Official Series Description


Lab Data Summary

Aggregate lab data for the HUBBARD soil series. This aggregation is based on all pedons with a current taxon name of HUBBARD, 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 HUBBARD 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
91AUMN16751973MN145035 (1675)Hubbard3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.4706383,-94.1259155
91AUMN13441977MN0031344Hubbard2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.2479706,-93.485527
91AUMN0178S1957MN141178Hubbard4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.4726372,-94.0883865
91A40A2039S1960MN171004Hubbard6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.3216591,-93.8474579
91AUMN0343S1960MN171343Hubbard2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.3782501,-93.9345016
91AUMN0013S1963MN141013Hubbard1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.3180847,-93.7530594
91AUMN0014S1963MN141014Hubbard1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.3149986,-93.7581406
91AUMN1669S1973MN1451669Hubbard2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.539205,-94.162524
91AUMN3269S1980MN0973269Hubbard4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.0744973,-94.3624955
91AUMN3934S1986MN1413934Hubbard2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.3905563,-93.8960266
91AUMN4375S1990MN141026 (4375)Hubbard3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.3112106,-93.7471619
91AUMN4374S1990MN141088 (4374)Hubbard3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.4154625,-93.8975906
91A92P0195S1991MN141001Hubbard6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.415212,-93.947981
91A13N0479S2012MN009006Hubbard6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.7587367,-94.2136883
91A13N0480S2012MN009011Hubbard6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.7306517,-94.178635
91A13N0481S2012MN009017Hubbard6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.6876278,-94.1971389
91A13N0482S2012MN097006Hubbard6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.113181,-94.334728

Water Balance

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

Click the image to view it full size.

Click the image to view it full size.

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

Click the image to view it full size.

Click the image to view it full size.

Soil series sharing subgroup-level classification with HUBBARD, 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-2010-09-13-03 | Wright County -

    Typical pattern of soils and parent material in the Hubbard-Mosford association (Soil Survey of Wright County, Minnesota).

  2. MN-2010-09-13-07 | Wright County -

    A landscape view of some soils in areas of outwash, flood plain, and glacial till in Wright County (Soil Survey of Wright County, Minnesota).

  3. WI-2012-03-23-30 | Pepin County - March 1964

    Cross section showing the geology and the associated soils in Pepin County (Soil Survey of Pepin County, WI; 1964).

Map Units

Map units containing HUBBARD 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
Hubbard loamy sand, 0 to 2 percent slopesD67A53563959352w0mkmn00319721:15840
Hubbard loamy sand, 1 to 6 percent slopesD67B400227654112w0mlmn00319721:15840
Hubbard loamy sand, 2 to 12 percent slopesD67C13633959372w0mmmn00319721:15840
Urban land-Hubbard complex, Mississippi River Valley, 0 to 8 percent slopesD64B12828853572smhhmn00319721:15840
Hubbard-Mosford complex, Mississippi River Valley, 0 to 3 percent slopesD62A7127654472smhfmn00319721:15840
Hubbard coarse sand, 2 to 6 percent slopesHuB10395936f904mn00319721:15840
Hubbard loamy sand, 0 to 2 percent slopesD67A1305227654152w0mkmn00920071:12000
Hubbard loamy sand, 1 to 6 percent slopesD67B639927654162w0mlmn00920071:12000
Hubbard loamy sand, 0 to 2 percent slopesD7A2528709869rtp0mn00920071:12000
Hubbard loamy sand, 2 to 6 percent slopesD7B1756709870rtp1mn00920071:12000
Hubbard loamy sand, 6 to 12 percent slopesD7C558729058sgn0mn00920071:12000
Hubbard loamy sand, 2 to 12 percent slopesD67C51127654172w0mmmn00920071:12000
Hubbard, bedrock substratum-Rock outcrop complex, 1 to 8 percent slopesD54B122785255vc3tmn00920071:12000
Hubbard-Mosford complex, Mississippi River Valley, 0 to 3 percent slopesD62A1007528862smhfmn00920071:12000
Hubbard loamy sand, Mississippi River Valley, 18 to 35 percent slopesD67E9327654182smhdmn00920071:12000
Hubbard loamy sand, 18 to 35 percent slopesD7E44753012t8kqmn00920071:12000
Hubbard loamy sand, 0 to 2 percent slopesD67A687827654192w0mkmn02119931:20000
Hubbard loamy sand, 1 to 6 percent slopesD67B211127654202w0mlmn02119931:20000
Hubbard loamy sand, Mississippi River Valley, 0 to 2 percent slopesD67A300227326782sln1mn03520091:24000
Hubbard loamy sand, Mississippi River Valley, 2 to 6 percent slopesD67B107727326792sln2mn03520091:24000
Hubbard loamy sand, well drained, Mississippi River Valley, 0 to 3 percent slopesD100A59627326882slndmn03520091:24000
Sandberg-Hubbard complex, Mississippi River Valley, 0 to 3 percent slopesD97A33027326842sln8mn03520091:24000
Hubbard loamy sand, Mississippi River Valley, 6 to 12 percent slopesD67C20427326802sln3mn03520091:24000
Hubbard loamy sand, 1 to 6 percent slopes7B2180396882f9znmn03719801:15840
Urban land-Hubbard complex, 0 to 6 percent slopes865B1228396894fb01mn03719801:15840
Hubbard loamy sand, 6 to 12 percent slopes7C1168396883f9zpmn03719801:15840
Hubbard loamy sand, 0 to 1 percent slopes7A808396881f9zmmn03719801:15840
Hubbard loamy sand, 12 to 18 percent slopes7D752396884f9zqmn03719801:15840
Urban land-Hubbard complex, Mississippi River Valley, 0 to 8 percent slopesD64B150604352212smhhmn05320011:12000
Hubbard loamy sand, 0 to 2 percent slopesD67A44554516322w0mkmn05320011:12000
Hubbard loamy sand, 1 to 6 percent slopesD67B31734516312w0mlmn05320011:12000
Hubbard loamy sand, 2 to 12 percent slopesD67C6744516302w0mmmn05320011:12000
Urban land-Hubbard, bedrock substratum complex, 0 to 8 percent slopesD29B558435214glw5mn05320011:12000
Hubbard loamy fine sand, 2 to 7 percent slopesHu997398358fcj8mn05919561:20000
Hubbard loamy fine sand, 0 to 2 percent slopesH447398356fcj6mn05919561:20000
Hubbard loamy fine sand, 7 to 12 percent slopesHp79398357fcj7mn05919561:20000
Hubbard loamy sand, lake beach, 2 to 8 percent slopesC114B22116764401t8gqmn09520061:12000
Hubbard loamy sand, lake beach, 8 to 20 percent slopesC114D4116764411t8grmn09520061:12000
Hubbard loamy sand, 0 to 2 percent slopesD67A1307327654262w0mkmn09719871:20000
Hubbard loamy sand, 1 to 6 percent slopesD67B867627654272w0mlmn09719871:20000
Hubbard loamy sand, 1 to 6 percent slopes7B133154359542w0mlmn11119961:20000
Hubbard loamy sand, 0 to 2 percent slopes7A102344359532w0mkmn11119961:20000
Hubbard loamy sand, 2 to 12 percent slopes7C25254359552w0mmmn11119961:20000
Hubbard-Mosford complex, Mississippi River Valley, 0 to 3 percent slopesD62A3769927654362smhfmn14119941:15840
Hubbard loamy sand, 1 to 6 percent slopesD67B1495027654342w0mlmn14119941:15840
Hubbard loamy sand, 0 to 2 percent slopesD67A587927654352w0mkmn14119941:15840
Hubbard loamy sand, 2 to 12 percent slopesD67C356227654332w0mmmn14119941:15840
Hubbard-Verndale, acid substratum, complex, Mississippi River Valley, 0 to 3 percent slopesD61A168027654372smhgmn14119941:15840
Hubbard loamy sand, 2 to 6 percent slopes7B665431502gh0fmn14119941:15840
Hubbard-Verndale complex, 0 to 3 percent slopes1224501431435ggy8mn14119941:15840
Hubbard loamy sand, 0 to 2 percent slopes7A399431501gh0dmn14119941:15840
Hubbard loamy sand, 6 to 12 percent slopes7C131431503gh0gmn14119941:15840
Hubbard loamy sand, 1 to 6 percent slopesD67B1867627654392w0mlmn14519801:15840
Hubbard loamy sand, 0 to 2 percent slopesD67A1122727654382w0mkmn14519801:15840
Urban land-Hubbard complex, Mississippi River Valley, 0 to 8 percent slopesD64B313927654412smhhmn14519801:15840
Hubbard loamy sand, 2 to 12 percent slopesD67C300427654402w0mmmn14519801:15840
Hubbard loamy sand, 1 to 6 percent slopes7B95394285712w0mlmn15319851:20000
Hubbard loamy sand, 0 to 2 percent slopes7A46844285702w0mkmn15319851:20000
Hubbard loamy sand, 1 to 6 percent slopes7B124616770401t932mn16319781:15840
Hubbard loamy sand, 12 to 18 percent slopes7D75716770421t934mn16319781:15840
Hubbard loamy sand, 6 to 12 percent slopes7C45216770411t933mn16319781:15840
Hubbard-Mosford complex, Mississippi River Valley, 0 to 3 percent slopesD62A42074350422smhfmn17119981:12000
Hubbard loamy sand, 1 to 6 percent slopesD67B12154336332w0mlmn17119981:12000
Hubbard-Verndale, acid substratum, complex, Mississippi River Valley, 0 to 3 percent slopesD61A10984350432smhgmn17119981:12000
Hubbard loamy sand, 0 to 2 percent slopesD67A7554336172w0mkmn17119981:12000
Hubbard loamy sand, 2 to 12 percent slopesD67C6614336322w0mmmn17119981:12000
Hubbard loamy sand, river valleys, 0 to 3 percent slopes, occasionally flooded702A30131821152yt31wi00119781:20000
Hubbard loamy sand, river valleys, 0 to 3 percent slopes, occasionally flooded702A6031821352yt31wi05319941:12000
Hubbard loamy sand, 0 to 6 percent slopesHrB1994421189g48rwi09519781:15840
Hubbard-Mosford complex, 0 to 6 percent slopes119B1724276502mh59wi09519781:15840
Hubbard loamy sand, river valleys, 0 to 3 percent slopes, occasionally flooded702A3431821612yt31wi09719721:20000
Hubbard loamy sand, 0 to 6 percent slopesHrB1413422150g58rwi10919751:15840
Hubbard loamy sand, loamy substratum, 0 to 6 percent slopesHsB1249422151g58swi10919751:15840
Hubbard loamy sand, loamy substratum, 6 to 12 percent slopesHsC598422152g58twi10919751:15840
Hubbard loamy sand, river valleys, 0 to 3 percent slopes, occasionally flooded702A245931821982yt31wi14119711:12000

Map of Series Extent

Approximate geographic distribution of the HUBBARD 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 .