Official Series Description


Lab Data Summary

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

Click the image to view it full size.



Click the image to view it full size.

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the LONJON series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

Click the image to view it full size.

Select annual climate data summaries for the LONJON series and siblings. 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 LONJON 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 .

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

Competing Series

Soil series competing with LONJON share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

Click the image to view it full size.

Select annual climate data summaries for the LONJON 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 LONJON 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 .

Click the image to view it full size.

Click the image to view it full size.

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.

Soil series sharing subgroup-level classification with LONJON, 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 LONJON 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
Sprollow, dry-Lonjon complex, 30 to 60 percent slopes19013450791571vkpkid71220081:24000
Pinegap-Lonjon complex, 35 to 65 percent slopes160416315447255qzid71220081:24000
Lonjon-Monida-Chokecherry complex, 5 to 50 percent slopes141321115451355s9id71220081:24000
Sprollow, dry-Lonjon-Mumford complex, 15 to 30 percent slopes1922660791574vkpnid71220081:24000
Lonjon-Sprollow-Mumford complex, 30 to 60 percent slopes144253315449055rkid71220081:24000
Sprollow-Wursten-Lonjon complex, 5 to 25 percent slopes193145915445055q8id71220081:24000
Sprollow-Lonjon-Mumford complex, 15 to 30 percent slopes191135615436255mfid71220081:24000
Lonjon-Mumford-Rock outcrop complex, 25 to 50 percent slopes142126215448955rjid71220081:24000
Lonjon-Kucera, dry-Sprollow, dry complex, 5 to 25 percent slopes1401229791552vknyid71220081:24000
Sprollow-Lonjon complex, 30 to 60 percent slopes18994115444955q7id71220081:24000
Lonjon-Sheep Creek-Dipcreek complex, 10 to 50 percent slopes14348815471671nxymid71220081:24000
Lonjon-Kucera-Sprollow complex, 10 to 25 percent slopes13919915432255l4id71220081:24000
Lonjon-Monida-Chokecherry complex, 5 to 50 percent slopes14131309390655s9id7131:24000
Lonjon-Sheep Creek-Dipcreek complex, 10 to 50 percent slopes143130939071nxymid7131:24000
Lonjon silt loam, 2 to 10 percent slopesLCD2510503868jx9tut60419801:24000
Lonjon silt loam, 10 to 30 percent slopesLCE1440503869jx9vut60419801:24000
Sprollow, dry-Lonjon complex, 30 to 60 percent slopes19015423962652lfhwut60419801:24000
Lonjon stony loam, 30 to 60 percent slopes886232481888j5fsut61819951:24000
Pinegap-Lonjon complex, 35 to 65 percent slopes160316971255qzwy7231:24000
Lonjon-Sprollow-Mumford complex, 30 to 60 percent slopes144316971155rkwy7231:24000

Map of Series Extent

Approximate geographic distribution of the LONJON 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 .