streambed_conductance

streambed semipervious layer hydraulic conductivity [L/T].
Reeves et al. (2009) estimate this as the vertical hydraulic
conductivity of the aquifer (<code>Kv</code>; L/T), which is itself often estimated
as 10% of the horizontal hydraulic conductivity (<code>Kh*0.1</code>; L/T)

Kriv

streambed semipervious layer thickness [L]
Reeves et al. (2009) estimate this as the vertical distance from
the streambed to the top of the well screen, or the length of the
well screen, whichever is greater [L].

briv

Implementation of analytical models for estimating streamflow
depletion due to groundwater pumping, and other related tools. Functions
are broadly split into two groups: (1) analytical streamflow depletion
models, which estimate streamflow depletion for a single stream reach
resulting from groundwater pumping; and (2) depletion apportionment
equations, which distribute estimated streamflow depletion among multiple
stream reaches within a stream network. See Zipper et al. (2018) <doi:10.1029/2018WR022707>
for more information on depletion apportionment equations and Zipper et
al. (2019) <doi:10.1029/2018WR024403> for more information on analytical
depletion functions, which combine analytical models and depletion apportionment
equations.

Samuel C. Zipper

streamDepletr

Estimate Streamflow Depletion Due to Groundwater Pumping

Ben Kerr

Tom Gleeson

Qiang Li

Foundry Spatial Ltd. 

streambed_conductance function

<dl><dt>w</dt>
<dd>stream width [L]</dd>
<dt>Kriv</dt>
<dd>streambed semipervious layer hydraulic conductivity [L/T].
Reeves et al. (2009) estimate this as the vertical hydraulic
conductivity of the aquifer (<code>Kv</code>; L/T), which is itself often estimated
as 10% of the horizontal hydraulic conductivity (<code>Kh*0.1</code>; L/T)</dd>
<dt>briv</dt>
<dd>streambed semipervious layer thickness [L]
Reeves et al. (2009) estimate this as the vertical distance from
the streambed to the top of the well screen, or the length of the
well screen, whichever is greater [L].</dd></dl>

Arguments

Estimate streambed conductance. — streambed_conductance

<dl>

<dt>w</dt>
<dd>stream width [L]</dd>


<dt>Kriv</dt>
<dd>streambed semipervious layer hydraulic conductivity [L/T].
Reeves et al. (2009) estimate this as the vertical hydraulic
conductivity of the aquifer (<code>Kv</code>; L/T), which is itself often estimated
as 10% of the horizontal hydraulic conductivity (<code>Kh*0.1</code>; L/T)</dd>


<dt>briv</dt>
<dd>streambed semipervious layer thickness [L]
Reeves et al. (2009) estimate this as the vertical distance from
the streambed to the top of the well screen, or the length of the
well screen, whichever is greater [L].</dd>

</dl>

streambed_conductance: Estimate streambed conductance.

Description

Usage

Value

Arguments

References

Examples