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Figure 11 | SpringerPlus

Figure 11

From: Geophysical assessments of renewable gas energy compressed in geologic pore storage reservoirs

Figure 11

ERT modelling results. (a) Input or true (ρtrue) models, (b, c, f, g) output resistivity (ρ ERT ) tomograms with rms-error, and (d, e, h, i) corresponding residual Δρ models with their average values. Inversion is conducted using constrains of incorporating ρ region (b-e) and boundaries (f-i). These inversions are conducted for synthetic borehole ERT data (contaminated with 0.6% simulation errors) before and after adding 3% random noise error. The low residuals (average <9%) reflect well the advantage of constraining of ERT inversions by the seismic mapping results for an accurate reconstruction of the gas phase of downward gradual desaturation. The vertical black dots mark the borehole electrodes and the continuous lines mark the interfaces.

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