Official Series Description


Lab Data Summary

Aggregate lab data for the UNISON soil series. This aggregation is based on all pedons with a current taxon name of UNISON, 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 UNISON 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
130B86P093786NC099004Unison7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.334446,-83.2258301
130B87P082787NC199004Unison7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.8888893,-82.2125015
14800P1120S2000VA107002Unison3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.005047,-77.922928

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the UNISON 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 UNISON 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 UNISON 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 UNISON 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 UNISON 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 UNISON 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 UNISON 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 UNISON, 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-2010-09-27-02 | Burke County - 2006

    Typical relationship between soils, landform, and parent material in the Colvard-Unison and Fairview-Rhodhiss general soil map units (Soil Survey of Burke County, North Carolina; 2006).

Map Units

Map units containing UNISON 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
Unison loam, 8 to 15 percent slopesUnC95616721951t41snc02120061:12000
Unison loam, 2 to 8 percent slopesUnB75816721941t41rnc02120061:12000
Unison-Urban land complex, 2 to 8 percent slopesUrB18816721971t41vnc02120061:12000
Unison loam, 15 to 30 percent slopesUnD12116721961t41tnc02120061:12000
Unison-Urban land complex, 8 to 15 percent slopesUrC12016721981t41wnc02120061:12000
Unison fine sandy loam, 2 to 8 percent slopesUnB28861170333xs8nc02320001:24000
Unison fine sandy loam, 8 to 15 percent slopesUnC18931170343xs9nc02320001:24000
Unison fine sandy loam, 15 to 25 percent slopesUnD1491170423xsknc02320001:24000
Unison loam, 2 to 8 percent slopesUnB2581912788226dvnc07520071:12000
Unison loam, 8 to 15 percent slopesUnC841912789226dwnc07520071:12000
Unison loam, 8 to 15 percent slopesUsC68216714981t3b9nc11520061:12000
Unison loam, 2 to 8 percent slopesUsB28116714971t3b8nc11520061:12000
Unison loam, 15 to 30 percent slopesUsD26916714961t3b7nc11520061:12000
Unison loam, 8 to 15 percent slopesUsC1134547877ld3gnc19919971:12000
Unison loam, 2 to 8 percent slopesUsB778547876ld3fnc19919971:12000
Unison loam, 15 to 30 percent slopesUsD626547878ld3hnc19919971:12000
Unison loam, 2 to 5 percent slopesUnB1616526496knvrtn01920001:24000
Unison-Urban land complex, 5 to 12 percent slopesUuC1383526498knvttn01920001:24000
Unison loam, 5 to 12 percent slopesUnC1331526497knvstn01920001:24000
Unison very stony silt loam, 7 to 15 percent slopes90C1220516494kbg3va00319811:15840
Unison silt loam, 2 to 7 percent slopes89B970516490kbfzva00319811:15840
Unison very stony silt loam, 2 to 7 percent slopes90B580516493kbg2va00319811:15840
Unison silt loam, 7 to 15 percent slopes89C310516491kbg0va00319811:15840
Unison very stony silt loam, 15 to 25 percent slopes90D250516495kbg4va00319811:15840
Unison loam, 7 to 15 percent slopes, very stony44C7561367784lb6va00920041:24000
Unison loam, 7 to 15 percent slopes43C6611367774lb5va00920041:24000
Unison loam, 2 to 7 percent slopes43B4081367754lb3va00920041:24000
Unison loam, 2 to 7 percent slopes, very stony44B231367764lb4va00920041:24000
Unison fine sandy loam, 2 to 7 percent slopes86B3085518078kd36va01519781:15840
Unison fine sandy loam, 7 to 15 percent slopes, eroded86C21267518079kd37va01519781:15840
Unison cobbly fine sandy loam, 15 to 45 percent slopes87E991518083kd3cva01519781:15840
Unison cobbly fine sandy loam, 7 to 15 percent slopes87C736518082kd3bva01519781:15840
Unison cobbly fine sandy loam, 2 to 7 percent slopes87B691518081kd39va01519781:15840
Unison fine sandy loam, 15 to 25 percent slopes, eroded86D2367518080kd38va01519781:15840
Unison loam, 2 to 7 percent slopesUnB443516912kbwlva07919831:15840
Unison loam, 7 to 15 percent slopesUnC403516913kbwmva07919831:15840
Unison loam, 0 to 2 percent slopesUnA186516911kbwkva07919831:15840
Unison loam, 7 to 15 percent slopesUnC801517057kc18va11319671:15840
Unison loam, 2 to 7 percent slopesUnB592517056kc17va11319671:15840
Unison loam, 15 to 25 percent slopesUnD436517058kc19va11319671:15840
Unison very stony silt loam, 15 to 25 percent slopesUsD349517060kc1cva11319671:15840
Unison very stony silt loam, 7 to 15 percent slopesUsC165517059kc1bva11319671:15840
Unison-Urban land complex, 2 to 7 percent slopes32B2129517110kc2zva12119801:15840
Unison and Braddock soils, 2 to 7 percent slopes30B1183517106kc2vva12119801:15840
Unison and Braddock soils, 7 to 15 percent slopes30C1183517107kc2wva12119801:15840
Unison and Braddock soils, 15 to 25 percent slopes30D1092517108kc2xva12119801:15840
Unison and Braddock cobbly soils, 7 to 15 percent slopes31C981517109kc2yva12119801:15840
Unison-Urban land complex, 7 to 15 percent slopes32C534517111kc30va12119801:15840
Unison-Urban land complex, 15 to 25 percent slopes32D431517112kc31va12119801:15840
Unison loam, 2 to 7 percent slopes49B18241371184lp5va12519921:24000
Unison loam, 7 to 15 percent slopes49C10091371194lp6va12519921:24000
Unison loam, 15 to 25 percent slopes49D3981371204lp7va12519921:24000
Unison fine sandy loam, 7 to 15 percent slopes49C2737517288kc8qva13919951:20000
Unison fine sandy loam, 2 to 7 percent slopes49B1357517286kc8nva13919951:20000
Unison fine sandy loam, 15 to 25 percent slopes49D994517289kc8rva13919951:20000
Unison-Thurmont complex, 7 to 15 percent slopes, very stonyStC30195174692tmclva15719581:20000
Unison-Thurmont complex, 15 to 25 percent slopes, very stonyStD12965174702tmcmva15719581:20000
Craigsville-Unison complex, 2 to 7 percent slopes, very stonyStB9015174682w06jva15719581:20000
Unison loam, gently sloping phaseUnB524517473kcgpva15719581:20000
Unison cobbly loam, sloping phaseUcC453517472kcgnva15719581:20000
Unison loam, eroded sloping phaseUnC2305517474kcgqva15719581:20000
Unison cobbly loam, gently sloping phaseUcB271517471kcgmva15719581:20000
Unison loam, gently sloping fragipan variantUpB203517475kcgrva15719581:20000
Unison fine sandy loam, 2 to 7 percent slopes, eroded71B23070518467kdhrva16519801:20000
Unison fine sandy loam, 7 to 15 percent slopes, eroded71C21225518468kdhsva16519801:20000
Unison cobbly fine sandy loam, 7 to 15 percent slopes, eroded72C21142518470kdhvva16519801:20000
Unison cobbly fine sandy loam, 2 to 7 percent slopes, eroded72B2700518469kdhtva16519801:20000
Unison cobbly fine sandy loam, 15 to 30 percent slopes, eroded72D2673518471kdhwva16519801:20000
Unison loam, 2 to 7 percent slopes59B2860520792kgxrva17119881:15840
Unison loam, 7 to 15 percent slopes59C1116520793kgxsva17119881:15840
Unison gravelly loam, 2 to 7 percent slopes60B829520796kgxwva17119881:15840
Unison cobbly loam, 2 to 7 percent slopes61B654520798kgxyva17119881:15840
Unison cobbly loam, 7 to 15 percent slopes61C629520799kgxzva17119881:15840
Unison gravelly loam, 7 to 15 percent slopes60C626520797kgxxva17119881:15840
Unison loam, 7 to 15 percent slopes39C2661518856kdx9va18719801:15840
Unison loam, 15 to 25 percent slopes39D1427518857kdxbva18719801:15840
Unison loam, 2 to 7 percent slopes39B995518855kdx8va18719801:15840
Unison cobbly loam, 7 to 15 percent slopes40C321518859kdxdva18719801:15840
Unison-Urban land complex, 2 to 7 percent slopes586B18830257592xvcqva8201:12000
Unison cobbly fine sandy loam-Urban land complex, 15 to 45 percent slopes587E1530257662xvcrva8201:12000
Unison fine sandy loam, 15 to 25 percent slopes, eroded86D21330257652xd69va8201:12000
Unison fine sandy loam, 7 to 15 percent slopes, eroded86C2930257612xd68va8201:12000
Unison cobbly fine sandy loam, 7 to 15 percent slopes87C730257672xd6bva8201:12000
Unison fine sandy loam, 2 to 7 percent slopes86B530257622xd67va8201:12000
Unison cobbly fine sandy loam, 15 to 45 percent slopes87E130257682xd6cva8201:12000

Map of Series Extent

Approximate geographic distribution of the UNISON 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 .