Official Series Description


Lab Data Summary

Aggregate lab data for the NARROWS soil series. This aggregation is based on all pedons with a current taxon name of NARROWS, 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 NARROWS 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 NARROWS 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 NARROWS 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 NARROWS 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 NARROWS 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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Competing Series

Soil series competing with NARROWS 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 NARROWS 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 NARROWS 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.

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

Soil series sharing subgroup-level classification with NARROWS, 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 NARROWS 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
Narrows silty clay loam, 1 to 8 percent slopes3C105226114762r94tid76120181:24000
Knep-Narrows-Libeg complex, 2 to 8 percent slopes15C45626114612pbb4id76120181:24000
Crookedrun-Narrows-Trailhollow complex, 0 to 6 percent slopes935C1725980062pg9smt60520071:24000
Crookedrun-Narrows complex, 0 to 4 percent slopes98B235524263752mfv5mt61220111:24000
Philipsburg-Narrows complex, 2 to 8 percent slopes782C158724850172pdvvmt61220111:24000
Narrows-Tepete complex, 0 to 4 percent slopes350B147425128642qbypmt61220111:24000
Hellroaring-Narrows-Littletable complex, 0 to 4 percent slopes250B141625128632qbynmt61220111:24000
Knep-Narrows-Libeg complex, 2 to 8 percent slopes15C65824825772pbb4mt61220111:24000
Narrows-Crookedrun complex, 1 to 8 percent slopes197C5991484074zfbmt61220111:24000
Sagedale-Narrows complex, 0 to 8 percent slopes118C3351484034zf6mt61220111:24000
Narrows-Dutchhollow, frequently flooded-Crookedrun complex, 0 to 4 percent slopes973B22325976352mfv9mt61220111:24000
Narrows-Limadam complex, 0 to 8 percent slopes780C17624850162pdvtmt61220111:24000
Hellroaring-Narrows-Littletable complex, 0 to 4 percent slopes250B724125174362qbynmt61420121:24000
Crookedrun-Narrows-Trailhollow complex, 0 to 6 percent slopes935C404124864102pg9smt61420121:24000
Narrows-Dutchhollow, frequently flooded-Crookedrun complex, 0 to 4 percent slopes973B251924263792mfv9mt61420121:24000
Lehunt, saline-Narrows complex, 0 to 2 percent slopes983A236224263842mfvgmt61420121:24000
Matsingale, frequently ponded-Limadam-Narrows complex, 0 to 2 percent slopes949A202325187132pp9xmt61420121:24000
Narrows-Crookedrun complex, 1 to 8 percent slopes197C183725174344zfbmt61420121:24000
Philipsburg-Narrows complex, 2 to 8 percent slopes782C158925174502pdvvmt61420121:24000
Narrows-Matsingale, frequently ponded-Tepete, frequently ponded complex, 0 to 2 percent slopes912A130825187322ppbgmt61420121:24000
Narrows-Tepete complex, 0 to 4 percent slopes350B118325187312qbypmt61420121:24000
Crookedrun-Narrows complex, 0 to 4 percent slopes98B82525174352mfv5mt61420121:24000
Tepete, frequently ponded-Matsingale, frequently ponded-Narrows, saline complex, 0 to 2 percent slopes1009A73025208222ppbtmt61420121:24000
Narrows-Limadam complex, 0 to 8 percent slopes780C3825416372pdvtmt61420121:24000
Dipman-Narrows associationDN378515269453wmwy62319711:20000

Map of Series Extent

Approximate geographic distribution of the NARROWS 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 .