Soil Data Explorer - CLIFFORD

Official Series Description

Lab Data Summary

Aggregate lab data for the CLIFFORD soil series. This aggregation is based on all pedons with a current taxon name of CLIFFORD, 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 CLIFFORD 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
136	04N1092	04NC097026	Clifford	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	36.0350571,-80.9693069
136	00P0975	S2000NC097006	Clifford	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	35.7860489,-81.0008926
136	00P0981	S2000NC097012	Clifford	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	35.9213142,-80.9127502

Water Balance

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

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

Soil series sharing subgroup-level classification with CLIFFORD, 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. NC-2010-09-28-11 | Surry County - 2007

   Relationship of soils, landscape, and geology in the Fairview-Clifford general soil map unit (Soil Survey of Surry County, North Carolina; 2007).

2. VA-2010-11-05-09 | Culpeper County -

   Relationship of soils and landscape in the Piedmont Granite Gneiss (Soil Survey of Culpeper County, Virginia).

Map Units

Map units containing CLIFFORD 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
Clifford sandy clay loam, 2 to 8 percent slopes, moderately eroded	CeB2	14905	2390342	2sjdl	nc003	1988	1:24000
Clifford-Urban land complex, 2 to 8 percent slopes	CfB	1362	2390343	2l7bv	nc003	1988	1:24000
Clifford sandy loam, 2 to 6 percent slopes	CfB	18304	2431241	2mlx4	nc035	1969	1:15840
Clifford sandy loam, 6 to 10 percent slopes	CfC	16776	2431242	2mlx5	nc035	1969	1:15840
Clifford sandy loam, 10 to 15 percent slopes	CfD	4710	2431243	2mlx6	nc035	1969	1:15840
Clifford sandy clay loam, 6 to 10 percent slopes, moderately eroded	CgC2	3151	2431258	2tqd1	nc035	1969	1:15840
Clifford sandy clay loam, 2 to 6 percent slopes, moderately eroded	CgB2	578	2431257	2tqcz	nc035	1969	1:15840
Clifford sandy loam, 2 to 8 percent slopes	CrB	1344	2432814	2tqd2	nc057	1985	1:24000
Clifford sandy loam, 8 to 15 percent slopes	CrD	272	2432816	2tqd4	nc057	1985	1:24000
Clifford sandy clay loam, 2 to 8 percent slopes, moderately eroded	CsB2	20	2432820	2sjdl	nc057	1985	1:24000
Clifford-Urban land complex, 2 to 8 percent slopes	CuB	18	2432826	2mnk8	nc057	1985	1:24000
Clifford sandy clay loam, 8 to 15 percent slopes, moderately eroded	CsD2	10	2432821	2tqd0	nc057	1985	1:24000
Clifford sandy clay loam, 2 to 8 percent slopes, moderately eroded	CfB2	10492	2424559	2sjdl	nc059	1988	1:24000
Clifford sandy clay loam, 8 to 15 percent slopes, moderately eroded	CfC2	300	2679282	2tqd0	nc059	1988	1:24000
Clifford sandy loam, 2 to 6 percent slopes	ClB	20936	2433507	2mp87	nc067	1970	1:15840
Clifford sandy loam, 6 to 10 percent slopes	ClC	8605	2433512	2mp8d	nc067	1970	1:15840
Clifford sandy loam, 10 to 15 percent slopes	ClD	1900	2433480	2mp7c	nc067	1970	1:15840
Clifford clay loam, 6 to 10 percent slopes, moderately eroded	CmC2	1698	2433478	2mp79	nc067	1970	1:15840
Clifford clay loam, 2 to 6 percent slopes, moderately eroded	CmB2	983	2433477	2mp78	nc067	1970	1:15840
Clifford sandy loam, 2 to 6 percent slopes	CkB	19268	2433062	2mnsw	nc081	1975	1:20000
Clifford sandy clay loam, 2 to 6 percent slopes, moderately eroded	ClB2	10177	2433067	2tqcz	nc081	1975	1:20000
Clifford sandy loam, 6 to 10 percent slopes	CkC	5240	2433064	2mnsy	nc081	1975	1:20000
Clifford sandy clay loam, 6 to 10 percent slopes, moderately eroded	ClC2	4284	2433068	2tqd1	nc081	1975	1:20000
Clifford sandy loam, 10 to 15 percent slopes	CkD	1212	2433066	2mnt0	nc081	1975	1:20000
Clifford-Urban land complex, 2 to 10 percent slopes	CmB	714	2433070	2mnt4	nc081	1975	1:20000
Clifford sandy clay loam, 6 to 10 percent slopes, moderately eroded	CmC2	16589	2424519	2tqd1	nc097	2011	1:12000
Clifford sandy clay loam, 2 to 6 percent slopes, moderately eroded	CmB2	15833	2424517	2tqcz	nc097	2011	1:12000
Clifford-Urban land complex, 2 to 10 percent slopes	CrC	2011	2424480	2mcw1	nc097	2011	1:12000
Braddock-Clifford complex, 8 to 15 percent slopes	BnD	1828	2424761	2md53	nc097	2011	1:12000
Bentley-Clifford complex, 2 to 6 percent slopes	BeB	1076	2424681	2md2j	nc097	2011	1:12000
Clifford sandy loam, 6 to 10 percent slopes	CkC	938	2424518	2mcx8	nc097	2011	1:12000
Clifford sandy loam, 2 to 6 percent slopes	CkB	606	2424516	2mcx6	nc097	2011	1:12000
Clifford-Urban land complex, 10 to 25 percent slopes	CrE	67	2424482	2mcw3	nc097	2011	1:12000
Clifford sandy loam, 2 to 6 percent slopes	CmB	150	2439283	2mw8k	nc145	1987	1:24000
Clifford sandy loam, 6 to 10 percent slopes	CmC	45	2439282	2mw8j	nc145	1987	1:24000
Clifford sandy clay loam, 2 to 8 percent slopes, moderately eroded	CgB2	76548	2388995	2sjdl	nc157	1983	1:24000
Clifford-Urban land complex, 2 to 10 percent slopes	ChC	5196	2388996	2l5yd	nc157	1983	1:24000
Clifford sandy loam, 2 to 8 percent slopes	CfB	3102	2388994	2tqd2	nc157	1983	1:24000
Clifford sandy clay loam, 2 to 8 percent slopes, moderately eroded	CeB2	7724	2388444	2sjdl	nc169	1992	1:24000
Clifford sandy clay loam, 8 to 15 percent slopes, moderately eroded	CeC2	2208	2388446	2tqd0	nc169	1992	1:24000
Clifford fine sandy loam, 2 to 8 percent slopes	CcB	1845	2388440	2tqd5	nc169	1992	1:24000
Clifford sandy clay loam, 2 to 8 percent slopes, moderately eroded	CrB2	7588	1427583	2sjdl	nc171	2005	1:24000
Clifford sandy clay loam, 2 to 6 percent slopes, moderately eroded	CcB2	47411	2396720	2tqcz	nc197	1960	1:15840
Clifford sandy clay loam, 6 to 10 percent slopes, moderately eroded	CcC2	22879	2396723	2tqd1	nc197	1960	1:15840
Clifford fine sandy loam, 2 to 6 percent slopes	CaB	7836	2396719	2lfzj	nc197	1960	1:15840
Clifford fine sandy loam, 6 to 10 percent slopes	CaC	4719	2396721	2lfzl	nc197	1960	1:15840
Clifford gravelly fine sandy loam, 2 to 6 percent slopes, moderately eroded	CgB2	1857	2397955	2lh8d	nc197	1960	1:15840
Clifford gravelly fine sandy loam, 6 to 10 percent slopes, moderately eroded	CgC2	1798	2397963	2lh8n	nc197	1960	1:15840
Clifford clay loam, 2 to 6 percent slopes, severely eroded	CeB3	952	2396710	2lfz7	nc197	1960	1:15840
Clifford gravelly fine sandy loam, 2 to 6 percent slopes	CgB	558	2397953	2lh8b	nc197	1960	1:15840
Clifford gravelly fine sandy loam, 6 to 10 percent slopes	CgC	538	2397958	2lh8h	nc197	1960	1:15840
Clifford loam, 2 to 6 percent slopes, moderately eroded	CbB2	479	2397973	2lh8z	nc197	1960	1:15840
Clifford loam, 6 to 10 percent slopes	CbC	250	2397974	2lh90	nc197	1960	1:15840
Clifford loam, 7 to 15 percent slopes	5C	36695	136687	4l78	va009	2004	1:24000
Clifford loam, 15 to 25 percent slopes	5D	18133	136688	4l79	va009	2004	1:24000
Clifford loam, 2 to 7 percent slopes	5B	15417	136686	4l77	va009	2004	1:24000
Clifford loam, 25 to 50 percent slopes	5E	8425	136689	4l7b	va009	2004	1:24000
Clifford clay loam, 15 to 25 percent slopes, severely eroded	4D	5742	136684	4l75	va009	2004	1:24000
Clifford clay loam, 7 to 15 percent slopes, severely eroded	4C	4666	136683	4l74	va009	2004	1:24000
Clifford loam, 25 to 50 percent slopes, very stony	6E	2669	136693	4l7g	va009	2004	1:24000
Clifford clay loam, 25 to 50 percent slopes, severely eroded	4E	2438	136685	4l76	va009	2004	1:24000
Clifford loam, 15 to 25 percent slopes, very stony	6D	1663	136692	4l7f	va009	2004	1:24000
Clifford loam, 7 to 15 percent slopes, very stony	6C	760	136691	4l7d	va009	2004	1:24000
Clifford clay loam, 2 to 7 percent slopes, severely eroded	4B	431	136682	4l73	va009	2004	1:24000
Clifford loam, 2 to 7 percent slopes, very stony	6B	40	136690	4l7c	va009	2004	1:24000
Clifford fine sandy loam, 7 to 15 percent slopes	7C	54332	135994	2vy6s	va019	1985	1:24000
Clifford fine sandy loam, 2 to 7 percent slopes	7B	38424	135993	2xx5x	va019	1985	1:24000
Clifford fine sandy loam, 2 to 7 percent slopes	CeB	422	519183	2yztm	va035	1965	1:15840
Clifford fine sandy loam, 7 to 15 percent slopes	CeC	316	519185	2yztp	va035	1965	1:15840
Clifford fine sandy loam, 2 to 7 percent slopes, moderately eroded	CeB2	209	519184	2yztn	va035	1965	1:15840
Clifford fine sandy loam, 7 to 15 percent slopes, moderately eroded	CeC2	202	519186	2yztq	va035	1965	1:15840
Clifford loam, 7 to 15 percent slopes	8C	3178	1726191	1vy7l	va047	2006	1:24000
Clifford loam, 2 to 7 percent slopes	8B	2814	1726190	1vy7k	va047	2006	1:24000
Clifford sandy loam, 2 to 7 percent slopes	9B	2844	1587400	2tqd3	va049	2005	1:24000
Clifford clay loam, 7 to 15 percent slopes, severely eroded	11C	2250	1587402	1q8tj	va049	2005	1:24000
Clifford sandy loam, 7 to 15 percent slopes, very stony	10C	356	1587401	1q8th	va049	2005	1:24000
Clifford fine sandy loam, 8 to 15 percent slopes	7C	116337	581948	2vy5y	va067	2004	1:24000
Clifford fine sandy loam, 15 to 25 percent slopes	7D	71719	581949	mjkk	va067	2004	1:24000
Clifford-Hickoryknob complex, 25 to 45 percent slopes	8E	57611	581951	mjkm	va067	2004	1:24000
Clifford fine sandy loam, 2 to 8 percent slopes	7B	10608	581947	2tqd5	va067	2004	1:24000
Clifford-Urban land complex, 8 to 15 percent slopes	9C	832	581952	mjkn	va067	2004	1:24000
Clifford sandy loam, 2 to 8 percent slopes	8B	44186	1472795	2tqd2	va083	2004	1:24000
Clifford sandy loam, 8 to 15 percent slopes	8C	37993	1472796	2tqd4	va083	2004	1:24000
Clifford clay loam, 2 to 8 percent slopes, severely eroded	9B3	31798	1472798	1lfkm	va083	2004	1:24000
Clifford clay loam, 8 to 15 percent slopes, severely eroded	9C3	23314	1472799	1lfkn	va083	2004	1:24000
Clifford-Urban land complex, 2 to 8 percent slopes	10B	1117	1472797	1lfkl	va083	2004	1:24000
Clifford-Urban land complex, 8 to 20 percent slopes	10D	350	1472800	1lfkp	va083	2004	1:24000
Clifford sandy loam, 7 to 15 percent slopes	4C	51655	122388	30ymd	va089	1995	1:24000
Clifford sandy loam, 15 to 25 percent slopes	4D	35783	122389	30ymb	va089	1995	1:24000
Clifford sandy loam, 25 to 45 percent slopes	4E	34914	122390	30ymc	va089	1995	1:24000
Woolwine-Clifford complex, 25 to 45 percent slopes	21E	32318	122347	439p	va089	1995	1:24000
Woolwine-Clifford complex, 7 to 15 percent slopes	21C	21761	122343	439k	va089	1995	1:24000
Woolwine-Clifford complex, 15 to 25 percent slopes	21D	18019	122345	439m	va089	1995	1:24000
Clifford sandy loam, 2 to 7 percent slopes	4B	3521	122387	2tqd3	va089	1995	1:24000
Woolwine-Clifford complex, 2 to 7 percent slopes	21B	389	122341	439h	va089	1995	1:24000
Clifford fine sandy loam, 2 to 7 percent slopes, moderately eroded	CeB2	814	119804	2z1wb	va137	1966	1:15840
Clifford loam, 2 to 7 percent slopes, moderately eroded	CmB2	640	119806	2z1wd	va137	1966	1:15840
Clifford fine sandy loam, 7 to 15 percent slopes, moderately eroded	CeC2	357	119805	2z1wc	va137	1966	1:15840
Clifford clay loam, 4 to 15 percent slopes, severely eroded	CsC3	266	119808	2z1wg	va137	1966	1:15840
Clifford loam, 7 to 15 percent slopes, moderately eroded	CmC2	255	119807	2z1wf	va137	1966	1:15840
Clifford sandy clay loam, 2 to 8 percent slopes, moderately eroded	8B2	1418	1474036	2sjdl	va141	2008	1:24000
Clifford sandy clay loam, 8 to 15 percent slopes, moderately eroded	8C2	400	1474037	2tqd0	va141	2008	1:24000
Clifford sandy clay loam, 7 to 15 percent slopes, severely eroded	5C3	86511	120159	2yzrj	va143	1989	1:24000
Clifford sandy clay loam, 2 to 7 percent slopes, severely eroded	5B3	75074	120158	2yzrh	va143	1989	1:24000
Clifford sandy loam, 2 to 7 percent slopes	4B	39161	120015	2tqd3	va143	1989	1:24000
Clifford sandy loam, 7 to 15 percent slopes	4C	24213	120016	2yzrg	va143	1989	1:24000
Clifford-Urban land complex, 2 to 7 percent slopes	6B	3489	120160	2yzrk	va143	1989	1:24000
Clifford-Urban land complex, 7 to 20 percent slopes	6C	2419	120161	2yzrl	va143	1989	1:24000
Clifford fine sandy loam, 2 to 7 percent slopes	50B	792	2373805	2kp4c	va515	2008	1:24000
Clifford-Urban land complex, 2 to 7 percent slopes	51B	434	2373817	2kp4r	va515	2008	1:24000
Clifford fine sandy loam, 7 to 15 percent slopes	50C	383	2373806	2vy6s	va515	2008	1:24000
Clifford-Urban land complex, 7 to 20 percent slopes	51C	170	2373818	2kp4s	va515	2008	1:24000

Map of Series Extent

Approximate geographic distribution of the CLIFFORD 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).