Official Series Description


Lab Data Summary

Aggregate lab data for the UMBERLAND soil series. This aggregation is based on all pedons with a current taxon name of UMBERLAND, 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 UMBERLAND 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 UMBERLAND 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.

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Sibling Summary

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

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

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Geomorphic description summaries for the UMBERLAND 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 .

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

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Competing Series

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

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Select annual climate data summaries for the UMBERLAND series and competing. 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 UMBERLAND 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.

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Soil series sharing subgroup-level classification with UMBERLAND, 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 UMBERLAND 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
Umberland clay loamUM12210495659jms0nv62219721:24000
Umberland-Playas complexUR3802495661jms2nv62219721:24000
Yobe-Umberland complexYD2590495673jmsgnv62219721:24000
Umberland-Parran complexUN2578495660jms1nv62219721:24000
Dedmount-Umberland-Umberland, ponded association2451206476286hzm2nv76119881:24000
Sheffit-Umberland association94311336478537j1ypnv76619941:24000
Umberland association7617094478452j1vynv76619941:24000
Equis-Umberland-Duffer association7635428478454j1w0nv76619941:24000
Umberland-Wendane association7655172478456j1w2nv76619941:24000
Umberland-Playas association7625167478453j1vznv76619941:24000
Wendane-Logan-Umberland association16814857478682j23cnv76619941:24000
Umberland-Rubylake-Orupa association7642448478455j1w1nv76619941:24000
Umberland-Orupa association7671900478457j1w3nv76619941:24000
Boofuss-Wendane-Umberland association14411527478643j223nv76619941:24000
Umberland-Wendane association2605530479136j2l0nv76819851:63360
Gund-Umberland association44142654792732whlnnv76819851:63360
Wendane-Umberland association11414070479037j2gtnv76819851:63360
Umberland-Wendane-Ocala association2613790479138j2l2nv76819851:63360
Skullwak-Umberland-Wendane association6801785479295j2r4nv76819851:63360
Umberland silt loam, frequently flooded, 0 to 2 percent slopes262545479139j2l3nv76819851:63360
Umberland-Isolde association10904855476399hzqqnv77019951:24000
Parran-Umberland association13322477476436hzrxnv77019951:24000
Umberland-Ragtown association14438290477368j0qznv77119901:24000
Umberland silty clay loam, ponded14445642477369j0r0nv77119901:24000
Umberland-Benin association14423401477367j0qynv77119901:24000
Dedmount-Umberland association14013271477360j0qqnv77119901:24000
Umberland-Playas-Ragtown association14452562477370j0r1nv77119901:24000
Umberland-Dedmount association14472529477372j0r3nv77119901:24000
Ragtown-Umberland association11922081477311j0p4nv77119901:24000
Umberland association14461326477371j0r2nv77119901:24000
Umberland silty clay loam1440836477366j0qxnv77119901:24000
Skullwak-Umberland-Wendane association6806005479699j355nv77519851:24000
Umberland silty clay loam, ponded1110630479411j2vwnv77519851:24000
Gund-Umberland association4415954796782whlnnv77519851:24000

Map of Series Extent

Approximate geographic distribution of the UMBERLAND 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 .