Official Series Description


Lab Data Summary

Aggregate lab data for the HARDEMAN soil series. This aggregation is based on all pedons with a current taxon name of HARDEMAN, 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 HARDEMAN 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
78B80-OK-29-580-OK057-29-5Hardeman4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties34.8885444,-99.8862194
78C94P072094OK059013Hardeman7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.6388893,-99.6086121
78C97P0507s97OK-065-006 hardemanhardeman7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties34.6888885,-99.128891

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the HARDEMAN 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 HARDEMAN 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 HARDEMAN 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 HARDEMAN 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 HARDEMAN 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 HARDEMAN series and competing. 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 HARDEMAN 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.

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There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with HARDEMAN, 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-2012-02-16-41 | Harmon County - September 1984

    Typical pattern of soils and underlying material in the Tipton-Westview-Altus map unit (Soil Survey of Harmon County, Oklahoma; September 1984).

  2. TX-2010-11-03-50 | King County - 2007

    Typical pattern of the Grandfield-Shrewder-Devol and Delwin-Nobscot general soil map units (Soil Survey of King County, Texas; 2007).

  3. TX-2012-03-22-06 | Wheeler County - October 1975

    Relationship of soils in the Grandfield-Hardeman association to parent material and relief (Soil Survey of Wheeler County, TX; 1975).

Map Units

Map units containing HARDEMAN 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
Hardeman fine sandy loam, 1 to 3 percent slopes, coolHdmB84631012742tckhok00720211:24000
Westola occasionally flooded-Quinlan-Hardeman complex, 0 to 12 percent slopesWQHE3943815582zc1fok00720211:24000
Hardeman fine sandy loam, 1 to 3 percent slopes, cool3034263816672tckhok00919781:24000
Hardeman fine sandy loam, 3 to 5 percent slopes, cool3125643816682tckjok00919781:24000
Hardeman-Likes-Fortyone complex, 3 to 20 percent slopesHLFF5862350030yjbok00919781:24000
Hardeman fine sandy loam, 5 to 8 percent slopes, coolHaD13183823262tckkok03919731:24000
Hardeman fine sandy loam, 8 to 15 percent slopes, coolEfE282523823672tcklok04319611:24000
Quinlan-Hardeman complex, 5 to 20 percent slopesQp26425382393dtx8ok04319611:24000
Hardeman fine sandy loam, 3 to 5 percent slopes, coolEfC151363823652tckjok04319611:24000
Hardeman fine sandy loam, 5 to 8 percent slopes, coolEfD116813823662tckkok04319611:24000
Hardeman fine sandy loam, 1 to 3 percent slopes, coolEfB49703823642tckhok04319611:24000
Hardeman-Likes-Devol complex, 3 to 20 percent slopesBr21533823552tckmok04319611:24000
Hardeman-Likes-Devol complex, 3 to 20 percent slopesBn355233824222tckmok04519631:24000
Hardeman-Southside-Arnett complex, 3 to 20 percent slopesHSAF1131075429230yjcok05520051:24000
Hardeman fine sandy loam, 1 to 3 percent slopes, coolHdmB29486481652tckhok05520051:24000
Hardeman fine sandy loam, 3 to 5 percent slopes, coolHdmC23576481662tckjok05520051:24000
Arnett-Hardeman complex, 3 to 15 percent slopesArHF6693781952yd7bok05520051:24000
Hardeman-Southside-Arnett complex, 3 to 20 percent slopesHSAF4774138503530yjcok05719821:24000
Hardeman fine sandy loam, 1 to 3 percent slopes, cool2543799754572tckhok05719821:24000
Hardeman fine sandy loam, 3 to 5 percent slopes, cool2623959754582tckjok05719821:24000
Hardeman fine sandy loam, 5 to 8 percent slopes, cool2710159754592tckkok05719821:24000
Hardeman fine sandy loam, 8 to 15 percent slopes, cool296649754612tcklok05719821:24000
Hardeman fine sandy loam, 5 to 12 percent slopes, moderately eroded2854097546030yj6ok05719821:24000
Westola-Quinlan-Hardeman complex, 0 to 12 percent slopesWQHE41808383108dvnbok05919981:24000
Hardeman fine sandy loam, 1 to 3 percent slopes, coolHdmB124793829982tckhok05919981:24000
Hardeman fine sandy loam, 3 to 5 percent slopes, coolHdmC28743829992tckjok05919981:24000
Kingsdown-Hardeman complex, 0 to 12 percent slopesKiHE2782383205dvrgok05919981:24000
Hardeman-Grandmore complex, 1 to 3 percent slopesHdGB258738305230yj7ok05919981:24000
Hardeman-Grandmore complex, 3 to 5 percent slopesHdGC39838305330yj8ok05919981:24000
Hardeman fine sandy loam, 1 to 3 percent slopes, coolHdmB79043923742tckhok06520001:24000
Hardeman fine sandy loam, 0 to 1 percent slopesHdmA435639237330yj5ok06520001:24000
Hardeman fine sandy loam, 3 to 5 percent slopes, coolHdmC25983923752tckjok06520001:24000
Arnett-Hardeman complex, 3 to 15 percent slopesArHF22513923772yd7bok06520001:24000
Hardeman fine sandy loam, 5 to 8 percent slopes, coolHdmE19293923762tckkok06520001:24000
Hardeman fine sandy loam, 5 to 8 percent slopes, coolHaD58003834542tckkok07519731:24000
Hardeman fine sandy loam, 3 to 5 percent slopes, coolHaC45943834532tckjok07519731:24000
Hardeman fine sandy loam, 1 to 3 percent slopes, coolHaB15633834522tckhok07519731:24000
Hardeman fine sandy loam, 1 to 3 percent slopes, coolEnB14913838262tckhok09319651:24000
Hardeman fine sandy loam, 3 to 5 percent slopes, coolEnC8023838272tckjok09319651:24000
Hardeman-Likes-Devol complex, 3 to 20 percent slopesPcE305473847592tckmok12919611:24000
Hardeman fine sandy loam, 1 to 3 percent slopes, coolHaB89563849522tckhok14119681:24000
Hardeman-Likes-Fortyone complex, 3 to 20 percent slopesHaE260738495430yjbok14119681:24000
Hardeman fine sandy loam, 3 to 5 percent slopes, coolHaC20773849532tckjok14119681:24000
Hardeman fine sandy loam, 3 to 5 percent slopes, cool2876143850122tckjok14919761:24000
Hardeman fine sandy loam, 1 to 3 percent slopes, cool2742023850112tckhok14919761:24000
Hardeman fine sandy loam, 5 to 8 percent slopes, cool2926393850132tckkok14919761:24000
Hardeman fine sandy loam, 1 to 3 percent slopes, coolHarB51143851972tckhok15119951:24000
Hardeman fine sandy loam, 3 to 5 percent slopes, coolHarC49373851982tckjok15119951:24000
Hardeman fine sandy loam, 5 to 8 percent slopes, coolHarD41833851992tckkok15119951:24000
Hardeman fine sandy loam, 8 to 15 percent slopes, coolHarE37793852002tcklok15119951:24000
Hardeman-Devol complex, 8 to 20 percent slopesEpE909038527230yj4ok15319611:24000
Hardeman loam, 3 to 5 percent slopesEmC675938527030yj9ok15319611:24000
Hardeman-Devol complex, 5 to 8 percent slopesEpD544738527130yj3ok15319611:24000
Hardeman fine sandy loam, 1 to 3 percent slopes, coolEfB39403852692tckhok15319611:24000
Hardeman fine sandy loam, 5 to 12 percent slopesHaE85303627132t3rptx02319711:24000
Hardeman fine sandy loam, 3 to 5 percent slopesHaC33883627122t3rntx02319711:24000
Hardeman fine sandy loam, dry, 1 to 3 percent slopesEfB10543638142t3rrtx07519611:20000
Hardeman fine sandy loam, dry, 0 to 1 percent slopesEfA2953638132t3rqtx07519611:20000
Hardeman fine sandy loam, dry, 3 to 5 percent slopesEfC2893638152t3rstx07519611:20000
Hardeman fine sandy loam, dry, 3 to 5 percent slopesHaC12553645922t3rstx10119691:20000
Hardeman fine sandy loam, dry, 1 to 3 percent slopesHaB10593645912t3rrtx10119691:20000
Hardeman fine sandy loam, dry, 5 to 12 percent slopesHaD10183645932t3rttx10119691:20000
Hardeman fine sandy loam, dry, 0 to 1 percent slopesHaA4883645902t3rqtx10119691:20000
Hardeman fine sandy loam, dry, 1 to 3 percent slopesHdB3746446622t3rrtx15320041:24000
Hardeman fine sandy loam, 3 to 8 percent slopesHaD14433100963f7d3tx15520211:24000
Hardeman fine sandy loam, 1 to 3 percent slopesHaB135131561172t3rmtx15520211:24000
Hardeman fine sandy loam, 0 to 1 percent slopesHaA83331561152t3rltx15520211:24000
Hardeman fine sandy loam, dry, 1 to 3 percent slopesEfB69453669322t3rrtx19119651:20000
Hardeman fine sandy loam, dry, 0 to 1 percent slopesEfA66243669312t3rqtx19119651:20000
Hardeman soils, wind-hummockyEh3967366934d9tltx19119651:20000
Hardeman fine sandy loam, dry, 3 to 5 percent slopesEfC23363669332t3rstx19119651:20000
Hardeman fine sandy loam, 1 to 3 percent slopesHaB51113671342t3rmtx19719651:20000
Hardeman fine sandy loam, 0 to 1 percent slopesHaA15733671332t3rltx19719651:20000
Hardeman fine sandy loam, 3 to 5 percent slopesHaC15723671352t3rntx19719651:20000
Hardeman fine sandy loam, 8 to 30 percent slopes, severely erodedHaE211733671362z16ptx19719651:20000
Hardeman-Miles complex, 5 to 12 percent slopesEpD15753674862z16qtx20719601:20000
Hardeman fine sandy loam, 1 to 5 percent slopes, moderately erodedEnC28033674852z16ntx20719601:20000
Hardeman fine sandy loam, 1 to 3 percent slopesEnB8013674842t3rmtx20719601:20000
Hardeman fine sandy loam, dry, 1 to 5 percent slopesHaC13603685882y892tx26919991:31680
Hardeman fine sandy loam, 5 to 12 percent slopes1680153687162t3rptx27519751:24000
Hardeman fine sandy loam, 3 to 5 percent slopes1547193687152t3rntx27519751:24000
Hardeman fine sandy loam, 1 to 3 percent slopes1444453687142t3rmtx27519751:24000
Hardeman fine sandy loam, 0 to 1 percent slopes1329193687132t3rltx27519751:24000
Hardeman soils, strongly slopingYHD3526369983ddzytx30719701:24000
Hardeman fine sandy loam, dry, 5 to 12 percent slopesHaD16163722762t3rttx43319701:24000
Hardeman fine sandy loam, 2 to 5 percent slopesHaC530393202f64ytx45319691:20000
Hardeman fine sandy loam, 5 to 12 percent slopesHaE316393203f64ztx45319691:20000
Hardeman soils and Urban land, 3 to 12 percent slopesHdE235393204f650tx45319691:20000
Hardeman fine sandy loam, 5 to 8 percent slopes, coolHaD84333733062tckktx48319701:24000
Hardeman fine sandy loam, 3 to 5 percent slopes, coolHaC17993733052tckjtx48319701:24000
Hardeman fine sandy loam, 1 to 3 percent slopesHaB32453733562t3rmtx48519721:20000
Hardeman fine sandy loam, 3 to 5 percent slopesHaC4533733572t3rntx48519721:20000
Hardeman fine sandy loam, 1 to 3 percent slopesEfB42963734152t3rmtx48719601:20000
Hardeman fine sandy loam, 0 to 1 percent slopesEfA14713734142t3rltx48719601:20000

Map of Series Extent

Approximate geographic distribution of the HARDEMAN 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 .