Official Series Description


Lab Data Summary

Aggregate lab data for the MADRID soil series. This aggregation is based on all pedons with a current taxon name of MADRID, 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 MADRID 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
14390P011588NY035005Madrid4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.0144463,-74.5897217

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the MADRID 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 MADRID 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 MADRID 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 MADRID 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 MADRID 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 MADRID series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the MADRID 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 .

There are insufficient data to create the 2D hillslope position figure.

There are insufficient data to create the 3D hills figure.

There are insufficient data to create the 3D mountains figure.

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 MADRID, 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 MADRID 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
Madrid fine sandy loam, 8 to 15 percent slopesMaC4082901879qywny01919951:24000
Madrid fine sandy loam, 3 to 8 percent slopesMaB2122901869qyvny01919951:24000
Madrid sandy loam, 3 to 8 percent slopesMdB48682918709sq5ny04519811:15840
Madrid sandy loam, 8 to 15 percent slopesMdC39972918719sq6ny04519811:15840
Nellis and Madrid soils, 25 to 50 percent slopesNmE28962918912wrf4ny04519811:15840
Madrid sandy loam, 15 to 25 percent slopesMdD17992918729sq7ny04519811:15840
Madrid sandy loam, 0 to 3 percent slopesMdA1052918699sq4ny04519811:15840
Madrid loam, 8 to 15 percent slopes77C114931128662yfw2ny05120191:24000
Madrid loam, 3 to 8 percent slopes77B65831128652yfw1ny05120191:24000
Madrid loam, 25 to 50 percent slopes77F33331128682yfw4ny05120191:24000
Madrid loam, 15 to 25 percent slopes77D20931128672yfw3ny05120191:24000
Madrid fine sandy loam, 3 to 8 percent slopesMdB84492927299tlwny05519671:15840
Madrid fine sandy loam, 0 to 3 percent slopesMdA33502927289tlvny05519671:15840
Madrid very stony fine sandy loam, 3 to 8 percent slopesMeB14712927319tlyny05519671:15840
Madrid fine sandy loam, 8 to 15 percent slopesMdC7252927309tlxny05519671:15840
Madrid fine sandy loam, 2 to 8 percent slopesMdB83232936039vj2ny06719731:20000
Ontario and Madrid soils, 15 to 25 percent slopesOpD40492936352w3qgny06719731:20000
Madrid fine sandy loam, 8 to 15 percent slopesMdC16622936049vj3ny06719731:20000
Madrid gravelly loam, 2 to 8 percent slopesMgB14882936079vj6ny06719731:20000
Madrid fine sandy loam, 8 to 15 percent slopes, erodedMdC212092936059vj4ny06719731:20000
Madrid fine sandy loam, rollingMdCK11362936069vj5ny06719731:20000
Madrid gravelly loam, 8 to 15 percent slopesMgC4142936089vj7ny06719731:20000
Madrid fine sandy loam, 3 to 8 percent slopesMdB20262940529vzkny07319731:15840
Madrid fine sandy loam, 8 to 15 percent slopesMdC6522940539vzlny07319731:15840
Howard-Madrid complex, rollingHrC130452948169ws6ny10119721:15840
Howard-Madrid complex, undulatingHrB110042948159ws5ny10119721:15840
Howard-Madrid complex, 20 to 30 percent slopesHrD100552948179ws7ny10119721:15840
Madrid fine sandy loam, undulatingMaB13922948309wsnny10119721:15840
Madrid fine sandy loam, rollingMaC2892948319wspny10119721:15840
Madrid gravelly fine sandy loam, 2 to 8 percent slopesMdB102372957529xrdny11719721:15840
Madrid gravelly fine sandy loam, 8 to 15 percent slopesMdC41902957539xrfny11719721:15840
Madrid gravelly fine sandy loam, 15 to 25 percent slopesMdD8802957549xrgny11719721:15840
Howard-Madrid gravelly loams, 8 to 15 percent slopesHoC71762953749xc6ny12119691:20000
Howard-Madrid gravelly loams, 3 to 8 percent slopesHoB44172953739xc5ny12119691:20000
Howard-Madrid gravelly loams, 15 to 25 percent slopesHoD10252953759xc7ny12119691:20000
Madrid loam, 2 to 8 percent slopesMdB9572953969xcxny12119691:20000
Howard-Madrid channery silt loams, 8 to 15 percent slopesHrC6712953779xc9ny12119691:20000
Howard-Madrid channery silt loams, 3 to 8 percent slopesHrB5692953769xc8ny12119691:20000
Madrid fine sandy loam, 2 to 8 percent slopesMaB5582953949xcvny12119691:20000
Howard-Madrid channery silt loams, 15 to 25 percent slopesHrD3782953789xcbny12119691:20000
Madrid loam, 8 to 15 percent slopesMdC3772953979xcyny12119691:20000
Madrid fine sandy loam, 8 to 15 percent slopesMaC2062953959xcwny12119691:20000

Map of Series Extent

Approximate geographic distribution of the MADRID 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 .