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Bonanza Creek Experimental Forest & Caribou-Poker Creeks Research Watershed

Introduction

Moose in Bonanza Creek Experimental Forest

The Bonanza Creek Experimental Forest and Caribou-Poker Creeks Research Watershed are the only designated forest research facilities in the true boreal forest zone of the United States. Both are on Alaska state land, with Forest Service and university research activities conducted under a long-term lease and cooperative agreement, respectively. Bonanza Creek, located about 20 km southwest of Fairbanks, Alaska, was established in 1963 with about 3,360 ha of upland, interior Alaska boreal forest. In 1969, the forest was enlarged to 5,053 ha to include representative flood-plain forests along the Tanana River. Bonanza Creek lies within the Tanana Valley State Forest, a unit managed by the Alaska Division of Forestry. It is leased to the USDA Forest Service’s Pacific Northwest Research Station for the exclusive purpose of conducting research in forestry. Bonanza Creek was declared a Long-Term Ecological Research (LTER) site by the National Science Foundation in 1987.


Caribou-Poker Creeks is a 10,400-ha upland research site located 45 km north of Fairbanks that is dedicated to research into hydrologic and environmental questions about the discontinuous-permafrost boreal forest of the Yukon-Tanana Upland of central Alaska. In 1969, a cooperative agreement signed by the Interagency Technical Committee for Alaska and the Alaska Department of Natural Resources designated the basin as the Caribou-Poker Creeks Research Watershed. In 1996, the Water and Environmental Research Center of the University of Alaska assumed management of the watershed.


Climate


The climate in interior Alaska is strongly continental, with cold winters and warm, relatively dry summers; it is characterized by drastic seasonal fluctuation in day length (> 21 hours on June 21 and < 3 hours on December 21). Mean annual temperatures in the Tanana Valley area average between -2 and -5 °C. July temperatures average 16.3 °C, whereas in January the average is -23.5 °C. Periods of extreme cold in the vicinity of -40 to -45 °C can occur at any time from late November through February. Daily maximum temperatures occasionally reach 35 to 37 °C in June and July, often with only modest night cooling because of the persisting daylight. The growing season is short (100 days or less).


Annual precipitation in interior Alaska is 250 to 500 mm. About 35 percent of this precipitation falls between October and April as snow. Although precipitation amounts during the growing season may be low, evaporation rates are also low because of the relatively short growing season and cool temperatures. Even so, as much as 75 to 100 percent of the summer precipitation may be lost as evapotranspiration. Snow covers the ground from mid-October until mid- to late April, and maximum accumulation averages 75 to100 cm. Soil temperatures are consistently low.


Soils


In this area of Alaska, soils are uniformly immature and range from cold poorly drained soils with shallow permafrost to warm well-drained soils in the uplands that support mature white spruce communities. Parent material falls into three main categories: (1) bedrock composed of Precambrian schist, (2) thick loess deposits originating from glacial periods, and (3) alluvial deposits in flood plains. Slope and aspect are critical in the formation of permafrost. North-facing slopes are usually underlain by permafrost, contrasting sharply with south-Bonanza Creek Experimental Forest/Caribou-Poker Creeks Research Watershed (Alaska) facing slopes and their warm, well-drained soils. Poorly drained black spruce flats of interior Alaska are also largely underlain by permafrost.


Tree and grassland in winter.

Vegetation


The taiga forest of Alaska consists of a mosaic of forest, grassland, shrubs, bogs, and alpine tundra. The forest is dominated by young stands in various stages of succession; mature stands more than 200 years old are rare due to frequent fires. In areas relatively protected from fires, such as the river flood plains, the active erosion and meandering of the silt-laden, glacially fed rivers results in the active production of newly vegetated silt bars and the rapid erosion of older, mature stands.


Upland forest types range from highly productive aspen, paper birch, and white spruce stands on well-drained, south-facing slopes to permafrost and moss-dominated black spruce forests of low productivity on north-facing slopes, lowlands, and lower slopes. Flood plain forests of balsam poplar and white spruce are productive on recently formed river alluvium where permafrost is absent, but slow-growing black spruce and bogs occupy the older terraces that are underlain by permafrost.


Long-Term Data Bases


There are climate data for both Bonanza Creek and Caribou-Poker Creeks. The Bonanza Creek LTER also has a long-term vegetation data base. There are data for all LTER successional control sites, including tree-growth measurements, litter collections, seedfall counts, seedling establishment; thaw depth (permafrost), and 15- and 30- year records for thaw depth after fire, as well as archived soil samples and archived herbarium specimens and snow-course measurements. All data from the LTER site are cataloged at www.lter.uaf.edu.


Research, Past and Present


Much of the early Forest Service research in Alaska was conducted by scientists from the Pacific Northwest Forest and Range Experiment Station’s Institute of Northern Forestry (INF). Early research on white spruce seed production began in 1958 and continued through 1992. From 1957 until 1966, INF personnel conducted destructive sampling and stem analysis for the development of growth and yield tables for white spruce, aspen, and birch. Both flood plain and upland stands within Bonanza Creek were used extensively. Demonstration plots were established for different silvicultural systems on an upland white spruce site in 1972, and various aspects of natural regeneration (including seedfall, seedling survival, density and growth, nutrient status, and competition) also were evaluated. Sprout and sap production in birch stands has also been studied. Beginning in 1962, INF and the University of Alaska cooperated in studies of the effects of red squirrel foraging on white spruce cone and seed production. This work was later expanded to include the red squirrel response to various silvicultural treatments.


Between 1964 and 1967, nutrient relationships in birch and black spruce stands on north-facing slopes were studied at Bonanza Creek. This work was expanded to include above- and below-ground biomass and nutrient cycling in white spruce and birch stands on slopes of all aspects. Numerous permanent plots have been used to study species composition, successional relationships, and soil temperature fluctuations. Research has also focused on the spruce and Ips beetles, large aspen tortrix, spear-marked black moth, and the larch bud moth. More recently, Bonanza Creek has been the site of studies of flood plain soil moisture dynamics and formation of salt crust on freshly deposited alluvium, forest reestablishment and insect and disease dynamics following wildfire, and tree-species provenance tests.


Research at Caribou-Poker Creeks in recent years has examined the performance of electrical resistivity, ground penetrating radar, and transient electromagnetic surveys to determine subsurface conditions. Hydrologic monitoring has been essential in developing a computer model capable of predicting runoff rates and volumes from watersheds with permafrost distribution ranging from 2 to 53 percent. An experimental oil spill conducted in the mid-1970s has provided critically valuable data demonstrating natural degradation processes following oil spills on thick organic soils and continues to provide information on vegetation recovery and the natural resilience of subarctic forests.


Major Research Accomplishments and Effects on Management


Research at the Bonanza Creek LTER site has contributed substantively to understanding the relationship between “independent” factors and internal ecosystem dynamics in causing successional change in the boreal forest of Alaska. Major findings of the program are that species effects are strong in the boreal forest and successional changes in species composition are not a simple consequence of changes in competitive balance but involve species-driven changes in biogeochemistry and the physical environment. In addition, vertebrate herbivores are a powerful force driving successional change through their effects on plant competitive interactions and biogeochemistry and succession influences exchanges of methane, carbon dioxide, water, and energy in ways that could affect climate.


Collaborators


At these Alaska sites, collaborators have come from the University of Alaska- Fairbanks, National Science Foundation's LTER Program, Alaska Cooperatively Implemented Information Management System, Water and Environmental Research Center, Cold Regions Research and Engineering Laboratory, Tanana Chiefs Conference, Alaska Division of Forestry, Alaska Boreal Forest Council, Alaska Fire Service, Alaska Department of Fish and Game, Arctic Region Supercomputing Center, USDI Geological Survey, Fish and Wildlife Service, and Bureau of Land Management.


Research Opportunities


Research topics at the Bonanza Creek LTER site vary widely, with 30 principal investigators listed in the current proposal.
Lat. 64° 8' N, long. 148° 0' W (BNEF)
Lat. 65° 16' N, long. 147° 5' W (CPCRW)


Contact Information


Bonanza Creek Experimental Forest
USDA Forest Service
Pacific Northwest Research Station
University of Fairbanks Alaska
P.O. Box 756780
Fairbanks, AK 99775-6780
Tel: (907) 474-5881
http://www.fs.fed.us/pnw/exforests/bonanza-creek/index.shtml



1Information has been updated since original publication.


pnw > exforests > Bonanza Creek

USDA Forest Service - Pacific Northwest Research Station
Last Modified:  Monday, 16 December 2013 at 14:18:57 CST


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