Official Series Description


Lab Data Summary

Aggregate lab data for the JERICHO soil series. This aggregation is based on all pedons with a current taxon name of JERICHO, 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 JERICHO were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

There are insufficient data to create the lab data summary figure.


Water Balance

Monthly water balance estimated using a leaky-bucket style model for the JERICHO 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 JERICHO 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 JERICHO 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 JERICHO 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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Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

Competing Series

Soil series competing with JERICHO 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 JERICHO 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 JERICHO 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.

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 JERICHO, 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. UT-2012-03-22-01 | Box Elder County, Western Part - September 1997

    Relationship of soils and parent material in the Lembos-Acana-Kunzler general soil map unit (Soil Survey of Box Elder County Utah, Western Part; 1997).

Map Units

Map units containing JERICHO 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
Chainlink-Rouette-Jericho association3443166824062102lrvpnv70920121:24000
Jericho-Chainlink association13088224061962lrv7nv70920121:24000
Jericho-Peeko-Izar association76024515475118hyddnv76519861:24000
Amtoft-Jericho-Tecomar association302319125474990hy88nv76519861:24000
Jericho-Pequop-Yuko association7657095475123hydknv76519861:24000
Enko-Jericho association1744060474919hy5znv76519861:24000
Jericho-Peeko-Gance association7624060475120hydgnv76519861:24000
Jericho-Gance association7614030475119hydfnv76519861:24000
Jericho-Jericho silt loam association7643605475122hydjnv76519861:24000
Jericho-Pamison-Peeko association7632215475121hydhnv76519861:24000
Armespan-Jericho association158015185478663j22rnv76619941:24000
Jericho very gravelly loam, 2 to 8 percent slopes41010178478714j24dnv76619941:24000
Kyler-Amtoft-Jericho association154210037478659j22mnv76619941:24000
Gravier-Jericho association1138919478585j207nv76619941:24000
Jericho-Armespan association4117795478715j24fnv76619941:24000
Jericho association15506606478660j22nnv76619941:24000
Jericho-Xeric Torriorthents association15705237478662j22qnv76619941:24000
Jericho-Jericho, silt loam association3501726478301j1q2nv76619941:24000
Jericho-Jericho, silt loam association76889026339022rgp7nv76619941:24000
Jericho-Armespan-Jericho, moderately steep association130680922156252dcjsnv77820131:24000
Jericho-Armespan association302112722156702dcl7nv77820131:24000
Jericho-Armespan association302132076479987j3ggnv77920041:24000
Escalante-Summermute-Jericho association306019913480004j3h0nv77920041:24000
Jericho-Xeric Torriorthents association109017741479931j3dnnv77920041:24000
Armespan-Jericho association135017192479970j3fxnv77920041:24000
Jericho-Armespan-Jericho, thin surface association130610240479954j3fdnv77920041:24000
Jericho-Summermute-Escalante association13209387479963j3fpnv77920041:24000
Jericho-Armespan association, warm13056497479953j3fcnv77920041:24000
Jericho-Summermute-Armespan association32106406480029j3htnv77920041:24000
Eastmore-Armespan-Jericho association1800559594652610ry3nv77920041:24000
Armespan-Jericho-Chainlink association13013902479949j3f7nv77920041:24000
Tarnach-Jericho association40013578480107j3lbnv77920041:24000
Chainlink-Rouette-Jericho association34433227640995pj08nv77920041:24000
Jericho-Rouette association32123087480030j3hvnv77920041:24000
Tarnach-Kyler-Jericho association32532949480042j3j7nv77920041:24000
Jericho-Chainlink association13082234479956j3fgnv77920041:24000
Armespan-Jericho-Ungene association13101892479958j3fjnv77920041:24000
Jericho-Escalante-Dakent association41301682480128j3m0nv77920041:24000
Jericho-Linoyer association1298968479947j3f5nv77920041:24000
Baberwit-Jericho association3100802480008j3h4nv77920041:24000
Scalade-Jericho-Medburn association6155683114755417j3wnv77920041:24000
Acana-Jericho association, 3 to 10 percent slopes327197481237j4rsut60119851:24000
Lembos-Jericho-Scalade complex, 1 to 30 percent slopes468375481255j4scut60119851:24000
Jericho-Amtoft complex, 20 to 50 percent slopes414671481250j4s6ut60119851:24000
Jericho gravelly fine sandy loam, 4 to 15 percent slopesJaD35140482526j63cut60819811:24000
Scalade-Jericho-Medburn association, 2 to 15 percent slopes5535158482163j5qnut61119921:24000
Jericho gravelly sandy loam, dry, 2 to 8 percent slopes2917357482133j5pput61119921:24000
Jericho-Summermute-Armespan association80227313897171hn3lut61119921:24000
Jericho-Xeric Torriorthents association81138813897111hn3dut61119921:24000
Armespan-Jericho-Chainlink association7610713897121hn3fut61119921:24000

Map of Series Extent

Approximate geographic distribution of the JERICHO 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 .