Official Series Description


Lab Data Summary

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

Soil series sharing subgroup-level classification with GEERTSEN, 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 GEERTSEN 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
Bushvalley, very stony-Woodhall families, complex, 40 to 70 percent slopes221C7705507539k147co6501:24000
Averett, very stony-Geertsen-Millerlake complex, 20 to 70 percent slopesDMG1742714268391jwr2ut0131:24000
Northorn-Millerlake-Geertsen complex, 10 to 50 percent slopes, very stonyTNF881214160751jjjvut0131:24000
Geertsen-Agassiz complex, 30 to 70 percent slopesGcG5005506549k039ut60919741:24000
Geertsen loam, 30 to 70 percent slopesGaG2645506548k038ut60919741:24000
Agassiz-Geertsen-Rock outcrop association, very steepAGG1555506503k01tut60919741:24000
Faim-Clayburn-Geertsen families complex, 3 to 20 percent slopes412331287430gwmut6451:24000
Faim-Geertsen families complex, 5 to 25 percent slopes411A331287330gwlut6451:24000
Merino-Castino-Geertsen families complex, 8 to 50 percent slopes402331287030gwhut6451:24000
Wrenman-Geertsen-Clayburn families complex, 20 to 60 percent slopes109A515132432682zscjut6451:24000
Geertsen family, dry, 30 to 70 percent slopes109487332432672zscqut6451:24000
Geertsen-Adek families complex, 30 to 60 percent slopes110B374132432742zsckut6451:24000
Castino-Geertsen families complex, 20 to 50 percent slopes110267932432722zscmut6451:24000
Geertsen-Merino families complex, 5 to 40 percent slopes4011744331286930gwgut6451:24000
Kebler, extremely bouldery-Geertsen, rubbly families complex, 8 to 35 percent slopesR181546623884ny69ut6471:24000
Clayburn-Goosepeak complex, 10 to 35 percent slopes -- Draft750525515052qttfwy6291:24000
Inchau-Geertsen-Beaveridge-like complex, 15 to 60 percent slopes -- Draft550725515022qttbwy6291:24000
Geertsen-Surdal-Spearhead families, complex, 15 to 75 percent slopes2173250480595zwy6291:24000
Geertsen-Beaveridge-like-Proposal-like complex, 6 to 35 percent slopes -- Draft740125515082qttjwy6291:24000
Geertsen-Surdal-Spearhead families, complex, 15 to 75 percent slopes21711973157789595zwy65620081:24000
Sigbird-Guffey-Geertsen families, complex, 15 to 40 percent slopes2668679157813596rwy65620081:24000
Cundiyo-Geertsen families, complex, 25 to 45 percent slopes2063163157782595rwy65620081:24000
Geertsen-Silvercliff families-Rock outcrop complex, 25 to 55 percent slopes22823231577965966wy65620081:24000

Map of Series Extent

Approximate geographic distribution of the GEERTSEN 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 .