Official Series Description


Lab Data Summary

Aggregate lab data for the LOUP soil series. This aggregation is based on all pedons with a current taxon name of LOUP, 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 LOUP 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
6580P018880NE149001Loup7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.5777779,-99.4786148
6588P003387NE031103Loup7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.4544449,-100.9355545
6540A2132S1977NE089003Loup6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.3299904,-98.8323364

Water Balance

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

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Competing Series

Soil series competing with LOUP 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 LOUP 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 LOUP 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.

Click the image to view it full size.

Click the image to view it full size.

Soil series sharing subgroup-level classification with LOUP, 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. NE-2012-02-13-18 | Greeley County - April 1993

    Typical pattern of soils and parent material in the Hord-Cozad and the Boel-Loup-Leshara associations (Soil Survey of Greeley County, Nebraska; April 1993).

  2. NE-2012-02-13-27 | Holt County - March 1983

    Typical pattern of soils in the Els-Valentine-Ipage association and their relationship to topography and parent material (Soil Survey of Holt County, Nebraska; March 1983).

  3. NE-2012-02-13-29 | Holt County - March 1983

    Typical pattern of soils in the Elsmere-Ipage-Loup association and their relationship to topography and parent material (Soil Survey of Holt County, Nebraska; March 1983).

  4. NE-2012-02-13-33 | Hooker County - January 1964

    Diagram showing typical topography, soils, and parent materials in Hooker County. Symbols below soil names identify range sites, as follows: CS=Choppy Sands; WL=Wet Land; Sb=Subirrigated; Sv=Sandy; So=Sands; and TB=Thin Breaks (Soil Survey of Hooker County, Nebraska; January 1964).

  5. NE-2012-02-13-63 | Nance County - July 1960

    A cross section along the eastern side of Nance County showing the relationship of the soils to the geological materials (Soil Survey of Nance County, Nebraska; July 1960).

  6. NE-2012-02-13-77 | Rock County - May 1985

    Typical pattern of soils and parent material in the Els-Valentine-Tryon association (Soil Survey of Rock County, Nebraska; May 1985).

  7. NE-2012-02-13-78 | Rock County - May 1985

    Typical pattern of soils and parent material in the Loup-Elsmere association (Soil Survey of Rock County, Nebraska; May 1985).

  8. NE-2012-02-13-99 | Sherman County - May 1990

    Typical pattern of soils and parent material in the Loup-Bolent-Barney and Gibbon-Wann-Saltine associations (Soil Survey of Sherman County, Nebraska; May 1990).

  9. NE-2012-02-14-06 | Thomas County - August 1965

    Sketch of the soil associations in Thomas County: 1. Valentine, rolling; 2. Valentine, rolling-Anselmo; 3. Valentine, hilly; 4. Valentine, hilly-Dunday; 5. Dunday-Loup (Soil Survey of Thomas County, Nebraska; August 1965).

  10. NE-2012-02-14-07 | Thomas County - August 1965

    Diagram showing typical soils and parent materials in Thomas County. Symbols below soil names identify range sites as follows: (Sa) Sands; (CS) Choppy Sands; (Sy) Sandy; (Sb) Subirrigated; (WL) Wet Land; (TB) Thin Breaks; (SwG) Shallow to Gravel (Soil Survey of Thomas County, Nebraska; August 1965).

  11. NE-2012-02-14-11 | Valley County - October 1985

    Typical pattern of soils and parent material in the Cozad-Hord and Boel-Loup-Leshara associations (Soil Survey of Valley County, Nebraska; October 1985).

  12. NE-2012-02-14-17 | Wheeler County - September 1988

    Pattern of soils and parent material in the Els-Valentine-Ipage association (Soil Survey of Wheeler County, Nebraska; September 1988).

  13. SD-2012-03-14-01 | Bennett County - May 1971

    Typical association of Valentine, Mosher, Minatare, Loup, Keith, Rosebud, Oglala, and Canyon soils in the southern part of Bennett County (Soil Survey of Bennett County, SD; 1971).

  14. SD-2012-03-15-95 | Shannon County - April 1971

    Representative pattern of soils in associations 9 and 14 (Soil Survey of Shannon County, SD; 1971).

  15. SD-2012-03-15-99 | Todd County - April 1974

    Typical pattern of soils in associations 8 and 10. Areas of association 10 are commonly within areas of association 8 (Soil Survey of Todd County, SD; 1974).

Map Units

Map units containing LOUP 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
Loup-Boel loamy sands, 0 to 3 percent slopes351082895214362fco61819761:24000
Valent-Loup complex, 0 to 9 percent slopes713542952542yvrcco61819761:24000
Loup fine sandy loam, drained, 0 to 3 percent slopes46672432426971gb98ne00319751:20000
Loup fine sandy loam, 0 to 1 percent slopes466213322159472v9vzne00319751:20000
Loup fine sandy loam, frequently ponded466957426970gb97ne00319751:20000
Loup fine sandy loam, 0 to 1 percent slopes4662123022190872v9vzne00519731:24000
Loup mucky peat467028024347312ymc9ne00519731:24000
Loup loam, occasionally flooded42661212427050gbctne01119661:20000
Loup fine sandy loam, rarely flooded43764422166592ddm4ne01119661:20000
Loup fine sandy loam, 0 to 1 percent slopes466279421000082v9vzne01719871:20000
Loup-Els complex, 0 to 3 percent slopes467566471000102zbfdne01719871:20000
Loup fine sandy loam, frequently ponded466920761000093c23ne01719871:20000
Elsmere-Loup complex, 0 to 3 percent slopes456122322191722v9vyne01719871:20000
Loup loam, 0 to 3 percent slopes4672176117000671v21wne01919671:20000
Loup fine sandy loam, 0 to 1 percent slopes4662259121004052v9vzne03119951:24000
Elsmere-Loup complex, 0 to 3 percent slopes4561194751003762v9vyne03119951:24000
Loup mucky peat4670881224333302ymc9ne03119951:24000
Gannett and Loup loams, occasionally flooded4260325116995881v1kfne04119801:20000
Loup fine sandy loam, rarely flooded4376146116997991v1s7ne07119841:20000
Loup fine sandy loam, frequently ponded466933316998001v1s8ne07119841:20000
Loup fine sandy loam, occasionally flooded42657422192622dhb3ne07119841:20000
Loup fine sandy loam, 0 to 1 percent slopes46621022192642v9vzne07119841:20000
Gannett-Loup fine sandy loams, 0 to 3 percent slopes45851662516988421v0scne07519731:24000
Gannett-Loup fine sandy loams, drained, 0 to 3 percent slopes4586430916988431v0sdne07519731:24000
Loup-Gannett loamy fine sands, frequently ponded4676151416988451v0sgne07519731:24000
Loup-Gannett loamy fine sands, drained, 0 to 3 percent slopes467774316988461v0shne07519731:24000
Loup fine sandy loam, 0 to 1 percent slopes46628822192862v9vzne07519731:24000
Elsmere-Loup complex, 0 to 3 percent slopes4561526686722v9vyne07519731:24000
Loup loam, occasionally flooded4266158216999611v1ygne07719871:20000
Loup fine sandy loam, loamy substratum, 0 to 2 percent slopes4668129017001621v24yne07920031:12000
Loup loam, 0 to 3 percent slopes46722522282392dsnpne07920031:12000
Loup fine sandy loam, 0 to 1 percent slopes4662468891001242v9vzne08919811:20000
Loup fine sandy loam, frequently ponded466994171001253c5vne08919811:20000
Elsmere-Loup complex, 0 to 3 percent slopes456140626686922v9vyne09119611:24000
Loup fine sandy loam, 0 to 1 percent slopes466226526686942v9vzne09119611:24000
Loup mucky peat467014726686952ymc9ne09119611:24000
Loup fine sandy loam, loamy substratum, 0 to 2 percent slopes46683122289032dtc3ne09319681:12000
Loup loam, occasionally flooded42661922288922dtbrne09319681:12000
Loup fine sandy loam, 0 to 1 percent slopes466298373577052v9vzne10319771:20000
Ord-Loup fine sandy loams, 0 to 1 percent slopes42489602357721d07dne10319771:20000
Loup fine sandy loam, frequently ponded4669882357706d06xne10319771:20000
Loup complex, rarely flooded4380244316992051v152ne11119711:24000
Loup fine sandy loam, 0 to 1 percent slopes466270516993712v9vzne11319691:24000
Loup fine sandy loam, occasionally flooded426549816995461v1j2ne11519861:20000
Loup fine sandy loam, 0 to 1 percent slopes466293817002212v9vzne11719661:31680
Loup mucky peat467015224332802ymc9ne11719661:31680
Loup loamy fine sand, frequently ponded46741872427418gbrpne11919811:20000
Loup fine sandy loam, rarely flooded4376622171252df35ne11919811:20000
Loup fine sandy loam, occasionally flooded4265422282702dsppne12119781:20000
Loup silt loam, occasionally flooded42671129427485gbtvne12519581:20000
Loup fine sandy loam, occasionally flooded4265657427484gbttne12519581:20000
Loup fine sandy loam, rarely flooded43762958427581gbxyne13919701:20000
Loup soils, rarely flooded4379857427582gbxzne13919701:20000
Loup loam, frequently ponded4673918427653gc08ne14119841:20000
Loup fine sandy loam, 0 to 1 percent slopes4662252681002442v9vzne14919821:20000
Loup fine sandy loam, frequently ponded466932531002453c9qne14919821:20000
Loup fine sandy loam, 0 to 1 percent slopes4662411017000051v1zwne16319871:20000
Loup loam, frequently ponded4673201217000061v1zxne16319871:20000
Loup loam, occasionally flooded4266422288722dtb3ne16319871:20000
Loup fine sandy loam, occasionally flooded4265712426841gb52ne16719801:20000
Loup loam, occasionally flooded4266547016999061v1wpne17519831:20000
Loup fine sandy loam, rarely flooded43764722288652dt9wne17519831:20000
Loup fine sandy loam, rarely flooded43761281516998511v1txne18319841:20000
Elsmere-Loup complex, 0 to 3 percent slopes45611140216998362v9vyne18319841:20000
Loup fine sandy loam, frequently ponded4669428816998521v1tyne18319841:20000
Loup fine sandy loam, 0 to 1 percent slopes466219522198882v9vzne18319841:20000
Loup loamy fine sandLp67029389672wbptsd00519761:20000
Loup loamy fine sand, frequently pondedLo2923545922wbpvsd00519761:20000
Elsmere-Loup complex, 0 to 3 percent slopesT059A267113900642v9vysd00720041:20000
Loup fine sandy loam, 0 to 2 percent slopesLo2519352752cv23sd00720041:20000
Loup fine sandy loam, 0 to 1 percent slopesT092A89813900942v9vzsd00720041:20000
Loup mucky peatT093A45713900952ymc9sd00720041:20000
Loup loam, 0 to 1 percent slopesT094A29813900961hnhtsd00720041:20000
Loup-Elsmere loamy fine sandsLe15967353013cvbjsd12119671:31680
Elsmere-Loup complex, 0 to 3 percent slopesT059A99713915522v9vysd12119671:31680
Loup fine sandy loam, 0 to 1 percent slopesT092A37913915792v9vzsd12119671:31680
Loup mucky peatT093A12913915802ymc9sd12119671:31680
Loup-Lamo complex, 0 to 3 percent slopesWe14942925524cv6psd61019651:20000
Loup fine sandy loam, 0 to 2 percent slopesLs17282582717cv3zsd61320111:24000
Elsmere-Loup complex, 0 to 3 percent slopesT059A71125827682v9vysd61320111:24000
Loup loam, 0 to 1 percent slopesT094A6125827801hv3bsd61320111:24000
Loup mucky peatT093A3825827792ymc9sd61320111:24000

Map of Series Extent

Approximate geographic distribution of the LOUP 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 .