Official Series Description


Lab Data Summary

Aggregate lab data for the TOP soil series. This aggregation is based on all pedons with a current taxon name of TOP, 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 TOP 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
43C04N0426S2003OR023010Top6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.8936195,-119.4671783

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the TOP 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 TOP 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 TOP 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 TOP 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 terrace figure.

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

Competing Series

Soil series competing with TOP 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 TOP series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

Click the image to view it full size.

Geomorphic description summaries for the TOP 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 terrace figure.

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

Soil series sharing subgroup-level classification with TOP, 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 TOP 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
Top-McGarr complex, 12 to 35 percent north slopes167D72706215722p2or60419881:24000
Top-McGarr complex, 35 to 65 percent north slopes167E69426215822p3or60419881:24000
Top silt loam, 12 to 35 percent north slopes166D23826215522p0or60419881:24000
Top silt loam, 35 to 60 percent north slopes166E3866215622p1or60419881:24000
Top-Harlow complex, 20 to 50 percent north slopes4013BO2333120163vylbor60720181:24000
Lamulita-Top-Gaib complex, 2 to 20 percent slopes4017AO1583120174rctror60720181:24000
Lamulita-Top-Gaib complex, 20 to 50 percent north slopes4017BO923120167rctqor60720181:24000
Top-Boardtree complex, 2 to 30 percent slopes4014AO65312016421zp5or60720181:24000
Lamulita-Top-Gaib complex, 20 to 50 percent north slopes4017BO5103122530rctqor62620181:24000
Lamulita-Top-Gaib complex, 2 to 20 percent slopes4017AO643385317rctror62620181:24000
Lamulita-Top-Gaib complex, 20 to 50 percent north slopes410E81413425155rctqor6271:24000
Top-Gwinly-Lamulita complex, 20 to 50 percent slopes445E300834263081nvb6or6271:24000
Top-Klicker-Gaib complex, 2 to 20 percent slopes412C168734251851r334or6271:24000
Lamulita-Top-Gaib complex, 50 to 75 percent north slopes410F15183429435rctpor6271:24000
Lamulita-Top-Gaib complex, 2 to 20 percent slopes410C14233425068rctror6271:24000
Top-Boardtree complex, 2 to 30 percent slopes402C1249342516921zp5or6271:24000
Top-Klicker-Gaib complex, 20 to 50 percent slopes412E85834251231r336or6271:24000
Top-Alding complex, 20 to 50 percent north slopes184E78234295801hx3sor6271:24000
Top-Harlow complex, 20 to 50 percent north slopes401E7733425057vylbor6271:24000
Top-Harlow complex, 2 to 20 percent slopes401C55934320221qfw1or6271:24000
Top-Sharpridge-Lamulita complex, 5 to 35 percent south slopes400C384434217772r5c7or6771:24000
Top-Harlow complex, 20 to 50 percent north slopes401E11453421957vylbor6771:24000
Lamulita-Top-Gaib complex, 2 to 20 percent slopes410C8133422011rctror6771:24000
Top-Klicker-Gaib complex, 20 to 50 percent slopes412E34634246101r336or6771:24000
Lamulita-Top-Gaib complex, 20 to 50 percent north slopes410E1533424746rctqor6771:24000
Top-Boardtree complex, 2 to 30 percent slopes402C79342479521zp5or6771:24000
Top-Klicker-Gaib complex, 2 to 20 percent slopes412C4034248591r334or6771:24000

Map of Series Extent

Approximate geographic distribution of the TOP 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 .