Official Series Description


Lab Data Summary

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

Click the image to view it full size.

Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
93A95P0479S1995MN137553PEQUAYWAN6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.2140007,-91.8964996

Water Balance

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

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

Click the image to view it full size.

Competing Series

Soil series competing with PEQUAYWAN 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 PEQUAYWAN 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 PEQUAYWAN 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 .

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.

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

Click the image to view it full size.

Soil series sharing subgroup-level classification with PEQUAYWAN, 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 PEQUAYWAN 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
Aldenlake-Pequaywan complex, 0 to 18 percent slopes, pittedF2-20D809227745472rn26mn03120131:24000
Aldenlake-Pequaywan complex, 0 to 8 percent slopes, pittedF2-20B260127745132rn25mn03120131:24000
Aldenlake-Pequaywan complex, 0 to 45 percent slopes, pittedF2-20F70627747042rn27mn03120131:24000
Aldenlake-Pequaywan complex, 0 to 6 percent slopesF2-14B50427744772rn20mn03120131:24000
Pequaywan fine sandy loam, 0 to 3 percent slopesF2-13A30227746312rn1zmn03120131:24000
Cloquet-Pequaywan complex, 0 to 18 percent slopes, pittedF10D202311484520h02mn03120131:24000
Rollins-Pequaywan complex, 0 to 8 percent slopes, pittedF1-30B3829437432rn1tmn03120131:24000
Aldenlake-Pequaywan complex, 0 to 18 percent slopes, pittedF2-20D783027422212yz7nmn07520131:24000
Rollins-Pequaywan complex, 0 to 18 percent slopes, pittedF1-30D313327422132yz7tmn07520131:24000
Aldenlake-Pequaywan complex, 0 to 45 percent slopes, pittedF2-20F285727422222rn27mn07520131:24000
Aldenlake-Pequaywan complex, 0 to 6 percent slopesF2-14B245027422172yz7mmn07520131:24000
Aldenlake-Pequaywan complex, 0 to 8 percent slopes, pittedF2-20B182127422202rn25mn07520131:24000
Pequaywan fine sandy loam, 0 to 3 percent slopesF2-13A142027422162yz7qmn07520131:24000
Rollins-Pequaywan complex, 0 to 45 percent slopes, pittedF1-30F138227422142yz7vmn07520131:24000
Cloquet-Pequaywan complex, 0 to 18 percent slopes, pittedF10D1340311496920h02mn07520131:24000
Rollins-Pequaywan complex, 0 to 8 percent slopes, pittedF1-30B114827422122yz7smn07520131:24000
Pequaywan loam, 0 to 3 percent slopesF19A4793114972wmdxmn07520131:24000
Cloquet-Pequaywan complex, 0 to 45 percent slopes, pittedF10E459311497020h03mn07520131:24000
Thistledew-Pequaywan complex, 2 to 12 percent slopesB281C252424079802ltpsmn61320161:24000
Cloquet-Pequaywan complex, 0 to 45 percent slopes, pittedF10E440251514420h03mn61320161:24000
Cloquet-Pequaywan complex, 0 to 18 percent slopes, pittedF10D297251514220h02mn61320161:24000
Pequaywan loam, 0 to 3 percent slopesF19A1302494001wmdxmn61320161:24000
Aldenlake-Pequaywan complex, pitted, 0 to 8 percent slopesF122B19150449631h2w7mn61520071:24000
Aldenlake-Pequaywan complex, pitted, 0 to 18 percent slopesF122D16585449632h2w8mn61520071:24000
Rollins-Pequaywan complex, pitted, 0 to 18 percent slopesF124D13219449637h2wfmn61520071:24000
Rollins-Pequaywan complex, pitted, 0 to 8 percent slopesF124B9044449636h2wdmn61520071:24000
Pequaywan fine sandy loam, 0 to 3 percent slopesF125A5298449639h2whmn61520071:24000
Rollins-Pequaywan complex, pitted, 0 to 45 percent slopesF124F3456449638h2wgmn61520071:24000
Aldenlake-Pequaywan complex, pitted, 0 to 45 percent slopesF122F2118449633h2w9mn61520071:24000
Aldenlake-Pequaywan complex, 0 to 6 percent slopesF118B1191449621h2vxmn61520071:24000
Cloquet-Pequaywan complex, 0 to 18 percent slopes, pittedF10D6721186145920h02mn61720071:24000
Cloquet-Pequaywan complex, 0 to 45 percent slopes, pittedF10E2420186146020h03mn61720071:24000
Aldenlake-Pequaywan complex, pitted, 0 to 8 percent slopesF122B22683072844h2w7mn61720071:24000
Aldenlake-Pequaywan complex, pitted, 0 to 18 percent slopesF122D13283072845h2w8mn61720071:24000
Rollins-Pequaywan complex, pitted, 0 to 8 percent slopesF124B10193072846h2wdmn61720071:24000
Pequaywan loam, 0 to 3 percent slopesF19A964186146920h0dmn61720071:24000
Rollins-Pequaywan complex, pitted, 0 to 18 percent slopesF124D4083072847h2wfmn61720071:24000
Rollins-Pequaywan complex, pitted, 0 to 45 percent slopesF124F3873072848h2wgmn61720071:24000
Pequaywan fine sandy loam, 0 to 3 percent slopesF125A3193072849h2whmn61720071:24000
Aldenlake-Pequaywan complex, pitted, 0 to 8 percent slopesF122B361217158351vlgjmn61920091:24000
Aldenlake-Pequaywan complex, pitted, 0 to 18 percent slopesF122D256617158361vlgkmn61920091:24000
Pequaywan fine sandy loam, 0 to 3 percent slopesF125A163317158431vlgsmn61920091:24000
Aldenlake-Pequaywan complex, 0 to 6 percent slopesF118B91817158251vlg6mn61920091:24000
Aldenlake-Pequaywan complex, pitted, 0 to 45 percent slopesF122F50917158371vlglmn61920091:24000
Rollins-Pequaywan complex, pitted, 0 to 18 percent slopesF124D31417158411vlgqmn61920091:24000
Rollins-Pequaywan complex, pitted, 0 to 8 percent slopesF124B17417158401vlgpmn61920091:24000
Rollins-Pequaywan complex, pitted, 0 to 45 percent slopesF124F15217158421vlgrmn61920091:24000
Cloquet-Pequaywan complex, pitted, 0 to 18 percent slopesF10D1131823025wmf6mn62120061:24000
Pequaywan loam, 0 to 3 percent slopesF19A424823016wmdxmn62120061:24000
Cloquet-Pequaywan complex, pitted, 0 to 45 percent slopesF10E167823072wmgqmn62120061:24000

Map of Series Extent

Approximate geographic distribution of the PEQUAYWAN 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 .