Official Series Description


Lab Data Summary

Aggregate lab data for the GWIN soil series. This aggregation is based on all pedons with a current taxon name of GWIN, 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 GWIN 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
1098P0224S1997OR023014GWIN6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.5383339,-119.4816666
43A82P043182ID061001GWIN6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.438755,-116.3896332
986P024185ID069029Gwin6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.3463898,-116.7483368

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the GWIN 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 GWIN 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 GWIN 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 GWIN 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 GWIN 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 GWIN 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 GWIN 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 GWIN, 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 GWIN 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
Lawyer-Elmore-Gwin families association, 1 to 20 percent slopes.20448740470519hsm1ca70319831:24000
Pass Canyon-Fordice-Gwin families association, 1 to 20 percent slopes.22426000470539hsmpca70319831:24000
Pass Canyon-Fordice-Gwin families association, 20 to 40 percent slopes.22525730470540hsmqca70319831:24000
Lawyer-Elmore-Gwin families association, 20 to 40 percent slopes.20520230470520hsm2ca70319831:24000
Ridd-Los Gatos-Grin families association, 5 to 35 percent slopes.2379272470551hsn2ca70319831:24000
Pass Canyon-Gwin-Fordice families association, 40 to 70 percent slopes.2267340470541hsmrca70319831:24000
Searles-Gwin families-Lava flows complex, 1 to 10 percent slopes.2476675470561hsndca70319831:24000
Gwin-Pass Canyon families-Lthic xerorthents, mesic complex, 20 to 40 percent slopes.1766210470491hsl4ca70319831:24000
Gwin-Pass Canyon families-Lithic Xerorthents, mesic complex, 40 to 70 percent slopes.1775280470492hsl5ca70319831:24000
Lawyer-Elmore-Gwin families association, 40 to 60 percent slopes.2063750470521hsm3ca70319831:24000
Gwin-Pass Canyon families-Lithic Xerorthents, mesic complex, 1 to 20 percent slopes.1752110470490hsl3ca70319831:24000
Ruckles-Gwin families-Rock outcrop association, 20 to 40 percent slopes.2451693470559hsnbca70319831:24000
Gwin-Ruckles families-Rock outcrop association, 40 to 70 percent slopes.178673470493hsl6ca70319831:24000
Bobbitt family, moderately deep-Gwin family association, 35 to 50 percent slopes.8la443059827ht2yca70719831:24000
Bobbitt family, moderately deep-Gwin family association,0 to 35 percent slopes.74887470980ht2xca70819841:24000
Bobbitt family, moderately deep-Gwin family association, 35 to 50 percent slopes.82552470981ht2yca70819841:24000
Gwin-McDesh-Rock outcrop complex, 4 to 25 percent slopes603431425192712163bid00120121:24000
McDesh-Immig-Gwin complex, 4 to 25 percent slopes6000200251926221634id00120121:24000
McDesh-Shafer-Gwin complex, 4 to 25 percent slopes600314025192642166zid00120121:24000
Kettenbach-Gwin-Kettenbach, moist complex, 30 to 75 percent slopes5760367796702y6tpid61119941:24000
Gwin-Vollmer complex, 5 to 25 percent slopes413791796532nwgid61119941:24000
Larabee-Gwin association, 35 to 75 percent slopes722519796872nxkid61119941:24000
Gwin-Kettenbach complex, very rocky, 35 to 75 percent slopes57j964679209qsrzid61119941:24000
Gwin-Kettenbach complex, 35 to 75 percent slopes1003593775589v120id61220031:24000
Kettenbach-Gwin-Rock outcrop complex, 45 to 75 percent slopes1392444777366v2xbid61220031:24000
Gwin-Kettenbach-Keuterville complex, 10 to 25 percent slopes101342777365v2x9id61220031:24000
Gwin-Mehlhorn stony loams, 45 to 65 percent slopesGmE1547615408955bmid61819651:24000
Gwin-Mehlhorn stony loams, 12 to 45 percent slopesGmD776515408855blid61819651:24000
Kettenbach-Gwin-Kettenbach, moist complex, 30 to 75 percent slopes2y6tp279630989052y6tpid61819651:24000
Gwin-Klicker stony loams, 40 to 65 percent slopesGkE133515408755bkid61819651:24000
Gwin-Sallyann stony loams, 35 to 65 percent slopesGsE100215409055bnid61819651:24000
Gwin-Meland stony loams, 12 to 45 percent slopes2y6tl97830989042y6tlid61819651:24000
Mehlhorn-Gwin loams, 25 to 45 percent slopesMgD52015411955clid61819651:24000
Gwin-Rock outcrop complex, 40 to 65 percent slopes903369812892ql7id65619921:24000
Starveout-Gwin-McDaniel association, 3 to 45 percent slopes1911091811972qh8id65619921:24000
Gwin very stony loam, 30 to 60 percent slopes, extremely stonyGwF6321805552ptkid66019621:15840
Gwin very stony loam, 0 to 30 percent slopes, extremely stonyGwE6297805542ptjid66019621:15840
Gwin very stony loam, 60 to 80 percent slopes, extremely stonyGwG4852805562ptlid66019621:15840
Mehlhorn-Gwin very stony loams, 30 to 60 percent slopes, extremely stonyMdF4593806232pwrid66019621:15840
Mehlhorn-Gwin very stony loams, 0 to 30 percent slopes, extremely stonyMdE1650806222pwqid66019621:15840
Gwin stony loam, 12 to 30 percent slopes, very stonyGtE441805532pthid66019621:15840
McDesh-Immig-Gwin complex, 4 to 25 percent slopes600423825198152qrqid68320121:24000
Hann-Gwin-Shafer complex, 2 to 25 percent slopes601115225209062prj7id68320121:24000
Gwin-Flybow complex, 4 to 25 percent slopes605113225196802qrvid68320121:24000
McDesh-Gwin-Shafer complex, 8 to 35 percent slopes61975425197482qv8id68320121:24000
Gwin-Flybow-Rock outcrop complex, 35 to 65 percent slopes63056625197072qs1id68320121:24000
Hovelton-Gwin complex, 15 to 65 percent slopes62228725198052qq2id68320121:24000
Gwin-Rock outcrop complex, 40 to 70 percent slopes4051DO1091831208052ygc6or60720181:24000
Gwin-Rockly-Rock outcrop complex, 20 to 50 percent south slopes4007BO893331208072ygf7or60720181:24000
Gwin-Klickson-Kettenbach complex, 60 to 90 percent slopes6121DO263531207952mtd0or60720181:24000
Gwin-Kettenbach-Rock outcrop complex, 60 to 90 percent south slopes6060DS19093120192nj36or60720181:24000
Gwin-Rockly-Rock outcrop complex, 2 to 20 percent slopes4007AO1336312015721zl8or60720181:24000
Gwin-Klicker-Rock outcrop complex, 30 to 70 percent slopes3386CO119731208042xt3xor60720181:24000
Gwin-Bobbitt complex, 20 to 50 percent south slopes4023BO1071312017121zpyor60720181:24000
Gwin-Bobbitt complex, 2 to 20 percent slopes4023AO327312017021zpxor60720181:24000
Umatilla-Kahler-Gwin complex, 35 to 70 percent slopes5859CO32031202421nz0qor60720181:24000
Gwin-Kettenbach-Rock outcrop complex, 30 to 60 percent south slopes6060CS283120191nj34or60720181:24000
Gwin-Kettenbach-Rock outcrop complex, 60 to 90 percent south slopes84F26404224mwor62519791:20000
Gwin-Rockly-Rock outcrop complex, 20 to 50 percent south slopes4007BO154731225242ygf7or62620181:24000
Gwin-Rockly-Rock outcrop complex, 2 to 20 percent slopes4007AO496312252821zl8or62620181:24000
Gwin-Rockly-Rock outcrop complex, 50 to 90 percent south slopes4007DO159338531321zlbor62620181:24000
Gwin-Kettenbach-Rock outcrop complex, 60 to 90 percent south slopes6060DS8992437448nj36or63120181:24000
Gwin-Kettenbach-Rock outcrop complex, 30 to 60 percent south slopes6060CS3632437447nj34or63120181:24000
Umatilla-Kahler-Gwin complex, 35 to 70 percent slopes5859CO33824868491nz0qor63120181:24000
Gwin-Rock outcrop complex, 40 to 70 percent slopes4051DO724978172539or63120181:24000
Gwin-Klickson-Kettenbach complex, 60 to 90 percent slopes6121DO324374682mtd0or63120181:24000
Gwin-Rock outcrop complex, 40 to 70 percent slopes15F7646128621rzor64819771:24000
Gwin extremely stony silt loam, 12 to 40 percent slopes14E216128521ryor64819771:24000
Gwin-Rock outcrop complex, 40 to 70 percent slopes35F93354644892539or66719841:20000
Umatilla-Kahler-Gwin association, 35 to 70 percent slopes108F72290644202512or66719841:20000
Buckcreek-Gwin association, 45 to 70 percent slopes13F30270644522523or66719841:20000
Gwin-Klicker-Rock outcrop complex, 30 to 70 percent slopes34F16256644882538or66719841:20000
Gwin-Rockly-Rock outcrop complex, 20 to 50 percent south slopes4007BO7331214952ygf7or66719841:20000
Gwin-Kettenbach-Rock outcrop complex, 60 to 90 percent south slopes9515720848242v88or67019991:24000
Gwin-Kettenbach-Rock outcrop complex, 30 to 60 percent south slopes948151848232v87or67019991:24000
Gwin-Klickson-Kettenbach association, 60 to 90 percent slopes96459848252v89or67019991:24000
Gwin-Ninetysix complex, 30 to 70 percent north slopes214F19433916772nb76or6771:24000
Gwin very stony loam, 7 to 40 percent slopes140E65339167126bror6771:24000
Rock outcrop-Gwin complex, 15 to 70 percent south slopes141F21339165526bsor6771:24000
Gwin-Rockly-Rock outcrop complex, 20 to 50 percent south slopes168D18339168121zl9or6771:24000
Gwin-Linville complex, 30 to 65 percent slopes39773768534299swa07519751:20000
Gwin-Tucannon complex, 3 to 30 percent slopes40386368536299vwa07519751:20000
Gwin-Klickson-Kettenbach complex, 60 to 90 percent slopes6121DO25531225712ygdxwa60319841:24000
Gwin-Rockly-Rock outcrop complex, 20 to 50 percent south slopes4007BO21431225782ygdmwa60319841:24000
Gwin-Rockly-Rock outcrop complex, 50 to 90 percent south slopes4007DO20631225792ygdnwa60319841:24000
Gwin extremely rocky silt loam, 30 to 65 percent slopesGwF20524696682bhcwa61319671:20000
Gwin-Rockly-Rock outcrop complex, 50 to 90 percent south slopes4007DO97331146482ygdnwa61319671:20000
Gwin-Rockly-Rock outcrop complex, 20 to 50 percent south slopes4007BO27331146472ygdmwa61319671:20000
Gwin extremely stony silt loam, 10 to 50 percent slopesGnF24448698022bmpwa62319701:20000
Gwin-Rock outcrop complex, 10 to 50 percent slopesGrF11771698032bmqwa62319701:20000
Gwin-Rockly-Rock outcrop complex, 20 to 50 percent south slopes4007BO34331146882ygdmwa62319701:20000
Gwin-Rockly-Rock outcrop complex, 50 to 90 percent south slopes4007DO26631146892ygdnwa62319701:20000
Gwin cobbly silt loam, 30 to 65 percent slopes742419764732kkwwa63920031:24000
Gwin rocky silt loam, 30 to 60 percent slopesGrF8432713362d75wa67119611:31680
Gwin rocky silt loam, 0 to 30 percent slopes, erodedGrD21547713352d74wa67119611:31680
Gwin very rocky silt loam, 30 to 60 percent slopes, erodedGvF21347713382d77wa67119611:31680
Klicker-Gwin-Rockland complex, 30 to 60 percent slopesKrF1274713532d7qwa67119611:31680
Gwin-Rockland complex, 45 to 60 percent slopesGwF590713392d78wa67119611:31680
Gwin rocky silt loam, 0 to 30 percent slopesGrD273713342d73wa67119611:31680
Gwin-Rockly-Rock outcrop complex, 20 to 50 percent south slopes4007BO17831146652ygdmwa67119611:31680
Gwin very rocky silt loam, 0 to 30 percent slopes, erodedGvD2119713372d76wa67119611:31680
Klicker-Gwin-Rockland complex, 60 percent and steeper slopesKrG69713542d7rwa67119611:31680
Gwin-Rock outcrop complex, 40 to 70 percent slopes4051DO1731146632ygf6wa67119611:31680
Gwin very cobbly loam, 35 to 60 percent slopes20232470866452x50wa67620141:12000
Gwin very cobbly loam, 12 to 35 percent slopes2022980866472x52wa67620141:12000
Lorena-Gwin complex, 0 to 12 percent slopes4805940867632x8twa67620141:12000
Gwin very cobbly loam, 0 to 12 percent slopes2021490866502x55wa67620141:12000
Gwin-Rockly-Rock outcrop complex, 50 to 90 percent south slopes4007DO468231145182ygdnwa71420181:24000
Gwin-Rockly-Rock outcrop complex, 20 to 50 percent south slopes4007BO418031145172ygdmwa71420181:24000
Gwin-Klickson-Kettenbach complex, 60 to 90 percent slopes6121DO207231145052ygdxwa71420181:24000
Gwin-Rock outcrop complex, 40 to 70 percent slopes4051DO11031145122ygf6wa71420181:24000

Map of Series Extent

Approximate geographic distribution of the GWIN 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 .