Abstract
The limits of elastic behaviour change with the nature of the impulse applied to a target and the size of volume interrogated by a measurement, since it is the preexisting defects sampled within its rise that determine the response observed. This review considers a range of solids of different material classes and tracks the development of the strength of the material during shock loading, from yield at the Hugoniot elastic limit, across the weak shock regime, to its transition to strong shock behaviour. It is shown that at this stress, the weak shock limit (WSL), the shear component of the applied stress exceeds the theoretical strength of the material. Beyond this threshold, there are a number of new responses that confirm a transition from an inhomogeneous to a homogeneous state. Further, whilst strength rises across the weak shock regime, it saturates at the WSL. For instance, failure in shocked glasses transitions from localised fracture initiated at target boundaries to a global failure at this threshold at the theoretical strength. Sapphire′s strength asymptotes to the theoretical strength of the strongest direction in its lattice. Finally, the fourthpower dependence of strain rate upon stress appears to be a consequence of the homogeneous flow in the strong shock regime. This review suggests that µ/2π is a good approximation for the unrelaxed theoretical strength of solids at increasing stresses beyond the WSL. The methodology unfolded here represents a new means to experimentally determine the ultimate shear strength of solids.
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Introduction
The strength of a target constructed from its constituent components is a vital measure to quantify its resistance to failure during loading, yet strength is a term which returns different levels according to the speed and severity with which one applies force. Science texts have derived a framework to classify the concept built over hundreds of years [1,2,3]. The discussion herein will show the strength of solids changing at different scales and across different regimes of applied, dynamic loading. There have been other reviews of strength measured during shock loading, but this focuses particularly on the transition in behaviour as one crosses from the weak to the strong shock regimes and beyond [4,5,6,7,8,9,10,11,12,13]. It will consider particularly compression states, and span the elastic regime, through to solids in states at the boundary with warm dense matter [10, 14,15,16,17,18,19]. In the lower stress regimes, the role of the initial distributions of defects in the asreceived materials is key, and their significance across the boundary, between the so called weak and strong shock regimes, will be discussed in detail [4, 20].
The asreceived microstructures of common engineering materials, and their states under ambient conditions, are the key consideration in the weak shock regime, where a wave loads material to a shear stress less than its theoretical strength. Thus metals, as well as brittle materials, polymers and composites, show a variety of behaviours in this regime [20, 21]. However, there is a thread that will be traced showing the behaviour of solids becoming ever more homogeneous as compression increases [18, 22]. In the weak shock regime, there is key dependence on the preexisting defect structure encountered by the impulse since this leads to an inhomogeneous stress state seeded at these locations behind the front. In the strong shock regime dislocations are nucleated homogeneously at the front, which implies hydrodynamic flow behind the shock. Both these states are mediated by the effects of the increased temperature accessed as greater amplitudes of loading are delivered [4, 23, 24]. It is hoped that the treatment presented here will draw together key features of response in a consistent manner across very different amplitudes of insult, to illustrate the role of applied stress thresholds in the behaviour of solids under shock loading.
Background
The effect of confining pressure on condensed matter has been a subject of active research and debate through the centuries [2, 20]. In particular there has been a focus on the failure of materials or structures under forces applied to the component or material in question [21]. The development of solid mechanics has created a framework in which dynamic loading leads to components of force decomposed into hydrostatic and deviatoric components and formal definitions of strength and criteria for damage were developed alongside these [1,2,3, 25]. Over time these concepts have been applied at smaller length scales and the increased strength of smaller and smaller components drives nanoscale research e.g. [26]. Thresholds delineate behaviour, beginning with measurements of the elastic/inelastic strains that fail a material.
The strain, and the strain rate (its speed of its application) are typically used as indicators that determine response to load. Here we will think in terms of the temporal components used to assign strain rate that may be divided into a time over which the impulse rises and a duration before it is released. These will be compared with the relaxation times for the operating micromechanics that accommodates the applied strain. Many solids are polycrystalline materials and, in more rapid loading, their response is governed by the transition from strain across the bulk to that within an individual grain as the applied pulse length decreases [6, 27]. Impact, lasershock, explosives or electromagnetic pulses provide a suite of impulses of varying amplitudes and durations that excite phenomena at the fastest rates to overcome strength within a material. In this respect, the shock is a critical tool that pumps a material within a particular loading envelope and probes a suite of mechanisms excited across the scales (Fig. 1). A range of techniques have been developed to analyse response and determine strength [28,29,30,31,32,33]. However, whilst an impulse appears to rise discontinuously at a longer timescale, at a lower one that rise will appear ramped. Nevertheless, ultimately it is the bonding within matter that mediates the strain induced and the mechanisms that operate.
There are two basic classes of structural response in crystalline solids considered here—the movement of planes down slip directions, and cleavage of interfaces in disordered or brittle materials. Of course, applying an impulsive load to matter will also trigger thermal effects and while some mediate the response observed, reaction may also be triggered within excited energetic materials. Planes in a deforming solid may slip past one another, or stacking may reorder by slight shifts in position in order to accommodate the displacements applied at an interface. As is well known, slip is mediated by dislocations in crystalline solids or alternatively twinning may occur if Peierls stress is high or where excess extra energy is required to insert a new atomic plane (see in [34] for example). In covalent materials, and in those where slip is difficult, cleavage is generally the preferred mechanism to induce the failure that accommodates strain [3, 34]. Finally, martensitic phase transformation, that operates with a very similar atomic movement to that induced in twinning, may occur in some solids as applied stress increases [5]. As stress amplitudes increase, more and more slip planes are activated to accommodate greater forces until eventually the crystal slips on every atomic plane at the point at which the shear strength of the material is overcome.
Strength in the Weak Shock Regime
Theoretical Strength
In compression, the yield strength refers to a limit beyond which the valence electronic shear strength is exceeded and the solid adopts a new stable electronic conformation [35, 36]. Of course, such strength approaches a theoretical limit as the volume of material considered shrinks to atomic dimensions [37, 38]. Discussion of how to determine this theoretical strength began with the work of Frenkel and OrowanPolanyi, and has been extended and made more accurate over the years [26, 39,40,41,42,43,44]. Whilst there is still no agreed method to measure the theoretical shear strength, it may be determined by a range of methods of increasing computational complexity, particularly now that ab initio methods are routinely used to determine values for particular slip systems in ideal lattices of ionic or covalent crystals [45,46,47]. The theoretical shear strength for a material (τ_{Th}) may be estimated analytically using a range of methods, but one simple and powerful approximation, after Frenkel, is given by the shear modulus µ/2π [26, 41, 42]. This value is used in what follows but is, of course, an approximation. Other workers have calculated values for the ideal shear strength in the range µ/18–µ/4π using ab initio calculations deforming unconstrained crystals to failure [48,49,50]. This range has been shown to be consistent with nanoindentation data (indenter 50–1000 nm) in the metals Al and Ni [51]. However, these calculated values correspond to the fully relaxed state although other calculations also show that lattices have an energy of order twice this magnitude giving a calculated shear strength close to µ/2π [49, 52]. Thus, in what follows, this latter value will be adopted as a representative value for the theoretical shear strength in the shocked state.
Yield Strength and Tensile Strength
Investigation over many years has shown yield strength to increase with strain rate. This means of framing the problem has served macroscale engineering problems well. However, the strength at failure is never more than a fraction of the theoretical strength because of preexisting stacking and volume defects. The Hugoniot elastic limit (HEL) is the yield stress in onedimensional strain for a solid. Polycrystalline materials are generally composed of grains of random orientation with amorphous or low order regions between them and thus, in the general case, appear isotropic beyond the mesoscale unless worked or alloyed to achieve a particular texture. These observations are represented mathematically in constitutive descriptions of materials typically used in macroscale simulations of engineering structures under load [6, 53]. More complex behaviour is found for anisotropic materials, for instance the triclinic αalumina (sapphire) crystal that shows a range of HELs between r axis ca. 12 and c axis, 21 GPa [54]. In contrast, the alumina AD995, that consists of a polycrystalline composite of these crystals with random orientation, has an HEL of 6.7 GPa which is much less than that for the loading in 1D down the weakest direction. It can however plastically yield down easy directions in a 3D strain state at the mesoscale in this composite and recovery of shocked AD995 shows the onset of twinning in suitably oriented grains at this stress [55]. It is this first yield in the composite that bounds a region of mixed response where some grains behind the shock are still not plastically yielding up to the point where the shock amplitude exceeds the yield stress down the c direction. We shall return to higher amplitude loading of this alumina in section ‘Strength in the Strong Shock Regime’ below.
There is a volume of preexisting defects typically found within solids at the mesoscale that sets the boundary for the deformation that follows when it is shocked [34]. In rapid loading, dislocations or tensile failure paths are generated behind shock pulses. Dislocation theory provides examples illustrating these including FrankRead sources in FCC metals at lower strain rates for instance, moving to homogeneous nucleation at strain rates greater than 10^{7} s^{−1} [48, 61, 62]. If pulses are applied slowly, plasticity is stabilised around these preexisting defect sites since the strain fields around them remain uniform; if pulses are longer in duration then the volume across which the applied strain is distributed is larger. Those that are faster rising sample smaller volumes and thus sweep fewer preexisting defect sites as they propagate. Thus, failure is pushed to higher load amplitudes. This is illustrated in Fig. 2, which shows measurements of compressive and tensile strengths in planar shock experiments; longer, more slowly rising pulses induced by flyer plates and shorter, rapidly rising ones induced by lasers. In both cases the metal loaded is pure, (FCC) aluminium—one of the standards investigated in dynamic experiments [23, 56, 58, 63,64,65,66,67,68,69]. The pulse lengths are limited by the loading methods and sample geometries adopted. In Fig. 2a. the magnitude of the elastic precursor (the Hugoniot elastic limit; HEL) is measured for different pulse loadings on pure aluminium films and shows an increase in measured compressive strength with decreasing pulse length. In Fig. 2b, the spall strength of the foil is shown and as loading time reduces, the tensile strength again increases.
Of course, as the duration and the risetime of the pulse are reduced, there is a corresponding decrease in the target volume sampled and thus the number of preexisting defects within the microstructure that are accessed. This fails the material at higher stress levels and results in increased shear and tensile strengths measured in the target. There are two manufacturing routes for the aluminium targets in each class of experiment; rolled sheets in the case of the plate impact experiments or vapour deposited films for those in the laser loading. Both of these present a different defect population to each respective impulse, although the experimental measurements acquired will integrate a distribution of responses to each [21, 34]. In both cases the strengths recorded asymptote to higher values ultimately reaching the stress at which the theoretical strength is reached for pure aluminium which is ca. 18 GPa derived using the approximation (5) described below.
There is a critical threshold in behaviour crossed between ca. 1 (compression) and 10 ns (tension) (ca. 10 µm) and this corresponds to the confinement of the changing state of strain within grains. Here the pulse risetime samples a number of inclusions and stacking defects alone without failing additional grain boundaries or second phases of lower strength [4, 20, 21, 28]. This corresponds to a critical strain rate at which measured yield strength is seen to rise rapidly and which, for aluminium, is ca. 10^{6}–10^{7} s^{−1}. Other authors have discussed transition to a phonon drag mechanism at this stress [70]. In spall, failure occurs by interactions that supply a dispersive tensile impulse and so this region is somewhat wider. Nevertheless, this rapid loading filters many of the failure mechanisms that might occur at defects at larger scale and renders the material to appear stronger as a result. Inertial confinement ensures that the volumes accessed become sufficiently small that the loading period of interest has been probed before the presence of boundaries can relieve the strain and in shock loading this region confines the strain to be uniaxial at the macroscale [4, 21].
Related behaviour is seen in other FCC metals such as copper or nickel, which also harden with strain rate as dislocations entangle during rapid loading, whilst in BCC tantalum, strength increases with strain rate without hardening on unloading since the Peierls stress is much higher and the nucleated dislocation density much lower [21, 28, 29, 31, 33, 53, 71,72,73,74,75]. Ceramics show a similar behaviour, with strength remaining constant as loading pulse length decreases, until the rise of the load no longer probes the weaker glass matrix and starts to purely strain the hard crystals contained [76,77,78,79,80,81]. Finally, in polymers, strength rises as the pulse probes smaller, crosslinked sectors (such as spherulite structures for thermoplastics) [82,83,84,85,86,87,88,89,90,91,92]. It is clear that the scale of the volumes probed in matter, the times taken for mechanisms to complete, and the magnitude of the disturbance applied, all have a marked effect on the responses observed. The microscale/mesoscale boundary is a critical length scale where behaviour in metals, for instance, transits from polycrystalline texture to periodic order and this is reflected in response at high strain rate in materials under load. In both cases the strengths recorded asymptote to the theoretical strength of aluminium which, calculated using the formalism described below, is ca. 18 GPa.
Compressibility
There are thresholds in compressive behaviour that, when applied to a pulse, open up new modes of response for a microstructure [14, 16, 17]. The elasticinelastic transition is the first of these accessed as stress amplitude increases. Beyond this stress, crystalline solids inelastically deform at stacking and volume defects that trigger slip, twinning or fracture in materials [34]. However, in the region above the elastic limit, most materials deform by processes that compress it to a more homogeneous state. First order, martensitic phase transformations may occur at higher stress levels and melting or other transformations at higher pressures again [5, 23, 93,94,95]. However, until the theoretical strength of the material has been exceeded, volume defects, present initially in the material for instance, have not been eliminated and there are still inhomogeneous states behind the front. There comes a stress level however, at which the processes triggered are driven sufficiently quickly that they complete in a single front travelling faster than the elastic wavespeed within the material. Above this threshold, the front separates virgin from homogeneously deformed material and the width of the front, representing the time to complete these processes, decreases monotonically with increasing applied stress level [96].
The point at which this overdrive occurs represents the end of weak shock behaviour and defines the weak shock limit (WSL). At this point the shear component of the stress applied exceeds the theoretical strength of the material. A single shock drives at a velocity U_{s} and overtakes the elastic precursor so that the shock speed is equal to longitudinal wave speed, c_{L}, to overdrive the material of initial density, ρ, Fig. 3a [24]. Compendia of data gathered in shock compression measurements on many solids have been collected over the years and several sources for these are archived in a series of key sources [97,98,99]. These show that the shock velocity, U_{s}, typically shows a linear relation as a function of the particle velocity, u_{p}, thus
The overdrive stress, the longitudinal stress, σ_{WSL}, that has a shear component corresponding to the theoretical strength, τ_{Th}, is given by
An approximation can be made for isotropic materials, assuming a simple Tresca yield criterion, to relate the strength in one dimensional strain (the HEL) to the shear strength at this stress through
The ratio α between the yield and shear stresses will be used to connect elastic stress and shear states where
There are various means to calculate or deduce a value for the shear modulus of solids and this value can be converted to a longitudinal stress equivalent by using (3). For instance, it is possible to deduce the ambient shear modulus µ of the material, by ultrasonically measuring shear wave speeds, c_{s}, in asreceived samples under ambient conditions. This measurement can be used to deduce a theoretical strength through µ/2π where
thus, values for the elastic stress corresponding to the theoretical strength can be calculated since the weak shock limit corresponds to the elastic limit of a defect free material. Values for the WSL can thus be recovered in several manners and these will be used as a framework to discuss the strength limits in a range of materials at the transition from weak to strong shock behaviour. However, it should be noted that the yield criteria (3) is an approximation first since it uses mechanics derived for a macroscale response and secondly since it assumes isotropy which is a reasonable approximation for polycrystalline, ductile metals at the macroscale but not for the anisotropic materials. The equation σ_{WSL} = α τ_{Th} is consistent with the compendium of shock measurements examined for realistic values of a across all of the data so far reviewed by the author.
Strength in the Strong Shock Regime
Figure 3 shows the theoretical shear strength correlated with the observed limit of weak shock behaviour across a range of materials. This regime is dominated by valence electron bond strength. Inner core electron interactions are only seen at a much higher threshold where compressions exceed several hundred GPa; this region will not be considered further in this paper. The stress corresponding to the theoretical strength, σ_{WSL}, is equal to ατ_{Th} (Eq. 4), where the factor α depends upon the initial, ambient properties of the element sampled. As discussed, the relations derived above apply to isotropic materials with no assumptions made about microstructure, however, it is nevertheless remarkable that clear trends are observed in mapping Hugoniot data for a great range of materials.
Of course the WSL has a numerical value greater than the theoretical strength, and at least for the elements listed in [24], lies between two extremes determined by structure (Fig. 3b). The data for these curves are largely taken from shock experiments and were gathered in the post war period [97,98,99]. The two dotted lines bound the data and represent the ratio α, through Eq. (4), using values for the Poisson’s ratio of 1/3 and 1/4, typical of ductile and brittle materials. It is clear that BCC and covalent materials lie on a different trajectory to their more densely structured FCC counterparts even though their initial Poisson’s ratio is close to 1/3, whilst others lie in states between these two limits. Despite the uncertainties in calculating theoretical strength by this treatment, these trends are clear, and there are indications both here and in other work that Poisson’s ratio retains importance beyond the elastic limit. This indicates that the behaviour of materials in the weak shock regime is not fully hydrodynamic reflected in changes in the Poisson’s ratio until the WSL is reached [100].
Above the WSL, inhomogeneous states are confined to the zone spanned by the shock rise. States behind the shock are inhomogeneous in the weak shock region. Processes within the front have been discussed extensively by Grady in his work on the structure of shock waves. He has shown that in the strong shock regime, the strain rate in the pulse is proportional to the shock amplitude to the power four, \(\dot{\varepsilon }\propto {\sigma }^{4}\), and has discussed the energy balances inside the front that lie behind this relationship [96, 101, 102]. At lower stresses, lower powers are recovered. Again, this indicates that the equilibration of inhomogeneous states takes a time which has a strong dependence on the stress level attained. In crystalline systems, slip processes transit from activation of slower, preexisting dislocations and new loops created by Frank–Read sources for instance, to homogeneous nucleation above their theoretical shear strength [103]. The transition will be explored in brittle systems below.
Quartz and glasses are both important natural and engineering materials and also illustrate a suite of densification mechanisms that complete at the weak shock transition in strong, covalent brittle solids [105, 106]. Two sources of data for quartz and for the more open structure sodalime (SL) glass are combined in Fig. 4 [76, 97, 98, 107]. At lower loading amplitudes, the processes operating in the inhomogeneous region between the elastic and shock fronts are easily seen since glass is transparent. Failure waves are phenomena by which glass is seen to densify, and a fracture front lags behind a pseudoelastic shock travelling ahead of it [78, 106,107,108,109,110]. Figure 4a shows a streak sequence taken after the deformation of sodalime glass shocked to a stress of ca. 5 GPa. Impact induces an elastic front that progresses across the target and reaches the free surface after ca. 3.5 µs. As it reflects, the interface is accelerated, and darkened areas show decompression at the free rear surface. Further, a slower, dark fracture front propagates back towards the impact face behind the release. Two vertical lines are ruled onto the far surface of the target to fix a spatial scale for the sequence. Viewed through the compressing glass, these are refracted and deflected by the moving front and compressed material behind both shock and release indicate that both the refractive index and the Poisson’s ratio, v, are changing [100, 108, 109, 111].
The first front travels at a velocity which settles to an elastic wave speed but is initially some 20% slower than this. This unsteady behaviour is also observed in sapphire in the weak shock region. Further, the shock rise (and thus its width) broadens with travel distance. There is a second, parallel region seen following the shock, which denotes a relaxation in stress behind the front that is seen here since schlieren imaging displays regions of changing compression. The failure front, which is believed to be fracture, follows at a slower speed (around 2 mm µs^{−1}), ca. half of the shear wave speed at this stress level. The imaging of a transparent material gives detail not normally directly observable, showing incubation times and details of operating mechanisms in the compression of this partially filled glass. As the amplitude of the impulse becomes greater, failure mechanisms become overdriven and the dark front is seen to merge into the shock.
Above the stress amplitude at which all deformation is within a single front, the value of U_{S} increases linearly with u_{p} and the compression of the openstructured glass follows the same path as the quartz single crystal data seen in Fig. 4b. There is a clear transition here to a linear behaviour (indicated by the dotted line) and at a stress of ca. 14 GPa the openstructured glass compresses and assumes the same trajectory as that of crystalline quartz. Interestingly, both diamond anvil and shock compression experiments on quartz and glass have shown changes in refractive index and in the Poisson’s ratio as pressure increases, and these appear to saturate at ca. 14 GPa [108, 111,112,113,114,115]. At this value, densification processes are complete in the open structured glass as verified by several independent classes of measurement and both SL and quartz share the same values of c_{0}, S and of course the same Poisson’s ratio (that of the quartz). Calculating the value of the WSL for both silicates in the manner indicated above shows a common value of 14 GPa. Of course, whilst Poisson’s ratio has changed for the open structured glass as pressure has increased, this will also occur beyond the WSL. This behaviour has analogies for all classes of metal, brittle and covalent materials loaded by shock as the reader will appreciate [79, 116,117,118,119,120,121,122].
An analogous behaviour is observed in aluminas and sapphire as their strength evolves while impact stress increases. Figure 5a shows the unit cell with assignments of key structural planes and normal directions. Loading down the c direction has the greatest resistance to shear whilst that down r or n planes (which are ca. 60° to the c axis) shows the lowest. At first yield, it has been noted that single crystal sapphire (density 3.989 g cm^{−3}) shows HELs in the range 12–21 GPa [54]. The response to shock down seven directions of the αalumina unit cell has been studied by Kanel et al. who noted the complex evolution of the loading history of the material and the steadiness of the wave up to 86 GPa [121]. The behaviour in this regime is dominated by unsteady waves and elastic precursor decay evident down all loading directions. Like the glass described above, the elastic front does not settle to a steady value for some run distance, which suggests that shear strength is developing in this region as suggested previously by Duvall [125]. The alumina AD995 shows composite behaviour. The quoted value for the HEL (6.7 GPa) represents a lower limit for plasticity within favourably oriented crystals down the r direction and twinning is observed in some grains of the shockrecovered composite microstructure above this stress level as noted above [55].
The shock velocityparticle velocity data illustrate the change in behaviour at the upper limit of elastic behaviour—the WSL (Fig. 5b). Data is presented from a series of investigations of single crystal and (composite) alumina AD995 [98, 119, 123, 124]. The data presented follow a scatter of trajectories below the value of the WSL (U_{s} = c_{L} = 11.26 mm µs^{−1}). This corresponds to a WSL stress of 123 GPa calculated from (2). This scatter in values of the constant S reflects compressibility changes with pressure down the different loading directions which is manifested in the unsteady wave propagation discussed above. Above the WSL however the material is in a homogeneous state and settles to a single curve.
The measured strengths are shown in Fig. 5c and follow a monotonic rise until ca. 70 GPa [55, 119, 124]. Ultrasonic measurements and calculations of the shear modulus of αalumina down different directions give values between 145 and 175 GPa. These shear moduli reflect the unit cell, with the highest values for shock recorded for loading down the c axis [0001] but easier shear down planes down the r direction [\(1\stackrel{}{1}02\)]. The alumina AD995 again provides an interesting test case, containing a range of crystals arranged with random orientation to the applied shock. The measured strengths for AD995 rise from the measured elastic strength at the HEL of ca. 5 GPa to a peak of ca. 21 GPa [124]. This compares with the calculated value of the theoretical strength for the r direction of 23 GPa which, using (3), implies a WSL of 70 GPa (red symbol on figure). The theoretical strength in the c direction is 31 GPa at a WSL stress of ca. 123 GPa as seen above. Interestingly this lies in the range within which Urtiew observed shockcompressed sapphire to lose transparency in the infrared [126]. More recently, the electrical resistivity of shocked sapphire was found to begin to decrease significantly with increasing shock pressures above 130 GPa, which adds weight to these observations [127].
Discussion
The limit of elastic behaviour defines a point at which defects already present within a sample seed deformation during loading when further activated by a shock wave. In macroscopic experiments, this defines the stress threshold beyond which inelastic work is first possible. The loading impulse further determines the regions sampled and filters the mechanisms that can operate there. Strain rates of 10^{5}–10^{6} imply sampled volumes of tens of microns in dimension within the rising front. Typically, a 2 µs pulse loads a ca. 10 µm volume which cannot be released on the timescales of classical shock experiments and thus fixes uniaxial strain conditions at the macroscale at least.
The typical operating deformation mechanisms in inert materials include slip, fracture, twinning and martensitic phase transformation. The latter two processes occur quickly, with motion of only half an atomic spacing necessary to move planes past one another. Nonetheless they still result in fixed strain increments. To apply greater deformation to a material requires slip or fracture and these processes tend to operate more slowly and continue for as long as a driver is maintained. As stresses get higher, or the volume loaded in the rise of the pulse gets smaller, the theoretical strength of the material is approached. This can be seen in the experiments of Fig. 2 above. These observations suggest that the scale of the region in which loading is applied should be included into the constitutive description of the material explicitly if the observed behaviours are to be modelled with fidelity.
As loading pulses of higher amplitudes are applied, the theoretical strength is eventually exceeded, preexisting volume defects are closed, and work is done homogeneously nucleating dislocations and heating uniformly across the front. The transition to a homogeneous state, at the weak shock limit, requires all operating deformation mechanisms to complete within a single front. This may be seen directly in glasses (Fig. 4) where delay of inelastic processes at lower stresses accelerates into a single front at higher. Since failure processes can be simultaneously sensed and visualised, operating mechanisms can be identified. These observations in a range of materials where shock data exists, suggest that µ/2π is a good approximation for the unrelaxed theoretical strength and thus that this value is most applicable for estimating strength in this region during shock loading.
The HEL defines the lowest threshold for the strength of a material while the WSL defines the limiting stress for elastic behaviour. This transition not only fixes the ultimate strength of solids but stabilises the refractive index of glasses and, as seen above, controls transparency and conductivity thresholds [100, 111, 113]. By such investigations, the transition to homogeneous nucleation can be tracked using shock methods and this work suggests that the ultimate shear strength of new materials might be measured directly using this technique [48]. Finally, the front itself then obeys the SwegleGrady, fourth power relation, with the work done by the impulse, and the time taken to complete the processes operating, determining its extent [96, 101, 102, 128].
Closure
This review has highlighted the strength of solids across the weak and strong shock regimes and illustrated a critical threshold, the weak shock limit, that separates the two. This threshold divides inhomogeneous from homogeneous states behind a propagating shock. The following conclusions and inferences may be drawn.

(i)
In the weak shock regime, the nature of the driving impulse controls the critical length scales probed by the front and thus the defect distribution in the asreceived material fixes the response.

(ii)
Above the WSL, the shear component of the stress applied exceeds the theoretical strength of the material and inelasticity is homogeneously nucleated behind the front.

(iii)
The strength of a material rises from the Hugoniot elastic limit at the start of the weak shock regime to the theoretical strength at the HEL. Beyond the WSL the strength may plateau or, as pulse amplitudes increase, other phase changes such as melting may occur that change the state of the material (e.g. [129, 130]).

(iv)
The WSL is the longitudinal stress who’s shear component exceeds the theoretical strength, and that admits a regime of homogeneous flow behind the front. The methods outlined in this article can thus be used to infer the ultimate shear strength of solids.

(v)
Above the WSL, a range of further phenomena are observed such as luminescence, conductivity transitions, absorption, changes in transparency and stabilisation of the refractive index in transparent solids.

(vi)
The WSL may indicate the start of fourth power behaviour in shocked solid phase materials and this implies a constancy of energy and temporal duration through strong shock fronts [96].
Future Perspectives
The observations presented here suggest new frontiers exist at high pressure to explore extreme compressions. In the weak shock regime, better representations of the preexisting defect structures present in matter can be gained from 5D (positional, elemental, chemical) information, gleaned from new national facility diagnostics (through tomography, diffraction, spectroscopy) [131,132,133,134,135,136,137,138]. This will allow predictive, first principles modelling of the inhomogeneous states accessed in these materials (e.g. [131]) under more extreme conditions. Challenging problems, and the increased availability of extreme environments and advanced numerical techniques, make work in this area as exciting and important as ever.
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Acknowledgements
I would like to thank my children, Freya and Oliver who helped to gather and process so much of the data used here, to Zvi Rosenberg for inspiring my interest in strength in shocked brittle materials and to colleagues with whom I have discussed these concepts over the last years. I thank the reviewers and editors and particularly Dennis Grady for helpful comments that greatly improved the manuscript.
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