Soil Data Explorer - LUZENA

Official Series Description

Lab Data Summary

Aggregate lab data for the LUZENA soil series. This aggregation is based on all pedons with a current taxon name of LUZENA, 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 LUZENA were used in the calculation. Source: KSSL snapshot (updated 2020-03-13). 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 LUZENA 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 LUZENA 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 LUZENA 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 LUZENA 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 LUZENA 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 LUZENA 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 LUZENA 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.

Soil series sharing subgroup-level classification with LUZENA, 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 LUZENA 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
Yellowhorse-Luzena family complex, 1 to 10 percent slopes	92	17575	52264	1rcy	az623	1994	1:24000
Faraway-Luzena complex, 20 to 40 percent slopes	FlE	36235	52853	1rzy	az637	1968	1:31680
Faraway-Luzena complex, 40-60 percent slopes	FlF	33111	52854	1rzz	az637	1968	1:31680
Luzena cobbly loam, 0 to 30 percent slopes	LwD	20890	52881	1s0v	az637	1968	1:31680
Luzena very rocky loam, 10 to 30 percent slopes	LxD	7549	52882	1s0w	az637	1968	1:31680
Rock outcrop-Luzena complex, 20 to 90 percent slopes	34	32075	54458	1tnq	az663	1979	1:24000
Luzena very cobbly loam, very cobbly subsoil variant, 15 to 30 percent slopes	LvE	2017	53722	1swz	az665	1971	1:20000
Luzena gravelly clay loam, 5 to 15 percent slopes	LuD	733	53721	1swy	az665	1971	1:20000
Fanno-Luzena association, rolling	FaD	8455	1425171	1jv08	az667	1971	1:20000
Luzena gravelly loam, deep variant, 5 to 20 percent slopes	LuD	4850	1426115	1jvzq	az667	1971	1:20000
Luzena-Thunderbird complex, 3 to 20 percent slopes	78	38538	798411	vst6	az697	2005	1:24000
Luzena-Thunderbird complex, 3 to 20 percent slopes	20	16880	54503	1tq5	az699	1993	1:24000
Kellypoint-Luzena complex, 2 to 15 percent slopes	55	41888	615942	nny3	az701	2001	1:24000
Yellowhorse-Luzena-Sponiker association, 2 to 15 percent slopes	169	7386	616061	np1y	az701	2001	1:24000
Luzena-Kellypoint complex, 2 to 35 percent slopes	76	2601	615965	nnyv	az701	2001	1:24000
Luzena-Rock outcrop association, very steep	53	185772	56536	1wtr	nm660	1981	1:48000
Rock outcrop-Luzena association, extremely steep	73	69724	56518	1wt5	nm660	1981	1:48000
Lehmans-Luzena association, very steep	50	11091	56533	1wtn	nm660	1981	1:48000
Luzena-Rock outcrop association, 10 to 35 percent slopes	31	156565	59299	1zpw	nm662	1979	1:48000
Rock outcrop-Luzena association, 25 to 60 percent slopes	53	69171	59323	1zqn	nm662	1979	1:48000
Luzena very gravelly sandy clay loam, 5 to 25 percent slopes	30	11302	59298	1zpv	nm662	1979	1:48000
Abrazo-Luzena complex, 3 to 15 percent slopes	1	10573	59275	1zp3	nm662	1979	1:48000
Abrazo-Luzena complex, 15 to 45 percent slopes	2	3490	59286	1zpg	nm662	1979	1:48000

Map of Series Extent

Approximate geographic distribution of the LUZENA 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).