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Carya glabra

Species of tree

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Carya glabra
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Through Canada, Wood and Massachusetts

Habitat

Native range

The range of pignut hickory covers nearly all of the eastern United States. The species grows in central Florida and northward through North Carolina to southern Massachusetts. It also grows north of the Gulf Coast through Alabama, Mississippi north to Missouri and extreme southeastern Iowa, and the Lower Peninsula of Michigan.

The best development of this species is in the lower Ohio River Basin. It prevails over other species of hickory in the Appalachian forests. Pignut makes up much of the hickory harvested in Kentucky, West Virginia, the Cumberland Mountains of Tennessee, and the hill country of the Ohio Valley.

Pignut hickory is also found in Canada in extreme southern Ontario. It does however have a limited range and is restricted to the Niagara Peninsula, southern Halton Region, the Hamilton area along western Lake Ontario, and southward along the northern shore of Lake Erie and pockets of extreme southwestern Ontario.

Climate

Pignut hickory grows in a humid climate with an average annual precipitation of 760 to 2,030 mm (30 to 80 in) of which 510 to 1,020 mm (20 to 40 in) is rain during the growing season. Average snowfall varies from little to none in the South to 2,540 mm (100 in) or more in the mountains of West Virginia, upstate New York, and western North Carolina (25).

Within the range of pignut hickory, average annual temperatures vary from 7 °C (45 °F) in the north to 21 °C (70 °F) in Florida. Average January temperature varies from −4 to 16 °C (25 to 61 °F) and average July temperature varies from 21 to 27 °C (70 to 81 °F). Extremes of 46 and −30 °C (115 and −22 °F) have been recorded within the range. The growing season varies by latitude and elevation from 140 to 300 days.

Mean annual relative humidity ranges from 70 to 80 percent with small monthly differences; daytime relative humidity often falls below 50% while nighttime humidity approaches 100%.

Mean annual hours of sunshine range from 2,200 to 3,000. Average January sunshine varies from 100 to 200 hours, and July sunshine from 260 to 340 hours. Mean daily solar radiation ranges from 12.57 to 18.86 million J m± (300 to 450 langleys). In January daily radiation varies from 6.28 to 12.57 million J m± (150 to 300 langleys), and in July from 20.95 to 23.04 million J m± (500 to 550 langleys).

According to one classification of climate (20), the range of pignut hickory south of the Ohio River, except for a small area in Florida, is designated as humid, mesothermal. That part of the range lying north of the Ohio River is designated humid, mesothermal. Part of the species range in peninsular Florida is classed as subhumid, mesothermal. Mountains in Pennsylvania, West Virginia, North Carolina, and Tennessee are classed as wet, microthermal, and mountains in South Carolina and Georgia are classed as wet, mesothermal. Throughout its range, precipitation is rated adequate during all seasons.

Soils and topography

Pignut hickory frequently grows on dry ridgetops and sideslopes throughout its range but it is also common on moist sites, particularly in the mountains and Piedmont. In the Great Smoky Mountains pignut hickory has been observed on dry sandy soils at low elevations. Whittaker placed pignut in a submesic class and charted it as ranging up to 1,480 m (4,860 ft)-the hickory with the greatest elevational range in the Great Smoky Mountains. In southwest Virginia, south-facing upper slopes from 975 to 1,050 m (3,199 to 3,445 ft) of Beanfield Mountain are dominated by pignut hickory, northern red oak Quercus rubra), and white oak (Q. alba). This site is the most xeric habitat on the mountain because of high insolation, 70 percent slopes, and medium- to coarse-textured soils derived from Clinch sandstone. Mid-elevation slopes from 800 to 975 m (2,625 to 3,199 ft) are dominated by chestnut oak (Q. prinus), northern red oak, and pignut hickory and coincide with three shale formations.

The range of pignut hickory encompasses 7 orders, 12 suborders, and 22 great groups of soils. About two-thirds of the species range is dominated by Ultisols, which are low in bases and have subsurface horizons of clay accumulation. They are usually moist but are dry during part of the warm season. Udults is the dominant suborder and Hapludults and Paleudults are the dominant great groups. These soils are derived from a variety of parent materials-sedimentary and metamorphic rocks, glacial till, and in places varying thickness of loess-which vary in age from Precambrian to Quaternary.

A wide range of soil fertility exists as evidenced by soil orders-Alfisols and Mollisols which are medium to high in base saturation to Ultisols which are low in base saturation. Pignut hickory responds to increases in soil nitrogen similarly to American beech (Fagus grandifolia), sugar maple (Acer saccharum), and blackgum (Nyssa sylvatica). These species are rated as intermediate in nitrogen deficiency tolerance and consequently are able to grow with lower levels of nitrogen than are required by "nitrogen- demanding" white ash (Fraxinus americana), yellow-poplar (Liriodendron tulipifera), and American basswood (Tilia americana). Hickories are considered "soil improvers" because their leaves have a relatively high calcium content.

Associated forest cover

Hickories are consistently present in the broad eastern upland climax forest association commonly called oak-hickory, but they are not generally abundant. Locally, hickories may make up to 20 to 30 percent of stand basal area, particularly in slope and cove forests below the escarpment of the Cumberland Plateau and in second-growth forests in the Cumberland Mountains, especially on benches. It has been hypothesized that hickory will replace chestnut (Castanea dentata) killed by the blight (Cryphonectria parasitica) in the Appalachian Highlands. On Beanfield Mountain in Giles County, Virginia, the former chestnut-oak complex has changed to an oak-hickory association over a period of 50 years. This association is dominated by pignut hickory with an importance value of 41.0 (maximum value = 300), northern red oak (36.0), and chestnut oak (25.0). White oak, red maple (Acer rubrum), and sugar maple are subdominant species.

Pignut hickory is an associated species in 20 of the 90 forest cover types listed by the Society of American Foresters for the eastern United States (6):

Northern forest region

53 White Pine-Chestnut Oak

Central forest region

40 Post Oak-Blackjack Oak
44 Chestnut Oak
45 Pitch Pine
46 Eastern Redcedar
52 White Oak-Black Oak-Northern Red Oak
53 White Oak
55 Northern Red Oak
57 Yellow-Poplar-Tulip tree
59 Yellow-Poplar-White Oak-Northern Red Oak
64 Sassafras-Persimmon
110 Black Oak

Southern forest region

75 Shortleaf Pine
76 Shortleaf Pine-Oak
78 Virginia Pine-Oak
79 Virginia Pine
80 Loblolly Pine-Shortleaf Pine
81 Loblolly Pine
82 Loblolly Pine-Hardwood
83 Longleaf Pine-Slash Pine

Because the range of pignut hickory is so extensive, it is not feasible to list the associated trees, shrubs, herbs, and grasses, which vary according to elevation, topographic conditions, edaphic features, and geographic locality.

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