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The saturation n and quadrature conductivity p exponents tend to increase slightly with increasing water salinity when using a linear conductivity model.
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Here, we use a simple approach [20] by calculating the thermal conductivity at different tube lengths and then using a linear fitting according to the formula 1 κ p = a + b l.
Heterogeneity in the maximum conductivity of the slow delayed rectifier current (IKs) was introduced using a linear relation with the activation time in a previous simulation.
For biases below 0.60 V, were the inversion layer describing the n-type conductivity can be found, an electron concentration of 5.6 × 10 cm−3 was calculated using a linear fitting of the experimental points presented in Fig. 5b.
Conductivity was measured by using a Seven Excellence Conductivity Meter with a conductivity probe Inlab 731.
Electrolyte leakage from the leaf samples was evaluated by measuring ion conductivity using a conductivity meter (FE30, Mettler-Toledo Group, Switzerland).
Results are presented showing simulated reconstructions using a piecewise constant conductivity representation, and a (bi linear conductivity representation with C° continuity across conductivity elements.
This was done using a Jenway conductivity meter.
H2 consumption was recorded using a thermal conductivity detector (TCD).
Conductivity was measured by using a benchtop conductivity meter (Mettler-Toledo, USA).
The initial electrical conductivity (E1) was read using a FE30 conductivity meter (Mettler Toledo, Shanghai, China).
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