Soil Data Explorer - LAMBERT

Official Series Description

Lab Data Summary

Aggregate lab data for the LAMBERT soil series. This aggregation is based on all pedons with a current taxon name of LAMBERT, 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 LAMBERT were used in the calculation. Source: KSSL snapshot (updated 2020-03-18). 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
54	96P0155	S1994ND053457	Lambert	8	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	47.6505547,-104.0358353
58A	40A3717	S1971MT111001	Lambert	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	45.9499283,-108.2507477

Water Balance

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

There are insufficient data to create the 3D hills figure.

There are insufficient data to create the 3D mountains figure.

There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with LAMBERT, 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 LAMBERT 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
Lambert-Dimyaw complex, 15 to 65 percent slopes	Lm	106504	342020	2wbx4	mt021	1971	1:24000
Lambert-Rock outcrop, soft complex, 15 to 70 percent slopes	Ld	102754	342018	cgwv	mt021	1971	1:24000
Tinsley-Lambert complex, 15 to 65 percent slopes	Tg	74625	342045	cgxq	mt021	1971	1:24000
Lambert gravelly loam, 20 to 40 percent slopes	La	37551	342015	cgwr	mt021	1971	1:24000
Lonna-Lambert complex, 4 to 25 percent slopes	Cm	29973	342003	cgwc	mt021	1971	1:24000
Lambert-Kirby complex, 15 to 65 percent slopes	Lr	26531	342021	cgwy	mt021	1971	1:24000
Zahill-Lambert complex, 15 to 65 percent slopes	Zm	21770	342065	cgyc	mt021	1971	1:24000
Lambert-Yetull complex, 15 to 65 percent slopes	Le	17790	342019	cgww	mt021	1971	1:24000
Lambert-Dimyaw complex, 15 to 65 percent slopes	385F	1872	1487338	1lxpn	mt021	1971	1:24000
Hillon-Lambert complex, 15 to 65 percent slopes	331F	1219	1596507	1ql97	mt021	1971	1:24000
Lambert-Blanchard complex, 15 to 65 percent slopes	382F	786	1487337	1lxpm	mt021	1971	1:24000
Lambert-Rock outcrop, soft, complex, 15 to 70 percent slopes	384F	507	1487335	1lxpk	mt021	1971	1:24000
Cherry-Lambert complex, 4 to 25 percent slopes	214E	182	1487319	1lxp1	mt021	1971	1:24000
Lambert-Ringling complex, 15 to 65 percent slopes	383F	24	1487339	1lxpp	mt021	1971	1:24000
Lambert-Dimyaw complex, 15 to 65 percent slopes	LfF	114364	345345	2wbx4	mt083	1973	1:24000
Zahill-Lambert complex, 15 to 65 percent slopes	ZbF	88550	345378	cld7	mt083	1973	1:24000
Lambert-Badland complex	Lc	80774	345343	clc3	mt083	1973	1:24000
Lambert-Ringling complex, 15 to 65 percent slopes	LhF	14006	345346	clc6	mt083	1973	1:24000
Lambert-Blanchard complex, 8 to 25 percent slopes	LeD	8985	345344	clc4	mt083	1973	1:24000
Lambert gravelly loam, 15 to 40 percent slopes	LaE	5956	345340	clc0	mt083	1973	1:24000
Lambert-Zahill complex, 20 to 50 percent slopes	LcF	54233	348856	cq0f	mt091	1971	1:24000
Lambert-Shale outcrop complex, 15 to 65 percent slopes	LbF	19637	348855	cq0d	mt091	1971	1:24000
Lambert silty clay loam, 4 to 8 percent slopes	LaC	3872	348853	cq0b	mt091	1971	1:24000
Wabek-Lambert complex, 15 to 35 percent slopes	WbE	3075	348877	cq13	mt091	1971	1:24000
Lambert silty clay loam, 8 to 15 percent slopes	LaD	2452	348854	cq0c	mt091	1971	1:24000
Lambert silty clay loam, 2 to 4 percent slopes	LaB	674	348852	cq09	mt091	1971	1:24000
Lambert soils, 7 to 35 percent slopes	Ld	14559	345755	clsd	mt111	1966	1:20000
Lambert-Badland-Cabba complex, 6 to 45 percent slopes	E3185F	2481	2707100	1vzvg	nd007	1998	1:24000
Lambert-Vanda, high precipitation-Rhoades, barren complex, 0 to 9 percent slopes	E3247C	278	2707102	1vzvl	nd007	1998	1:24000
Lambert-Lambert, gullied complex, 2 to 15 percent slopes	E3245D	268	2563572	2q527	nd011	1969	1:20000
Lambert silt loam, 0 to 6 percent slopes	E3241B	89	2563570	d32x	nd011	1969	1:20000
Lambert silt loam, 6 to 15 percent slopes	E3241D	24	2563571	2q526	nd011	1969	1:20000
Lambert-Vanda, high precipitation-Rhoades, barren complex, 0 to 9 percent slopes	E3247C	4979	2707226	1vzvl	nd025	1981	1:20000
Lambert-Badland-Cabba complex, 6 to 45 percent slopes	E3185F	385	2758486	1vzvg	nd025	1981	1:20000
Lambert-Badland-Cabba complex, 6 to 45 percent slopes	E3185F	1156	2707304	1vzvg	nd033	1985	1:24000
Cherry-Lambert, gullied-Havrelon, occasionally flooded complex, 0 to 6 percent slopes	E3235B	215	2759750	d32s	nd033	1985	1:24000
Lambert-Badland-Cabba complex, 6 to 45 percent slopes	E3185F	168	2525846	1vzvg	nd037	1985	1:20000
Lambert-Badland-Cabba complex, 6 to 45 percent slopes	E3185F	12047	2715095	1vzvg	nd053	2003	1:24000
Lambert-Vanda, high precipitation-Rhoades, barren complex, 0 to 9 percent slopes	E3247C	3502	2715102	1vzvl	nd053	2003	1:24000
Lambert silt loam, 0 to 6 percent slopes	E3241B	1428	2715101	d32x	nd053	2003	1:24000
Cherry-Lambert, gullied-Havrelon, occasionally flooded complex, 0 to 6 percent slopes	E3235B	1235	2715100	d32s	nd053	2003	1:24000
Lambert-Brandenburg complex, 2 to 25 percent slopes	E3027E	585	2715089	d32y	nd053	2003	1:24000
Lambert-Vanda, high precipitation-Rhoades, barren complex, 0 to 9 percent slopes	E3247C	2142	2699276	1vzvl	nd057	1976	1:20000
Lambert silt loam, 6 to 15 percent slopes	E3241D	1290	2715853	2q526	nd087	1974	1:20000
Lambert-Vanda, high precipitation-Rhoades, barren complex, 0 to 9 percent slopes	E3247C	458	2715855	1vzvl	nd087	1974	1:20000
Lambert-Lambert, gullied complex, 2 to 15 percent slopes	E3245D	423	2715854	2q527	nd087	1974	1:20000
Lambert silt loam, 0 to 6 percent slopes	E3241B	229	2715852	d32x	nd087	1974	1:20000
Lambert-Badland-Cabba complex, 6 to 45 percent slopes	E3185F	1719	1713550	1vzvg	nd089	1965	1:20000
Lambert-Vanda, high precipitation-Rhoades, barren complex, 0 to 9 percent slopes	E3247C	1026	2715999	1vzvl	nd089	1965	1:20000

Map of Series Extent

Approximate geographic distribution of the LAMBERT 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).