Official Series Description


Lab Data Summary

Aggregate lab data for the URANDA soil series. This aggregation is based on all pedons with a current taxon name of URANDA, and applied along 1-cm thick depth slices. Solid lines are the slice-wise median, bounded on either side by the interval defined by the slice-wise 5th and 95th percentiles. The median is the value that splits the data in half. Five percent of the data are less than the 5th percentile, and five percent of the data are greater than the 95th percentile. Values along the right hand side y-axis describe the proportion of pedon data that contribute to aggregate values at this depth. For example, a value of "90%" at 25cm means that 90% of the pedons correlated to URANDA were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

There are insufficient data to create the lab data summary figure.


Water Balance

Monthly water balance estimated using a leaky-bucket style model for the URANDA soil series. Monthly precipitation (PPT) and potential evapotranspiration (PET) have been estimated from the 50th percentile of gridded values (PRISM 1981-2010) overlapping with the extent of SSURGO map units containing each series as a major component. Monthly PET values were estimated using the method of Thornthwaite (1948). These (and other) climatic parameters are calculated with each SSURGO refresh and provided by the fetchOSD function of the soilDB package. Representative water storage values (“AWC” in the figures) were derived from SSURGO by taking the 50th percentile of profile-total water storage (sum[awc_r * horizon thickness]) for each soil series. Note that this representation of “water storage” is based on the average ability of most plants to extract soil water between 15 bar (“permanent wilting point”) and 1/3 bar (“field capacity”) matric potential. Soil moisture state can be roughly interpreted as “dry” when storage is depleted, “moist” when storage is between 0mm and AWC, and “wet” when there is a surplus. Clearly there are a lot of assumptions baked into this kind of monthly water balance. This is still a work in progress.

Click the image to view it full size.



Click the image to view it full size.

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the URANDA series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

Click the image to view it full size.

Select annual climate data summaries for the URANDA series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

Click the image to view it full size.

Geomorphic description summaries for the URANDA series and siblings. Series are sorted according to hierarchical clustering of proportions and relative hydrologic position within an idealized landform (e.g. top to bottom). Most soil series (SSURGO components) are associated with a hillslope position and one or more landform-specific positions: hills, mountain slopes, terraces, and/or flats. Proportions can be interpreted as an aggregate representation of geomorphic membership. The values printed to the left (number of component records) and right (Shannon entropy) of stacked bars can be used to judge the reliability of trends. Small Shannon entropy values suggest relatively consistent geomorphic association, while larger values suggest lack thereof. Source: SSURGO component records .

Click the image to view it full size.

Click the image to view it full size.

There are insufficient data to create the 3D mountains figure.

Click the image to view it full size.

Click the image to view it full size.

Competing Series

Soil series competing with URANDA share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

Click the image to view it full size.

Select annual climate data summaries for the URANDA series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the URANDA series and competing. Series are sorted according to hierarchical clustering of proportions and relative hydrologic position within an idealized landform (e.g. top to bottom). Proportions can be interpreted as an aggregate representation of geomorphic membership. Most soil series (SSURGO components) are associated with a hillslope position and one or more landform-specific positions: hills, mountain slopes, terraces, and/or flats. The values printed to the left (number of component records) and right (Shannon entropy) of stacked bars can be used to judge the reliability of trends. Shannon entropy values close to 0 represent soil series with relatively consistent geomorphic association, while values close to 1 suggest lack thereof. Source: SSURGO component records .

There are insufficient data to create the 2D hillslope position figure.

There are insufficient data to create the 3D hills figure.

There are insufficient data to create the 3D mountains figure.

There are insufficient data to create the 3D terrace figure.

There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with URANDA, arranged according to family differentiae. Hovering over a series name will print full classification and a small sketch from the OSD. Source: snapshot of SC database .

Block Diagrams

No block diagrams are available.

Map Units

Map units containing URANDA as a major component. Limited to 250 records.

Map Unit Name Symbol Map Unit Area (ac) Map Unit Key National Map Unit Symbol Soil Survey Area Publication Date Map Scale
Uranda-Larson loams, 0 to 3 percent slopesF226A219325876592q3xnnd0051:12000
Larson-Uranda loams, 0 to 3 percent slopesF222A75525876142q3xgnd0051:12000
Larson-Uranda loams, 3 to 6 percent slopesF222B68925877292q3xhnd0051:12000
Uranda-Larson loams, 0 to 3 percent slopesG226A38125737002q4hjnd0051:12000
Larson-Uranda loams, 0 to 3 percent slopesG222A16825738102q4hpnd0051:12000
Larson-Uranda-Esmond loams, 6 to 15 percent slopesF223D14925877422q3xjnd0051:12000
Uranda-Larson loams, 0 to 3 percent slopesG226A169525762352q4hjnd0271:12000
Uranda-Larson loams, 0 to 3 percent slopesG226A313125764062q4hjnd03119901:20000
Larson-Uranda loams, 0 to 3 percent slopesG222A12725763992q4hpnd03119901:20000
Uranda-Larson loams, 0 to 3 percent slopesG226A133325765942q4hjnd03919911:24000
Uranda-Larson loams, 0 to 3 percent slopesF226A1925872192q3xnnd06919751:20000
Larson-Uranda loams, 3 to 6 percent slopesF222B1225872662q3xhnd06919751:20000
Uranda-Larson loams, 0 to 3 percent slopesG226A625822762q4hjnd06919751:20000
Larson-Uranda loams, 0 to 3 percent slopesF222A425871852q3xgnd06919751:20000
Uranda-Larson loams, 0 to 3 percent slopesF226A26125880762q3xnnd07919901:24000
Uranda-Larson loams, 0 to 3 percent slopesG226A245125819602q4hjnd08319901:20000
Larson-Uranda loams, 0 to 3 percent slopesG222A3325797362q4hpnd09119911:20000
Uranda-Larson loams, 0 to 3 percent slopesG226A1125813502q4hjnd09319901:24000
Uranda-Larson loams, 0 to 3 percent slopesG226A1834625796232q4hjnd10319661:12000
Larson-Uranda loams, 0 to 3 percent slopesG222A1373325796162q4hpnd10319661:12000

Map of Series Extent

Approximate geographic distribution of the URANDA soil series. To learn more about how this distribution was mapped, or to compare this soil series extent to others, use the Series Extent Explorer (SEE) application. Source: generalization of SSURGO geometry .