Official Series Description


Lab Data Summary

Aggregate lab data for the POINSETT soil series. This aggregation is based on all pedons with a current taxon name of POINSETT, 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 POINSETT 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
102A89P038687SD011009Poinsett6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.5133324,-96.9775009
102A88P032487SD039008Poinsett8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.6022224,-96.5438919
102A40A2441S1957SD029007Poinsett6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.1124992,-97.3722229
102AUMN1146S1970MN0831146Poinsett3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.3612823,-96.0781326
102AUMN1945S1975MN1731945Poinsett2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.7486992,-96.4496155
102AUMN1946S1975MN1731946Poinsett3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.7345695,-96.4455795

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the POINSETT 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 POINSETT 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 POINSETT 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 POINSETT 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 POINSETT 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 POINSETT series and competing. 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 POINSETT 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 mountains figure.

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

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Soil series sharing subgroup-level classification with POINSETT, 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. MN-2010-09-27-04 | Lac qui Parle County -

    Typical pattern of soils and underlying material in the Waubay-Poinsett-Colvin association (Soil Survey of Lac qui Parle County, Minnesota).

  2. SD-2010-11-01-01 | Brookings County - 2004

    Typical pattern of soils and parent material in the Poinsett-Buse-Waubay association (Soil Survey of Brookings County, South Dakota; 2004).

  3. SD-2010-11-01-08 | Hamlin County - 2003

    Typical pattern of soils and underlying material in the Poinsett-Waubay-Buse association (Soil Survey of Hamlin County, South Dakota; 2003).

  4. SD-2012-03-14-16 | Clark County - 1999

    Typical pattern of soils and underlying material in the Poinsett-Waubay-Buse association (Soil Survey of Clark County, SD; 1999).

  5. SD-2012-03-15-01 | Codington County - December 1966

    Diagram showing the relative position of the major soils in association 1 (Soil Survey of Codington County, SD; 1966).

  6. SD-2012-03-15-03 | Codington County - December 1966

    Diagram showing the relative position of the major soils in association 4 (Soil Survey of Codington County, SD; 1966).

  7. SD-2012-03-15-18 | Day County - August 1997

    Typical pattern of soils and underlying material in the Nutley-Sinai and Poinsett-Waubay-Forman associations (Soil Survey of Day County, SD; 1997).

  8. SD-2012-03-15-62 | Kingsbury County - November 1997

    Typical pattern of soils and underlying material in the Poinsett-Waubay-Buse association (Soil Survey of Kingsbury County, SD; 1997).

  9. SD-2012-03-15-63 | Kingsbury County - November 1997

    Typical pattern of soils and underlying material in the Poinsett-Hetland association (Soil Survey of Kingsbury County, SD; 1997).

Map Units

Map units containing POINSETT 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
Poinsett-Buse complex, 2 to 6 percent slopes741B6878430338gfswmn07319941:20000
Poinsett-Waubay silty clay loams, 1 to 6 percent slopes284B38924302792rkz3mn07319941:20000
Poinsett-Waubay silty clay loams, 1 to 6 percent slopesJ195B356614800882rkz3mn08120071:12000
Rusklyn-Poinsett complex, 6 to 12 percent slopes, moderately erodedJ198C258014800891lp4tmn08120071:12000
Poinsett-Waubay silty clay loams, 1 to 6 percent slopesJ195B370914862102rkz3mn08320081:12000
Rusklyn-Poinsett complex, 6 to 12 percent slopes, moderately erodedJ198C250514862111lwj9mn08320081:12000
Poinsett-Waubay silty clay loams, 1 to 6 percent slopesJ195B471614816522rkz3mn10120081:12000
Poinsett-Waubay silty clay loams, 1 to 6 percent slopesJ195B53114817072rkz3mn17319791:20000
Rusklyn-Poinsett complex, 6 to 12 percent slopes, moderately erodedJ198C223116539391sj1wmn17319791:20000
Poinsett-Buse-Waubay complex, 1 to 6 percent slopesPbB371434187922tlc8sd01119951:24000
Poinsett-Buse-Waubay complex, 2 to 9 percent slopesPbC249314187932tlc9sd01119951:24000
Poinsett-Waubay silty clay loams, 1 to 6 percent slopesPwB131634187952rkz3sd01119951:24000
Buse-Poinsett complex, 9 to 15 percent slopesBpD5537418731g1qgsd01119951:24000
Poinsett-Waubay silty clay loams, 0 to 2 percent slopesPwA35224187942t5qvsd01119951:24000
Buse, very stony-Poinsett complex, 9 to 25 percent slopesBrD1423418732g1qhsd01119951:24000
Poinsett-Waubay silty clay loams, 1 to 6 percent slopesPwB437814177772rkz3sd02519921:20000
Poinsett-Rusklyn-Waubay silty clay loams, 1 to 6 percent slopesPrB321044177752rkz5sd02519921:20000
Poinsett-Waubay silty clay loams, 0 to 2 percent slopesPwA165014177762t5qvsd02519921:20000
Poinsett-Rusklyn silty clay loams, 6 to 9 percent slopesPoC7071417774g0qlsd02519921:20000
Poinsett-Buse-Waubay complex, 1 to 6 percent slopesPnB40314177722tlc8sd02519921:20000
Poinsett-Buse-Waubay complex, 2 to 9 percent slopesPnC4174177732tlc9sd02519921:20000
Poinsett-Waubay silty clay loams, 0 to 2 percent slopesG794A9527980292sd5zsd02519921:20000
Poinsett-Buse-Waubay complex, 1 to 6 percent slopesJ162B5395116842962tlc8sd02920061:12000
Poinsett-Waubay silty clay loams, 0 to 2 percent slopesJ164A1052416842942t5qvsd02920061:12000
Poinsett-Buse-Waubay complex, 2 to 9 percent slopesJ162C765616843042tlc9sd02920061:12000
Poinsett-Waubay silty clay loams, 1 to 6 percent slopesJ164B435116842952rkz3sd02920061:12000
Poinsett-Rusklyn-Waubay silty clay loams, 1 to 6 percent slopesJ163B322316843072rkz5sd02920061:12000
Buse-Poinsett complex, 6 to 9 percent slopesJ118C162316843051tjnfsd02920061:12000
Poinsett-Rusklyn-Waubay silty clay loams, 1 to 6 percent slopesPsB178534171202rkz5sd03719921:20000
Poinsett-Waubay silty clay loams, 1 to 6 percent slopesPwB134864171222rkz3sd03719921:20000
Poinsett-Waubay silty clay loams, 0 to 2 percent slopesPwA54344171212t5qvsd03719921:20000
Poinsett-Rusklyn silty clay loams, 6 to 9 percent slopesPrC2045417119g01gsd03719921:20000
Poinsett-Buse-Waubay complex, 1 to 6 percent slopesPnB11898000622tlc8sd03719921:20000
Poinsett-Waubay silty clay loams, 1 to 6 percent slopesPwB80244168922rkz3sd03919921:20000
Poinsett-Waubay silty clay loams, 0 to 2 percent slopesPwA56184168912t5qvsd03919921:20000
Poinsett silty clay loam, 6 to 9 percent slopesPoC677416890fzt2sd03919921:20000
Poinsett-Waubay silty clay loams, 0 to 2 percent slopesPo15224181782t5qvsd05119771:20000
Poinsett-Buse-Waubay complex, 1 to 6 percent slopesPsB621014173022tlc8sd05719921:20000
Poinsett-Waubay silty clay loams, 1 to 6 percent slopesPwB474924173052rkz3sd05719921:20000
Poinsett-Waubay silty clay loams, 0 to 2 percent slopesPwA134194173042t5qvsd05719921:20000
Poinsett-Buse-Waubay complex, 2 to 9 percent slopesPsC82254173032tlc9sd05719921:20000
Buse-Poinsett complex, 6 to 9 percent slopesByC7887417264g064sd05719921:20000
Buse-Poinsett complex, 9 to 15 percent slopesByD1742417265g065sd05719921:20000
Poinsett-Buse-Waubay complex, 1 to 6 percent slopesPoB744794175032tlc8sd07719921:20000
Poinsett-Waubay silty clay loams, 1 to 6 percent slopesPwB480784175072rkz3sd07719921:20000
Poinsett-Buse-Waubay complex, 2 to 9 percent slopesPoC207664175042tlc9sd07719921:20000
Poinsett-Waubay silty clay loams, 0 to 2 percent slopesPwA127154175062t5qvsd07719921:20000
Poinsett-Rusklyn-Waubay silty clay loams, 1 to 6 percent slopesPrB18624175052rkz5sd07719921:20000
Poinsett-Forman complex, 2 to 6 percent slopesPoB9286416595fzhksd09119701:20000
Forman-Poinsett complex, 6 to 9 percent slopesFxC9023416563fzgjsd09119701:20000
Forman-Poinsett complex, 9 to 15 percent slopesFxD8407416564fzgksd09119701:20000
Poinsett-Forman complex, 2 to 6 percent slopesG791B568527993772sd5tsd09119701:20000
Poinsett-Waubay silty clay loams, 1 to 6 percent slopesPwB27744165972rkz3sd09119701:20000
Forman-Poinsett complex, 6 to 9 percent slopesG791C267927993782sd5vsd09119701:20000
Forman-Poinsett complex, 9 to 15 percent slopesG791D130427993792sd5wsd09119701:20000
Poinsett-Waubay silty clay loams, 0 to 2 percent slopesPwA7244165962t5qvsd09119701:20000
Poinsett-Waubay silty clay loams, 0 to 2 percent slopesG794A39627993812sd5zsd09119701:20000
Poinsett-Waubay silty clay loams, 0 to 2 percent slopesPoA116744178592t5qvsd10919771:20000
Poinsett-Waubay silty clay loams, 1 to 6 percent slopesPoB66454178602rkz3sd10919771:20000

Map of Series Extent

Approximate geographic distribution of the POINSETT 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 .