Official Series Description


Lab Data Summary

Aggregate lab data for the LULA soil series. This aggregation is based on all pedons with a current taxon name of LULA, 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 LULA 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
11207N057507KS059104Lula7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.4861111,-95.1661111
11207N057607KS107103Lula7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.3166667,-95.0011111
112M05013022005MO013002Lula4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.2615111,-94.2431278
112M05013052005MO013005Lula4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.4076944,-94.2277778
112M05217032005MO217003Lula4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.3819722,-94.4710833
11208N00302007KS031105Lula7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.4035667,-95.5406278
11207N05772007KS139100Lula7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.5269444,-95.7561111
11205N0815S2005KS099001Lula6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.3725281,-95.342308
11208N0032S2007KS037107Lula7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.5755234,-94.8418198
11208N0033S2007KS099108Lula7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.372467,-95.3433075
11208N0031S2007KS207106Lula7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.8561211,-95.5569305
11208N0024S2007OK147110Lula7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.9846802,-95.8795013
116BM94097221994MO097022Lula4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.2927778,-94.3397222
116BM94097441994MO097044Lula3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.265,-94.3222222
116BM99097131999MO097013Lula4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.2789917,-94.3213583

Water Balance

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

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

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

Competing Series

Soil series competing with LULA 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 LULA 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 LULA 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 LULA, 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-2012-01-20-32 | Coffey County - July 1982

    Typical pattern of soils in Summit-Kenoma-Lula association (Soil Survey of Coffey County, Kansas; 1982).

  2. KS-2012-01-20-41 | Crawford County - December 1973

    Typical cross section of the major soils that formed in material weathered from clayey shale or limestone that is calcareous or is neutral in reaction. These soils are in associations 5, 6, and 7 (Soil Survey of Crawford County, Kansas; 1973).

  3. KS-2012-01-25-01 | Osage County - March 1985

    Typical pattern of soils and parent material in the Eram-Lula-Summit association (Soil Survey of Osage County, Kansas; 1985).

  4. OK-2012-02-17-36 | Pontotoc County - April 1973

    Pattern of soils in the Lula-Talpa-Scullin association (Soil Survey of Pontotoc County, Oklahoma; April 1973).

Map Units

Map units containing LULA 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
Lula silt loam, 0 to 1 percent slopes8795714714534111ksd7ks01919721:24000
Lula silt loam, 1 to 3 percent slopes351301571226m5dnok02319771:24000
Lula silt loam, 1 to 3 percent slopesLuB7701065152tgtyok03519681:20000
Lula silt loam, 3 to 5 percent slopesLuC1031065163kv0ok03519681:20000
Lula loam, 1 to 3 percent slopes3416535383298dvvgok06919761:24000
Claremore-Lula complex, 3 to 5 percent slopes8681838331530x5sok06919761:24000
Lula silt loam, 1 to 3 percent slopesLuB44651065622tgtyok09719721:24000
Lula silt loam, 1 to 3 percent slopes423747383949dwjgok09919821:24000
Catoosa-Shidler-Lula complex, 1 to 3 percent slopes69157623401nxpqok11319751:24000
Lula silt loam, 1 to 3 percent slopes3055156234252tgtyok11319751:24000
Lula silt loam, 1 to 3 percent slopesLulB16116759141t7xrok11720071:24000
Lula-Shidler complex, 3 to 5 percent slopesLxC19105384640dx7rok12319671:24000
Lula loam, 3 to 5 percent slopesLuC7703384638dx7pok12319671:24000
Lula loam, 1 to 3 percent slopesLuB4851384637dx7nok12319671:24000
Lula loam, 3 to 5 percent slopes, erodedLuC21991384639dx7qok12319671:24000
Lula silt loam, 1 to 3 percent slopes306621067122tgtyok14319751:12000
Lula silt loam, 1 to 3 percent slopesLuB3671067732tgtyok14519721:24000

Map of Series Extent

Approximate geographic distribution of the LULA 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 .