Official Series Description


Lab Data Summary

Aggregate lab data for the HATBORO soil series. This aggregation is based on all pedons with a current taxon name of HATBORO, 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 HATBORO 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
14899P056899DE003001HATBORO5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.7307861,-75.7571361
14899P056999DE003002HATBORO6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.7348444,-75.762775
14800P061199MD005001Hatboro6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.4667778,-76.5722806
14800P0615S1999MD005100Hatboro5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.5230844,-76.4984722
14800P1340S2000MD005007Hatboro7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.4972639,-76.6978639

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the HATBORO 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 HATBORO 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 HATBORO 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 HATBORO 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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Competing Series

Soil series competing with HATBORO 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 HATBORO 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 HATBORO 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 hills figure.

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

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Soil series sharing subgroup-level classification with HATBORO, 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. MD-2010-09-07-03 | Frederick County - 2002

    Relationship of soils, topography, and underlying material in the Mt. Airy-Glenelg-Blocktown general soil map unit (Soil Survey of Frederick County, Maryland; 2002).

  2. MD-2010-09-10-01 | Cecil County -

    Elsinboro-Delanco-Sassafras association (Soil Survey of Cecil County, Maryland).

  3. MD-2010-09-10-02 | Cecil County -

    Glenelg-Brinklow-Manor-Glenville association (Soil Survey of Cecil County, Maryland).

  4. MD-2010-09-10-06 | Howard County - 2008

    Relationship of soils, topography, and underlying material in the Occoquan-Brinklow-Glenelg general soil map unit (Soil Survey of Howard County, Maryland; 2008).

  5. MD-2012-02-03-06 | Baltimore County - March 1976

    Cross section showing typical soil pattern in the Chester-Glenelg association (Soil Survey of Baltimore County, Maryland; March 1976).

  6. MD-2012-02-03-08 | Baltimore County - March 1978

    Cross section showing relationships of parent material and topography to certain soil series of Baltimore County. Fall line shown in drawing separates soil of Piedmont Province (left) from soils of Atlantic Coastal Plain (right) (Soil Survey of Baltimore County, Maryland; March 1976).

  7. MD-2012-02-03-18 | Frederick County - 2002

    Relationship of soils, topography, and underlying material in the Mt. Airy-Glenelg-Blocktown general soil map unit (Soil Survey of Frederick County, Maryland; 2002).

  8. NC-2010-09-28-10 | Surry County - 2007

    Relationship of soils, landscape, and geology in the Fairview general soil map unit and the Colvard and Suches general soil map unit (Soil Survey of Surry County, North Carolina; 2007).

  9. PA-2012-03-12-27 | Bucks and Philadelphia Counties - July 1975

    Typical pattern of soils and underlying material in the Urban land-Howell soil association (Soil Survey of Bucks and Philadelphia Counties County, PA; 1975).

Map Units

Map units containing HATBORO 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
Hatboro-Codorus complex, 0 to 3 percent slopes, frequently floodedHw355324798542p7h9de00320091:24000
Delanco-Codorus-Hatboro complex, 0 to 8 percent slopes, floodedDcB250724798602p7hhde00320091:24000
Hatboro silt loam, 0 to 3 percent slopes, frequently floodedHt35124798532p7h8de00320091:24000
Codorus and Hatboro soils, 0 to 2 percent slopes, frequently floodedCHA17321377334mb0md00320031:12000
Hatboro silt loams, 0 to 3 percent slopesHbA500224036822lp74md00520101:12000
Hatboro silt loam, 0 to 3 percent slopesHaA712224958362ptkdmd01320101:12000
Hatboro-Codorus complex, 0 to 3 percent slopes, floodedHw333824406992mxr7md01520091:12000
Hatboro silt loam, 0 to 3 percent slopes, frequently floodedHt153824406982mxr6md01520091:12000
Delanco-Codorus-Hatboro complex, 0 to 8 percent slopes, floodedDcB36624407082mxrjmd01520091:12000
Codorus and Hatboro silt loams, 0 to 3 percent slopesCgA6347534793kyhdmd02120011:12000
Hatboro-Codorus silt loams, 0 to 3 percent slopesHdA4246534818kyj6md02120011:12000
Foxville and Hatboro soils, 0 to 3 percent slopesFxA1933534811kyhzmd02120011:12000
Codorus and Hatboro silt loams, 0 to 3 percent slopesCo5055792809vlzhmd02720041:12000
Hatboro-Codorus silt loams, 0 to 3 percent slopesHa4167793006vm5vmd02720041:12000
Codorus and Hatboro soils, 0 to 2 percent slopes, frequently floodedCp24514793971lnfhmd02720041:12000
Hatboro silt loam, 0 to 3 percent slopes, frequently flooded54A10772533647kx9fmd03119891:15840
Codorus and Hatboro soils, frequently floodedCF250124552972ndy4md03320091:12000
Codorus-Hatboro-Urban land complex, frequently floodedCh123024552982ndy5md03320091:12000
Hatboro silt loamHh197534406ky2xmd04319981:12000
Foxville and Hatboro soilsFO113534327ky0cmd04319981:12000
Hatboro-Codorus complex, 0 to 3 percent slopes, frequently flooded50A7835338862w06dmd51019931:12000
Hatboro-Codorus complex, 0 to 3 percent slopes, frequently floodedHcA33095333532w06dmd60019721:15840
Hatboro silt loamHb3266533396kx1bmd60019721:15840
Hatboro loam, 0 to 2 percent slopes, frequently floodedHaA21123903372l7bnnc00319881:24000
Hatboro sandy loam, 0 to 2 percent slopes, frequently floodedHaA3261170083xrgnc02320001:24000
Hatboro loam, 0 to 2 percent slopes, frequently floodedHaA115426792402r935nc02720121:12000
Hatboro loam, 0 to 2 percent slopes, frequently floodedHaA26524314182mm2vnc03519691:15840
Hatboro loam, 0 to 2 percent slopes, frequently floodedHaA530024338062mpkwnc06719701:15840
Hatboro loam, 0 to 2 percent slopes, frequently floodedHdA253724334392mp61nc08119751:20000
Hatboro loamHa1849546863lc1rnc08919741:20000
Hatboro loam, 0 to 2 percent slopes, frequently floodedHaA31524244782mcvznc09720111:12000
Codorus and Hatboro soils, 0 to 2 percent slopes, frequently floodedCoA354124392852mw8mnc14519871:24000
Hatboro silt loam, 0 to 2 percent slopes, frequently flooded, long durationHbA389723899652l6ynnc15719831:24000
Hatboro loam, 0 to 2 percent slopes, frequently floodedHaA28814276301jxklnc17120051:24000
Hatboro loam, 0 to 2 percent slopes, frequently floodedHaA57123890752l60ync19319931:24000
Hatboro soils, 0 to 2 percent slopes, frequently floodedHsA102223980122lhb7nc19719601:15840
Hatboro loam, 0 to 2 percent slopes, frequently floodedHaA56123980142lhb9nc19719601:15840
Hatboro-Codorus complex, 0 to 3 percent slopes, frequently floodedHcuAt273214239872w06gnj01919701:24000
Hatboro-Codorus complex, 0 to 3 percent slopes, frequently floodedHcuAt282514036802w06gnj02119691:24000
Hatboro-Codorus complex, 0 to 3 percent slopes, frequently floodedHcuAt23813954112w06gnj02319851:24000
Hatboro-Codorus complex, 0 to 3 percent slopes, frequently floodedHcuAt439914440352w06gnj02719741:24000
Hatboro-Codorus complex, 0 to 3 percent slopes, frequently floodedHcuAt206914049872w06gnj03519721:24000
Hatboro-Codorus complex, 0 to 3 percent slopes, frequently floodedHcuAt122614526612w06gnj03919891:24000
Hatboro-Codorus complex, 0 to 3 percent slopes, frequently floodedHcuAt3811474812w06gnj04120071:12000
Hatboro silt loamHc5194545594l9qtpa00119911:24000
Hatboro silt loamHa4848543651l7q4pa01719971:24000
Hatboro-Codorus complex, 0 to 3 percent slopes, frequently floodedHbA12585436372w06gpa01719971:24000
Nanticoke-Hatboro silt loamsNa604543686l7r8pa01719971:24000
Hatboro silt loamHa1287314864101lwqqpa02920081:24000
Urban land-Hatboro complexUro16916120381r3g7pa02920081:24000
Hatboro silt loamHc9699216rglcpa04119801:15840
Hatboro silt loam, 0 to 3 percent slopes, frequently floodedHaA3347239618330cgmpa04519601:20000
Hatboro silt loamHm135545150l98hpa05519991:24000
Hatboro silt loamHa1953541182l54hpa09120081:12000
Hatboro-Codorus complex, 0 to 3 percent slopes, frequently floodedHbA1805432762w06gpa09520071:12000
Hatboro silt loamHa77114795191lnkfpa10119711:15840
Hatboro-Codorus complex, 0 to 3 percent slopes, frequently floodedHbA11314795062w06gpa10119711:15840
Hatboro silt loamHc1775542864l6wrpa13319901:24000
Hatboro loam, occasionally floodedHt1154526538knx3tn09120001:24000
Hatboro silt loam, frequently floodedHu15560975ltqztn09120001:24000
Hatboro silt loam, 0 to 2 percent slopes, occasionally flooded9535505165032v7kbva00319811:15840
Hatboro sandy loam, 0 to 3 percent slopes, frequently flooded1A211230484419va01320021:24000
Codorus-Hatboro complex, 0 to 3 percent slopes, frequently flooded2A15123049441bva01320021:24000
Codorus-Hatboro complex, 0 to 3 percent slopes, frequently flooded12A2012924793792p6zzva02920101:24000
Hatboro loam, 0 to 2 percent slopes, frequently flooded21A252024794112p710va02920101:24000
Hatboro silt loamHa9341519216kf8xva03519651:15840
Codorus-Hatboro silt loamsCs840519201kf8fva03519651:15840
Hatboro-Toxaway silt loamsHb674519217kf8yva03519651:15840
Codorus and Hatboro soils, 0 to 2 percent slopes, frequently flooded10A136017263021vyc5va04720061:24000
Codorus and Hatboro soils, 0 to 2 percent slopes, occasionally flooded30A1216522503192fjmyva05920071:12000
Hatboro silt loam, 0 to 2 percent slopes, frequently flooded49A110322503822fjpzva05920071:12000
Wheaton-Hatboro complex, 0 to 2 percent slopes, frequently flooded106A4722505592fjwpva05920071:12000
Hatboro silt loam, 0 to 2 percent slopes, frequently flooded4A5202189524621m4zva06120061:12000
Hatboro sandy loam, 0 to 3 percent slopes, frequently flooded26A65811914759228gfva06320071:24000
Hatboro sandy loam, 0 to 3 percent slopes, frequently flooded32A3720516749kbqbva07720061:24000
Hatboro loamHb1900516894kbw0va07919831:15840
Codorus and Hatboro soils, 0 to 2 percent slopes, frequently flooded14A2283114728051lfkvva08320041:24000
Hatboro loam, 0 to 2 percent slopes, frequently flooded4A3318642010pk20va10720061:12000
Hatboro-Codorus complex, 0 to 3 percent slopes, frequently floodedAc4455169152w06dva11319671:15840
Hatboro loam, 0 to 2 percent slopes, frequently flooded21A5391369464lhmva12519921:24000
Hatboro-Codorus complex, 0 to 3 percent slopes, frequently floodedMx48961198822w06dva13719661:15840
Hatboro silt loam, 0 to 2 percent slopes, frequently floodedWe10091199412zhh7va13719661:15840
Hatboro loam, 0 to 2 percent slopes, frequently flooded29A87814738041lgm2va14120081:24000
Hatboro silt loam, 0 to 2 percent slopes, frequently flooded41A17231200102yztgva14319891:24000
Hatboro-Codorus complex, 0 to 2 percent slopes27A3742521170kh9yva15319851:15840
Hatboro silt loam, 0 to 2 percent slopes26A322521169kh9xva15319851:15840
Hatboro-Codorus complex, 0 to 3 percent slopes, frequently floodedAd16545173922w06dva15719581:20000
Codorus and Hatboro soils, 0 to 2 percent slopes, occasionally flooded30A2291912968226lnva51020071:12000
Hatboro silt loam, 0 to 2 percent slopes, occasionally flooded95724964532v7kbva54020111:24000
Codorus and Hatboro soils, 0 to 2 percent slopes, occasionally flooded30A7619078822219lva60020071:12000
Hatboro silt loam, 0 to 2 percent slopes, frequently flooded49A11912937226knva60020071:12000
Codorus and Hatboro soils, 0 to 2 percent slopes, occasionally flooded30A11190783722184va61020071:12000

Map of Series Extent

Approximate geographic distribution of the HATBORO 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 .