Official Series Description


Lab Data Summary

Aggregate lab data for the CHERRY soil series. This aggregation is based on all pedons with a current taxon name of CHERRY, 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 CHERRY 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
5240A3522S1950MT085003Cherry5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties48.0460548,-105.8229141
5482ND03313882ND033138Cherry5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.9122222,-103.7641667
58A91P089803MT021001-90-1Cherry7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.2153024,-105.1853549

Water Balance

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

There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with CHERRY, 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. ND-2012-02-08-30 | Mountrail County - June 1991

    Typical pattern of soils and parent material in the Cabba-Badland association (Soil Survey of Mountrail County, North Dakota; June 1991).

  2. ND-2012-02-08-53 | Stark County - February 1968

    Diagram showinig the relationship of some of the major soils in Stark County (Soil Survey of Stark County, North Dakota; February 1968).

Map Units

Map units containing CHERRY 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
Cambert-Cherry-Cabba silt loams, 12 to 25 percent slopes734E25134343660cjltmt01719951:24000
Cherry-Cambert-Cabba silt loams, 8 to 15 percent slopes562D15729343541cjgzmt01719951:24000
Cherry-Cambert silt loams, 2 to 8 percent slopes561C6991343540cjgymt01719951:24000
Cherry silt loam, 2 to 8 percent slopes56C2104343543cjh1mt01719951:24000
Cherry silt loam, 0 to 2 percent slopes56A90343542cjh0mt01719951:24000
Cherry-Cambert-Cabba silt loams, 4 to 15 percent slopes212D415814871861lxjrmt02119711:24000
Cherry-Cambert silt loams, 2 to 8 percent slopes211C380214871871lxjsmt02119711:24000
Cherry silt loam, 2 to 4 percent slopes21B371514870741lxf4mt02119711:24000
Cherry silt loam, 0 to 2 percent slopes21A241314870751lxf5mt02119711:24000
Cherry silt loam, 4 to 8 percent slopes21C240314870731lxf3mt02119711:24000
Cherry, Havrelon, and Trembles soils, 0 to 4 percent slopes, occasionally flooded215B142214873281lxpbmt02119711:24000
Cherry-Lambert complex, 4 to 25 percent slopes214E18214873191lxp1mt02119711:24000
Cherry silt loam, 0 to 4 percent slopes4438736344407ckcxmt05519811:24000
Cherry-Havrelon-Trembles complex, 0 to 2 percent slopes4517326344408ckcymt05519811:24000
Cherry silt loam, 0 to 2 percent slopes18926314857811lw2fmt05519811:24000
Cherry silt loam, 2 to 4 percent slopes19014014857801lw2dmt05519811:24000
Cherry-Cambert-Cabba silt loams, 4 to 15 percent slopes1845114570317g65mt05519811:24000
Cambert, calcareous-Cabba-Cherry, calcareous complex, 8 to 25 percent slopes224078344837cktsmt07919861:24000
Cherry-Cambert silt loams, calcareous, 2 to 8 percent slopes303025344864ckvnmt07919861:24000
Cherry, calcareous-Cambert, calcareous-Cabba silt loams, 4 to 15 percent slopes311984344869ckvtmt07919861:24000
Cherry silt loam, calcareous, 0 to 2 percent slopes28719344854ckvbmt07919861:24000
Aeric Fluvaquents-Cherry, calcareous complex, 0 to 8 percent slopes4682344903ckwxmt07919861:24000
Cherry silt loam, calcareous, 2 to 8 percent slopes29436344859ckvhmt07919861:24000
Cherry, calcareous-Typic Ustifluvents, complex, 0 to 8 percent slopes33263344877ckw2mt07919861:24000
Cherry, calcareous-Lisk-Cabba complex, 8 to 25 percent slopes3241344872ckvxmt07919861:24000
Cherry-Cambert silt loams, 2 to 8 percent slopes211C4083416775431t9m9mt08319731:24000
Cherry, Havrelon, and Trembles soils, occasionally floodedCh25793345330clbpmt08319731:24000
Cherry-Cambert-Cabba silt loams, 4 to 15 percent slopes212D2212622160432dcz8mt08319731:24000
Cherry silty clay loam, 0 to 2 percent slopesCeA15298345327clblmt08319731:24000
Cherry silty clay loam, 2 to 4 percent slopesCeB13600345328clbmmt08319731:24000
Cherry silt loam, 4 to 8 percent slopes21C327516775401t9m6mt08319731:24000
Cherry silt loam, 2 to 4 percent slopes21B206616775411t9m7mt08319731:24000
Cherry silty clay loam, 4 to 8 percent slopesCeC843345329clbnmt08319731:24000
Cherry silt loam, 0 to 2 percent slopes21A44116775421t9m8mt08319731:24000
Cherry silty clay loam, 2 to 4 percent slopesChB5775348840cpzxmt09119711:24000
Cherry silty clay loam, 4 to 8 percent slopesChC4660348841cpzymt09119711:24000
Cherry clay loam, 0 to 1 percent slopesCh641345401cldzmt10319611:20000
Cherry clay loam, shallow, 0 to 1 percent slopesCm475345403clf1mt10319611:20000
Cherry clay, moderately deep, 0 to 1 percent slopesCd341345398cldwmt10319611:20000
Cherry clay, 1 to 3 percent slopesCb290345396cldtmt10319611:20000
Cherry-Laurel clay loamsCn279345404clf2mt10319611:20000
Cherry clay, moderately deep, 1 to 3 percent slopesCf238345399cldxmt10319611:20000
Cherry clay loam, 1 to 3 percent slopesCk235345402clf0mt10319611:20000
Cherry clay, 0 to 1 percent slopesCa159345395cldsmt10319611:20000
Cherry clay, 3 to 8 percent slopesCc153345397cldvmt10319611:20000
Cherry clay, moderately deep, 3 to 8 percent slopesCg55345400cldymt10319611:20000
Cherry silt loam, 4 to 9 percent slopesCk4389345620cln1mt10919561:31680
Cherry silt loam, 0 t0 3 percent slopesCg2423345618clmzmt10919561:31680
Cherry silt loam, saline, 0 to 3 percent slopesCh1029345619cln0mt10919561:31680
Cherry silt loam, saline, 4 to 9 percent slopesCm801345621cln2mt10919561:31680
Cherry silty clay loam, 2 to 8 percent slopesCe4345345902cly4mt60719701:24000
Farland-Cherry silt loams, 2 to 8 percent slopes17108358348219cpbwmt66119821:24000
Cabba-Cambert-Cherry silt loams, 8 to 15 percent slopes1051703348212cpbnmt66119821:24000
Cherry silt loam, 2 to 8 percent slopes1237976348214cpbqmt66119821:24000
Cherry silt loam, 0 to 6 percent slopesE3203B99625635432q524nd01119691:20000
Cherry silt loam, 6 to 9 percent slopesE3203C29225635441vzvknd01119691:20000
Cherry clay loam, 2 to 6 percent slopesCrB15399281212b36nd01119691:20000
Cherry clay loam, 6 to 9 percent slopesCrC9899281312b37nd01119691:20000
Cherry clay loam, 0 to 2 percent slopesCrA8799281112b35nd01119691:20000
Cherry silt loam, 6 to 9 percent slopesE3203C159827072251vzvknd02519811:20000
Cherry silt loam, 0 to 6 percent slopesE3203B127927072242q524nd02519811:20000
Cherry-Cabba silt loams, 9 to 45 percent slopesE3161F9622707220d33tnd02519811:20000
Cherry-Cabba silt loams, 9 to 45 percent slopesE3161F123712707303d33tnd03319851:24000
Cherry silt loam, 6 to 9 percent slopesE3203C552827073061vzvknd03319851:24000
Cherry silt loam, 0 to 6 percent slopesE3203B237727073052q524nd03319851:24000
Cherry-Lambert, gullied-Havrelon, occasionally flooded complex, 0 to 6 percent slopesE3235B2152759750d32snd03319851:24000
Cherry-Cabba-Brandenburg complex, 9 to 35 percent slopesE3025F462759748d1wwnd03319851:24000
Cherry-Cabba silt loams, 9 to 45 percent slopesE3161F323182715094d33tnd05320031:24000
Cherry silt loam, 6 to 9 percent slopesE3203C408027150991vzvknd05320031:24000
Cherry silt loam, 0 to 6 percent slopesE3203B307527150982q524nd05320031:24000
Cherry-Cabba-Brandenburg complex, 9 to 35 percent slopesE3025F27472715088d1wwnd05320031:24000
Cherry-Lambert, gullied-Havrelon, occasionally flooded complex, 0 to 6 percent slopesE3235B12352715100d32snd05320031:24000
Cherry-Cabba silt loams, 9 to 45 percent slopesE3161F59492662449d33tnd05519741:20000
Cherry-Cabba silt loams, 9 to 45 percent slopesE3161F31562662507d33tnd06119881:24000
Cherry silt loam, 6 to 9 percent slopesE3203C72127158511vzvknd08719741:20000
Cherry silt loam, 0 to 6 percent slopesE3203B31527158502q524nd08719741:20000
Cherry silt loam, 6 to 9 percent slopesE3203C116617135531vzvknd08919651:20000
Cherry silt loam, 0 to 6 percent slopesE3203B53717135522q524nd08919651:20000
Cherry silt loam, 0 to 6 percent slopesE3203B266326625822q524nd10519931:24000
Cherry silt loam, 6 to 9 percent slopesE3203C199226625721vzvknd10519931:24000
Cherry silt loam, 0 to 6 percent slopes2343194339054cct7nd10519931:24000
Cherry silt loam, 6 to 9 percent slopes234441339055cct8nd10519931:24000

Map of Series Extent

Approximate geographic distribution of the CHERRY 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 .