Official Series Description


Lab Data Summary

Aggregate lab data for the BRODALE soil series. This aggregation is based on all pedons with a current taxon name of BRODALE, 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 BRODALE 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
104UMN2328S1976MN037035 (2328)Brodale3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.6089516,-92.8740997
105UMN1355S1971MN0491355Brodale2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.4979362,-92.4818649
105UMN1555S1972MN1571555Brodale3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.1943626,-92.4774399

Water Balance

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

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

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

Competing Series

Soil series competing with BRODALE 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 BRODALE 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 BRODALE 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 BRODALE, 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

No block diagrams are available.

Map Units

Map units containing BRODALE 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
Etter-Brodale complex, 25 to 60 percent slopes1898F1595396804f9x4mn03719801:15840
Brodale-Bellechester complex, 30 to 60 percent slopes, rockyN1155F2483968952t7zfmn03719801:15840
Brodale-Rock outcrop complex, 18 to 45 percent slopes880F2263118999fb02mn03719801:15840
Brodale channery loam, deep, 30 to 60 percent slopes, rockyN150F731190002xvskmn03719801:15840
Brodale-Bellechester complex, 30 to 60 percent slopes, rockyN1155F104831190602t7zfmn04520081:12000
Brodale-Bellechester-Rock outcrop complex, 60 to 90 percent slopesN1155G35723723472t7zgmn04520081:12000
Brodale channery loam, deep, 20 to 30 percent slopesN150E9031190612xvscmn04520081:12000
Brodale flaggy fine sandy loam, 20 to 30 percent slopesN155E3123723482xvslmn04520081:12000
Brodale channery loam, deep, 30 to 60 percent slopes, rockyN150F723723532xvskmn04520081:12000
Brodale-Bellechester complex, 30 to 60 percent slopes, rockyN1155F303917130882t7zfmn04920071:12000
Brodale, flaggy-Schapville complex, 18 to 80 percent slopes, rockyN632G297517116361vg32mn04920071:12000
Brodale-Bellechester-Rock outcrop complex, 60 to 90 percent slopesN1155G34117130912t7zgmn04920071:12000
Brodale channery loam, deep, 20 to 30 percent slopesN150E19131190092xvscmn04920071:12000
Brodale flaggy fine sandy loam, 20 to 30 percent slopesN155E16617130832xvslmn04920071:12000
Brodale channery loam, deep, 30 to 60 percent slopes, rockyN150F9531190102xvskmn04920071:12000
Brodale-Bellechester complex, 30 to 60 percent slopes, rockyN1155F64933982892t7zfmn05519811:15840
Etter-Brodale complex, rocky, 25 to 50 percent slopes1898F1856398247fcdpmn05519811:15840
Brodale channery loam, deep, 20 to 30 percent slopesN150E28624008022xvscmn10919771:15840
Brodale-Sogn complex, 12 to 25 percent slopes973D1643400820fg2pmn10919771:15840
Brodale-Bellechester complex, 25 to 60 percent slopes898F1276400819fg2nmn10919771:15840
Brodale-Bellechester complex, 30 to 60 percent slopes, rockyN1155F107631190152t7zfmn10919771:15840
Brodale flaggy fine sandy loam, 20 to 30 percent slopesN155E4234008012xvslmn10919771:15840
Brodale channery loam, deep, 30 to 60 percent slopes, rockyN150F24431190142xvskmn10919771:15840
Brodale-Eyota complex, 12 to 35 percent slopes1116F2256429542gdz6mn13119961:12000
Brodale-Bellechester complex, 30 to 60 percent slopes, rockyN1155F72422162062t7zfmn15720081:12000
Brodale-Bellechester-Rock outcrop complex, 60 to 90 percent slopesN1155G2422161702t7zgmn15720081:12000
Brodale flaggy fine sandy loam, 20 to 30 percent slopesN155E322162132xvslmn15720081:12000
Brodale flaggy loam, 20 to 50 percent slopes488F135816771281t95xmn16319781:15840
Brodale-Bellechester complex, 30 to 60 percent slopes, rockyN1155F86574290612t7zfmn16919871:20000
Bellechester-Brodale complex, rocky, 15 to 60 percent slopes898F822429101gdhzmn16919871:20000
Brodale channery loam, deep, 30 to 60 percent slopes, rockyN150F631190192xvskmn16919871:20000
Brodale-Bellechester-Rock outcrop complex, 60 to 90 percent slopes1155G221325616722t7zgwi01119601:12000
Brodale-Bellechester-Rock outcrop complex, 60 to 90 percent slopes1155G196725014212t7zgwi02319601:12000
Brodale, deep-Lacrescent, very stony-Rock outcrop complex, 60 to 90 percent slopes1150G334431190232xvsjwi04319591:20000
Brodale-Bellechester-Rock outcrop complex, 60 to 90 percent slopes1155G74828098302t7zgwi04319591:20000
Brodale-Bellechester-Rock outcrop complex, 60 to 90 percent slopes1155G32825014222t7zgwi06320011:12000
Brodale-Bellechester complex, 30 to 60 percent slopes, rocky1155F75825144422t7zfwi08119811:12000
Brodale-Bellechester-Rock outcrop complex, 60 to 90 percent slopes1155G71225014232t7zgwi09119981:12000
Brodale-Bellechester-Rock outcrop complex, 60 to 90 percent slopes1155G102016910112t7zgwi09320061:12000
Brodale-Bellechester-Rock outcrop complex, 60 to 90 percent slopes1155G9025014242t7zgwi10320021:12000
Brodale-Bellechester-Rock outcrop complex, 60 to 90 percent slopes1155G28025014252t7zgwi12319651:12000

Map of Series Extent

Approximate geographic distribution of the BRODALE 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 .