Official Series Description


Lab Data Summary

Aggregate lab data for the JORY soil series. This aggregation is based on all pedons with a current taxon name of JORY, 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 JORY 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
106N1044S2006OR053001Jory7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.9372978,-123.3473282
240A0867S1955OR003002JORY6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.6363907,-123.2938919
240A0864S1955OR047005JORY6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.8419456,-123.0055542
240A0865S1955OR047006JORY6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.8822212,-123.0052795
240A0929S1960OR047005JORY5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.8691673,-122.7541656
240A0930S1960OR047006JORY5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.8675003,-122.8369446
201N0510S2000OR003035Jory6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.6948051,-123.288414
201N0910S2001OR043002Jory6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.3369446,-122.9377747
201N1203S2001OR053001Jory7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.0411911,-123.1389694
201N1184S2001OR071008Jory7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.3503571,-123.0109177
201N1187S2001OR071009Jory6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.2910538,-123.0329971
201N1190S2001OR071010Jory7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.277195,-123.0508041
201N1193S2001OR071011Jory7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.2808876,-123.027916
206N0238S2005OR047001Jory7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.7889748,-122.9817429
206N0232S2005OR071004Jory7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.1942444,-123.3642578
206N0236S2005OR071008Jory7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.1942444,-123.3992615
206N0237S2005OR071009Jory7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.2009125,-123.3873138
206N1046S2006OR071006Jory7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.1245842,-123.3493881
206N1051S2006OR071011Jory7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.1418343,-123.1694717
206N1057S2006OR071017Jory7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.3838615,-123.2396393
540A0871S1955OR019002JORY6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.5475006,-123.2519455
583P0557S1983OR019001JORY6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.5597229,-123.2566681
583P0558S1983OR019002Jory6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.5436096,-123.2486115

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the JORY 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 JORY 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 JORY 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 JORY 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 JORY 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 JORY 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 JORY 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.

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 JORY, 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 JORY 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
Jory-Gelderman complex, 12 to 30 percent slopes9820155852462vpwor00320041:24000
Jory silty clay loam, sedimentary bedrock, 12 to 20 percent slopes958078853242vsdor00320041:24000
Bellpine-Jory complex, 30 to 60 percent slopes207399853182vs6or00320041:24000
Bellpine-Jory complex, 12 to 20 percent slopes186426853162vs4or00320041:24000
Bellpine-Jory complex, 20 to 30 percent slopes195360853172vs5or00320041:24000
Jory silty clay loam, basalt bedrock, 2 to 12 percent slopes914955852842vr3or00320041:24000
Jory silty clay loam, sedimentary bedrock, 2 to 12 percent slopes944730853232vscor00320041:24000
Jory silty clay loam, sedimentary bedrock, 20 to 30 percent slopes964294853252vsfor00320041:24000
Jory silty clay loam, basalt bedrock, 12 to 20 percent slopes922974853062vrtor00320041:24000
Bellpine-Jory complex, 2 to 12 percent slopes172742853152vs3or00320041:24000
Jory-Dupee complex, 2 to 12 percent slopes97918854232vwlor00320041:24000
Jory-Nekia complex, 12 to 20 percent slopes99675852812vr0or00320041:24000
Jory silty clay loam, basalt bedrock 20 to 30 percent slopes93540853072vrvor00320041:24000
Jory-Nekia complex, 20 to 30 percent slopes100396852822vr1or00320041:24000
Gelderman-Jory complex, 2 to 12 percent slopes7135612585nkftor00320041:24000
Jory silty clay loam, 12 to 20 percent slopes36D129336234922w8or05319771:20000
Jory silty clay loam, 20 to 30 percent slopes36E94566235022w9or05319771:20000
Jory silty clay loam, 2 to 12 percent slopes36C62726234822w7or05319771:20000
Jory silty clay loam, 30 to 50 percent slopes37E37516235222wcor05319771:20000
Jory silty clay loam, 2 to 30 percent slopes37D18516235122wbor05319771:20000
Jory silt loam, 2 to 12 percent slopes35C12726234522w4or05319771:20000
Jory silt loam, 12 to 20 percent slopes35D5936234622w5or05319771:20000
Jory silt loam, 20 to 30 percent slopes35E4146234722w6or05319771:20000
Jory-Bellpine complex, 12 to 20 percent slopes2747D33527111731j8bxor05319771:20000
Jory-Bellpine complex, 20 to 30 percent slopes2747E19527111691vcyxor05319771:20000
Jory-Gelderman complex, 12 to 30 percent slopes2759E16914045851j4l6or05319771:20000
Jory-Bellpine complex, 2 to 12 percent slopes2747C10627111571j8bwor05319771:20000
Jory silty clay loam, sediments, 2 to 12 percent slopes2754C9714046121j4m2or05319771:20000
Jory silty clay loam, sediments, 12 to 20 percent slopes2754D7414046131j4m3or05319771:20000
Bellpine-Jory complex, 30 to 60 percent slopes2752F6814045831j4l4or05319771:20000
Bellpine-Jory complex, 20 to 30 percent slopes2752E5014045821j4l3or05319771:20000
Jory silty clay loam, 30 to 60 percent slopes2711F4927111351j8blor05319771:20000
Gelderman-Jory complex, 12 to 20 percent slopes2748D3927111601j8bzor05319771:20000
Jory-Bellpine complex, 30 to 60 percent slopes2747F3227111501vcyyor05319771:20000
Bellpine-Jory complex, 2 to 12 percent slopes2752C2714045801j4l1or05319771:20000
Jory silty clay loam, sediments, 20 to 30 percent slopes2754E814046141j4m4or05319771:20000
Jory-Nekia complex, 20 to 30 percent slopes2718E614045751j4kwor05319771:20000
Gelderman-Jory complex, 20 to 30 percent slopes2748E427111711j8c0or05319771:20000
Bellpine-Jory complex, 12 to 20 percent slopes2752D314045811j4l2or05319771:20000
Gelderman-Jory complex, 2 to 12 percent slopes2748C127111471j8byor05319771:20000
Jory silty clay loam, 30 to 60 percent slopes23F13556145621ygor06719751:20000
Jory silty clay loam, 20 to 30 percent slopes23E6106145521yfor06719751:20000
Jory silty clay loam, 12 to 20 percent slopes23D4996145421ydor06719751:20000
Jory silty clay loam, 7 to 12 percent slopes23C4686145321ycor06719751:20000
Jory silty clay loam, 2 to 7 percent slopes23B2016145221ybor06719751:20000
Jory-Bellpine complex, 30 to 60 percent slopes2747F6427111101vcyyor06719751:20000
Jory-Bellpine complex, 20 to 30 percent slopes2747E4427111091vcyxor06719751:20000
Jory-Gelderman silt loams, 2 to 12 percent slopes2782C4027111181j8d5or06719751:20000
Jory-Bellpine complex, 2 to 12 percent slopes2747C3627111071j8bwor06719751:20000
Jory silt loam, 12 to 20 percent slopes2783D3427111191j8d6or06719751:20000
Jory-Bellpine complex, 12 to 20 percent slopes2747D3227111081j8bxor06719751:20000
Jory silt loam, 30 to 60 percent slopes2783F927111201j8d8or06719751:20000
Jory-Bellpine complex, 12 to 20 percent slopes2747D616327314411j8bxor07119671:24000
Jory-Bellpine complex, 20 to 30 percent slopes2747E543327114211vcyxor07119671:24000
Jory-Bellpine complex, 2 to 12 percent slopes2747C415827113371j8bwor07119671:24000
Jory silty clay loam, 12 to 20 percent slopes2711D289927113911j8bjor07119671:24000
Jory-Bellpine complex, 30 to 60 percent slopes2747F265627112911vcyyor07119671:24000
Jory silty clay loam, diabase, 30 to 60 percent slopes2797F260627112781vcz6or07119671:24000
Jory-Gelderman silty clay loams, 2 to 12 percent slopes2780C239427113781j8d0or07119671:24000
Jory silty clay loam, diabase, 20 to 30 percent slopes2797E162627113801vcz5or07119671:24000
Jory silty clay loam, 20 to 30 percent slopes2711E157527113081j8bkor07119671:24000
Jory silty clay loam, 30 to 60 percent slopes2711F127527113271j8blor07119671:24000
Jory silty clay loam, diabase, 2 to 12 percent slopes2796C122127314481vcz3or07119671:24000
Jory silty clay loam, diabase, 12 to 20 percent slopes2797D104127113211vcz4or07119671:24000
Gelderman-Jory complex, 2 to 12 percent slopes2748C59427112681j8byor07119671:24000
Gelderman-Jory complex, 12 to 20 percent slopes2748D54127113731j8bzor07119671:24000
Jory silty clay loam, hummocky, 5 to 30 percent slopes2812E48427113812p8vgor07119671:24000
Jory silt loam, 12 to 20 percent slopes2783D43627314451j8d6or07119671:24000
Jory-Gelderman silt loams, 2 to 12 percent slopes2782C43227113181j8d5or07119671:24000
Jory-Nekia complex, 12 to 20 percent slopes2786D40127113381j8dmor07119671:24000
Jory-Nekia complex, 2 to 12 percent slopes2786C24327113591j8dkor07119671:24000
Jory-Nekia complex, 20 to 30 percent slopes2786E21227113661j8dnor07119671:24000
Jory silt loam, 30 to 60 percent slopes2783F17827113751j8d8or07119671:24000
Jory silty clay loam, 2 to 12 percent slopes2711C17627112711qfmnor07119671:24000
Jory silt loam, 20 to 30 percent slopes2783E14627112901j8d7or07119671:24000
Gelderman-Jory complex, 20 to 30 percent slopes2748E3427314321j8c0or07119671:24000
Jory silty clay loam, 2 to 8 percent slopes45B2997561656224xor61019821:20000
Jory silty clay loam, 8 to 15 percent slopes45C1201961657224yor61019821:20000
Jory silty clay loam, 15 to 30 percent slopes45D575161658224zor61019821:20000
Jory stony silt loam, 3 to 8 percent slopes46B2360616602251or61019821:20000
Jory stony silt loam, 8 to 15 percent slopes46C1856616612252or61019821:20000
Jory stony silt loam, 15 to 30 percent slopes46D958616622253or61019821:20000
Jory silty clay loam, 30 to 60 percent slopes45E346616592250or61019821:20000
Jory silt loam, 30 to 60 percent slopes2783F11827110851j8d8or61019821:20000
Jory silt loam, 20 to 30 percent slopes2783E6927110841j8d7or61019821:20000
Jory-Nekia complex, 12 to 20 percent slopes2786D3127110901j8dmor61019821:20000
Jory silt loam, 12 to 20 percent slopes2783D2227110831j8d6or61019821:20000
Jory-Gelderman silt loams, 2 to 12 percent slopes2782C1727110821j8d5or61019821:20000
Jory-Nekia complex, 2 to 12 percent slopes2786C327110891j8dkor61019821:20000
Jory silty clay loam, 12 to 20 percent slopes63D7882627142381or63719811:20000
Jory silty clay loam, 2 to 12 percent slopes63C4872627132380or63719811:20000
Jory silty clay loam, 20 to 30 percent slopes63E3267627152382or63719811:20000
Bellpine-Jory complex, 30 to 60 percent slopes2752F13514215161jq6cor63719811:20000
Jory silty clay loam, sediments, 12 to 20 percent slopes2754D6514215491jq7for63719811:20000
Jory silty clay loam, sediments, 20 to 30 percent slopes2754E5214215501jq7gor63719811:20000
Jory-Nekia complex, 20 to 30 percent slopes2718E4714215411jq75or63719811:20000
Bellpine-Jory complex, 20 to 30 percent slopes2752E4614215151jq6bor63719811:20000
Bellpine-Jory complex, 12 to 20 percent slopes2752D2014215141jq69or63719811:20000
Jory silty clay loam, sediments, 2 to 12 percent slopes2754C1414215481jq7dor63719811:20000
Bellpine-Jory complex, 2 to 12 percent slopes2752C614215131jq68or63719811:20000
Jory silty clay loam, 2 to 12 percent slopes51C94156432824y3or63919831:20000
Jory silty clay loam, 12 to 20 percent slopes51D60256432924y4or63919831:20000
Jory silty clay loam, 20 to 30 percent slopes51E22056433024y5or63919831:20000
Jory silty clay loam, 30 to 50 percent slopes51F6956433124y6or63919831:20000
Jory silty clay loam, 2 to 7 percent slopesJoB119796410524pxor64319661:20000
Jory silty clay loam, 7 to 12 percent slopesJoC79516410624pyor64319661:20000
Jory silty clay loam, 12 to 20 percent slopesJoD36526410724pzor64319661:20000
Jory silty clay loam, 20 to 30 percent slopesJoE5016410824q0or64319661:20000
Jory silty clay loam, 20 to 30 percent slopes113E94866625926ydor64919941:24000
Nekia-Jory complex, 30 to 60 percent slopes160E8064664402747or64919941:24000
Jory silty clay loam, 12 to 20 percent slopes113D61226625726ybor64919941:24000
Jory-Ritner complex, 30 to 60 percent slopes114F24886626226yhor64919941:24000
Jory silty clay loam, 2 to 12 percent slopes113C15226625526y8or64919941:24000
Ritner-Jory complex, 60 to 90 percent slopes208G1291665632786or64919941:24000
Jory silty clay loam, 30 to 60 percent slopes113F9126626126ygor64919941:24000
Tishar-Jory complex, 30 to 60 percent slopes249F4866668327d2or64919941:24000
Tishar-Jory complex, 3 to 30 percent slopes249E2966668127d0or64919941:24000

Map of Series Extent

Approximate geographic distribution of the JORY 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 .