Soil Data Explorer - HAWTHORNE

Official Series Description

Lab Data Summary

Aggregate lab data for the HAWTHORNE soil series. This aggregation is based on all pedons with a current taxon name of HAWTHORNE, 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 HAWTHORNE 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
123	85P0182	1982TN003018	Hawthorne	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	35.3553848,-86.4802551

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the HAWTHORNE 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 HAWTHORNE 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 HAWTHORNE 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 HAWTHORNE 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 terrace figure.

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

Competing Series

Soil series competing with HAWTHORNE 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 HAWTHORNE 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 HAWTHORNE 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 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 HAWTHORNE, 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. TN-2010-11-02-02 | Cannon County - 2003

   Typical pattern of soils and parent material in the Hawthorne-Dellrose-Gladdice-Rock outcrop general soil map unit (Soil Survey of Cannon County, Tennessee; 2003).

2. TN-2010-11-02-07 | Dickson County -

   The relationship of soils and landscape in the Hawthorne-Sulphura-Sengtown and Wolftever-Beason-Melvin general soil map units (Soil Survey of Dickson County, Tennessee).

3. TN-2010-11-02-22 | Moore County - 2006

   Typical pattern of soils and parent material in the Hawthore-Dellrose-Mimosa general soil map unit (Soil Survey of Moore County, Tennessee; 2006).

4. TN-2010-11-02-24 | Moore County - 2006

   Typical pattern of soils and parent material in the Mimosa-Barfield-Rock outcrop general soil map unit (Soil Survey of Moore County, Tennessee; 2006).

5. TN-2012-03-16-02 | Cheatham County - 2002

   Relationship of soils to topography and the underlying material in the Beason-Wolftever-Melvin-Arrington and Hawthorne-Sulphura-Sengtown general soil map units (Soil Survey of Cheatham County, TN; 2002).

6. TN-2012-03-16-03 | Cheatham County - 2002

   Relationship of soils to topography and the underlying material in the Byler-Nolin-Armour-Arrington general soil map unit. The Hawthorne and Suphura soils are adjacen to the map unit (Soil Survey of Cheatham County, TN; 2002).

7. TN-2012-03-16-05 | Dickson County - 2002

   The relationship of soils, landscape, and parent material in the Hawthorne-Sulphura-Sengtown and the Wolftever-Beason-Melvin general soil map units (Soil Survey of Dickson County, TN; 2002).

Map Units

Map units containing HAWTHORNE 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
Hawthorne-Sengtown-Sugargrove complex, 20 to 70 percent slopes	HsF	6142	2232300	2dxwp	ky610	1968	1:12000
Sugargrove-Sengtown-Hawthorne complex, 12 to 20 percent slopes, severely eroded	ShD3	270	2232260	2dxvd	ky610	1968	1:12000
Hawthorne-Sengtown-Sugargrove complex, 20 to 70 percent slopes, severely eroded	HsF3	226	2623443	2qykj	ky610	1968	1:12000
Hawthorne gravelly silt loam, 15 to 45 percent slopes	HhE	8154	529381	2v5ck	tn003	1998	1:24000
Hawthorne gravelly silt loam, 5 to 15 percent slopes	HhC	4987	529380	2v648	tn003	1998	1:24000
Sugargrove-Sengtown-Hawthorne complex, 12 to 25 percent slopes	SuE	31650	2545390	2qshn	tn005	2011	1:12000
Hawthorne, Sengtown, and Sugargrove soils, 25 to 70 percent slopes	HTF	25038	2545345	2qsg4	tn005	2011	1:12000
Hawthorne gravelly silt loam, 12 to 25 percent slopes	HtE	6440	2545343	2qsg2	tn005	2011	1:12000
Sugargrove-Sengtown-Hawthorne complex, 5 to 12 percent slopes	SuC	2621	2545391	2qshp	tn005	2011	1:12000
Hawthorne gravelly silt loam, 5 to 12 percent slopes	HtC	303	2545344	2qsg3	tn005	2011	1:12000
Hawthorne gravelly silt loam, 20 to 60 percent slopes	HbF	24069	524436	2z6xv	tn015	1999	1:24000
Hawthorne gravelly silt loam, 5 to 20 percent slopes	HbD	1706	524435	2z6xy	tn015	1999	1:24000
Hawthorne-Sulphura association, 20 to 60 percent slopes	HsF	67381	527015	2v5c6	tn021	1991	1:24000
Hawthorne gravelly silt loam, 12 to 20 percent slopes	HaD	10891	527014	2v59f	tn021	1991	1:24000
Hawthorne gravelly silt loam, 5 to 12 percent slopes	HaC	8124	527013	kpdf	tn021	1991	1:24000
Hawthorne gravelly silt loam, 20 to 60 percent slopes	HbF	13691	531121	2z6xv	tn027	2002	1:24000
Hawthorne gravelly silt loam, 5 to 20 percent slopes	HbD	5091	636814	2z6xy	tn027	2002	1:24000
Hawthorne gravelly silt loam, 20 to 60 percent slopes	HbF	18413	2987677	2z6xv	tn031	1956	1:20000
Hawthorne-Sugargrove complex, 5 to 20 percent slopes	HsD	3959	524866	2z6xt	tn031	1956	1:20000
Hawthorne gravelly silt loam, 20 to 60 percent slopes	HbF	27644	527044	2z6xv	tn041	1968	1:15840
Hawthorne-Rock outcrop complex, 40 to 80 percent slopes	HrF	8147	527045	2z6xx	tn041	1968	1:15840
Hawthorne-Sugargrove complex, 5 to 20 percent slopes	HsD	7939	527043	2z6xt	tn041	1968	1:15840
Hawthorne-Sulphura association, 20 to 60 percent slopes	HsF	37475	527108	2v5c6	tn043	1993	1:24000
Hawthorne-Sugargrove complex, 5 to 12 percent slopes	HgC	3305	527107	kphg	tn043	1993	1:24000
Hawthorne gravelly silt loam, 12 to 20 percent slopes	HaD	1422	527106	2v59f	tn043	1993	1:24000
Sugargrove-Sengtown-Hawthorne complex, 12 to 25 percent slopes	SuE	2005	2545312	2qs9t	tn079	2012	1:12000
Hawthorne, Sengtown, and Sugargrove soils, 25 to 70 percent slopes	HTF	841	2545261	2qs85	tn079	2012	1:12000
Hawthorne gravelly silt loam, 12 to 25 percent slopes	HtE	88	2545260	2qs84	tn079	2012	1:12000
Sugargrove-Sengtown-Hawthorne complex, 5 to 12 percent slopes	SuC	64	2545313	2qs9v	tn079	2012	1:12000
Hawthorne-Sulphura association, 20 to 60 percent slopes	HsF	10113	527467	2v5c6	tn081	1997	1:24000
Hawthorne gravelly silt loam, 20 to 60 percent slopes	HbF	47750	530190	2z6xv	tn087	1999	1:24000
Hawthorne-Rock outcrop complex, 40 to 80 percent slopes	HrF	21880	530214	2z6xx	tn087	1999	1:24000
Hawthorne gravelly silt loam, 5 to 20 percent slopes	HbD	10923	530189	2z6xy	tn087	1999	1:24000
Hawthorne gravelly silt loam, 15 to 50 percent slopes	HwF	30614	525836	2v646	tn103	1999	1:24000
Hawthorne gravelly silt loam, 5 to 15 percent slopes	HwC	10163	525835	2v647	tn103	1999	1:24000
Hawthorne gravelly silt loam, 20 to 60 percent slopes	HbF	45420	527703	2z6xv	tn111	1992	1:24000
Hawthorne gravelly silt loam, 5 to 20 percent slopes	HbD	19569	527702	2z6xy	tn111	1992	1:24000
Hawthorne and Dellrose association, 25 to 55 percent slopes	HWE	19893	524082	klbw	tn117	1999	1:24000
Hawthorne gravelly silt loam, 5 to 15 percent slopes	HtC	4593	524080	2v648	tn117	1999	1:24000
Hawthorne gravelly silt loam, 15 to 45 percent slopes	HtE	227	524081	2v5ck	tn117	1999	1:24000
Hawthorne-Bodine complex, 20 to 60 percent slopes	HbF	17077	625743	p048	tn127	2002	1:24000
Hawthorne-Sugargrove complex, 5 to 20 percent slopes	HsC	9672	625744	p049	tn127	2002	1:24000
Hawthorne gravelly silt loam, 20 to 60 percent slopes	HbF	5258	843327	2z6xv	tn133	2003	1:24000
Hawthorne-Rock outcrop complex, 40 to 80 percent slopes	HrF	2339	843328	2z6xx	tn133	2003	1:24000
Faywood-Hawthorne complex, 5 to 12 percent slopes	FhC	1528	843362	x9l7	tn133	2003	1:24000
Hawthorne gravelly silt loam, 5 to 20 percent slopes	HbD	831	843326	2z6xy	tn133	2003	1:24000
Hawthorne-Sugargrove complex, 5 to 20 percent slopes	HsD	582	843337	2z6xt	tn133	2003	1:24000
Biffle, Hawthorne, and Sulphura soils, very steep, rocky	BSF	64445	560604	ltc0	tn135	2000	1:24000
Hawthorne gravelly silt loam, 20 to 60 percent slopes	HbF	1173	528203	2z6xv	tn149	1974	1:15840
Hawthorne gravelly silt loam, 20 to 60 percent slopes	HbF	14963	529820	2z6xv	tn159	1992	1:24000
Hawthorne gravelly silt loam, 5 to 20 percent slopes	HbD	2085	529819	2z6xy	tn159	1992	1:24000
Hawthorne gravelly silt loam, 12 to 20 percent slopes	Nc	10808	2396942	2v59f	tn161	1953	1:20000
Hawthorne gravelly silt loam, 20 to 60 percent slopes	HbF	268	529863	2z6xv	tn177	1965	1:15840
Hawthorne gravelly silt loam, 20 to 60 percent slopes	HbF	1381	528464	2z6xv	tn189	1988	1:20000
Hawthorne gravelly silt loam, 5 to 20 percent slopes	HbD	335	528463	2z6xy	tn189	1988	1:20000
Hawthorne gravelly silt loam, 20 to 60 percent slopes	HbF	1566	528628	2z6xv	tn604	1974	1:20000
Hawthorne gravelly silt loam, 20 to 60 percent slopes	HbF	18748	2427408	2z6xv	tn610	1960	1:15840
Hawthorne-Sugargrove complex, 5 to 20 percent slopes	HsD	2090	2427407	2z6xt	tn610	1960	1:15840

Map of Series Extent

Approximate geographic distribution of the HAWTHORNE 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).