Sentence examples for shallower storage from inspiring English sources

Accordingly, we interpret these cycles as the result of successive movement of individual magma batches migrating upward from deeper to shallower storage systems located along a NE dipping conduit.

Contrary to this, including conservation of energy is heavier on computing time but is likely to be required for storage scenarios where the injectant stream is significantly different in temperature to the reservoir and most critically for shallower storage reservoirs where CO2 is close to its critical point.

The Schaulager (or viewing warehouse) houses its forward-looking permanent collection in an innovative form of shallow storage, uncrated and installed in closed rooms on several floors overlooking an atrium and the galleries below.

This indicates a relatively short residence time of this magma in shallow storage below what would become the site of Surtsey Volcano - short enough to preclude significant closed-system crystallization and/or differentiation.

No periods of deflation were observed in the GPS data after these events, and we believe the total volume of magma accumulated in this region, ~ 0.2 km3, remains in a shallow storage system beneath Akutan Volcano.

Shallow CO2 storage sites in the Northern North Sea and other regions that have been loaded by Quaternary ice sheets are likely to behave in a similar manner.

Sand dams are shallow groundwater storage systems, which are designed on the assumption of reduced evaporation as the water table falls.

By using fibre-optic-thermometers, nearly every requested spatial resolution can be achieved and easily be adjusted to the needs of actual test sites for shallow geothermal storage exploration.

By contrast, since gravity changes mainly reflect annually varying shallow water storage as discussed in Hydrology (e.g., Wahr et al. 2004), we expect another relation between earthquakes and gravity changes: some shallow earthquakes may be triggered by water movement around the surface (e.g., Bettinelli et al. 2008; Johnson et al. 2017).

Therefore, we assume that the Aso-N·C rupture bands could not have reached a depth of more than −2 or −3 km msl beneath Kusasenrigahama because rocks at this depth experience plastic deformation as a shallow magma storage region, which is not conducive for volcanic earthquakes (e.g., Japan Meteorological Agency 2013).

Finally, the established SWAT was used to estimate both shallow groundwater table fluctuation and shallow aquifer water storage change in time and space.