1 Curved Capillary Barriers Making better use of gravity.

Slides:



Advertisements
Similar presentations
Gauss’s Law Electric Flux
Advertisements

Flood Profile Modeling with Split Flows and Weirs
1 Chapter 7 Length of flange Introduction As the bending moment decreases towards the support, the flange plate may be varied and a smaller flange.
Regional Processing Convolutional filters. Smoothing  Convolution can be used to achieve a variety of effects depending on the kernel.  Smoothing, or.
Example: Uniform Flow at Known Q and y
Distribution of Microcracks in Rocks Uniform As in igneous rocks where microcrack density is not related to local structures but rather to a pervasive.
Chapter 4- Leaky Aquifers
Creating a Chartres Labyrinth 11 Steps to reproducing your own Chartres Labyrinth.
Design of Highway Vertical Alignment Chapter 16
Copyright © Cengage Learning. All rights reserved. Conic Sections.
Limited Space and Mobile Antennas
Infiltration Infiltration is the process by which water penetrates from ground surface into the soil. Infiltration rate is governed by: rainfall rate hydraulic.
Fall 2008Physics 231Lecture 4-1 Capacitance and Dielectrics.
Chapter 8 Coordinate Systems.
1 Next adventure: The Flow of Water in the Vadose Zone The classic solutions for infiltration and evaporation of Green and Ampt, Bruce and Klute, and Gardner.
MECH 221 FLUID MECHANICS (Fall 06/07) Chapter 9: FLOWS IN PIPE
MECH 221 FLUID MECHANICS (Fall 06/07) Chapter 10: OPEN CHANNEL FLOWS
6.0 ELASTIC DEFLECTION OF BEAMS
Momentum Heat Mass Transfer
Montwood High School Physics R. Casao
Calculus and Analytic Geometry I Cloud County Community College Fall, 2012 Instructor: Timothy L. Warkentin.
Graphs. The results of an experiment are often used to plot a graph. A graph can be used to verify the relation between two variables and, at the same.
Stream Function Definitions
Body Waves and Ray Theory
CHAPTER 37 : INTERFERENCE OF LIGHT WAVES
Ways to express Bernoulli equation Energy per unit volume: Energy per unit mass: Energy per unit weight: - conservation of energy (no friction loss)
Urban Storm Drain Design: Typical urban roadway characteristics
7.1. Mean Shift Segmentation Idea of mean shift:
Isoquants, Isocosts and Cost Minimization
Slope of a Line Lesson 13.2 Pre-AP Geometry. Lesson Focus The purpose of this lesson is to introduce and study the slope of a line.
Section 17.2 Position, Velocity, and Acceleration.
Lecture Notes Applied Hydrogeology
Two Dimensional Hydraulic Fracture Simulations Using FRANC2D
Mass Transfer Coefficient
Unit 1, Chapter 2 Integrated Science. Unit One: Forces and Motion 2.1 Using a Scientific Model to Predict Speed 2.2 Position and Time 2.3 Acceleration.
DIFFERENTIAL EQUATIONS 10. DIFFERENTIAL EQUATIONS Unfortunately, it’s impossible to solve most differential equations in the sense of obtaining an explicit.
Also known as a dot that went for a walk..  Line defines shape and form. For example, look at this outline map.
Typical Mean Dynamic Balances in Estuaries Along-Estuary Component 1. Barotropic pressure gradient vs. friction Steady state, linear motion, no rotation,
Lecture 20 Ground Water (3) Ground water movement
CE 3354 Engineering Hydrology Lecture 21: Groundwater Hydrology Concepts – Part 1 1.
OC FLOW: ENERGY CONCEPTS, CHANNEL ANALYSIS
MECH 221 FLUID MECHANICS (Fall 06/07) Chapter 8: BOUNDARY LAYER FLOWS
Principles of Technology Physics
5.5 Non-uniform circular motion 5.6 Drag Velocity
11 -1 Chapter 12 On-Line Algorithms On-Line Algorithms On-line algorithms are used to solve on-line problems. The disk scheduling problem The requests.
Chapter 22 Electric Fields The Electric Field: The Electric Field is a vector field. The electric field, E, consists of a distribution of vectors,
Typical Mean Dynamic Balances in Estuaries Along-Estuary Component 1. Barotropic pressure gradient vs. friction Steady state, linear motion, no rotation,
PHY 151: Lecture 6A 6.1 Newton’s Law of Universal Gravity 6.2 Gravitational Formula 6.3 Extending Particle in Uniform Circular Motion Model.
1 George Washington Bridge 本章简要介绍索的特性和分析方法,主要包括索的特征、 索内力的变化、重力(竖向荷载作用下索的分析、广义索定 理以及确定索状拱的方法。与桁架相比,索只能承受轴向拉 力,内力单一,但必须形成一定的曲线才能承受不与索轴重 合的荷载,使其构成和分析独具特色。将索变形限定在较小.
Tom Wilson, Department of Geology and Geography Environmental and Exploration Geophysics I tom.h.wilson Department of Geology and.
Chapter 8: Internal Forced Convection
SACE Stage 2 Physics Circular Motion.
CHAPTER 3 SUB-SURFACE DRAINAGE THEORY
1. CHAPTER 3 SUB-SURFACE DRAINAGE THEORY ERNST EQUATION 2.
Arc Length & Surfaces of Revolution (7.4)
Since all points on the x-axis have a y-coordinate of 0, to find x-intercept, let y = 0 and solve for x Since all points on the y-axis have an x-coordinate.
Graphing Linear Equations
Pimpri Chinchwad Polytechnic, Nigdi.
Lecture 20 Ground Water (3) Ground water movement
Chapter 22 Electric Fields.
Next adventure: The Flow of Water in the Vadose Zone
9. Modelling linear relationships
Fig. P4.65, p.108.
Section 1.2 Straight Lines.
Limits and Continuity A BRIEF PREVIEW OF CALCULUS: TANGENT LINES AND THE LENGTH OF A CURVE 1.2 THE CONCEPT OF LIMIT 1.3 COMPUTATION OF LIMITS 1.4.
Graphing Linear Equations
Direction Fields and Euler's Method
Graphing Linear Equations
Geomath Geology Final Review - Part 2 tom.h.wilson
Presentation transcript:

1 Curved Capillary Barriers Making better use of gravity

2 The Idea: Use the gradient optimally  A capillary barrier under uniform application, the diverted flux increases linearly horizontally.  In the case of a barrier where the slope in the down dip direction is constant, first failure will always be near the down-dip end of the interface, while the upper portion of the interface could handle much more flow without local penetration.  if the slope were greater toward the down-dip portion, the diversion could be increased prior to breakthrough.  It would appear logical to increase the slope of the barrier in proportion to the expected local flux, which increases linearly with down-slope distance.  A capillary barrier under uniform application, the diverted flux increases linearly horizontally.  In the case of a barrier where the slope in the down dip direction is constant, first failure will always be near the down-dip end of the interface, while the upper portion of the interface could handle much more flow without local penetration.  if the slope were greater toward the down-dip portion, the diversion could be increased prior to breakthrough.  It would appear logical to increase the slope of the barrier in proportion to the expected local flux, which increases linearly with down-slope distance.

3 More on optimal use...  optimal use of the total fall in elevation is achieved when the break-through flux through the interface is constant along the entire length of the interface.  If we posit to have selected a barrier geometry such that this flux penetrates the barrier at all points, then  the pressure is also uniform along the textural interface.  the vertical moisture profile in the upper media is uniform  there will be no gradients in pressure in directions tangent to the interface.  Barrier parallel flux will be driven by gravitational potential, equal to the local slope of the interface.  optimal use of the total fall in elevation is achieved when the break-through flux through the interface is constant along the entire length of the interface.  If we posit to have selected a barrier geometry such that this flux penetrates the barrier at all points, then  the pressure is also uniform along the textural interface.  the vertical moisture profile in the upper media is uniform  there will be no gradients in pressure in directions tangent to the interface.  Barrier parallel flux will be driven by gravitational potential, equal to the local slope of the interface.

4  For a given location, the lateral rate of flow, Q, is given by:  T is the thickness of the interface,  K(z) is the hydraulic conductivity a distance z above the interface, and  S is the local slope of the interface.  Since the vertical moisture profile is identical at all locations, the integral is constant  For a given location, the lateral rate of flow, Q, is given by:  T is the thickness of the interface,  K(z) is the hydraulic conductivity a distance z above the interface, and  S is the local slope of the interface.  Since the vertical moisture profile is identical at all locations, the integral is constant So let’s do some math...

5 Two possible geometries

6 Linear Roof Solution  For a linear-roof design, Q = q x,  x = horizontal distance from crest  q = incident flux. But since Q = SC we immediately find that using the parameterization  Putting this into the governing eq. integrating:  use of a parabolic interface for linear-roof capillary barriers will provide optimal diversion.  For a linear-roof design, Q = q x,  x = horizontal distance from crest  q = incident flux. But since Q = SC we immediately find that using the parameterization  Putting this into the governing eq. integrating:  use of a parabolic interface for linear-roof capillary barriers will provide optimal diversion.

7 What does this buy us?  To estimate the improvement in barrier performance obtained using the curved interface, consider a barrier which has a total fall of H over a horizontal distance L.  For the straight barrier, we get a diversion capacity of CL/H  For a parabolic system we get a diversion of 2CL/H  The parabolic interface provides a factor of two increase in diversion capacity for a given total elevation loss.  To estimate the improvement in barrier performance obtained using the curved interface, consider a barrier which has a total fall of H over a horizontal distance L.  For the straight barrier, we get a diversion capacity of CL/H  For a parabolic system we get a diversion of 2CL/H  The parabolic interface provides a factor of two increase in diversion capacity for a given total elevation loss.

8 How about a circular cover?  It is straightforward to compute the optimum shape of a circular-roof diversion.  For any radial distance r from the peak, the total flux intercepted by the barrier will be  r 2 q  which transects a circumference with length 2  r.  The local lateral flow will be qr/2, which by comparison to the linear-roof, implies an optimal interface parameterized by z = r 2 q/C.  The slope should be half that of a linear-roof for any given distance from the crest.  It is straightforward to compute the optimum shape of a circular-roof diversion.  For any radial distance r from the peak, the total flux intercepted by the barrier will be  r 2 q  which transects a circumference with length 2  r.  The local lateral flow will be qr/2, which by comparison to the linear-roof, implies an optimal interface parameterized by z = r 2 q/C.  The slope should be half that of a linear-roof for any given distance from the crest.

9 Segmented changing slope  construction of a smoothly changing slope presents logistical difficulties.  Approximate by a series of n straight segments of equal horizontal extent and linearly increasing slope.  For a barrier with total horizontal extent H and total fall L, the slope of the most down-dip segment is  construction of a smoothly changing slope presents logistical difficulties.  Approximate by a series of n straight segments of equal horizontal extent and linearly increasing slope.  For a barrier with total horizontal extent H and total fall L, the slope of the most down-dip segment is

10 Expected Performance  In a segmented system, first leakage would occur at the lowest end of each segment simultaneously, since the diverted flux/slope ratio will be minimal and equal for all segments at these points.  Using 3 and 5 straight segments the diversion capacity is predicted to be at least 75% and 83% respectively of the diversion of a smoothly curved interface, demonstrating a rapid convergence to the optimal performance.  In a segmented system, first leakage would occur at the lowest end of each segment simultaneously, since the diverted flux/slope ratio will be minimal and equal for all segments at these points.  Using 3 and 5 straight segments the diversion capacity is predicted to be at least 75% and 83% respectively of the diversion of a smoothly curved interface, demonstrating a rapid convergence to the optimal performance.