Official Series Description


Lab Data Summary

Aggregate lab data for the MHOON soil series. This aggregation is based on all pedons with a current taxon name of MHOON, 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 MHOON 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
131AM03031012003MO031001Mhoon4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.1272621,-89.7841034
131AM03031022003MO031002Mhoon4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.1281815,-89.7830276
131AM03031042003MO031004Mhoon4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.2273102,-89.6388245
131AM05143032005MO14303MHOON4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.55,-89.45

Water Balance

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

Competing Series

Soil series competing with MHOON 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 MHOON 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 MHOON 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.

Click the image to view it full size.

Click the image to view it full size.

Soil series sharing subgroup-level classification with MHOON, 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. KY-2012-01-27-16 | Carlisle and Hickman Counties - July 1997

    Relationship of soils to topography and underlying material in the Convent-Adler-Mhoon general soil map unit in Carlisle County (Soil Survey of Carlisle and Hickman Counties, Kentucky; July 1997).

  2. KY-2012-01-27-19 | Carlisle and Hickman Counties - July 1997

    Relationship of soils to topography and underlying material in the Convent-Adler-Mhoon general soil map unit in Hickman County (Soil Survey of Carlisle and Hickman Counties, Kentucky; July 1997).

  3. LA-2012-04-27-10 | Terrebonne Parish - February 1960

    Diagram showing the relationships of the soils in Terrebonne Parish from Minerva Plantation on Little Bayou Black in sec. 9, T. 16 S., R. 16 E., southwest to Bayou Copasaw in sec. 8, T. 18 S., R. 15 E (Soil Survey of Terrebonne Parish, Louisiana; February 1960).

  4. MS-2012-04-26-09 | De Soto County - September 1959

    Soil associations in De Soto County (Soil Survey of De Soto County, Mississippi; September 1959).

Map Units

Map units containing MHOON 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
Mhoon fine sandy loam3421060564142ly14ar03119761:20000
Mhoon soils, frequently flooded355230564143ly15ar03119761:20000
Mhoon silt loamMh1200564175ly26ar03519701:20000
Mhoon soils, frequently floodedMh5830564101lxztar07719741:20000
Mhoon soils, frequently floodedMF15746565978lzycar09519741:20000
Mhoon soils, frequently floodedMh3950564245ly4gar10719711:20000
Mhoon silt loamMo39645564283ly5par11119731:20000
Convent-Mhoon complex, 0 to 2 percent slopes, frequently floodedCu3189654158pypwky07520021:12000
Mhoon silt loam, pondedMo1050655037pzm7ky07520021:12000
Convent-Mhoon complex, 0 to 2 percent slopes, occasionally floodedCt461654152pyppky07520021:12000
Mhoon silty clay loam, 0 to 2 percent slopes, frequently floodedMo16715974161qm7kky60219721:12000
Convent-Mhoon silt loams, frequently floodedCt12007570523m4nzky61119911:20000
Mhoon silt loam, pondedMo4758570537m4pfky61119911:20000
Mhoon silty clay loamMh162016784301tbjxla07719801:24000
Mhoon silty clay loamMh2813973821hx2vla12120041:24000
Mhoon silt loam, 0 to 1 percent slopes, rarely flooded86039255225008612pzz1mo03119781:24000
Mhoon silt loam, 0 to 1 percent slopes, occasionally flooded8603810732571701z0ccmo03119781:24000
Mhoon silt loam, 0 to 1 percent slopes, frequently flooded8612878325715662r038mo03119781:24000
Mhoon silt loam, 0 to 1 percent slopes8207320326366322r1klmo03119781:24000
Mhoon silt loam, 0 to 1 percent slopes, rarely flooded86039184325008592pzz1mo13319781:24000
Mhoon silt loam, 0 to 1 percent slopes, occasionally flooded860385062689871z0ccmo13319781:24000
Mhoon silt loam, 0 to 1 percent slopes, rarely flooded8603996925008602pzz1mo20119781:24000
Mhoon silt loam, 0 to 1 percent slopes, occasionally flooded860381902689912z0ccmo20119781:24000
Mhoon silt loam, 0 to 1 percent slopes, occasionally flooded860388017894082z0ccmo20719831:24000
Mhoon silt loam, 0 to 1 percent slopes, rarely flooded86039201925008582pzz1mo20719831:24000
Mhoon silt loamMa221567505m1jmms01119561:20000
Mhoon silty clay, 0 to 3 percent slopesMa116567654m1pfms02719561:24000
Mhoon silty clay, nearly level phaseMm1189567780m1thms03319551:24000
Mhoon silty clay, 0 to 2 percent slopesMh507568054m23bms05519601:20000
Mhoon silty clay, 0 to 2 percent slopesMh503568432m2hjms12519601:20000
Mhoon silty clay loam, 0 to 2 percent slopesMh376568763m2v6ms15119591:20000
Mhoon silt loam, 0 to 2 percent slopes, frequently flooded, longMh182833348722zym7tn04519631:15840
Levees and borrow pits (Levees and Mhoon)Lb1527567127m14ftn09519661:20000
Mhoon clay (sic)Mh744567128m14gtn09519661:20000
Mhoon silt loam, 0 to 2 percent slopes, frequently flooded, longMh12733348752zym7tn13119661:15840

Map of Series Extent

Approximate geographic distribution of the MHOON 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 .