Official Series Description


Lab Data Summary

Aggregate lab data for the GRAIL soil series. This aggregation is based on all pedons with a current taxon name of GRAIL, 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 GRAIL 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
5475ND0250021975ND025002Grail5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.3455556,-102.3755556
5477ND0010171977ND001017Grail3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.9627385,-102.405822
5478ND0370121978ND037012Grail2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.1563889,-101.9111111
5461ND08901161ND089011Grail5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.7647222,-103.1772222
5477ND00101677ND001016Grail4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.9747222,-102.0413889

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the GRAIL 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 GRAIL 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 GRAIL 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 GRAIL 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 GRAIL 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 GRAIL 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 GRAIL 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 GRAIL, 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-2010-09-27-19 | Morton County - 2002

    Typical pattern of soils and underlying materials in the Regent-Daglum-Morton association (Soil Survey of Morton County, North Dakota; 2002).

  2. ND-2012-02-08-04 | Grant County - September 1988

    Typical pattern of soils and parent material in the Amor-Regent-Cabba association (Soil Survey of Grant County, North Dakota; September 1988).

  3. SD-2012-03-15-07 | Corson County - July 1995

    Pattern of soils and parent material in the Reeder-Cabba association (Soil Survey of Corson County, SD; 1995).

Map Units

Map units containing GRAIL 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
Grail-Wyola silty clay loams, 2 to 6 percent slopesE0813B33513155706d1xhmt02519911:24000
Wyola-Grail silty clay loams, 0 to 2 percent slopesE0835A3003422031vzs8mt02519911:24000
Grail silty clay loamGr2227348849cq06mt09119711:24000
Wyola-Grail silty clay loams, 0 to 2 percent slopesE0835A39013456561vzs8mt10919561:31680
Grail-Wyola silty clay loams, 2 to 6 percent slopesE0813B2956345631d1xhmt10919561:31680
Grail soils, 2 to 15 percent slopesGt6307345724clrdmt11119661:20000
Grail clay loam, 2 to 4 percent slopesGr993345722clrbmt11119661:20000
Grail silty clay, 0 to 1 percent slopesGs233345723clrcmt11119661:20000
Grail clay loam, 15 to 35 percent slopesGS947124284682mj0pmt60719701:24000
Wayden-Grail complex, hillyWG6200346214cm86mt60719701:24000
Grail clay loam, 2 to 8 percent slopesGo2061345965cm05mt60719701:24000
Grail clay loam, 8 to 15 percent slopesGr1395345967cm07mt60719701:24000
Grail silty clay, 0 to 2 percent slopesGt919345968cm08mt60719701:24000
Grail clay loam, 0 to 2 percent slopesGn727345964cm04mt60719701:24000
Grail clay loam, 0 to 4 percent slopes2111395348151cp8pmt65519751:24000
Grail clay loam, 4 to 8 percent slopes226854348152cp8qmt65519751:24000
Grail silty clay loam, 0 to 4 percent slopes2210967348225cpc2mt66119821:24000
Grail silty clay loam, 0 to 2 percent slopesE0811A1308025257251vzs4nd00119831:20000
Belfield-Grail-Arnegard complex, saline, 0 to 2 percent slopesE0609A99125257231vzs3nd00119831:20000
Belfield-Grail clay loams, 0 to 2 percent slopesE0605A11525257722r4h0nd00119831:20000
Wyola-Grail silty clay loams, 0 to 2 percent slopesE0835A5427556391vzs8nd00119831:20000
Belfield-Grail clay loams, 0 to 2 percent slopesE0605A362226990412r4h0nd00719981:24000
Wyola-Grail silty clay loams, 0 to 2 percent slopesE0835A70226990461vzs8nd00719981:24000
Grail silty clay loam, 0 to 2 percent slopesE0811A517525635561vzs4nd01119691:20000
Grail silt loam, 0 to 2 percent slopesE0812A483225635552rdbcnd01119691:20000
Wyola-Grail silty clay loams, 0 to 2 percent slopesE0835A212625636051vzs8nd01119691:20000
Grail-Wyola silty clay loams, 2 to 6 percent slopesE0813B17242563558d1xhnd01119691:20000
Grail-Farland silt loams, 2 to 6 percent slopesE0814B94125635572rdbdnd01119691:20000
Grail-Rhoades silty clay loams, 0 to 2 percent slopesGoA81599283412b3xnd01119691:20000
Belfield-Grail-Arnegard complex, saline, 0 to 2 percent slopesE0609A73725635291vzs3nd01119691:20000
Grail-Rhoades silty clay loams, 2 to 6 percent slopesGoB47699283512b3ynd01119691:20000
Belfield-Grail clay loams, 0 to 2 percent slopesE0605A15227584452r4h0nd01119691:20000
Grail silt loam, 2 to 6 percent slopesGeB10499283012b3snd01119691:20000
Grail silty clay loam, 2 to 6 percent slopesGlB7299283212b3vnd01119691:20000
Grail silty clay loam, 0 to 2 percent slopesGlA4399283112b3tnd01119691:20000
Grail silt loam, 0 to 2 percent slopesGeA2999282912b3rnd01119691:20000
Grail soils, saline, 0 to 2 percent slopesGm899283312b3wnd01119691:20000
Grail silty clay loam, 0 to 2 percent slopesC471A1087525641402q4w1nd01519671:20000
Belfield-Rhoades-Grail complex, 0 to 2 percent slopesC523A392125641322q3b6nd01519671:20000
Grail silty clay loam, 2 to 6 percent slopesC471B185325641412q4w2nd01519671:20000
Grail silty clay loam,till, 0 to 2 percent slopesE0807A44626617292qz7jnd01519671:20000
Grail silty clay loam, till, 2 to 6 percent slopesE0807B22726617082q38znd01519671:20000
Wyola-Grail silty clay loams, 0 to 2 percent slopesE0835A15626616891vzs8nd01519671:20000
Belfield-Grail clay loams, 0 to 2 percent slopesE0605A1184827071722r4h0nd02519811:20000
Grail silty clay loam, 0 to 2 percent slopesE0811A648117131681vzs4nd02519811:20000
Wyola-Grail silty clay loams, 0 to 2 percent slopesE0835A544727071871vzs8nd02519811:20000
Grail-Wyola silty clay loams, 2 to 6 percent slopesE0813B45142707184d1xhnd02519811:20000
Grail-Belfield clay loams, 2 to 6 percent slopesE0623B942758469d1xgnd02519811:20000
Belfield-Grail-Arnegard complex, saline, 0 to 2 percent slopesE0609A227071731vzs3nd02519811:20000
Grail silty clay loam,till, 0 to 2 percent slopesE0807A296526618182qz7jnd02919791:20000
Grail silty clay loam, 0 to 2 percent slopesC471A216225643212q4w1nd02919791:20000
Grail silty clay loam, 2 to 6 percent slopesC471B4225958142q4w2nd02919791:20000
Belfield-Grail-Arnegard complex, saline, 0 to 2 percent slopesE0609A665527072731vzs3nd03319851:24000
Grail silty clay loam, 0 to 2 percent slopesE0811A215727072761vzs4nd03319851:24000
Grail-Wyola silty clay loams, 2 to 6 percent slopesE0813B42759731d1xhnd03319851:24000
Grail silty clay loam, 0 to 2 percent slopesE0811A1772117154851vzs4nd03719851:20000
Belfield-Grail clay loams, 0 to 2 percent slopesE0605A54625258412r4h0nd03719851:20000
Belfield-Grail clay loams, 0 to 2 percent slopesE0605A3503725257802r4h0nd04119861:20000
Wyola-Grail silty clay loams, 0 to 2 percent slopesE0835A1598525257831vzs8nd04119861:20000
Belfield-Grail-Arnegard complex, saline, 0 to 2 percent slopesE0609A638825257811vzs3nd04119861:20000
Grail silty clay loam, 0 to 2 percent slopesE0811A576117185821vzs4nd04119861:20000
Grail silt loam, 0 to 2 percent slopesE0812A7127556762rdbcnd04119861:20000
Grail silty clay loam, 0 to 2 percent slopesC471A1325966662q4w1nd04319851:20000
Grail silty clay loam, till, 2 to 6 percent slopesE0807B67626618712q38znd04719921:20000
Grail silty clay loam, 2 to 6 percent slopesC471B29125955042q4w2nd04719921:20000
Grail silty clay loam, 0 to 2 percent slopesC471A9425955032q4w1nd04719921:20000
Grail silty clay loam,till, 0 to 2 percent slopesE0807A8426618842qz7jnd04719921:20000
Grail silty clay loam, 2 to 6 percent slopesC471B95225955262q4w2nd05119921:24000
Grail silty clay loam, till, 2 to 6 percent slopesE0807B19626620042q38znd05119921:24000
Grail silty clay loam, 0 to 2 percent slopesC471A19425955252q4w1nd05119921:24000
Grail silty clay loam,till, 0 to 2 percent slopesE0807A1826620172qz7jnd05119921:24000
Belfield-Grail clay loams, 0 to 2 percent slopesE0605A1573827150352r4h0nd05320031:24000
Wyola-Grail silty clay loams, 0 to 2 percent slopesE0835A1021627150411vzs8nd05320031:24000
Grail silty clay loam, 0 to 2 percent slopesC471A581625666782q4w1nd05519741:20000
Grail silty clay loam, 2 to 6 percent slopesC471B47725666792q4w2nd05519741:20000
Grail silty clay loam, till, 2 to 6 percent slopesE0807B30026624702q38znd05519741:20000
Grail-Haplustolls complex, 0 to 3 percent slopesC1015A12427752582xfnvnd05519741:20000
Grail silty clay loam,till, 0 to 2 percent slopesE0807A11526624892qz7jnd05519741:20000
Belfield-Grail complex, 0 to 2 percent slopesC527A325671552q1ntnd05519741:20000
Belfield-Grail clay loams, 0 to 2 percent slopesE0605A759817150972r4h0nd05719761:20000
Grail-Belfield clay loams, 2 to 6 percent slopesE0623B44572699265d1xgnd05719761:20000
Grail silty clay loam, 0 to 2 percent slopesE0811A274026992641vzs4nd05719761:20000
Grail-Wyola silty clay loams, 2 to 6 percent slopesE0813B24892699266d1xhnd05719761:20000
Wyola-Grail silty clay loams, 0 to 2 percent slopesE0835A156426993121vzs8nd05719761:20000
Grail silt loam, 0 to 2 percent slopesE0812A227585442rdbcnd05719761:20000
Belfield-Grail clay loams, 0 to 2 percent slopesE0605A2984917183292r4h0nd05919981:20000
Grail-Belfield clay loams, 2 to 6 percent slopesE0623B208902699167d1xgnd05919981:20000
Wyola-Grail silty clay loams, 0 to 2 percent slopesE0835A524526992081vzs8nd05919981:20000
Grail silty clay loam, 0 to 2 percent slopesE0811A482117183371vzs4nd05919981:20000
Grail silt loam, 0 to 2 percent slopesE0812A28927596632rdbcnd05919981:20000
Grail-Wyola silty clay loams, 2 to 6 percent slopesE0813B82759664d1xhnd05919981:20000
Grail-Farland silt loams, 2 to 6 percent slopesE0814B327596652rdbdnd05919981:20000
Belfield-Grail complex, 0 to 2 percent slopesC527A108225667652q1ntnd06119881:24000
Wyola-Grail silty clay loams, 0 to 2 percent slopesE0835A19126625131vzs8nd06119881:24000
Grail silt loam, 0 to 2 percent slopesE0812A471125259092rdbcnd06519711:20000
Grail-Farland silt loams, 2 to 6 percent slopesE0814B310325259112rdbdnd06519711:20000
Grail-Wyola silty clay loams, 2 to 6 percent slopesE0813B17222525910d1xhnd06519711:20000
Grail silty clay loam, 0 to 2 percent slopesE0811A156125259081vzs4nd06519711:20000
Wyola-Grail silty clay loams, 0 to 2 percent slopesE0835A46325259141vzs8nd06519711:20000
Grail-Belfield clay loams, 2 to 6 percent slopesE0623B1442755696d1xgnd06519711:20000
Belfield-Grail clay loams, 0 to 2 percent slopesE0605A1484826990722r4h0nd08519921:24000
Grail-Wyola silty clay loams, 2 to 6 percent slopesE0813B70012699093d1xhnd08519921:24000
Grail-Belfield clay loams, 2 to 6 percent slopesE0623B39742699092d1xgnd08519921:24000
Wyola-Grail silty clay loams, 0 to 2 percent slopesE0835A390626991261vzs8nd08519921:24000
Grail silty clay loam, 0 to 2 percent slopesE0811A272826990911vzs4nd08519921:24000
Belfield-Grail-Arnegard complex, saline, 0 to 2 percent slopesE0609A104426990731vzs3nd08519921:24000
Grail-Wyola clay loams, 2 to 6 percent slopes231344337816cbj9nd08519921:24000
Grail silty clay loam, 0 to 2 percent slopesE0811A330227073771vzs4nd08719741:20000
Wyola-Grail silty clay loams, 0 to 2 percent slopesE0835A318727073861vzs8nd08719741:20000
Grail silt loam, 0 to 2 percent slopesE0812A270327073782rdbcnd08719741:20000
Grail-Farland silt loams, 2 to 6 percent slopesE0814B89527073802rdbdnd08719741:20000
Grail-Wyola silty clay loams, 2 to 6 percent slopesE0813B7102707379d1xhnd08719741:20000
Belfield-Grail clay loams, 0 to 2 percent slopesE0605A45327073682r4h0nd08719741:20000
Belfield-Grail-Arnegard complex, saline, 0 to 2 percent slopesE0609A1527585061vzs3nd08719741:20000
Belfield-Grail clay loams, 0 to 2 percent slopesE0605A1361127159712r4h0nd08919651:20000
Grail silty clay loam, 0 to 2 percent slopesE0811A660317134781vzs4nd08919651:20000
Wyola-Grail silty clay loams, 0 to 2 percent slopesE0835A369327159821vzs8nd08919651:20000
Grail-Wyola silty clay loams, 2 to 6 percent slopesE0813B22842715981d1xhnd08919651:20000
Belfield-Grail-Arnegard complex, saline, 0 to 2 percent slopesE0609A166127159731vzs3nd08919651:20000
Wyola-Grail silty clay loams, 0 to 2 percent slopesE0835A166826625591vzs8nd10519931:24000
Wyola-Grail silty clay loams, 0 to 6 percent slopes2357802339068cctpnd10519931:24000
Grail silty clay loam, 0 to 2 percent slopesC471A28826616632q4w1nd10519931:24000
Belfield-Grail complex, 0 to 2 percent slopesC527A2225967882q1ntnd10519931:24000
Grail silty clay loam, 0 to 2 percent slopesC471A336527978882q4w1sd02119781:20000
Grail silty clay loam2951354688cx2ksd02119781:20000
Grail silty clay loam, 0 to 2 percent slopesGr145233561651vzs4sd03119861:24000
Grail-Daglum complex, 0 to 3 percent slopesGrA3593355745cy5nsd06319841:24000
Grail silt loam, 0 to 3 percent slopesGkA833355744cy5msd06319841:24000
Grail silty clay loam, 0 to 2 percent slopesC471A127227987192q4w1sd08919801:20000
Belfield-Grail clay loams, 0 to 2 percent slopesBcA150483546142r4h0sd10519771:24000
Grail silt loam, 0 to 3 percent slopes, rarley floodedGr40923546312zzvvsd10519771:24000
Grail silt loam, 0 to 3 percent slopes, rarley floodedGr21173558442zzvvsd13719851:24000
Eapa-Grail complex, 2 to 6 percent slopesEgB30729355436cxvpsd60119831:24000
Eapa-Grail complex, 6 to 9 percent slopesEgC14776355437cxvqsd60119831:24000
Grail silt loam, 0 to 3 percent slopes, rarley floodedGr217832567482zzvvsd60119831:24000

Map of Series Extent

Approximate geographic distribution of the GRAIL 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 .