Official Series Description


Lab Data Summary

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

Click the image to view it full size.

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

Soil series sharing subgroup-level classification with GLEAN, 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

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

  1. NV-2012-05-09-10 | Lander County, North Part - May 1992

    Typical relationship of general soil map units and landscapes: Sonoma-Rixie-Paranat (3); Orovada-Broyles-Shabliss (7); Buffaran-Allor-Chiara (11); Bioya-Chiara-Cortez (12); Robson-Akerue-Buffaran (16); Sumine-Chen-Rock outcrop (19); and Quarz-Walti-Glean (21) (Soil Survey of Lander County, Nevada, North Part; May 1992).

Map Units

Map units containing GLEAN 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
Searles-Glean association, 5 to 30 percent slopes35819170487706jchgca60820001:24000
Searles-Glean association, 30 to 50 percent slopes35918862487707jchhca60820001:24000
Alomax-Glean-Rock outcrop association, 9 to 50 percent slopes1026986487320jc30ca60820001:24000
Devada-Glean-Sumine association, 30 to 50 percent slopes1745081487444jc70ca60820001:24000
Glean-Searles association, 30 to 50 percent slopes2283412487520jc9gca60820001:24000
Madeline-Glean-Devada association, 9 to 50 percent slopes2782361487586jcclca60820001:24000
Glean very gravelly sandy loam, 30 to 50 percent slopes2271240487519jc9fca60820001:24000
Glean very gravelly sandy loam, 5 to 30 percent slopes226927487518jc9dca60820001:24000
Glean extremely stony sandy loam, 9 to 50 percent slopesGpF237332330682zmsqca61419671:24000
Glean extremely stony sandy loam, 9 to 50 percent slopesGpF20232330692zmsqca71919821:24000
Ola-Glean families complex, 15 to 30 percent slopes.3382924471451htl3ca73219981:24000
Glean family, 0 to 50 percent slopes.2151117471410htjsca73219981:24000
Rubble land-Nanamkin-Glean families complex, 30 to 80 percent slopes.205409471407htjpca73219981:24000
Glean-Rock outcrop-Rubble land associationGH4375476088hzdpnv61219681:24000
Bucan-Glean-Rock outcrop associationBW3227476032hzbwnv61219681:24000
Glean-Walti-Cleavage association400141125193732qj95nv61219681:24000
Glean-Devils-Rock outcrop association9223268474093hxbbnv62519811:24000
Glean-Devils association9213205474092hxb9nv62519811:24000
Fulstone variant-Devils-Glean association9111795474091hxb8nv62519811:24000
Glean-Ticino-Hartig association923316474094hxbcnv62519811:24000
Glean variant-Hartig variant-Rubble land association1091281473880hx3gnv62519811:24000
Burnborough-Glean association1031205473870hx34nv62519811:24000
McIvey-Chen-Welch association4329429282722w2v1nv76619941:24000
Loncan-Gando-Glean association6211485479285j2qtnv76819851:63360
Typic Argixerolls-Torripsammentic Haploxerolls-Glean association32101200479210j2ndnv76819851:63360
Glean-Gando association404890479267j2q7nv76819851:63360
Minneha-Drit-Glean association5915444644117pm7znv77319811:24000
Glean-Sup-Genoa association3342465644055pm5znv77319811:24000
Softscrabble-Glean-Genoa association5412075644107pm7nnv77319811:24000
Trid-Roloc-Glean association9751410644210pmbznv77319811:24000
Borda variant-Glean association1221100643999pm45nv77319811:24000
Glean-Genoa-Rubble land association3321020644054pm5ynv77319811:24000
Genoa-Glean association321970644051pm5vnv77319811:24000
Burnborough-Glean association961470644204pmbsnv77319811:24000
Borda variant-Glean-Chen association123420644000pm46nv77319811:24000
Slaven-Glean-Cleavage association120311377479436j2wpnv77519851:24000
Glean-Walti-Cleavage association4008855479664j341nv77519851:24000
Roca-Glean-Bregar association8757220479739j36gnv77519851:24000
Locane-Sumine-Glean association35616350479637j335nv77519851:24000
Rock outcrop-Loncan variant-Glean association13922060479454j2x8nv77519851:24000
Loncan-Gando-Glean association70112658479874j3btnv77619831:63360
Eightmile-Loncan-Glean association3113910479815j38xnv77619831:63360
Glean-Gando association8513712479899j3cmnv77619831:63360
Walti-Glean association7832322479886j3c6nv77619831:63360

Map of Series Extent

Approximate geographic distribution of the GLEAN 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 .