Soil Data Explorer - THEDALUND

Official Series Description

Lab Data Summary

Aggregate lab data for the THEDALUND soil series. This aggregation is based on all pedons with a current taxon name of THEDALUND, 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 THEDALUND 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
67B	12N7618	S2012CO005001	Thedalund	8	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.7153056,-103.814

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the THEDALUND 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 THEDALUND 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 THEDALUND 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 THEDALUND 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 THEDALUND 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 THEDALUND 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 THEDALUND 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 THEDALUND, 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

No block diagrams are available.

Map Units

Map units containing THEDALUND 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
Terry-Olney-Thedalund sandy loams, 5 to 20 percent slopes	TeE	20532	94164	34zk	co005	1971	1:20000
Renohill-Litle-Thedalund complex, 9 to 30 percent slopes	RtE	15968	94151	34z4	co005	1971	1:20000
Baca-Thedalund loams, 3 to 9 percent slopes	BhD	8845	94110	34xt	co005	1971	1:20000
Thedalund clay loam, 9 to 20 percent slopes	ThE	3227	94165	34zl	co005	1971	1:20000
Thedalund clay loam, 9 to 20 percent slopes, eroded	ThE2	1590	94166	34zm	co005	1971	1:20000
Thedalund silty clay loam	Th	910	94214	3515	co009	1966	1:20000
Thedalund-Kim-Shingle complex, 9 to 20 percent slopes	109	9067	94470	359f	co075	1974	1:24000
Thedalund-Keota loams, 3 to 9 percent slopes	67	4417	95162	360r	co617	1980	1:24000
Thedalund-Keota loams, 0 to 3 percent slopes	66	2149	95161	360q	co617	1980	1:24000
Thedalund loam, 1 to 3 percent slopes	64	7628	95246	363g	co618	1976	1:24000
Thedalund loam, 3 to 9 percent slopes	65	3505	95247	363h	co618	1976	1:24000
Kim-Thedalund loams, 3 to 15 percent slopes	56	4659	497705	jpx0	co644	1980	1:24000
Thedalund loam, 3 to 9 percent slopes	108	3439	497644	jpv1	co644	1980	1:24000
Thedalund loam, 0 to 3 percent slopes	107	591	497643	jpv0	co644	1980	1:24000
Midway-Thedalund complex, hilly	MVf	121951	346067	cm3g	mt607	1970	1:24000
Thedalund-Rock outcrop complex, hilly	THg	52566	346179	cm72	mt607	1970	1:24000
Thedalund-Wibaux stony loams, hilly	THn	47033	346184	cm77	mt607	1970	1:24000
Thedalund-Midway complex, rolling	THe	37944	346177	cm70	mt607	1970	1:24000
Thedalund-Fort Collins complex, rolling	THc	36043	346175	cm6y	mt607	1970	1:24000
Midway-Thedalund complex, rolling	MVe	35130	346066	cm3f	mt607	1970	1:24000
Thedalund-Clapper complex, hilly	THa	26528	346173	cm6w	mt607	1970	1:24000
Thedalund-McRae loams, dissected	THd	14257	346176	cm6z	mt607	1970	1:24000
Thedalund-Wibaux complex, very steep	THo	13437	346185	cm78	mt607	1970	1:24000
Thedalund-Wibaux complex, rolling	THm	13334	346183	cm76	mt607	1970	1:24000
Travessilla-Thedalund loams, rolling	TS	9892	346187	cm7b	mt607	1970	1:24000
Thedalund-Nelson complex, rolling	THf	6700	346178	cm71	mt607	1970	1:24000
Thedalund loam, undulating	Tg	5890	346193	cm7j	mt607	1970	1:24000
Thedalund-Rock outcrop complex, very steep	THh	5207	346180	cm73	mt607	1970	1:24000
Thedalund-Travessilla loams, rolling	THk	4800	346181	cm74	mt607	1970	1:24000
Thedalund-Cushman loams, undulating	THb	4714	346174	cm6x	mt607	1970	1:24000
Thedalund-Wibaux loams, undulating	THl	1712	346182	cm75	mt607	1970	1:24000
Thedalund clay loam, 4 to 8 percent slopes	Te	2120	347157	cn7m	mt611	1971	1:24000
Thedalund clay loam, 8 to 15 percent slopes	Tf	1781	347158	cn7n	mt611	1971	1:24000
Razor-Thedalund clay loams, 4 to 15 percent slopes	Rb	1343	347119	cn6d	mt611	1971	1:24000
Cheeta-Rock outcrop-Thedalund complex, 10 to 60 percent slopes, extremely stony	AMG	15117	2398205	2lhjg	ut013		1:24000
Thedalund family, moist	72	63338	504570	jy1g	ut624	1985	1:24000
Thedalund family, stony	73	37170	504571	jy1h	ut624	1985	1:24000
Mesa-Chipeta-Thedalund family complex	31	29052	504525	jy00	ut624	1985	1:24000
Thedalund family-Rock outcrop-Badland association	74	17112	504572	jy1j	ut624	1985	1:24000
Thedalund family, cool	71	1257	504569	jy1f	ut624	1985	1:24000
Sandoval-Thedalund family complex	59	1107	504555	jy0z	ut624	1985	1:24000
Kim-Zigweid loams, 3 to 10 percent slopes	90	2435	349370	cqk0	wy011	1978	1:24000
Thedalund loam, 6 to 10 percent slopes	184	1417	349269	cqfr	wy011	1978	1:24000
Alice-Thedalund complex, 3 to 10 percent slopes	13	529	349209	30wnq	wy011	1978	1:24000
Alice-Thedalund complex, 10 to 30 percent slopes	14	111	349220	cqd5	wy011	1978	1:24000
Shingle-Thedalund loams, 3 to 45 percent slopes -- Draft	490	2500	152237	53dw	wy603		1:24000
Thedalund clay loam, 0 to 3 percent slopes -- Draft	50A		152593	53sc	wy629		1:24000
Shingle-Thedalund-Midway complex, 0 to 35 percent slopes -- Draft	350		152526	53q6	wy629		1:24000
Zigweid-Thedalund-Shingle association, 6 to 35 percent slopes -- Draft	351		2483488	2pc8j	wy629		1:24000

Map of Series Extent

Approximate geographic distribution of the THEDALUND 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).