Soil Data Explorer - PERRY

Official Series Description

Lab Data Summary

Aggregate lab data for the PERRY soil series. This aggregation is based on all pedons with a current taxon name of PERRY, 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 PERRY 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
131B	85P0751	85LA021003	Perry	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	32.2402763,-92.0527802
131B	86P0923	86LA067002	Perry	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	32.8216667,-91.621109
131B	40A4399	S1960AR041001	Perry	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	33.7169456,-91.4477768
131B	40A4400	S1960AR041002	Perry	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	33.8402786,-91.2511139
131B	40A4105	S1972LA123003	PERRY	1	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	32.9399986,-91.4755554
134	40A4104	S1972LA123002	PERRY	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	33.0029373,-91.4165192

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the PERRY 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 PERRY 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 PERRY 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 PERRY 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 hills figure.

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

Competing Series

Soil series competing with PERRY 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 PERRY 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 PERRY 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 hills figure.

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

Soil series sharing subgroup-level classification with PERRY, 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. LA-2012-02-01-01 | Bossier Parish - August 1962

   Physiographic relationships of general soil areas in the northwestern part of Bossier Parish. The area represented is about 12 miles square (Soil Survey of Bossier Parish, Louisiana; August 1962).

2. LA-2012-02-01-03 | Richland Parish - September 1993

   Relationship of soils, landscape, and parent material in Richland Parish (Soil Survey of Richland Parish, Louisiana; September 1993).

3. LA-2012-04-27-09 | St. Mary Parish - March 1959

   Diagram showing elevations and soil materials of some of the soils and miscellaneous land types in St. Mary Parish (Soil Survey of St. Mary Parish, Louisiana; March 1959).

Map Units

Map units containing PERRY 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
Perry clay, 0 to 1 percent slopes, frequently flooded	18A	37259	579286	2rxg3	ar001	1995	1:24000
Perry clay, 0 to 1 percent slopes	17A	15183	579285	2ry5y	ar001	1995	1:24000
Perry clay, 0 to 1 percent slopes	19	43147	565068	2ry5y	ar003	1977	1:20000
Perry clay, 0 to 1 percent slopes	PeA	110401	565276	2ry5y	ar017	1964	1:20000
Perry clay, 1 to 3 percent slopes	PeU	2777	565277	2rxg8	ar017	1964	1:20000
Perry silt loam, 0 to 1 percent slopes	Pr	833	565278	2rxg9	ar017	1964	1:20000
Perry clay, 0 to 1 percent slopes	Pe	24156	564199	2ry5y	ar041	1968	1:20000
Perry silt loam, 0 to 1 percent slopes	Pc	326	564198	2rxg9	ar041	1968	1:20000
Perry clay, 0 to 1 percent slopes	Pe	34339	565465	2ry5y	ar043	1972	1:24000
Perry clay, 0 to 1 percent slopes, occasionally flooded, Arkansas River	24	9929	565500	2rxg5	ar045	1975	1:20000
Perry clay, 0 to 1 percent slopes, occasionally flooded	32	4474	565658	2tglb	ar057	1976	1:20000
Perry clay, occasionally flooded	25	5940	566097	m026	ar105	1980	1:20000
Perry clay, 0 to 1 percent slopes, rarely flooded	Pe	32940	566193	2rxgz	ar119	1972	1:20000
Rilla-Perry complex, undulating	RpB	3502	566199	m05h	ar119	1972	1:20000
Perry Urban land complex, 0 to 1 percent slopes	Pu	1890	566194	2rxh2	ar119	1972	1:20000
Perry clay, 0 to 1 percent slopes	26	143079	564847	2ry5y	ar660	1975	1:20000
Perry clay, 0 to 1 percent slopes, occasionally flooded, Arkansas River	27	20953	564848	2rxg5	ar660	1975	1:20000
Perry silty clay, 0 to 1 percent slopes	27	68414	564310	2rxgc	ar680	1980	1:20000
Perry silty clay, 0 to 1 percent slopes, frequently flooded	28	18853	564311	2rxgd	ar680	1980	1:20000
Perry clay, 0 to 1 percent slopes, occasionally flooded, Arkansas River	Pg	40987	1725658	2rxg5	la021	1985	1:24000
Perry silty clay loam	Pe	8214	1725656	1vxpb	la021	1985	1:24000
Perry-Hebert complex, gently undulating	Pk	7321	1725659	1vxpf	la021	1985	1:24000
Perry clay	Pf	2356	1725657	1vxpc	la021	1985	1:24000
Perry clay, 0 to 1 percent slopes, occasionally flooded, Arkansas River	Pd	9897	1722410	2rxg5	la025	1983	1:24000
Perry silty clay loam	Pa	5830	1722409	1vt9l	la025	1983	1:24000
Perry clay, frequently flooded	Pe	353	1722411	1vt9n	la025	1983	1:24000
Perry clay, 0 to 1 percent slopes, occasionally flooded	Pe	2060	1724552	2tglb	la031	1986	1:24000
Perry clay, frequently flooded	Pe	2739	1017147	134f6	la039	1970	1:24000
Gallion-Perry complex, gently undulating	Ga	4219	824185	wnmm	la045	1973	1:24000
Perry clay, 0 to 1 percent slopes	Pc	107028	569814	m3y3	la067	1981	1:24000
Perry clay, 0 to 1 percent slopes, occasionally flooded, Arkansas River	Pg	6935	569816	2rxg5	la067	1981	1:24000
Hebert and Perry soils, 0 to 1 percent slopes, frequently flooded	HY	5726	569797	2s1z0	la067	1981	1:24000
Perry clay, gently undulating	Pe	1579	569815	m3y4	la067	1981	1:24000
Perry clay, occasionally flooded	Pe	4348	1903122	21wc1	la069	1983	1:24000
Perry clay, 0 to 1 percent slopes, occasionally flooded, Arkansas River	Pe	48527	1725297	2rxg5	la073	1969	1:24000
Perry clay, frequently flooded	Pc	10601	1725296	1vx9q	la073	1969	1:24000
Hebert-Perry complex, gently undulating	HpB	636	1725288	1vx9g	la073	1969	1:24000
Perry clay	Pr	1862	1720680	1vrht	la081	1973	1:24000
Perry clay	Pd	32950	1714796	1vkd0	la083	1988	1:24000
Perry clay, 0 to 1 percent slopes, occasionally flooded, Arkansas River	Pe	13917	1714797	2rxg5	la083	1988	1:24000
Hebert-Perry complex, occasionally flooded	Hp	4083	1714787	1vkcq	la083	1988	1:24000
Perry silty clay loam	Pc	2628	1714795	1vkcz	la083	1988	1:24000
Gallion-Perry complex, gently undulating	Gp	5836	823535	wmyn	la097	1983	1:24000
Gallion-Perry complex, gently undulating	Gp	6233	824151	wnlj	la099	1974	1:24000
Perry clay, frequently flooded	PF	4929	1725356	1vxcn	la111	1992	1:24000
Hebert and Perry soils, 0 to 1 percent slopes, frequently flooded	HP	704	1725343	2s1z0	la111	1992	1:24000
Perry clay	16	4250	570373	m4j4	la123	1975	1:24000
Perry clay, 0 to 1 percent slopes, occasionally flooded	Pe	1058	1725971	2tglb	la127	1991	1:24000
Perry clay, 0 to 1 percent slopes, occasionally flooded	22	6855	575267	2tglb	tx037	1978	1:20000

Map of Series Extent

Approximate geographic distribution of the PERRY 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).