Soil Data Explorer - CHANDLER

Official Series Description

Lab Data Summary

Aggregate lab data for the CHANDLER soil series. This aggregation is based on all pedons with a current taxon name of CHANDLER, 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 CHANDLER 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
130B	91P0216	90NC121003	Chandler	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	35.9474983,-82.0583344
n/a	00P0688	S2000NC021009	Chandler	6	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 CHANDLER 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 CHANDLER 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 CHANDLER 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 CHANDLER 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 CHANDLER 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 CHANDLER 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 CHANDLER 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 CHANDLER, 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-2012-02-07-21 | Jackson County - June 1997

   Relationship of soils, aspect, and parent material in the Chandler-Fannin-Cashiers general soil map unit (Soil Survey of Jackson County, North Carolina; June 1997).

Map Units

Map units containing CHANDLER 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
Chandler loam, 25 to 60 percent slopes	CCF	575	124461	45hw	ga137	1960	1:20000
Chandler loam, 60 to 95 percent slopes	CCG	185	124462	45hx	ga137	1960	1:20000
Chandler loam, 15 to 25 percent slopes	CCE	120	124460	45hv	ga137	1960	1:20000
Chandler and Rock land, 60 to 90 percent slopes	CrG	8305	125254	46bg	ga605	1967	1:15840
Chandler complex, 25 to 75 percent slopes	CsF	5905	125255	46bh	ga605	1967	1:15840
Chandler loam, 25 to 60 percent slopes	CCF	645	125648	46r5	ga632	1967	1:15840
Chandler silt loam, 25 to 45 percent slopes	CaF	7241	545895	lb1j	nc005	1967	1:15840
Chandler stony silt loam, 45 to 65 percent slopes	CdG	3355	545897	lb1l	nc005	1967	1:15840
Chandler stony silt loam, 25 to 45 percent slopes	CdF	856	545896	lb1k	nc005	1967	1:15840
Chandler silt loam, 10 to 25 percent slopes	CaE	841	545894	lb1h	nc005	1967	1:15840
Chandler loam, 25 to 65 percent slopes	CaF	10360	545942	lb31	nc009	1982	1:24000
Chandler-Micaville complex, 30 to 50 percent slopes, stony	CeE	4476	548046	ld8x	nc011	1997	1:12000
Chandler-Micaville complex, 50 to 95 percent slopes, stony	CeF	131	548047	ld8y	nc011	1997	1:12000
Chandler-Micaville complex, 15 to 30 percent slopes, stony	CeD	69	548045	ld8w	nc011	1997	1:12000
Chandler stony loam, 45 to 70 percent slopes	CaG	403	546845	lc15	nc089	1974	1:20000
Chandler gravelly fine sandy loam, 30 to 50 percent slopes	CdE	8624	547037	lc7c	nc099	1991	1:12000
Chandler gravelly fine sandy loam, 15 to 30 percent slopes	CdD	4250	547036	lc7b	nc099	1991	1:12000
Chandler gravelly fine sandy loam, 50 to 95 percent slopes	CdF	2987	547038	lc7d	nc099	1991	1:12000
Chandler gravelly fine sandy loam, 15 to 30 percent slopes, windswept	CeD	1839	547040	lc7g	nc099	1991	1:12000
Chandler gravelly fine sandy loam, 8 to 15 percent slopes	CdC	1004	547035	lc79	nc099	1991	1:12000
Chandler gravelly fine sandy loam, 30 to 50 percent slopes, windswept	CeE	751	547041	lc7h	nc099	1991	1:12000
Chandler gravelly fine sandy loam, 8 to 15 percent slopes, windswept	CeC	310	547039	lc7f	nc099	1991	1:12000
Chandler gravelly fine sandy loam, 50 to 95 percent slopes, windswept	CeF	96	547042	lc7j	nc099	1991	1:12000
Chandler gravelly fine sandy loam, 30 to 50 percent slopes	CdE	4157	545806	l9yn	nc113	1990	1:12000
Chandler gravelly fine sandy loam, 50 to 95 percent slopes	CdF	2115	545807	l9yp	nc113	1990	1:12000
Chandler gravelly fine sandy loam, 15 to 30 percent slopes	CdD	1141	545805	l9ym	nc113	1990	1:12000
Chandler-Micaville complex, 30 to 50 percent slopes, stony	CeE	2940	547550	lcrx	nc121	1997	1:12000
Chandler-Micaville complex, 50 to 95 percent slopes, stony	CeF	2182	547551	lcry	nc121	1997	1:12000
Chandler-Micaville complex, 15 to 30 percent slopes, stony	CeD	803	547549	lcrw	nc121	1997	1:12000
Chandler loam, 8 to 15 percent slopes	CdC	228	547548	lcrv	nc121	1997	1:12000
Chandler loam, 2 to 8 percent slopes	CdB	90	547547	lcrt	nc121	1997	1:12000
Chandler-Micaville complex, 50 to 95 percent slopes, stony	CeG	6858	2390368	2l7cn	nc175	1968	1:15840
Chandler-Micaville complex, 30 to 50 percent slopes, stony	CfF	2690	2390366	2l7cl	nc175	1968	1:15840
Chandler-Micaville complex, 15 to 30 percent slopes, stony	CdE	347	2390367	2l7cm	nc175	1968	1:15840
Chandler gravelly fine sandy loam, 15 to 30 percent slopes, stony	722D	200	2501823	2q8mk	nc175	1968	1:15840
Chandler gravelly fine sandy loam, 30 to 50 percent slopes, stony	722E	188	2501825	2q8mm	nc175	1968	1:15840
Chandler gravelly fine sandy loam, windswept, 30 to 50 percent slopes, stony	725E	15	2501826	2q8mn	nc175	1968	1:15840
Chandler gravelly fine sandy loam, windswept, 15 to 30 percent slopes, stony	725D	13	2501824	2q8ml	nc175	1968	1:15840
Chandler fine sandy loam, 30 to 50 percent slopes	CdE	9654	563207	lx1z	nc189	2001	1:12000
Chandler gravelly fine sandy loam, 25 to 80 percent slopes	CdF	1026	1383409	1hfk3	nc193	1993	1:24000
Chandler-Micaville complex, 30 to 50 percent slopes, stony	CeE	8103	547826	ld1t	nc199	1997	1:12000
Chandler-Micaville complex, 50 to 95 percent slopes, stony	CeF	3656	547827	ld1v	nc199	1997	1:12000
Chandler-Micaville complex, 15 to 30 percent slopes, stony	CeD	2585	547825	ld1s	nc199	1997	1:12000
Chandler-Micaville complex, 8 to 15 percent slopes	CdC	238	557503	lq3z	nc199	1997	1:12000
Talladega and Chandler loams, 25 to 60 percent slopes	TcF	6582	131000	4d9t	sc602	1960	1:20000
Talladega and Chandler loams, 10 to 25 percent slopes	TcE	108	130999	4d9s	sc602	1960	1:20000
Brownwood-Chandler complex, 45 to 95 percent slopes, very stony	6F	2942	581946	mjkg	va067	2004	1:24000
Brownwood-Chandler complex, 25 to 45 percent slopes, very stony	6E	2143	581945	mjkf	va067	2004	1:24000
Brownwood-Chandler complex, 15 to 25 percent slopes, very stony	6D	296	581944	mjkd	va067	2004	1:24000
Brownwood-Chandler complex, 8 to 15 percent slopes, very stony	6C	119	581943	mjkc	va067	2004	1:24000

Map of Series Extent

Approximate geographic distribution of the CHANDLER 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).