Sarscape 5 1 Crack 16
here, we comment on the possibility of the first degassing models, which consist of gas efflux and degassing. we estimate that the gas efflux during the first degassing (0.064×106m3) was much smaller than that of the second degassing (0.26×106m3). it is necessary to consider the possibility that the second degassing had a state of disequilibrium between gas and liquid. this could lead to a state in which the local gas efflux (0.26×106m3) was reduced. however, the volume of the gas efflux during the second degassing is about 2×104m3. therefore, the volume of gas efflux during the second degassing cannot be ignored. this means that the gas efflux during the first degassing was at least two orders of magnitude smaller than the gas efflux observed during the second degassing.
the license was changed to deal with the fact that envi’s source code is now available under a gpl-like license, and not any of the other sources of rights from which the various components were developed. it was also updated to note that envi is not an ide (e.g. plcb, etc) and that its purpose is merely that of visualization and post-processing of seismic data in preparation for other tools. this statement is also included in the license agreement.
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we observed the phreatic eruption of the hakone volcano using dinsar. the comparison of the observations with the surface displacements induced by the formation of a preexisting open crack indicates that the open crack was formed by the intrusion of fluids from depth. the open crack could potentially play a role in the phreatic eruption of the hakone volcano.
the potential to predict and mitigate a large fissure eruption is an important challenge for scientists, and thus, we emphasize the possibility of identifying the preexisting open cracks in the subsurface and developing a strategy to avoid such situations in the future (fujiwara et al. 2006 ; konno and noda 2007 ). although large eruptions cannot be predicted in detail, the development of a method to determine potential open cracks and fissures is important to avoid such events. the formation of open cracks in the subsurface is a natural process, and it is also important to understand that the formation of open cracks is not necessarily related to eruptions. it is, however, difficult to predict whether the formation of open cracks is related to future eruptions or not. although we do not know the exact location of open cracks, a high-resolution radar image before the eruption and well-preserved fumarole fields surrounding the fissure eruption can be helpful in this regard.
we used the technique of sarmap for the initial processing of the data. the dinsar results are produced by image unwrapping and source modeling. we used a single crack model with a fixed horizon length, which was estimated from the surface displacement map from the first orbit (table 2 ; fig. 1 a, b). we extracted the displacement area and calculated the volume of the crack by varying the horizontal length of the crack from the initial model. the absolute value of the residuals of the derived volume change was less than 4cm (fig. 2 a, b). we then changed the horizontal length of the crack to 2m. the absolute value of the residuals of the derived volume change was also less than 4cm (fig. 2 a, b), suggesting that the horizontal length of the crack was less than 2m. the extracted model fit the observed ground displacements in the northeastern area (fig. 6 a, b), but it does not reproduce displacements in the middle area between the open crack and mount sounzan (fig. 5 c, d). we consider that the source model needs to be extended to include the middle area between the open crack and mount sounzan.