Residual Saturation
Residual Saturation - Related Videos
01:59
Solution Equilibrium and Saturation
0 Views •
2020
Imagine adding a small amount of sugar to a glass of water, stirring until all the sugar has dissolved, and then adding a bit more. You can repeat this process until the sugar concentration of the solution reaches its natural limit, a limit determined primarily by the relative strengths of the solute-solute, solute-solvent, and solvent-solvent attractive forces. You can be certain that you have reached this limit because, no matter how long you stir the solution, undissolved sugar remains. The...
01:26
Residual Stresses
0 Views •
2024
Residual stresses reside in a structure even after removing the original stress inducer. This phenomenon often arises from varied plastic deformations across different parts of a structure. Consider a rod stretched beyond its yield point. It will not regain its original length due to permanent deformation. Even after load removal, the rod does not entirely lose stress because of uneven plastic deformations, resulting in residual stresses. The computation of these stresses in structures is...
01:07
Residual Plots
0 Views •
2023
A residual plot is a statistical representation of data used to analyze correlation and regression results. It helps verify the requirements for drawing specific conclusions about correlation and regression. To obtain the residual plot, first, the residual for each data value is calculated, which is simply the vertical distance between the observed and the predicted value obtained from the regression equation. When the residual values are plotted against the variable x, it is called a residual...
08:19
Patterning via Optical Saturable Transitions - Fabrication and Characterization
0 Views •
Cited by 1 •
2014
We report that the diffraction limit of conventional optical lithography can be overcome by exploiting the transitions of organic photochromic derivatives induced by their photoisomerization at low light intensities.1-3 This paper outlines our fabrication technique and two locking mechanisms, namely: dissolution of one photoisomer and electrochemical oxidation.
01:19
Special considerations while measuring oxygen saturation
0 Views •
2024
Assessing respiratory rate concurrently with pulse measurement is fundamental to patient care, providing valuable insights into the patient's respiratory function. The normal breathing rate for an adult usually falls within a normal range of 12 to 20 breaths per minute. Abnormal respiratory rates can signal underlying health conditions or the need for immediate intervention. Ensuring accuracy in vital sign recordings while prioritizing patient comfort and minimizing anxiety is important.
FAQs
Capillary forces can hold fluid within small or irregular pores after displacement begins. Interfacial tension at the boundary between fluids and the geometry of connected pore spaces promote the formation of disconnected regions. Once these regions lose continuity, an applied pressure gradient may no longer move them, increasing the amount of immobilized fluid.
Wettability influences how each fluid interacts with the surfaces of the porous medium and therefore affects where fluids remain during drainage or imbibition. Because surface preference changes the distribution of fluids within pore spaces, it also changes how readily regions become disconnected. Residual saturation consequently depends on the fluid, solid, and displacement conditions together.
Drainage and imbibition displace fluids in opposite directions, so they reorganize fluid regions differently within the pore network. Changes in capillary forces, interfacial tension, pore geometry, and wettability can alter which regions remain connected or become trapped. This means the retained-fluid outcome depends not only on the medium, but also on the displacement process.
Immobilization depends on whether capillary forces and interfacial tension can maintain disconnected fluid regions against the applied pressure gradient. Pore geometry and wettability also control the stability and distribution of those regions. When these effects prevent reconnection or movement, additional pressure may not produce further displacement, leaving residual saturation as an important flow-model parameter.
Engineers use residual saturation as a parameter describing the portion of pore volume that remains unavailable for further movement by the displaced fluid. Including it helps models represent the effects of trapped, disconnected regions rather than assuming complete displacement. More accurate values improve predictions of multiphase flow and support engineering decisions involving porous subsurface materials.
Estimation requires attention to the porous medium, the fluids involved, and the displacement history, including whether drainage or imbibition occurs. Engineers account for capillary forces, interfacial tension, pore geometry, and wettability because these controls determine fluid trapping. The resulting estimate can then be used to improve multiphase-flow models for the relevant system.
Residual saturation indicates how much displaced fluid may remain trapped in reservoir-rock pore spaces rather than continuing toward production pathways. This information helps engineers evaluate the limits of displacement and represent trapped fluids in recovery predictions. Better estimates support resource-extraction decisions by connecting pore-scale immobilization with expected multiphase-flow behavior.
In groundwater and soils, retained fluid affects predictions of contaminant transport through porous materials. In subsurface carbon dioxide storage, it helps engineers evaluate how much fluid may remain immobilized and how storage performance should be represented. Across these applications, improved estimates strengthen decisions about remediation and subsurface storage by refining multiphase-flow predictions.