Substrate digestibility throughout the depth profile of the sheet can be compared as the weight-adjusted conversion efficiency to CO2 gas.
The corresponding limits on the distance and optical depth of the dust sheet is 3.65 ± 1.05 pc and 0.047 ± 0.006 respectively.
While the 2-mm depth of the soil sheet is 10 20 times the average diameter of an Arabidopsis root (between 100 and 200 microns [ Meijon et al., 2013]), we evaluated whether rhizotron-grown plants exhibited any obvious stress as a consequence of physical constriction.
Other agents such as metal based inks also lead to localised collagen degradation around inked areas throughout the depth of the parchment sheets [7].
Calculate the depth of the seat.
The measured SP signatures generated by these graphite sheets (Bigalke et al. 2004; Lehmann et al. 1998; Srivastava and Agarwal 2009; Stoll et al. 1995) can be inverted to extract information of some geologic significance such as depths, extensions in depth, and inclinations of the sheets.
Furthermore, this scheme alternatively formulates the forward problem (which is defined by a closed-form solution) in terms of the depth to the top of the sheet rather than in terms of the depth to its center.
It is essential that this condition be satisfied as (left (z - frac {a}{2}sin theta right)) amounts to the depth to the top of the sheet (Figure 1).
As an example, a negative value for the depth to the top of the sheet means that the sheet virtually extends into the air, which is geologically erroneous and unacceptable in this context (Sharma and Biswas 2013).
Sharma and Biswas (2013) formulated the forward solution (1) in terms of the depth to the center of the sheet (z) as Vleft x, z, a, k, thetaright) = k ; log frac{left[x^{2} + left z - frac{a}{2}sinthetaright)^{2} right]}{left[ (x-acostheta)^{2} + left z + frac{a}{2}sinthetaright)^{2} right]}, (2).
Formula (2) can be re-written equivalently in terms of the depth to the top (h) of the sheet rather than the depth to its center (z) as (Figure 1) Vleft x, h, a, k, thetaright) = k ; log frac{left[x^{2} + h^{2} right]}{left[ (x-acostheta)^{2} + left(h + asinthetaright)^{2} right]}.
