. Key properties, such as specific gravity (Gs), particle-size distribution (PSD), and plasticity (i.e., Atterberg Limits), are important for supporting advanced analyses, including in situ void ratio and critical state parameters, hydraulic regime, deposition plans, settlement analysis, and initial liquefaction assessment.

Bauxite residue is recognised for its high specific gravity (Gs), largely attributable to the iron mineral content [46,57], is primarily fine-grained, with a predominant silt fraction, and is characterised as a material with low plasticity [34,40,76,77].

While these classifications define the general properties of bauxite residue, a closer analysis of published data indicates substantial regional variability. For example, Figure 5, which consolidates the spectrum of PSDs documented in the literature from twenty-six distinct sources, reveals that the Bayer process can produce residues with gradings ranging from coarse sand to silty clay, with the silt content varying between 20% and 93%. Similarly, a regional overview of plasticity data reported in the literature indicates that the values of liquid limit (LL), plastic limit (PL), and plasticity index (PI) of bauxite residue fall within a broad range of 11%–87%, 10%–45%, and 0%–52%, respectively, as illustrated by Figure 6.

Table 3. Parameter intervals of bauxite residue index properties reported in the literature for residues produced in different countries.

Country	Specific Gravity	Particle Size Distribution (%)			Atterberg Limits (%)
		Clay	Silt	Sand	LL	PL	PI
Global 1	2.56–4.22	1–58	20–93	0–50	11–87	10–45	0–52
Australia	2.93–3.1	13–54	40–78	2–39	40–65	24–37	7–39
Brazil	2.86–3.99	1–58	20–93	0–50	31–64	16–36	5–34
China	-	-	-	-	43–64	35–42	8–22
Germany	-	20–57	28–38	15–42	42–46	28–29	14–17
Greece	-	-	-	-	35–37	30–33	4–5
Guinea	-	-	-	-	76	45	31
India	2.7–3.45	8–32	51–92	0–28	11–46	10–36	0–13
Italy		29	38	33	42	34	8
Jamaica	2.92–4.22	-	-	-	87	35	52
Spain	3.44	2–38	38–83	10–29	37–41	30–35	6–8
Turkey	2.56–2.87	12–18	77–88	0–5	41–46	30–37	4–12
UK	3.05	20	76	4	54	40	14
USA	2.84–3.72	16–32	30–64	4–50	41–62	33–40	0–26

¹ [16,21,27,34,38,39,40,41,46,47,49,50,55,57,73,74,77,78,79,80,81,82,83,84,85,86,87,88,89,90,91,92,93,94,95,96,97,98,99,100,101].

summarises regional values of specific gravity, particle-size distribution, and Atterberg limits reported in the literature for bauxite residue, and the Supplementary Materials detail relevant information regarding the sources considered and testing methodology used.

4.2. Mechanical Behaviour

4.2.1. Compressibility and Compaction

The mechanical behaviour of bauxite residue is uniquely defined by a paradox: despite the absence of clay minerals and low plasticity, it usually exhibits geotechnical properties characteristic of clay-rich tailings, particularly high compressibility [76]. This behaviour is strongly influenced by the parent material of the bauxite ores and the processes employed during refinery processing.

Table 4. Parameter intervals of bauxite residue compression index reported for residues produced in different countries.

Country	Compression Index
Global 1	0.05–0.65
Australia	0.27–0.58
Brazil	0.12–0.65
India	0.05–0.10
Spain	0.20
UK	0.34–0.41
USA	0.12–0.56

¹ [39,40,75,83,89,92,95,97,100,102].

summarises the regional values of the compression index (Cc) reported in the literature for different operations, showing considerable variation across regions. A significant portion of the samples, particularly those from the UK, Australia, and the USA, fall into the highly compressible category, while the Indian database is a notable outlier, with consistently lower values. This suggests that mineralogical constituents, specifically the type and quantity of iron minerals and particle surface interactions, influence the consolidation behaviour. Furthermore, the chemical environment plays an important role, as the high alkalinity of caustic soda and variations in pore fluid pH can alter compressibility parameters; for instance, leaching or acid neutralisation may reduce the compression indices [40,92,99,102].

Similarly, the compaction characteristics of the red mud are highly sensitive to the residue composition and alkalinity, the ore source and extraction processing conditions, and the compaction effort. Research indicates that the mineral phases inherent to the orebody produce unique “compaction fingerprints”. As a result, the interval of maximum dry density reported in the literature is broad, from 12.4 to 20.0 kN/m³, while the optimum moisture content ranges from 20% to 45%, as detailed in

Table 5. Parameter intervals of bauxite residue compaction properties reported in the literature for residues produced in different countries.

Country	Effort Type 1	Maximum Dry Density (kN/m3)	Optimum Moisture Content (%)
Global 2	SP	12.4–16.6	26–45
	MP	15.2–20.0	20–30
Australia	SP	12.4	35
Brazil	SP	14.0–16.3	26–34
India	SP	12.6–15.6	33–45
	MP	16.8–20	20–28
Spain	SP	16.6	28
USA	SP	14.8–15.6	32–33
	MP	15.2–17.5	24–30

¹ SP = Standard Proctor; MP = Modified Proctor. ² [16,83,87,89,92,95,97,100,102].

. Consequently, bauxite residue operations can require site-specific compaction strategies, where higher energy levels or chemical additives may be necessary to ensure structural stability [92].

4.2.2. Shear Strength

Shear strength is arguably the key property for quantifying a material’s physical resistance. Figure 7 summarises the regional information available for untreated bauxite residue, including drained (CD) and undrained (CU) triaxial test data. The reported internal friction angle (Φ’) ranges from 18° to 43°, with data concentrated between 30° and 36°. For apparent cohesion (c’), the range is between 0 and 80 kPa, and most of the values are in the interval between 0 and 26 kPa [16,40,49,75,82,83,85,90,94,95,97,100,102,103]. The reported cohesion intercept (c’) is treated herein as an ‘apparent cohesion’, resulting from curve-fitting over specific stress ranges, or potentially from cementation bonding.

The Supplementary Materials detail relevant information, test methods and sources considered in this work. It is important to highlight that, perhaps unexpectedly, a considerable number of studies on this material do not present the experimental results graphically. Because of this, the evaluation of undrained shear strength parameters was limited to vane shear tests. These values are presented in the Supplementary Materials.

What has drawn considerable attention among researchers is the ability of a finely ground material to achieve such high internal friction angles as typically exhibited by bauxite residue.

Bauxite residue exhibits behavioural similarities to structured, cemented soils. During shearing, cemented soils are described by an initial yield surface that reflects particle bonding, with strains mainly elastic and limited in magnitude. Plastic strains may occur after the yield point. Therefore, the stress–strain relationship shows an initial peak, after which cementation bonds begin to degrade, typically at low axial strain. This leads to a decrease in strength as the frictional forces of smaller, individual particles become predominantly mobilised [104]. In some cases, a second peak can develop, driven by an increase in particle frictional strength, as illustrated schematically in Figure 8.

This model of cementation very likely applies to bauxite residue due to the presence of cementing mineral agents, such as DSP sodalite, and is supported by data on the residue’s shear response reported in the literature (Figure 9). Previous research shows that at lower confining pressures, bauxite residue usually exhibits a gradual increase in shear resistance up to 2%–8% axial strain, likely due to cementation bonds, followed by softening, occasionally reaching a second peak before a further reduction in shear resistance beyond 10% axial strain.

Cementation might also account for the limited increase in tip resistance with depth seen in many cone penetration tests with pore pressure measurements (CPTu) conducted in BR deposits, unlike the more common pattern in which tip resistance increases with depth due to overburden effects [76,105,106]. This is because the cementation bonds are not significantly affected by compressive loads, which limits variations in void ratio despite the increase in effective stress in situ.

Although the residue’s mechanical behaviour may be affected by the presence of cementation bonds, this alone does not explain the high internal friction angles reported in the literature, particularly at higher confining pressures in triaxial tests. It is plausible that the pronounced angularity of the particles could be a large contributor to enhancing interlocking and, consequently, frictional resistance [6,94,95,100].

Data on the undrained shear strength and strength ratio (i.e., the ratio of the undrained shear strength (S_u) to its effective overburden stress) of bauxite residue are even scarcer than on drained strength. Vane shear tests performed on a German deposit reported an undrained strength ratio of 0.39 at peak and 0.07 in residual or remoulded conditions, as seen in Figure 10. This figure shows a decrease of 80% in peak undrained shear strength by the end of the test, reaching residual S_u values of the order of 10 kPa. This suggests that the residue can exhibit high sensitivity. Sensitivity (S_t) in this context is defined by the ratio between the peak undisturbed and the remoulded (sometimes referred to as residual) undrained shear strength at the same water content.

While the vane result is of interest, the condition considered as a residual strength in this context is possibly one of deformation so extreme that it is difficult to assess its representativeness of a real field condition. Triaxial tests mostly indicate that although the material exhibits potential for strength loss, the process unfolds in a non-abrupt manner, and in most cases, the residual strength is not fully developed even at 25% axial strain, as illustrated in Figure 11.

5. Parameter Variability—Potential Causes and Chemical–Mechanical Relationship

Establishing a geotechnical database is a crucial initial step towards enhancing the operational safety of bauxite residue storage facilities. Given the material’s high alkalinity and the reliance on long-term storage deposits, maintaining physical stability throughout the operational and closure phases is the primary defence against structural failure and subsequent environmental contamination. Therefore, development of a global database provides a benchmark, offering a framework for alumina refineries to compare their site-specific test results against established typical ranges for this material.

As previously established, the mineralogy of the raw bauxite ore dictates the chemical boundary conditions of the Bayer process, shaping the resulting residue characteristics. Specifically, the caustic concentrations and temperatures required to extract alumina from monohydrate bauxites (boehmite/diaspore) alter the precipitation kinetics of DSPs and iron mineral matrices compared to those derived from trihydrate (gibbsite) digestion. This distinction in the refining conditions defines the material’s initial structure and, consequently, can contribute to variability in geotechnical parameters. Furthermore, residue management, disposal methods, and storage time vary among sites and influence the material properties post-deposition [31]. The facility’s operating history, local climate-driven weathering, and leaching govern the progression of in situ carbonation and pore fluid change, leading to a progressive decrease in total alkalinity and salt concentration, alongside the degradation of sodalite and calcite concentrations over time, shifting the material’s structural bonding and long-term aggregate stability [21,107].

However, the variability in the material’s geotechnical properties, detailed per region in

Table 6. Synthesis of global bauxite residue geotechnical parameters segregated by macro-region, presenting the mean value, Coefficient of Variation (COV, %), and the number of data points (N) for each engineering property.

Property	Africa	Asia	Australia	Europe	North America	South America
Specific Gravity	-	3.08 (8%; 24)	3.02 (2%; 3)	3.25 (8%; 2)	3.55 (11%; 16)	3.43 (9%; 41)
Clay fraction (%)	-	21% (51%; 13)	29% (43%; 11)	26% (71%; 12)	24% (25%; 8)	14% (93%; 33)
Sand fraction (%)	-	10% (79%; 13)	16% (65%; 11)	24% (108%; 12)	30% (54%; 8)	27% (58%; 33)
Plasticity Index (%)	31% (0%; 1)	7% (67%; 25)	20% (56%; 8)	9% (49%; 10)	12% (55%; 11)	12% (48%; 38)
Compression index	-	0.08 (26%; 10)	0.44 (36%; 3)	0.32 (27%; 4)	0.32 (48%; 6)	0.28 (47%; 21)
MDD (kN/m3)	-	15.7 (13%; 23)	12.4 (0%; 1)	16.6 (0%; 1)	15.8 (6%; 8)	14.8 (5%; 12)
OMC (%)	-	31% (24%; 23)	35% (0%; 1)	28% (0%; 1)	29% (13%; 8)	30% (10%; 12)
Peak Friction Angle (°)	-	33.1 (13%; 5)	39.2 (13%; 8)	39.7 (5%; 3)	39.1 (11%; 6)	30.6 (19%; 22)
Cohesion (kPa)	-	24 (75%; 5)	5 (161%; 8)	27 (173%; 3)	6 (90%; 6)	16 (131%; 22)

Note: Data points are formatted as Mean (COV%; $N$), where COV represents the Coefficient of Variation and $N$ denotes the total number of observations compiled from the literature. A hyphen (-) indicates a lack of published quantitative data for that specific parameter within the region.

, is markedly more pronounced than that observed in other mine tailings. An illustrative example of this issue can be seen in the data reported for operations in Brazil, South America. The coefficient of variation (CV) for geotechnical parameters from Brazilian operations indicates a high level of dispersion for most properties. However, all these samples originate from the same country and most likely share the same orebody origin, given bauxite extraction in Brazil. This highlights another significant matter: regional characteristics are not the sole source of parameter variation.

Beyond regional composition differences, an important yet frequently overlooked factor is how chemical characteristics affect the physical and mechanical properties of red mud—including both those intrinsic to the refining process and those triggered by external influences. In this context, it is essential to evaluate how standardised laboratory protocols may inadvertently modify these chemical conditions, potentially producing parameters that may not accurately reflect in situ performance.

To understand this relationship, the following subsections address considerations of potential chemical–mechanical coupling effects relevant to red muds.

5.1. Thermal Treatments

The leading process capable of altering the chemical features of red mud is thermal treatment, specifically drying. Most standardised laboratory protocols recommend drying the samples, either by air or in an oven, as an initial step in specimen preparation. Although common, evidence suggests this practice can alter residue structure by promoting particle aggregation.

Several authors report changes in particle-size distribution after drying, indicating that oven drying reduces the proportion of fines, while increasing the sand content [16,83]. This difference can be substantial, with the clay fraction reported to decrease by 7 times upon oven-drying the red mud at 100 °C compared to air-drying [95].

While less definitive than the trends observed in PSD, a relationship between drying methods and plasticity also seems to exist. Specifically, a decrease in the plasticity index is often observed after oven-drying bauxite residue compared to air-drying [83]. This effect remains a point of debate, however, as some laboratory data show only minor variations in plasticity indices [78,95]. This inconsistency could partly stem from the lower precision of plasticity testing compared with other soil properties. Nevertheless, there is precedent for the view that drying induces an irreversible alteration in the plasticity of red mud that cannot be restored upon rehydration [74], even if the observed changes are sometimes small in magnitude.

These behavioural changes strengthen the view that red mud is a material susceptible to chemical bonding. This is attributed to the loss of residual or attached water from interstitial voids during oven drying, which promotes strong interparticle attraction. Consequently, the drying process may also indirectly influence the shear strength. Although this mechanism has not been explicitly examined in literature, drying-induced particle aggregation can lead to a loose soil structure, and previous studies suggest that coarser bauxite residues tend to have increased porosity and greater sensitivity [73,102].

To isolate laboratory-induced variability from inherent material heterogeneity, global baseline means were compared by drying pretreatment (

Table 7. Quantitative comparison of global mean geotechnical parameters for bauxite residue subjected to different pre-testing laboratory drying methods (air-dried vs. oven-dried), including the relative change ($\Delta$) in measured properties.

Property	Air-Dried	Oven-Dried	Relative Change, Δ (%)
Atterberg Limits	$N$ = 28	$N$ = 22
Liquid Limit (%)	39%	43%	↑	8%
Plastic Limit (%)	26%	29%	↑	13%
Plasticity Index (%)	13%	13%	↓	<1%
Particle Size Distribution	$N$ = 11	$N$ = 21
Clay Fraction (%)	12%	14%	↑	19%
Silt Fraction (%)	74%	57%	↓	22%
Sand Fraction (%)	15%	28%	↑	94%
Particle Density	$N$ = 26	$N$ = 17
Specific Gravity (-)	3.24	3.37	↑	4%
Shear Resistance	$N$ = 4	$N$ = 1
Friction angle, φ’ (º)	36.8	30.5	↓	17%
Cohesion, c’ (kPa)	9	0	↓	100%

N = Number of observations in the group. The arrows denote an increase (↑) or decrease (↓) in the mean values of the variables under different conditions.

). Oven-drying significantly alters the particle size distribution (PSD), causing a 22% reduction in the silt-sized fraction and a near-doubling of the sand-sized fraction (from 15% to 28%). In contrast, the effects on plasticity are modest. Oven-drying increased the Liquid and Plastic limits, but because both thresholds shift concurrently, the resulting Plasticity Index remains virtually unaltered (Δ = −1%).

In highly alkaline tailings, these thermal shifts indicate temperature-driven microstructural and mineralogical alterations, such as the aggregation of fine particles or changes in the hydration state of sodalite (DSP) frameworks. This divergence highlights the need to standardise pre-test treatments; mixing data from different drying protocols may compromise the reliability of geotechnical design predictions. Comparisons of shear strength parameters across drying conditions must be interpreted with strict caution due to database limitations ($N$ = 5 observations, with only one oven-dried sample), this being a critical point for future experimental investigation.

5.2. Salinity and pH

Although processed bauxite residue is highly saline, the vast majority of studies on geotechnical behaviour do not account for dissolved salts and their influence on geotechnical properties. In this context, two issues require attention: the first is the correction of geotechnical properties for total dissolved solids concentration [108,109], and the second concerns changes in residue properties when subjected to leaching, weathering or neutralisation processes that reduce salt content within the system.

Perhaps the most critical property for which salt correction is relevant is specific gravity, as dissolved salts artificially alter the measured mass and fluid density during laboratory testing. Because specific gravity is a foundational parameter, failing to correct for salt concentration creates a domino effect, leading to inaccurate calculations of the void ratio, porosity, and state parameter, ultimately compromising the accuracy of engineering models that predict the facility settlement, shear strength and stresses. One approach to correcting for salinity is to leach the residue with distilled water to reduce soluble alkalis and salts. This process has been shown to reduce Gs values to 2.84–3.27 [102], compared with the higher baseline of 3.21–3.72 [83] observed in untreated samples from North America, presented in

Table 8. Quantitative comparison of North American mean geotechnical parameters for bauxite residue subjected to different pre-testing saline treatments, including the relative change ($\Delta$) in measured properties.

Property	Untreated	Leached	Relative Change, Δ (%)
Atterberg Limits	$N$ = 10	$N$ = 5
Liquid Limit (%)	47%	45%	↓	4%
Plastic Limit (%)	35%	38%	↑	8%
Plasticity Index (%)	13%	8%	↓	43%
Particle Density	$N$ = 7	$N$ = 3
Specific Gravity (-)	3.55	3.09	↓	13%

N = Number of observations in the group. The arrows denote an increase (↑) or decrease (↓) in the mean values of the variables under different conditions.

. However, there is still limited data on the reproducibility of this testing method. Most studies on bauxite residue do not address salinity-related property corrections, raising uncertainty about the reliability of the database for this property.

The second issue concerns the physicochemical changes that occur when the material experiences a reduction in salt concentration, altering the internal balance of interparticle and particle–fluid chemical forces. These mechanisms are particularly pronounced in bauxite residue, where the macroscopic behaviour is governed by these complex, surface-level chemical forces.

For instance, leaching the red mud with water to reduce the dissolved solids content has been shown to reduce the plasticity of the residue [102], as seen in Table 8. Conversely, Atterberg limit tests performed using process liquor instead of water have been shown to increase the plasticity index [74]. This indicates that the material’s plasticity is dynamic and governed by physicochemical interactions between particle surfaces and the pore fluid. There are currently limitations in understanding how chemical sensitivity varies and how to manage these changes during testing to ensure consistent, repeatable results.

The chemical–mechanical coupling is equally prominent when examining the effects of chemical treatment and neutralisation (

Table 9. Quantitative comparison of global mean geotechnical parameters for untreated and neutralised bauxite residue, highlighting the relative percentage change ($\Delta$) in consistency limits, particle size fractions, and specific gravity.

Property	Untreated	Neutralised	Relative Change, Δ (%)
Atterberg Limits	$N$ = 66	$N$ = 16
Liquid Limit (%)	42%	35%	↓	16%
Plastic Limit (%)	29%	26%	↓	8%
Plasticity Index (%)	13%	9%	↓	34%
Particle Size Distribution	$N$ = 35	$N$ = 9
Clay Fraction (%)	15%	13%	↓	13%
Silt Fraction (%)	64%	56%	↓	13%
Sand Fraction (%)	21%	31%	↑	50%
Particle Density	$N$ = 46	$N$ = 17
Specific Gravity (-)	3.26	3.33	↑	2%

N = Number of observations in the group. The arrows denote an increase (↑) or decrease (↓) in the mean values of the variables under different conditions.

). The high concentration of sodium ions (Na⁺), especially in fresh red mud, enhances interparticle repulsion forces, affecting the material particle size distribution. However, when salinity and pH decrease (naturally through weathering or artificially via neutralisation), sodium is replaced by calcium ions (Ca⁺), forming micro- and macro-aggregates on the residue structure. Therefore, the proportion of the sand-sized fraction can increase in these conditions [25,69,71,72]. This aggregation mechanism is quantitatively supported by global particle-size trends, in which neutralisation induces a 50% relative increase in the sand fraction (from 21% to 31%) and a 13% reduction in both the clay and silt fractions. Furthermore, this structural reorganisation affects plasticity; neutralisation reduces the Liquid Limit by 16% and the Plasticity Index by 34%, while the mean Specific Gravity shows a modest increase of 2% (3.26 to 3.33). Neutralising the highly alkaline residue shifts the residue toward a coarser, less plastic geotechnical matrix, potentially governed by chemically induced aggregation.

As for strength, more than 95% of the studies compiled in this review report that shear strength tests were conducted exclusively with non-process water (e.g., tap or distilled water). For some tailings, this practice is unlikely to affect the material’s properties; however, the mechanical behaviour of bauxite residue appears to be sensitive to pore fluid chemistry. Leaching and neutralisation have been associated with reductions in void ratios and compression indices, as well as reductions in undrained shear strength, and appear to promote a more viscous behaviour, particularly at higher moisture contents [40,41].

Critical state studies of bauxite residue indicate variations in pore fluid chemistry, particularly the replacement of process liquor with non-process water, have been associated with reduced salinity and with lower critical-state lines than in specimens saturated with process liquor [38,49,100]. These changes are attributed to alterations in void ratio, compressibility, and specimen fabric, indicating that the residue chemistry influences the mechanical behaviour of bauxite residue. Nevertheless, the selection of pore fluid in shear strength testing of bauxite residue is rarely addressed in the literature, with most studies employing non-process water without a systematic evaluation of the effects of this parameter. Methodological differences and the absence of a standardised approach may therefore partly explain the variability in reported strength parameter values.

Figure 12 synthesises the main chemical–mechanical processes of bauxite residue as documented in the literature.

6. Gaps and Research Directions

This review highlighted current limitations in the understanding of the geotechnical behaviour of bauxite residue. Some sources in this review are dated or overlook variability in geotechnical parameters caused by composition, processing, or testing methods.

One general obstacle appears to be the approach to replicating field conditions in laboratory practice. A significant portion of the studies included in this review examine material properties using standard soil mechanics methods. However, as highlighted earlier in the paper, the selection of laboratory methods is important, as it influences results by altering geochemical interactions and even the fabric, potentially leading to misinterpretation of data if not assessed. This challenge is exacerbated by the fact that studies addressing relevant factors (e.g., composition, pore chemistry, aggregation) usually do so in isolation, thereby contributing to a fragmented and poorly consolidated knowledge base.

Given these considerations, a gap analysis was conducted to identify research needs and priorities related to red mud geotechnical characterisation, as described in

Table 10. Research needs and directions for future research on the characterisation of geotechnical parameters of bauxite residue.

Category	Knowledge Gap	Proposed Directions
Contextual	The impact of geochemical features on characterisation and shear strength parameters remains underexplored. Changes in the material fabric influenced by chemical factors are largely unaddressed. There is no consensus on how best to replicate field conditions in laboratory settings. Although studies indicate that the material may experience substantial strength loss under shear, the mechanisms underlying this behaviour remain poorly understood. Test results indicate that residual strength is not fully mobilised at axial strains of 25%.	Adopt multi-scale testing frameworks that couple geotechnical tests with micro-analytical monitoring (such as SEM, XRD and pore fluid concentration tracking). Utilise high-strain apparatuses to capture post-peak degradation and fully mobilise residual strength under varying chemical conditions. Design comparative testing programs to evaluate sample preparation protocols (such as oven-drying at different temperatures) and conduct sensitivity analyses. Use controlled leaching to remove salt prior to testing or measure the total salt concentration to correct the soil-phase equations.
Conceptual	There is no consensus on how temperature affects the Atterberg limits.
Methodological	Studies rarely report any correction to BR properties due to pore fluid density. No consensus exists regarding the appropriate method for drying BR samples prior to experimental testing. Drying may induce particle aggregation and increase porosity.

. The analysis was designed to synthesise the main limitations in current research and their implications for the operation and stability of bauxite residue storage facilities. To provide structure and clarity, the gaps were categorised into three main types, in order of priority: (i) contextual—relating to under-studied topics; (ii) conceptual—involving conflicting or inconsistent theoretical frameworks; and (iii) methodological—concerning the selection and application of laboratory techniques and interpretation of results.

Implications and Priorities

The definition of index properties for geomaterials affects the engineering team’s perception of a storage facility operation. For instance, specific gravity provides information on expected settling behaviour and the in situ void ratio, while particle size distribution influences perceptions of the facility’s hydraulic regime. It is still common to use PSD data as input to define hydraulic functions and soil-water characteristic curves in numerical models [110,111,112]. Moreover, current geotechnical practices continue to exhibit a surprisingly persistent reliance on empirical correlations between plasticity indicators and shear strength or static liquefaction potential [113,114,115]. Consequently, inaccurate estimates of these properties can lead to serious misjudgements of material behaviour, with potential implications for both design and risk assessment. Examples of how these properties manifest in practice include: influencing the effectiveness of the facility disposal plan, impacts on predicted pore pressure and effective stresses within the facility, as well as on long-term seepage and stability studies, thus increasing the environmental risk of contamination due to the facility’s possible collapse and the subsequent release of hazardous red mud into nearby areas.

As shown in this review, the greatest challenge in red mud characterisation lies in replicating and controlling the chemical characteristics while simulating field conditions during experimental tests. For example, most standardised laboratory protocols recommend oven-drying samples. Although common, the practice can modify the residue structure by promoting particle aggregation. This highlights the importance of selecting appropriate methods for handling and drying red mud samples prior to testing. Moreover, evidence indicates that pH and salt concentration decrease over time after deposition, which may also affect the residue microstructure and fabric; however, studies evaluating these time-dependent changes in geotechnical properties are scarce.

The fabric of bauxite residue appears to be so fundamental and complex that even minor variations could affect it. For instance, most of the compiled experimental strength data were obtained by oven-drying the samples and using non-process water (e.g., tap or distilled water). For some tailings, this practice is unlikely to affect the material’s properties; however, given the chemical nature of bauxite residue, this may not be the case. Another potential issue is that drying preserves the total salt mass within the sample, which, if followed by saturation of the specimen with process liquor, could artificially increase the salt concentration, thereby deviating from in situ conditions.

Another important knowledge gap concerns the strain magnitude required by the material to reach the residual state. Studies on this topic are mostly dated and suffer from methodological limitations. When strength loss is observed, it typically occurs gradually and requires large strains to develop fully—a condition usually barely achievable in triaxial tests. It is also worth considering that the limited vane shear test data available in the literature suggest that the residue can exhibit alarmingly low undrained shear strength values (of the order of S_u ≈ 10 kPa). Given that the material does not exhibit abrupt strength loss but may exhibit very low shear resistance at large strains, the selection of parameters for operational stability analyses might differ from those adopted for extreme conditions, such as seismic or dam-break events. Broader assessments, including residual mechanical behaviour, are important for ensuring safe and sustainable aluminium production and avoiding further environmental accidents.

7. Conclusions

This review established a geotechnical database of bauxite residue properties, demonstrating that the complexity of material composition, processing conditions, and variations in experimental protocols result in considerable variability across sites. To establish an industry benchmark, this work compiled globally reported parameters and highlighted critical contextual, conceptual, and methodological knowledge gaps. Because of the material’s extreme sensitivity to chemical changes, the parameter ranges synthesised herein serve as a conceptual reference, as site-specific testing remains necessary for facility design.

To assist engineers in predicting material behaviour and ensuring safer stability design, this review summarises some practical guidelines based on the residue’s baseline conditions and testing methods:

• Information regarding the source of the residue and the conditions under which it was processed prior to deposition is important. Variations in ore composition and processing generally result in different initial matrices, which in turn affect the residue’s composition and physical and geotechnical properties.
• The general challenge in determining reliable geotechnical parameters is replicating field conditions. Standard soil mechanics practices, such as oven drying and the use of non-process water, are critical taboos. These pre-test treatments can modify the residue’s chemistry and structure, leading to severe mischaracterisation that can culminate in structural collapse or catastrophic environmental accidents. Additionally, reliable test protocols must account for the presence and concentration of salts within the pore fluid to correct geotechnical parameters.
• Predicting long-term and operational stability requires looking beyond peak strength and evaluating undrained shear strength at very large strains, as the material exhibits gradual post-peak strength loss that can reach critically low residual values.
• Tracking the chemical evolution of the residue under weathering scenarios is important for closure and post-closure design. Practitioners must account for the effects of weathering and leaching in older deposits, as these processes may progressively lower pH and salinity, affecting structural bonds and altering long-term aggregate stability compared to freshly deposited slurry.

This work includes a database that compiles geotechnical parameters and methodologies reported worldwide. Although many questions remain, this initiative consolidates global knowledge to provide a practical basis for engineers. Advancing this field will require additional integrated geochemical and geotechnical research, along with improved, material-specific experimental protocols, to support safer and sustainable management of bauxite residue storage facilities.