Ground flow formula (Water Overlay): Difference between revisions

Latest revision as of 13:29, 5 March 2024

Ground flow is different from surface flow, since it has to account for the slowdown and porousness of the medium. In general, horizontal ground flow is calculated using formulas described in Harbaugh 2005^[1]^[2]. However, when an aquifer is present, the Aquifer formula is applied.

It depends on the configuration of the HYDRAULIC_CONDUCTIVITY_WITH_THICKNESS attribute value in the Water Overlay what Hydraulic Conductivity formula is used:

A value $<=0$ means Hydraulic Conductivity without Thickness formula will be used.
A value $>0$ means Hydraulic Conductivity with Thickness formula will be used.

Hydraulic Conductivity without Thickness

Two adjacent cells, where ground water level of cell 1 is larger than cell 2.

The flow between the two cells is calculated as:

$\Delta w_{t}=w_{1,t}-w_{2,t}$

$B_{bb}=max(B_{1}-d_{b,1},B_{2}-d_{b,2})$

$A_{c,t}=\Delta x\cdot ({\bar {w_{t}}}-B_{bb})$

$K=min(K_{1},K_{2})$

$V_{K,t}={\frac {\Delta w\cdot K\cdot A_{c,t}}{\Delta x}}\cdot \Delta t$

where:

w_{n,t}

= The ground water level of cell

n

at time

t

.

B_{c}

= the datum height of the surface of cell c, set by the elevation or a Terrain elevation prequel.

d_{b,c}

= The ground bottom distance of the cell c, defined by a Bottom distance prequel or a general GROUND_BOTTOM_DISTANCE_M of the Water Overlay.

B_{bb}

= the datum height of the bottom boundary at the edge of interaction between the two cells.

K_{n}

= The hydraulic conductivity of the cell, defined in HYDRAULIC_CONDUCTIVITY_MD of the ground terrain.

A_{c,t}

= Area of conductance at time

t

.

\Delta w

= Ground water level difference at time

t

.

\Delta t

= Computational timestep in seconds.

\Delta x

= Size of grid cell.

{\bar {w_{t}}}

= Averaged ground water level at time

t

, based on water levels in ground, WATER_STORAGE_PERCENTAGE and potentially the surface water level, when the ground is filled to the top.

V_{K,t}

= The amount of water to be transported at time

t

between one cell and the other.

Hydraulic Conductivity with Thickness

The flow between the two cells is calculated as:

$\Delta w_{t}=w_{1,t}-w_{2,t}$

$KD=min(KD_{1},KD_{2})$

$V_{KD,t}={\frac {\Delta w\cdot KD\cdot \Delta x}{\Delta x}}\cdot \Delta t$

where:

w_{n,t}

= The ground water level of cell

n

at time

t

.

KD_{n}

= The hydraulic conductivity of the cell, multiplied with the thickness of the layer, defined in HYDRAULIC_CONDUCTIVITY_WITH_THICKNESS_MD of the ground terrain.

\Delta w

= Ground water level difference at time

t

.

\Delta t

= Computational timestep in seconds.

\Delta x

= Size of grid cell.

V_{KD,t}

= The amount of water to be transported at time

t

between one cell and the other.

Aquifer formula

When an aquifer is present, its hydraulic diffusivity is used to calculate the water flow.

Based on conditions being true, the calculated volume of water that is transported through the aquifer is calculated as:

V_{a,t}={\begin{cases}{\dfrac {\Delta w_{t}\cdot {KD}_{a}\cdot \Delta x}{\Delta x}}\cdot \Delta t&{\text{if }}w_{n,t}>z_{a}{\text{ and }}KD_{a}>0\\V_{K(D),t}&{\text{otherwise}}\end{cases}}

Where:

\Delta w_{t}

= Ground water level difference between the two adjacent cells at time

t

;

{KD}_{a}

= The AQUIFER_KD attribute of aquifer.

\Delta x

= Size of grid cell.

\Delta t

= Computational timestep in seconds.

w_{n,t}

= Ground water level in cell

n

at time

t

;

z_{a}

= the datum height of the aquifer at the cell.

V_{K(D),t}

= The calculated amount of water to be transported at time

t

between one cell and the other.

V_{a,t}

= Volume in

m^{3}

that flows between the two adjacent cells due to the aquifer at time

t

.

References

↑ Harbaugh, A.W., 2005, MODFLOW-2005, the U.S. Geological Survey modular ground-water model-the Ground-Water Flow Process: U.S. Geological Survey Techniques and Methods 6-A16, variously paginated.
↑ Langevin, C.D., Hughes, J.D., Banta, E.R., Niswonger, R.G., Panday, Sorab, and Provost, A.M. (2017) ∙ Documentation for the MODFLOW 6 Groundwater Flow Model: U.S. Geological Survey Techniques and Methods, book 6, chap. A55 ∙ p 31 ∙ found at: https://doi.org/10.3133/tm6A55 (last visited 2019-02-04)

Models

Surface • Ground • Rain • Evaporation • Infiltration • Elevation • Breach • Sewer • Storage • Tracer flow • Border • Order
Model formulas

Timestep • Season • Surface water level • Groundwater level
Flow formulas

Surface flow • Surface infiltration • Ground flow • Ground infiltration • Surface evaporation • Ground evaporation • Ground bottom flow
Hydraulic structure formulas

Culvert • Weir • Breach growth • Breach flow • Pump • Sewer Overflow • Inlet • Drainage
Related

Building attributes • Hydrological features • Hydraulic structures • Terrain attributes • Model attributes • Results • Simulation data

[Harbaugh-1] Harbaugh, A.W., 2005, MODFLOW-2005, the U.S. Geological Survey modular ground-water model-the Ground-Water Flow Process: U.S. Geological Survey Techniques and Methods 6-A16, variously paginated.

[Modflow-2] Langevin, C.D., Hughes, J.D., Banta, E.R., Niswonger, R.G., Panday, Sorab, and Provost, A.M. (2017) ∙ Documentation for the MODFLOW 6 Groundwater Flow Model: U.S. Geological Survey Techniques and Methods, book 6, chap. A55 ∙ p 31 ∙ found at: https://doi.org/10.3133/tm6A55 (last visited 2019-02-04)

[1]

[2]

@@ Line 1: / Line 1: @@
-Underground flow is different from surface flow, since it has to account for the slowdown and porousness of the medium. In general, horizontal underground flow is calculated using formulas described in Harbaugh 2005<ref name="Harbaugh"/><ref name="Modflow"/>. However, when an [[Hydraulic features (Water Overlay)#Aquifer|aquifer]] is present, the aquifer variant is applied.
+Ground flow is different from surface flow, since it has to account for the slowdown and porousness of the medium. In general, horizontal ground flow is calculated using formulas described in Harbaugh 2005<ref name="Harbaugh"/><ref name="Modflow"/>. However, when an [[Aquifer (Water_Overlay)|aquifer]] is present, the [[ground flow formula (Water Overlay)#Aquifer formula|Aquifer formula]] is applied.
-===Default horizontal flow===
+It depends on the configuration of the [[Hydraulic conductivity with thickness (Water Overlay)|HYDRAULIC_CONDUCTIVITY_WITH_THICKNESS]] attribute value in the [[Water Overlay]] what Hydraulic Conductivity formula is used:
-[[File:Undergroundflow.png|right|400px|thumb|Two adjacent cells, where underground water level of cell 1 is larger than cell 2.]]
+* A value <math><= 0</math> means [[Ground flow formula (Water Overlay)#Hydraulic Conductivity without Thickness|Hydraulic Conductivity without Thickness]] formula will be used.
+* A value <math>> 0</math> means [[Ground flow formula (Water Overlay)#Hydraulic Conductivity with Thickness|Hydraulic Conductivity with Thickness]] formula will be used.
+===Hydraulic Conductivity without Thickness===
+[[File:Undergroundflow2.png|right|400px|thumb|Two adjacent cells, where ground water level of cell 1 is larger than cell 2.]]
 The flow between the two cells is calculated as:
-: Δw = w<sub>1</sub> - w<sub>2</sub>
-: B<sub>ex</sub> = max ( B<sub>1</sub> , B<sub>2</sub> ) - D<sub>ground</sub>
+<math>\Delta w_t = w_{1,t} - w_{2,t}</math>
-: A<sub>c</sub> = Δx * ( w<sub>avg</sub> - B<sub>ex</sub> )
-: C = min(C<sub>1</sub> , C<sub>2</sub> )
+<math>B_{bb} = max ( B_{1}- d_{b,1} , B_{2}- d_{b,2} ) </math>
-: q = Δw * C * A<sub>c</sub> / Δx * Δt
+<math>A_{c,t} = \Delta x \cdot ( \bar{w_{t}} - B_{bb} )</math>
+<math>K = min(K_{1} , K_{2} )</math>
+<math>V_{K,t} = \frac{\Delta w \cdot K \cdot A_{c,t}}{ \Delta x} \cdot \Delta t</math>
 where:
-: w<sub>n</sub> = The underground water level of cell n.
+: <math>w_{n,t}</math> = The [[Groundwater level formula (Water Overlay)|ground water level]] of cell <math>n</math> at time <math>t</math>.
-: B<sub>n</sub> = The surface elevation of cell n.
+: <math>B_c</math> = the datum height of the surface of cell c, set by the [[Elevation (Water Overlay)|elevation]] or a [[Terrain elevation prequel (Water Overlay)|Terrain elevation prequel]].
-: C<sub>n</sub> = The ground conductance of cell n. For this we use the vertical infiltration speed.
+: <math>d_{b,c}</math> = The ground bottom distance of the cell c, defined by a [[Bottom distance prequel (Water Overlay)|Bottom distance prequel]] or a general [[Ground_bottom_distance_m_(Water_Overlay)|GROUND_BOTTOM_DISTANCE_M]] of the Water Overlay.
-: D<sub>ground</sub> = The configured [[Ground_bottom_distance_m_(Water_Overlay)|ground bottom distance]].
+: <math>B_{bb}</math> = the datum height of the bottom boundary at the edge of interaction between the two cells.
-: A<sub>c</sub> = Area of conductance.
+: <math>K_n</math> = The hydraulic conductivity of the cell, defined in [[Terrain hydraulic conductivity md (Water Overlay)|HYDRAULIC_CONDUCTIVITY_MD]] of the ground terrain.
-: Δw = Underground water level difference.
+: <math>A_{c,t}</math> = Area of conductance at time <math>t</math>.
-: Δt = Computational timestep.
+: <math>\Delta w</math> = Ground water level difference at time <math>t</math>.
-: Δx = Size of grid cell.
+: <math>\Delta t</math> = Computational [[Timestep formula (Water Overlay)|timestep]] in seconds.
-: w<sub>avg</sub> = Averaged underground water level, based on water levels in underground, underground storage fraction and potentially the surface water level, when the underground is filled to the top.
+: <math>\Delta x</math> = Size of grid cell.
+: <math>\bar{w_{t}}</math> = Averaged ground water level at time <math>t</math>, based on water levels in ground, [[Terrain water storage percentage (Water Overlay)|WATER_STORAGE_PERCENTAGE]] and potentially the [[Surface water level formula (Water Overlay)|surface water level]], when the ground is filled to the top.
+: <math>V_{K,t}</math> = The amount of water to be transported at time <math>t</math> between one cell and the other.
+<br clear=both>
-===Aquifer formula===
+===Hydraulic Conductivity with Thickness===
-When an aquifer is present, its hydraulic diffusivity is used to calculate the water flow.
+The flow between the two cells is calculated as:
+<math>\Delta w_t = w_{1,t} - w_{2,t}</math>
-First, the hydraulic diffusivity dictates the fraction of the water height difference which will flow.
+<math>KD = min(KD_{1} , KD_{2} )</math>
-: ''F = 2 * sqrt( KD / WSP<sub>source</sub> ) * sqrt( Δt ) * ( 1 / cell )''
-Based on this fraction, the actual amount of water flow is calculated.
+<math>V_{KD,t} = \frac{\Delta w \cdot KD \cdot \Delta x }{ \Delta x} \cdot \Delta t</math>
-: ''Δw = ( (WL<sub>source</sub>/WSP<sub>source</sub>) - (WL<sub>target</sub>/WSP<sub>source</sub>) ) * F''
-Where:
+where:
-* Δw = The underground flow which takes place.
+: <math>w_{n,t}</math> = The [[Groundwater level formula (Water Overlay)|ground water level]] of cell <math>n</math> at time <math>t</math>.
-* Δt = Computational timestep.
+: <math>KD_n</math> = The hydraulic conductivity of the cell, multiplied with the thickness of the layer, defined in [[Terrain hydraulic conductivity with thickness md (Water Overlay)|HYDRAULIC_CONDUCTIVITY_WITH_THICKNESS_MD]] of the ground terrain.
-* cell = Cell size.
+: <math>\Delta w</math> = Ground water level difference at time <math>t</math>.
+: <math>\Delta t</math> = Computational [[Timestep formula (Water Overlay)|timestep]] in seconds.
+: <math>\Delta x</math> = Size of grid cell.
+: <math>V_{KD,t}</math> = The amount of water to be transported at time <math>t</math> between one cell and the other.
-* F = Fraction of water which flows between cells
+===Aquifer formula===
+When an [[Aquifer (Water_Overlay)|aquifer]] is present, its [[Aquifer kd (Water Overlay)|hydraulic diffusivity]] is used to calculate the water flow.
-* KD = The [[Aquifer kd (Water Overlay)|AQUIFER_KD]] attribute of aquifer.
+Based on conditions being true, the calculated volume of water that is transported through the aquifer is calculated as:
-* WSP<sub>source</sub> = The WATER_STORAGE_PERCENTAGE attribute of the underground terrain type of the origin cell.
+: <math>V_{a,t} =
-* WSP<sub>target</sub> = The WATER_STORAGE_PERCENTAGE attribute of the underground terrain type of the target cell.
+\begin{cases}
-* WL<sub>source</sub> = The amount of water in the saturated zone of the source cell. The height of the water column if the equivalent amount of water was placed on the surface.
+ \dfrac{ \Delta w_{t} \cdot {KD}_a \cdot \Delta x}{\Delta x} \cdot \Delta t & \text{if } w_{n,t} > z_a  \text{ and } KD_a > 0 \\
-* WL<sub>target</sub> = The amount of water in the saturated zone of the target cell. The height of the water column if the equivalent amount of water was placed on the surface.
+ V_{K(D),t}  & \text{otherwise}
+\end{cases}
+</math>
-==See also==
+Where:
-*[[Underground model (Water Overlay)#Horizontal flow and aquifers| Underground horizontal flow]]
+: <math>\Delta w_{t}</math> = Ground water level difference between the two adjacent cells at time <math>t</math>;
+: <math>{KD}_a</math> = The [[Aquifer kd (Water Overlay)|AQUIFER_KD]] attribute of aquifer.
+: <math>\Delta x</math> = Size of grid cell.
+: <math>\Delta t</math> = Computational [[Timestep formula (Water Overlay)|timestep]] in seconds.
+: <math>w_{n,t}</math> = Ground water level in cell <math>n</math> at time <math>t</math>;
+: <math>z_a</math> = [[Aquifer datum (Water Overlay)|the datum height of the aquifer]] at the cell.
+: <math>V_{K(D),t}</math> = The calculated amount of water to be transported at time <math>t</math> between one cell and the other.
+: <math>V_{a,t}</math> = Volume in <math>m^{3}</math> that flows between the two adjacent cells due to the aquifer at time <math>t</math>.
-==References==
+{{article end
+|related=
+The following topics are related to this formula.
+; Features
+: [[Aquifer (Water Overlay)]]
+; Formulas
+: [[Groundwater level formula (Water Overlay)]]
+: [[Ground infiltration formula (Water Overlay)]]
+; Models
+: [[Ground model (Water Overlay)]]
+: [[Infiltration model (Water Overlay)]]
+: [[Tracer flow model (Water Overlay)]]
+|seealso=
+* [[Ground model (Water Overlay)#Horizontal flow and aquifers| Ground model]]
+|references=
 <references>
 <ref name="Modflow">Langevin, C.D., Hughes, J.D., Banta, E.R., Niswonger, R.G., Panday, Sorab, and Provost, A.M. (2017) ∙ Documentation for the MODFLOW 6 Groundwater Flow Model: U.S. Geological Survey Techniques and Methods, book 6, chap. A55 ∙ p 31 ∙ found at:  https://doi.org/10.3133/tm6A55 (last visited 2019-02-04)</ref>
 <ref name="Harbaugh">Harbaugh, A.W., 2005, MODFLOW-2005, the U.S. Geological Survey modular ground-water model-the Ground-Water Flow Process: U.S. Geological Survey Techniques and Methods 6-A16, variously paginated.</ref>
 </references>
-{{Template:WaterOverlay_nav}}
+}}
+{{WaterOverlay formula nav}}

Ground flow formula (Water Overlay): Difference between revisions

Latest revision as of 13:29, 5 March 2024

Contents

Hydraulic Conductivity without Thickness

Hydraulic Conductivity with Thickness

Aquifer formula

Related

See also

References

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Ground flow formula (Water Overlay): Difference between revisions

Latest revision as of 13:29, 5 March 2024

Hydraulic Conductivity without Thickness

Hydraulic Conductivity with Thickness

Aquifer formula

Related

See also

References

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