Official Series Description


Lab Data Summary

Aggregate lab data for the SAUNOOK soil series. This aggregation is based on all pedons with a current taxon name of SAUNOOK, 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 SAUNOOK 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
130B86P075086NC087005Saunook7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.4505539,-82.9616699
130B87P081787NC121001Saunook7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.1305542,-82.1522217
130B87P082887NC199005Saunook7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.8927765,-82.3438873

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the SAUNOOK 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 SAUNOOK 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 SAUNOOK 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 SAUNOOK 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 SAUNOOK 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 SAUNOOK 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 SAUNOOK 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 SAUNOOK, 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

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

  1. NC-2012-02-07-18 | Jackson County - June 1997

    Relationship of soils, aspect, parent material, and landscape position in the Evard-Cowee-Saunook-Trimont general soil map unit (Soil Survey of Jackson County, North Carolina; June 1997).

Map Units

Map units containing SAUNOOK 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
Saunook-Evard complex, 10 to 25 percent slopesSaE25050531784kvcbga63719901:20000
Saunook-Evard complex, 25 to 45 percent slopes, stonySnF19850531785kvccga63719901:20000
Saunook-Porters complex, 45 to 60 percent slopes, stonySpG7200531786kvcdga63719901:20000
Saunook-Thunder complex, 15 to 30 percent slopes, very stonyShD5183548104ldbsnc01119971:12000
Saunook loam, central mountains, 8 to 15 percent slopesSaC40775480982xpcpnc01119971:12000
Saunook loam, central mountains, 15 to 30 percent slopes, very stonySbD26985480992xpcsnc01119971:12000
Saunook-Thunder complex, 8 to 15 percent slopes, very stonyShC949548103ldbrnc01119971:12000
Saunook-Nikwasi complex, 2 to 15 percent slopesSgC812548102ldbqnc01119971:12000
Saunook loam, central mountains, 2 to 8 percent slopesSaB4295480972xpcqnc01119971:12000
Saunook silt loam, 8 to 15 percent slopes, stonySdC375481012xpcznc01119971:12000
Thunder-Saunook complex, 15 to 30 percent slopes, very boulderyTsD25548116ldc5nc01119971:12000
Thunder-Saunook complex, 30 to 50 percent slopes, very boulderyTsE10548117ldc6nc01119971:12000
Saunook silt loam, 2 to 8 percent slopesScB55481002xpcync01119971:12000
Thunder-Saunook complex, 8 to 15 percent slopes, very boulderyTsC3548115ldc4nc01119971:12000
Saunook loam, high precipitation, 15 to 30 percent slopes, stony121D55625092312xpcmnc08919741:20000
Saunook loam, high precipitation, 30 to 50 percent slopes, stony121E11025091392xpcnnc08919741:20000
Saunook loam, high precipitation, 8 to 15 percent slopes121C7325091402vx58nc08919741:20000
Saunook loam, high precipitation, 2 to 8 percent slopes121B1025091382xpclnc08919741:20000
Saunook gravelly loam, 8 to 15 percent slopesSaC39865471002xkfnnc09919911:12000
Saunook gravelly loam, 15 to 30 percent slopes, stonySbD36805471022vx53nc09919911:12000
Saunook gravelly loam, 15 to 30 percent slopesSaD27735471012vx57nc09919911:12000
Saunook gravelly loam, 2 to 8 percent slopesSaB6485470992vx56nc09919911:12000
Saunook gravelly loam, 15 to 30 percent slopes, stonySbD100415458602vx53nc11319901:12000
Saunook loam, 8 to 15 percent slopesScC59765458632vx52nc11319901:12000
Saunook gravelly loam, 30 to 50 percent slopes, stonySbE2218545861lb0fnc11319901:12000
Saunook loam, 2 to 8 percent slopesScB16785458622vx51nc11319901:12000
Saunook gravelly loam, 8 to 15 percent slopes, stonySbC14155458592vx54nc11319901:12000
Thunder-Saunook complex, 15 to 30 percent slopes, very boulderyTsD8678547597lctfnc12119971:12000
Saunook-Thunder complex, 15 to 30 percent slopes, stonySdD7761547587lct3nc12119971:12000
Saunook silt loam, 8 to 15 percent slopes, stonyScC68685475862xpcznc12119971:12000
Thunder-Saunook complex, 30 to 50 percent slopes, very boulderyTsE4739547598lctgnc12119971:12000
Thunder-Saunook complex, 8 to 15 percent slopes, very boulderyTsC2242547596lctdnc12119971:12000
Saunook silt loam, 2 to 8 percent slopesSaB14545475852xpcync12119971:12000
Saunook-Thunder complex, 30 to 50 percent slopes, stonySdE718547588lct4nc12119971:12000
Thunder-Saunook complex, 2 to 8 percent slopes, very boulderyTsB272547595lctcnc12119971:12000
Saunook loam, 15 to 30 percent slopes, stonyTsE454523904052l7dvnc17519681:15840
Saunook loam, high precipitation, 15 to 30 percent slopes, stony121D439225018062xpcmnc17519681:15840
Saunook loam, 8 to 15 percent slopesTsD346923904062l7dwnc17519681:15840
Saunook loam, high precipitation, 8 to 15 percent slopes121C146425018052vx58nc17519681:15840
Saunook loam, high precipitation, 30 to 50 percent slopes, stony121E48825018042xpcnnc17519681:15840
Saunook loam, high precipitation, 2 to 8 percent slopes121B9225018032xpclnc17519681:15840
Saunook loam, central mountains, 8 to 15 percent slopesSnC48215297412xpcpnc18920011:12000
Saunook loam, central mountains, 15 to 30 percent slopesSnD32375297422xpcrnc18920011:12000
Saunook loam, central mountains, 15 to 30 percent slopes, very stonySoD23725297442xpcsnc18920011:12000
Saunook-Nikwasi complex, 2 to 15 percent slopesSwC1558529750ks7qnc18920011:12000
Saunook loam, central mountains, 30 to 50 percent slopes, very stonySoE13865297452xpcvnc18920011:12000
Saunook loam, central mountains, 8 to 15 percent slopes, very stonySoC9255297432xpctnc18920011:12000
Saunook loam, central mountains, 2 to 8 percent slopesSnB8625297402xpcqnc18920011:12000
Saunook cobbly loam, central mountains, 8 to 15 percent slopesSkC6215297382xkfknc18920011:12000
Saunook cobbly loam, central mountains, 15 to 30 percent slopesSkD5635297392xkfjnc18920011:12000
Thunder-Saunook complex, 15 to 30 percent slopes, very boulderyTsD6277547868ld35nc19919971:12000
Thunder-Saunook complex, 30 to 50 percent slopes, very boulderyTsE4630547869ld36nc19919971:12000
Saunook-Thunder complex, 15 to 30 percent slopes, stonySdD3726547865ld32nc19919971:12000
Saunook sandy loam, 8 to 15 percent slopes, stonyScC32225478642xpcxnc19919971:12000
Thunder-Saunook complex, 8 to 15 percent slopes, very boulderyTsC1158547867ld34nc19919971:12000
Saunook sandy loam, 2 to 8 percent slopesSaB6135478632xpcwnc19919971:12000
Thunder-Saunook complex, 2 to 8 percent slopes, very boulderyTsB278547866ld33nc19919971:12000
Saunook-Urban land complex, 2 to 15 percent slopesSkC50219126202267fnc60520071:12000
Saunook gravelly loam, 8 to 15 percent slopesSaC4425563142xkfnnc60520071:12000
Saunook gravelly loam, 15 to 30 percent slopesSaD1835563152vx57nc60520071:12000
Saunook gravelly loam, 2 to 8 percent slopesSaB1365563132vx56nc60520071:12000
Saunook loam, basin, 15 to 30 percent slopes, stonySdD154565468002vx4znc60619911:12000
Saunook loam, basin, 8 to 15 percent slopes, stonySdC93175467992vx4ync60619911:12000
Saunook loam, basin, 30 to 50 percent slopes, very stonySeE36175468012vx50nc60619911:12000
Saunook loam, basin, 2 to 8 percent slopesScB32455467982vx4xnc60619911:12000
Saunook-Urban land complex, 2 to 15 percent slopesSfC250546802lbzsnc60619911:12000
Saunook loam, central mountains, 8 to 15 percent slopesSaC8475265542xpcptn09120001:24000
Saunook loam, 15 to 30 percent slopes, stonySaD4114803071lpcvtn64020071:24000
Saunook-Urban land complex, 8 to 15 percent slopes, stonySdC1114803061lpcttn64020071:24000
Saunook loam, 15 to 25 percent slopes, very stony30D37031367544l9fva00920041:24000
Saunook loam, 7 to 15 percent slopes, very stony30C36111367524l9cva00920041:24000
Saunook loam, 2 to 7 percent slopes, very stony30B6171367504l99va00920041:24000
Saunook loam, 25 to 50 percent slopes, very stony30E5721367554l9gva00920041:24000
Saunook loam, 7 to 15 percent slopes29C5561367514l9bva00920041:24000
Saunook loam, 2 to 7 percent slopes29B3731367494l98va00920041:24000
Saunook loam, 15 to 25 percent slopes29D2821367534l9dva00920041:24000
Saunook loam, 15 to 25 percent slopes, very stony40D32281370844ln2va12519921:24000
Saunook loam, 7 to 15 percent slopes, very stony40C26561370824ln0va12519921:24000
Saunook loam, 7 to 15 percent slopes39C8501370644lmfva12519921:24000
Saunook loam, 25 to 50 percent slopes, very stony40E8211370864ln4va12519921:24000
Saunook loam, 15 to 25 percent slopes39D2901370654lmgva12519921:24000
Saunook loam, 8 to 15 percent slopes41C174614742631lh2wva14120081:24000
Saunook-Thunder complex, 15 to 25 percent slopes, very stony42D59814742751lh38va14120081:24000
Saunook loam, 2 to 8 percent slopes41B57214742621lh2vva14120081:24000
Saunook loam, 15 to 25 percent slopes41D47014742641lh2xva14120081:24000
Saunook-Thunder complex, 8 to 15 percent slopes, very stony42C46314742741lh37va14120081:24000
Saunook-Thunder complex, 2 to 8 percent slopes, very stony42B1714742731lh36va14120081:24000
Thunder-Saunook complex, 15 to 35 percent slopes, very bouldery66E170225148622qdddva16320101:24000
Thunder-Saunook complex, 35 to 55 percent slopes, very bouldery66F162225148632qddfva16320101:24000
Thunder-Saunook complex, 3 to 15 percent slopes, very bouldery66C120425148612qddcva16320101:24000

Map of Series Extent

Approximate geographic distribution of the SAUNOOK 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 .