Download A Biomass Future for the North American Great Plains: Toward by Norman J. Rosenberg PDF

By Norman J. Rosenberg

The North American nice Plains is a huge worldwide breadbasket yet its agriculture is under pressure through drought, warmth, destructive winds, soil erosion and declining flooring water assets. Biomass creation and processing at the Plains might partly fix a perennial vegetative disguise and create employment possibilities. This publication explores the prospect that the ecology and economic system of the Plains zone, and comparable areas, would get advantages from the advent of perennial biomass crops.

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Extra resources for A Biomass Future for the North American Great Plains: Toward Sustainable Land Use and Mitigation of Greenhouse Warming (Advances in Global Change Research)

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1936, Report of the Great Plains Drought Area Committee. Report to President Franklin D. Roosevelt, The White House, Washington, DC, August 27, 1936. Franklin D. Roosevelt Library, Hopkins Papers, Box 13. E. ), chap. 10. Climate Change and US Water Resources, Wiley-Interscience, New York, pp. 223–240. Jenny, 1941, Factors of Soil Formation: A System of Quantitative Pedology, McGraw-Hill, New York, 281 pp. J. ), Encyclopedia of the Great Plains, University of Nebraska Press, Lincoln, Nebraska, pp.

See Color Plates) The Physical Environment 27 such as dunes, steep slopes, and flood plains. Entisols make up about 16% of the world’s ice-free land surface; • Inceptisols are soils of semiarid to humid environments that generally exhibit only moderate degrees of soil weathering and development. Inceptisols have a wide range in characteristics and occur in a wide variety of climates. Inceptisols. make up about 17% of the world’s ice-free land surface; • Aridisols are soils that are too dry for the growth of mesophytic plants (plants living in a temperate environment and receiving average amounts of moisture).

These lands are used for cropping and pasture. 4. 1. Introduction The Great Plains is a region whose climate varies from the arid in northeastern New Mexico to the sub-humid at the eastern borders of Nebraska and Kansas and central Oklahoma and Texas. So it is a region of deficit precipitation, very 28 Chapter 2 Figure 2-7. html) (See Color Plates) The Physical Environment 29 much dependant on its water resources for maintenance of its economy. Its rivers and groundwater resources are described below.

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