Infiltration in porous media (soils)

0.0(0)
studied byStudied by 0 people
0.0(0)
full-widthCall Kai
learnLearn
examPractice Test
spaced repetitionSpaced Repetition
heart puzzleMatch
flashcardsFlashcards
GameKnowt Play
Card Sorting

1/16

encourage image

There's no tags or description

Looks like no tags are added yet.

Study Analytics
Name
Mastery
Learn
Test
Matching
Spaced

No study sessions yet.

17 Terms

1
New cards

What is a representative elementary volume? and what is the use

the bridge between microscopic and macroscopic diagram. allows us to define porous media properties at this scale

2
New cards

How do you calculate porosity (n)?

n = porosity = (volume of voids/sample volume)

3
New cards

What is water content?

water content (pheta) = volume of water/ sample volume

4
New cards

What is the degree of saturation (s)?

saturation (s) = water content (pheta)/ porosity (n)

where s is between 0 and 1

5
New cards

What is hydraulic conductivity K (m/s)?

permeability

= a measure of the ease with which a fluid can move through a porous material

6
New cards

What does hydraulic conductivity depend on?

  • soil type (sand, clay or gravel)

  • fluid used (water, oil, industrial fluids)

  • degree of saturation

7
New cards
<p>What is a capillary or matrix potential (cm) represented by phi?</p>

What is a capillary or matrix potential (cm) represented by phi?

a measure of the strength of attraction of water to the soil matrix

  • it is negative for unsaturated soils (as there is no water)

  • when it is positive it is known as capillary suction

<p>a measure of the strength of attraction of water to the soil matrix</p><ul><li><p>it is negative for unsaturated soils (as there is no water)</p></li><li><p>when it is positive it is known as <strong>capillary suction</strong></p></li></ul><p></p>
8
New cards

What is hydraulic head?

a measure of the total energy per unit weight of a liquid at a specific point, usually expressed as a height or length

<p><span><span>a measure of the total energy per unit weight of a liquid at a specific point, usually expressed as a height or length</span></span></p>
9
New cards

What is Darcy’s law?

the volumetric flow rate Q (m3/s) through a porous material

is proportional to the gradient in the hydraulic head h (m)

<p><span><span>the volumetric flow rate </span><em><span>Q</span></em><span> (m</span><sup><span>3</span></sup><span>/s) through a porous material</span></span></p><p style="text-align: left;"><span><span>is proportional to the gradient in the hydraulic head </span><em><span>h</span></em><span> (m)</span></span></p>
10
New cards

What is darcy flux (q)?

Darcy flux, specific discharge, Darcy velocity

            = flow per cross-sectional area

<p><span><span>Darcy flux, specific discharge, Darcy velocity</span></span></p><p style="text-align: left;"><span><span>&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp; = flow per cross-sectional area</span></span></p>
11
New cards

What is seepage velocity and how is it different to darcy flux?

q is not the actual water flow velocity as A includes the solid and pore space. 

As the water can only flow through the pores, the seepage velocity v (m/s) is v = q/n

so seepage velocity is the actual flow of water through the pores

<p><span><em><span>q</span></em><span> is not the actual water flow velocity as </span><em><span>A </span></em><span>includes the solid and pore space.&nbsp;</span></span></p><p style="text-align: left;"><span><span>As the water can only flow through the pores, the seepage velocity </span><em><span>v</span></em><span> (m/s) is v = q/n</span></span></p><p style="text-align: left;"></p><p style="text-align: left;"><span><span>so seepage velocity is the actual flow of water through the pores</span></span></p>
12
New cards

What are the different sections of the cross section of infiltrating water?

  • water

  • saturated zone

  • transmission zone

  • wetting zone

  • wetting front

<ul><li><p>water</p></li><li><p>saturated zone</p></li><li><p>transmission zone</p></li><li><p>wetting zone</p></li><li><p>wetting front</p></li></ul><p></p>
13
New cards

How can we achieve sustainable stormwater management?

through the use of low impact development (LID) also known as blue-green measures where we implement natural water management into our build environment

  • this includes green roofs, ponds, vegetated filter strip

  • they minimise imperviousness and maximise the use of pervious pavement and vegetation and contaminant source reduction

14
New cards

What is infiltration rate?

flow rate equal to the darcy flux at the surface of the water

<p>flow rate equal to the darcy flux at the surface of the water </p>
15
New cards

What happens when rainfall rate is greater than K_sat? (greater than the permeability)

q = rainfall rate up until ponding time

After this point, the hydraulic gradient at the surface has sufficiently

decreased so that the flow through soil can no longer match the rate

of rainfall it is receiving

16
New cards

what is ponding time?

the time it takes for water to begin accumulating on the soil surface, starting from the moment rainfall begins

17
New cards

What is Green & Ampt approximation?

an apporcimation for infiltration rate i through time

  • assumes rectangular flow so the cumulative infiltration (I) is the volume of water is calculated as a cuboid

  • when rainfall rate < K_sat

<p>an apporcimation for infiltration rate i through time</p><ul><li><p>assumes rectangular flow so the cumulative infiltration (I) is the volume of water is calculated as a cuboid</p></li><li><p>when rainfall rate &lt; K_sat</p></li></ul><p></p>