Soil Data Explorer - CARLISLE

Official Series Description

Lab Data Summary

Aggregate lab data for the CARLISLE soil series. This aggregation is based on all pedons with a current taxon name of CARLISLE, 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 CARLISLE 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
140	88PA081062	1988PA081062	Carlisle	1	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	41.5791667,-76.8286111
140	88PA081074	1988PA081074	Carlisle	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	41.4494444,-76.8386111
140	90P0654	90NY077004	Carlisle	n/a	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	42.5763893,-75.0108337
140	90P0656	90NY077006	Carlisle	1	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	42.5216675,-75.3305588
144A	84P0764	S1984NY071001	Carlisle	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	41.3367609,-74.4565462
144A	84P0765	S1984NY071002	Carlisle	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	41.3375943,-74.4551573
144A	84P0768	S1984NY071005	Carlisle	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	41.3370387,-74.4554351
144A	84P0769	S1984NY071006	Carlisle	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	41.3370387,-74.4559906
n/a	CO-120	1959-OH029-120	Carlisle	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	SK-016	1964-OH151-016	Carlisle	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	LG-028	1971-OH091-028	Carlisle	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	CR-031	1973-OH033-031	Carlisle	3	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 CARLISLE 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 CARLISLE 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 CARLISLE 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 CARLISLE 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).

Competing Series

Soil series competing with CARLISLE 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 CARLISLE 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 CARLISLE 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.

Soil series sharing subgroup-level classification with CARLISLE, 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. CT-2011-05-31-05 | Fairfield County - 1981

   Typical pattern of soils and parent material in the Carlisle-Adrian-Saco map unit (Soil Survey of Fairfield County, Conneticut; 1981).

2. CT-2011-05-31-06 | New London County - 1983

   Typical pattern soils in the Charlton-Canton-Hollis general soil map unit (Soil Survey of New London County, Conneticut; 1983).

3. IN-2012-01-19-15 | Elkhart County - April 1974

   Relationship of soils to topography and underlying materials in the Riddles-Crosby-Miami association (Soil Survey of Elkhart County, Indiana; 1974).

4. IN-2012-01-19-35 | Lake County - July 1972

   Oakville-Tawas, Plainfield-Watseka, Maumee-Bono-Warners, and Alida-Del Rey-Whitaker soil associations. The Oakville-Tawas association is on the left (Soil Survey of Lake County, Indiana; 1972).

5. IN-2012-01-19-43 | Pulaski County - January 1968

   Topographical relationships between the soils on sand ridges, in depressional outwash areas, and in organic deposits (Soil Survey of Pulaski County, Indiana; 1968).

6. MA-2012-02-01-05 | Berkshire County - February 1988

   Typical pattern of soils and parent material in the Tunbridge-Lyman-Peru general soil map unit (Soil Survey of Berkshire County, Massachusetts; February 1988).

7. NY-2012-02-15-40 | Rockland County - October 1990

   Relationship between soils, landscape position, and parent materials in Rockland County (Soil Survey of Rockland County, New York; October 1990).

8. OH-2012-02-16-27 | Defiance County - July 1984

   Typical pattern of soils in the Blount-Glynwood-Pewamo Association (Soil Survey of Defiance County, Ohio; July 1984).

Map Units

Map units containing CARLISLE 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
Carlisle muck, 0 to 2 percent slopes	CarabA	1734	3332505	2zdk5	mi035	1977	1:15840
Carlisle muck, 0 to 2 percent slopes	CarabA	302	3332506	2zdk5	mi037	1974	1:15840
Carlisle muck, 0 to 2 percent slopes	CarabA	5011	3332517	2zdk5	mi049	1967	1:20000
Carlisle and Linwood mucks	Cd	4710	186833	68dw	mi049	1967	1:20000
Carlisle muck, 0 to 2 percent slopes	CarabA	95	3332525	2zdk5	mi051	1966	1:15840
Carlisle muck, lake moderated snowy, 0 to 2 percent slopes	CaraeA	10003	3332532	30n5c	mi055	1963	1:15840
Carlisle muck, 0 to 2 percent slopes	CarabA	136	2437765	2zdk5	mi065	1977	1:15840
Carlisle muck, 0 to 2 percent slopes	CarabA	10819	187913	2zdk5	mi067	1965	1:15840
Carlisle muck, 0 to 2 percent slopes	CarabA	16914	3332575	2zdk5	mi087	1966	1:15840
Carlisle muck, disintegration moraine, 0 to 2 percent slopes	CaracA	4785	3332581	2zdl1	mi091	1957	1:20000
Carlisle muck, 0 to 2 percent slopes	CarabA	2019	3332579	2zdk5	mi091	1957	1:20000
Carlisle muck, 0 to 2 percent slopes	CarabA	33998	3332584	2zdk5	mi093	1968	1:20000
Carlisle and Linwood mucks	Cd	16	2423818	2mc5p	mi093	1968	1:20000
Kerston-Carlisle-Glendora complex, frequently flooded	9	7775	192612	6gf9	mi105	1992	1:15840
Carlisle muck, 0 to 2 percent slopes	CarabA	32824	3332611	2zdk5	mi117	1956	1:20000
Carlisle muck, lake moderated cool, 0 to 2 percent slopes	CaraaA	168	3332608	2zdl0	mi117	1956	1:20000
Tawas and Carlisle mucks	Tc	5809	187383	68zm	mi121	1966	1:15840
Carlisle muck, lake moderated cool, 0 to 2 percent slopes	CaraaA	6465	3332616	2zdl0	mi123	1990	1:15840
Carlisle muck, lake moderated, 0 to 2 percent slopes	CaradA	1425	3332619	2zdkz	mi123	1990	1:15840
Carlisle muck, 0 to 2 percent slopes	CarabA	305	3332621	2zdk5	mi123	1990	1:15840
Carlisle muck, 0 to 2 percent slopes	CarabA	384	3332628	2zdk5	mi125	1980	1:15840
Carlisle and Linwood mucks	104	48	2423661	2mc0m	mi125	1980	1:15840
Houghton and Carlisle soils	71	8215	189079	6brb	mi127	1992	1:15840
Kerston and Carlisle mucks, frequently flooded	97	3977	189098	6bry	mi127	1992	1:15840
Carlisle muck, lake moderated, 0 to 2 percent slopes	CaradA	4273	3332636	2zdkz	mi139	1967	1:15840
Carlisle muck, 0 to 2 percent slopes	CarabA	22	3332642	2zdk5	mi147	1969	1:20000
Carlisle and Linwood mucks, 0 to 2 percent slopes	CdA0	6641	188242	69wb	mi151	1955	1:15840
Carlisle muck, 0 to 2 percent slopes	CcA0	996	188241	69w9	mi151	1955	1:15840
Carlisle muck, 0 to 2 percent slopes	CarabA	7	3332646	2zdk5	mi151	1955	1:15840
Carlisle muck, 0 to 2 percent slopes	CarabA	13266	3332650	2zdk5	mi155	1967	1:12000
Carlisle and Linwood mucks	Cd	30	2424375	2mcrn	mi155	1967	1:12000
Carlisle muck	101	115	2396655	2lfxg	mi157	1984	1:15840
Carlisle and Linwood mucks, 0 to 2 percent slopes	122A	21	2508120	69wb	mi157	1984	1:15840
Carlisle muck, 0 to 2 percent slopes	119A	14	2508117	69w9	mi157	1984	1:15840
Carlisle muck, disintegration moraine, 0 to 2 percent slopes	CaracA	5	3332669	2zdl1	mi161	1974	1:20000
Carlisle muck, lake moderated cool, 0 to 2 percent slopes	CaraaA	2449	3332673	2zdl0	mi600	1983	1:15840
Carlisle-Adrian mucks, 0 to 2 percent slopes, frequently flooded	CarbAt	7	1395407	1hv14	nj023	1985	1:24000
Carlisle muck	Ca	662	288702	9pdz	ny001	1985	1:15840
Carlisle muck	92	914	289744	9qhl	ny009	2002	1:24000
Carlisle muck	Ce	1702	289788	9qk0	ny013	1988	1:15840
Carlisle muck	Cc	1717	289978	9qr4	ny017	1982	1:15840
Carlisle and Palms soils	Ce	283	290592	9rcy	ny025	1999	1:24000
Carlisle muck	CcA	3361	633022	p7q2	ny037	2004	1:24000
Carlisle muck	Cc	862	291612	9sfv	ny039	1985	1:24000
Carlisle muck	Cm	3277	2518306	9sw6	ny043	2018	1:24000
Carlisle muck	Cd	5568	291792	9smn	ny045	1981	1:15840
Carlisle-Palms complex, 0 to 2 percent slopes	92A	2276	3105719	2y9wq	ny051	2019	1:24000
Carlisle muck	Ce	2940	292532	9tdj	ny053	1975	1:15840
Carlisle muck	Ca	487	292802	9tp7	ny057	1973	1:24000
Carlisle muck	95	3610	293507	9vdz	ny065	1993	1:24000
Carlisle muck, drained	295	550	293396	9v9d	ny065	1993	1:24000
Carlisle muck	Ce	9791	293543	9vg4	ny067	1973	1:20000
Carlisle muck, 0 to 3 percent slopes	92A	3310	2378531	2kv1t	ny069	2012	1:12000
Carlisle muck	Cb	842	294007	9vy3	ny073	1973	1:15840
Carlisle muck	Ce	15420	294102	9w15	ny075	1973	1:15840
Carlisle muck	Ce	1019	294186	9w3w	ny077	1993	1:24000
Carlisle muck	Ca	400	309555	bd3n	ny093	1973	1:15840
Carlisle muck	Cc	687	294591	9wjy	ny097	1976	1:15840
Carlisle muck	Cc	2598	294795	9wrj	ny101	1972	1:15840
Carlisle muck	Ca	3248	295053	9x0v	ny105	1984	1:15840
Carlisle, Palms, and Alden soils, ponded	Ce	2319	295054	9x0w	ny105	1984	1:15840
Carlisle muck	Cd	12152	295708	9xpz	ny117	1972	1:15840
Carlisle muck, 0 to 3 percent slopes	92A	2209	3250296	2kv1t	ny123	1948	1:12000
Carlisle muck	Cf	607	288144	9ntz	oh005	1976	1:15840
Carlisle muck, 0 to 1 percent slopes	CgA	263	298871	b100	oh007	2001	1:12000
Carlisle silty clay loam	Ca	105	169675	5pkd	oh011	1979	1:15840
Carlisle muck, Central Ohio clayey till plain, drained, 0 to 2 percent slopes	Cb	3	1146232	2t6mk	oh011	1979	1:15840
Carlisle muck	Ca	2593	171421	5rcq	oh021	1966	1:15840
Carlisle muck, undrained	Cb	509	171695	5rnk	oh023	1997	1:15840
Carlisle muck, drained	Ca	125	171694	5rnj	oh023	1997	1:15840
Carlisle muck, 0 to 1 percent slopes	CeA	301	298745	b0vy	oh029	2005	1:12000
Carlisle muck, Central Ohio clayey till plain, drained, 0 to 2 percent slopes	Ck	96	168551	2t6mk	oh033	1975	1:15840
Carlisle silty clay loam	Cg	164	287285	9my8	oh035	1978	1:15840
Carlisle muck	Ca	378	168491	5nb6	oh037	1984	1:15840
Carlisle muck, disintegration moraine, drained, 0 to 2 percent slopes	Ca	684	168435	2t6mp	oh039	1981	1:15840
Carlisle muck, Central Ohio clayey till plain, drained, 0 to 2 percent slopes	Cb	216	172231	2t6mk	oh045	1998	1:12000
Carlisle muck	Cc	200	167882	5mpk	oh049	1977	1:15840
Carlisle muck, ponded	Cf	2170	287534	9n69	oh055	1979	1:15840
Carlisle muck, Central Ohio clayey till plain, drained, 0 to 2 percent slopes	Ca	933	168926	2t6mk	oh065	1987	1:15840
Carlisle muck	Ce	620	286880	9mj6	oh075	1989	1:15840
Carlisle muck, Central Ohio clayey till plain, drained, 0 to 2 percent slopes	Ce	1318	167964	2t6mk	oh077	1988	1:15840
Carlisle muck, Central Ohio clayey till plain, 0 to 2 percent slopes	Cf	944	167965	2t6mf	oh077	1988	1:15840
Carlisle muck	Cg	818	286790	9mf9	oh085	1976	1:15840
Carlisle muck	Ca	280	171004	5qy8	oh089	1986	1:15840
Carlisle muck, Central Ohio clayey till plain, drained, 0 to 2 percent slopes	Ca	2575	171098	2t6mk	oh091	1977	1:15840
Carlisle muck, Central Ohio clayey till plain, 0 to 2 percent slopes	Cc	495	171099	2t6mf	oh091	1977	1:15840
Carlisle mucky silt loam	Cg	446	287742	9nf0	oh093	1972	1:15840
Carlisle muck	Ca	160	169889	5ps9	oh097	1978	1:15840
Carlisle muck	Ch	578	816734	wdw8	oh099	1966	1:15840
Carlisle muck, Central Ohio clayey till plain, 0 to 2 percent slopes	Cb	10	1400468	2t6mf	oh101	1984	1:15840
Carlisle muck	Ch	1645	288324	9p0s	oh103	1974	1:15840
Carlisle muck, Central Ohio clayey till plain, drained, 0 to 2 percent slopes	Ca	73	169923	2t6mk	oh107	1975	1:15840
Carlisle muck	Ca	50	170231	5q4b	oh113	1969	1:15840
Carlisle muck, Central Ohio clayey till plain, 0 to 2 percent slopes	Cb	321	170344	2t6mf	oh117	1986	1:15840
Carlisle muck	Cf	183	171240	5r5w	oh129	1977	1:15840
Carlisle muck	Cg	6359	288416	9p3r	oh133	1973	1:15840
Carlisle muck, ponded	Cr	20	1717814	1vnjc	oh133	1973	1:15840
Carlisle muck, Central Ohio clayey till plain, drained, 0 to 2 percent slopes	Ck	1412	170739	2t6mk	oh139	1971	1:15840
Carlisle muck	Cd	174	170846	5qs5	oh141	1997	1:15840
Carlisle muck, Central Ohio clayey till plain, 0 to 2 percent slopes	Ca	365	169969	2t6mf	oh147	1978	1:15840
Carlisle muck, Central Ohio clayey till plain, drained, 0 to 2 percent slopes	Ca	137	170025	2t6mk	oh149	1977	1:15840
Carlisle muck	Ch	5745	287965	9nn6	oh151	1967	1:15840
Carlisle muck	Cg	6396	825310	wpsx	oh153	1969	1:20000
Carlisle muck, ponded	Ch	1030	287005	9mn7	oh155	1986	1:15840
Carlisle muck	Ch	2344	287177	9mts	oh169	1981	1:15840
Carlisle muck, ponded	Ck	766	287178	9mtt	oh169	1981	1:15840
Carlisle muck, disintegration moraine, drained, 0 to 2 percent slopes	Ca	5479	168136	2t6mp	oh171	1975	1:15840
Carlisle muck, Central Ohio clayey till plain, drained, 0 to 2 percent slopes	Ck	352	169602	2t6mk	oh175	1980	1:15840
Carlisle muck	CA	650	538258	l235	pa027	1975	1:20000
Carlisle muck	CM	9187	296159	9y5j	pa039	1973	1:20000
Carlisle muck	Cm	1592	2633035	2rg6b	pa049	2012	1:12000
Muck and Peat	Mp	1929	296246	9y8b	pa085	1967	1:20000
Carlisle silt loam	Ca	802	297103	9z4z	pa117	1973	1:20000
Carlisle mucky peat, 0 to 2 percent slopes	24A	1755	281424	9fv6	vt003	1992	1:20000
Cabot-Carlisle association, undulating, very stony	403B	227	281474	9fwt	vt003	1992	1:20000
Carlisle muck	Ce	6323	281780	9g6p	vt011	1976	1:20000
Carlisle muck	CaA	3498	279243	9ckv	vt013	1956	1:20000

Map of Series Extent

Approximate geographic distribution of the CARLISLE 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).