Official Series Description


Lab Data Summary

Aggregate lab data for the MORD soil series. This aggregation is based on all pedons with a current taxon name of MORD, 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 MORD 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
48B92P081392CO049001Mord7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.2936096,-106.422226

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the MORD 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 MORD 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 MORD 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 MORD 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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Competing Series

Soil series competing with MORD 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 MORD 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 MORD 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.

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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 MORD, 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

No block diagrams are available.

Map Units

Map units containing MORD 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
Mord loam, 4 to 15 percent slopesMrD5394497801jq03co64619731:24000
Mord family stony loam, 15 to 40 percent slopes232C8439509314k2zhco6471:24000
Mord family stony loam, 5 to 20 percent slopes, very stony115083509264k2xwco6471:24000
Mord loam, 3 to 15 percent slopes552619497881jq2pco64919771:24000
Mord loam, 15 to 30 percent slopes562341497882jq2qco64919771:24000
Mord family, 5 to 40 percent slopes359B550214149851jhdpco6541:24000
Cowdrey-Mord families-Rubble land complex, 15 to 45 percent slopes422B229232086442zd64co6541:24000
Charcol-Mord complex, 25 to 50 percent slopes16633497954jq51co65519841:24000
Charcol-Mord complex, 12 to 25 percent slopes15293497953jq50co65519841:24000
Mord loam, 5 to 30 percent slopesMoE6233498216jqfhco66219681:24000
Loberg-Mord association, hillyLV77301468544xt7mt60019691:24000
Mord stony loam, steepMZc59611468724xttmt60019691:24000
Swifton-Mord-Rubble land association, very steepSW33791469254xwjmt60019691:24000
Bridger-Mord association, hillyBM26701467684xqgmt60019691:24000
Mord loam, slopingMz10851468944xvjmt60019691:24000
Swifton-Mord-Rubble land association, very steepSW21729682324xwjmt6321:24000
Baird Hollow-Mord complex, 15 to 40 percent slopes3154223483836j7gmut63419971:24000
Mord gravelly loam, 4 to 25 percent slopes4271608483960j7lmut63419971:24000
Mord loam, 11 to 33 percent slopes -- draft227596724322602mmz0wy0411:24000
Mord loam, 11 to 33 percent slopes -- draft4227387924944742mmz0wy7231:24000

Map of Series Extent

Approximate geographic distribution of the MORD 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 .