Official Series Description


Lab Data Summary

Aggregate lab data for the WINK soil series. This aggregation is based on all pedons with a current taxon name of WINK, 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 WINK 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
4290P0495S1990NM013004Wink6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.6002502,-106.7334976

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the WINK 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 WINK 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 WINK 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 WINK 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 mountains figure.

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Competing Series

Soil series competing with WINK 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 WINK series and competing. 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 WINK 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 mountains figure.

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Click the image to view it full size.

Soil series sharing subgroup-level classification with WINK, 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 WINK 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
Ratliff-Wink fine sandy loamsMN48981376446dmqfnm02519671:20000
Wink fine sandWF15906376482dmrlnm02519671:20000
Wink loamy fine sandWK9772376483dmrmnm02519671:20000
Kermit-Wink complex, 0 to 3 percent slopesKE7505376429dmpwnm02519671:20000
Madurez-Wink associatin, gently slopingMWA51200556651vxnnm60019731:24000
Wink fine sandy loam, 0 to 5 percent slopesWaB17202557091vz2nm60019731:24000
Wink-Madurez associationWM13470557081vz1nm60019731:24000
Bluepoint-Wink, severely eroded complexBd39000556321vwlnm60019731:24000
Madurez-Wink association, undulatingMWB6000556661vxpnm60019731:24000
Wink-Embudo complex, 0 to 5 percent slopesWeB2760557101vz3nm60019731:24000
Wink-Madurez association, gently slopingWU49757558491w3lnm61219701:24000
Madurez-Wink association, undulatingMK36273558121w2dnm61219701:24000
Wink fine sandy loamWO11935558481w3knm61219701:24000
Wink loamy sandWk10859558501w3mnm61219701:24000
Wink loamy sand, hummockyWn6363558521w3pnm61219701:24000
Bluepoint-Wink complex, hummockyBs5903557771w18nm61219701:24000
Wink loamy sand, clayey substratumWm1144558511w3nnm61219701:24000
Wink-Caliza complex, 1 to 15 percent slopesWr910558531w3qnm61219701:24000
Wink complex, 1 to 9 percent slopes, erodedWs798558541w3rnm61219701:24000
Simona and Wink fine sandy loams, 0 to 3 percent slopes, erodedSN9673559221w5ynm61419661:20000
Wink loamy fine sand, 0 to 3 percent slopes, erodedWK6978559351w6cnm61419661:20000
Bluepoint-Onite-Wink association, nearly levelBOA11991635633pbf9nm64619761:24000
Wink-Dona Ana association, gently sloping8639426565661wvqnm66019811:48000
Wink silt loam, gently sloping851007565651wvpnm66019811:48000
Wink-Dona Ana loamy sands, 1 to 3 percent slopes6035863571441xgcnm66419841:24000
Copia-Wink-Tonuco complex, 0 to 18 percent slopes203814624843582rkmmnm68820141:24000
Wink-Pintura complexWP187555634598p9bxnm6901:24000
Wink-Harrisburg associationWH143501634597p9bwnm6901:24000
Wink fine sandy loam, nearly levelWNA2702586241z03tx61519941:31680
Hueco-Wink association, hummockyHW165095696628rcwwtx62419671:31680
Wink association, levelWKA24024696642rcxbtx62419671:31680

Map of Series Extent

Approximate geographic distribution of the WINK 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 .