Official Series Description


Lab Data Summary

Aggregate lab data for the MYATT soil series. This aggregation is based on all pedons with a current taxon name of MYATT, 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 MYATT 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
133AS86AL-105-586AL105005-pgmMyatt3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.5861111,-87.2122222
133AS88AL-087-188AL087001-pgmMyatt3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.4727778,-85.7561111
133A40A4813S1963MS073002MYATT6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties31.0899315,-89.3861771
133A40A4814S1963MS073004MYATT5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties31.2410393,-89.4600677
133A40A4066S1965NC163003MYATT7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.2352867126465,-78.3677825927734
153A82P0196S1981SC051011Myatt6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties33.9667969,-78.966423

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the MYATT 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 MYATT 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 MYATT 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 MYATT 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 MYATT 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 MYATT 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 MYATT 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 MYATT, 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. AR-2012-05-08-03 | Bradley County - April 1961

    General soil areas (Soil Survey of Bradley County, Arkansas; April 1961).

  2. FL-2012-04-25-01 | Gadsden County - January 1961

    Main geologic formations and other topographic features in a segment of Gadsden County, and the positions of soils in some soil series (Soil Survey of Gadsden County, Florida; January 1961).

  3. LA-2012-02-01-01 | Bossier Parish - August 1962

    Physiographic relationships of general soil areas in the northwestern part of Bossier Parish. The area represented is about 12 miles square (Soil Survey of Bossier Parish, Louisiana; August 1962).

  4. SC-2012-03-14-06 | Bamberg County - January 1966

    Soil series and land types in soil associations 6 and 7 and their relation to the landscape and underlying material (Soil Survey of Bamberg County, SC; 1966).

  5. SC-2012-03-14-09 | Calhoun County - 1963

    Major soils in the Izagor-Myatt soil association and their relationship to the landscape (Soil Survey of Calhoun County, SC; 1963).

  6. SC-2012-03-14-22 | Lee County - March 1963

    Major soils in association 4 and their position on the Lynches River terrace. Wehadkee silt loam, which is in soil association 7, lies between the terrace and the river (Soil Survey of Lee County, SC; 1963).

Map Units

Map units containing MYATT 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
Myatt-Bibb associationMY15895328075c0d2al00119721:20000
Myatt very fine sandy loamMy11509328178c0hdal00319611:20000
Myatt fine sandy loam, 0 to 1 percent slopes, rarely floodedMyA151022330302dyn7al00720071:24000
Myatt-Bibb association, levelMYA26468328523c0vjal02119671:20000
Myatt loamMt2914328531c0vsal02119671:20000
Myatt fine sandy loam, 0 to 1 percent slopes, occasionally floodedMyA4950600092n4ftal02520041:24000
Myatt very fine sandy loamMd5673329003c1c0al04519581:20000
Myatt loamy sandMb5530329278c1mwal05119481:20000
Myatt silt loamMy10129329478c1vbal05719631:15840
Myatt fine sandy loam, 0 to 2 percent slopesMy130363296832vxx2al06320131:
Myatt fine sandy loam, 0 to 2 percent slopes, frequently floodedMyA3524945492psflal07520101:24000
Myatt loam, 0 to 1 percent slopes, rarely floodedMyA3063330478c2wlal08719971:24000
Myatt silt loam181300330619c314al09319761:20000
Byars and Myatt soilsBf6469330887c39sal10119581:20000
Myatt fine sandy loam, 0 to 1 percent slopes, rarely floodedMyA8040331244c3p9al10519961:24000
Myatt-Columbus complex, 0 to 2 percent slopes, occasionally floodedMcA4760331289c3qral10719971:24000
Myatt fine sandy loam, 0 to 1 percent slopes, occasionally floodedMaA3070331271c3q5al10719971:24000
Myatt-Kalmia complex, mound phase (amy, kalmia)MK18336565161lz30ar01119591:20000
Myatt-Osier associationMO6240324847bx0yga18519751:20000
Myatt sandy loamMya1840324981bx58ga28319621:20000
Myatt-Osier associationMO4165325435bxmxga61219751:20000
Myatt fine sandy loam, occasionally floodedMy20748569747m3vyla06319871:24000
Myatt fine sandy loam, 0 to 1 percent slopesMt135895697462syw2la06319871:24000
Myatt fine sandy loam, occasionally floodedMy292317216421vshvla09119911:24000
Myatt fine sandy loamMt228217216411vshtla09119911:24000
Myatt fine sandy loam, 0 to 1 percent slopesMt592623270092syw2la10319851:24000
Myatt fine sandy loam, frequently floodedMy37373327010bz8qla10319851:24000
Myatt fine sandy loamMt1677315365161nkw1la10519851:24000
Myatt fine sandy loam, occasionally floodedMy1439215365171nkw2la10519851:24000
Myatt fine sandy loam, frequently floodedMy2064017241441vw3kla11719891:24000
Myatt fine sandy loam, 0 to 1 percent slopesMt1168717241432syw2la11719891:24000
Myatt silt loam, 0 to 2 percent slopes (daleville)MyA599332276c4rlms03919671:20000
Myatt loam, 0 to 1 percent slopes, occasionally flooded222594332562c51tms05919971:24000
Myatt fine sandy loam, 0 to 2 percent slopesMy8653330232vxx2ms08119681:20000
Myatt fine sandy loam, 0 to 2 percent slopesMy249083331852vxx2ms09519631:15840
Myatt loam (trebloc)My1417333499c611ms10519681:20000
Myatt silt loam, frequently floodedMy939333817c6c9ms11719951:24000
Myatt loamMt809334286c6vfms14719651:20000
Myatt very fine sandy loamMy50021162523wz2nc19119681:20000
Myatt-Paxville complex, 0 to 2 percent slopes, occasionally floodedMyA174016065981qxsrsc06120051:24000
Myatt-Slagle complex, 0 to 2 percent slopes12A193412103641ydva03319961:24000
Myatt loam, 0 to 2 percent slopes, rarely flooded19163971188562y7jvva04119741:15840
Myatt loam, 0 to 2 percent slopes, rarely flooded615401191502y7jvva08519761:15840
Myatt variant fine sandy loam4614351191243zyqva08519761:15840
Myatt fine sandy loamMy888119256402zva08719731:15840
Myatt fine sandy loam930770119333405gva09319821:15840
Myatt loam, 0 to 2 percent slopes18A278694698r9wmva10119951:15840
Myatt loam13142111963240h3va11919821:15840
Myatt loam, 0 to 2 percent slopes16A22183705278rnwxva17519961:24000
Myatt loam, 0 to 2 percent slopes, rarely flooded649851204552y7jvva17719801:15840
Myatt loam, 0 to 2 percent slopes17A1255917230851vv0dva18320061:24000
Myatt silt loam, 0 to 2 percent slopes, occasionally flooded14A295124817932p9hvva65319911:24000

Map of Series Extent

Approximate geographic distribution of the MYATT 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 .