Official Series Description


Lab Data Summary

Aggregate lab data for the ROBIN soil series. This aggregation is based on all pedons with a current taxon name of ROBIN, 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 ROBIN were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

Click the image to view it full size.

Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
1393P004892ID011001Robin7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.0516663,-111.7777786
1393P004992ID011001ARobin7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.0516663,-111.7777786
1393P005092ID011001BRobin7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.0516663,-111.7777786
1393P005192ID011001CRobin7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.0516663,-111.7777786
1393P005292ID011001DRobin6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.0516663,-111.7777786
1393P005392ID011002Robin7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.0891685,-111.8041687
1393P005492ID011002ARobin7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.0891685,-111.8041687
1393P005592ID011002BRobin7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.0891685,-111.8041687
1393P005692ID011002CRobin7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.0891685,-111.8041687
1393P005792ID011002DRobin7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.0891685,-111.8041687
1340A1045S1964ID011038Robin5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.1763878,-111.7738876
1313N97448S2013ID029003Robin7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.846362,-112.086236
n/a40A1046S1964ID011039Robin5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

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

Click the image to view it full size.



Click the image to view it full size.

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the ROBIN series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

Click the image to view it full size.

Select annual climate data summaries for the ROBIN series and siblings. 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 ROBIN 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 .

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

Competing Series

Soil series competing with ROBIN share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

Click the image to view it full size.

Select annual climate data summaries for the ROBIN 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 ROBIN 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.

Click the image to view it full size.

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 ROBIN, 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. ID-2011-06-01-04 | Bingham Area - 1973

    Representative pattern of soils in association 4 (Soil Survey of Bingham Area, Idaho; 1973).

  2. ID-2011-06-01-09 | Bingham Area - 1973

    Representative pattern of soils in association 9 (Soil Survey of Bingham Area, Idaho; 1973).

Map Units

Map units containing ROBIN 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
Lanoak family-Robin complex, 10 to 35 percent slopes30787231636212ppdhid70919761:24000
Robin-Davtone family, complex, 5 to 30 percent slopes56328031636252pwvqid70919761:24000
Robin silt loam, steepRKG1763828132s5did71019681:24000
Robin silt loam, 20 to 30 percent slopesRKF1530828122s5cid71019681:24000
Robin silt loam, 4 to 20 percent slopesRKE1434828112s5bid71019681:24000
Lanoak family-Robin complex, 10 to 35 percent slopes30725131732322ppdhid71019681:24000
Lanoak family-Robin complex, 10 to 35 percent slopes3076131732432ppdhid71119831:24000
Jedediah family-Robin complex, 10 to 40 percent slopes, MLRA 133091531732452q7wgid71119831:24000
Lanoak family-Robin complex, 10 to 35 percent slopes307686924929712ppdhid7131:24000
Jedediah family-Robin complex, 10 to 40 percent slopes, MLRA 13309399625086322q7wgid7131:24000
Dranburn-Robin complex, 15 to 45 percent slopes43-F299429170632sltkid7131:24000
Robin-Davtone family, complex, 5 to 30 percent slopes563217824974162pwvqid7131:24000
Jedediah family-Robin complex, 10 to 40 percent slopes, MLRA 43B309434429809052x01yid7131:24000
Hagenbarth-Lanark-Robin complex, 2 to 15 percent slopes60502629810682xxddid7131:24000
Lanark-Hagenbarth-Robin complex, 0 to 5 percent slopes870A1729810722618zid7131:24000
Dranburn-Robin complex, 15 to 45 percent slopes43301631635682sltkid71419971:24000
Lanoak family-Robin complex, 10 to 35 percent slopes30714431733642ppdhid71519941:24000
Lanark-Hagenbarth-Robin complex, 0 to 5 percent slopes870A585720270272618zid7161:24000
Hagenbarth-Lanark-Robin complex, 2 to 15 percent slopes6050418630740312xxddid7161:24000
Jedediah family-Robin complex, 10 to 40 percent slopes, MLRA 13309428586342q7wgid75819981:24000
Robin silt loam, 4 to 30 percent slopes464588841942tlyid76919781:24000
Robin silt loam, rollingRNF36559800062p7vid77019681:24000
Robin silt loam, 4 to 12 percent slopesRoD17999800152p84id77019681:24000
Robin-Gilispie complex, rollingRPF16290800082p7xid77019681:24000
Robin-Woolsted-Lanark complex, 0 to 4 percent slopes60551070332389002z9l7id77019681:24000
Robin silt loam, 0 to 4 percent slopesRoB3173800142p83id77019681:24000
Robin-Swanner association, steepRSG1983800112p80id77019681:24000
Robin silt loam, steepRNG1838800072p7wid77019681:24000
Sheege-Robin association, hillySRF1611800242p8fid77019681:24000
Robin-Swanner association, hillyRSF1376800102p7zid77019681:24000
Sheege-Robin association, steepSRG1328800252p8gid77019681:24000
Hagenbarth-Lanark-Robin complex, 2 to 15 percent slopes6050126332389072xxddid77019681:24000
Robin silt loam, 12 to 20 percent slopesRoE1247800162p85id77019681:24000
Robin-Gilispie complex, steepRPG1042800092p7yid77019681:24000
Lanark-Robin silt loams, rollingLRF1034799402p5qid77019681:24000
Lanark-Hagenbarth-Robin complex, 0 to 5 percent slopes870A85332389112618zid77019681:24000
Jedediah family-Robin complex, 10 to 40 percent slopes, MLRA 1330915628586572q7wgwy62319711:20000

Map of Series Extent

Approximate geographic distribution of the ROBIN 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 .