Soil Data Explorer - DOGUE

Official Series Description

Lab Data Summary

Aggregate lab data for the DOGUE soil series. This aggregation is based on all pedons with a current taxon name of DOGUE, 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 DOGUE 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
133A	S95AL-087-2	95AL087002-pgm	Dogue	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	32.4288889,-85.9458333
136	88P0669	88NC169002	Dogue	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	36.2913895,-80.1944427

Water Balance

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

Competing Series

Soil series competing with DOGUE 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 DOGUE 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 DOGUE 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 DOGUE, 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-2012-02-07-39 | Polk County - 1998

   The relationship between soils, landscape, and parent material in the Riverview-Chewacla-Buncombe general soil map unit. The Buncombe soils are in convex areas adjacent to the stream channel; the Chewacla soils are in the lower, concave areas further from the channel; and the Riverview soils occur in the remaining areas of the flood plain. The clayey Masada, Dogue, and Roanoke soils are on the higher stream terraces (Soil Survey of Polk County, North Carolina; 1998).

Map Units

Map units containing DOGUE 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
Dogue fine sandy loam, 0 to 2 percent slopes, rarely flooded	DgA	6441	330456	c2vw	al087	1997	1:24000
Dogue fine sandy loam, 0 to 2 percent slopes, rarely flooded	DgA	14100	331341	c3sf	al113	1997	1:24000
Dogue sandy loam, 0 to 2 percent slopes	DgA	1110	324575	bwr5	ga033	1982	1:20000
Dogue loam, 1 to 2 percent slopes	DgA	395	124821	45wh	ga215	1980	1:15840
Dogue fine sandy loam, 0 to 3 percent slopes	DgA	4280	324868	bx1m	ga245	1979	1:15840
Dogue-Urban land complex, 0 to 3 percent slopes	DhA	1885	324869	bx1n	ga245	1979	1:15840
Dogue sandy loam, 0 to 2 percent slopes	DgA	1359	325832	by1q	ga638	1987	1:20000
Dogue fine sandy loam, gently undulating, rarely flooded	DgB	2401	2403467	2lp06	ms153	2008	1:24000
Dogue fine sandy loam, 1 to 4 percent slopes	DgB	1972	111568	3r2z	nc013	1986	1:24000
Dogue sandy loam, 2 to 6 percent slopes	DgB	2450	111421	3qy7	nc015	1984	1:24000
Dogue sandy loam, 0 to 2 percent slopes	DgA	2350	111420	3qy6	nc015	1984	1:24000
Dogue sandy loam, 6 to 12 percent slopes	DgC	550	111422	3qy8	nc015	1984	1:24000
Dogue sandy loam, 0 to 3 percent slopes	DgA	1599	115479	3w54	nc017	1983	1:24000
Dogue fine sandy loam, 0 to 2 percent slopes	DgA	4527	811388	w79t	nc041	1982	1:24000
Dogue fine sandy loam, 2 to 6 percent slopes	DgB	3075	811389	w79v	nc041	1982	1:24000
Dogue fine sandy loam, 0 to 2 percent slopes	DgA	2746	811083	w6zz	nc051	1981	1:24000
Dogue fine sandy loam, 0 to 3 percent slopes	DgA	4802	1015550	132rp	nc065	1976	1:20000
Dogue fine sandy loam, 1 to 4 percent slopes	DgB	1161	116127	3wv1	nc137	1984	1:24000
Dogue fine sandy loam, 2 to 6 percent slopes	DgB	1636	811426	w7c1	nc143	1982	1:24000
Dogue fine sandy loam, 0 to 2 percent slopes	DgA	1116	811425	w7c0	nc143	1982	1:24000
Dogue fine sandy loam, 0 to 3 percent slopes	DgA	2987	116205	3wxk	nc187	1979	1:24000
Dogue fine sandy loam, 2 to 7 percent slopes, rarely flooded	9B	1794	118209	3z06	va007	1994	1:24000
Dogue fine sandy loam, 0 to 2 percent slopes, rarely flooded	9A	1360	118208	3z05	va007	1994	1:24000
Dogue silt loam, 2 to 6 percent slopes	18B	6581	117810	3ylb	va036	1993	1:24000
Dogue silt loam, 0 to 2 percent slopes	18A	630	117809	3yl9	va036	1993	1:24000
Dogue silt loam, 6 to 10 percent slopes	18C	144	117811	3ylc	va036	1993	1:24000
Dogue loam, variant, 0 to 4 percent slopes	68B	982	118929	3zrf	va041	1974	1:15840
Dogue fine sandy loam, 2 to 7 percent slopes, rarely flooded	15B	3179	1587408	1q8tq	va049	2005	1:24000
Dogue fine sandy loam, 0 to 2 percent slopes, rarely flooded	15A	1011	1587407	1q8tp	va049	2005	1:24000
Dogue loam, 0 to 2 percent slopes	8A	748	121505	42fj	va057	1985	1:20000
Dogue fine sandy loam, 0 to 2 percent slopes	4A	2310	118974	3zsw	va073	1978	1:15840
Dogue fine sandy loam, 2 to 6 percent slopes	4B	659	118975	3zsx	va073	1978	1:15840
Dogue silt loam, 2 to 8 percent slopes, rarely flooded	20B	542	1472812	1lfl2	va083	2004	1:24000
Caroline-Dogue complex, 7 to 15 percent slopes, eroded	13C2	3830	119076	3zx5	va085	1976	1:15840
Dogue loam	23	3070	119094	3zxr	va085	1976	1:15840
Caroline-Dogue complex, 2 to 7 percent slopes, eroded	13B2	890	119075	3zx4	va085	1976	1:15840
Altavista-Dogue complex, 0 to 2 percent slopes	2A	2693	119684	40js	va127	1985	1:15840
Dogue fine sandy loam, 0 to 2 percent slopes	13A	2138	119663	40j3	va127	1985	1:15840
Dogue silt loam, 2 to 7 percent slopes	10B	2290	120175	411m	va145	1984	1:15840
Dogue silt loam, 7 to 15 percent slopes	10C	187	120176	411n	va145	1984	1:15840
Dogue silt loam, 0 to 2 percent slopes	10A	165	120174	411l	va145	1984	1:15840
Dogue fine sandy loam, 2 to 6 percent slopes	4B	926	120374	4181	va159	1980	1:20000
Dogue loam	16	739	120391	418l	va177	1980	1:15840
Dogue loam, 0 to 2 percent slopes	DoA	2266	120516	41dm	va179	1970	1:15840
Dogue loam, 2 to 6 percent slopes	DoB	501	120517	41dn	va179	1970	1:15840
Dogue loam, 2 to 6 percent slopes	13B	600	122509	43gx	va181	1997	1:24000
Dogue loam, 0 to 2 percent slopes	11A	1834	1723053	1vtzc	va183	2006	1:24000
Dogue loam, 2 to 6 percent slopes	11B	319	1723055	1vtzf	va183	2006	1:24000
Dogue loam	16	6	2376403	2krv5	va630	2008	1:12000
Dogue fine sandy loam, 2 to 6 percent slopes	DoB	902	120698	41lh	va631	1973	1:15840
Dogue fine sandy loam, 0 to 2 percent slopes	DoA	233	120697	41lg	va631	1973	1:15840
Dogue loam	12	1497	120799	41pr	va695	1981	1:15840
Dogue loam, 0 to 4 percent slopes, rarely flooded	13A	7	140083	4prt	va760	2004	1:24000
Dogue fine sandy loam, 2 to 6 percent slopes, eroded	5B2	2300	120873	41s4	va800	1979	1:15840
Dogue fine sandy loam, 0 to 2 percent slopes	5A	1700	120872	41s3	va800	1979	1:15840

Map of Series Extent

Approximate geographic distribution of the DOGUE 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).