Official Series Description


Lab Data Summary

Aggregate lab data for the NORGE soil series. This aggregation is based on all pedons with a current taxon name of NORGE, 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 NORGE 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
80A72-OK-09-0272-OK017-09-02Norge4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.5146361,-97.997775
80A76-OK60-3276-OK119-60-32Norge4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.1212139,-97.0957889
80A81P017980OK017003Norge7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.5391655,-98.0486145
80A40A4700S1953OK117037Norge4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.2461128,-96.559166
80A40A4716S1953OK117038Norge4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.3977776,-96.710556
80A40A4717S1953OK117039Norge4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.4061127,-96.6727753
80A74-OK-60-7S1974OK119007Norge4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.1189194,-97.1016833
80A90P0953S1990OK103008Norge7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.5741653,-97.2336121

Water Balance

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

There are insufficient data to create the 3D mountains figure.

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Click the image to view it full size.

Competing Series

Soil series competing with NORGE 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 NORGE series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the NORGE 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 .

There are insufficient data to create the 2D hillslope position figure.

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 NORGE, 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. OK-2010-09-29-12 | Noble County - 2005

    Typical pattern of soils and underlying material in the Norge-Bethany-Kirkland general soil map unit (Soil Survey of Noble County, Oklahoma; 2005).

  2. OK-2010-09-29-13 | Noble County - 2005

    Typical pattern of soils and underlying material in the Milan-Norge-Bethany general soil map unit (Soil Survey of Noble County, Oklahoma; 2005).

  3. OK-2012-02-16-04 | Blaine County - February 1968

    Typical pattern of soils in associations 1, 3, 4, and 6 (Soil Survey of Blaine County, Oklahoma; February 1968).

  4. OK-2012-02-16-12 | Cleveland County - April 1987

    Typical pattern of soils and underlying material in the Renfrow-Grainola-Grant map unit and the Port-Weswood map unit (Soil Survey of Cleveland County, Oklahoma; April 1987).

  5. OK-2012-02-16-13 | Cleveland County - April 1987

    Typical pattern of soils and underlying material in the Norge-Teller-Vanoss map unit and Asher-Keokuk-Canadian map unit (Soil Survey of Cleveland County, Oklahoma; April 1987).

  6. OK-2012-02-16-33 | Garfield County - October 1967

    Typical pattern of soils in the Renfrow-Vernon-Kirkland association (Soil Survey of Garfield County, Oklahoma; October 1967).

  7. OK-2012-02-16-34 | Garfield County - October 1967

    Typical pattern of soils in the Kirkland-Bethany-Tabler association (Soil Survey of Garfield County, Oklahoma; October 1967).

  8. OK-2012-02-17-03 | Logan County - June 1960

    Soils of the Zaneis-Lucien-Chickasha and the Renfrow-Vernon-Kirkland associations on red clays, sandstone, siltstone, and alluvium. They have developed largely on the Wellington, Garber, and Hennessey formations that dip successively toward the west (Soil Survey of Logan County, Oklahoma; June 1960).

  9. OK-2012-02-17-23 | Pawnee County - March 1959

    Prairie and forest soils formed in recent alluvium, and in adjoining areas of silty and sandy mantle material (Soil Survey of Pawnee County, Oklahoma; March 1959).

  10. OK-2012-02-17-26 | Payne County - April 1987

    Typical pattern of soils and underlying material in the Agra-Coyle and Steedman-Lucien-Grainola map units (Soil Survey of Payne County, Oklahoma; April 1987).

  11. OK-2012-02-17-30 | Payne County - April 1987

    Typical pattern of soils and underlying material in the Norge-Teller-Konawa map unit (Soil Survey of Payne County, Oklahoma; April 1987).

Map Units

Map units containing NORGE 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
Norge silt loam, 1 to 3 percent slopes64012169713828942wtwcks01519701:24000
Olpe-Norge complex, 2 to 7 percent slopes8859779113828982xlh6ks01519701:24000
Norge silt loam, 3 to 7 percent slopes6402608413828952wtwdks01519701:24000
Norge silty clay loam, 3 to 7 percent slopes, eroded6403476813828962wtwfks01519701:24000
Norge silt loam, 0 to 1 percent slopes6400306413828932wtwbks01519701:24000
Norge silt loam, 1 to 3 percent slopes64012054213829532wtwcks03519771:24000
Norge silt loam, 3 to 7 percent slopes6402762213829542wtwdks03519771:24000
Norge silty clay loam, 3 to 7 percent slopes, eroded6403348413829552wtwfks03519771:24000
Olpe-Norge complex, 2 to 7 percent slopes885957313829572xlh6ks03519771:24000
Norge loam, 1 to 3 percent slopesNoB146793817542tp5bok01119651:24000
Norge loam, 0 to 1 percent slopesNoA7565381753dt7mok01119651:24000
Norge loam, 3 to 5 percent slopesNoC67383817552tp5cok01119651:24000
Norge-Pawhuska complex, 0 to 3 percent slopesNsA5226381757dt7rok01119651:24000
Norge loam, 5 to 8 percent slopesNoD11973817562tp5dok01119651:24000
Norge silt loam, 3 to 5 percent slopesNrC132793819072tp4qok01519671:24000
Norge silt loam, 1 to 3 percent slopesNrB125363819062tp4hok01519671:24000
Norge silt loam, 1 to 3 percent slopesNrB486313819662tp4hok01719721:24000
Norge silt loam, 3 to 5 percent slopesNrC459453819672tp4qok01719721:24000
Norge silt loam, 5 to 8 percent slopesNrD36553819682tp4rok01719721:24000
Norge-Ashport silt loams complex, 0 to 8 percent slopes, frequently flooded33476338210030g73ok02719841:24000
Norge silt loam, 3 to 5 percent slopes8242253821472tp4qok02719841:24000
Norge silt loam, 1 to 3 percent slopes8130783821462tp4hok02719841:24000
Norge silt loam, 5 to 8 percent slopes, eroded832992382148dtncok02719841:24000
Vanoss-Urban land-Norge complex, 0 to 3 percent slopes741295382138dtn1ok02719841:24000
Norge silt loam, 5 to 8 percent slopes856233821502tp4rok02719841:24000
Norge-Urban land complex, 3 to 8 percent slopes86310382151dtngok02719841:24000
Norge silt loam, 1 to 3 percent slopesNorB22913800572tp4hok03119651:24000
Norge silt loam, 3 to 5 percent slopesNorC19213800562tp4qok03119651:24000
Norge loam, 1 to 3 percent slopesNoB74273825092tp5bok04719651:24000
Norge loam, 3 to 5 percent slopes, erodedNoC270093825112tp5gok04719651:24000
Norge loam, 5 to 8 percent slopes, erodedNoD23898382513dv14ok04719651:24000
Norge loam, 3 to 5 percent slopesNoC14803825102tp5cok04719651:24000
Norge loam, 5 to 8 percent slopesNoD8953825122tp5dok04719651:24000
Norge silt loam, 1 to 3 percent slopes5434413825882tp4hok04919821:24000
Norge silt loam, 0 to 1 percent slopes537133825872rj9wok04919821:24000
Norge silt loam, 1 to 3 percent slopes34123813826542tp4hok05119751:24000
Norge silt loam, 3 to 5 percent slopes, eroded3548473826552tp4vok05119751:24000
Norge silt loam, 0 to 1 percent slopes3337543826532rj9wok05119751:24000
Norge silt loam, 3 to 5 percent slopes3630243827252tp4qok05319831:24000
Norge silt loam, 3 to 5 percent slopes, eroded3712913827262tp4vok05319831:24000
Norge silt loam, 1 to 3 percent slopesNorB936234812tp4hok07119651:24000
Norge silt loam, 3 to 5 percent slopesNorC886234822tp4qok07119651:24000
Norge silt loam, 3 to 5 percent slopes, erodedNorC2236234832tp4vok07119651:24000
Norge loam, 1 to 3 percent slopesNoB8363835192tp5bok08119661:24000
Norge loam, 3 to 5 percent slopesNoC5253835202tp5cok08119661:24000
Norge loam, 3 to 5 percent slopes, erodedNoC23753835212tp5gok08119661:24000
Norge silt loam, 3 to 5 percent slopes, erodedNorC283803836602tp4vok08319941:12000
Norge silt loam, 1 to 3 percent slopesNorB37053836592tp4hok08319941:12000
Norge silt loam, 0 to 1 percent slopesNorA5833836582rj9wok08319941:12000
Norge silt loam, 1 to 3 percent slopes448543839512tp4hok09919821:24000
Norge silt loam, 1 to 3 percent slopesNorB256583840952tp4hok10319941:24000
Norge silt loam, 3 to 5 percent slopes, erodedNorC2138203840972tp4vok10319941:24000
Norge silt loam, 3 to 5 percent slopesNorC74603840962tp4qok10319941:24000
Milan-Pawhuska-Norge complex, 3 to 5 percent slopes, erodedMPNC24802384081dwnqok10319941:24000
Norge-Urban land complex, 1 to 5 percent slopesNoUC11723840932tp4tok10319941:24000
Norge silt loam, 0 to 1 percent slopesNorA11373840942rj9wok10319941:24000
Norge-Urban land complex, 1 to 5 percent slopesNoUC66893843372tp4tok10919961:12000
Norge silt loam, 1 to 3 percent slopesNorB20033843382tp4hok10919961:12000
Norge silt loam, 3 to 5 percent slopes, erodedNorC212353843402tp4vok10919961:12000
Norge silt loam, 3 to 5 percent slopesNorC11423843392tp4qok10919961:12000
Norge-Pawhuska complex, 1 to 5 percent slopes4316568623438nxqxok11319751:24000
Norge silt loam, 3 to 5 percent slopes39106116234342tp4qok11319751:24000
Norge silt loam, 1 to 3 percent slopes3859236234332tp4hok11319751:24000
Norge silt loam, 3 to 5 percent slopes, eroded4152426234362tp4vok11319751:24000
Norge, Agra, and Prue soils, 3 to 8 percent slopes, gullied4217606234372yhf9ok11319751:24000
Norge silt loam, 5 to 8 percent slopes4012386234352tp4rok11319751:24000
Norge silt loam, 1 to 3 percent slopesNorB697814231812tp4hok11720071:24000
Norge silt loam, 3 to 5 percent slopes, erodedNorC2653814129982tp4vok11720071:24000
Norge silt loam, 3 to 5 percent slopesNorC453514231782tp4qok11720071:24000
Milan-Pawhuska-Norge complex, 3 to 5 percent slopes, erodedMPNC21201910057223krok11720071:24000
Norge loam, 1 to 3 percent slopesNogB3219017622tp5bok11720071:24000
Norge loam, 3 to 5 percent slopes, erodedNogC22319017642tp5gok11720071:24000
Norge loam, 3 to 5 percent slopesNogC1919017632tp5cok11720071:24000
Norge loam, 3 to 5 percent slopes, eroded3573263845322tp5gok11919831:24000
Norge loam, 1 to 3 percent slopes3350243845302tp5bok11919831:24000
Norge loam, 3 to 5 percent slopes3427583845312tp5cok11919831:24000
Norge-Urban land complex, 1 to 5 percent slopes1612293845112tp4tok11919831:24000
Norge loam, 1 to 3 percent slopes3113703846922tp5bok12519751:24000
Norge loam, 3 to 5 percent slopes3210663846932tp5cok12519751:24000

Map of Series Extent

Approximate geographic distribution of the NORGE 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 .