Official Series Description


Lab Data Summary

Aggregate lab data for the NORWOOD soil series. This aggregation is based on all pedons with a current taxon name of NORWOOD, 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 NORWOOD 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
150A93P0490S1993TX089001Norwood7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties29.5080547,-96.3499985

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the NORWOOD 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 NORWOOD 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 NORWOOD 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 NORWOOD 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 NORWOOD 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 NORWOOD 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 NORWOOD 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.

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Soil series sharing subgroup-level classification with NORWOOD, 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. OK-2012-02-17-32 | Pittsburg County - May 1971

    Major soils and underlying material in soil associations 1, 2, 3, and 7 (Soil Survey of Pittsburg County, Oklahoma; May 1971).

  2. OK-2012-02-17-41 | Roger Mills County - August 1963

    Typical pattern of soils in associations 6, 7, and 9 (Soil Survey of Roger Mills County, Oklahoma; August 1963).

  3. OK-2012-02-17-42 | Roger Mills County - August 1963

    Typical pattern of soils in association 8. Woodward silt loam is a variation, which is described in the section "Descriptions of Soils" (Soil Survey of Roger Mills County, Oklahoma; August 1963).

  4. TX-2010-11-02-32 | Colorado County - 2006

    Pattern of soils and underlying material in the Norwood-Brazoria-Mohat general soil map unit (Soil Survey of Colorado County, Texas; 2006).

  5. TX-2010-11-04-02 | Matagorda County - 2001

    Typical pattern of soils and underlying material in the Brazoria-Norwood-Clemville general soil map unit (Soil Survey of Matagorda County, Texas; 2001).

  6. TX-2012-03-19-16 | Austin and Waller Counties - March 1984

    Pattern of soils in the Brazoria-Norwood association (Soil Survey of Austin and Waller Counties, TX; 1984).

  7. TX-2012-03-21-09 | Haskell County - March 1961

    Soils developed in red-bed clay and shale (Soil Survey of Haskell County, TX; 1961).

  8. TX-2012-03-22-02 | Wharton County - March 1974

    Relationship of soils to the landscape in association 4 (Soil Survey of Wharton County, TX; 1974).

  9. TX-2012-03-22-10 | Wilbarger County - September 1962

    Block diagram showing the geographical association of some of the soils developed in clays and shales. Norwood clay loam, which formed in recent alluvium, is in soil association 6 (Soil Survey of Wilbarger County, TX; 1962).

Map Units

Map units containing NORWOOD 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
Norwood silty clay loamNo20173566192m058ar11919721:20000
Norwood silty clay loamNo1089566389m0cmar13119711:20000
Coushatta silt loam, gently undulatingNr90424047762lqcfla04319821:24000
Norwood silt loamNd165916784311tbjyla07719801:24000
Norwood silt loam, 0 to 1 percent slopes, rarely flooded615817381845dtblok01319741:24000
Norwood silty clay loam, 0 to 1 percent slopes, rarely floodedNo1323571698m5wwok06119721:24000
Norwood loam, 0 to 1 percent slopes, rarely flooded461969571431m5m8ok07919811:24000
Norwood silty clay loam, 0 to 1 percent slopes, rarely flooded441173571429m5m6ok07919811:24000
Norwood silty clay loam, 1 to 3 percent slopes, rarely flooded45143571430m5m7ok07919811:24000
Norwood silt loam, 0 to 1 percent slopes, rarely flooded4213321064053kqfok10119841:24000
Norwood loam, 0 to 1 percent slopes, rarely flooded33132343630662vv3ctx03919791:20000
Norwood-Asa silt loams complex, 1 to 8 percent slopes, rarely flooded3529563630682zrtztx03919791:20000
Norwood silt loam, 1 to 5 percent slopes, rarely flooded3421463630672vv3dtx03919791:20000
Norwood loam, 0 to 1 percent slopes, rarely floodedNoA89423643032vv3ctx08919971:24000
Norwood silty clay loam, 0 to 1 percent slopes, occasionally floodedNrA6393364304d72rtx08919971:24000
Norwood silt loam, rarely floodedNw2406365540d8cmtx14719891:24000
Norwood loam, 0 to 1 percent slopes, rarely floodedNc185583659552vv3ctx15719561:20000
Norwood silty clay loam, 0 to 1 percent slopes, rarely floodedNd55323659562vv3ftx15719561:20000
Norwood silt loam, 0 to 1 percent slopes, rarely floodedNoA2190366798d9p6tx18519881:24000
Oklared-Norwood complex, frequently floodedOn877366801d9p9tx18519881:24000
Norwood silty clay loam, 0 to 1 percent slopes, rarely floodedNrA70366799d9p7tx18519881:24000
Norwood loam, 0 to 1 percent slopes, rarely floodedNo63173705162vv3ctx32119911:24000
Kiomatia and Norwood soils, frequently flooded382619373166dj9mtx47719791:24000
Oklared-Norwood complex, 0 to 1 percent slopes, occasionally flooded521302373182djb4tx47719791:24000
Norwood silt loam, 0 to 1 percent slopes, rarely flooded501174373180djb2tx47719791:24000
Norwood loam, 0 to 1 percent slopes, rarely floodedNoA210453732642vv3ctx48119681:20000
Norwood silt loam, 1 to 5 percent slopes, rarely floodedNoB42133732652vv3dtx48119681:20000
Mohat rarely flooded-Norwood frequently flooded complex, 1 to 8 percent slopesNr15493732662vv3gtx48119681:20000
Norwood silty clay loam, 0 to 1 percent slopes, rarely floodedNrA96943738752vv3ftx60019811:24000
Mohat rarely flooded-Norwood frequently flooded complex, 1 to 8 percent slopesOn94573738772vv3gtx60019811:24000
Norwood loam, 0 to 1 percent slopes, rarely floodedNoA14553738742vv3ctx60019811:24000
Norwood silt loam, 0 to 1 percent slopes, occasionally flooded381871393368f6b9tx61419751:20000

Map of Series Extent

Approximate geographic distribution of the NORWOOD 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 .