Sentence examples for condition of fluid from inspiring English sources

The gray square indicates the P-T condition of fluid inclusions at locality W1 estimated by Lewis and Byrne (2003).

This performance indicates that gel with a certain extent of strength can be achieved under the condition of fluid flow.

The classical boundary condition of fluid dynamics, i.e. the no-slip condition is violated during the flow of various complex fluids including polymer melts and polymeric suspensions.

The design of the device relies on condition of fluid flow and beam shaping for realization of adjustable 3D optical traps, which is achieved by means of a holographic optical trapping device.

This is because for any change in the reservoir geometry or any change in the condition of fluid flow (e.g., transient, late transient, semi-steady state or steady state) a new analytic expression needs to be developed.

The DEM model that was used in this study is observed to be independent of reservoir geometry as well as the condition of fluid flow since it was shown that it worked for both linear and radial flow without modification.

The newly developed model combines rock properties, fluid properties, rock-fluid properties and also dynamic conditions of fluid flowing into the shaly sandstone porous medium.

This letter addresses how electromagnetic and seismic methods complement each other to help define the storage conditions of fluid processes in subduction.

However, as a result of the nonlinear free surface boundary conditions of fluid sloshing in a two-dimensional rectangular container, a closed-form solution describing the response behaviour is unavailable.

The DEM based model proposed in this study is appeared to be unique in nature with capability to be used for any reservoir with higher degrees of complexity associated with the shape and geometry of its porous media, conditions of fluid flow, as well as initial and boundary conditions.

Based on this assumption, we can imagine the path of a geofluid as follows; the geofluid moves up accompanying DLF earthquakes and accumulates in the middle crust, forming geofluid reservoirs; then, the geofluid moves further up towards the seismogenic zone, if the conditions of fluid migration are fulfilled.