Mantle Convection and Surface Expressions. Группа авторов

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СКАЧАТЬ 2.2, black symbols) appears to support higher differential stresses than Fp compositions (Merkel et al., 2002; Singh et al., 2004). In all Fp measurements except those of J.‐F. Lin et al. (2009) Fp exhibits a steep rise in differential stress with pressure as noted by Marquardt & Miyagi (2015). The reason for the discrepancy between the data of J.‐F. Lin et al. (2009) and the other measurements is not clear. There is one very low data point (brown cross) from Miyagi & Wenk (2016). This data point was collected immediately after conversion to Brg + Fp, and as the sample has not yet been deformed, this point is not reflective of a flow stress. By ~60 GPa differential stress values in Fp achieves similar values to those of Per. It is possible that differences between Per and Fp may be due to composition, but the effects of grain size on the yield strength should be explored. Singh et al. (2004) suggest a significant effect of grain size on the strength of Per but the difference in grain size – for example between Singh et al. (2004) and Marquardt & Miyagi (2015) – is not known, as recovered samples were not studied for microstructure (in the latter case, due to anvil failure).

Figure 2.2 Summary of high‐pressure differential stress measurements on periclase and ferropericlase. Measurements in periclase are in black and ferropericlase are in colored symbols.

      During higher‐temperature deformation at 1400 K (Figure 2.2, red open squares), the results of Immoor et al. (2018) show a similar steep trend with pressure, but the magnitude is lower than the room temperature experiments of Marquardt & Miyagi (2015). The results of Immoor et al. (2018) are also generally consistent with the results from Miyagi et al. (2013) (Figure 2.2, open circles), which used resistive heating and laser + resistive heating to achieve high temperatures in the DAC. Notably, all three of these studies used the same Fp sample. Data points from Miyagi et al. (2013) at ~775 K (Figure 2.2, yellow open circles) and ~1000 K (Figure 2.2, orange open circles) using resistive heating are very close to the values of Immoor et al. (2018). The ~2300 K data point using resistive + laser heating (Figure 2.2, red open circle) is slightly below the data of Immoor et al. (2018), but with overlapping error bars. One should note that the error bars on these data sets represent the range of lattice strains measured on various lattice planes, and large error bars are associated with the large plastic anisotropy of this phase.

      The data points of Girard et al. (2016) at ~ 2000 K (Figure 2.2, blue open diamonds) represent the only large volume experiment at these pressures. Only data collected after ~20 % strain was used for these data points, as this is where steady state stress levels are achieved. These data points lie far below the DAC measurements, and also have a greater separation from the measurements of Marquardt & Miyagi (2015) than the ~2300 K measurement of Miyagi et al. (2013). This difference may be due to lower strain rates in RDA, but may also be due to grain size and the fact that this sample was deformed as part of a two‐phase assemblage. There is additionally another low data point from Miyagi & Wenk (2016) that was annealed at ~1600 K for ~30 minutes (Figure 2.2, yellow cross). It is unsurprising that this point is low, as this is essentially a stress relaxation experiment.

      When comparing DAC experiments to DAC experiments, the results on Per (Merkel et al., 2002; Singh et al., 2004) are quite consistent. Aside from the data of J.‐F. Lin et al. (2009), room‐temperature results of Marquardt & Miyagi (2015), Miyagi et al. (2013) Miyagi & Wenk (2016), and Tommaseo et al. (2006) are all quite similar, particularly when considering compositional variations between these experiments. There is not an obvious trend for strength and composition. However, a low‐pressure deformation study by Long et al. (2006) found that Fp samples with high Fe contents (>50%) develop texture faster than samples with low Fe contents, indicating a weakening with high Fe content. The effects of Fe content, grain size, strain rate, and temperature still need to be systematically explored for Fp at mantle conditions.

       CaSiO3 Perovskite.

Flow strength measurements on major mantle silicates are even more limited than measurements on Fp. Two differential stress measurements in the DAC exist for Ca‐Pv. Shieh et al. (2004) used energy dispersive x‐ray diffraction to measure differential stress in Ca‐Pv to ~60 GPa (Figure 2.3, black open circles). Miyagi et al. (2009) used angle dispersive x‐ray diffraction to measure differential stresses to 49 GPa (Figure 2.3, black closed circles). There is a large discrepancy between these measurements, with the values of Miyagi et al. (2009) about twice as large as those of Shieh et al. (2004). In addition to potential differences in grain size, there are a couple possibilities for differences in strength measurements. Shieh et al. (2004) used a natural sample (unspecified composition), while Miyagi et al. (2009) used a synthetic starting material; thus, starting material composition could play a role. Perhaps a more likely explanation is the use of laser absorbers in these experiments. In the work of Shieh et al. (2004), Pt was mixed in the sample to use as a laser absorber. In contrast, in the work of Miyagi et al. (2009), amorphous boron was mixed with the sample. It is possible that presence of boron can artificially raise the strength of the sample through doping or pining at grain boundaries. In any case, if the values of Miyagi et al. (2009) are reflective of flow strength, then Ca‐Pv would have the highest room temperature flow strength of the major mantle silicates. However, if the measurements of Shieh et al. (2004) represent the true room temperature flow strength, then Ca‐Pv has a similar room temperature flow strength to Brg.

Figure 2.3 Summary of high‐pressure differential stress measurement on CaSiO₃ perovskite, bridgmanite and MgSiO₃ post‐perovskite. Measurements on CaSiO₃ perovskite are shown in black symbols, measurements on bridgmanite are shown in closed colored symbols, and measurements on MgSiO₃ post‐perovskite are shown with open colored symbols.

       Bridgmanite.

      Of the measurements on Brg, one measurement was made in the DAC on a presynthesized sample using ruby fluorescence and the pressure gradient technique (Meade & Jeanloz, 1990). Two measurements have been made in the DAC with angle dispersive diffraction on a presynthesized sample (Merkel et al., 2003) or samples synthesized in‐situ from enstatite, olivine, and ringwoodite (Miyagi & Wenk, 2016). All of these DAC experiments were performed at room temperature, aside from two data points from Miyagi & Wenk (2016) where samples were annealing at ~1600K for 30 minutes. Two studies using large volume apparatus have also been performed. Chen et al. (2002) performed stress relaxation experiments using a DIA type apparatus and determined stress levels from x‐ray line broadening. More recently, Girard et al. (2016) performed high shear strain experiments using СКАЧАТЬ