Soil Data Explorer - HARDEMAN

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 (updated 2020-03-18). Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

Pedons used in the lab summary:

MLRA	Lab ID	Pedon ID	Taxonname	CI	NSSL / NASIS Reports	Link To SoilWeb GMap
78B	80-OK-29-5	80-OK057-29-5	Hardeman	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	34.8885444,-99.8862194
78C	94P0720	94OK059013	Hardeman	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	36.6388893,-99.6086121
78C	97P0507	s97OK-065-006 hardeman	hardeman	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	34.6888885,-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.

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 (updated 2024-10-24), parsed OSD records (updated 2024-10-23) and snapshot of SC database (updated 2024-10-23).

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 (updated 2024-10-23).

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 (updated 2024-10-23).

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

Competing Series

Soil series competing with HARDEMAN share the same family level classification in Soil Taxonomy. Source: parsed OSD records (updated 2024-10-23) and snapshot of the SC database (updated 2024-10-23).

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 (updated 2024-10-23).

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 (updated 2024-10-23).

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 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 (updated 2024-10-23).

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, cool	HdmB	846	3101274	2tckh	ok007	2021	1:24000
Westola occasionally flooded-Quinlan-Hardeman complex, 0 to 12 percent slopes	WQHE	394	381558	2zc1f	ok007	2021	1:24000
Hardeman fine sandy loam, 1 to 3 percent slopes, cool	30	3426	381667	2tckh	ok009	1978	1:24000
Hardeman fine sandy loam, 3 to 5 percent slopes, cool	31	2564	381668	2tckj	ok009	1978	1:24000
Hardeman-Likes-Fortyone complex, 3 to 20 percent slopes	HLFF	58	623500	30yjb	ok009	1978	1:24000
Hardeman fine sandy loam, 5 to 8 percent slopes, cool	HaD	1318	382326	2tckk	ok039	1973	1:24000
Hardeman fine sandy loam, 8 to 15 percent slopes, cool	EfE	28252	382367	2tckl	ok043	1961	1:24000
Quinlan-Hardeman complex, 5 to 20 percent slopes	Qp	26425	382393	dtx8	ok043	1961	1:24000
Hardeman fine sandy loam, 3 to 5 percent slopes, cool	EfC	15136	382365	2tckj	ok043	1961	1:24000
Hardeman fine sandy loam, 5 to 8 percent slopes, cool	EfD	11681	382366	2tckk	ok043	1961	1:24000
Hardeman fine sandy loam, 1 to 3 percent slopes, cool	EfB	4970	382364	2tckh	ok043	1961	1:24000
Hardeman-Likes-Devol complex, 3 to 20 percent slopes	Br	2153	382355	2tckm	ok043	1961	1:24000
Hardeman-Likes-Devol complex, 3 to 20 percent slopes	Bn	35523	382422	2tckm	ok045	1963	1:24000
Hardeman-Southside-Arnett complex, 3 to 20 percent slopes	HSAF	11310	754292	30yjc	ok055	2005	1:24000
Hardeman fine sandy loam, 1 to 3 percent slopes, cool	HdmB	2948	648165	2tckh	ok055	2005	1:24000
Hardeman fine sandy loam, 3 to 5 percent slopes, cool	HdmC	2357	648166	2tckj	ok055	2005	1:24000
Arnett-Hardeman complex, 3 to 15 percent slopes	ArHF	669	378195	2yd7b	ok055	2005	1:24000
Hardeman-Southside-Arnett complex, 3 to 20 percent slopes	HSAF	4774	1385035	30yjc	ok057	1982	1:24000
Hardeman fine sandy loam, 1 to 3 percent slopes, cool	25	4379	975457	2tckh	ok057	1982	1:24000
Hardeman fine sandy loam, 3 to 5 percent slopes, cool	26	2395	975458	2tckj	ok057	1982	1:24000
Hardeman fine sandy loam, 5 to 8 percent slopes, cool	27	1015	975459	2tckk	ok057	1982	1:24000
Hardeman fine sandy loam, 8 to 15 percent slopes, cool	29	664	975461	2tckl	ok057	1982	1:24000
Hardeman fine sandy loam, 5 to 12 percent slopes, moderately eroded	28	540	975460	30yj6	ok057	1982	1:24000
Westola-Quinlan-Hardeman complex, 0 to 12 percent slopes	WQHE	41808	383108	dvnb	ok059	1998	1:24000
Hardeman fine sandy loam, 1 to 3 percent slopes, cool	HdmB	12479	382998	2tckh	ok059	1998	1:24000
Hardeman fine sandy loam, 3 to 5 percent slopes, cool	HdmC	2874	382999	2tckj	ok059	1998	1:24000
Kingsdown-Hardeman complex, 0 to 12 percent slopes	KiHE	2782	383205	dvrg	ok059	1998	1:24000
Hardeman-Grandmore complex, 1 to 3 percent slopes	HdGB	2587	383052	30yj7	ok059	1998	1:24000
Hardeman-Grandmore complex, 3 to 5 percent slopes	HdGC	398	383053	30yj8	ok059	1998	1:24000
Hardeman fine sandy loam, 1 to 3 percent slopes, cool	HdmB	7904	392374	2tckh	ok065	2000	1:24000
Hardeman fine sandy loam, 0 to 1 percent slopes	HdmA	4356	392373	30yj5	ok065	2000	1:24000
Hardeman fine sandy loam, 3 to 5 percent slopes, cool	HdmC	2598	392375	2tckj	ok065	2000	1:24000
Arnett-Hardeman complex, 3 to 15 percent slopes	ArHF	2251	392377	2yd7b	ok065	2000	1:24000
Hardeman fine sandy loam, 5 to 8 percent slopes, cool	HdmE	1929	392376	2tckk	ok065	2000	1:24000
Hardeman fine sandy loam, 5 to 8 percent slopes, cool	HaD	5800	383454	2tckk	ok075	1973	1:24000
Hardeman fine sandy loam, 3 to 5 percent slopes, cool	HaC	4594	383453	2tckj	ok075	1973	1:24000
Hardeman fine sandy loam, 1 to 3 percent slopes, cool	HaB	1563	383452	2tckh	ok075	1973	1:24000
Hardeman fine sandy loam, 1 to 3 percent slopes, cool	EnB	1491	383826	2tckh	ok093	1965	1:24000
Hardeman fine sandy loam, 3 to 5 percent slopes, cool	EnC	802	383827	2tckj	ok093	1965	1:24000
Hardeman-Likes-Devol complex, 3 to 20 percent slopes	PcE	30547	384759	2tckm	ok129	1961	1:24000
Hardeman fine sandy loam, 1 to 3 percent slopes, cool	HaB	8956	384952	2tckh	ok141	1968	1:24000
Hardeman-Likes-Fortyone complex, 3 to 20 percent slopes	HaE	2607	384954	30yjb	ok141	1968	1:24000
Hardeman fine sandy loam, 3 to 5 percent slopes, cool	HaC	2077	384953	2tckj	ok141	1968	1:24000
Hardeman fine sandy loam, 3 to 5 percent slopes, cool	28	7614	385012	2tckj	ok149	1976	1:24000
Hardeman fine sandy loam, 1 to 3 percent slopes, cool	27	4202	385011	2tckh	ok149	1976	1:24000
Hardeman fine sandy loam, 5 to 8 percent slopes, cool	29	2639	385013	2tckk	ok149	1976	1:24000
Hardeman fine sandy loam, 1 to 3 percent slopes, cool	HarB	5114	385197	2tckh	ok151	1995	1:24000
Hardeman fine sandy loam, 3 to 5 percent slopes, cool	HarC	4937	385198	2tckj	ok151	1995	1:24000
Hardeman fine sandy loam, 5 to 8 percent slopes, cool	HarD	4183	385199	2tckk	ok151	1995	1:24000
Hardeman fine sandy loam, 8 to 15 percent slopes, cool	HarE	3779	385200	2tckl	ok151	1995	1:24000
Hardeman-Devol complex, 8 to 20 percent slopes	EpE	9090	385272	30yj4	ok153	1961	1:24000
Hardeman loam, 3 to 5 percent slopes	EmC	6759	385270	30yj9	ok153	1961	1:24000
Hardeman-Devol complex, 5 to 8 percent slopes	EpD	5447	385271	30yj3	ok153	1961	1:24000
Hardeman fine sandy loam, 1 to 3 percent slopes, cool	EfB	3940	385269	2tckh	ok153	1961	1:24000
Hardeman fine sandy loam, 5 to 12 percent slopes	HaE	8530	362713	2t3rp	tx023	1971	1:24000
Hardeman fine sandy loam, 3 to 5 percent slopes	HaC	3388	362712	2t3rn	tx023	1971	1:24000
Hardeman fine sandy loam, dry, 1 to 3 percent slopes	EfB	1054	363814	2t3rr	tx075	1961	1:20000
Hardeman fine sandy loam, dry, 0 to 1 percent slopes	EfA	295	363813	2t3rq	tx075	1961	1:20000
Hardeman fine sandy loam, dry, 3 to 5 percent slopes	EfC	289	363815	2t3rs	tx075	1961	1:20000
Hardeman fine sandy loam, dry, 3 to 5 percent slopes	HaC	1255	364592	2t3rs	tx101	1969	1:20000
Hardeman fine sandy loam, dry, 1 to 3 percent slopes	HaB	1059	364591	2t3rr	tx101	1969	1:20000
Hardeman fine sandy loam, dry, 5 to 12 percent slopes	HaD	1018	364593	2t3rt	tx101	1969	1:20000
Hardeman fine sandy loam, dry, 0 to 1 percent slopes	HaA	488	364590	2t3rq	tx101	1969	1:20000
Hardeman fine sandy loam, dry, 1 to 3 percent slopes	HdB	374	644662	2t3rr	tx153	2004	1:24000
Hardeman fine sandy loam, 3 to 8 percent slopes	HaD	1443	3100963	f7d3	tx155	2021	1:24000
Hardeman fine sandy loam, 1 to 3 percent slopes	HaB	1351	3156117	2t3rm	tx155	2021	1:24000
Hardeman fine sandy loam, 0 to 1 percent slopes	HaA	833	3156115	2t3rl	tx155	2021	1:24000
Hardeman fine sandy loam, dry, 1 to 3 percent slopes	EfB	6945	366932	2t3rr	tx191	1965	1:20000
Hardeman fine sandy loam, dry, 0 to 1 percent slopes	EfA	6624	366931	2t3rq	tx191	1965	1:20000
Hardeman soils, wind-hummocky	Eh	3967	366934	d9tl	tx191	1965	1:20000
Hardeman fine sandy loam, dry, 3 to 5 percent slopes	EfC	2336	366933	2t3rs	tx191	1965	1:20000
Hardeman fine sandy loam, 1 to 3 percent slopes	HaB	5111	367134	2t3rm	tx197	1965	1:20000
Hardeman fine sandy loam, 0 to 1 percent slopes	HaA	1573	367133	2t3rl	tx197	1965	1:20000
Hardeman fine sandy loam, 3 to 5 percent slopes	HaC	1572	367135	2t3rn	tx197	1965	1:20000
Hardeman fine sandy loam, 8 to 30 percent slopes, severely eroded	HaE2	1173	367136	2z16p	tx197	1965	1:20000
Hardeman-Miles complex, 5 to 12 percent slopes	EpD	1575	367486	2z16q	tx207	1960	1:20000
Hardeman fine sandy loam, 1 to 5 percent slopes, moderately eroded	EnC2	803	367485	2z16n	tx207	1960	1:20000
Hardeman fine sandy loam, 1 to 3 percent slopes	EnB	801	367484	2t3rm	tx207	1960	1:20000
Hardeman fine sandy loam, dry, 1 to 5 percent slopes	HaC	1360	368588	2y892	tx269	1999	1:31680
Hardeman fine sandy loam, 5 to 12 percent slopes	16	8015	368716	2t3rp	tx275	1975	1:24000
Hardeman fine sandy loam, 3 to 5 percent slopes	15	4719	368715	2t3rn	tx275	1975	1:24000
Hardeman fine sandy loam, 1 to 3 percent slopes	14	4445	368714	2t3rm	tx275	1975	1:24000
Hardeman fine sandy loam, 0 to 1 percent slopes	13	2919	368713	2t3rl	tx275	1975	1:24000
Hardeman soils, strongly sloping	YHD	3526	369983	ddzy	tx307	1970	1:24000
Hardeman fine sandy loam, dry, 5 to 12 percent slopes	HaD	1616	372276	2t3rt	tx433	1970	1:24000
Hardeman fine sandy loam, 2 to 5 percent slopes	HaC	530	393202	f64y	tx453	1969	1:20000
Hardeman fine sandy loam, 5 to 12 percent slopes	HaE	316	393203	f64z	tx453	1969	1:20000
Hardeman soils and Urban land, 3 to 12 percent slopes	HdE	235	393204	f650	tx453	1969	1:20000
Hardeman fine sandy loam, 5 to 8 percent slopes, cool	HaD	8433	373306	2tckk	tx483	1970	1:24000
Hardeman fine sandy loam, 3 to 5 percent slopes, cool	HaC	1799	373305	2tckj	tx483	1970	1:24000
Hardeman fine sandy loam, 1 to 3 percent slopes	HaB	3245	373356	2t3rm	tx485	1972	1:20000
Hardeman fine sandy loam, 3 to 5 percent slopes	HaC	453	373357	2t3rn	tx485	1972	1:20000
Hardeman fine sandy loam, 1 to 3 percent slopes	EfB	4296	373415	2t3rm	tx487	1960	1:20000
Hardeman fine sandy loam, 0 to 1 percent slopes	EfA	1471	373414	2t3rl	tx487	1960	1:20000

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 (updated 2024-10-30).