Official Series Description


Lab Data Summary

Aggregate lab data for the PADDYKNOB soil series. This aggregation is based on all pedons with a current taxon name of PADDYKNOB, 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 PADDYKNOB were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

There are insufficient data to create the lab data summary figure.


Water Balance

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

There are insufficient data to create the 3D terrace figure.

There are insufficient data to create the 3D flats position figure.

Competing Series

Soil series competing with PADDYKNOB 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 PADDYKNOB 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 PADDYKNOB 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 PADDYKNOB, 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 PADDYKNOB 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
Paddyknob-Madsheep complex, 15 to 35 percent slopes, very stony48D89914514871kqd5va01720051:24000
Paddyknob-Madsheep complex, 35 to 55 percent slopes, very stony48E58114514881kqd6va01720051:24000
Paddyknob-Madsheep complex, 8 to 15 percent slopes, very stony48C28814514861kqd4va01720051:24000
Paddyknob-Madsheep complex, 35 to 55 percent slopes, very stony44F641625120932q9jbva09120101:24000
Paddyknob-Madsheep complex, 15 to 35 percent slopes, very stony44E608125120922q9j9va09120101:24000
Paddyknob-Madsheep complex, 8 to 15 percent slopes, very stony44C180725120942q9jcva09120101:24000
Mandy-Paddyknob-Rock outcrop complex, 8 to 35 percent slopes, very stony37D57216711431t2yvva16720061:24000
Paddyknob gravelly loam, 15 to 35 percent slopes, very stony40D464522175kjccva18519961:24000
Paddyknob-Rock outcrop complex, 35 to 80 percent slopes, extremely stony39E269522155kjbqva18519961:24000
Paddyknob gravelly loam, 35 to 55 percent slopes, very stony40E180522176kjcdva18519961:24000
Paddyknob-Rock outcrop complex, 15 to 35 percent slopes, extremely stony39D158522154kjbpva18519961:24000
Paddyknob - Rock outcrop complex, 35 to 60 percent slopes, very stony245E19325568862r7dxva6061:24000
Paddyknob - Rock outcrop complex, 3 to 15 percent slopes, very stony245C12425568842r7dvva6061:24000
Paddyknob gravelly loam, 15 to 35 percent slopes, very stony446D10125568882r7dzva6061:24000
Paddyknob - Rock outcrop complex, 15 to 35 percent slopes, very stony245D5825568852r7dwva6061:24000
Paddyknob gravelly loam, 3 to 15 percent slopes, very stony446C5125568872r7dyva6061:24000
Paddyknob-Madsheep complex, 35 to 55 percent slopes, very stonyPamF655527362452q9jbwv07519921:24000
Paddyknob-Madsheep complex, 15 to 35 percent slopes, very stonyPamE287427362472q9j9wv07519921:24000
Paddyknob-Madsheep complex, 8 to 15 percent slopes, very stonyPamC100027362462q9jcwv07519921:24000

Map of Series Extent

Approximate geographic distribution of the PADDYKNOB 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 .