Official Series Description


Lab Data Summary

Aggregate lab data for the NEWALLA soil series. This aggregation is based on all pedons with a current taxon name of NEWALLA, 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 NEWALLA 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
84A80-OK-14-3680-OK027-14-36Newalla4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.2321556,-97.188125
84A80-OK-14-3780-OK027-14-37Newalla4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.0725889,-97.2061528

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the NEWALLA 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 NEWALLA 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 NEWALLA 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 NEWALLA 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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Click the image to view it full size.

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.

Competing Series

Soil series competing with NEWALLA 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 NEWALLA 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 NEWALLA 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 NEWALLA, 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-2010-09-29-05 | Logan County - 2006

    Typical pattern of soils and underlying material in the Stephenville-Darsil-Harrah general soil map unit (Soil Survey of Logan County, Oklahoma; 2006).

  2. OK-2010-09-29-11 | Noble County - 2005

    Typical pattern of soils and underlying material in the Darnell-Grainola-Newalla-Harrah general soil map unit (Soil Survey of Noble County, Oklahoma; 2005).

  3. OK-2012-02-16-11 | Cleveland County - April 1987

    Typical pattern of soils and underlying material in the Stephenville-Harrah-Newalla map unit, the Stephenville-Littleaxe-Darsil map unit, and the Pulaski-Tribbey map unit (Soil Survey of Cleveland County, Oklahoma; April 1987).

Map Units

Map units containing NEWALLA 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
Stephenville-Darnell-Newalla complex, 3 to 8 percent slopesSEND611253820822y2rjok02719841:24000
Stephenville-Darnell-Newalla complex, 3 to 8 percent slopes, erodedSEND21189430900662y2rlok02719841:24000
Stephenville-Darnell-Newalla complex, 3 to 8 percent slopes, gulliedSEND4974630900652y2s6ok02719841:24000
Newalla fine sandy loam, 1 to 5 percent slopes6728473821302td5vok02719841:24000
Newalla sandy clay loam, 3 to 8 percent slopes, gullied68989382131dtmtok02719841:24000
Stephenville and Newalla soils, 3 to 8 percent slopes, gullied7015805382606dv44ok04919821:24000
Newalla fine sandy loam, 1 to 5 percent slopes50871427849602td5vok04919821:24000
Newalla fine sandy loam, 3 to 5 percent slopes, eroded5253663825862tq5wok04919821:24000
Newalla fine sandy loam, 1 to 5 percent slopes6043183826832td5vok05119751:24000
Newalla fine sandy loam, 3 to 5 percent slopes, eroded6118953826842tq5wok05119751:24000
Stephenville and Newalla soils, 3 to 8 percent slopes, severely erodedScC31734383248dvsvok06719671:24000
Newalla fine sandy loam, 1 to 5 percent slopesWhC11493832632td5vok06719671:24000
Stephenville-Darnell-Newalla complex, 3 to 8 percent slopes, erodedSEND21780430900682y2rlok08319941:12000
Stephenville-Darnell-Newalla complex, 3 to 8 percent slopesSEND1115630900692y2rjok08319941:12000
Newalla fine sandy loam, 1 to 5 percent slopesNewB23883836572td5vok08319941:12000
Stephenville-Urban land-Newalla complex, 1 to 8 percent slopesSUND3433836752scj0ok08319941:12000
Newalla-Gullied land complex, 3 to 8 percent slopesNeGD4196383656dw70ok08319941:12000
Newalla-Darnell complex, 8 to 45 percent slopes, very boulderyNeDG4151384092dwp2ok10319941:24000
Stephenville-Darnell-Newalla complex, 3 to 8 percent slopesSEND448230900732y2rjok10719961:24000
Stephenville-Darnell-Newalla complex, 3 to 8 percent slopesSEND5997130900772y2rjok10919961:12000
Stephenville-Urban land-Newalla complex, 1 to 8 percent slopesSUND123513843562scj0ok10919961:12000
Stephenville-Darnell-Newalla complex, 3 to 8 percent slopes, erodedSEND21013530900792y2rlok10919961:12000
Newalla fine sandy loam, 1 to 5 percent slopesNewB7613843352td5vok10919961:12000
Newalla fine sandy loam, 3 to 5 percent slopes, erodedNewC25753843362tq5wok10919961:12000
Newalla fine sandy loam, 1 to 5 percent slopesWhC147973846632td5vok12319671:24000
Newalla-Stephenville complex, 3 to 8 percent slopes, severely erodedWkC310833384664dx8jok12319671:24000
Newalla fine sandy loam, 1 to 5 percent slopes5442653847172td5vok12519751:24000
Stephenville and Newalla soils, 1 to 8 percent slopes, severely erodedSw323744384889dxhsok13719601:24000
Newalla fine sandy loam, 1 to 5 percent slopesWdB171373848912td5vok13719601:24000
Newalla-Darnell complex, 5 to 35 percent slopesWn5199384893dxhxok13719601:24000
Newalla fine sandy loam, 1 to 5 percent slopes, erodedWdB22823384892dxhwok13719601:24000

Map of Series Extent

Approximate geographic distribution of the NEWALLA 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 .