Official Series Description


Lab Data Summary

Aggregate lab data for the PYWELL soil series. This aggregation is based on all pedons with a current taxon name of PYWELL, 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 PYWELL were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

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Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
4478P055778ID017012Pywell5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties48.0088882,-116.7375031

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the PYWELL 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 PYWELL 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 PYWELL 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 PYWELL 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 .

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.

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Click the image to view it full size.

Competing Series

Soil series competing with PYWELL 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 PYWELL 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 PYWELL 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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Click the image to view it full size.

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

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Click the image to view it full size.

Soil series sharing subgroup-level classification with PYWELL, 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 PYWELL 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
Pywell-DeVoignes complex, unprotected, undrained, 0 to 1 percent slopes1511152152846541jid60120021:24000
Pywell muck, protected, drained, 0 to 1 percent slopes1509011528452x6t2id60120021:24000
Pywell-DeVoignes complex, partially drained, 0 to 2 percent slopes200813152904543did60120021:24000
Pywell muck, unprotected, undrained, 0 to 1 percent slopes2015791529052x6t4id60120021:24000
Pywell-Hoodoo complex, 0 to 1 percent slopes427782152999546gid60419811:24000
Pywell muck, 0 to 1 percent slopes, occasionally flooded4110361529982x6t1id60419811:24000
Pywell muck, unprotected, undrained, 0 to 1 percent slopes75986453402x6t4id60419811:24000
Pywell muck, 0 to 2 percent slopes, frequently flooded159730794492x6szid60619761:24000
Pywell-Bellslake complex, 0 to 3 percent slopes8000482662933nvfhid60619761:24000
DeVoignes-Pywell complex, 0 to 1 percent slopes15836813898031hn6cid62020131:24000
Pywell muck, protected, partially drained, 0 to 1 percent slopes1503113897942x6t3id62020131:24000
Pywell-Hoodoo complex, 0 to 1 percent slopes546g3812936680546gid6701:24000
Pywell muck2nnw2029366432nnwid6701:24000
Pywell-DeVoignes complex, partially drained, 0 to 2 percent slopes543d162936705543did6701:24000
Pywell muck, unprotected, undrained, 0 to 1 percent slopes543f112936738543fid6701:24000
Pywell-DeVoignes complex, unprotected, undrained, 0 to 1 percent slopes541j112936762541jid6701:24000
Pywell-Devoignes complex, partially drained, 0 to 2 percent slopes200A30699232rglwmt63419881:24000
Pywell-Bellslake complex, 0 to 3 percent slopes80002444621224nvfhwa06320121:24000
Pywell muck, 0 to 3 percent slopes, ponded1047011583112x6t0wa65119811:24000
Pywell-Bellslake complex, 0 to 3 percent slopes8000352651259nvfhwa65119811:24000

Map of Series Extent

Approximate geographic distribution of the PYWELL 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 .