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It is obvious that polymerization at a certain depth is possible when the dye bleaches because the change of the depth of polymerization is controlled by the rate of the bleaching process [ 2, 3].
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Fig. 5. Temporal changes of the depth variation of (a) the void ratio ψ, (b) the melt pressure p′ in the conduit and (c) the volatile concentration in melt c. Figure 6 shows the spatio-temporal distribution of volcanic deformation caused by magma ascent.
The data on pulsatile displacements of the cornea and iris and the changes of the depth of the gap between them were retrieved from the sequences.
As described by Konnerth et al. (2006), the reduced elastic modulus (E r ) was calculated from the initial slope of the unloading curve and indentation creep (C IT ) was defined as the relative change of the indentation depth while the applied load is held constant.
Based on the SO2 fluxes and the gas compositions, the conduit magma convection is considered to be the gas supply mechanism at the Shinmoedake, and the degassing pressure changes are attributed to the change of depth of the convecting magma column top.
Based on the SO2 fluxes and the gas compositions, the conduit magma convection is considered as the gas supply mechanism at Shinmoedake, and the degassing pressure change is attributed to the change of depth of the convecting magma column top.
After any change of depth, the pressure of gases in the blood passing through the brain catches up with ambient pressure within a minute or two, which results in a delayed narcotic effect after descending to a new depth.
Analysis of read-depth is an effective method for CNV detection, relying on detection of changes in the depth of coverage across the genome as being indicative of changes in the underlying copy-number [ 23].
Therefore the variation of the volcanic gas composition can be caused by changes of the degassing depth in the shallow part of the conduit system at <500-m depth.
The results were interpreted in terms of changes in the depth of transition between successive horizons.
c The change of depth from the bottom to the surface is performed without problem.
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