Official Series Description


Lab Data Summary

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

Competing Series

Soil series competing with JUSTESEN 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 JUSTESEN 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 JUSTESEN 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 JUSTESEN, 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 JUSTESEN 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
McCarey-Justesen-Rock outcrop complex, 2 to 15 percent slopes7516464793642nl4id68019851:24000
McCarey-Justesen loams, 2 to 8 percent slopes743123793632nl3id68019851:24000
Justesen loam, 2 to 4 percent slopes521311793392nkbid68019851:24000
Justesen loam, 4 to 8 percent slopes53910793402nkcid68019851:24000
Justesen loam, 12 to 30 percent slopes55678793422nkfid68019851:24000
Justesen loam, 8 to 12 percent slopes54302793412nkdid68019851:24000
Soen-Justesen-Howcan complex, 4 to 35 percent slopes204-CL11231736172sghid7031:24000
Justesen-Drage complex, 2 to 15 percent slopes98-CL7531736092smvid7031:24000
Bothwell-Hades-Justesen complex, 6 to 25 percent slopes137526198432v06qid7131:24000
Bothwell-Hades-Justesen complex, 6 to 25 percent slopes233022485266j8yrid71419971:24000
Bothwell-Hades-Justesen complex, 6 to 25 percent slopes13-O17331733262v06qid71419971:24000
Justesen silt loam, 12 to 25 percent slopes572369485652j9c6id71519941:24000
Bothwell-Hades-Justesen complex, 6 to 25 percent slopes13154431635882v06qid71519941:24000
Justesen-Ririe-Buist complex, 12 to 20 percent slopes58651485653j9c7id71519941:24000
Justesen silt loam, 4 to 12 percent slopes56609485651j9c5id71519941:24000
Justesen-Drage complex, 2 to 15 percent slopes983701832612smvid75219991:24000
Soen-Justesen-Howcan complex, 4 to 35 percent slopes2041330830952sghid75219991:24000
Justesen-Drage complex, 1 to 20 percent slopes474473790572n87id76319981:24000
Soen-Justesen complex, 4 to 12 percent slopes1151566789392n4fid76319981:24000
Justesen-Drage complex, 1 to 20 percent slopes2714115314091ndk9id78019981:24000
McCarey-Justesen complex, 2 to 8 percent slopes403715316001ndrgid78019981:24000
Justesen loam, 4 to 8 percent slopes263215314051ndk5id78019981:24000
Justesen loam, 2 to 4 percent slopes25915314031ndk3id78019981:24000
Justesen loam, 4 to 15 percent slopesJeD2594482533j63lut60819811:24000

Map of Series Extent

Approximate geographic distribution of the JUSTESEN 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 .