Official Series Description


Lab Data Summary

Aggregate lab data for the COMBEST soil series. This aggregation is based on all pedons with a current taxon name of COMBEST, 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 COMBEST 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
43A91P088291MT089004Combest4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.460556,-115.0338898
43A91P086091MT089015Combest6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.459446,-115.0291672

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the COMBEST 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 COMBEST 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 COMBEST 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 COMBEST 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 terrace figure.

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

Competing Series

Soil series competing with COMBEST 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 COMBEST 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 COMBEST 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 COMBEST, 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 COMBEST 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
Combest and Kadygulch families, high stream terraces and escarpments13UA1238628090342tr3pmt60319891:24000
Kadygulch-Combest families, association, colluvial aprons and alluvial fans15UA279328090412tr3xmt60319891:24000
Combest-Rubble land complex, 40 to 70 percent slopes211G1512995564576mmt60319891:24000
Combest gravelly ashy silt loam, 35 to 60 percent slopes21F14529955675771mt60319891:24000
Combest gravelly ashy silt loam, 15 to 35 percent slopes21E392995566576zmt60319891:24000
Combest gravelly ashy silt loam, 15 to 35 percent slopes21E6059580918mhh9mt61820081:24000
Winkler-Combest complex, 8 to 35 percent slopes201E332116927601ttg5mt61820081:24000
Combest gravelly ashy silt loam, 35 to 60 percent slopes21F2278580932mhhrmt61820081:24000
Winkler-Combest complex, 35 to 60 percent slopes201F100116927641ttg9mt61820081:24000
Combest-Sharrott-Rock outcrop complex, 40 to 85 percent slopes211G951796038vqbnmt61820081:24000
Combest gravelly ashy silt loam, 4 to 15 percent slopes21D907581105mhpbmt61820081:24000
Wildgen-Finleypoint-Combest complex, 8 to 30 percent slopes273E640804797w0g6mt61820081:24000
Kadygulch-Combest families, association, colluvial aprons and alluvial fans15UA029952872tr3xmt61820081:24000
Combest gravelly ashy silt loam, 35 to 60 percent slopes21F4524099202lwqcmt61919881:24000
Combest and Kadygulch families, high stream terraces and escarpments13UA9029953212tr3pmt63819851:24000
Kadygulch-Combest families, association, colluvial aprons and alluvial fans15UA829953272tr3xmt63819851:24000
Combest gravelly ashy silt loam, 15 to 35 percent slopes21E3843155898576zmt65119971:24000
Combest gravelly ashy silt loam, 35 to 60 percent slopes21F30781559005771mt65119971:24000
Combest-Rubble land complex, 40 to 70 percent slopes211G1624155887576mmt65119971:24000
Combest and Kadygulch families, high stream terraces and escarpments13UA29429953982tr3pmt65119971:24000
Combest gravelly ashy silt loam, 4 to 15 percent slopes821D7815633457p1mt65119971:24000
Kadygulch-Combest families, association, colluvial aprons and alluvial fans15UA3629954022tr3xmt65119971:24000

Map of Series Extent

Approximate geographic distribution of the COMBEST 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 .