by R. Samson1, P. Girouard2, j. OmieIan3 and J. Henning4
1Executive Director and 3 Research Scientist, Resource Efficient Agricultural Production (REAP) Canada, Box 125, Ste. Anne de Bellevue, Quebec, Canada H9X 3V9
2 Graduate Student and 4Associate Professor of Agricultural Economics, Macdonald Campus of McGill University, Ste. Anne de Bellevue, Quebec, Canada H9X 3V9
Increased research on C3 and C4 perennial biomass crops is generating a significant amount of information on the potential of these feedstocks to produce large quantities of low cost biomass. In many parts of North America it appears that both C3 and C4 species are limited by water availability particularly on marginal soils. In much of North America, rainfall is exceeded by evaporation. High transpiration rates by fast growing trees and rainfall interception by the canopy appear to indicate that this can further exacerbate the problem of water availability. C4 perennial grasses appear to have distinct advantages over C3 species planted in monoculture systems particularly on marginal soils. C4 grasses historically predominated over much of the land that is now available for biomass production because of their adaptation to low humidity environments and periods of low soil moisture. The planting of short rotation forestry (SRF) species in an energy agroforestry system is proposed as an alternative production strategy which could potentially alleviate many of the problems associated with SRF monocultures. Energy agroforestry would be complementary to both production of conventional farm crops and C4 perennial biomass crops because of beneficial micro climatic effects.
Studies involving fast growing plantations of trees have been ongoing since the early 1970's in North America by the United States Department of Energy and Natural Resources Canada. More recently herbaceous feedstocks have received increased attention for their biomass production potential. However, few attempts have been made to understand climatic influences on the choice of biomass feedstocks or the potential to integrate production of woody and herbaceous biomass crops. This paper will discuss the major constraints to monoculture production of short rotation forestry (SRF) and warm season grasses and outline the potential advantages of an integrated production of the two feedstocks. It is believed that a better understanding of the native vegetation of North America and how climatic conditions influenced its development will help biomass scientists understand the choice of biomass feedstocks and strategies to modify the climatic conditions to favour biomass production.
Crop production strategies need to be developed which are as efficient as possible in capturing sunlight (solar energy) and storing it in plants (solar battery). Desirable characteristics for energy feedstocks include:
We know that to achieve these objectives several issues must be considered:
Based on these criteria, the fastest, most resource efficient crops to grow would be perennial C4 grasses. Since 1986 the US Department of Energy (DOE) has extensively evaluated herbaceous and woody biomass crops for biomass production. It is not surprising then that the lowest cost feedstock production that has been achieved in North America has been with switchgrass (Panicum virgatum), a C4 prairie grass. Several studies have estimated production costs below US$30.00/tonne (Sladden et al., 1991; Parrish et al., 1990).
Recent reports by European biomass scientists have further highlighted the significant yield and physiological advantages that C4 grasses hold over C3 species (i.e. cool season grasses or fast growing trees) for biomass production (Jones et al. 1987; Long et al. 1990; Stander, 1989; Rutherford and Heath, 1992). As a result of a number of these reports and promising early biomass yields from C4 species, much of the current research in Europe is now evaluating the perennial C4 grass Miscanthus and the annual C4 species sweet sorghum.
American ecologists early in the 19th century demonstrated that water relations had a powerful influence on the distribution of plants. Most authors have credited much of the development of the concept to Transeau (in Stuckey, 1981) who in 1905 wrote:
" Investigation shows that forests, grasslands and deserts are arranged about certain centers, which owe their positions on the continent mainly to climatic causes. That such centers cannot be correlated with the distribution of heat or rainfall alone is evidenced by examination of the monthly, seasonal and annual distribution of these elements.
The fact that so large a part of early adaptations shown by plants are more or less directly connected with transpiration, led the writer to construct a map (see figure 2.) combining the figures for rainfall and evaporation. The amount of evaporation depends upon the temperature of the evaporating surface, the relative humidity of the air and the velocity of the wind. Therefore if we combine the figures for rainfall and evaporation we have a number which will represent at least four climatic factors, that must powerfully influence the water relations and distributions of plants.
The Great Plains are marked by an amount of rainfall equal to 20-60 percent of the evaporation. Where the ratio rises to between 60 and 80 percent, the prairie region, where dense forests are confined to the river bottoms, is indicated. The region where "open forests", "oak openings" and "groves" occur on the uplands and dense forests on the low grounds, is indicated by the 80-100% ratios.
The two maps (Figure 1 and Figure 2) that originated from Transeau's work provide a general indication of how vegetation in North America evolved as a result of climatic conditions. Biomass scientists need to understand the native vegetation and climatic conditions of an area to more effectively understand constraints to biomass production. Few biomass scientists may realize that a prairie peninsula (figure 2) once extended from the North Central region of the United States into the northeastern States of Ohio and Michigan and that low soil moisture periods combined with low humidity were among the primary reasons that this ecosystem evolved. The information provided by Transeau's search for an explanation for the prairie peninsula in North America may prove invaluable for scientists looking to understand ecological constraints to maximizing biomass production. For example, many North American (SRF) researchers working in unirrigated monocultures frequently find that low biomass yields are obtained in the areas where the rainfall to evaporation ratio is lower than 100%. Even in areas where the natural landscape has a rainfall to evaporation ratio from 100150%, the yield potential of SRF systems may be water limited because rapid accumulation of biomass increases water loss through transpiration.
Figure 1. Map of eastern United States showing the ratio of rainfall to evaporation in percentages in different regions; prairie region is the 60 percent to100 percent ratio.
Figure 2. Map of north central United States showing peninsula-like projection of prairie vegetation between the shortgrass region and the forested areas at the time of the "Xerothermic period" as viewed by Transeau ( Stuckey, 1981)
Preliminary Assessment of Barriers to SRF Productivity
The low water use efficiency of SRF systems may be the primary reason that yields have not increased when researchers have left small plots and gone to field scale conditions. A summary of large plot and field scale studies (unirrigated sites with borders) from a recent International Energy Agency (IEA) publication indicates current yields being obtained (Table 1).
Europe |
Species |
Yield (ODT/ha/yr) |
Austria |
Willows |
10.5 |
Sweden |
Willows |
11 |
England |
Willows & poplars |
6-11 |
Denmark |
Willows |
8.1 |
USA |
||
Pennsylvania |
Poplars |
10.4 |
Wisconsin |
Poplars |
7.5 |
Washington |
Poplars |
15.1 |
- ODT = Oven Dry Tonne
France |
Poplars |
7.9 ODT/ha |
Auclair and Bouvarel, 1992 |
Ontario, Canada |
Poplars |
2-3 ODT/ha |
Hendry, 1990 |
The Washington study was the only study to have average yields above 11 ODT/ha. This was performed in a high rainfall area of the Pacific Northwest of the United States. If this study is observed as an anomaly for North America (because of the area's unique climatic conditions relative to the rest of North America), it appears that most field scale yields are in the range of 7-11 ODT/ha. This would agree with Hansen (1988), in his review of SRIC (Short Rotation Intensive Culture) yields, who states 7-11 t/ha as a reasonable estimate of potential SRIC field yields.
The problem of low water use efficiency by the trees in field scale plantations has been identified by several researchers (Dickmann et al., 1992; Grip et al., 1989; Persson and Jansson, 1989; Halldin and Lindroth, 1989). In some areas in Sweden where plantings have been made on bogs, willows have lowered the water table (Persson, 1989). A water balance study in Sweden which simulated a production of 12 t/ha indicated an evaporation of 526 mm, of which 375 mm was transpiration, 56 mm interception and 95 mm soil evaporation. This rate of evaporation was 22% higher than the Penman open water evaporation rate of 430 mm (Grip et al., 1989). Several other Swedish studies have also indicated evaporation rates of SRF systems being 10-50% higher than the potential evaporation by the Penman formula (Persson and Jansson, 1988; Halldin and Lindroth, 1989). It should not be surprising that water availability is proving to be a primary factor limiting yield for high biomass producing systems. Forage scientists have demonstrated that biomass production is water limited for C3 and C4 grasses on marginal sites in northeastern North America (Stout et al., 1988; Stout, 1992), and that forage productivity Of C3 grasses is a good predictor of SRF yields on a site (Wells and Fribourg, 1992). While average rainfall in northeastern North America may be similar to that of Sweden, the intensity of rainfall (frequent storms resulting in higher runoff) and the more continental climate of North America (lower relative humidity), suggest that the moisture use problem would be exacerbated in North America for SRF, particularly on marginal soils (due to low water holding capacity), The low water use efficiency of monoculture plantations of willows or poplars (C3 species) indicates that the real yield potential for SRF in most of North America is only about 1/2 of that required for economic production, 23 t/ha (Kenney et al., 1991). Yields of 7-11 ODT/ha would put biomass costs in the range of US$ 65-85/ tonne (Turhollow, 1992). Thus, an alternative to monoculture SRF systems needs to be developed if plantation forestry is to have a viable energy future in North America, since plantations using irrigation systems are not an option (economically or ecologically) for energy production. The agronomic and economic problems with the monoculture SRF include:
Most land suitable for biomass production from plantations in North America has a rainfall to evaporation ratios of 50-110% (Figure 1). The prairie region, found in the 60-100% rainfall/evaporation area, occupies a major portion of this land base. The native prairie grasses that were dominant in this area were the C4 perennial grasses. Among the most common were big bluestem (Andropogon gerardii little bluestem (Schizachyrium scoparium), Indiangrass (Sorghastrum nutans), switchgrass (Panicum virgatum) and prairie cordgrass (Spartina pectinata) (Weaver and Fitzpatrick, 1934). These species have all shown potential to produce biomass yields greater than 10 t/ha on unirrigated sites (Stubbendieck and Nielsen, 1989; Gould and Dexter, 1986; USDA, 1991). The most thoroughly researched species has been switchgrass. It has many desirable characteristics for biomass production including:
Several other prairie species have also shown potential to produce biomass yields as high or higher than the tallgrass prairie species, particularly outside of the main prairie region. Two of the more promising species are prairie sandreed (Calamovilfa longifolia) and Eastern Gamagrass (Tripsacum dactyloides) which have performed well in biomass trials in the Northern US Great Plains (USDA, 1989) and Southern Illinois respectively (Kaiser, 1989). The native range of these plants compared to that of switchgrass give an indication that they may be as well or better adapted to these particular areas than switchgrass. (Figure 3)
Many of the problems inherent in the SRF system may be reduced or eliminated if an agroforestry approach to energy production is taken. This approach to using trees for energy production has been suggested by others including Newman et al. (1990), Soltner (1991) and Ronneberg (1992). The trees grown in a SRF production system would be used as windbreaks on high value land in order to protect adjacent agricultural crops. The main reasons why an agroforestry approach may be more successful in North America than the monoculture plantation concept are the following:
1) by limiting the plantation to at most a few rows of trees, the availability of sunlight and water would be increased thereby improving tree productivity; (2) compared to conventional windbreaks which are harvested after 25-35 years for timber, SRF windbreaks for energy would make it possible to get a first return after 5 years. The trees would be seen as an asset and not occupiers of valuable crop land; (3) while the reduced competition from the adjacent agricultural crops would benefit the trees, the crops would also benefit from the trees. The benefits of windbreaks have been well documented and include reduced wind speed, increased humidity levels, higher day time temperatures, higher soil moisture, reduced wind and water erosion and increased snow trapping (reviewed by Kort, 1988). (4) in most instances where short rotation windbreaks would be grown in conjunction with field crops, they probably would not need to be fertilized as most farmers tend to overfertilize their crops. The deep root system of the trees would help to recycle nutrients lost in the deepest layers of the soil.
Regarding crop yields, studies have indicated that perennial forage crops (alfalfa and mixed hay) are highly responsive to windbreaks (Kort, 1988). Establishment of windbreaks could potentially have a very beneficial effect on C4 grass growth, particularly in its northern range, because of their ability to reduce the chilling effect of high winds and increase daytime temperatures. Thus, systems could be developed where fast growing trees would be planted in windbreaks while a C4 grass such as switchgrass would be grown in between. Those systems would be entirely dedicated to energy production. Because perennial grasses such as switchgrass can be grown effectively on marginal agricultural land, those systems would also help to take out of production either temporarily or permanently land that cannot sustain annual field cropping. In this case, the trees will probably have to be harvested at longer intervals due to a slower growth rate. However, the lower land cost of those marginal soils should compensate for the longer rotation.
Finally, because SRF harvesting technologies are not well developed, trees planted in windbreaks could be harvested using a chain saw and a tractor pulled wood chipper. One two row design of this simplified energy agroforestry scheme has been proposed by Soltner (1991) (figure 4). This system would enable at least one row to remain as a windbreak while the other row was harvested or in early coppice regrowth. REAP-Canada is currently assessing this approach to energy agroforestry using combinations of willows, poplars and black locusts in an on-farm research program in Central Canada. The combination of one row of black locust with a row of poplar or willow may enable an opportunity to reduce/ eliminate the competition problems that have sometimes been reported with legume/ non-legume tree mixtures in block plantings (Heilman and Stettler, 1985; Heilman, 1989) and the need for N fertilization.
Figure 4. Two row windbreak system with two different species and harvest cycles (Soltner, 1991)
If biomass production systems are to advance significantly in achieving the goal of low cost and abundant biomass, a greater understanding, of ecological and physiological processes needs to be achieved. Much of the land base in North America that is available for biomass production has significant moisture limitations. C4 grasses have well developed characteristics for optimizing growth under these conditions compared to C3 species. The best opportunity to use fast growing trees for biomass production appears to lie with their application in agroforestry systems. Energy production in the form of windbreaks would enable an optimization of growth of fast growing trees while complementing production of traditional farm crops or C4 perennial biomass energy crops. The production of "green energy" from biomass can only be realized if an ecological approach to biomass production is taken.
Auclair, D. and L. Bouvarel. 1992. Influence of spacing and short rotations on Populus trichocarpa x deltoides coppice. Can J. For. Res. 22: 541- 548.
Balasko, J.A., D.M. Burner and W.V. Thayne. 1984. Yield and quality of switchgrass grown without soil amendments. Agron. J. 76: 204-208.
Beadle, C.L. and S.P. Long. 1985. Photosynthesis- is it limiting to biomass production. Biomass. 8: 119-168.
Brown, R.H. 1985. Growth Of C3 and C4 grasses under low N levels. Crop Sci. 25: 954-957.
Cherney, J.H., K.D. Johnson, J.J. Volenec and K.S. Anliker. 1988. Chemical composition of herbaceous grass and legume species grown for maximum biomass production. Biomass. 17: 215-233.
Clark, F.E. 1977. Internal cycling of nitrogen in shortgrass prairie. Ecology 58: 1322-1333.
Dickmann, D.I., Z. Liu, P. Nguyen and K. Pregitzer. 1992. Photosynthesis, water relations, and growth of two hybrid Populus genotypes during a severe drought. Can. J. For. Res. 22: 1094-1106.
Faix,J.J., C.J. Kaiser, F.C. Hinds. 1980. "Quality, yield and survival of Asiatic bluestems and an eastern gamagrass in southern Illinois". J. of Range Management 33: 388-390.
Gould, J.M. and L.B. Dexter. 1986. Warm season grasses-new agricultural crop for the cornbelt. p. 235-238. In G.K. Clambey and R.H. Pemble. (eds.) Proceedings of the Ninth North American Prairie Conference. Tri-College Center for Environmental Studies, Moorhead, Minnesota. 264 p.
Grip, H., S. Halldin and A. Lindroth. 1989. Water use by intensively cultivated willow using estimated stomatal parameter values. Hydrological processes 3: 51-63.
Halldin, S. and A. Lindroth. 1989. Water use by willow in southern Sweden. Estimation of Areal Evapotranspiration. Proc. of a workshop held in Vancouver, B.C. Canada, August 1987. IAHS Publ. no. 177.
Hansen, E.A. 1988. SRIC yields: A look to the future. IN Lothner, D.C., Bradley, D.P. and Gambles, R.L. (eds.) Proceedings of the IEA/BA Task 11 Workshop: Economic Evaluations of Short Rotation Biomass Energy Systems. Duluth, USA. August 11-13, 1987. IEA/BA Information Report 88-2 pp. 197-207.
Heilman,P.E. 1990. Growth and N status of Populus in mixture with red alder on recent volcanic mudflow from Mount Saint Helens. Can. J. For. Res. 20: 84-90.
Heilman, P.E. and R.F. Stettler. 1985. Mixed, short rotation culture of red alder and black cottonwood: growth, coppicing, nitrogen fixation and allelopathy. Forest Science 31: 607-616.
Hendry, J. 1990. Hybrid poplar harvest in Eastern Ontario. Poplar Council of Canada Newsletter, June 1990: 12.
Hetrick, B.A.D., D.G. Kitt, and G.T. Wilson. 1988. Mycorrhizal dependence and growth habit of warm-season and cool-season tallgrass prairie plants. Can. J. Bot. 66: 1376-1380.
Jacobson, E.T., D.A. Tober, R.J. Hass and D.C. Darris. 1986. The performance of selected cultivars of warm season grasses in the northern prairie and plain states. p. 215-221. In G.K. Clambey and R.H. Pemble. (eds.) Proceedings of the Ninth North American Prairie Conference. Tri-College Center for Environmental Studies, Moorhead, Minnesota. 264 p.
Jones, M.B., S.P. Long and S.F. McNally. 1987. The potential productivity Of C4 cordgrasses and galingale for low input biomass production in Europe. In G. Grassi, B. Delman, J.F. Molle, and H. Zibetta. Biomass for Energy and Industry. Elsevier Applied Sciences, London p. 106 -110.
Jung, G.A., J.A. Shaffer and W.L. Stout. 1988. Switchgrass and big bluestem response to amendments on strongly acid soil. Agron. J. 80: 669-676.
Jung, G.A., J.A Shaffer, W.L. Stout and M.T. Panciera. 1990. Warm season grass diversity in yield, plant morphology, and nitrogen concentration and removal in the Northeastern USA. Agron. J. 82: 21-26.
Kaiser, C.J. 1989. " C4 grass with legumes: an energy efficient biomass system". In Proc. XVI International Grassland Congress. Nice, France. pp. 457-458.
Kenney, W.A., R.L. Gambles, and L. Zuffa, 1991. Faculty of Forestry, University of Toronto, Economics and Yields of Energy Plantations: Status and Potential. DSS Contract No. 23440-0-9016/01 -SZ. Efficiency and Alternative Energy Branch, Energy Mines and Resources Canada, Ottawa, Ontario. (177 pp.)
Kort, J. 1988. Benefits of windbreaks to field and forage crops. Agric. Ecosys. Environ. 22/23: 165-190.
Ledin, S. and A. Alriksson, 1992. Handbook on How to Grow Short Rotation Forests. Swedish University of Agricultural Sciences, Section of Short Rotation Forestry. Uppsala, Sweden.
Long, S.P., L. Potter, M.J. Bingham and C.M. Stirling. 1990. An analysis of limitations to the production of C4 perennial grasses as ligno-cellulosic biomass crops, with reference to trials in E. England. In Grassi, G., G. Gosse, and G. dos Santos, Biomass for Energy and Industry, 5th European Conference., Vol. 1. Policy, Environment, Production and Harvesting, Elsevier Applied Science, London. p. 1235-1241.
Morris, R.J., R.H. Fox and G.A. Jung. 1982. Growth, P uptake, and quality of warm & cool season grasses on a low available P soil. Agron. J. 74: 125-129.
Newman, S.M., J. Park, J. Wainwright, P. Oliver, J.M. Acworth and N. Hutton. "Tree Productivity, Economic and Light Use Efficiency of Poplar Silvoarable Systems for Energy". 5th European Conference on Biomass for Energy and Environment, Agriculture and Industry. 1990. p. 176-180.
Parrish, D.J., D.D. Wolf, W.L. Daniels, D.H. Vaugham and J.S. Cundiff. 1990. Perennial species for optimum production of biomass in the Piedmont. Oak Ridge National Laboratory. ORNL./Sub/85-27413/5. Persson, G. 1989. Energy forest water balance on a raised bog. Scand. J. For. Res. 4: 29-39.
Persson, G. and P. Jansson. 1989. Simulated water balance of a willow stand on clay soil. p. 147-162. In K.L. Perttu and P.J. Kowalik (eds.) Modelling of Energy Forestry, Water Relations and Economics: Simulation Monographs 30, Pudoc, Wageningen.
Ramunda, R.A., C.M. Tate and T.R. Seastedt. 1992. "Effects of tallgrass prairie vegetation on the concentrations and seasonality of nitrate-nitrogen in soil water and streams". IN D.S. Smith and C.A. Jacobs. (eds.) Proceedings of the twelve North American Prairie Conference. University of Northern Iowa, Cedar Falls, Iowa. 218 pages.
Ronneberg, R. 1992. The Hedgerow Project: A review of the Literature. Published by the Hedgerow Foundation. Forest Resource Center, Lanesboro, Minnesota. 43 pages.
Rutherford, 1. and M.C. Heath. 1992. The Potential of Miscanthus as a Fuel Crop. ETSU B 1354. Final Report to the Department of Trade and Industry. Great Britain. 123 pages.
Sharpley, A.N. and S.J. Smith. 1991. "Effects of cover crops on surface water quality". IN W.L. Hargrove, Cover Crops for Clean Water. Soil and Water Conservation Society, Ankeny Iowa. 198 pages.
Sladden, S.E., D.I. Bransby and G.E. Aitken. 1991. Biomass yield, composition and production costs for eight switchgrass varieties in Alabama. Biomass and Bioenergy 1(2): 119-122.
Smith, D.K. and S.B. Greenfield. 1979. Distribution of chemical constituents among shoot parts of timothy and switchgrass at anthesis. J. Plant Nutrition 1: 81-89.
Soltner, D. 1991. Planter des Haies. Collection Sciences et Techniques Agricoles, Le Clos Lorelle, Ste Gemmes sur Loire, France. 207 pages.
Stander, W. 1989. Determination of the Highest Biomass Producing Plant Genera (C4Grasses) of the World for Temperate Climates, Assessment Study for the Commission of the European Communities, Munich, Germany. 74 p.
Stout, W.L. 1992. "Water-Use Efficiency of Grasses as Affected by Soil, Nitrogen, and Temperature". Soil Sci. Soc. Am. J. 56: 897-902.
Stout, W.L., G.A Jung and J. A Shaffer. 1988. Effects of soil and nitrogen on water use efficiency of tall fescue and switchgrass under humid conditions. Soil Sci. Soc. Amer. J. 52: 429-434.
Stubbendieck, J., S.L. Hatch, and C.H. Butterfield. 1992. North American Range Plants. University of Nebraska Press, Lincoln, Nebraska. 493 p.
Stubbendieck, J. and C.A. Nielsen. 1989. Influence of harvest and nitrogen fertilizer on four warm season grasses. p. 139-142. In T.B. Bragg and J. Stubbendieck (eds.) Proceedings of the Eleventh North American Prairie Conference, University of Nebraska Prining, Lincoln. 292 p.
Stuckey, R.L. 1981. "Origin and Development of the Concept of the Prairie Peninsula". Proceedings of the 6th North American Prairie Conference. Ohio Biol. Surv. Biol. Notes No. 15. p. 4.
Thomas, E.D. and R.L. Lucey. 1987. Warm season grasses in northern New York. Proc. 1987 Amer. Forage & Grass. Conf. p. 239-243.
Turhollow, A. 1992. "Feedstocks for Ethanol Production in the United States". IN Ethanol Feedstock Meeting, April 15, 1992 . Ottawa, Ontario. Canada Center for Mineral and Energy Technology (CANMET). pp. 3-21.
USDA, 1989. Technical Report 1988-1989. Bismarck Plant Materials Center. USDA, Soil Conservation Service, Bismarck, North Dakota. 180 p.
USDA. 1991. 1991 Annual Report. Big Flats Plant Material Center, Big Flats, New York.
Weaver, J.E. and R.W. Darland. 1949. Soil-root relationships of certain native grasses.