Official Series Description


Lab Data Summary

Aggregate lab data for the ENKO soil series. This aggregation is based on all pedons with a current taxon name of ENKO, 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 ENKO 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
2491P018990NV013002Enko8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.0466652,-117.7186127
2587P060387ID073001Enko7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.2527771,-116.706665
2581P0763S1981NV007494ENKO6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.6957436,-115.6842422

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the ENKO 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 ENKO 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 ENKO 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 ENKO 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 ENKO 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 ENKO 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 ENKO 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 mountains figure.

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

Soil series sharing subgroup-level classification with ENKO, 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. OR-2010-09-29-04 | Harney County Area - 2006

    Soil and landscape relationship in Catlow Valley (Soil Survey of Harney County Area, Oregon; 2006).

  2. OR-2012-05-10-27 | Harney County Area - 2006

    Soil and landscape relationship in Catlow Valley (Soil Survey of Harney County Area, Oregon; 2006).

Map Units

Map units containing ENKO 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
Hardtrigger-Enko complex, 2 to 15 percent slopes7115225486256j9zpid67519921:24000
Enko-Enko, gravelly association22414626339982rhhpnv62119711:24000
Enko-Kelk association228926339972rhhnnv62119711:24000
Enko-Shabliss-Orovada association5071374426338382rgmcnv76319861:24000
Cherry Spring-Enko association272777326338332rgm6nv76319861:24000
Enko-Enko, strongly sloping association12421612477051j0drnv76319861:24000
Enko fine sandy loam, 2 to 8 percent slopes37037026338312rgm4nv76319861:24000
Grina-Enko association32275428292362t6h2nv76420211:24000
Oupico-Enko association69112645475095hycnnv76519861:24000
Valmy-Enko association59011408475061hybknv76519861:24000
Enko-Kelk-Enko, nearly level association1709115474917hy5xnv76519861:24000
Chiara-Dewar-Enko association14487854749082t6wlnv76519861:24000
Chiara-Wieland-Enko association374739026338532rgmvnv76519861:24000
Enko-Chiara-Kelk association1715600474918hy5ynv76519861:24000
Enko-Jericho association1744060474919hy5znv76519861:24000
Chuska-Dewar-Enko association2512775474965hy7gnv76519861:24000
Zapa-Enko association4072445475021hy98nv76519861:24000
Cobre-Enko association30362265474996hy8gnv76519861:24000
Toano-Enko-Sondoa association2090885474944hy6snv76519861:24000
Cobre-Enko association03821026338762rgnknv76519861:24000
Chiara-Dewar-Enko association273157234782792t6wlnv76619941:24000
Peeko-Enko-Izar association1837921478246j1n9nv76619941:24000
Cobre-Enko association3824399478321j1qqnv76619941:24000
Oupico-Enko association2803508478285j1pknv76619941:24000
Valmy-Enko association2113294478262j1ntnv76619941:24000
Enko-Kelk-Enko, nearly level association170175426338792rgnnnv76619941:24000
Chiara-Parisa-Enko association2791623478284j1pjnv76619941:24000
Enko-Kelk association1831627478706j244nv76619941:24000
Enko-Chiara-Kelk association1778426338832rgnsnv76619941:24000
Wieland-Enko association127132122478734j251nv76719861:24000
Enko-Rad association22628224478839j28fnv76719861:24000
Chiara-Wieland-Enko association37419841478893j2b5nv76719861:24000
Enko-Kelk assoication22816876478841j28hnv76719861:24000
Enko-Zevadez-Puett association2229892478835j289nv76719861:24000
Bunky-Grina-Enko association3318013478888j2b0nv76719861:24000
Enko-Enko, gravelly association2247579478837j28cnv76719861:24000
Zevadez-Enko-Puett association1356886478748j25hnv76719861:24000
Enko-Kelk-Connel association2236017478836j28bnv76719861:24000
Enko-Kelk-Enko, very fine sandy loam association2215812478834j288nv76719861:24000
Enko-Wieland-Enko, moderately steep association2274502478840j28gnv76719861:24000
Grina-Enko, moderately steep-Enko association3224152478884j29wnv76719861:24000
Enko-Hunnton association2253626478838j28dnv76719861:24000
Kelk-Kelk, occasionally flooded-Enko association1413255478749j25jnv76719861:24000
Enko-Kelk-Enko, nearly level association170178226338642rgn6nv76719861:24000
Bloor-Enko association2821254478865j298nv76719861:24000
Enko-Puett association2291027478842j28jnv76719861:24000
Enko-Orovada association, gently sloping49119035479280j2qnnv76819851:63360
Chedehap-Enko-Ricert association1506130479061j2hlnv76819851:63360
Glyphs-Enko association20155090479088j2jgnv76819851:63360
Jung-McVegas-Enko association38482945479251j2pqnv76819851:63360
Enko-Glyphs association4922790479281j2qpnv76819851:63360
Enko-Orovada association49311004792822whmtnv76819851:63360
Gwena-Enko-Frewa association128013802475199hyh0nv76919861:24000
Shabliss-Enko-Valmy association1707062475237hyj7nv76919861:24000
Cherry Spring-Enko association27221540479578j318nv77519851:24000
Enko fine sandy loam, 2 to 8 percent slopes3708000479649j33knv77519851:24000
Enko-Shabliss-Orovada association507449026338392rgmdnv77519851:24000
Enko-Puett association8237290479895j3chnv77619831:63360
Enko-Davey-McConnel association8227233479894j3cgnv77619831:63360
Enko loam, 0 to 2 percent slopes*8211075479893j3cfnv77619831:63360
Hunnton-Zevadez-Enko association117413907475431hyqhnv77719931:24000
Enko-Goldrun association5029674475761hz24nv77719931:24000
Enko very fine sandy loam, 2 to 8 percent slopes 1/5057572475764hz27nv77719931:24000
Wholan-Bliss-Enko association10237206475363hyn9nv77719931:24000
Enko very fine sandy loam, 0 to 2 percent slopes 1/5035136475762hz25nv77719931:24000
Enko loamy very fine sand, 0 to 2 percent slopes 1/5014843475760hz23nv77719931:24000
Kelk-Enko complex, 0 to 2 percent slopes 1/7332968475903hz6qnv77719931:24000
Enko-Shabliss-Orovada association5072772475766hz29nv77719931:24000
Shabliss-Enko-Dugchip association5362582475780hz2rnv77719931:24000
Enko fine sandy loam, 2 to 4 percent slopes 1/11922432475445hyqynv77719931:24000
Enko-Shabliss complex, 2 to 8 percent slopes5041701475763hz26nv77719931:24000
Enko loam, 0 to 2 percent slopes 1/1194821475446hyqznv77719931:24000
Shabliss-Enko-Valmy association532683475776hz2mnv77719931:24000
Enko-Orovada association22208204808572whmtnv78119941:24000
Enko-Catlow complex, 1 to 7 percent slopes9452555490975jgwxor62819971:24000
Enko loamy sand, 2 to 8 percent slopes9333911490974jgwwor62819971:24000
Enko-Catlow association, 2 to 20 percent slopes9627998490977jgwzor62819971:24000
Enko-Catlow complex, 7 to 15 percent slopes951826490976jgwyor62819971:24000
Enko loamy sand, 2 to 8 percent slopes2923698916898011tqcqor63520061:24000
Enko-McConnel complex, 0 to 5 percent slopes2941369616898031tqcsor63520061:24000
Firelake-Enko complex, 1 to 20 percent slopes309915116898181tqd8or63520061:24000
Enko sandy loam, 0 to 6 percent slopes290671116897991tqcnor63520061:24000
Enko loam, 1 to 10 percent slopes291430616898001tqcpor63520061:24000
Seharney-Rabbithills-Enko complex, 1 to 20 percent slopes575379716900751tqnkor63520061:24000
Enko-Catlow complex, 7 to 15 percent slopes293106616898021tqcror63520061:24000
Enko loamy sand, 2 to 8 percent slopes430B3317209781vrtfor63619911:24000
Enko loamy sand, 2 to 8 percent slopesOR009369582026336260kpor64420211:24000
Enko-Catlow association, 2 to 20 percent slopesOR009631402026338260kror64420211:24000

Map of Series Extent

Approximate geographic distribution of the ENKO 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 .