Official Series Description


Lab Data Summary

Aggregate lab data for the PURCHASE soil series. This aggregation is based on all pedons with a current taxon name of PURCHASE, 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 PURCHASE 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
134M87207011987MO207001Purchase3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.9945831,-89.959198

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the PURCHASE 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 PURCHASE 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 PURCHASE 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 PURCHASE 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 PURCHASE 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 PURCHASE 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 PURCHASE 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 PURCHASE, 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 PURCHASE 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
Purchase-Loring complex, 6 to 12 percent slopes, severely erodedPuC357158570645m4sxky08319951:12000
Purchase-Loring complex, 4 to 6 percent slopes, severely erodedPuB317368570644m4swky08319951:12000
Brandon-Purchase-Smithdale complex, 12 to 20 percent slopes, erodedBdD29939570618m4s1ky08319951:12000
Purchase silt loam, 12 to 20 percent slopes, severely erodedPrD38132570642m4stky08319951:12000
Purchase-Brandon complex, 6 to 12 percent slopes, severely erodedPsC33791570643m4svky08319951:12000
Providence-Purchase complex, 6 to 12 percent slopes, severely erodedPeC33339570639m4sqky08319951:12000
Loring-Purchase complex, 12 to 20 percent slopes, severely erodedLpD31020515973581qm5pky60219721:12000
Loring-Purchase complex, 6 to 12 percent slopes, severely erodedLpC31016015973571qm5nky60219721:12000
Grenada-Purchase complex, 6 to 12 percent slopes, severely erodedGsC3762615973511qm5gky60219721:12000
Grenada-Purchase complex, 4 to 6 percent slopes, severely erodedGsB3640215973501qm5fky60219721:12000
Purchase-Lax-Brandon complex, 6 to 12 percent slopes, severely erodedPlC33222622325942dy65ky61019681:12000
Brandon-Purchase-Lax complex, 12 to 20 percent slopes, severely erodedBpD32164026234362qyk6ky61019681:12000
Purchase-Lax-Brandon complex, 6 to 12 percent slopes, erodedPlC2828226234422qykhky61019681:12000
Lax-Purchase-Providence complex, 6 to 12 percent slopes, severely erodedLpC3471922325882dy5zky61019681:12000
Purchase-Loring complex, 6 to 12 percent slopes, severely erodedPuC3372722324342dy10ky61019681:12000
Purchase-Lax-Brandon complex, 4 to 6 percent slopes, severely erodedPlB3180726234382qyk7ky61019681:12000
Grenada-Purchase complex, 4 to 6 percent slopes, severely erodedGsB3156022323932dxzpky61019681:12000
Purchase-Loring complex, 4 to 6 percent slopes, severely erodedPuB39422324292dy0vky61019681:12000
Brandon-Purchase-Lax complex, 12 to 20 percent slopes, erodedBpD26226234352qyk5ky61019681:12000

Map of Series Extent

Approximate geographic distribution of the PURCHASE 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 .