Official Series Description


Lab Data Summary

Aggregate lab data for the CHEHULPUM soil series. This aggregation is based on all pedons with a current taxon name of CHEHULPUM, 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 CHEHULPUM 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 CHEHULPUM 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 CHEHULPUM 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 CHEHULPUM 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 CHEHULPUM 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 flats position figure.

Competing Series

Soil series competing with CHEHULPUM 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 CHEHULPUM 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 CHEHULPUM 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 CHEHULPUM, 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 CHEHULPUM 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
Goodin-Dupee-Chehulpum complex, 12 to 20 percent slopes73666610186ngyfor00320041:24000
Goodin-Dupee-Chehulpum complex, 2 to 12 percent slopes72423610185ngydor00320041:24000
Steiwer-Chehulpum complex, 12 to 30 percent slopes148134854282vwror00320041:24000
Steiwer-Chehulpum complex, 3 to 12 percent slopes14750854552vxmor00320041:24000
Steiwer-Chehulpum complex, 30 to 60 percent slopes14920854292vwsor00320041:24000
Chehulpum-Steiwer complex, 12 to 40 percent slopes16E27826230922tzor05319771:20000
Chehulpum silt loam, 3 to 12 percent slopes15C18476230722txor05319771:20000
Chehulpum silt loam, 12 to 40 percent slopes15E18026230822tyor05319771:20000
Steiwer-Chehulpum complex, 12 to 30 percent slopes2726E527111651j8btor05319771:20000
Steiwer-Chehulpum complex, 3 to 12 percent slopes2726C127111591j8bsor05319771:20000
Goodin-Dupee-Chehulpum complex, 2 to 12 percent slopes, eroded2765C108027113921j8c8or07119671:24000
Goodin-Dupee-Chehulpum complex, 12 to 20 percent slopes, eroded2765D80327113071j8c9or07119671:24000
Steiwer-Chehulpum complex, 12 to 30 percent slopes2726E68827114061j8btor07119671:24000
Steiwer-Chehulpum complex, 3 to 12 percent slopes2726C28427113531j8bsor07119671:24000
Steiwer-Chehulpum complex, hummocky, 20 to 60 percent slopes, stony2815F10827113642p8ttor07119671:24000
Steiwer-Chehulpum complex, 30 to 60 percent slopes2726F10627112771j8bvor07119671:24000
Steiwer-Chehulpum complex, hummocky, 3 to 20 percent slopes, stony2815D827314332p8tror07119671:24000
Chehulpum silt loam, 3 to 12 percent slopes28C1596626542363or63719811:20000
Chehulpum silt loam, 12 to 40 percent slopes28E554626552364or63719811:20000
Chehulpum silt loam, 3 to 12 percent slopes22C12156427824whor63919831:20000
Chehulpum silt loam, 12 to 35 percent slopes22E7406427924wjor63919831:20000
Steiwer and Chehulpum silt loams, 3 to 40 percent slopesSCE33926414324r4or64319661:20000

Map of Series Extent

Approximate geographic distribution of the CHEHULPUM 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 .