Salt crystallization is a major cause of weathering of rocks, artworks and monuments. Damage can only occur if crystals continue to grow in confinement, i.e. within the pore space of these materials, thus generating mechanical stress. We report the direct measurement, at the microscale, of the force exerted by growing alkali halide salt crystals while visualizing their spontaneous nucleation and growth. The experiments reveal the crucial role of the wetting films between the growing crystal and the confining walls for the development of the pressure. Our results suggest that the measured force originates from repulsion between the similarly charged confining wall and the salt crystal separated by a ~1.5 nm liquid film. Indeed, if the walls are made hydrophobic, no film is observed and no repulsive forces are detected. We also show that the magnitude of the induced pressure is system specific explaining why different salts lead to different amounts of damage to porous materials.
Salt weathering affects porous materials such as rock outcrops and minerals within the soil profile but also engineering structures monuments and artworks (Fig. 1). There is compelling evidence that its influence will increase due to global climate change1,2. Refs 1 and 2 underline the great importance of atmospheric moisture change as a threat to heritage, despite the fact that often only temperature is identified as the key aspect of climate change. The risk factors related to such a change include sea level rise, intense rainfall, flooding and changes in humidity cycles which can considerably amplify phase changes in freeze-thaw cycles and salt crystallization. In the case of sodium chloride contaminated stones, it has been also shown how humidity fluctuations (i.e. deliquescence followed by drying) induce the recrystallization of large NaCl crystals in the pores at the subsurface of the porous material leading to damage after several cycles3.
Moreover, changes in humidity affect also the growth of microorganisms in stone and wood2. Drier summers overall, for instance, may increase salt weathering of stone and desiccate the soils that protect archaeological remains and support the foundations of buildings. In this way, many ancient structures and historical artworks, such as the Valley of the Kings (Egypt), the Petra site (in southern Jordan) and a large number of frescos and sculptures have already been partially or even completely destroyed by salt attack4,5,6,7,8,9,10,11,12.
Arguments explaining that growing crystals can generate stresses have been given for more than 150 years ago, since Lavalle and subsequently Becker reported that a crystal can grow under external pressure13,14. They assumed that the crystal could grow and overcome the external forces provided the surface is in contact with supersaturated solution15,16,17,18. In its simplest form, the crystallization pressure Pcrystallization was approximated by the chemical potential difference between salt molecules in the crystal and in the supersaturated salt solution:
with ν the number of different ions, R the gas constant, T the temperature, Vm the molar volume of the solid phase and S the supersaturation, which is the ratio of the solute concentrations in the solution c and in the saturated solution cs16,17,18,19,20.
More formally, this requires an activity product K[P] greater than the solubility product at atmospheric pressure K, as described by Freundlich equation for a crystal under pressure . Although several such theoretical corrections have been made on this equation by taking into account the water activities and the size of the crystal17,19,20,21,22, it does not fully explain the different experimental results reported in literature, notably the very different weathering effect of different salts.
The direct measurement of the force exerted by a growing crystal in confinement is challenging, as illustrated by the small number of experimental results reported16,23,24,25,26. Previous studies consider the growth of a pre-existing crystal confined between two plates under a load and immersed in a salt solution. On the one hand, some evidence that a crystal under stress can grow has been reported25, in addition to a displacement of the wall due to crystal growth15,16 or a repulsive force between a crystal and a wall using AFM26. On the other hand, other groups have reported the dissolution of the loaded face and the growth of unloaded ones23,27: a crystal in a supersaturated solution can simply grow in a direction in which it is not confined and not exert a pressure. Therefore, the debate about the mechanism involved in the development of such a pressure continues.
We report experimental results obtained with an innovative setup which permits to visualize the spontaneous primary nucleation and growth during the evaporation of the salt solution while directly measuring the force exerted by a crystal during its growth in confinement. Here, we do not impose a certain supersaturation, or impose a given load; we rather measure the force that the growing crystal exerts with its spontaneous precipitation. This should be contrasted with earlier attempts to measure the pressure exerted during a secondary nucleation process (growth of pre-existing crystal), for which only very modest supersaturations were considered23.
Experimental Methods and Materials
Two alkali halides salts, sodium chloride (NaCl) and potassium chloride (KCl), are studied firstly because of their abundance and similar crystalline stucture (i.e. cubic rock-salt structure). The second incentive for this choice of materials is that recently in experiments on the evaporation of NaCl solutions it became clear that primary nucleation results in very high supersaturations S = c/cs ~ 1.6 ± 0.2 at the onset of crystallization28,29. As the exerted pressure scales with ln(S), these recent findings suggest a scenario in which the force exerted by a growing crystal should be more easily detected than in previous experiments.
Our experimental setup is as follows (Fig. 2). A very small drop (V0 ~ 0.2 μl) of the salt solution (NaCl or KCl) close to saturation (S = c/cs = 0.9, with , ) is deposited on a cleaned glass slide on an inverted microscope. The second glass slide that is used to confine the drop from above with a microscale gap is attached to a mechanical testing machine (a rheometer) that allows to (i) control and measure the gap between the plates, (ii) detect the normal force on the plate during the crystal growth and (iii) deduce the surface area of the salt crystal that is in contact with the plates. The latter is done by applying very small oscillations to the upper plate and measuring the resistance of the material between the two plates to a small shear force. In parallel, by direct visualization using a CCD camera coupled to the inverted optical microscope, we follow the evaporation of the entrapped salt solution and determine the volume change (knowing the diameter of the droplet and the gap between the two plates), the concentration at the onset of the crystal precipitation and visualize the crystal growth in the solution. Experiments are done at controlled relative humidities of 40% and 4%.
In our climatic chamber (Fig. 2), the relative humidity is fixed by controlling the partial vapor pressure Pw entering the set up chamber at the laboratory temperature T2 (21 °C)30. This is done by flowing air through water at a given temperature T1 using a water bath thermostat. Once this air flow arrives in the chamber at the temperature T2 (21 °C), the partial vapor pressure Pw(T2) will be then equal to the saturated vapor pressure at T1 and consequently the relative humidity of the chamber will be fixed as:
Thus, by changing T1, the relative humidity can be fixed to a desired value in the chamber very precisely (±2%).
Results and Interpretation
Once the salt solution is entrapped between the two glass plates, an attractive (negative) capillary force (F ~ −3.5 10−3 ± 1.0 10−3 N) is detected; the measured force is in good agreement with the calculated theoretical value by considering the gap distance, the surface tension of the salt solution and its contact angle with the glass plate31 (see Supplementary Information). Upon evaporation of the water, generally a single crystal is observed to form. In the first 5 seconds after its precipitation, the crystal size grows to fill the gap (50 μm) with a film of solution between the crystal faces and the glass plates (Fig. 3).
With the further growth of the crystal, we find that a strong repulsive (positive) force develops, increasing in time. A steep increase of the force is detected when there is no more solution around the sides of the crystal (i.e. no more lateral growth): the remaining salt solution is in the liquid film that is observed between the glass plates and the crystal. Its subsequent evaporation induces the formation of steps on the confined face of the crystal25 and the precipitation of small microcrystallites around the main crystal (‘efflorescence’)32,33 (Figs 3 and 4). For NaCl, the maximum value of the force ΔF ~ 0.03 ± 0.007 N is achieved when the remaining film of salt solution is thinner than the optical resolution of the microscope (Fig. 3).
In order to convert the measured force into a pressure, we measure the area of contact between the salt crystal and the glass plates using the rheometer (see Supplementary Information). The latter gives the shear modulus of any solid material that occupies the gap between the two plates, by measuring the shear stress necessary for a certain imposed deformation. The bulk salt solution is liquid and does not resist shear, whereas the salt crystal does34. For the evaluation of the area of contact, we use the apparent shear modulus at the end of drying experiments where no more water is left, because the mechanical behaviour of the very thin film between the crystal and the wall is less clear. An independent series of measurements at ~4% relative humidity (i.e. very dry air) show comparable results at the end of drying, showing that the results are not affected by e.g. capillary condensation in the gap between the crystal and the walls. The growth of the crystal is indeed observed to lead to a strong increase of the apparent shear modulus that increases in a similar fashion as the force, although more intermittently. For the experiment shown in Fig. 3, the contact area is A ~ 136 μm2; the total area of one of the crystal face is much larger, on the order of ~2–3 105 μm2. This then gives a crystallization pressure deduced from the measured force and contact area of about 220 ± 50 MPa for experiment in Fig. 3, a very large pressure that is comparable to the yield stress of NaCl35 and is sufficient to damage e.g., the sandstones of Fig. 136,37. It is difficult to compare this to earlier AFM measurements of such interactions26, since these were done on a different salt in contact with a different wall.
At the end of each drying experiment, the precipitated microcrystal is gently removed and analysed by SEM; it shows very complex microscale step architecture, in line with the obersvations of Fig. 3(e,f). Surprisingly, the height of the NaCl microcrystals is found to be around 120 ± 20 μm (Fig. 4), i.e. larger than the gap that was imposed between the two plates (~50 μm). This occurs because the confined crystal continues to grow and bends the thin microscope slide that confines it. This explains why a plateau is reached for the measured force at the end of drying; the growth of the micro crystal can be considered as a three point bending experiment. In this case, the estimated magnitude of the force required to make a deformation of about ~50 μm of the glass plate is about F ~ 0.026 N which is of the same order of magnitude as the value of the force achieved at the end of experiment (with with ; with L = 67 mm, E = 69 109 Pa for glass, the thickness of the glass slide is h = 0.9 mm and a crystal size b ~ 0.8 mm and a deformation S ~ 50 μm). These results obtained at the microscale confirm once again the arguments given at the beginning of the 20th century that a growing crystal in confinement can lift a load if the latter is in contact with a film of solution14,15.
The importance of thin liquid films for the crystallization pressure was already underlined theoretically15,16,17,18,19,20,21,22: in order for a crystallization pressure to develop, one needs to maintain a film of liquid by some repulsive forces between the crystal and the wall as this allows for continued crystal growth by the addition of extra ions to the crystal lattice. If a growing crystal fully bridges the gap between two confining walls, no crystallization pressure can be developed since no extra layers of salt can be added to give rise to such a pressure. Subsequently, we have performed the same experiment with glass plates that are made hydrophobic by a silanization treatment. Indeed, in this case, as the formation of a wetting film is prevented, no repulsive force is detected during growth within the experimental uncertainty (Fig. 3). These experimental results make DLVO-type thin-film forces an obvious candidate for the origin of the crystallization pressure21,38. The Van der Waals forces through a thin film of salt solution between a salt crystal and a glass surface are attractive and thus could not lead to a pressure pushing the two surfaces apart. A charge repulsion between the two surfaces, provided they have the same charge. If this were the case, the disjoining pressure Π(l) within a film of thickness l, pushing the two surfaces apart, would be of the (simplified) form Π(l) ~ A exp(−κl), with , σ the charge density at the surface, ε and ε0 the relative permittivity of the bulk and free space, respectively and the Debye screening length with [NaCl] the molar sodium chloride concentration38.
This suggests a rather strong variation of the pressure with the salt concentration in the solution. Indeed, performing a large number of experiments, a strong correlation is found between the measured pressure and the salt concentration in the solution around the crystal (Fig. 5a). We use the concentration in the solution at the onset of crystal precipitation because it is the one we can determine with the greatest accuracy; Moreover, the crystal reaches the gap in the first 5 seconds and itgrows only logarithmically slowly33, i.e. slower than the evaporation. Also due to the slowness of the diffusion of ions (DNa+ ~ 1.3 10−9 m2/s in water) over the typical time scale in the experiment (~1000s) there will be little exchange between the entrapped film and the remaining solution besides the crystal; the typical size of the reservoir is ~1 cm, whereas the diffusion length is at most a fraction of a mm.
As an independent check that the salt concentration in the liquid film entrapped between the crystal and the wall is indeed high and hence comparable to that at the onset of salt precipitation, we stop the experiment when the maximum force and maximum shear modulus are achieved but a thin liquid film is still visible under the microscope (t ~ 150 min); the concentration at the onset of precipitation was 1.4 in this experiment. The crystal is gently removed and after further drying the upper crystal face (i.e. confined face) is observed using scanning-electron microscopy (SEM). The microphotographs reveal the formation of large amount of tiny dendritic crystals (Fig. 4); these are characteristic of high supersaturation. Indeed such a kinetics of growth have been reported for supersatruation above 1.428.
Assuming, then, that the concentration in the film equals the supersaturation at the onset of crystallization, we can compare with the simplified model for an electrostatic repulsion. We find that the measured pressure as a function of the supersaturation closely follows the expression for the disjoining pressure Π(l) ~ A exp(−κl), with a constant film thickness l of about 1.5 nm (Fig. 5a). This value is again in very good agreement with the expected magnitude for such a film (l ~ 2 nm)21,38. This is perhaps surprising that this simple DLVO-type expression38, gives such a good description of our data; both non linear terms in the Poisson-Boltzman treatment of this problem could become important at these high saturations as well as non-DLVO forces such as hydration forces at distance lower than 1 nm26,39,40,41,42,43,44. This merits further discussion, but is beyond the scope of this paper.
The scenario of a repulsive force requires that the crystal/solution and the solution/glass interfaces carry a charge of identical sign. Although it is known that glass surfaces are charged negatively when in contact with water and a low concentration of salt45, it is less evident that this remains the case if they are in contact with a highly saturated salt solution46,47,48. Consequently, we have determined the surface charges in highly concentrated salt solutions (i.e. close to saturation) by measuring the adsorption of cationic (Methylene Blue/C16H18ClN3S, at 8.10−6 M) and anionic dye (Eosine Y/C20H6Br4Na2O5, at 1.2.10−5 M) onto glass and crystals surfaces in contact with a highly concentrated salt solution. Methylene blue adsorption is widely used for the determination of both surface areas and exchange capacities of clay minerals49. Using a UV/Vis-Spectrometer one can measure the decoloration of a dye solution due to the adsorption of the dye on the oppositely charged surfaces (in our case on the glass surface and salt crystals) and determine in this way the nature of the charge of a given surface and its charge density (see Supplementary Information). These experiments show that glass, NaCl and KCl are all negatively charged since they adsorb the cationic dye and thus allow for the development of a repulsive disjoining pressure (Fig. 5).
More quantitatively, these measurments allows to estimate the surface charge density σ at the silica surface in contact with water and both NaCl and KCl solutions (see Supplementary Information). In pure water we find σ ~ 0.22 C.m−2 in good agreement with reported values38. The surface charge density of glass decreases in contact with salt solutions: σ ~ 0.12 C.m−2 for NaCl and σ ~ 0.072 C.m−2 for KCl. The lower charge density for the KCl solution is probably due to the larger size of K+ (ionic radius of 1.33 Å) compared to Na+ (0.96 Å), which results in smaller hydrated radii. Due to a smaller radius, the K+ ions bind more easily to the negatively charged silica surface at high concentrations46. Since the surface charge features directly in the amplitude A of the disjoining pressure, one would anticipate a much smaller crystallization pressure for KCl compared to NaCl. Indeed, if we repeat the experiments of force measurements with KCl solution, we find much smaller repulsive force (F ~ 0.008 N); in a typical experiment at the end of drying the induce repulsive pressure is P ~ 30 ± 15 MPa - roughly an order of magnitude smaller than for NaCl, in line with the significantly smaller surface charge of KCl (Fig. 3). Reflecting these lower pressures we also find much less damage when we expose pieces of sandstone to multiple dissolution/drying cycles using a KCl solution compared to NaCl3. Unfortunately, the range of supersaturations achieved in the several experiments with KCl was very narrow (S = 1.22 ± 0.05), which does not allow us to plot the measured pressure as a function of different concentration for this case.
Thus, the dependence of the force on salt concentration, surface charge and wettability of the glass makes a strong point that the observed forces are due to the disjoining pressure of the thin liquid film between two charged surfaces. It is interesting to compare this disjoining pressure with the thermodynamic crystallization pressure17,20. The disjoining pressure opposes the contact between the crystal and the wall by sustaining the liquid film. It is only when the magnitude of the crystallization pressure reaches the disjoining pressure that the crystal is forced into the contact with the wall by disrupting this thin film. As discussed theoretically by Scherer21, the disjoining pressure sets therefore an upper bound to the crystallization pressure. Our experimental results show indeed that for NaCl, for a supersaturation of S ~1.5, the calculated crystallization pressure20 is on the order of 135 MPa, similar to the disjoining pressure measured here (150 MPa ± 50) at this supersaturation. This means that up to this supersaturation, because of higher disjoining pressure compare to the crystallization pressure, the liquid film is sustained. Therefore the crystal can grow and exerce a crystallization pressure exceeding the tensile strength of stones (sandstone ~0.9 MPa50); crystallization can thus induce damage in the stone. It should be noted that salt damage becomes more visible for sodium chloride after several cycles of changing the humidity, because with cycling the recrystallization induces the precipitation of larger crystals within the pores3 (i.e in confinement) rather than inducing efflorescence of small microcrystallites onto the surface of the porous material. Thus the weathering due to in-pore crystallization becomes more pronounced with increasing number of cycles.
In conclusion, we have performed a direct measurement of the pressure exerted by the spontaneous precipitation of a salt microcrystal during evaporation in a confinement similar to that found in porous materials The results obtained for the growth of KCl and NaCl crystals between hydrophilic and hydrophobic glass walls suggests that the pressure originates from a repulsive interaction between charged surfaces separated by the liquid film. The magnitude of the measured pressure can be very high. The subtle dependence of the generated stress on the wetting and the surface charge properties that we report can also explain the experimentally observed variability for different salts crystallizing in different materials16,23,24,25,26. Hydrophobic treatments such as water repellent or consolidant products have for instance been used in the past19,51,52,53; We show here experimentally how a hydrophobic treatment that supresses the surface charge and wetting film could in principle prevent the development of crystallization pressure when salt crystallizes in the pore space (i.e. confinement). Although such treatments might help to limit the adverse effects of salt crystallization in practice, they also might could have unintended consequences with regards to other weathering mechanisms. It is worthwhile to mention that such unintended effects are likely not due to the chemical treatment itself but rather to its heterogeneity. The efficiency of hydrophobic treatments strongly depends on the impregnation depth of the chemicals in the stone, which in turn affects the wetting properties of the porous materials and modify the flow of the liquid within the porous matrix28,53,54,55,56. A heterogeneous hydrophobic treatment can lead to the formation of entrapped liquid pockets in untreated hydrophilic regions in the porous materials and if salt crystallizes here this may lead to weathering. The understanding of the processes that are at the origin of alterations of porous artworks is of great importance for managing and preserving them for future generations.
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The authors declare no competing financial interests.
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Desarnaud, J., Bonn, D. & Shahidzadeh, N. The Pressure induced by salt crystallization in confinement. Sci Rep 6, 30856 (2016). https://doi.org/10.1038/srep30856
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