Official Series Description


Lab Data Summary

Aggregate lab data for the PINERUN soil series. This aggregation is based on all pedons with a current taxon name of PINERUN, 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 PINERUN 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
116AM90209121990MO209014Pinerun4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.8244722,-93.5066111
116AM92209451992MO209182Pinerun4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.9019722,-93.3733528
116AM92209491992MO209186Pinerun4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.7948389,-93.407275
116BM90209071990MO209007Pinerun4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.8616667,-93.5833333
116BM91209171991MO209042Pinerun4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.8382333,-93.3547833
116BM92209081992MO209127Pinerun4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.9258694,-93.4463944
116BM92209091992MO209128Pinerun4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.9258694,-93.4466417
116BM92209161992MO209143Pinerun4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.8274389,-93.3712167
116BM92209581992MO209200Pinerun4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.9655806,-93.5997417
116BM93209041993MO209205Pinerun4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.9228417,-93.5887861
116BM96119241996MO119062Pinerun4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.7361889,-94.1272222
116BM96119251996MO119063Pinerun4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.7358444,-94.12735
116BM96119261996MO119064Pinerun4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.7357222,-94.1271917
116BM96119271996MO119065Pinerun4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.7349722,-94.1273833
116BM96119281996MO119066Pinerun4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.7349434,-94.1275482

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the PINERUN 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 PINERUN 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 PINERUN 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 PINERUN 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 PINERUN 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 PINERUN 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 PINERUN 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 PINERUN, 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 PINERUN 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
Pinerun silt loam, 0 to 2 percent slopes, occasionally flooded7540294425365892qq0qmo00919901:24000
Pinerun silt loam, 1 to 3 percent slopes, occasionally flooded7640269026730322rt1cmo00919901:24000
Pinerun-Waben complex, 2 to 5 percent slopes7540513025365972qq0tmo00919901:24000
Pinerun gravelly silt loam, 1 to 3 percent slopes, occasionally flooded7540455425365952qq0smo04319821:24000
Pinerun silt loam, 1 to 3 percent slopes, occasionally flooded7640255126730522rt1cmo04319821:24000
Pinerun silt loam, 0 to 2 percent slopes, occasionally flooded7540226125365902qq0qmo04319821:24000
Pinerun-Waben complex, 2 to 5 percent slopes754055925365982qq0tmo04319821:24000
Pinerun-Waben complex, 2 to 5 percent slopes7540519125365962qq0tmo10919791:24000
Cedargap, frequently flooded-Pinerun, occasionally flooded complex, 1 to 3 percent slopes717531038808600w4dwmo11920041:24000
Cedargap, frequently flooded-Pinerun, occasionally flooded complex, 0 to 2 percent slopes7675371926731292rt0ymo11920041:24000
Pinerun-Waben complex, 2 to 5 percent slopes75405295625365992qq0tmo20919981:24000
Pinerun silt loam, 0 to 2 percent slopes, occasionally flooded75402280625365882qq0qmo20919981:24000
Pinerun gravelly silt loam, 1 to 3 percent slopes, occasionally flooded75404147325365942qq0smo20919981:24000
Pinerun-Waben complex, 0 to 3 percent slopes76405145726731722rt1fmo20919981:24000
Pinerun gravelly silt loam, 0 to 2 percent slopes, occasionally flooded76404127626731712rt1dmo20919981:24000
Pinerun silt loam, 1 to 3 percent slopes, occasionally flooded7640222726731692rt1cmo20919981:24000

Map of Series Extent

Approximate geographic distribution of the PINERUN 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 .