Official Series Description


Lab Data Summary

Aggregate lab data for the LETCHER soil series. This aggregation is based on all pedons with a current taxon name of LETCHER, 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 LETCHER 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
55B40A28221966ND027009Letcher7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.68782,-98.96435
55B40A28231966ND027010Letcher6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.71727,-98.95459

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the LETCHER 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 LETCHER 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 LETCHER 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 LETCHER 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 LETCHER 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 LETCHER 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 LETCHER 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 LETCHER, 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. ND-2012-02-08-66 | Wells County - June 1970

    Parent material and position of soils in association 8 (Soil Survey of Wells County, North Dakota; June 1970).

  2. SD-2012-03-14-11 | Brown County - April 1993

    Typical pattern of soils and parent material in the Niobell-Noonan-Williams association (Soil Survey of Brown County, SD; 1993).

Map Units

Map units containing LETCHER 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
Embden-Letcher fine sandy loams, 0 to 2 percent slopesF360A95925877272q549nd0051:12000
Letcher fine sandy loam, 0 to 2 percent slopesG358A3925738262q50mnd0051:12000
Letcher fine sandy loam, 0 to 2 percent slopesF358A277625860552q547nd00919811:20000
Swenoda-Letcher fine sandy loams, 0 to 3 percent slopesG779A479525753772q60nnd02119891:20000
Kratka-Letcher fine sandy loams, 0 to 2 percent slopesG355A207925753202q50jnd02119891:20000
Letcher fine sandy loam, 0 to 2 percent slopesG358A114425753212q50mnd02119891:20000
Stirum-Letcher fine sandy loams, 0 to 2 percent slopesG363A98925753242q5bfnd02119891:20000
Egeland-Letcher fine sandy loams, till substratum, 0 to 6 percent slopesG373B91527655512sd2ynd02119891:20000
Letcher-Wyrene sandy loams, 0 to 2 percent slopesG357A348525762892q50lnd0271:12000
Letcher fine sandy loam, 0 to 2 percent slopesG358A62325762902q50mnd0271:12000
Letcher fine sandy loam, 0 to 2 percent slopesG358A68125764392q50mnd03119901:20000
Letcher-Swenoda fine sandy loams, 0 to 3 percent slopesG778A73125766772q60mnd03919911:24000
Swenoda-Letcher fine sandy loams, 0 to 3 percent slopesG779A925771302q60nnd04519661:20000
Letcher fine sandy loam, 0 to 2 percent slopesG358A625770682q50mnd04519661:20000
Letcher fine sandy loam, 0 to 2 percent slopesG358A88925713612q50mnd04919871:20000
Letcher fine sandy loam, 0 to 2 percent slopesF358A72525857762q547nd04919871:20000
Letcher fine sandy loam, 0 to 2 percent slopesG358A9425773162q50mnd0631:12000
Letcher fine sandy loam, 0 to 2 percent slopesF358A371025872832q547nd06919751:20000
Letcher fine sandy loam, 0 to 2 percent slopesG358A57825823022q50mnd06919751:20000
Embden-Letcher fine sandy loams, 0 to 2 percent slopesF360A725872642q549nd06919751:20000
Glyndon-Letcher loams, 0 to 2 percent slopesI551A118626413521vh7qnd07319921:20000
Letcher-Lemert sandy loams, 0 to 2 percent slopesI210A79426412701nys5nd07319921:20000
Letcher fine sandy loam, 0 to 2 percent slopesG358A2425811692q50mnd07319921:20000
Letcher-Lemert sandy loams, 0 to 2 percent slopesI210A5626410561nys5nd07720051:12000
Glyndon-Letcher loams, 0 to 2 percent slopesI551A1218629271vh7qnd07720051:12000
Letcher fine sandy loam, 0 to 2 percent slopesF358A444625881972q547nd07919901:24000
Letcher fine sandy loam, 2 to 6 percent slopesF358B197725880872q548nd07919901:24000
Glyndon-Letcher loams, 0 to 2 percent slopesI551A3026412611vh7qnd08119591:12000
Letcher-Lemert sandy loams, 0 to 2 percent slopesI210A3826413671nys5nd09119911:20000
Letcher fine sandy loam, 0 to 2 percent slopesG358A488625796502q50mnd10319661:12000
Egeland-Letcher fine sandy loams, till substratum, 0 to 6 percent slopesG373B266827977622sd2ysd01319871:20000
Letcher-Swenoda-Ferney complex, 0 to 3 percent slopesG359A126527977582sd2qsd01319871:20000
Swenoda-Letcher fine sandy loams, 0 to 3 percent slopesG779A227977082q60nsd01319871:20000
Egeland-Letcher fine sandy loams, till substratum, 0 to 6 percent slopesG373B22827992472sd2ysd08919801:20000
Letcher loam, terrace, 0 to 2 percent slopesG306A4927992452sd2ksd08919801:20000
Swenoda-Letcher fine sandy loams, 0 to 3 percent slopesG779A44227993182q60nsd09119701:20000

Map of Series Extent

Approximate geographic distribution of the LETCHER 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 .