Official Series Description


Lab Data Summary

Aggregate lab data for the JOCAL soil series. This aggregation is based on all pedons with a current taxon name of JOCAL, 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 JOCAL 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
22A84P088984CA115013Jocal7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.5708351,-121.1041641
22A91P072490CA109106Jocal6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.9166679,-119.9797211
22A96P013395CA612015Jocal6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.630574,-121.1782667
22A08N0160S07CA009006Jocal6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.3818054,-120.4303589
22A09N0865S09CA009001Jocal6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.2040558,-120.5448914
22A10N0455S2009SMM011Jocal2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.3636093,-120.4424973

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the JOCAL 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 JOCAL 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 JOCAL 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 JOCAL 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 JOCAL 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 JOCAL 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 JOCAL 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 hills figure.

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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.

Soil series sharing subgroup-level classification with JOCAL, 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 JOCAL 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
Sites-Jocal taxadjuncts, 15 to 30 percent slopes8811686461351hh29ca61220051:24000
Sites-Jocal taxadjuncts, 30 to 50 percent slopes8821393461350hh28ca61220051:24000
Sites-Jocal taxadjuncts, 2 to 15 percent slopes8801199461352hh2bca61220051:24000
Sites-Jocal taxadjuncts, 50 to 70 percent slopes88390461418hh4gca61220051:24000
Jocal loam, 8 to 15 percent slopes176yu4114065661j6n3ca61220051:24000
Sites-Jocal complex, 2 to 30 percent slopes2303160460537hg71ca61819911:24000
Mariposa-Jocal complex, 30 to 75 percent slopes, N Low Montane19030954604972xhjyca61819911:24000
Sites-Jocal-Mariposa complex, 30 to 50 percent slopes2312450460538hg72ca61819911:24000
Jocal loam, 3 to 8 percent slopes1751830460482hg58ca61819911:24000
Jocal loam, cool, 3 to 8 percent slopes1781420460485hg5cca61819911:24000
Jocal loam, 15 to 30 percent slopes1771390460484hg5bca61819911:24000
Jocal-Sites-Mariposa complex, 2 to 30 percent slopes1801295460487hg5fca61819911:24000
Jocal-Sites-Mariposa complex, 30 to 50 percent slopes1811225460488hg5gca61819911:24000
Jocal loam, cool, 8 to 30 percent slopes179800460486hg5dca61819911:24000
Jocal loam, 8 to 15 percent slopes176205460483hg59ca61819911:24000
Jocal-Fiddletown complex, 30 to 60 percent slopes8287442224554952nf4jca63020181:24000
Jocal gravelly silt loam, 8 to 30 percent slopes828688524554922nf4fca63020181:24000
Jocal loam, 8 to 15 percent slopes176yc3515460281nwrwca71319841:24000
Jocal loam, 3 to 8 percent slopes175yc3215460261nwrtca71319841:24000
Jocal loam, cool, 8 to 30 percent slopes179yc1115460301nwryca71319841:24000
Jocal-Jocal variant-Cryumbrepts, wet complex, 50 to 75 percent s lopesJZG18562464714hlksca71919821:24000
Mariposa-Jocal complex, 30 to 75 percent slopes, N Mid MontaneMAG159424647382xhjzca71919821:24000
Jocal-Sites-Mariposa complex, 2 to 30 percent slopesJYE5728464711hlkpca71919821:24000
Mariposa-Jocal complex, 2 to 30 percent slopesMAE5158464736hllhca71919821:24000
Jocal-Sites-Mariposa complex, 30 to 50 percent slopesJYF2475464713hlkrca71919821:24000
Sites-Jocal complex, 2 to 30 percent slopesSKE2254464794hlncca71919821:24000
Horseshoe-Jocal-Mariposa complex, 2 to 30 percent slopesHRE1242464685hljvca71919821:24000
Mariposa-Jocal complex, 2 to 30 percent slopes, alteredMAE5740464737hlljca71919821:24000
Jocal-Sites-Mariposa complex, 2 to 30 percent slopes, alteredJYE5551464712hlkqca71919821:24000
Sites-Jocal-Mariposa complex, 30 to 50 percent slopesSKF307464796hlnfca71919821:24000
Mariposa-Jocal complex, 30 to 75 percent slopes, N Low Montane190yc23929247692xhjyca71919821:24000
Sites-Jocal complex, 2 to 30 percent slopes, alteredSKE5222464795hlndca71919821:24000
Mariposa-Jocal complex, 30 to 75 percent slopes, C Low Montane170enf3029247712xhk0ca71919821:24000
Jocal loam, 5 to 30 percent slopes15021012464900hlrsca72419851:24000
Mariposa-Jocal complex, 30 to 75 percent slopes, C Low Montane170106554649202xhk0ca72419851:24000
Jocal loam, 30 to 50 percent slopes1519179464901hlrtca72419851:24000
Jocal-Mariposa-Umbrepts association, 30 to 75 percent slopes1544486464904hlrxca72419851:24000
Mariposa-Jocal complex, 5 to 30 percent slopes1692872464919hlsdca72419851:24000
Jocal-Hartless complex, 5 to 30 percent slopes1522288464902hlrvca72419851:24000
Jocal-Hartless complex, 30 to 50 percent slopes1532225464903hlrwca72419851:24000
Jocal-Sites loams, 5 to 30 percent slopes complex155794464905hlryca72419851:24000
Mariposa-Jocal complex, 30 to 75 percent slopes, N Mid MontaneMAGtnf529247662xhjzca72419851:24000
Jocal-Fiddletown complex, 30 to 60 percent slopes8287141431152452nf4jca73119811:24000
Jocal gravelly silt loam, 8 to 30 percent slopes828639231152442nf4fca73119811:24000

Map of Series Extent

Approximate geographic distribution of the JOCAL 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 .