Official Series Description


Lab Data Summary

Aggregate lab data for the JACOT soil series. This aggregation is based on all pedons with a current taxon name of JACOT, 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 JACOT 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
43A79-ID-1812179ID057001Jacot4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.8119431,-116.3611908
43A92P097092ID035032Jacot6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.5533333,-115.7288895
43A05N0113S2004ID057001Jacot6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.7957764,-116.8160019
43A16N1904S2016ID057002AJacot6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.9076694,-116.4858222
43A16N1905S2016ID057002BJacot6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.9076694,-116.4858222
43A16N1906S2016ID057002CJacot6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.9076694,-116.4858222
43A16N1907S2016ID057002DJacot6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.9076694,-116.4858222
43A16N1908S2016ID057002EJacot6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.9076694,-116.4858222
43A16N1909S2016ID057002FJacot6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.9076694,-116.4858222
43A16N1910S2016ID057002GJacot6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.9076694,-116.4858222
43A16N1918S2016ID057004AJacot6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.9117833,-116.4861889
43A16N1919S2016ID057004BJacot6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.9117833,-116.4861889
43A16N1920S2016ID057004CJacot6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.9117833,-116.4861889
43A16N1921S2016ID057004DJacot6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.9117833,-116.4861889
43A16N2077S2016ID057004EJacot6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.9117833,-116.4861889
43A16N1922S2016ID057004FJacot6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.9117833,-116.4861889
43A16N2078S2016ID057004GJacot6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.9117833,-116.4861889
43A17N0015S2016ID057005AJacot6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.9147556,-116.4456972
43A17N0016S2016ID057005BJacot6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.9147556,-116.4456972
43A17N0017S2016ID057005CJacot6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.9147556,-116.4456972
43A17N0018S2016ID057005DJacot6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.9147556,-116.4456972
43A17N0019S2016ID057005EJacot6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.9147556,-116.4456972
43A17N0020S2016ID057005FJacot6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.9147556,-116.4456972
43A17N0021S2016ID057005GJacot6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.9147556,-116.4456972

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the JACOT 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 JACOT 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 JACOT 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 JACOT 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 terrace figure.

There are insufficient data to create the 3D flats position figure.

Competing Series

Soil series competing with JACOT 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 JACOT 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 JACOT 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 .

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

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 JACOT, 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 JACOT 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
Jacot, warm-Mushel complex, 35 to 70 percent slopesJm26942644910pn2kid05720131:24000
Jacot-Vassar-Lado complex, 30 to 70 percent slopesJb2692516892561tpt4id05720131:24000
Jacot, cool-Brequito-Jacot, warm complex, 30 to 65 percent slopesJb43325644904pn2cid05720131:24000
Jacot-Mushel complex, 35 to 70 percent slopesJm13036644908pn2hid05720131:24000
Jacot-Lado-Vassar complex, 10 to 30 percent slopesJb1300716892551tpt3id05720131:24000
Vassar-Jacot-Aldermand complex, 30 to 65 percent slopesJb5299116892571tpt5id05720131:24000
Keeler-Jacot complex, 30 to 55 percent slopesJg4j1687250197254ppid05720131:24000
Jacot-Vassar complex, 10 to 30 percent slopesJm31424814010wb1did05720131:24000
Jacot, warm-Bouldercreek-Jacot, warm, moist complex, 35 to 60 percent slopesBj11400644261pmdmid05720131:24000
Jacot-Bouldercreek complex, 35 to 65 percent slopesBj2974644262pmdnid05720131:24000
Vassar-Jacot complex, 8 to 30 percent slopesJj167816892581tpt6id05720131:24000
Cassyhill-Noil-Jacot complex, 45 to 90 percent slopesIh1527704713rn9pid05720131:24000
Jacot-Garveson complex, 35 to 65 percent slopesJg3j8225019712w2gtid05720131:24000
Jacot-Hysing complex, dry, 3 to 15 percent slopes51407326629492wftid60419811:24000
Jacot-Hysing complex, 15 to 30 percent slopes51416026629502wfvid60419811:24000
Jacot-Hysing complex, 30 to 55 percent slopes5142165526629142wfwid60619761:24000
Jacot-Hysing complex, 15 to 30 percent slopes5141130026629132wfvid60619761:24000
Jacot-Hysing complex, dry, 15 to 30 percent slopes514361026629152wfxid60619761:24000
Jacot-Hysing complex, dry, 30 to 55 percent slopes5144473099007nvf1id60619761:24000
Jacot-Hysing complex, dry, 3 to 15 percent slopes51401726629112wftid60619761:24000
Jacot-Garveson ashy silt loams, 10 to 35 percent slopes52461015346754pkid60819941:24000
Jacot-Garveson complex, 35 to 65 percent slopes5344121534682w2gtid60819941:24000
Jacot ashy silt loam, 35 to 65 percent slopes50425915346554phid60819941:24000
Keeler-Jacot complex, 30 to 55 percent slopes56351915347154ppid60819941:24000
Jacot-Blackprince complex, 35 to 65 percent slopes51299215346654pjid60819941:24000
Jacot-Garveson complex, 15 to 35 percent slopes1181777776690v26jid61220031:24000
Jacot-Garveson complex, 35 to 65 percent slopes11916297766912w2gtid61220031:24000
Keeler-Jacot complex, 30 to 55 percent slopes137217776695v26pid61220031:24000
Jacot ashy silt loam, 35 to 65 percent slopes54ph288285098454phid6701:24000
Jacot-Hysing complex, 30 to 55 percent slopes51429837859592wfwwa06320121:24000
Jacot-Hysing complex, 15 to 30 percent slopes51418835859582wfvwa06320121:24000
Jacot-Hysing complex, dry, 15 to 30 percent slopes51434024859602wfxwa06320121:24000
Jacot-Hysing complex, dry, 3 to 15 percent slopes51403052859572wftwa06320121:24000
Jacot, dry-Micapeak complex, 30 to 55 percent slopes50531529858912wcpwa06320121:24000
Jacot-Hysing complex, dry, 30 to 55 percent slopes5144588621210nvf1wa06320121:24000
Jacot-Hysing complex, dry, 3 to 15 percent slopes51409626513332wftwa06519781:24000
Jacot-Hysing complex, 30 to 55 percent slopes51422226513342wfwwa06519781:24000
Jacot-Hysing complex, 30 to 55 percent slopes514233826512572wfwwa65119811:24000
Jacot-Hysing complex, dry, 15 to 30 percent slopes514310226512582wfxwa65119811:24000
Jacot-Hysing complex, dry, 3 to 15 percent slopes51403526512552wftwa65119811:24000
Jacot-Hysing complex, 15 to 30 percent slopes51411826512562wfvwa65119811:24000

Map of Series Extent

Approximate geographic distribution of the JACOT 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 .