Resin Capsules for On-Site Assessment of Soil Nutrient Supply in Lowland Rice Fields

1997 ◽  
Vol 61 (4) ◽  
pp. 1202-1213 ◽  
Author(s):  
A. Dobermann ◽  
M. F. Pampolino ◽  
M. A. A. Adviento
Author(s):  
A. Dobermann ◽  
R. Nagarajan ◽  
P. Stalin ◽  
P. Mutukhrishnan ◽  
Ma. A. A. Adviento

2012 ◽  
Vol 93 (3) ◽  
pp. 229-232
Author(s):  
Andrew J. Tanentzap ◽  
William G. Lee ◽  
David A. Coomes

2021 ◽  
Author(s):  
Zuonan Cao ◽  
Zhenhuan Guan ◽  
Peter Kühn ◽  
Jinsheng He ◽  
Thomas Scholten

<p>Many species showed that their richness and distribution shifts climate-driven towards higher elevation in Tibetan Plateau. However, vegetation and soil data from alpine grassland elevational gradients are rare (Huang et al., 2018). It is mostly unknown how the "grass-line" will respond to global warming and whether soils play a significant role in the vegetation pattern in high-altitude regions. At a local scale, the growth and distribution of vegetation at its upper limit may depend on nutrient limitation, as shown for treelines from the Himalayas. For example, the limited nutrient supply of soil N, K, Mg, and P becomes more intense with elevation, which declines in nutrient supply spatially coincides with abrupt changes in vegetation composition and growth parameters (Schwab et al., 2016). And low soil nutrient availability could affect tree growth in the Rolwaling Himal, Nepal treeline ecotone (Drollinger et al., 2017). To better understand the interrelationship between soil properties and grass growth at this upper limit, we took random soil samples in 3 altitudes, 3 geomorphic positions with 3 depth increments from Haibei grassland, northern Tibetan Plateau. Soil properties, like texture, bulk density, total C, N, and P fractions, were analyzed and compared to vegetation data.<br>Further, soil and vegetation data from open-top chambers (OTC) experiments to simulate global warming were analyzed better to understand the role of temperature for grass line-shift. The first results show that species composition change with altitude towards grassland plant communities with lower demands for P, which can be compared with the nutrient addition experiment that P addition alone significantly affects species diversity and biomass in the same area (Ren et al., 2016). We suppose that specific combinations of soil properties could limit grass growth and be even more marked than the warming, which controls biodiversity and biomass production in high mountain grassland ecosystems. </p>


Forests ◽  
2020 ◽  
Vol 11 (4) ◽  
pp. 371 ◽  
Author(s):  
Makoto Watanabe ◽  
Hiroka Hiroshima ◽  
Yoshiyuki Kinose ◽  
Shigeaki Okabe ◽  
Takeshi Izuta

Ozone is a phytotoxic gaseous air pollutant and its negative effects on forest production are a major concern. To understand the effects of ozone on forest production, it is important to clarify the nitrogen use efficiency (NUE) for tree growth under elevated ozone conditions, because nitrogen is a primal limiting factor of forest production in many cool-temperate forests. Soil nutrient conditions are considered factors affecting ozone susceptibility of tree growth. Therefore, in the present study, we investigated the effects of ozone on NUE for the growth of Siebold’s beech (Fagus crenata Blume) seedlings grown under different soil nutrient conditions. Seedlings of Siebold’s beech were grown under three gas treatments (charcoal-filtered air or ozone at 1.0 or 1.5 times the ambient concentration) in combination with three soil nutrient conditions (non-fertilised, low-fertilised or high-fertilised) for two growing seasons. Based on the dry mass and nitrogen concentration in each plant organ, we calculated NUE and its components, including nitrogen productivity (NP) and the mean residence time of nitrogen (MRT) during the second growing season. Ozone did not decrease the NUE of the seedlings during the second growing season, whereas leaf level photosynthetic nitrogen use efficiency (PNUE), a component of NP, was decreased by ozone. On the other hand, the soil nutrient supply decreased the NUE of the seedlings. Reductions in both NP and MRT were attributed to the decrease in NUE because of soil nutrient supply, whereas PNUE did not respond to soil nutrient supply. There was no significant interaction of ozone and soil nutrient supply on the NUE, or its components, of the seedlings. Our results indicated that there is a difference in the response between the NUE for individual growth and that of leaf level PNUE of Siebold’s beech seedlings to ozone and soil nutrient supply.


2020 ◽  
Vol 143 ◽  
pp. 107739 ◽  
Author(s):  
Hai-Yan Zhang ◽  
Priscila Goncalves ◽  
Elizabeth Copeland ◽  
Shan-Shan Qi ◽  
Zhi-Cong Dai ◽  
...  

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