Description Usage Format Source References Examples
Location and average flow conditions for model boundaries in the major tributary canyons and upper part of the Wood River Valley, south-central Idaho.
1 |
An object of SpatialPolygonsDataFrame class containing a set of 22 Polygons and a data.frame with the following variable:
tributary name
minimum land-surface datum (elevation) along the transect, in meters above the North American Vertical Datum of 1988 (NAVD 88).
mean saturated thickness along the transect line, in meters; estimated as the distance between the estimated water table and bedrock elevations.
width of the tributary canyon, or length of the transect line, in meters.
land surface elevation gradient perpendicular to the cross-sectional transect line, a dimensionless quantity.
hydraulic conductivity in meters per day.
estimated saturated cross-sectional area, in square meters;
its geometry is represented as the lower-half of an ellipse with
width and height equal to TribWidth
and BdrkDepth
, respectively.
groundwater flow rate, in cubic meters per day, calculated using a Darcian analysis.
land-surface area defined by the basin above the cross-sectional transect line.
label that describes the relative basin size; where
"big"
indicates a basin area greater than 10 square miles (25.9 square kilometers), and
"small"
indicates a basin area that is less than this breakpoint value.
mean precipitation rate within the basin area, in meters per day.
mean precipitation flow rate, in cubic meters per day,
calculated by multiplying PrecipRate
by BasinArea
.
ratio of darcy flow rate to precipitation flow rate,
or DarcyFlow
divided by PrecipFlow
, a dimensionless quantity.
estimated average volumetric flow rate, in cubic meters per day.
Geographic coordinates are in units of meters, in conformance with the North American Datum of 1983 (NAD 83), and placed in the Idaho Transverse Mercator projection (IDTM).
U.S. Geological Survey, accessed on July 2, 2015;
a Keyhole Markup Language (KML) file created in
Google Earth with polygons drawn by hand in
areas of known specified flow boundaries.
Transect lines are defined by the polygon boundaries within the extent of
alluvium aquifer (see alluvium.extent
dataset).
The land surface gradient (LandGrad
) was estimated from the
land.surface
dataset.
Hydraulic conductivity (K
) is the average of two geometric means of hydraulic conductivity
in the unconfined aquifer taken from table 2 in Bartolino and Adkins (2012).
The U.S. Geologic Survey StreamStats tool
(Ries and others, 2004) was used to delineate the basin area (BasinArea
) and
estimate the precipitation rate (PrecipRate
).
See the appendix C. Package Dataset Creation for the R code used to calculate the
flow estimates (Flow
).
Bartolino, J.R., and Adkins, C.B., 2012, Hydrogeologic framework of the Wood River Valley aquifer system, south-central Idaho: U.S. Geological Survey Scientific Investigations Report 2012-5053, 46 p., available at https://pubs.usgs.gov/sir/2012/5053/.
Ries, K.G., Steeves, P.A., Coles, J.D., Rea, A.H., and Stewart, D.W., 2004, StreamStats–A U.S. Geological Survey web application for stream information: U.S. Geological Survey Fact Sheet FS-2004-3115, 4 p., available at https://pubs.er.usgs.gov/publication/fs20043115.
1 2 3 | sp::plot(tributaries, border = "red")
sp::plot(alluvium.extent, add = TRUE)
str(tributaries@data)
|
Add the following code to your website.
For more information on customizing the embed code, read Embedding Snippets.