Official Series Description


Lab Data Summary

Aggregate lab data for the PONTO soil series. This aggregation is based on all pedons with a current taxon name of PONTO, 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 PONTO 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
22BUCD734710273-CA-47-102xPONTO3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.2713737,-122.2852402
22BUCD774714377-CA-47-143xPONTO4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.2378731,-121.8670883

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the PONTO 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 PONTO 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 PONTO 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 PONTO 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 flats position figure.

Competing Series

Soil series competing with PONTO 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 PONTO 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 PONTO 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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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 PONTO, 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 PONTO 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
Neer-Ponto stony sandy loams, 15 to 50 percent slopes complex1965460459105hdqvca60219781:24000
Ponto-Neer complex, 2 to 15 percent slopes2095370459118hdr8ca60219781:24000
Neer-Ponto complex, 15 to 50 percent slopes1972350459106hdqwca60219781:24000
Ponto sandy loam, 5 to 15 percent slopes2081350459117hdr7ca60219781:24000
Neer-Ponto complex, 2 to 30 percent slopes25919078487108jbw5ca60419941:24000
Ponto sandy loam, 2 to 15 percent slopes2865995487161jbxwca60419941:24000
Neer-Ponto complex, 30 to 50 percent slopes2604623487110jbw7ca60419941:24000
Carberry, warm-Ponto complex, 2 to 15 percent slopes1284010486846jblqca60419941:24000
Neer-Ponto, dark surface, complex, 30 to 50 percent slopes2583350487106jbw3ca60419941:24000
Carberry, warm-Ponto complex, 15 to 30 percent slopes1293145486848jblsca60419941:24000
Ponto-Wyntoon complex, 2 to 15 percent slopes2881804487165jby0ca60419941:24000
Ponto-Neer, dark surface, complex, 15 to 30 percent slopes2871735487163jbxyca60419941:24000
Ponto-Neer complex, 2 to 15 percent slopes209sc2207186768620pgyca70719831:24000
Neer-Ponto stony sandy loams, 15 to 50 percent slopes196sc1727186767820pgpca70719831:24000
Neer-Ponto complex, 2 to 30 percent slopes259im1316186894620qslca70719831:24000
Ponto sandy loam, 2 to 15 percent slopes286im336186896620qt7ca70719831:24000
Neer-Ponto complex, 30 to 50 percent slopes260im309186894820qsnca70719831:24000
Neer-Ponto complex, 15 to 50 percent slopes197sc309186768020pgrca70719831:24000
Neer-Ponto, dark surface, complex, 30 to 50 percent slopes258im168186894420qsjca70719831:24000
Ponto-Wyntoon complex, 2 to 15 percent slopes288im2186896820qt9ca70719831:24000
Ponto variant-Neer complex, 30 to 50 percent slopesFFF1127464649hlhpca71919821:24000
Ponto variant-Neer-Rock outcrop complex, 30 to 75 percent slopes , severely erodedFGG3975464650hlhqca71919821:24000
Ponto variant-Neer complex, 2 to 30 percent slopesFFE447464648hlhnca71919821:24000

Map of Series Extent

Approximate geographic distribution of the PONTO 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 .