Official Series Description


Lab Data Summary

Aggregate lab data for the GREYS soil series. This aggregation is based on all pedons with a current taxon name of GREYS, 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 GREYS 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
1340A1091S1956ID081010Greys4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.8719444,-111.1191635
43B85P002884ID043001Greys6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.0869446,-111.2444458
43B40A1092S1956ID081009Greys4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.8608322,-111.0797195

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the GREYS 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 GREYS 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 GREYS 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 GREYS 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 GREYS 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 GREYS 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 GREYS 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 GREYS, 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 GREYS 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
Greys silt loam, lee side hillslope, 8 to 30 percent slopes13548184724314382mm3hid65020111:24000
Greys-Liza complex, 8 to 30 percent slopes13544179324294602mk1pid65020111:24000
Greys-Dranyon complex, 12 to 30 percent slopes43B728134824282852mhtsid65020111:24000
Greys-Liza complex, 0 to 8 percent slopes1354352324294592mk1nid65020111:24000
Greys-Dranyon complex, 2 to 12 percent slopes43B73047724283432mhwnid65020111:24000
Greys silt loam, 2 to 16 percent slopes1354545724314392mm3jid65020111:24000
Greys-Pavohroo-Sedgway association, 8 to 20 percent slopes11246826842s17id70919761:24000
Lanoak-Greys association, 12 to 20 percent slopes712677829462s9pid71119831:24000
Lanoak-Greys association, 4 to 12 percent slopes701996829452s9nid71119831:24000
Camelback-Greys complex, 20 to 30 percent slopes241494828942s80id71119831:24000
Greys-Pavohroo-Sedgway association, 8 to 20 percent slopes45110231635342v06mid71119831:24000
Greys-Pavohroo-Sedgway association, 8 to 20 percent slopes4524925202162v06mid7131:24000
Greys-Turnerville silt loams, 12 to 20 percent slopes40301317815046551kqid75819981:24000
Greys silt loam, 12 to 20 percent slopes125796202365025xs1id75819981:24000
Greys-Turnerville silt loams, 4 to 12 percent slopes4029450515046651krid75819981:24000
Greys-Dranyon complex, 12 to 30 percent slopes43B72891025185722qf5pid75819981:24000
Greys silt loam, 20 to 30 percent slopes13-C676202365125xs2id75819981:24000
Greys-Liza complex, 8 to 30 percent slopes1354454625152532qf52id75819981:24000
Greys-Robana silt loams, 12 to 20 percent slopes2764202366625xskid75819981:24000
Greys-Dranyon complex, 2 to 12 percent slopes43B7305225185732qf5qid75819981:24000
Greys-Liza complex, 0 to 8 percent slopes135433025152522qf51id75819981:24000
Greys-Turnerville silt loams, 1 to 4 percent slopes4028715046351knid75819981:24000
Greys-Robana silt loams, 4 to 12 percent slopes263058837412t4bid76219881:24000
Greys-Robana silt loams, 12 to 20 percent slopes271672837422t4cid76219881:24000
Greys-Turnerville silt loams, 4 to 12 percent slopes291463837442t4fid76219881:24000
Greys-Robana silt loams, 1 to 4 percent slopes251082837402t49id76219881:24000
Greys-Turnerville silt loams, 12 to 20 percent slopes30594837462t4hid76219881:24000
Greys-Turnerville silt loams, 1 to 4 percent slopes28420837432t4did76219881:24000
Greys silt loam, 20 to 30 percent slopes137469839542tc6id76619781:24000
Greys silt loam, 12 to 20 percent slopes122788839532tc5id76619781:24000
Greys-Turnerville silt loams, 12 to 20 percent slopes40308523706752kkwdid76619781:24000
Greys silt loam, lee side hillslope, 8 to 30 percent slopes135488125152352qf4hid76619781:24000

Map of Series Extent

Approximate geographic distribution of the GREYS 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 .