Official Series Description


Lab Data Summary

Aggregate lab data for the KIPSON soil series. This aggregation is based on all pedons with a current taxon name of KIPSON, 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 KIPSON 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
7469KS12701769KS127017Kipson1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.6240005,-96.9006653
7479P031879KS127001Kipson6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.6472206,-96.8899994
7601KS20105101KS201051Kipson3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.6216469,-96.8820114

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the KIPSON 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 KIPSON 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 KIPSON 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 KIPSON 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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Click the image to view it full size.

Competing Series

Soil series competing with KIPSON 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 KIPSON 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 KIPSON 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 KIPSON, 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

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

  1. KS-2012-01-23-37 | Hodgeman County - June 1973

    Typical pattern of soils and parent materials across the Sawlog Valley, about 4 miles north of the Hodgeman-Ford County line (Soil Survey of Hodgeman County, Kansas; 1973).

  2. KS-2012-01-24-19 | Morris County - November 1974

    Typical pattern of soils and underlying material in association 5 (Soil Survey of Morris County, Kansas; 1974).

  3. KS-2012-01-25-19 | Republic County - November 1967

    Distribution of the soils in the Crete-Butler-Hastings association (Soil Survey of Republic County, Kansas; 1967).

  4. KS-2012-01-25-20 | Republic County - November 1967

    Distribution of the soils in the Hastings-Crete-Geary association (Soil Survey of Republic County, Kansas; 1967).

  5. KS-2012-01-25-21 | Republic County - November 1967

    Distribution of the soils in the Kipson-Tully-Crete association (Soil Survey of Republic County, Kansas; 1967).

  6. KS-2012-01-25-23 | Republic County - November 1967

    Distribution of the soils in the Muir-Carr-Humbarger association (Soil Survey of Republic County, Kansas; 1967).

  7. KS-2012-01-25-30 | Saline County - May 1992

    Pattern of soils and parent material in the Crete-Longford association (Soil Survey of Saline County, Kansas; 1992).

  8. KS-2012-01-25-31 | Saline County - May 1992

    Pattern of soils and parent material in the Irwin-Clime association (Soil Survey of Saline County, Kansas; 1992).

  9. KS-2012-01-26-29 | Washington County - August 1993

    Typical pattern of soils and parent material in the Crete-Kipson-Tully association (Soil Survey of Washington County, Kansas; 1993).

  10. NE-2012-02-13-67 | Nemaha County - December 1985

    Typical pattern of soils and parent material in the Monona-Ida and Onawa-Haynie-Albaton associations (Soil Survey of Nemaha County, Nebraska; December 1985).

  11. OK-2012-02-17-50 | Stephens County - 1964

    Typical pattern of soils in association 4 (Soil Survey of Stephens County, Oklahoma; 1964).

Map Units

Map units containing KIPSON 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
Kipson-Sogn complex, 5 to 30 percent slopes4725331311521542ww04ks01319941:24000
Kipson-Sogn complex, 5 to 30 percent slopes47251370414546612ww04ks02719831:24000
Kipson soils, 5 to 30 percent slopes47152831213820642ww02ks02919721:24000
Kipson-Sogn complex, 5 to 30 percent slopes47255414545572ww04ks04119771:24000
Kipson-Clime complex, 6 to 20 percent slopes47204914545562ww03ks04119771:24000
Kipson-Sogn complex, 5 to 30 percent slopes472521014803282ww04ks08519761:24000
Kipson silty clay loam, 5 to 30 percent slopes4710444113827822ww01ks11519811:24000
Kipson-Sogn complex, 5 to 30 percent slopes47255102214570702ww04ks11719771:24000
Kipson-Sogn complex, 5 to 30 percent slopes47251053314545042ww04ks12719701:24000
Kipson silty clay loam, 5 to 30 percent slopes4710873614060052wtw3ks13119801:24000
Kipson-Sogn complex, 5 to 30 percent slopes472522314060062ww04ks13119801:24000
Kipson soils, 5 to 30 percent slopes471599813821342ww02ks14319781:24000
Kipson-Sogn complex, 5 to 30 percent slopes472531114810712ww04ks14919841:24000
Kipson soils, 5 to 30 percent slopes47152563314552352ww02ks15719651:24000
Kipson complex, 3 to 15 percent slopes4705167914332502ww00ks15919711:24000
Kipson-Sogn complex, 5 to 30 percent slopes4725103314723162ww04ks16119701:24000
Kipson-Clime complex, 6 to 20 percent slopes4720525213821742ww03ks16919891:24000
Kipson-Sogn complex, 5 to 30 percent slopes4725139214734582ww04ks17719661:24000
Kipson-Sogn complex, 5 to 30 percent slopes47251681814548872ww04ks20119881:24000
Kipson soils, 5 to 30 percent slopes4715681314548862ww02ks20119881:24000
Kipson complex, 7 to 30 percent slopes4160466816919702wvzqne06119741:20000
Rock Outcrop-Kipson complex, 7 to 45 percent slopes41681422193092wvzzne06119741:20000
Kipson-Sogn complex, 3 to 30 percent slopes4166278316911092wvzxne06720001:12000
Kipson-Sogn-Rock Outcrop complex, 11 to 60 percent slopes4167162716911102wvzyne06720001:12000
Kipson silt loam, 7 to 30 percent slopes4161551216918122wvzrne09519701:20000
Kipson soils, 11 to 30 percent slopes4162622192142wvzsne09519701:20000
Kipson-Benfield complex, 11 to 25 percent slopes4163167416915772wvztne09719841:20000
Monona-Kipson complex, 30 to 70 percent slopes8096191716916801tsbbne12719831:20000
Sogn-Kipson complex, 7 to 30 percent slopes3920145116916992vhh6ne12719831:20000
Benfield-Kipson silty clay loams, 6 to 11 percent slopes, eroded7555129316916532ww0jne12719831:20000
Benfield-Kipson silty clay loams, 11 to 30 percent slopes755659716916542ww0kne12719831:20000
Kipson silt loam, 7 to 30 percent slopes416130416920822wvzrne12919741:20000
Monona-Shelby-Kipson complex, 30 to 70 percent slopes8101474616915421ts5wne13119791:20000
Kipson-Benfield complex, 7 to 20 percent slopes416471916915302wvzvne13119791:20000
Monona-Kipson complex, 30 to 70 percent slopes80963822193252dhd4ne13119791:20000
Kipson-Benfield silty clay loams, 7 to 17 percent slopes4165777916916172wvzwne13319691:15840
Kipson-Sogn complex, 3 to 30 percent slopes4166372216916182wvzxne13319691:15840
Kipson-Benfield complex, 11 to 25 percent slopes41635622193992wvztne13319691:15840
Kipson-Sogn complex, 3 to 30 percent slopes41661135816910442wvzxne14719671:20000
Kipson-Benfield silty clay loams, 7 to 17 percent slopes4165848516910422wvzwne14719671:20000
Benfield-Kipson silty clay loams, 3 to 9 percent slopes, severely eroded7554266416910282ww0hne14719671:20000
Kipson soils, 11 to 30 percent slopes4162245216924292wvzsne16919651:20000
Kipson silt loam, 7 to 30 percent slopes4161125422187322wvzrne16919651:20000
Wakeen and Kipson silty clay loams, 6 to 11 percent slopes2900104516924442wvznne16919651:20000
Wakeen and Kipson variant silty clay loams, 6 to 11 percent slopes, severely eroded290132816924452wvzpne16919651:20000
Kipson silt loam, 7 to 30 percent slopes4161982716920272wvzrne18119671:20000
Rock Outcrop-Kipson complex, 7 to 45 percent slopes416871716920382wvzzne18119671:20000
Kipson complex, 7 to 30 percent slopes41601022290762wvzqne18119671:20000

Map of Series Extent

Approximate geographic distribution of the KIPSON 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 .