Official Series Description


Lab Data Summary

Aggregate lab data for the YAGO soil series. This aggregation is based on all pedons with a current taxon name of YAGO, 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 YAGO 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
1311N0245S2010ID005002Yago6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.3517223,-112.2595704

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the YAGO 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 YAGO 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 YAGO 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 YAGO 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 flats position figure.

Competing Series

Soil series competing with YAGO 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 YAGO 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 YAGO 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 flats position figure.

Soil series sharing subgroup-level classification with YAGO, 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 YAGO 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
Yago, very bouldery surface-Manila, extremely stony surface, complex, 10 to 35 percent slopes, MLRA 133089131636222pwvlid70919761:24000
Yago, very stony surface-Toponce complex, 20 to 50 percent slopesYTD633163628n4cwid70919761:24000
Lanoak-Yago, very stony surface, complex, 5 to 20 percent slopes4268625584352pwvhid71019681:24000
Yago, very bouldery surface-Dranyon-Beaverdam complex, 5 to 30 percent slopes226014225584442pcynid71019681:24000
Broadhead-Yago, extremely stony surface, complex, 4 to 12 percent slopes15190031635202szw6id71119831:24000
Broadhead-Yago complex, 12 to 20 percent slopes161563828852s7qid71119831:24000
Broadhead-Hades-Yago complex, 4 to 20 percent slopes141426828832s7nid71119831:24000
Yago, very stony surface-Toponce complex, 20 to 50 percent slopesYTD3673173260n4cwid71119831:24000
Yago, very bouldery surface-Manila, extremely stony surface, complex, 10 to 35 percent slopes, MLRA 133089031732442pwvlid71119831:24000
Yago, very bouldery surface-Dranyon-Beaverdam complex, 5 to 30 percent slopes22605525584342pcynid71119831:24000
Yago, very stony surface-Manila-Faim complex, 20 to 50 percent slopes5491331732562rg07id71119831:24000
Yago, very bouldery surface-Manila, extremely stony surface, complex, 20 to 45 percent slopes, MLRA 43B308435431733152x01xid71220081:24000
Yago, very stony surface-Manila-Faim complex, 20 to 50 percent slopes549413926198752rg07id7131:24000
Yago, very stony surface-Toponce complex, 20 to 50 percent slopesYTD29902520244n4cwid7131:24000
Yago, very bouldery surface-Dranyon-Beaverdam complex, 5 to 30 percent slopes2260162025145972pcynid7131:24000
Broadhead-Hades-Yago, very stony surface, complex, 5 to 35 percent slopesBHE13822917057n4b7id7131:24000
Yago, very bouldery surface-Manila, extremely stony surface, complex, 10 to 35 percent slopes, MLRA 1330872424974142pwvlid7131:24000
Lanoak-Yago, very stony surface, complex, 5 to 20 percent slopes4268724974112pwvhid7131:24000
Yago-Manila-Hades complex, 20 to 40 percent slopes13344726198422v07nid7131:24000
Yago, very bouldery surface-Manila, extremely stony surface, complex, 20 to 45 percent slopes, MLRA 43B3084323629809042x01xid7131:24000
Broadhead-Yago, extremely stony surface, complex, 4 to 12 percent slopes154028304332szw6id7131:24000
Yago, very stony surface-Valmar complex, 8 to 25 percent slopes960AA24252024620g5nid7131:24000
Yago, very stony surface-Manila-Faim complex, 20 to 50 percent slopes5498731733482rg07id71419971:24000
Broadhead-Hades-Yago, very stony surface, complex, 5 to 35 percent slopesBHE823173331n4b7id71419971:24000
Broadhead-Hades-Yago complex, 4 to 20 percent slopes3047485274j8z0id71419971:24000
Broadhead-Yago complex, 12 to 20 percent slopes3125485275j8z1id71419971:24000
Yago, very stony surface-Toponce complex, 20 to 50 percent slopesYTD203173335n4cwid71419971:24000
Yago-Manila-Hades complex, 20 to 40 percent slopes133615031636172v07nid71519941:24000
Manila-Yago complex, 4 to 12 percent slopes783395485675j9cyid71519941:24000
Manila-Yago complex, 12 to 30 percent slopes791770485676j9czid71519941:24000
Yago, very stony surface-Manila-Faim complex, 20 to 50 percent slopes5496531733792rg07id71519941:24000
Yago, very bouldery surface-Dranyon-Beaverdam complex, 5 to 30 percent slopes2260166924841432pcynid7161:24000
Hades-Yago, very stony surface-Bancroft complex, 8 to 25 percent slopes2250145124846842pdj3id7161:24000
Yago, very stony surface-Toponce complex, 20 to 50 percent slopesYTD1300600032n4cwid7161:24000
Broadhead-Hades-Yago, very stony surface, complex, 5 to 35 percent slopesBHE1103599981n4b7id7161:24000
Yago, very stony surface-Valmar complex, 8 to 25 percent slopes960AA1091186067120g5nid7161:24000
Broadhead-Yago, very stony surface, complex, 12 to 35 percent slopesBYE693599987n4bfid7161:24000
Broadhead-Yago, very stony surface, complex, 4 to 12 percent slopesBYD217599986n4bdid7161:24000
Lanoak-Yago, very stony surface, complex, 5 to 20 percent slopes424231634222pwvhid7161:24000

Map of Series Extent

Approximate geographic distribution of the YAGO 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 .