Fertilizer N uptake of paddy rice in two soils with different fertility under experimental warming with elevated CO2 |
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Authors: | Hong-Shik Nam Jin-Hyeob Kwak Sang-Sun Lim Woo-Jung Choi Sun-Il Lee Dong-Suk Lee Kwang-Seung Lee Han-Yong Kim Sang-Mo Lee Miwa Matsushima |
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Affiliation: | 1. National Academy of Agricultural Science, Rural Development Administration, Suwon, South Korea 2. Department of Renewable Resources, University of Alberta, Edmonton, AB, Canada 3. Department of Rural & Bio-systems Engineering and Climate Change Research Center for Agriculture and Forest, Chonnam National University, Gwangju, South Korea 4. Department of Applied Plant Science and Climate Change Research Center for Agriculture and Forest, Chonnam National University, Gwangju, South Korea 6. National Instrumentation Center for Environmental Management, Seoul National University, Seoul, 151-742, South Korea 5. Graduate School of Horticulture, Chiba University, Matsudo, Chiba-Ken, Japan
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Abstract: | Background and aims Only limited information is available in the research area on the effect of elevated CO2 concentration ([CO2]) and air temperature (Tair) on the fertilizer N uptake by rice. This study was conducted to investigate changes in rice uptake of N derived from fertilizer (NDFF) and soil (NDFS) as well as fertilizer N uptake efficiency (FUE) with elevated [CO2] and Tair in two soils with different fertility. Methods Rice (Oryza sativa L.) plants were grown with 15N-urea for two growing seasons (2007 in the less fertile and 2008 in the more fertile soil) in temperature gradient chambers under two (ambient and elevated) levels of [CO2] and Tair regimes. At harvest, dry matter (DM) and N uptake amount of rice compartments (root, shoot, and grain) were determined. Results The DM of whole rice increased (P?0.01) with co-elevation of [CO2] and Tair in both years (by 28.0 % in 2007 and by 27.4 % in 2008). The DM in 2008 was greater than that in 2007 by 48.1 to 63.1 % probably due to better soil fertility as well as longer sunshine hours (456 h vs. 568 h). Co-elevation of [CO2] and Tair increased total N uptake, NDFF, and NDFS by 19.4 to 29.1 % in general compared to the ambient conditions. The FUE increased with co-elevation of [CO2] and Tair from 46.5 to 59.5 % in 2007 and from 36.7 to 43.8 % in 2008. Conclusions The projected global warming with elevated [CO2] is expected to increase FUE via enhanced DM accumulation with less increments in the soils that have higher indigenous soil N availabilities. |
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