Soil Data Explorer - LANOAK

Official Series Description

Lab Data Summary

Aggregate lab data for the LANOAK soil series. This aggregation is based on all pedons with a current taxon name of LANOAK, 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 LANOAK 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 LANOAK 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 LANOAK series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot (updated 2024-02-21), parsed OSD records (updated 2023-10-02) and snapshot of SC database (updated 2023-10-02).

Select annual climate data summaries for the LANOAK 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 LANOAK 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).

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

Competing Series

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

Select annual climate data summaries for the LANOAK 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 LANOAK 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 2D hillslope position figure.

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 terrace figure.

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

Soil series sharing subgroup-level classification with LANOAK, 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 LANOAK 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
Lanoak silt loam, 12 to 20 percent slopes	31	4295	82606	2ryq	id709	1976	1:24000
Lanoak silt loam, 20 to 30 percent slopes	32	3365	82607	2ryr	id709	1976	1:24000
Lanoak silt loam, 4 to 12 percent slopes	30	3166	82605	2ryp	id709	1976	1:24000
Lanoak family-Robin complex, 10 to 35 percent slopes	307	872	3163621	2ppdh	id709	1976	1:24000
Lanoak silt loam, 30 to 45 percent slopes	33	647	82608	2rys	id709	1976	1:24000
Hades-Lanoak-Camelback complex, 20 to 50 percent slopes	106	68	82685	2s18	id709	1976	1:24000
Lanoak silt loam, hilly	LAF	19737	82740	2s31	id710	1968	1:24000
Lanoak silt loam, 4 to 12 percent slopes	LAC	2256	82738	2s2z	id710	1968	1:24000
Lanoak silt loam, 12 to 20 percent slopes	LAE	1384	82739	2s30	id710	1968	1:24000
Lanoak-Yago, very stony surface, complex, 5 to 20 percent slopes	42	686	2558435	2pwvh	id710	1968	1:24000
Lanoak silt loam, 0 to 4 percent slopes	LAB	271	82737	2s2y	id710	1968	1:24000
Lanoak family-Robin complex, 10 to 35 percent slopes	307	251	3173232	2ppdh	id710	1968	1:24000
Lanoak-Hades-Rexburg, very deep, complex, 4 to 20 percent slopes	480GG	144	3238959	2wg11	id710	1968	1:24000
Dranburn-Broadhead-Lanoak complex, 10 to 30 percent slopes	470D	17	3238958	n466	id710	1968	1:24000
Camelback-Cedarhill, high precipitation-Lanoak complex, 20 to 50 percent slopes	23	12355	3163521	2v063	id711	1983	1:24000
Hades-Camelback-Lanoak complex, 20 to 50 percent slopes	50	6750	3163536	2v06h	id711	1983	1:24000
Lanoak-Hades complex, 6 to 20 percent slopes	72	5601	3163544	2szx2	id711	1983	1:24000
Hondoho-Camelback-Lanoak complex, 20 to 50 percent slopes	56	4480	3163539	2v05n	id711	1983	1:24000
Lanoak-Camelback complex, 20 to 50 percent slopes	69	4256	3163543	2szx3	id711	1983	1:24000
Lanoak-Watercanyon-Rexburg complex, 12 to 20 percent slopes	73	3915	3163545	2szx1	id711	1983	1:24000
Lanoak silt loam, 12 to 20 percent slopes	67	3882	82941	2s9j	id711	1983	1:24000
Lanoak silt loam, 4 to 12 percent slopes	66	2740	82940	2s9h	id711	1983	1:24000
Lanoak-Greys association, 12 to 20 percent slopes	71	2677	82946	2s9p	id711	1983	1:24000
Lanoak-Greys association, 4 to 12 percent slopes	70	1996	82945	2s9n	id711	1983	1:24000
Lanoak silt loam, 20 to 30 percent slopes	68	1529	82942	2s9k	id711	1983	1:24000
Hades-Lanoak complex, 4 to 12 percent slopes	49	1525	82921	2s8w	id711	1983	1:24000
Lanoak silt loam, 1 to 4 percent slopes	65	378	82939	2s9g	id711	1983	1:24000
Lanoak family-Robin complex, 10 to 35 percent slopes	307	61	3173243	2ppdh	id711	1983	1:24000
Lanoak-Arbone complex, 12 to 25 percent slopes	134	660	154318	55l0	id712	2008	1:24000
Lanoak-Rexburg complex, 1 to 4 percent slopes	135	533	154315	55kx	id712	2008	1:24000
Lanoak silt loam, 1 to 4 percent slopes	130	521	154313	55kv	id712	2008	1:24000
Iphil-Lanoak-Watercanyon complex, 12 to 25 percent slopes	109	500	154303	55kj	id712	2008	1:24000
Lanoak silt loam, 4 to 8 percent slopes	131	470	154314	55kw	id712	2008	1:24000
Lanoak silt loam, 8 to 12 percent slopes	132	427	154316	55ky	id712	2008	1:24000
Lanoak silt loam, 12 to 20 percent slopes	133	200	154317	55kz	id712	2008	1:24000
Lanoak family-Robin complex, 10 to 35 percent slopes	307	6869	2492971	2ppdh	id713		1:24000
Lanoak-Camelback complex, 20 to 50 percent slopes	69	2343	2520217	2szx3	id713		1:24000
Camelback-Cedarhill, high precipitation-Lanoak complex, 20 to 50 percent slopes	23	883	2514572	2v063	id713		1:24000
Lanoak-Yago, very stony surface, complex, 5 to 20 percent slopes	42	687	2497411	2pwvh	id713		1:24000
Lanoak-Hades complex, 6 to 20 percent slopes	72	554	2514588	2szx2	id713		1:24000
Hades-Camelback-Lanoak complex, 20 to 50 percent slopes	50	276	2514581	2v06h	id713		1:24000
Hondoho-Camelback-Lanoak complex, 20 to 50 percent slopes	56	232	2514583	2v05n	id713		1:24000
Lanoak-Dranburn-Ricafied complex, 15 to 55 percent slopes	2450	142	2917053	2pt1h	id713		1:24000
Dranburn-Broadhead-Lanoak complex, 10 to 30 percent slopes	470D	81	2520241	n466	id713		1:24000
Lanoak silt loam, 12 to 20 percent slopes	67-B	58	2514587	2s9j	id713		1:24000
Lanoak-Watercanyon-Rexburg complex, 12 to 20 percent slopes	73	52	2514589	2szx1	id713		1:24000
Lanoak-Hades-Lanark complex, 4 to 24 percent slopes	7012	47	2981069	2yvfb	id713		1:24000
Lanoak-Broadhead-Hades complex, 25 to 50 percent slopes	77-F	27	3163230	2yy48	id713		1:24000
Rexburg-Watercanyon-Lanoak complex, 12 to 20 percent slopes	105	17	2619910	2v07b	id713		1:24000
Lanoak-Arbone complex, 8 to 20 percent slopes	480K	12	2520239	5bnw	id713		1:24000
Lanoak silt loam, 0 to 4 percent slopes	480A	2	2965721	5bnp	id713		1:24000
Lanoak-Broadhead complex, 12 to 30 percent slopes	76	4014	485324	j90m	id714	1997	1:24000
Lanoak silt loam, 0 to 4 percent slopes	74	2402	485322	j90k	id714	1997	1:24000
Lanoak-Broadhead-Hades complex, 25 to 50 percent slopes	77	2360	3163571	2yy48	id714	1997	1:24000
Lanoak silt loam, 4 to 12 percent slopes	75	1407	485323	j90l	id714	1997	1:24000
Lanoak-Thatcher complex, 12 to 30 percent slopes	79	1342	485327	j90q	id714	1997	1:24000
Huffman-Harroun-Lanoak complex, 2 to 12 percent slopes	60	455	485307	j902	id714	1997	1:24000
Lanoak-Hades complex, 6 to 20 percent slopes	78	294	485326	j90p	id714	1997	1:24000
Hades-Lanoak-Camelback complex, 20 to 50 percent slopes	47	38	485292	j8zl	id714	1997	1:24000
Lanoak silt loam, 4 to 8 percent slopes	480B	31	3173389	5bnq	id714	1997	1:24000
Rexburg-Lanoak complex, 12 to 25 percent slopes	101	3345	485568	j98h	id715	1994	1:24000
Rexburg-Watercanyon-Lanoak complex, 12 to 20 percent slopes	105	2179	3163607	2v07b	id715	1994	1:24000
Rexburg-Lanoak complex, 4 to 12 percent slopes	100	1777	485567	j98g	id715	1994	1:24000
Rexburg-Lanoak-Watercanyon complex, 4 to 12 percent slopes	102	1595	485569	j98j	id715	1994	1:24000
Lanoak silt loam, 0 to 4 percent slopes	67	1134	485663	j9ck	id715	1994	1:24000
Lanoak-Hondoho complex, 6 to 20 percent slopes	69	408	485665	j9cm	id715	1994	1:24000
Lanoak silt loam, 12 to 30 percent slopes	68	376	485664	j9cl	id715	1994	1:24000
Lanoak family-Robin complex, 10 to 35 percent slopes	307	144	3173364	2ppdh	id715	1994	1:24000
Lanoak-Camelback complex, 20 to 50 percent slopes	69-B	8	3173360	2szx3	id715	1994	1:24000
Lanoak-Hades-Rexburg, very deep, complex, 4 to 20 percent slopes	480GG	6103	2930234	2wg11	id716		1:24000
Ireland-Ricrest-Lanoak complex, 12 to 40 percent slopes	7034	3420	3175631	2z43q	id716		1:24000
Dranburn-Broadhead-Lanoak complex, 10 to 30 percent slopes	470D	3413	599856	n466	id716		1:24000
Lanoak-Dranburn-Ricafied complex, 15 to 55 percent slopes	2450	2248	2495465	2pt1h	id716		1:24000
Lanoak silt loam, 12 to 20 percent slopes	480J	2119	159211	5bnv	id716		1:24000
Lanoak silt loam, 0 to 4 percent slopes	480A	1899	159206	5bnp	id716		1:24000
Ireland-Lanoak complex, 10 to 35 percent slopes	420G	1283	1860315	20ft5	id716		1:24000
Iphil, very deep-Lanoak-Feeder complex, 4 to 12 percent slopes	405H	1228	159408	5bw6	id716		1:24000
Rexburg, very deep-Lanoak complex, 8 to 24 percent slopes	700S	1194	159242	5bpv	id716		1:24000
Lanoak-Hades-Lanark complex, 4 to 24 percent slopes	7012	1129	3156830	2yvfb	id716		1:24000
Lanoak silt loam, 4 to 8 percent slopes	480B	1085	159207	5bnq	id716		1:24000
Lanoak-Arbone complex, 8 to 20 percent slopes	480K	902	159212	5bnw	id716		1:24000
Lanoak-Rexburg, very deep, complex, 1 to 8 percent slopes	480G	701	159209	5bns	id716		1:24000
Lanoak silt loam, 8 to 12 percent slopes	480I	651	159210	5bnt	id716		1:24000
Iphil, very deep-Lanoak-Feeder complex, 12 to 25 percent slopes	405G	422	159195	5bnb	id716		1:24000
Lanoak silt loam, cool, 0 to 4 percent slopes	480AA	240	2249181	2fhg7	id716		1:24000
Hades-Camelback, very deep-Lanoak complex, 1 to 10 percent slopes	370AA	191	2248201	2fgfm	id716		1:24000
Lanoak silt loam, cool, 8 to 12 percent slopes	480II	188	2250064	2fjcq	id716		1:24000
Lanoak-Hades complex, 6 to 20 percent slopes	LHE	104	600003	n4by	id716		1:24000
Camelback-Cedarhill, high precipitation-Lanoak complex, 20 to 50 percent slopes	23	53	3136435	2v063	id716		1:24000
Lanoak-Yago, very stony surface, complex, 5 to 20 percent slopes	42	42	3163422	2pwvh	id716		1:24000
Lanoak-Hades-Rexburg, very deep, complex, 4 to 20 percent slopes	480GG	499	3238978	2wg11	id770	1968	1:24000

Map of Series Extent

Approximate geographic distribution of the LANOAK 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).