Official Series Description


Lab Data Summary

Aggregate lab data for the PENDEN soil series. This aggregation is based on all pedons with a current taxon name of PENDEN, 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 PENDEN 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
7381P0651S1981KS065001PENDEN7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.2619438,-99.6055527
7303N0878S2003KS055002Penden8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.1884861,-100.5375944
7306N1024S2006KS163001Penden7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.398304,-99.5579987

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the PENDEN 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 PENDEN 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 PENDEN 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 PENDEN 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 PENDEN 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 PENDEN 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 PENDEN 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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Click the image to view it full size.

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 PENDEN, 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. KS-2012-01-20-25 | Clark County - December 1982

    Typical pattern of soils in the Albion-Shellabarger association (Soil Survey of Clark County, Kansas; 1982).

  2. KS-2012-01-20-27 | Clark County - December 1982

    Typical pattern of soils in the Penden-Harney-Uly association (Soil Survey of Clark County, Kansas; 1982).

  3. KS-2012-01-20-45 | Decatur County - April 1989

    Typical pattern of soils and parent material in the Uly-Coly-Penden association (Soil Survey of Decatur County, Kansas; 1989).

  4. KS-2012-01-23-10 | Graham County - October 1986

    Typical pattern of soils and parent material in the Holdrege-Uly-Penden association (Soil Survey of Graham County, Kansas; 1986).

  5. KS-2012-01-23-11 | Graham County - October 1986

    Typical pattern of soils and parent material in the association (Soil Survey of Graham County, Kansas; 1986).

  6. KS-2012-01-23-34 | Hodgeman County - June 1973

    Pattern of soils in association 1 (Soil Survey of Hodgeman County, Kansas; 1973).

  7. KS-2012-01-23-35 | Hodgeman County - June 1973

    Pattern of soils in association 3 (Soil Survey of Hodgeman County, Kansas; 1973).

  8. KS-2012-01-23-36 | Hodgeman County - June 1973

    Pattern of soils in associations 6 and 12 (Soil Survey of Hodgeman County, Kansas; 1973).

  9. KS-2012-01-23-37 | Hodgeman County - June 1973

    Typical pattern of soils and parent materials across the Sawlog Valley, about 4 miles north of the Hodgeman-Ford County line (Soil Survey of Hodgeman County, Kansas; 1973).

  10. KS-2012-01-23-52 | Lane County - November 1972

    Pattern of soils in association 2 (Soil Survey of Lane County, Kansas; 1972).

  11. KS-2012-01-25-05 | Phillips County - September 1987

    Pattern of soils and parent material in the Holdrege-Uly association (Soil Survey of Phillips County, Kansas; 1987).

  12. KS-2012-01-25-06 | Phillips County - September 1987

    Pattern of soils and parent material in the Uly-Holdrege-Penden association (Soil Survey of Phillips County, Kansas; 1987).

  13. KS-2012-01-25-07 | Phillips County - September 1987

    Pattern of soils and parent material in the Holdrege-Uly-Wakeen association (Soil Survey of Phillips County, Kansas; 1987).

  14. KS-2012-01-26-02 | Sheridan County - March 1984

    Typical pattern of soils in the Ulysses-Colby-Keith association (Soil Survey of Sheridan County, Kansas; 1984).

  15. KS-2012-01-26-03 | Sheridan County - March 1984

    Typical pattern of soils in the Ulysses-Pendend-Colby association (Soil Survey of Sheridan County, Kansas; 1984).

  16. KS-2012-01-26-17 | Trego County - February 1990

    Pattern of soils and parent material in the Penden-Armo association (Soil Survey of Trego County, Kansas; 1990).

Map Units

Map units containing PENDEN 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
Penden clay loam, 7 to 15 percent slopes27504573313817342twdhks02519801:24000
Penden clay loam, 1 to 3 percent slopes27452044113817312twdtks02519801:24000
Penden clay loam, 3 to 7 percent slopes27471758613817322vdbzks02519801:24000
Penden clay loam, 3 to 7 percent slopes, eroded2748318513817332twdxks02519801:24000
Penden clay loam, 0 to 1 percent slopes2744258013817302twdsks02519801:24000
Penden-Canlon loams, 7 to 30 percent slopes27602601911505822twf6ks03919851:24000
Uly-Penden complex, 6 to 20 percent slopes282848611505892twd9ks03919851:24000
Campus-Penden complex, 5 to 15 percent slopes2566877311501102twfmks05119701:24000
Penden clay loam, 3 to 7 percent slopes274728511501592twd5ks05119701:24000
Penden loam, 7 to 15 percent slopes27546411501602twdkks05119701:24000
Penden-Roxbury complex, 0 to 15 percent slopes2765381061152334307nsks05519621:24000
Penden clay loam, 7 to 15 percent slopes2750357111523332twdhks05519621:24000
Penden-Tobin complex, 0 to 15 percent slopes27662469813804552twf3ks05719621:24000
Penden clay loam, 3 to 7 percent slopes27471119913804522twd5ks05719621:24000
Penden clay loam, 1 to 3 percent slopes2745384113804502twdtks05719621:24000
Penden clay loam, 7 to 15 percent slopes2750374113804542twdhks05719621:24000
Penden and Campus soils, 3 to 6 percent slopes, eroded2742271513804482twdzks05719621:24000
Penden clay loam, 0 to 1 percent slopes2744251613804492twdsks05719621:24000
Penden clay loam, 1 to 3 percent slopes, eroded2746154413804512twdvks05719621:24000
Penden clay loam, 3 to 7 percent slopes, eroded27488813804532twdxks05719621:24000
Kim-Penden silty clay loams, 3 to 6 percent slopes, eroded16436713804332yl3rks05719621:24000
Kim-Penden clay loams, 6 to 15 percent slopes16375765611506802yl3pks06319741:24000
Penden clay loam, 3 to 7 percent slopes2747845511506902twd5ks06319741:24000
Penden-Ulysses complex, 7 to 15 percent slopes2768324011506952twd8ks06319741:24000
Penden-Coly complex, 3 to 30 percent slopes2761153811506932twf1ks06319741:24000
Penden loam, 7 to 15 percent slopes275464411506912twdkks06319741:24000
Penden-Uly complex, 7 to 20 percent slopes276760711506942twd7ks06319741:24000
Penden-Bridgeport complex, 0 to 15 percent slopes275823111506922twdpks06319741:24000
Penden-Uly complex, 7 to 20 percent slopes27679254411508132twd7ks06519851:24000
Penden-Canlon loams, 7 to 30 percent slopes27601669911508122twf6ks06519851:24000
Penden loam, 3 to 7 percent slopes27531393511508112twd6ks06519851:24000
Penden clay loam, 3 to 7 percent slopes, eroded27481270011508102twdwks06519851:24000
Uly-Penden complex, 6 to 20 percent slopes2828468211508192twd9ks06519851:24000
Penden clay loam, 7 to 15 percent slopes27501143113805882twdhks06919651:24000
Penden clay loam, 3 to 7 percent slopes27471076013805862vdbzks06919651:24000
Penden clay loam, 3 to 7 percent slopes, eroded2748362113805872twdxks06919651:24000
Penden complex, 7 to 15 percent slopes, eroded2751104313805892yl3yks06919651:24000
Penden-Humbarger complex, 0 to 12 percent slopes27623987711524242twdqks08319661:24000
Penden silty clay loam, 3 to 7 percent slopes27573513411524212twdnks08319661:24000
Kim-Penden silty clay loams, 3 to 6 percent slopes, eroded16431944011523892yl3rks08319661:24000
Penden silty clay loam, 1 to 3 percent slopes27561530311524202twdmks08319661:24000
Penden silty clay loam, 0 to 1 percent slopes2755319511524192twdlks08319661:24000
Penden-Campus clay loams, 1 to 4 percent slopes2759280911524222twf0ks08319661:24000
Penden clay loam, 3 to 7 percent slopes2747124111524162twd5ks08319661:24000
Penden-Roxbury complex, 0 to 15 percent slopes276510451152425307nsks08319661:24000
Penden-Tobin complex, 0 to 15 percent slopes276676511524262twf3ks08319661:24000
Penden clay loam, 7 to 15 percent slopes275035611524182twdhks08319661:24000
Penden-Coly complex, 3 to 30 percent slopes276111911524232twf1ks08319661:24000
Penden clay loam, 3 to 7 percent slopes, eroded274810511524172twdwks08319661:24000
Penden and Campus soils, 3 to 6 percent slopes, eroded2742511524152twdzks08319661:24000
Richfield-Penden complex, 1 to 3 percent slopes17674988115228217p1dks09319611:24000
Penden clay loam, 0 to 1 percent slopes2744238211522772twdsks09319611:24000
Penden loam, 0 to 3 percent slopes2752273115227817p18ks09319611:24000
Penden-Roxbury complex, 0 to 15 percent slopes27652051152279307nsks09319611:24000
Penden clay loam, 7 to 15 percent slopes2750313805342twdhks09719831:24000
Penden clay loam, 7 to 15 percent slopes27503777011520352twdhks10119661:24000
Kim-Penden clay loams, 6 to 15 percent slopes1637452111520242yl3pks10119661:24000
Penden clay loam, 3 to 7 percent slopes2747351211520332twd5ks10119661:24000
Penden-Kim clay loams, 3 to 6 percent slopes, eroded2763348211520362twf2ks10119661:24000
Kim-Penden clay loams, 6 to 15 percent slopes, eroded1638252511520252yl3qks10119661:24000
Penden clay loam, 1 to 3 percent slopes274592111520322twdtks10119661:24000
Penden-Roxbury complex, 0 to 15 percent slopes27654761152037307nsks10119661:24000
Penden clay loam, 3 to 7 percent slopes, eroded274811911520342twdwks10119661:24000
Penden clay loam, 3 to 7 percent slopes2747121113818062vdbzks11919731:24000
Penden clay loam, 1 to 3 percent slopes274590313818052twdtks11919731:24000
Penden clay loam, 7 to 15 percent slopes275063413818082twdhks11919731:24000
Penden clay loam, 3 to 7 percent slopes, eroded27487313818072twdxks11919731:24000
Penden clay loam, 0 to 1 percent slopes27441913818042twdsks11919731:24000
Penden-Coly complex, 3 to 30 percent slopes27612587711520902twf1ks13519711:24000
Penden-Bridgeport complex, 0 to 15 percent slopes27581531211520892twdpks13519711:24000
Penden clay loam, 3 to 7 percent slopes27471224411520852twd5ks13519711:24000
Penden clay loam, 3 to 7 percent slopes, eroded2748321411520862twdwks13519711:24000
Penden loam, 7 to 15 percent slopes275486411520882twdkks13519711:24000
Penden clay loam, 7 to 15 percent slopes275052411520872twdhks13519711:24000
Penden-Humbarger complex, 0 to 12 percent slopes27626611520912twdqks13519711:24000
Kim-Penden clay loams, 6 to 15 percent slopes16375511520802yl3pks13519711:24000
Penden-Roxbury complex, 0 to 15 percent slopes2765211152092307nsks13519711:24000
Penden clay loam, 1 to 3 percent slopes27451111520842twdtks13519711:24000
Kim-Penden silty clay loams, 3 to 6 percent slopes, eroded16431011520812yl3rks13519711:24000
Uly-Penden complex, 6 to 20 percent slopes28286209111507762twd9ks13719731:24000
Penden-Canlon loams, 7 to 30 percent slopes276011011507672twf6ks13719731:24000
Penden-Uly complex, 7 to 20 percent slopes27675411507682twd7ks13719731:24000
Penden clay loam, 3 to 7 percent slopes27473713801372twd5ks14519761:24000
Penden-Humbarger complex, 0 to 12 percent slopes27621913801382twdqks14519761:24000
Uly-Penden complex, 6 to 20 percent slopes28283963311509282twd9ks14719851:24000
Penden loam, 3 to 7 percent slopes275320711509182twd6ks14719851:24000
Penden loam, 3 to 7 percent slopes27531302311502652twd6ks16319801:24000
Uly-Penden complex, 6 to 20 percent slopes28281278211502772twd9ks16319801:24000
Penden-Uly complex, 7 to 20 percent slopes276732311502682twd7ks16319801:24000
Penden-Canlon loams, 7 to 30 percent slopes276022711502672twf6ks16319801:24000
Penden loam, 7 to 15 percent slopes27546211502662twdkks16319801:24000
Penden clay loam, 3 to 7 percent slopes, eroded27484511502642twdwks16319801:24000
Penden clay loam, 3 to 7 percent slopes2747245711521362twd5ks16519781:24000
Penden clay loam, 7 to 15 percent slopes2750100111521372twdhks16519781:24000
Penden-Ulysses complex, 7 to 15 percent slopes27685876611500072twd8ks17919821:24000
Penden-Uly complex, 7 to 20 percent slopes2767530811500062twd7ks17919821:24000
Penden-Canlon loams, 7 to 30 percent slopes2760402311500052twf6ks17919821:24000
Penden loam, 3 to 7 percent slopes2753163811500042twd6ks17919821:24000
Uly-Penden complex, 6 to 20 percent slopes28285311500122twd9ks17919821:24000
Penden loam, 3 to 7 percent slopes2753644611511322twd6ks18319741:24000
Uly-Penden complex, 6 to 20 percent slopes28286311511432twd9ks18319741:24000
Penden loam, 7 to 15 percent slopes27544116211508742twdkks19519861:24000
Penden clay loam, 3 to 7 percent slopes27474067511508712twd5ks19519861:24000
Penden clay loam, 3 to 7 percent slopes, eroded27481697411508722twdwks19519861:24000
Penden-Uly complex, 7 to 20 percent slopes2767159711508752twd7ks19519861:24000
Penden loam, 3 to 7 percent slopes275354511508732twd6ks19519861:24000
Kim-Penden clay loams, 6 to 15 percent slopes163735511508612yl3pks19519861:24000
Campus-Penden complex, 5 to 15 percent slopes2566711508382twfmks19519861:24000
Penden clay loam, 0 to 1 percent slopes2744278011519462twdsks20319631:24000
Penden clay loam, 1 to 3 percent slopes274598711519472twdtks20319631:24000
Penden clay loam, 1 to 3 percent slopes, eroded274670111519482twdvks20319631:24000
Penden clay loam, 3 to 7 percent slopes274769211519492twd5ks20319631:24000

Map of Series Extent

Approximate geographic distribution of the PENDEN 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 .