Official Series Description


Lab Data Summary

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

There are insufficient data to create the lab data summary figure.


Water Balance

Monthly water balance estimated using a leaky-bucket style model for the STRINGAM 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 STRINGAM 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 STRINGAM 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 STRINGAM 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 STRINGAM 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 STRINGAM 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 STRINGAM 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 STRINGAM, 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 STRINGAM 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
Bickmore family, stony surface-Broad Canyon, very stony surface-Stringam complex, 30 to 75 percent slopes9644531732842wxblid71220081:24000
Stringam-Wayan family, complex, 22 to 50 percent slopes8051180026634312rq50id7131:24000
Kingmine family-Ezbin-Stringam complex, 25 to 65 percent slopes955622429638562wv1zid7131:24000
Hourglass family, extremely stony surface-Stringam-Namela family, extremely stony surface, complex, 10 to 60 percent slopes809430127334352slr0id7131:24000
Booneville-Stringam complex, 10 to 35 percent slopes891356729841632x03hid7131:24000
Kingmine family, stony surface-Woodhurst family-Stringam, stony surface, complex, 30 to 65 percent slopes963349629682352wxbjid7131:24000
Bickmore family, stony surface-Broad Canyon, very stony surface-Stringam complex, 30 to 75 percent slopes964331329682372wxblid7131:24000
Stringam-Wayan family, complex, 5 to 22 percent slopes848195327334582slrwid7131:24000
Moonlight-Kingmine family-Stringam complex, 25 to 70 percent slopes991190629638732wv2zid7131:24000
Kingmine family-Stringam complex, 20 to 60 percent slopes2018165429808792x01bid7131:24000
Stringam-Hagenbarth complex, 2 to 15 percent slopes900156129841592x03cid7131:24000
Stringam-Jumpstart-Kingmine family, complex, 15 to 50 percent slopes2004138029808662x00xid7131:24000
Ezbin-Stringam complex, 10 to 30 percent slopes830137826634362rq55id7131:24000
Booneville-Stringam complex, 10 to 35 percent slopes891122031634622x03hid7161:24000
Stringam-Wayan family, complex, 5 to 22 percent slopes84811031634382slrwid7161:24000
Bickmore family, stony surface-Broad Canyon, very stony surface-Stringam complex, 30 to 75 percent slopes9642231634802wxblid7161:24000
Stringam-Swifton families complex, 10 to 40 percent slopes3315435423764422krwfid75819981:24000
Stringam-Swifton families complex, 40 to 70 percent slopes3335285023764412krwdid75819981:24000
Stringam-Sweethollow complex, 1 to 40 percent slopes43B754182928093682pxflid75819981:24000
Hourglass family, extremely stony surface-Stringam-Namela family, extremely stony surface, complex, 10 to 60 percent slopes80912928586402slr0id75819981:24000
Stringam-Judkins complex, 1 to 6 percent slopes12372202367925xszid75819981:24000
Stringam-Sweethollow complex, 1 to 40 percent slopes43B754483824976912pxflid76120181:24000
Sudpeak-Stringam, gravelly subsoil complex, 0 to 3 percent slopes124628836932t2sid76219881:24000
Stringam-Judkins complex, 1 to 6 percent slopes123447836922t2rid76219881:24000
Clinetop, stony-Stringam-Taterheap, extremely stony families, complex, 4 to 70 percent slopes6234G258828324352v10jmt6321:24000
Uinta-Meekscabin-Stringam complex, 2 to 10 percent slopes2094308216521671sg6qwy0411:24000
Uinta-Meekscabin-Stringam complex, 15 to 35 percent slopes2101687616521681sg6rwy0411:24000
Stringam-Wayan family, complex, 22 to 50 percent slopes80511328586592rq50wy62319711:20000
Booneville-Stringam complex, 10 to 35 percent slopes89111030834772x03hwy62319711:20000
Kingmine family-Ezbin-Stringam complex, 25 to 65 percent slopes9559430834852wv1zwy62319711:20000
Stringam-Wayan family, complex, 5 to 22 percent slopes8483528586652slrwwy62319711:20000
Sedimentary Conglomerate Sideslopes (South), Subalpine Fir Complex36403792554695530xwy6351:24000
Sedimentary Moraines, Subalpine Fir-Big Sagebrush Complex33463032554691530kwy6351:24000
Sedimentary Moraines, Subalpine Fir Complex33471302554692530lwy6351:24000
Foothill Moraines, Subalpine Fir Complex6342842515450531xwy6351:24000
Sedimentary Conglomerate Sideslopes (North), Subalpine Fir Complex3642262554696530zwy6351:24000
Nooney family-Stringam deep family-Rock outcrop association, 15 to 60 percent slopes, Broadly Defined32161368620356ntjhwy66119851:24000
Sedimentary Till-Mantled Sideslopes (North), Subalpine Fir Complex364117375151867530ywy66219981:24000
Sedimentary Till-Mantled Sideslopes (West), Subalpine Fir Complex364877761518735314wy66219981:24000
Sedimentary Moraines, Subalpine Fir Complex33475118151856530lwy66219981:24000
Sedimentary Moraines, Subalpine Fir-Big Sagebrush Complex33464994151855530kwy66219981:24000
Sedimentary Conglomerate Sideslopes (North), Subalpine Fir Complex36424697151868530zwy66219981:24000
Sedimentary Chugwater Sideslopes (North), Subalpine Fir Complex364345071518695310wy66219981:24000
Sedimentary Conglomerate Sideslopes (South), Subalpine Fir Complex36403520151866530xwy66219981:24000
Sedimentary Till Plains, Subalpine Fir Complex33432539151853530hwy66219981:24000
Sedimentary Till Plains, Subalpine Fir-Willow Complex33412501151852530gwy66219981:24000
Foothill Moraines, Subalpine Fir Complex63421480151897531xwy66219981:24000
Watsondraw-Stringam, families, complex, 10 to 50 percent slopes50717926334732r7ftwy66219981:24000
Tigeron, stony-Herd-Stringam families, complex, 15 to 50 percent slopes24417520151974534dwy66320121:24000
Kingmine family-Ezbin-Stringam complex, 25 to 65 percent slopes9557930834552wv1zwy66320121:24000

Map of Series Extent

Approximate geographic distribution of the STRINGAM 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 .