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Global environment change and simulated forage quality of wheat II. Water and nitrogen stress
Institution:1. Department of Agrotechnology, Ferdowsi University of Mashhad, Iran & Gorgan University of Agricultural Sciences and Natural Resources, Iran;2. Golestan Agricultural and Natural Resources Research and Education Center, Agricultural Research, Education and Extension Organization (AREEO), Gorgan, Iran;3. Research and Transfer Centre “Sustainable Development & Climate Change Management” (FTZ-NK), Faculty of Life Sciences, Hamburg University of Applied Sciences, Ulmenliet 20, 21033, Hamburg, Germany;4. Faculty of Agriculture and Food Sciences, University of Sarajevo, Bosnia and Herzegovina;5. Department of Production Engineering, Logistics and Applied Computer Science, Faculty of Production and Power Engineering, Agricultural University Kraków, Kraków, Poland;6. Department of Economics and Rural Development, Gembloux Agro-Bio Tech, University of Liège, Gembloux, Belgium;7. Faculty of Environmental Sciences, Czech University of Life Sciences Prague, Prague, Czech Republic;8. Faculty of Environmental Science and Engineering, Babeş-Bolyai University, Cluj-Napoca, Romania
Abstract:Forage crops are frequently subjected to stress conditions resulting from inadequate supplies of water and N. Because forages grown under these stress conditions constitute an important resource in animal agriculture, this study was undertaken to assess possible changes in the nutritive value and productivity of forage crops as a consequence of global environment change. A relatively simple, mechanistic model of wheat was extended to simulate growth and important determinants of feed quality (N], leaf:stem, dry matter digestibility) in an annual, temperate climate C3 forage grass. Weather data for a semiarid region and different levels of applied N were used to examine the response of forage productivity to various levels of water and N availability. Not surprisingly, responses to global environment change were highly dependent on the availability of both water and N. When either resource was available at low levels, production of digestible dry matter was nearly unchanged by elevated CO2] or increased temperature. When compared at equivalent development stages, small increases in forage quality were simulated, mainly because higher temperature resulted in achievement of the initiation of grain fill at an earlier date. As N availability increased, differences in forage characteristics and productivity became more prominent. Elevated ambient CO2] increased vegetative mass, digestible dry matter, and concentration of digestible dry matter but decreased leaf:stem and N]. Increased temperature generally had an effect on forage traits that was opposite to the elevated CO2] response. The combined effects of both factors sometimes cancelled each other, but usually one of the factors was dominant. Negative effects of temperature tended to be aggravated by dry conditions. At crop maturity, positive effects of elevated atmospheric CO2] on forage productivity and quality were severely decreased by nutrient and physiological constraints. These simulations indicate that when forage crops are grown under irrigation in semiarid regions, there may be substantial and complex changes in productivity and feed quality as a consequence of warmer temperature and elevated atmospheric CO2]. Under rainfed conditions, these differences could be quite erratic and virtually unpredictable within the current range of interannual variation in forage productivity and quality.
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