Soil Data Explorer - PICKWICK

Official Series Description

Lab Data Summary

Aggregate lab data for the PICKWICK soil series. This aggregation is based on all pedons with a current taxon name of PICKWICK, 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 PICKWICK were used in the calculation. Source: KSSL snapshot (updated 2020-03-13). 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
122	92P0162	1991TN081001	Pickwick	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	35.7900009,-87.3669434
122	92P0165	1991TN081004	PICKWICK	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	35.8002777,-87.3550034
133A	40A5015	S1959TN071001	Pickwick	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	35.2536125,-88.2241669
133A	40A5016	S1959TN071006	Pickwick	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	35.1966667,-88.2330551
n/a	71KY-093-006	71KY-093-006	Pickwick	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	79KY-213-002	79KY-213-002	Pickwick	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a

Water Balance

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

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

Competing Series

Soil series competing with PICKWICK 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 PICKWICK 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 PICKWICK 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 terrace figure.

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

Soil series sharing subgroup-level classification with PICKWICK, 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-2012-02-17-45 | Sequoyah County - June 1970

   Typical pattern of soils in associations 1, 2, and 5 (Soil Survey of Sequoyah County, Oklahoma; June 1970).

2. OK-2012-02-17-47 | Sequoyah County - June 1970

   Typical pattern of soils in associations 2 and 4 (Soil Survey of Sequoyah County, Oklahoma; June 1970).

3. TN-2010-11-02-09 | Hickman County - 2008

   Typical pattern of soils and parent material in the Sengtown-Mountview-Dickson and Sengtown general soil map units (Soil Survey of Hickman County, Tennessee; 2008).

4. TN-2010-11-02-12 | Hickman County - 2008

   Typical pattern of soils and parent material in the Pickwick-Armour-Arrington general soil map unit (Soil Survey of Hickman County, Tennessee; 2008).

5. TN-2010-11-02-15 | Lewis County - 2006

   Typical pattern of soils and parent material in the Pickwick-Paden-Riverby-Trace general soil map unit (Soil Survey of Lewis County, Tennessee; 2006).

6. TN-2012-03-19-04 | Hardin County - June 1963

   Major soil series in associations 3 and 6 and their relationship to the landscape (Soil Survey of Hardin County, TN; 1963).

Map Units

Map units containing PICKWICK 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
Pickwick silt loam, 1 to 3 percent slopes	25	1173	565501	lzfz	ar045	1975	1:20000
Pickwick silt loam, 3 to 8 percent slopes, eroded	26	468	565502	lzg0	ar045	1975	1:20000
Pickwick silt loam, 3 to 8 percent slopes, eroded	PsC2	8124	565585	lzjp	ar047	1967	1:20000
Pickwick silt loam, 1 to 3 percent slopes, eroded	PsB2	5339	565584	lzjn	ar047	1967	1:20000
Pickwick silt loam, 3 to 8 percent slopes	PcC	10409	565866	lztr	ar071	1973	1:24000
Pickwick silt loam, 1 to 3 percent slopes	PcB	6302	565865	lztq	ar071	1973	1:24000
Pickwick silt loam, 3 to 8 percent slopes	38	5883	566144	m03q	ar115	1978	1:20000
Pickwick silt loam, 1 to 3 percent slopes	37	1200	566143	m03p	ar115	1978	1:20000
Pickwick silt loam, 3 to 8 percent slopes, eroded	PsC2	16760	566612	m0lt	ar143	1966	1:20000
Pickwick silt loam, 1 to 3 percent slopes	PsB	2354	566611	m0ls	ar143	1966	1:20000
Pickwick gravelly loam, 3 to 8 percent slopes, eroded	PkC2	1053	566609	m0lq	ar143	1966	1:20000
Pickwick gravelly loam, 8 to 12 percent slopes, eroded	PkD2	603	566610	m0lr	ar143	1966	1:20000
Pickwick silt loam, 3 to 8 percent slopes	43	8693	565003	lyxx	ar149	1985	1:20000
Pickwick silt loam, 1 to 3 percent slopes	42	4626	565002	lyxw	ar149	1985	1:20000
Pickwick silt loam, 2 to 6 percent slopes	PkB	5122	548731	lf00	ky141	1972	1:20000
Pickwick silt loam, 6 to 12 percent slopes	PkC	4930	548732	lf01	ky141	1972	1:20000
Pickwick silty clay loam, 6 to 12 percent slopes, severely eroded	PlC3	920	548733	lf02	ky141	1972	1:20000
Pickwick silt loam, eroded rolling phase	Pg	1766	327336	bzm7	tn039	2008	1:24000
Pickwick silty clay loam, severely eroded rolling phase	Po	1711	327342	bzmf	tn039	2008	1:24000
Pickwick silt loam, eroded undulating phase	Ph	1198	327337	bzm8	tn039	2008	1:24000
Pickwick silt loam, hilly phase	Pk	986	327338	bzm9	tn039	2008	1:24000
Pickwick silt loam, rolling phase	Pl	686	327339	bzmb	tn039	2008	1:24000
Pickwick silty clay loam, severely eroded hilly phase	Pn	521	327341	bzmd	tn039	2008	1:24000
Pickwick silt loam, undulating phase	Pm	336	327340	bzmc	tn039	2008	1:24000
Pickwick silt loam, eroded hilly phase	Pf	195	327335	bzm6	tn039	2008	1:24000
Pickwick silt loam, 2 to 5 percent slopes	PcB	3143	527357	kprj	tn055	1965	1:15840
Pickwick silt loam, 5 to 12 percent slopes, eroded	PcC2	713	527358	kprk	tn055	1965	1:15840
Pickwick silt loam, 5 to 12 percent slopes, severely eroded	PcC3	241	527359	kprl	tn055	1965	1:15840
Pickwick silty clay loam, 5 to 8 percent slopes, severely eroded	PwC3	5923	327613	bzx5	tn071	1961	1:15840
Pickwick silt loam, 5 to 8 percent slopes	PkC	5063	327608	bzx0	tn071	1961	1:15840
Pickwick silty clay loam, 2 to 5 percent slopes, severely eroded	PwB3	4516	327612	bzx4	tn071	1961	1:15840
Pickwick silt loam, 2 to 5 percent slopes	PkB	3252	327606	2sr8p	tn071	1961	1:15840
Pickwick silt loam, 2 to 5 percent slopes, eroded	PkB2	2777	327607	bzwz	tn071	1961	1:15840
Pickwick silty clay loam, 8 to 12 percent slopes, severely eroded	PwD3	2001	327614	bzx6	tn071	1961	1:15840
Pickwick silt loam, 8 to 12 percent slopes	PkD	1574	327610	bzx2	tn071	1961	1:15840
Pickwick silt loam, 5 to 8 percent slopes, eroded	PkC2	1494	327609	bzx1	tn071	1961	1:15840
Pickwick silt loam, 12 to 25 percent slopes	PkE	1173	327611	bzx3	tn071	1961	1:15840
Pickwick-Gullied land complex	Px	1072	327616	bzx8	tn071	1961	1:15840
Pickwick silty clay loam, 12 to 25 percent slopes, severely eroded	PwE3	574	327615	bzx7	tn071	1961	1:15840
Pickwick silt loam, 5 to 12 percent slopes, eroded	PkC2	5411	527482	kpwk	tn081	1997	1:24000
Pickwick silt loam, 2 to 5 percent slopes	PkB	4527	527481	kpwj	tn081	1997	1:24000
Pickwick silty clay loam, 5 to 12 percent slopes, severely eroded	PkC3	3843	527483	kpwl	tn081	1997	1:24000
Pickwick silt loam, eroded rolling phase	Pf	1326	527548	kpyp	tn083	1952	1:20000
Pickwick silt loam, eroded undulating phase	Pe	735	527547	kpyn	tn083	1952	1:20000
Pickwick silt loam, undulating phase	Pd	145	527546	kpym	tn083	1952	1:20000
Talbott-Pickwick silt loam, eroded rolling phase	Tb	124	527552	kpyt	tn083	1952	1:20000
Pickwick silt loam, 5 to 12 percent slopes, eroded	PkC2	636	530876	ktf1	tn101	1999	1:24000
Pickwick silt loam, 2 to 5 percent slopes	PkB	148	530875	ktf0	tn101	1999	1:24000
Pickwick silty clay loam, 5 to 12 percent slopes, severely eroded	PkC3	141	530877	ktf2	tn101	1999	1:24000
Pickwick silty clay loam, 5 to 12 percent slopes, severely eroded	PkC3	1317	327973	c08s	tn109	1994	1:20000
Pickwick silt loam, 2 to 5 percent slopes	PkB	566	327972	c08r	tn109	1994	1:20000
Pickwick silt loam, 5 to 12 percent slopes, eroded	PkC2	8046	527999	kqf7	tn125	1972	1:15840
Pickwick silt loam, 5 to 12 percent slopes	PkC	7463	527998	kqf6	tn125	1972	1:15840
Pickwick silt loam, 2 to 5 percent slopes	PkB	4099	527997	kqf5	tn125	1972	1:15840
Pickwick silt loam, 12 to 20 percent slopes	PkD	981	528000	kqf8	tn125	1972	1:15840
Pickwick silt loam, 5 to 12 percent slopes, severely eroded	PkC3	1203	560641	ltd6	tn135	2000	1:24000
Pickwick silt loam, 5 to 12 percent slopes, eroded	PkC2	760	560640	ltd5	tn135	2000	1:24000
Pickwick silt loam, 2 to 5 percent slopes, eroded	PkB2	319	560639	ltd4	tn135	2000	1:24000
Pickwick silty clay loam, 5 to 12 percent slopes, severely eroded	PkC3	7461	528188	kqmb	tn147	1965	1:15840
Pickwick silt loam, 5 to 12 percent slopes	PkC	1413	328034	c0br	tn181	1996	1:24000
Pickwick silt loam, 2 to 5 percent slopes	PkB	746	328033	2sr8p	tn181	1996	1:24000
Pickwick silty clay loam, 5 to 12 percent slopes, severely eroded	PkC3	497	328035	c0bs	tn181	1996	1:24000
Pickwick silt loam, 12 to 20 percent slopes	PkD	214	328036	c0bt	tn181	1996	1:24000
Pickwick silty clay loam, 12 to 20 percent slopes, severely eroded	PkD3	210	328037	c0bv	tn181	1996	1:24000

Map of Series Extent

Approximate geographic distribution of the PICKWICK 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).