Official Series Description


Lab Data Summary

Aggregate lab data for the GERST soil series. This aggregation is based on all pedons with a current taxon name of GERST, 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 GERST 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
3693P009392CO113191BGerst6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.1150017,-108.6619415
3693P009492CO113191CGerst7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.1150017,-108.6619415

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the GERST 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 GERST 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 GERST 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 GERST 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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Competing Series

Soil series competing with GERST 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 GERST 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 GERST 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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Soil series sharing subgroup-level classification with GERST, 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 GERST 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
Denco-Gerst complex, 4 to 40 percent slopes2592003629925p4h5co68619921:31680
Gerst-Walknolls, very stony complex, 10 to 60 percent slopesLYG31410017097741vd50ut0131:24000
Gerst-Clapper-Bullpen complex, 12 to 65 percent slopes, extremely stonyGME851624417082myssut0131:24000
Splimo-Gerst complex, 3 to 20 percent slopesFXD2602517096011vczfut0131:24000
Molen-Walknolls-Gerst complex, 3 to 20 percent slopesMLC390623799502kwjlut0131:24000
Gerst-Lazear-Rock outcrop complex, 4 to 20 percent slopesGSD357924822682pb05ut0131:24000
Walknolls-Gerst-Lanver complex, 5 to 60 percent slopesWRD178924402912mxb2ut0131:24000
Gerst loam, 4 to 40 percent slopes75129025037402pw0jut0131:24000
Denco-Gerst complex, 4 to 40 percent slopes6626500505609jz3zut04719991:24000
Gerst parachannery loam, 4 to 25 percent slopes7418192505618jz48ut04719991:24000
Gerst-Rock outcrop complex, 4 to 40 percent slopes774492505621jz4cut04719991:24000
Gerst loam, 4 to 40 percent slopes752602505619jz49ut04719991:24000
Gerst-Bullpen complex, 2 to 40 percent slopes76708505620jz4but04719991:24000
Walknolls-Gerst-Lanver complex, 5 to 60 percent slopesWRD3430438382mxb2ut04719991:24000
Molen-Walknolls-Gerst complex, 3 to 20 percent slopesMLC930438372kwjlut04719991:24000
Travessilla-Rock outcrop-Gerst complex12143657503696jx48ut61619831:24000
Gerst-Badland-Stormitt complex3520747503726jx57ut61619831:24000
Gerst-Strych-Badland complex, 50 to 70 percent slopes3710054503728jx59ut61619831:24000
Gerst-Badland-Rubbleland complex, 15 to 50 percent slopes338734503724jx55ut61619831:24000
Gerst-Travessilla complex385102503729jx5but61619831:24000
Gerst-Strych-Badland complex, 3 to 50 percent slopes364692503727jx58ut61619831:24000
Gerst-Badland-Rubbleland complex, 50 to 70 percent slopes344529503725jx56ut61619831:24000
Hideout-Gerst-Kaiar association, 3 to 30 percent slopes06749392504782jy89ut62320111:24000
Lazear-Gerst-Pacon complex, 3 to 35 percent slopes08345360504901jyd4ut62320111:24000
Gerst-Strych-Badland complex, 30 to 70 percent slopes05136042504902jyd5ut62320111:24000
Cedar Mountain-Lazear-Gerst complex, 5 to 30 percent slopes02732245504831jy9wut62320111:24000
Gerst-Lazear-Badland complex, 8 to 45 percent slopes04818291504907jydbut62320111:24000
Cedar Mountain-Gerst-Badland complex, 12 to 45 percent slopes02615724504909jyddut62320111:24000
Gerst-Lazear-Strych association, 15 to 60 percent slopes04915466504783jy8but62320111:24000
Gerst-Strych-Rock outcrop complex, 30 to 65 percent slopes0521001915369761nlbwut62320111:24000
Molen-Lazear-Gerst complex, 2 to 8 percent slopes1038651186027220frsut62320111:24000
Bunkin-Rock outcrop-Gerst association, 40 to 70 percent slopes01846501885368218wbut62320111:24000
Molen-Gerst complex, 20 to 45 percent slopes10213431885404218xhut62320111:24000
Gerst-Badland complex, 12 to 50 percent slopes0471244186256320j4put62320111:24000
Gerst-Tavaputs-Badland complex, 10 to 60 percent slopes053119116509281sdxrut62320111:24000
Gerst-Odome complex, 3 to 25 percent slopes050865189960221rphut62320111:24000
Hideout-Gerst-Kaiar association, 3 to 30 percent slopes31324151319410730njqut6251:24000
Cedar Mountain-Lazear-Gerst, very stony complex, 5 to 30 percent slopes3205226531938822z93mut6251:24000
Gerst family-Rock outcrop complex, 20 to 70 percent slopes531112504448jxxjut63619841:24000
Molen family-Lazear-Gerst complex, 2 to 8 percent slopes50826516302rm98ut68519901:24000
Gerst family-Cannonville-Rock outcrop,Straight Cliffs and Dakota Formation, complex, 20 to 50 percent slopes519210026728145sfpkut68620041:24000
Cushman-Gerst-Rock outcrop complex, 4 to 50 percent slopes5D32335670330zsnwy04319761:24000
Badland-Gerst-Birdsley complex, 30 to 70 percent slopes553231708932wxmswy6031:24000
Cushman-Gerst-Rock outcrop complex, 4 to 50 percent slopes5D32335825630zsnwy6171:24000
Badland-Gerst-Birdsley complex, 30 to 70 percent slopes553229690992wxmswy6291:24000
Gerst-Strych complex, 10 to 40 percent slopes1246948503968jxf1wy63819901:24000

Map of Series Extent

Approximate geographic distribution of the GERST 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 .