Official Series Description


Lab Data Summary

Aggregate lab data for the IPSON soil series. This aggregation is based on all pedons with a current taxon name of IPSON, 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 IPSON 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 IPSON 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 IPSON 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 IPSON 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 IPSON 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 IPSON 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 IPSON 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 IPSON 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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There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with IPSON, 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 IPSON 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
Ipson-Evanston complex, 6 to 30 percent slopes126386497625jptfco64419801:24000
Evanston-Ipson association, 3 to 20 percent slopes125253497624jptdco64419801:24000
Ipson-Trimad complex, 15 to 45 percent slopes12791497626jptgco64419801:24000
Ipson cobbly loam, 25 to 50 percent slopes572654497999jq6hco65519841:24000
Ipson cobbly loam, 3 to 25 percent slopes562318497998jq6gco65519841:24000
Eldgin-Ipson association, 8 to 25 percent slopes1254006483477j731ut6281:24000
Ipson-Secondledge complex, 15 to 50 percent slopes153195924227452tvd7ut6281:24000
Harol, very stony-Ipson association, 15 to 50 percent slopes1371640483619j77mut6281:24000
Ipson-Secondledge complex, 15 to 50 percent slopes1535544928102322tvd7ut6291:24000
Eldgin, very stony-Ipson, extremely stony association, 8 to 25 percent slopes.1251496125045282r80tut6291:24000
Harol, very stony-Ipson association, 15 to 50 percent slopes13741692958661j77mut6291:24000
Ipson cobbly loam, 8 to 25 percent slopes6912756504465jxy2ut63619841:24000
Ipson very cobbly loam, 25 to 60 percent slopes707608504467jxy4ut63619841:24000
Ipson very stony loam, dry, 5 to 25 percent slopes712746504468jxy5ut63619841:24000
Ipson family, 25 to 60 percent slopes, extremely stony171625258nzmmut6491:24000
Celeste family, rubbly-Ansari family, extremely stony-Ipson family, rubbly complex, 3 to 25 percent slopes230F2749791442vkkdut6511:24000
Ipson family, very stony-Waltershow family, extremely stony-Notter family, very stony complex, 8 to 25 percent slopes2652258791521vkmyut6511:24000
Evanston-Ipson complex, 0 to 20 percent slopes145260921045013hr0wy03119981:24000
Evanston-Ipson-Brownsto complex, 15 to 45 percent slopes146161021045023hr1wy03119981:24000
Rentsac-Brownsto-Ipson complex, 10 to 45 percent slopes21595581045713ht8wy03119981:24000
Ipson-Evanston complex, 6 to 30 percent slopes1703811044313hnrwy03119981:24000
Ipson-Evanston-Rock outcrop complex, 0 to 30 percent slopes1712651044323hnswy03119981:24000
Ipson-Evanston complex, 6 to 30 percent slopes1731168501714jv2bwy60119911:24000
Evanston-Ipson complex, 0 to 20 percent slopes2474615879981q9frwy60119911:24000
Ipson-Mantlemine-Beavwan complex, 3 to 8 percent slopes223231368502ypnlwy6291:24000
Ipson, very stony-Lolo-like, stony-Rock outcrop complex, 15 to 70 percent slopes751231709692z200wy6291:24000
Ipson-Evanston complex, 6 to 30 percent slopes1381030451049393j64wy72119941:24000
Ipson-Breece, dry-Evanston complex, 0 to 6 percent slopes137120191049383j63wy72119941:24000
Evanston-Ipson association, 3 to 20 percent slopes134108501049353j60wy72119941:24000
Ipson-Trimad complex, 15 to 45 percent slopes14178111049423j67wy72119941:24000
Ipson-Evanston-Rock outcrop complex, 0 to 30 percent slopes13958121049403j65wy72119941:24000
Ipson-Pinelli-Rock outcrop complex, 6 to 45 percent slopes14034991049413j66wy72119941:24000

Map of Series Extent

Approximate geographic distribution of the IPSON 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 .