Official Series Description


Lab Data Summary

Aggregate lab data for the HANNON soil series. This aggregation is based on all pedons with a current taxon name of HANNON, 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 HANNON 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
133AS04AL-041-104AL041001-pgmHannon3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.025,-86.3291667
133AS91AL-087-591AL087005-pgmHannon3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.2777778,-85.5513889
133AS91AL-087-691AL087006-pgmHannon3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.2777778,-85.5513889
135AS91AL-087-491AL087004-pgmHannon3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.2566667,-85.5541667

Water Balance

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

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 HANNON, 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 HANNON 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
Sumter-Hannon complex, 12 to 40 percent slopesShF156432720442zkvsal00119721:20000
Oktibbeha-Hannon complex, 1 to 3 slopes, erodedOnB2480328236c0k8al00520011:24000
Toxey-Brantley-Hannon complex, 3 to 8 percent slopes, erodedToC24590328604c0y4al02319981:24000
Sumter-Hannon complex, 12 to 35 percent slopes, erodedStE2291014138481jg70al04120051:24000
Hannon-Sumter complex, 2 to 8 percent slopes, erodedHsC2124014138471jg6zal04120051:24000
Sumter-Hannon complex, 8 to 12 percent slopes, severely erodedStE33584525149072qdgval08520111:24000
Sumter-Hannon complex, 3 to 8 percent slopes, severely erodedStD32142125149062qdgtal08520111:24000
Sumter-Hannon complex, 12 to 35 percent slopes, severely erodedStF31652825149082qdgwal08520111:24000
Sumter-Hannon complex, 1 to 3 percent slopesStB1351325149092qdgxal08520111:24000
Hannon-Sumter complex, 8 to 15 percent slopes, erodedHsE21128425149362qdw9al08520111:24000
Hannon-Sumter complex, 15 to 35 percent slopes, erodedHsF2905325149372qdwbal08520111:24000
Hannon clay loam, 1 to 3 percent slopesHnB198325149102x307al08520111:24000
Maytag-Hannon complex, 3 to 8 percent slopesMnD149125149112qdgzal08520111:24000
Hannon-Maytag complex, 3 to 8 percent slopes, erodedHoD26038330465c2w5al08719971:24000
Sumter-Hannon complex, 12 to 25 percent slopesStE5612330495c2x4al08719971:24000
Maytag-Hannon complex, 1 to 3 percent slopesMuB4588330477c2wkal08719971:24000
Hannon-Sumter complex, 5 to 12 percent slopesHsE1562330466c2w6al08719971:24000
Hannon clay loam, 1 to 3 percent slopesHnB8243304632x307al08719971:24000
Hannon clay, 3 to 5 percent slopes, erodedHnC2709330464c2w4al08719971:24000
Sumter-Hannon complex, 12 to 25 percent slopes, severely erodedShE33730331345c3skal11319971:24000
Hannon clay, 5 to 8 percent slopes, erodedHnD23570331350c3sqal11319971:24000
Hannon clay loam, 1 to 3 percent slopesHaB25903313482x307al11319971:24000
Hannon clay, 3 to 5 percent slopes, erodedHnC22500331349c3spal11319971:24000
Hannon-Sumter complex, 5 to 12 percent slopes, erodedHsE2870331338c3sbal11319971:24000
Prim-Suggsvile-Hannon complex, 10 to 40 percent slopesPsF548926421192rrw6al12920131:24000
Prim-Suggsville-Hannon complex, 2 to 10 percent slopesPsD198126421182rrw7al12920131:24000
Toxey-Brantley-Hannon complex, 3 to 8 percent slopes, erodedTxC24626421392rrwwal12920131:24000
Hannon-Oktibbeha complex, 5 to 8 percent slopes8618023984832lhtffl13320091:12000

Map of Series Extent

Approximate geographic distribution of the HANNON 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 .