SURFACE FORMS AND DEGRADATION

Một phần của tài liệu PHYSICAL TECHNIQUES IN THE STUDY OF ART, ARCHAEOLOGY AND CULTURAL HERITAGE VOLUME 2 (Trang 157 - 160)

Previously, we discussed the fact that aerosol size depended on its source (surf or white- caps), but as marine aerosols are hygroscopic, their size also depends on ambient RH.

Further, when an aerosol first breaks free of a wave, it has a seawater composition, and then it gradually equilibrates (and thus decreases in size). Thus, marine aerosols may take four forms (Cole et al., 2004b) – non-equilibrium, near-ocean aerosol (size range 6–300 mm), wet aerosol (3–150 mm), partially wet aerosol (1–60 mm) and dry aerosol (<1–20 mm) – depending on time of flight and ambient RH. These size ranges are based on aerosol mass or volume; mean sizes based on the number or the surface area of aerosols are much smaller. When these aerosols are deposited on a metal surface, a number of characteristic surface “forms” result from the surface–aerosol interaction (Cole et al., 2004b). These forms differ in the extent of retained salts, degree of surface alteration and in the forma- tion of corrosion nodules. For example, when a wet aerosol impacts on an aluminum surface (limited initial reactivity), a cluster of deposited salt crystals forms. These crystals have compositions of either NaCl, MgCl or CaSO4, indicating that the original seawater solutions have segregated. In contrast, if the same aerosol impacts on a galvanized steel surface, there will be strong oxide growth on the surface (predominately simonkolleite and gordaite), with the retention of a NaCl crystal on this oxide layer. Interestingly, rather than the clean crystal edges that are observed for the NaCl crystal formation on aluminum, the NaCl crystal on galvanized steel appears to blend into the underlying oxide. Further oxide formation tends to be favored at the grain boundaries and triple points on the galvanized surface (see Fig. 14).

Recent work by Cole et al. (2004c) investigated the phases that form when microliter saline drops were placed on zinc. This study demonstrated the variety of corrosion prod- ucts that may form, and highlighted the importance of mixed cation products in a situation where Na and Mg concentrations are several orders of magnitude higher than the Zn concentration generated by anodic activity. The study also highlighted that when dealing with microliter droplets, processes within the droplet (anodic and cathodic activity, mass transport and diffusion) can dramatically alter droplet chemistry and lead to corrosion products that would not be expected from the initial conditions.

The implications of these observations to the conservation of metallic objects are both direct and indirect. The study, of course, provides direct evidence for mechanisms of zinc corrosion in marine environments. It also reinforces that when considering objects exposed to marine conditions, consideration must be given to the size range of aerosols and to the chemistry of marine aerosol. Misleading results can be obtained if marine exposures are approximated with immersion or NaCl-only exposure. The unique dynamics of droplets are relevant not only to marine locations, but to all cases where corrosion is promoted by localized wetting or deposition of rain aerosol or hygroscopic particulates. Droplets with volumes in submicroliters can undergo significant changes in chemistry, unlike corrosion in immersed situations, and the chemical changes can either enhance or restrict corrosion.

Further, the studies indicate that the effectiveness of maintenance strategies will vary significantly with reactivity of the metal components of the object. For example, a strategy of frequent washing to decrease salt may have little effect on a very reactive metal such as zinc, since the degradation occurs immediately after the deposition of a marine aerosol, but it may be quite effective for aluminum objects where a significant number of cycles of hygroscopic wetting of deposited salts is required to induce damage.

7.2. Implications of pollutants to object degradation

In Fig. 15, the ion concentration in a droplet exposed to conditions of CO2at 400 ppm, SO2

from 20, 40, 75, 150 and 300 ppb and NH3at 20 ppb is given (Cole, 2000).

This examination of pollutant deposition and aqueous chemistry has a number of impli- cations to the conservation of metallic objects. Clearly, in the case of metallic objects Holistic Modeling of Gas and Aerosol Deposition and Degradation 149

Fig. 14. SEM micrograph showing increased activity between salts and a galvanized steel surface at grain boundaries and triple points.

located in the open, the implications are direct. In this case, the major implication is that a knowledge of the gaseous SOxmay not give a reliable measure of corrosivity. Deposition rates, which will depend highly on both rain and RH, and oxidants and catalysts (such as O3, H2O2 and Mn(II), Fe(III) and NO2), and any alkali precursors (e.g. ammonia), will control the pH of the resulting moisture films or drops.

In an interior environment, the possible deposition pathways for pollutants will be highly dependent on RH and on any hygroscopic particulates or aerosols. If RH is low and in the absence hygroscopic species, only direct gaseous deposition is possible. However, if the RH exceeds the deliquescent RH of particulates in the air or on metal surfaces, then pollutant deposition will be enhanced by the absorption of gaseous species into the aque- ous phases that form when the particulates wet. The deliquescent RH of some common salts are given in Table 6.

Fig. 15. Ion concentration as a function of gaseous SO2concentration and SO2:NH3ratio (from Cole, 2000).

20 40 75 100 150 200 300

HCO3 SO3

SO2 ppb H+ HSO3 10−3

10−4

10−5

10−6

10−7

10−8

Concentration, M/L

2−

An example where these factors may be in play is in the black spots on brass. It is observed that such black spots are favored by the presence of high RH and hygroscopic dust particles (Weichert et al., 2004). Further, SO2is readily absorbed into the aqueous phase (as indicated by its high HA). Thus, under these conditions, acidic sulfide- and sulfate-containing moisture phases are likely to form. The reaction of moist aerosols or surface droplets of such a composition with bronze could well lead to spotting, although the corrosion products likely to form would be chalcanthite (CuSO4.5H2O), antlerite (Cu3SO4(OH)4)) and brochantite (Cu4SO4(OH)6), rather than covellite (CuS).

Một phần của tài liệu PHYSICAL TECHNIQUES IN THE STUDY OF ART, ARCHAEOLOGY AND CULTURAL HERITAGE VOLUME 2 (Trang 157 - 160)

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