Soil Data Explorer - HAGGATT

Official Series Description

Lab Data Summary

Aggregate lab data for the HAGGATT soil series. This aggregation is based on all pedons with a current taxon name of HAGGATT, 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 HAGGATT 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
122	98P0120	S1997IN043006	HAGGATT	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.3880539,-86.0227814

Water Balance

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

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

Competing Series

Soil series competing with HAGGATT 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 HAGGATT 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 HAGGATT 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).

Soil series sharing subgroup-level classification with HAGGATT, 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

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

1. IN-2010-09-24-15 | Owen County -

   Typical pattern of soils and parent materials in the Zanesville-Tulip-Wellston and Crider-Haggatt associations (Soil Survey of Owen County, Indiana).

Map Units

Map units containing HAGGATT 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
Crider-Haggatt silt loams, karst, rolling, eroded	CxmC2	3798	201066	6r70	in019	2001	1:12000
Haggatt-Caneyville complex, karst, hilly, severely eroded	HujD3	2905	201135	6r97	in019	2001	1:12000
Haggatt-Caneyville silt loams, 12 to 25 percent slopes, eroded	HtwD2	2701	201123	6r8v	in019	2001	1:12000
Crider-Haggatt silt loams, 6 to 12 percent slopes, eroded	CxhC2	2390	201067	6r71	in019	2001	1:12000
Haggatt-Caneyville silt loams, karst, hilly, eroded	HuhD2	2251	201124	6r8w	in019	2001	1:12000
Crider-Haggatt complex, karst, rolling, severely eroded	CxnC3	1882	201069	6r73	in019	2001	1:12000
Haggatt-Caneyville complex, 12 to 25 percent slopes, severely eroded	HtzD3	1667	201125	6r8x	in019	2001	1:12000
Knobcreek-Navilleton-Haggatt silt loams, karst, rolling, eroded	KxoC2	1217	198263	6n9l	in019	2001	1:12000
Knobcreek-Haggatt-Caneyville silt loams, karst, hilly, eroded	KxpD2	894	201951	6s4k	in019	2001	1:12000
Crider-Haggatt complex, 6 to 12 percent slopes, severely eroded	CxgC3	653	201068	6r72	in019	2001	1:12000
Knobcreek-Haggatt-Caneyville silt loams, 12 to 25 percent slopes, eroded	KxmE2	471	210555	7233	in019	2001	1:12000
Knobcreek-Haggatt-Caneyville complex, 6 to 12 percent slopes, severely eroded	KxlC3	139	210527	7226	in019	2001	1:12000
Knobcreek-Haggatt-Caneyville complex, 12 to 25 percent slopes, severely eroded	KxlE3	24	210533	722d	in019	2001	1:12000
Haggatt silty clay loam, 12 to 18 percent slopes, severely eroded	HafD3	3768	1652582	1sgn3	in025	1970	1:20000
Haggatt silty clay loam, 6 to 12 percent slopes, severely eroded	HafC3	2414	1652581	1sgn2	in025	1970	1:20000
Haggatt silt loam, 12 to 18 percent slopes, eroded	HarD2	967	1652576	1sgmx	in025	1970	1:20000
Haggatt silt loam, 18 to 25 percent slopes, eroded	HarE2	753	1652577	1sgmy	in025	1970	1:20000
Knobcreek-Haggatt-Caneyville complex, 6 to 12 percent slopes, severely eroded	KxlC3	3088	185239	66rg	in043	2000	1:12000
Knobcreek-Haggatt-Caneyville silt loams, 12 to 25 percent slopes, eroded	KxmE2	3010	185240	66rh	in043	2000	1:12000
Knobcreek-Haggatt-Caneyville complex, 12 to 25 percent slopes, severely eroded	KxlE3	2638	185241	66rj	in043	2000	1:12000
Knobcreek-Navilleton-Haggatt silt loams, karst, rolling, eroded	KxoC2	2208	185242	66rk	in043	2000	1:12000
Knobcreek-Haggatt-Caneyville silt loams, karst, hilly, eroded	KxpD2	2068	185243	66rl	in043	2000	1:12000
Vertrees-Haggatt-Caneyville complex, karst, hilly, severely eroded	VccD3	37755	1678191	1tb96	in061	2007	1:12000
Caneyville-Haggatt-Knobcreek complex, karst, hilly, severely eroded	CbsD3	11346	798308	vspw	in061	2007	1:12000
Knobcreek-Navilleton-Haggatt complex, karst, rolling, severely eroded	KxrC3	9763	1716057	1vlpp	in061	2007	1:12000
Knobcreek-Haggatt-Caneyville complex, karst, hilly, severely eroded	KxsD3	7300	1716058	1vlpq	in061	2007	1:12000
Knobcreek-Haggatt-Caneyville silt loams, karst, hilly, eroded	KxpD2	6094	1585842	1q766	in061	2007	1:12000
Knobcreek-Navilleton-Haggatt silt loams, karst, rolling, eroded	KxoC2	5309	1585841	1q765	in061	2007	1:12000
Caneyville-Haggatt-Knobcreek silt loams, karst, hilly, eroded	CbrD2	5307	775595	v126	in061	2007	1:12000
Knobcreek-Haggatt-Caneyville complex, karst, rolling, severely eroded	KxtC3	5020	780681	v6c8	in061	2007	1:12000
Knobcreek-Haggatt-Caneyville complex, 6 to 12 percent slopes, severely eroded	KxlC3	2297	1585838	1q762	in061	2007	1:12000
Knobcreek-Haggatt-Caneyville silt loams, karst, rolling, eroded	KxtC2	1816	1698565	1v0hf	in061	2007	1:12000
Knobcreek-Haggatt-Caneyville complex, 12 to 25 percent slopes, severely eroded	KxlE3	1784	1585839	1q763	in061	2007	1:12000
Knobcreek-Haggatt-Caneyville silt loams, 12 to 25 percent slopes, eroded	KxmE2	1328	1585840	1q764	in061	2007	1:12000
Caneyville-Haggatt silty clay loams, karst, rolling, very severely eroded, very rocky	CbxD4	1210	1678193	1tb98	in061	2007	1:12000
Haggatt-Caneyville silt loams, 12 to 25 percent slopes, eroded	HcD2	1	975660	11r7x	in077	1982	1:15840
Haggatt silt loam, 12 to 18 percent slopes	HarD	1	1651495	1sfj1	in093	1982	1:15840
Crider-Haggatt silt loams, 6 to 12 percent slopes, eroded	CxhC2	252	1708124	1vbfs	in101	1984	1:15840
Haggatt-Caneyville silt loams, 12 to 25 slopes, eroded	HtwD2	237	1708140	1vbg9	in101	1984	1:15840
Haggatt silty clay loam, 12 to 18 percent slopes, severely eroded	HafD3	19	1442986	1kfjy	in117	1980	1:15840
Haggatt silt loam, 18 to 25 percent slopes, eroded	HarE2	1	1442987	1kfjz	in117	1980	1:15840
Haggatt silt loam, 12 to 18 percent slopes, severely eroded	HarD3	493	166033	5krx	in119	1997	1:12000
Haggatt-Caneyville silt loams, 18 to 25 percent slopes, eroded	HasE2	317	166034	5kry	in119	1997	1:12000
Haggatt silt loam, 12 to 18 percent slopes, eroded	HarD2	125	166032	5krw	in119	1997	1:12000
Ryker silt loam, 6 to 12 percent slopes, eroded	RtcC2	163	535889	kzmr	in123	1997	1:12000

Map of Series Extent

Approximate geographic distribution of the HAGGATT 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).