Soil Data Explorer - HAVERDAD

Official Series Description

Lab Data Summary

Aggregate lab data for the HAVERDAD soil series. This aggregation is based on all pedons with a current taxon name of HAVERDAD, 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 HAVERDAD were used in the calculation. Source: KSSL snapshot (updated 2020-03-13). 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
58B	91P0200	91WY005002	Haverdad	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.7461128,-105.1044464
58B	91P0201	91WY019001	Haverdad	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.2527771,-106.1330566
n/a	01N0853	S2001WY019002	Haverdad	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	01N0854	S2001WY019003	Haverdad	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the HAVERDAD 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 HAVERDAD 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 HAVERDAD 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 HAVERDAD 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 HAVERDAD 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 HAVERDAD 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 HAVERDAD 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 mountains figure.

Soil series sharing subgroup-level classification with HAVERDAD, 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 HAVERDAD 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
Haverdad clay loam, 0 to 3 percent slopes	284	136	1387764	1hl2l	mt643	1967	1:20000
Haverdad loam, alkali, 0 to 3 percent slopes	49	10073	503741	jx5q	ut616	1983	1:24000
Haverdad loam, moist, 1 to 5 percent slopes	50	9743	503743	jx5s	ut616	1983	1:24000
Haverdad loam, 1 to 8 percent slopes	48	6459	503740	jx5p	ut616	1983	1:24000
Haverdad silt loam	40	15018	55168	1vdm	ut631	1982	1:24000
Haverdad loam, 0 to 3 percent slopes	254	177	780261	v5xq	wy011	1978	1:24000
Clarkelen-Haverdad complex, 0 to 3 percent slopes, rarely flooded	137	24102	349588	2yv6y	wy027	1993	1:24000
Haverdad loam, overflow, 0 to 4 percent slopes	136	10828	349586	cqrz	wy027	1993	1:24000
Haverdad-Clarkelen complex, saline, 0 to 3 percent slopes	138	4848	349590	cqs3	wy027	1993	1:24000
Lohmiller-Haverdad complex, saline, 1 to 4 percent slopes	159	465	349632	cqtg	wy027	1993	1:24000
Coaliams-Haverdad complex, 0 to 3 percent slopes	135	24813	104492	3hqq	wy031	1998	1:24000
Forkwood-Kishona association	22	62777	152066	537c	wy043	1976	1:24000
Forkwood-Haverdad association	21	29732	152065	537b	wy043	1976	1:24000
Haverdad-Clarkelen complex, 0 to 4 percent slopes	46	32113	349450	cqml	wy045	1984	1:24000
Lohmiller-Haverdad complex, saline, 1 to 4 percent slopes	60	20131	349466	cqn3	wy045	1984	1:24000
Lohmiller-Haverdad complex, 1 to 4 percent slopes	59	7792	349464	cqn1	wy045	1984	1:24000
Haverdad-Clarkelen variant complex, saline, 0 to 4 percent slopes	47	5232	349451	cqmm	wy045	1984	1:24000
Haverdad-Clarkelen complex, saline, 0 to 3 percent slopes	156	160	1614841	1r6cn	wy045	1984	1:24000
Haverdad loam, overflow, 0 to 4 percent slopes	166	155	1650251	1sd6x	wy045	1984	1:24000
Haverdad, occasionally flooded-Kishona clay loams, 0 to 6 percent slopes	153	11770	349840	2ztzd	wy605	1995	1:24000
Haverdad loam, 0 to 3 percent slopes	151	9753	349836	cr11	wy605	1995	1:24000
Haverdad-Clarkelen complex, 0 to 4 percent slopes	152	2082	349838	cr13	wy605	1995	1:24000
Haverdad-Clarkelen complex, wet, 0 to 3 percent slopes	167	9497	1669827	1t1ld	wy609	2006	1:24000
Clarkelen-Haverdad complex, 0 to 3 percent slopes, rarely flooded	165	6880	1669691	2yv6y	wy609	2006	1:24000
Haverdad loam, wet, 0 to 3 percent slopes	164	5523	1669693	1t1g2	wy609	2006	1:24000
Haverdad loam, 0 to 3 percent slopes	162	3916	1669828	1t1lf	wy609	2006	1:24000
Clarkelen, wet-Haverdad, wet-Bigwinder complex, 0 to 3 percent slopes	125	1869	1669825	1t1lb	wy609	2006	1:24000
Haverdad-Lohmiller complex, 0 to 6 percent slopes, rarely flooded	168	830	1669692	2wlrw	wy609	2006	1:24000
Clarkelen-Bigwinder-Haverdad complex, 0 to 3 percent slopes, rarely flooded	129	615	1669671	2yv79	wy609	2006	1:24000
Haverdad loam, overflow, 0 to 4 percent slopes	163	55	1669813	1t1ky	wy609	2006	1:24000
Haverdad-Clarkelen complex, overflow, 0 to 3 percent slopes	166	13	1669807	1t1kr	wy609	2006	1:24000
Haverdad-Clarkelen complex, 0 to 4 percent slopes	152	49	817240	wfdl	wy619	1971	1:24000
Haverdad, occasionally flooded-Kishona clay loams, 0 to 6 percent slopes	153	35	817241	2ztzd	wy619	1971	1:24000
Haverdad-Clarkelen complex, 0 to 3 percent slopes	103	30	816585	wdqg	wy619	1971	1:24000
Haverdad-Clarkelen complex, saline, 0 to 3 percent slopes	195	6	816721	wdvv	wy619	1971	1:24000
Haverdad-Clarkelen complex, saline, 0 to 3 percent slopes	195	42386	502283	jvnp	wy625	1985	1:24000
Haverdad-Clarkelen complex, 0 to 3 percent slopes	194	20455	502282	jvnn	wy625	1985	1:24000
Haverdad loam, 0 to 4 percent slopes	193	1156	502281	jvnm	wy625	1985	1:24000
Clarkelen-Bigwinder-Haverdad complex, 0 to 3 percent slopes, rarely flooded	324	19	1421365	2yv79	wy625	1985	1:24000
Haverdad-Lohmiller complex, 0 to 6 percent slopes, rarely flooded	330	7	1426088	2wlrw	wy625	1985	1:24000
Haverdad clay loam, 0 to 3 percent slopes -- Draft	33A		152521	53q1	wy629		1:24000
Haverdad clay loam, 3 to 6 percent slopes -- Draft	33B		152522	53q2	wy629		1:24000
Shingle-Haverdad, frequently flooded complex, 0 to 80 percent slopes	255	9160	360997	d3n2	wy633	1987	1:24000
Haverdad-Draknab complex, 0 to 3 percent slopes	158	6510	361149	d3sz	wy633	1987	1:24000
Haverdad very fine sandy loam, 0 to 3 percent slopes	154	5170	361145	d3sv	wy633	1987	1:24000
Haverdad, moist-Worthenton complex, 0 to 3 percent slopes	161	4478	361158	d3t8	wy633	1987	1:24000
Shingle-Haverdad association, moist, 0 to 80 percent slopes	256	4379	360996	d3n1	wy633	1987	1:24000
Haverdad-Worthenton complex, 0 to 3 percent slopes	160	3846	361159	d3t9	wy633	1987	1:24000
Absted-Haverdad association, moist, 0 to 6 percent slopes	102	3487	339847	cdmt	wy633	1987	1:24000
Haverdad-Draknab complex, moist, 0 to 3 percent slopes	159	2623	361141	d3sq	wy633	1987	1:24000
Haverdad loam, moist, 0 to 3 percent slopes	155	2469	361144	d3st	wy633	1987	1:24000
Absted-Haverdad, rarely flooded very fine sandy loams, 0 to 6 percent slopes	101	1798	339845	cdmr	wy633	1987	1:24000
Haverdad-Boruff complex, 0 to 6 percent slopes, occasionally flooded	325	1165	361227	d3wh	wy633	1987	1:24000
Haverdad loam, moist, saline, 0 to 3 percent slopes	157	933	361142	d3sr	wy633	1987	1:24000
Haverdad silt loam, saline, 0 to 3 percent slopes	156	570	361143	d3ss	wy633	1987	1:24000
Clarkelen-Haverdad complex, 0 to 3 percent slopes, rarely flooded	649	12	2389975	2yv6y	wy633	1987	1:24000
Haverdad-Boruff complex, 0 to 3 percent slopes, occasionally flooded	285	6282	817620	wfsv	wy705	2003	1:24000
Haverdad clay loam, 0 to 3 percent slopes	284	1131	817626	wft1	wy705	2003	1:24000
Haverdad loam, 0 to 3 percent slopes	151	42	817536	wfq4	wy705	2003	1:24000
Haverdad-Lohmiller complex, 0 to 6 percent slopes, rarely flooded	120	20662	351498	2wlrw	wy709	1983	1:24000
Clarkelen-Bigwinder-Haverdad complex, 0 to 3 percent slopes, rarely flooded	109	13794	351487	2yv79	wy709	1983	1:24000
Haverdad loam, overflow, 0 to 4 percent slopes	228	541	1427846	1jxsk	wy709	1983	1:24000
Lohmiller-Haverdad complex, 1 to 4 percent slopes	240	101	1427897	1jxv6	wy709	1983	1:24000
Haverdad loam, 0 to 3 percent slopes	221	32	361295	d3yp	wy709	1983	1:24000
Haverdad-Clarkelen complex, 0 to 3 percent slopes	156	5585	503021	jwfh	wy713	1986	1:24000
Coaliams-Haverdad complex, 0 to 3 percent slopes	48	9	1414817	1jh78	wy715	1974	1:20000
Clarkelen-Haverdad complex, 0 to 3 percent slopes, rarely flooded	649	13442	1383920	2yv6y	wy719	2013	1:24000
Haverdad, occasionally flooded-Kishona clay loams, 0 to 6 percent slopes	727	10135	1469312	2ztzd	wy719	2013	1:24000
Haverdad, occasionally flooded-Kishona loams, 0 to 3 percent slopes	613	3768	1389329	1hmq2	wy719	2013	1:24000
Shingle-Haverdad, frequently flooded complex, 0 to 80 percent slopes	624	3359	1604042	1qv49	wy719	2013	1:24000
Haverdad loam, 0 to 3 percent slopes, rarely flooded	607	3099	1672817	1t4pv	wy719	2013	1:24000
Absted-Haverdad, rarely flooded very fine sandy loams, 0 to 6 percent slopes	664	545	1674095	1t612	wy719	2013	1:24000
Haverdad-Boruff complex, 0 to 3 percent slopes, occasionally flooded	617	14	1675382	1t7cl	wy719	2013	1:24000
Haverdad-Clarkelen-Kovich, warm, complex, 0 to 3 percent slopes	135	1777	104936	3j61	wy721	1994	1:24000

Map of Series Extent

Approximate geographic distribution of the HAVERDAD 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).