Official Series Description


Lab Data Summary

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

Soil series competing with SHAWA 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 SHAWA series and competing. 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 SHAWA 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 .

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Soil series sharing subgroup-level classification with SHAWA, 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 SHAWA 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
Shawa fine sandy loam, 3 to 9 percent slopesShC1142815956311qkczco02320091:24000
Shawa fine sandy loam, 0 to 3 percent slopesShA3778508489k23wco02320091:24000
Shawa loam, wet506100498621jqvkco63019751:24000
Shawa loam, 0 to 1 percent slopes482700498618jqvgco63019751:24000
Shawa loam, 1 to 3 percent slopes491400498619jqvhco63019751:24000
Shawa loam, 0 to 1 percent slopesSmA3884498682jqxjco63119721:24000
Shawa loam, 1 to 3 percent slopesSmB724498683jqxkco63119721:24000
Shawa loam, 0 to 4 percent slopes693880498504jqqsco63319811:24000
Shawa-Sandia family-Kolob family complex, 5 to 40 percent slopes1855545509551k374co66019941:24000
Shawa-Sandia family-Kolob family complex, 40 to 65 percent slopes1863062509552k375co66019941:24000
Shawa variant loam, 5 to 20 percent slopes612325583241ypfco66919821:24000
Shawa-Fughes complex, 30 to 60 percent slopes8062969507261k0v8co67220031:24000
Shawa-Fughes complex, 15 to 30 percent slopes8051210507260k0v7co67220031:24000
Shawa loam, 0 to 5 percent slopes12602737679srm3co67220031:24000
Shawa loam, 20 to 30 percent slopes725423507247k0ttco67220031:24000
Shawa loam, 5 to 20 percent slopes617169507218k0swco67220031:24000
Shawa loam, 3 to 20 percent slopes622465496726jnwfco68219861:24000
Shawa loam, 3 to 8 percent slopes805505497035jp6dco68519791:24000
Shawa loam, wet, 0 to 5 percent slopes812301497036jp6fco68519791:24000
Shawa loam, 1 to 3 percent slopes792233497033jp6bco68519791:24000
Shawa loam, 2 to 10 percent slopes1777416341842cgq5mt61319751:24000
Shawa loam, 10 to 20 percent slopes178807341843cgq6mt61319751:24000
Shawa-Farnuf-Castner complex, 4 to 25 percent slopes861D66541479244yxrmt63019911:24000
Shawa-Castner-Rock outcrop complex, 8 to 45 percent slopes161E52211477114ypwmt63019911:24000
Shawa loam, 2 to 8 percent slopes88B9911479314yxzmt63019911:24000
Shawa silty clay loam, 0 to 8 percent slopes522958348185cp9smt65519751:24000
Shawa clay loam, 0 to 3 percent slopesShB2138507892k1hmnm67019761:24000
Dula, frequently flooded-Shawa, moist complex, 0 to 4 percent slopesDuA28228862452tdjdnm67019761:24000
Dula, frequently flooded-Shawa, moist complex, 0 to 4 percent slopesDuA140327213712tdjdnm6721:24000
Shawa loam, moist, 0 to 8 percent slopesSwC89627214132sdjwnm6721:24000
Shawa clay loam, 0 to 3 percent slopesShB58327213542tl75nm6721:24000
Shawa loam, 0 to 1 percent slopesShA627702112v5q4nm6721:24000
Dula, frequently flooded-Shawa, moist complex, 0 to 4 percent slopesDuA20029344742tdjdnm6781:24000
Shawa loam, moist, 0 to 8 percent slopesSwC6829424642sdjwnm6781:24000
Chivers family-Villy-Shawa complex, 2 to 8 percent slopes15355024553132ndynut6421:63360
Shawa-Osote families association, 0 to 5 percent slopes2403334512444k67gut6461:24000
Sawdust-Shawa, calcareous families association, 2 to 8 percent slopes240A1004512443k67fut6461:24000

Map of Series Extent

Approximate geographic distribution of the SHAWA 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 .