Official Series Description


Lab Data Summary

Aggregate lab data for the DRYPOND soil series. This aggregation is based on all pedons with a current taxon name of DRYPOND, 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 DRYPOND 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 DRYPOND 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 DRYPOND series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

There are insufficient data to create the sibling sketch figure.

Select annual climate data summaries for the DRYPOND series and siblings. 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 DRYPOND 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 DRYPOND 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 DRYPOND 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 DRYPOND 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 DRYPOND, 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 DRYPOND 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
Drypond-Rock outcrop complex, 35 to 80 percent slopes, extremely stony13E1936518618kdnmva17319951:24000
Drypond-Rock outcrop complex, 15 to 35 percent slopes, extremely stony13D669518616kdnkva17319951:24000
Drypond-Rock outcrop complex, 15 to 35 percent slopes, extremely stony19D188522187kjcrva18519961:24000
Drypond-Rock outcrop complex, 35 to 80 percent slopes, extremely stony19E37522188kjcsva18519961:24000
Drypond-Rock outcrop complex, 25 to 80 percent slopes9F4013519398kfgsva19119981:15840
Drypond channery loam, 50 to 80 percent slopes10F2863519416kfhcva19119981:15840
Drypond-Rock outcrop complex, 10 to 65 percent slopes8E3615519027kf2tva19719881:15840
Marbleyard-Drypond complex, 35 to 60 percent slopes, very stony896E443025252982qm32va6061:24000
Marbleyard-Drypond complex, 35 to 60 percent slopes, rubbly896ES423525253002qm34va6061:24000
Marbleyard-Drypond complex, 60 to 80 percent slopes, very stony896F407625252992qm33va6061:24000
Drypond-Rock outcrop complex, 60 to 80 percent slopes845FR145625252882qm2rva6061:24000
Drypond-Rock outcrop complex, 35 to 60 percent slopes845ER96125253052qm39va6061:24000
Marbleyard-Drypond complex, 15 to 35 percent slopes, very stony896D94525252972qm31va6061:24000
Marbleyard-Drypond complex, 15 to 35 percent slopes, rubbly896DS66825253062qm3bva6061:24000
Drypond-Rock outcrop complex, 15 to 35 percent slopes845DR26525253042qm38va6061:24000
Marbleyard-Drypond complex, 3 to 15 percent slopes, very stony896C2025252962qm30va6061:24000
Drypond, thin solum-Rock outcrop complex, 35 to 60 percent slopes6F51931740402z3dbva8501:24000
Drypond, thin solum-Marbleyard complex, 35 to 55 percent slopes, extremely stony5F18631740382z3d8va8501:24000
Drypond, thin solum-Rock outcrop complex, 15 to 35 percent slopes6E17831740392z3d9va8501:24000
Marbleyard-Drypond, thin solum complex, 7 to 35 percent slopes, extremely stony16E7231740572z3dxva8501:24000
Marbleyard-Drypond, thin solum complex, 55 to 80 percent slopes, very stony16G1531740562z3dwva8501:24000
Drypond, thin solum-Rock outcrop complex, 60 to 80 percent slopes6G631740412z3dcva8501:24000

Map of Series Extent

Approximate geographic distribution of the DRYPOND 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 .