Official Series Description


Lab Data Summary

Aggregate lab data for the HERBMAN soil series. This aggregation is based on all pedons with a current taxon name of HERBMAN, 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 HERBMAN 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
48A87P071887CO015003Herbman7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.7999992,-105.9619446
48A09N0133S08CO069008Herbman6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.3265839,-105.5660858
48A02N0273S2001CO107006Herbman6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.9522209,-106.632225

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the HERBMAN 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 HERBMAN 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 HERBMAN 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 HERBMAN 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 flats position figure.

Competing Series

Soil series competing with HERBMAN 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 HERBMAN 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 HERBMAN 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 hills figure.

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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 HERBMAN, 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 HERBMAN 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
Herbman very gravelly sandy loam, 15 to 40 percent slopes172114497330jphxco64019841:24000
Herbman-Rock outcrop complex, 15 to 40 percent slopes181632497331jphyco64019841:24000
Rogert, very stony-Herbman-Rock outcrop complex, 30 to 70 percent slopes141419544974202tz4yco64119801:24000
Herbman-Sprucedale-Rock outcrop complex, 15 to 30 percent slopes6514804497511jpprco64119801:24000
Herbman-Sprucedale-Rock outcrop complex, 9 to 15 percent slopes643800497510jppqco64119801:24000
Rogert, very stony-Herbman-Rock outcrop complex, 30 to 70 percent slopes14126432102902tz4yco64319751:20000
Herbman-Sprucedale-Rock outcrop complex, 15 to 30 percent slopes65553210295jpprco64319751:20000
Herbman gravelly coarse sandy loam, 10 to 45 percent slopes, extremely stony65E1819506905k0gsco6481:24000
Herbman gravelly coarse sandy loam, 10 to 45 percent slopes, extremely stony65E5003106893k0gsco64919771:24000
Rogert, very stony-Herbman-Rock outcrop complex, 30 to 70 percent slopes5524775127272tz4yco65320001:24000
Herbman-Rock outcrop complex, 15 to 30 percent slopes14914512685k6h7co65320001:24000
Herbman-Rock outcrop complex, 9 to 15 percent slopes13312512686k6h8co65320001:24000
Herbman gravelly sandy loam, 3 to 9 percent slopes12259512684k6h6co65320001:24000
Herbman, moist-Kismuth complex, 25 to 65 percent slopes1204779505021jyj0co66320001:24000
Herbman very gravelly sandy loam, 25 to 65 percent slopes1193127505020jyhzco66320001:24000
Bowen family-Herbman family-Rock outcrop complex, 5 to 25 percent slopes707BK708666rsf6wy6221:24000
Cabin-Herbman complex, 6 to 40 percent slopes1399503502217jvlkwy62519851:24000
Legault family-Herbman family-Rock outcrop complex, 10 to 25 percent slopes654430708346rs2wwy6321:24000
Herbman family-Rock outcrop complex, 40 to 65 percent slopes583368708336rs2kwy6321:24000
Herbman-Zeesix families, complex, 10 to 25 percent slopes752484708356rs36wy6321:24000
Herbman family very gravelly loam, 25 to 40 percent slopes571465708337rs2lwy6321:24000

Map of Series Extent

Approximate geographic distribution of the HERBMAN 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 .