Official Series Description


Lab Data Summary

Aggregate lab data for the ORANGE soil series. This aggregation is based on all pedons with a current taxon name of ORANGE, 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 ORANGE were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

Click the image to view it full size.

Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
130B90P023389NC149005Orange6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.208889,-82.2911148
130B90P023489NC149006Orange6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.3952789,-82.2569427
13678P050378VA145009Orange6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.5417213,-78.008049
13640A4057S1965NC145006Orange6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.2634125,-78.8414078
13640A1301S1969VA109001ORANGE5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.9750481,-78.1497116
13640A1307S1969VA137002ORANGE6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.3250427,-77.7997055
n/a84P070584NC063013ORANGE6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

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

Click the image to view it full size.



Click the image to view it full size.

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the ORANGE series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

Click the image to view it full size.

Select annual climate data summaries for the ORANGE series and siblings. 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 ORANGE 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 .

Click the image to view it full size.

Click the image to view it full size.

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

Click the image to view it full size.

Click the image to view it full size.

Competing Series

Soil series competing with ORANGE share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

Click the image to view it full size.

Select annual climate data summaries for the ORANGE 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 ORANGE 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 ORANGE, 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 ORANGE 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
Jackland-Orange complex, 2 to 8 percent slopesJkB68529739202wx29nc03320161:24000
Orange silt loam, 0 to 3 percent slopesOr31401141163tr5nc13519751:20000
Orange gravelly loam, 2 to 7 percent slopesOrB58624412822myc1nc14519871:24000
Orange loam, 0 to 2 percent slopesOnA28724412802mybznc14519871:24000
Orange silt loam, 2 to 6 percent slopes, erodedOrB21331321454fhrsc02119601:20000
Orange loam, 0 to 4 percent slopesOaB46701311194dfnsc07919761:20000
Orange silt loam, 2 to 6 percent slopesOrB34531312294dk6sc08119601:20000
Orange silt loam, 6 to 10 percent slopes, erodedOrC22941312304dk7sc08119601:20000
Orange silt loam, 2 to 7 percent slopes63B6105164342xxyhva00319811:15840
Orange silt loam, 2 to 7 percent slopes, very stony64B3805164352xxyjva00319811:15840
Orange silt loam, 2 to 6 percent slopes, erodedOrB242461187693zl8va03719701:15840
Orange silt loam, 6 to 10 percent slopes, erodedOrC29761187703zl9va03719701:15840
Orange silt loam, 2 to 6 percent slopesOrB8641187683zl7va03719701:15840
Orange sandy loam, 2 to 6 percent slopes48B3131189063zqpva04119741:15840
Orange sandy loam, 6 to 12 percent slopes48C611189073zqqva04119741:15840
Orange silt loam, 2 to 7 percent slopes82B177222505032fjtwva05920071:12000
Hattontown-Orange complex, 2 to 7 percent slopes56B75222504122fjqyva05920071:12000
Orange silt loam, 7 to 15 percent slopes, very stony83C47922505052fjtyva05920071:12000
Hattontown-Orange complex, 7 to 15 percent slopes, very stony57C18422504152fjr1va05920071:12000
Orange silt loam, undulating phaseOc226412182842ryva06519501:15840
Orange silt loam, gravelly subsoil phaseOb56712182742rxva06519501:15840
Orange-Bremo silt loams, undulating phasesOa51312182642rwva06519501:15840
Orange loam, 2 to 7 percent slopes26B12371190123zv3va07519761:15840
Orange loam, 7 to 15 percent slopes26C3981190133zv4va07519761:15840
Rasalo-Orange complex, 2 to 8 percent slopes40B1205514728441lfm3va08320041:24000
Jackland-Orange complex, 2 to 8 percent slopes26B313414728231lflfva08320041:24000
Orange-Iredell complex, 2 to 7 percent slopes48B18401191273zytva08519761:15840
Helena-Orange complex, 7 to 15 percent slopes36C8601191103zy8va08519761:15840
Iredell-Orange complex, 7 to 15 percent slopes38C8501191123zybva08519761:15840
Orange loamOv1711192634036va08719731:15840
Orange silt loam, 2 to 7 percent slopesOrB1269119401407nva10919721:15840
Orange-Poindexter complex, 2 to 7 percent slopesOxB239119402407pva10919721:15840
Orange loam, 1 to 7 percent slopes18B765119457409gva11119791:20000
Orange silt loam, 1 to 6 percent slopesOaB2192611960540g7va11719901:24000
Orange silt loam, 6 to 12 percent slopesOaC88311960640g8va11719901:24000
Orange silt loam, concretionary variant, 2 to 7 percent slopesOgB124511989440rkva13719661:15840
Orange-Jackland silt loams, 0 to 2 percent slopesOrA9661198972zhg1va13719661:15840
Orange silt loam, concretionary variant, 0 to 2 percent slopesOgA94411989340rjva13719661:15840
Orange-Jackland silt loams, 2 to 7 percent slopesOrB3651198982zhg2va13719661:15840
Orange silt loam, concretionary variant, 2 to 7 percent slopes, moderately erodedOgB22741198952zhfzva13719661:15840
Orange-Jackland silt loams, 2 to 7 percent slopes, moderately erodedOrB21941198992zhg3va13719661:15840
Orange silt loam, concretionary variant, 7 to 15 percent slopes, moderately erodedOgC21021198962zhg0va13719661:15840
Orange loam, 0 to 4 percent slopes25B11521199772yzslva14319891:24000
Orange silt loam, undulating phaseOa8661202854155va14719501:20000
Orange-Iredell loams, 2 to 7 percent slopes33B1564120426419qva17719801:15840
Orange-Iredell loams, 7 to 15 percent slopes, eroded33C21119120427419rva17719801:15840
Orange loam, 2 to 6 percent slopesOrB130312055041fqva17919701:15840
Orange loam, 6 to 10 percent slopes, erodedOrC281212055141frva17919701:15840
Orange loam, 0 to 2 percent slopesOrA12912054941fpva17919701:15840
Hattontown - Orange complex, 2 to 7 percent slopes56B761907904221b9va60020071:12000
Hattontown-Orange complex, 7 to 15 percent slopes, very stony57C2830505352xn6rva60020071:12000
Orange silt loam, 2 to 7 percent slopes82B1219078912219wva60020071:12000

Map of Series Extent

Approximate geographic distribution of the ORANGE 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 .