Soil Data Explorer - HONDOHO

Official Series Description

Lab Data Summary

Aggregate lab data for the HONDOHO soil series. This aggregation is based on all pedons with a current taxon name of HONDOHO, 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 HONDOHO 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 HONDOHO 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 HONDOHO 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 HONDOHO 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 HONDOHO 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).

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

Competing Series

Soil series competing with HONDOHO 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 HONDOHO 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 HONDOHO 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 flats position figure.

Soil series sharing subgroup-level classification with HONDOHO, 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 HONDOHO 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
Wahtigup-Hondoho complex, 4 to 30 percent slopes	92	11116	3163511	2v06f	id709	1976	1:24000
Wahtigup-Hondoho complex, 30 to 60 percent slopes	93	10173	3163512	2v06g	id709	1976	1:24000
Arbone-Hondoho association, rolling	5	2811	82626	2rzc	id709	1976	1:24000
Hondoho-Arbone complex, steep	22	1875	82596	2ryd	id709	1976	1:24000
Arbone-Hondoho association, hilly	6	1814	82637	2rzq	id709	1976	1:24000
Cedarhill, high precipitation-Hondoho-Ridgecrest complex, 20 to 50 percent slopes	111	80	82683	2s16	id709	1976	1:24000
Hondoho very cobbly loam, 30 to 55 percent slopes	HOG	6023	3163513	2szw8	id710	1968	1:24000
Hondoho very cobbly loam, hilly	HOF	4713	82731	2s2r	id710	1968	1:24000
Wahtigup-Hondoho complex, 30 to 60 percent slopes	93	14	3173231	2v06g	id710	1968	1:24000
Valmar, low precipitation-Watercanyon-Hondoho complex, 20 to 50 percent slopes	119	9228	3163562	2szwf	id711	1983	1:24000
Hondoho-Arbone-Ririe complex, 20 to 50 percent slopes	54	9165	3163538	2v05p	id711	1983	1:24000
Hondoho-Arbone complex, 4 to 12 percent slopes	53	7599	3163537	2v05q	id711	1983	1:24000
Cedarhill, high precipitation-Hondoho-Ridgecrest, extremely stony surface, complex, 20 to 50 percent slopes	35	5406	3163530	2v06l	id711	1983	1:24000
Hades-Camelback-Hondoho complex, 30 to 60 percent slopes	47	5191	3163535	2v05r	id711	1983	1:24000
Wursten-Watercanyon variant-Hondoho complex, 12 to 40 percent slopes	123	5115	82877	2s7g	id711	1983	1:24000
Hondoho-Camelback-Lanoak complex, 20 to 50 percent slopes	56	4480	3163539	2v05n	id711	1983	1:24000
Arbone-Hondoho complex, 12 to 20 percent slopes	3	2652	3163518	2szw1	id711	1983	1:24000
Cedarhill, high precipitation-Hondoho-Arbone complex, 20 to 50 percent slopes	34	2457	3163529	2v05w	id711	1983	1:24000
Hondoho-Hades complex, 4 to 12 percent slopes	55	762	82928	2s93	id711	1983	1:24000
Swanner-Hondoho complex, 12 to 20 percent slopes	109	467	82861	2s6y	id711	1983	1:24000
Cedarhill-Hondoho-Ridgecrest complex, 25 to 55 percent slopes	209	63	3173241	2rfzv	id711	1983	1:24000
Ridgecrest-Hondoho-Lizdale association, 30 to 60 percent slopes	108-O	744	3173321	2v07d	id712	2008	1:24000
Hondoho, very stony surface-Clegg-Dranyon complex, 25 to 60 percent slopes	1035	29	3173293	2w9rt	id712	2008	1:24000
Hondoho-Ridgecrest-Hades association, 12 to 50 percent slopes	43	2043	2619847	2v06w	id713		1:24000
Ireland-Hondoho-Dranyon complex, 15 to 50 percent slopes	2550	1706	2520248	2pt1n	id713		1:24000
Hades-Camelback-Hondoho complex, 30 to 60 percent slopes	47	1694	2514580	2v05r	id713		1:24000
Ridgecrest-Hondoho-Lizdale association, 30 to 60 percent slopes	108	1574	2619839	2v07d	id713		1:24000
Hondoho, very stony surface-Clegg-Dranyon complex, 25 to 60 percent slopes	1035	687	2917036	2w9rt	id713		1:24000
Cedarhill-Hondoho-Ridgecrest complex, 25 to 55 percent slopes	209	483	2619859	2rfzv	id713		1:24000
Arbone-Hondoho-Cedarhill complex, 12 to 30 percent slopes	6	325	2619849	2v06p	id713		1:24000
Hondoho-Arbone-Ririe complex, 20 to 50 percent slopes	54	291	2619862	2v05p	id713		1:24000
Sprollow-Hondoho, stony surface, complex, 20 to 60 percent slopes	131	288	2917060	2sltp	id713		1:24000
Hondoho-Camelback-Lanoak complex, 20 to 50 percent slopes	56	232	2514583	2v05n	id713		1:24000
Cedarhill, high precipitation-Hondoho-Arbone complex, 20 to 50 percent slopes	34	188	2514579	2v05w	id713		1:24000
Arbone-Hondoho-Cedarhill complex, 4 to 12 percent slopes	5	182	2619848	2v06n	id713		1:24000
Cedarhill-Hondoho-Ridgecrest complex, 20 to 60 percent slopes	BHG	166	2965723	n4b8	id713		1:24000
Cedarhill, high precipitation-Hondoho-Ridgecrest, extremely stony surface, complex, 20 to 50 percent slopes	35	146	2520215	2v06l	id713		1:24000
Hondoho very cobbly loam, 30 to 55 percent slopes	HOG	89	2520225	2szw8	id713		1:24000
Hondoho-Hymas-Pavohroo association, 12 to 30 percent slopes	41	67	2619845	2v06t	id713		1:24000
Hondoho-Hymas-Pavohroo association, 30 to 60 percent slopes	42-O	50	2619846	2v06v	id713		1:24000
Arbone-Hondoho complex, 12 to 20 percent slopes	3	39	2619856	2szw1	id713		1:24000
Hondoho, stony surface-Ricrest complex, 4 to 40 percent slopes	54-F	33	2917062	2sltl	id713		1:24000
Wahtigup-Hondoho complex, 4 to 30 percent slopes	92	29	2619835	2v06f	id713		1:24000
Povey-Hades-Hondoho association, 10 to 50 percent slopes	91	21	2619883	2v077	id713		1:24000
Ridgecrest-Hondoho complex, 30 to 60 percent slopes	106	11	2619877	2v07c	id713		1:24000
Hondoho-Arbone complex, 4 to 12 percent slopes	53	3	2514582	2v05q	id713		1:24000
Povey-Hades-Hondoho, stony surface, complex, 10 to 50 percent slopes	121	1	3093889	j8wz	id713		1:24000
Wahtigup-Hondoho complex, 30 to 60 percent slopes	93	1	2619834	2v06g	id713		1:24000
Hondoho, stony surface-Sprollow-Hades complex, 12 to 50 percent slopes	55	0	3093897	j8zw	id713		1:24000
Valmar, low precipitation-Watercanyon-Hondoho complex, 20 to 50 percent slopes	119	0	2520214	2szwf	id713		1:24000
Hondoho, stony surface-Sprollow-Hades complex, 12 to 50 percent slopes	55	5103	485301	j8zw	id714	1997	1:24000
Sprollow-Hondoho, stony surface, complex, 20 to 60 percent slopes	131	2376	3163579	2sltp	id714	1997	1:24000
Povey-Hades-Hondoho, stony surface, complex, 10 to 50 percent slopes	121	1160	485211	j8wz	id714	1997	1:24000
Hondoho, stony surface-Ricrest complex, 4 to 40 percent slopes	54	1142	3163569	2sltl	id714	1997	1:24000
Hondoho-Vitale complex, 20 to 50 percent slopes	56	1057	485302	j8zx	id714	1997	1:24000
Cedarhill-Hondoho, stony surface-Ridgecrest, extremely stony surface complex, 20 to 50 percent slopes	36	514	485280	j8z6	id714	1997	1:24000
Hades-Camelback-Hondoho complex, 30 to 60 percent slopes	46	418	485291	j8zk	id714	1997	1:24000
Hondoho-Hades complex, 4 to 12 percent slopes	53	28	485299	j8zt	id714	1997	1:24000
Ridgecrest-Hondoho complex, 30 to 60 percent slopes	106	30467	3163608	2v07c	id715	1994	1:24000
Hondoho-Ridgecrest-Hades association, 12 to 50 percent slopes	43	25223	3163592	2v06w	id715	1994	1:24000
Hondoho-Hymas-Pavohroo association, 30 to 60 percent slopes	42	23181	3163591	2v06v	id715	1994	1:24000
Arbone-Hondoho-Cedarhill complex, 12 to 30 percent slopes	6	17809	3163587	2v06p	id715	1994	1:24000
Arbone-Hondoho-Cedarhill complex, 4 to 12 percent slopes	5	15698	3163586	2v06n	id715	1994	1:24000
Ridgecrest-Hondoho-Lizdale association, 30 to 60 percent slopes	108	10219	3163609	2v07d	id715	1994	1:24000
Ridgecrest-Hondoho-Hymas association, 30 to 60 percent slopes	107	9349	485574	j98p	id715	1994	1:24000
Hondoho-Calpac-Lizdale association, 30 to 70 percent slopes	40	8457	485634	j9bm	id715	1994	1:24000
Povey-Hades-Hondoho association, 10 to 50 percent slopes	91	3127	3163604	2v077	id715	1994	1:24000
Hondoho-Hymas-Pavohroo association, 12 to 30 percent slopes	41	2355	3163590	2v06t	id715	1994	1:24000
Ririe-Hondoho complex, 12 to 20 percent slopes	113	640	485581	j98x	id715	1994	1:24000
Lanoak-Hondoho complex, 6 to 20 percent slopes	69	408	485665	j9cm	id715	1994	1:24000
Ireland-Hondoho-Dranyon complex, 15 to 50 percent slopes	2550	2778	2495470	2pt1n	id716		1:24000
Cedarhill-Hondoho-Ridgecrest complex, 20 to 60 percent slopes	BHG	975	599982	n4b8	id716		1:24000
Hondoho-Arbone-Ririe, very deep complex, 15 to 50 percent slopes	400C	434	1861303	20gv1	id716		1:24000
Hondoho, stony surface-Ricrest complex, 4 to 40 percent slopes	54	400	2984139	2sltl	id716		1:24000
Buist-Hondoho complex, 1 to 12 percent slopes, extremely stony surface	THX	321	1862048	20hm2	id716		1:24000
Ridgecrest-Hondoho-Lizdale association, 30 to 60 percent slopes	108	6	3136546	2v07d	id716		1:24000
Sprollow-Hondoho, stony surface, complex, 20 to 60 percent slopes	131	6	2984136	2sltp	id716		1:24000
Hondoho gravelly loam, 4 to 30 percent slopes	37	5468	79005	2n6k	id763	1998	1:24000
Vicking family-Hondoho-Araveton complex, 4 to 15 percent slopes	3709		3406498	31fxn	wy723		1:24000

Map of Series Extent

Approximate geographic distribution of the HONDOHO 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).