Official Series Description


Lab Data Summary

Aggregate lab data for the BONNER soil series. This aggregation is based on all pedons with a current taxon name of BONNER, 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 BONNER 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
43A68C0096S1968WA065001Bonner7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties48.0901299,-117.6341476
4478P054778ID017002Bonner7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.9791679,-116.8525009
4478P055378ID017008Bonner6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties48.0266685,-116.8308334
4486P033686ID017002Bonner7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties48.0833321,-116.7916641
4468C0095S1968ID017001Bonner7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties48.1668053,-117.0141296
n/a68C0097S1968WA065002BONNER6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

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

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

Click the image to view it full size.

Click the image to view it full size.

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

Competing Series

Soil series competing with BONNER 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 BONNER 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 BONNER 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 BONNER, 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 BONNER 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
Bonner silt loam, cool, 0 to 4 percent slopes428980152996546cid60419811:24000
Bonner gravelly ashy silt loam, 0 to 4 percent slopes227139152974545nid60419811:24000
Kootenai-Bonner gravelly silt loams, 0 to 20 percent slopes254728152980545vid60419811:24000
Bonner gravelly silt loam, 30 to 65 percent slopes331181529855460id60419811:24000
Rathdrum-Bonner ashy silt loams, 0 to 8 percent slopes452483153002546kid60419811:24000
Bonner-Dufort outwash terraces, complex, 0 to 6 percent slopes2yxtj105531656342yxtjid60419811:24000
Kootenai-Bonner complex, 0 to 20 percent slopes12911719794192nmxid60619761:24000
Bonner gravelly silt loam, 0 to 8 percent slopes1088356793982nm7id60619761:24000
Bonner ashy silt loam, 0 to 8 percent slopes1078041793972nm6id60619761:24000
Rathdrum-Bonner complex, 0 to 7 percent slopes162830794522nnzid60619761:24000
Kootenai-Bonner gravelly silt loams, 0 to 20 percent slopes252873165648545vid60619761:24000
Bonner-Dufort outwash terraces, complex, 0 to 6 percent slopes2yxtj20331656462yxtjid60619761:24000
Rathdrum-Bonner ashy silt loams, 0 to 8 percent slopes45553165649546kid60619761:24000
Bonner silt loam, cool, 0 to 4 percent slopes546c9582936677546cid6701:24000
Bonner ashy silt loam, 0 to 8 percent slopes2nm66929366302nm6id6701:24000
Bonner gravelly silt loam, 30 to 65 percent slopes54602329366735460id6701:24000
Bonner gravelly silt loam, 0 to 8 percent slopes2nm71529366482nm7id6701:24000
Bonner ashy fine sandy loam, 0 to 8 percent slopes30305829783692v9hdwa06320121:24000
Bonner-Wapal complex, 8 to 15 percent slopes30311207783694v9hgwa06320121:24000
Bonner silt loam, 0 to 10 percent slopes353190115823359n9wa06519781:24000
Bonner cobbly silt loam, 0 to 10 percent slopes361392215823459nbwa06519781:24000
Bonner gravelly sandy loam, 30 to 65 percent slopes34679815823259n8wa06519781:24000
Bonner-Wapal complex, 8 to 15 percent slopes3031832651306v9hgwa06519781:24000
Bonner ashy fine sandy loam, 0 to 8 percent slopes3030382651305v9hdwa06519781:24000
Bonner gravelly silt loam, 0 to 10 percent slopes211129515838159t2wa65119811:24000
Bonner silt loam, 0 to 10 percent slopes201087215838059t1wa65119811:24000
Bonner ashy fine sandy loam, 0 to 8 percent slopes30304142651235v9hdwa65119811:24000

Map of Series Extent

Approximate geographic distribution of the BONNER 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 .