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An eco-hydrological model that couples the dynamics of woody vegetation cover and deep soil moisture (typically with a depth interval of 30 150 cm) was used to investigate the effect of stochastic intensity and the intermittency of precipitation on soil moisture in this deep interval, which affects woody vegetation cover.
Depth-dependent flow and chemistry results for the UFA contrasted with the EA; the deep interval (a high-flow zone) had distinctly different chemistry relative to the other two sampled intervals (particularly under ambient conditions), with higher concentrations of nitrate, atrazine, and chloroform (Katz et al. 2007).
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The current study did not show this change as the available data do not cover deep intervals when compared with other parts of the basin.
The results imply that the rapid sedimentation had little effect on the deeper interval around 900 mbsf, at least in terms of temperature gradient.
A region of higher mass flux was identified in the deepest interval of the S SW section of the domain, indicating the possible location of a zone with greater contaminant mass.
Our forward model results indicate a range of UCS that is broadly consistent with empirical relations in the shallower zone, but lower than predicted by these relations for the deeper interval.
Analysis from both wireline and well data (mudlog) revealed that very high overpressure approaching lithostatic pressures are expected at deeper intervals between 13,000 ft and beyond.
At the deeper intervals, there is thickening of sediment package at the central section where reservoirs are also juxtaposed against shale.
One element of that approval was the decision to proceed with the Carbon Dioxide Injection Project on Barrow Island, whereby CO2 separated from the reservoir gas from the Gorgon and Jansz-Io fields will be injected into a deep sandstone interval beneath Barrow Island.
Orthoconic nautiloids occur in a comparatively fossil poor deep water interval of the lower Šárka Formation with dominant pelagic organisms such as graptoloids and phyllocarids [20].
This linearity resulted in inconsistent heat flow between shallow (40 mW/m2; Expedition 315 Scientists 2009) and deep (56 mW/m2) intervals because of increased thermal conductivity at depth.
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