Soil Data Explorer - PROGRESSO

Official Series Description

Lab Data Summary

Aggregate lab data for the PROGRESSO soil series. This aggregation is based on all pedons with a current taxon name of PROGRESSO, 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 PROGRESSO were used in the calculation. Source: KSSL snapshot (updated 2020-03-18). Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

There are insufficient data to create the lab data summary figure.

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the PROGRESSO 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 PROGRESSO series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot (updated 2024-02-21), parsed OSD records (updated 2023-10-06) and snapshot of SC database (updated 2023-10-02).

Select annual climate data summaries for the PROGRESSO 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 2023-10-09).

Geomorphic description summaries for the PROGRESSO 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 2023-10-04).

Competing Series

Soil series competing with PROGRESSO share the same family level classification in Soil Taxonomy. Source: parsed OSD records (updated 2023-10-06) and snapshot of the SC database (updated 2023-10-02).

Select annual climate data summaries for the PROGRESSO 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 2023-10-09).

Geomorphic description summaries for the PROGRESSO 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 2023-10-04).

Soil series sharing subgroup-level classification with PROGRESSO, 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 2023-10-02).

Block Diagrams

No block diagrams are available.

Map Units

Map units containing PROGRESSO 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
Mellenthin-Progresso complex, 1 to 7 percent slopes	32	9758	52510	1rmw	az625	1992	1:24000
Puertecito-Meriwhitica-Progresso families complex, 2 to 8 percent slopes	99	4264	615990	nnzn	az701	2001	1:24000
Progresso-Skos complex, 2 to 15 percent slopes	39	26851	602471	2rqq2	az707	2011	1:24000
Skos-Progresso-Chedeski complex, 2 to 15 percent slopes	239	3028	2981410	2x2pn	az707	2011	1:24000
Olney-Progresso sandy loams, 3 to 15 percent slopes	61	22076	496500	jnn4	co627	1980	1:24000
Barx-Progresso complex, 3 to 12 percent slopes	17	26815	502007	jvcs	co675	1986	1:24000
Pinon-Bowdish-Progresso loams, cool, 1 to 12 percent slopes	75	21293	502119	jvhd	co675	1986	1:24000
Bond-Progresso complex, 3 to 30 percent slopes	25	6998	502026	jvdd	co675	1986	1:24000
Progresso loam, 3 to 6 percent slopes	81	4314	502129	jvhq	co675	1986	1:24000
Pinon-Progresso loams, 3 to 12 percent slopes	77	2513	502121	jvhg	co675	1986	1:24000
Progresso-Rock outcrop-Bowdish, stony complex, 3 to 12 percent slopes	MC65	1358	3170455	k0b0	co675	1986	1:24000
Progresso loam, 1 to 3 percent slopes	80	502	502125	jvhl	co675	1986	1:24000
Progresso loam, 6 to 12 percent slopes	82	386	502130	jvhr	co675	1986	1:24000
Barx-Progresso complex, 3 to 12 percent slopes	MC64	263	3170454	k09z	co675	1986	1:24000
Barx-Progresso complex, 3 to 12 percent slopes	MC64	3676	3170467	k09z	co676	1983	1:24000
Progresso-Rock outcrop-Bowdish, stony complex, 3 to 12 percent slopes	MC65	1077	3170468	k0b0	co676	1983	1:24000
Kech-Progresso loams, 3 to 15 percent slopes	46	14979	496624	jns4	co679	1976	1:24000
Progresso loam, 6 to 12 percent slopes	62	4437	496642	jnsq	co679	1976	1:24000
Progresso loam, 3 to 6 percent slopes	61	3764	496641	jnsp	co679	1976	1:24000
Progresso-Potts association, 1 to 6 percent slopes	63	3389	496643	jnsr	co679	1976	1:24000
Progresso-Mellenthin, stony complex, 3 to 12 percent slopes	7	16526	506762	k0b5	co680	1970	1:31680
Progresso-Rock outcrop-Bowdish, stony complex, 3 to 12 percent slopes	65	12810	506757	k0b0	co680	1970	1:31680
Barx-Progresso complex, 3 to 12 percent slopes	64	10817	506756	k09z	co680	1970	1:31680
Solirec-Progresso complex, 2 to 8 percent slopes	ScC	13949	1712032	1vghv	ut013		1:24000
Barx-Progresso complex, 3 to 12 percent slopes	664	28	2990973	k09z	ut624	1985	1:24000
Progresso-Mellenthin, stony complex, 3 to 12 percent slopes	MC7	396	3202641	k0b5	ut633	1983	1:24000
Kenzo-Retsabal-Progresso, cool complex, 2 to 30 percent slopes	5171	11774	627248	p1pt	ut686	2004	1:24000
Barx-Radnik, moist-Progresso, dry complex, 2 to 8 percent slopes	5112	11663	59804	2075	ut686	2004	1:24000
Progresso-Begay, dry complex, 1 to 8 percent slopes	5130	6459	59857	208w	ut686	2004	1:24000
Progresso, cool-Atchee family complex, 2 to 15 percent slopes	5167	2742	627243	p1pn	ut686	2004	1:24000

Map of Series Extent

Approximate geographic distribution of the PROGRESSO 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 2023-10-04).