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Exact(1)
The solution to Eq. (2) for the initial condition (4) is given (Carslaw and Jaeger, 1959, p. 259) by (5) for z ≪ a, z = a -r being the depth from the core surface.
Similar(59)
The vertical axis is the depth from the sea level.
The hydrostatic stress is calculated using Eq. 12, where ρ is the density of water at 20 °C (1000 kg/m3), and h is the depth from which the sample was recovered.
This is the depth from the wall to the counter or past the counter.
Furthermore, s D (h, t) is the depth wavelet coefficient from the frame F t) at the location h.
CSF-A is the depth (m) drilled from the sea floor regardless of potential gaps and overlaps between cores.
For Eq. (6), h is the depth of the cover, that is, the depth measured from the surface to the point of interest; K varies between 0.4 and 1.5 for depths below 1000 m (Eshiet and Sheng 2013).
These differences are to be expected considering the depths from which the samples were taken.
His lens is looking down into the depth, from which a light bounces back.
The depth of the source level z is, according to our consideration, the depth from which the ejecta trajectories separate from each other, which means it can be considered as the depth from which the eruption column starts to expand.
"There's no depth from the proscenium to the cyclorama," she said.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com