Official Series Description


Lab Data Summary

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

There are insufficient data to create the lab data summary figure.


Water Balance

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

Click the image to view it full size.

Click the image to view it full size.

Soil series sharing subgroup-level classification with HARRIET, 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. ND-2010-09-27-03 | Billings County - 2005

    Typical pattern of soils and underlying material in the Janesburg-Dogtooth association (Soil Survey of Billings County, North Dakota; 2005).

  2. ND-2010-09-27-05 | Burke County - 2003

    Typical pattern of soils and underlying material in the Noonan-Niobell association (Soil Survey of Burke County, North Dakota; 2003).

  3. ND-2010-09-27-16 | Morton County - 2002

    Typical pattern of soils and underlying materials in the Ekalaka-Lakota-Vebar-Desart association (Soil Survey of Morton County, North Dakota; 2002).

  4. ND-2010-09-27-18 | Morton County - 2002

    Typical pattern of soils and underlying materials in the Vebar-Parshall association (Soil Survey of Morton County, North Dakota; 2002).

  5. ND-2012-02-07-02 | Adams County - September 1987

    Typical pattern of soils and underlying material in the Belfield-Amor-Daglum association (Soil Survey of Adams County, North Dakota; September 1987).

  6. ND-2012-02-07-23 | Dickey County - May 1993

    Typical pattern of soils and parent material in the Cavour-Barnes association (Soil Survey of Dickey County, North Dakota; May 1993).

  7. ND-2012-02-07-28 | Divide County - 2002

    Typical pattern of soils and underlying material in the Noonan-Niobell association (Soil Survey of Divide County, North Dakota; 2002).

  8. ND-2012-02-07-34 | Dunn County - April 1982

    Typical pattern of soils and underlying material in the Baahish-Lakoa-Hidatsa association (Soil Survey of Dunn County, North Dakota; April 1982).

  9. ND-2012-02-08-11 | Hettinger County - May 1990

    Typical pattern of soils and underlying material in the Belfield-Amor-Regent association (Soil Survey of Hettinger County, North Dakota; May 1990).

  10. ND-2012-02-08-12 | Hettinger County - May 1990

    Typical pattern of soils and underlying material in the Daglum-Belfield-Amor association (Soil Survey of Hettinger County, North Dakota; May 1990).

  11. ND-2012-02-08-13 | Hettinger County - May 1990

    Typical pattern of soils and underlying material in the Harriet-Dagum-Belfield association (Soil Survey of Hettinger County, North Dakota; May 1990).

  12. SD-2012-03-14-09 | Brown County - April 1993

    Typical pattern of soils and parent material in the Aberdeen-Exline-Harriet and Williams-Bowbells associations (Soil Survey of Brown County, SD; 1993).

  13. SD-2012-03-14-11 | Brown County - April 1993

    Typical pattern of soils and parent material in the Niobell-Noonan-Williams association (Soil Survey of Brown County, SD; 1993).

  14. SD-2012-03-15-34 | Faulk County - January 1984

    Pattern of soils and parent material in the Max-Niobell-Noonan association (Soil Survey of Faulk County, SD; 1984).

Map Units

Map units containing HARRIET 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
Harriet loam, 0 to 2 percent slopes, occasionally floodedE4005A1916425257541vzvmnd00119831:20000
Korchea, saline-Fluvaquents, channeled-Harriet complex, 0 to 2 percent slopes, frequently floodedE4184A9727556622qz85nd00119831:20000
Harriet loam, 0 to 1 percent slopes, occasionally floodedF554A925877252q56rnd0051:12000
Harriet loam, 0 to 2 percent slopes, occasionally floodedE4005A398527071031vzvmnd00719981:24000
Harriet loam, low precipitation, 0 to 2 percent slopes, occasionally floodedL4009A3627070702q389nd00719981:24000
Korchea, saline-Fluvaquents, channeled-Harriet complex, 0 to 2 percent slopes, frequently floodedE4184A347025635652qz85nd01119691:20000
Harriet loam, 0 to 2 percent slopes, occasionally floodedE4005A108425635591vzvmnd01119691:20000
Harriet-Lallie complex, 0 to 2 percent slopes, occasionally floodedE4007A25425635601vzvnnd01119691:20000
Harriet loam, low precipitation, 0 to 2 percent slopes, occasionally floodedL4009A7225634932q389nd01119691:20000
Harriet, Regan, and Stirum soils, 0 to 2 percent slopes216920376341110cfyknd01319911:24000
Harriet-Regan-Stirum complex, 0 to 2 percent slopes, occasionally floodedC580A151525640802q2krnd01319911:24000
Harriet-Regan-Stirum complex, 0 to 2 percent slopes, occasionally floodedC580A1403525968212q2krnd01519671:20000
Harriet loam, 0 to 2 percent slopesC584A374425641582q4w9nd01519671:20000
Daglum-Belfield-Harriet occasionally flooded, complex, 0 to 2 percent slopesC525A124825641742q6lxnd01519671:20000
Harriet loam, 0 to 2 percent slopes, occasionally floodedE4005A11226617001vzvmnd01519671:20000
Harriet loam, 0 to 1 percent slopes, occasionally floodedG554A110625753572q5pmnd02119891:20000
Harriet loam, 0 to 2 percent slopesC584A6525642262q4w9nd02119891:20000
Harriet, Regan, and Stirum soils, 0 to 2 percent slopes21698665341310cg50nd02319921:24000
Harriet-Regan-Stirum complex, 0 to 2 percent slopes, occasionally floodedC580A264625642532q2krnd02319921:24000
Harriet loam, 0 to 2 percent slopes, occasionally floodedE4005A1783227072401vzvmnd02519811:20000
Harriet loam, low precipitation, 0 to 2 percent slopes, occasionally floodedL4009A2327071332q389nd02519811:20000
Harriet loam, 0 to 2 percent slopes, occasionally floodedE4005A1127426617861vzvmnd02919791:20000
Harriet loam, 0 to 2 percent slopesC584A740325643272q4w9nd02919791:20000
Ranslo-Harriet loams, 0 to 2 percent slopes, occasionally floodedC578A6925954632qyfqnd02919791:20000
Harriet-Regan-Stirum complex, 0 to 2 percent slopes, occasionally floodedC580A2725968342q2krnd02919791:20000
Harriet loam, 0 to 2 percent slopes, occasionally floodedE4005A1350025258871vzvmnd03719851:20000
Harriet loam, 0 to 2 percent slopes, occasionally floodedE4005A1121025258121vzvmnd04119861:20000
Harriet loam, 0 to 2 percent slopesC584A1027125644092q4w9nd04319851:20000
Harriet-Regan-Stirum complex, 0 to 2 percent slopes, occasionally floodedC580A9825966532q2krnd04319851:20000
Harriet loam, 0 to 1 percent slopes, occasionally floodedG554A237625771032q5pmnd04519661:20000
Harriet-Regan-Stirum complex, 0 to 2 percent slopes, occasionally floodedC580A572125966982q2krnd04719921:20000
Harriet loam, 0 to 2 percent slopes, occasionally floodedE4005A309426618661vzvmnd04719921:20000
Harriet loam, 0 to 1 percent slopes, occasionally floodedG554A752825713862q5pmnd04919871:20000
Harriet loam, 0 to 1 percent slopes, occasionally floodedF554A80825857402q56rnd04919871:20000
Harriet loam, 0 to 2 percent slopesC584A905325665992q4w9nd05119921:24000
Harriet-Regan-Stirum complex, 0 to 2 percent slopes, occasionally floodedC580A180925967642q2krnd05119921:24000
Harriet loam, 0 to 2 percent slopes, occasionally floodedE4005A60826620021vzvmnd05119921:24000
Ranslo-Harriet loams, 0 to 2 percent slopes, occasionally floodedC578A11925955342qyfqnd05119921:24000
Harriet loam, 0 to 2 percent slopes, occasionally floodedE4005A886526993331vzvmnd05320031:24000
Harriet loam, low precipitation, 0 to 2 percent slopes, occasionally floodedL4009A4627151632q389nd05320031:24000
Harriet-Regan-Stirum complex, 0 to 2 percent slopes, occasionally floodedC580A923825968682q2krnd05519741:20000
Harriet loam, 0 to 2 percent slopes, occasionally floodedE4005A450326624611vzvmnd05519741:20000
Harriet loam, 0 to 1 percent slopes, occasionally floodedG554A27225771942q5pmnd05519741:20000
Harriet loam, 0 to 2 percent slopes, occasionally floodedE4005A245926992691vzvmnd05719761:20000
Harriet loam, 0 to 2 percent slopes, occasionally floodedE4005A1294526991681vzvmnd05919981:20000
Harriet loam, 0 to 2 percent slopes, occasionally floodedE4005A579626625221vzvmnd06119881:24000
Harriet loam, 0 to 2 percent slopesC584A517425667562q4w9nd06119881:24000
Harriet-Regan-Stirum complex, 0 to 2 percent slopes, occasionally floodedC580A22025670872q2krnd06119881:24000
Harriet loam, 0 to 2 percent slopes, occasionally floodedE4005A273425259861vzvmnd06519711:20000
Harriet loam, 0 to 1 percent slopes, occasionally floodedF554A110025881612q56rnd07919901:24000
Harriet loam, 0 to 2 percent slopesC584A340325668032q4w9nd08319901:20000
Harriet loam, 0 to 1 percent slopes, occasionally floodedG554A168825819952q5pmnd08319901:20000
Harriet-Regan-Stirum complex, 0 to 2 percent slopes, occasionally floodedC580A825968712q2krnd08319901:20000
Velva-Harriet complex, 0 to 2 percent slopes, occasionally floodedE4703A17722699137d1y5nd08519921:24000
Harriet loam, 0 to 2 percent slopes, occasionally floodedE4005A146226990941vzvmnd08519921:24000
Harriet loam, 0 to 2 percent slopes, occasionally floodedE4005A1072827158561vzvmnd08719741:20000
Harriet loam, low precipitation, 0 to 2 percent slopes, occasionally floodedL4009A16927159452q389nd08719741:20000
Korchea, saline-Fluvaquents, channeled-Harriet complex, 0 to 2 percent slopes, frequently floodedE4184A2327585222qz85nd08719741:20000
Harriet loam, 0 to 2 percent slopes, occasionally floodedE4005A457327160001vzvmnd08919651:20000
Harriet-Lallie complex, 0 to 2 percent slopes, occasionally floodedE4007A12427160011vzvnnd08919651:20000
Harriet loam, strongly saline, 0 to 1 percent slopes, occasionally floodedF552A200225851212q56qnd10119671:20000
Harriet-Regan-Stirum complex, 0 to 2 percent slopes, occasionally floodedC580A141025968802q2krnd10119671:20000
Harriet loam, 0 to 1 percent slopes, occasionally floodedF554A70625852492q56rnd10119671:20000
Harriet and Vallers soils, strongly salineHk232352505ctt4nd10119671:20000
Harriet loam, 0 to 2 percent slopesC584A125669212q4w9nd10119671:20000
Harriet loam, 0 to 1 percent slopes, occasionally floodedG554A193225796732q5pmnd10319661:12000
Harriet-Regan-Stirum complex, 0 to 2 percent slopes, occasionally floodedC580A122025968812q2krnd10319661:12000
Harriet and Stirum soils, 0 to 2 percent slopes227012011339048cct1nd10519931:24000
Harriet-Regan-Stirum complex, 0 to 2 percent slopes, occasionally floodedC580A228925967822q2krnd10519931:24000
Harriet loam, 0 to 2 percent slopes, occasionally floodedE4005A170726625731vzvmnd10519931:24000
Ranslo-Harriet loams, 0 to 2 percent slopes, occasionally floodedG553A597527977922sd46sd01319871:20000
Harriet loam, 0 to 2 percent slopesC584A457927655752q4w9sd01319871:20000
Harriet loam, 0 to 1 percent slopes, occasionally floodedG554A403027976902q5pmsd01319871:20000
Ranslo-Harriet loams, 0 to 2 percent slopes, occasionally floodedC578A264527655822qyfqsd01319871:20000
Straw-Harriet loams, 0 to 2 percent slopesC498A161727655942rrqrsd01319871:20000
Koto-Harriet loams, 0 to 2 percent slopesC589A108227655992rrr1sd01319871:20000
La Prairie-Harriet loams, 0 to 2 percent slopes, occasionally floodedG555A38327977932sd47sd01319871:20000
Harriet loam, 0 to 2 percent slopesC584A612927978952q4w9sd02119781:20000
Ranslo-Harriet loams, 0 to 2 percent slopes, occasionally floodedC578A513727979072qyfqsd02119781:20000
Harriet silt loam15828354682cx2csd02119781:20000
Ranslo-Harriet silt loams71204354741cx48sd02119781:20000
Ranslo-Harriet loams, 0 to 2 percent slopes, occasionally floodedG553A34927980222sd46sd02519921:20000
Harriet loam, 0 to 1 percent slopes, occasionally floodedG554A12427979792q5pmsd02519921:20000
Harriet loam, strongly saline, 0 to 1 percent slopes, occasionally floodedG552A5327979782q5plsd02519921:20000
Harriet loamHd4417735g0pbsd02519921:20000
Harriet loamHd2928356167cym8sd03119861:24000
Ranslo-Harriet loams, 0 to 2 percent slopes, occasionally floodedG553A65327985102sd46sd03719921:20000
Harriet loam, 0 to 1 percent slopes, occasionally floodedG554A57727984642q5pmsd03719921:20000
Ranslo-Harriet loams, 0 to 2 percent slopes, occasionally floodedC578A1107127985802qyfqsd04519731:20000
Ranslo-Harriet loams, 0 to 2 percent slopes, occasionally floodedC578A874927986472qyfqsd04919811:20000
Ranslo-Harriet silt loamsRh3913355193cxlvsd04919811:20000
Harriet silt loamHa2286355171cxl4sd04919811:20000
Harriet loam, 0 to 2 percent slopesC584A192727986412q4w9sd04919811:20000
Ranslo-Harriet loams, 0 to 2 percent slopes, occasionally floodedC578A1416427987462qyfqsd08919801:20000
Harriet loam, 0 to 2 percent slopesC584A630927987312q4w9sd08919801:20000
Ranslo-Harriet loams, 0 to 2 percent slopes, occasionally floodedG553A152127992502sd46sd08919801:20000
Harriet loam, 0 to 1 percent slopes, occasionally floodedG554A39927988162q5pmsd08919801:20000
La Prairie-Harriet loams, 0 to 2 percent slopes, occasionally floodedG555A21427992512sd47sd08919801:20000
Ranslo-Harriet loams, 0 to 2 percent slopes, occasionally floodedG553A827993552sd46sd09119701:20000
Harriet loam, 0 to 2 percent slopesC584A37327994622q4w9sd10719831:20000
Ranslo-Harriet loams, 0 to 2 percent slopes, occasionally floodedG553A1439027996132sd46sd11519971:24000
Harriet loam, 0 to 1 percent slopes, occasionally floodedG554A314827995562q5pmsd11519971:24000
Harriet loam, 0 to 2 percent slopesC584A99527995002q4w9sd11519971:24000
Ranslo-Harriet loams, 0 to 2 percent slopes, occasionally floodedC578A83427995062qyfqsd11519971:24000
Harriet loam, strongly saline, 0 to 1 percent slopes, occasionally floodedG552A3627995552q5plsd11519971:24000
Harriet loam, 0 to 2 percent slopesC584A120028001032q4w9sd12919751:20000

Map of Series Extent

Approximate geographic distribution of the HARRIET 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 .