Nitrogen fixation and N transfer from peanut to rice cultivated in aerobic soil in an intercropping system and its effect on soil N fertility

The novel cultivation of paddy rice in aerobic soil reveals the great potential not only for water-saving agriculture, but also for rice intercropping with legumes and both are important for the development of sustainable agriculture. A two-year field experiment was carried out to investigate the yield advantage of intercropping peanut (Arachis hypogaea L., Zhenyuanza 9102) and rice (Oryza sativa L., Wuyujing 99-15) in aerobic soil, and its effect on soil nitrogen (N) fertility. A pot experiment was also conducted to examine the N₂-fixation by peanut and N transfer from peanut to rice at three N fertilizer application rates, i.e., 15, 75 and 150 kg N ha^–1 using a ¹⁵N isotope dilution method. The results showed that the relative advantage of intercropping, expressed as land equivalent ratio (LER), was 1.41 in 2001 and 1.36 in 2002. Both area-adjusted yield and N content of rice were significantly increased in the intercropping system while those of peanut were not significantly different between intercropping and monocropping systems. The yields of rice grain and peanut, for example, were increased by 29–37% and 4–7% in the intercropping system when compared to the crop grown in the monocropping system. The intercropping advantage was mainly due to the sparing effect of soil inorganic N contributed by the peanut. This result was proved by the higher soil mineral N concentration under peanut monocropping and intercropping than under the rice monocropping system.%Ndfa (nitrogen derived from atmosphere) by peanut was 72.8, 56.5 and 35.4% under monocropping and 76.1, 53.3 and 50.7% under the intercropping system at N fertilizer application rates of 15, 75 and 150 kg ha^–1, respectively. The ¹⁵N-based estimates of N transfer from peanut (%NTFL) was 12.2, 9.2 and 6.2% at the three N fertilizer application rates. N transferred from peanut accounted for 11.9, 6.4 and 5.5% of the total N accumulated in the rice plants in intercropping at the same three N fertilizer application rates, suggesting that the transferred N from peanut in the intercropping system made a contribution to the N nutrition of rice, especially in low-N soil.     

Identification of Slow Motions in the Reduced Recombinant High-potential Iron Sulfur Protein I (HiPIP I) from Ectothiorhodospira Halophila via 15N Rotating-frame NMR Relaxation Measurements

Rotating-frame 15N relaxation rate (R1) NMR experiments have been performed in order to study the dynamic behavior of the reduced recombinant high-potential iron-sulfur protein iso I (HiPIP I) from Ectothiorhodospira halophila, in the s to ms time range. Measurements of R1 were performed as a function of the effective spin-lock magnetic field amplitude by using both on and off-resonance radio frequency irradiation. The two data sets provided consistent results and were fit globally in order to identify possible exchange processes in an external loop of the reduced HiPIP I. The loop consists of residues 43-45 and the correlation time of the exchange process was determined to be 50 ± 8 s for the backbone nitrogen of Gln 44.     

抑制剂及其组合对尿素15N在小麦土壤系统中的行为和归宿的影响

应用加有脲酶抑制剂(HQ)、硝化抑制剂(DCD)及其组合的标记尿素进行春小麦盆栽试验.结果表明,在生长季节结束时,小麦回收,土壤残留和损失的肥料N各占施入N量的17.65～23.69%、43.72～56.32%和19.99～36.77%.其中,与单施尿素相比,两种抑制剂配合使用处理的肥料N总回收率高16.78%,小麦回收高5.96%.施用氮肥对籽粒贡献最大,占吸收肥料N量43.3～62.0%.     

Effect of Heat Shock on Intracellular Calcium Mobilization in Neuroblastoma × Glioma Hybrid Cells

Abstract: The effect of heat shock on agonist-stimulated intracellular Ca²⁺ mobilization and the expression of heat shock protein 72 (hsp72) in neuroblastoma × glioma hybrid cells (NG 108–15 cells) were examined. Hsp72 was expressed at 6 h after heat shock (42.5°C, 2 h), reached a maximum at 12 h, and decreased thereafter. Bradykinin-induced [Ca²⁺], rise was attenuated to 28% of control by heat shock at 2 h after heat shock, and reversion to the control level was seen 12 h later. When the cells were treated with quercetin or antisense oligodeoxyribonucleotide against hsp72 cDNA, the synthesis of hsp72 was not induced by heat shock, whereas bradykinin-induced [Ca²⁺]_i rise was abolished and the [Ca²⁺]_i rise was not restored. Recovery from this stressed condition was evident when cells were stimulated by the Ca²⁺-ATPase inhibitor thapsigargin, even in the presence of either quercetin or antisense oligodeoxyribonucleotide. Inositol 1,4,5-trisphosphate (IP₃) production was not altered by heat shock at 12 h after heat shock, whereas IP₃ receptor binding activity was reduced to 45.3%. In the presence of quercetin or antisense oligodeoxyribonucleotide, IP₃ receptor binding activity decreased and reached 27.2% of the control 12 h after heat shock. Our working thesis is that heat shock transiently suppresses the IPs-mediated intracellular Ca²⁺ signal transduction system and that hsp72 is involved in the recovery of bradykinin-induced [Ca²⁺]_i rise.     

The effect of root temperature on the induction of nitrate reductase activities and nitrogen uptake rates in arctic plant species

We investigated whether six arctic plant species have the potential to induce nitrate reductase (NR) activity when exposed to NO₃ ^--nitrogen under controlled environment conditions, using an in vivo assay that uses the rate of NO₂ ^--accumulation to estimate potential NR activity. We also assessed the effect of low root temperatures on NR activity, growth and nitrogen uptake (using ¹⁵N applications) in two of the selected species. Five of the six species (Cerastium alpinum, Dryas intergrifolia, Oxyria digyna, Saxifraga cernua and Salix arctica) were capable of inducing NR activity when exposed to solutions containing 0.5 mM NO₃ ^- at 20°C for 10 days. Although in vivo NR activity was not induced in Saxifraga oppositifolia under controlled conditions, we conclude that it was capable of growing successfully on NO₃ ^-, due to the presence of moderate rates of NR activity observed in both NH₄ ⁺-grown and NO₃ ^--treated plants. Exposure of O. digyna and D. integrifolia to 3°C root temperatures for two weeks, with the shoots kept at 20°C, resulted in root and leaf NR activity rates of NO₃ ^--treated plants being reduced to rates exhibited by NH₄ ⁺-grown plants. Although these decreases in NR in both species appeared to be due to limitations in NO₃ ^--uptake and growth rate (rather than direct low-temperature inhibition of NR synthesis per se), direct low-temperature inhibition of root NR synthesis could not be ruled out. In contrast to the temperature insensitivity of NH₄ ⁺ uptake in D. integrifolia, NO₃ ^--uptake in D. integrifolia was inhibited by low root temperatures. We conclude that the selected arctic species have the genetic potential to utilize NO₃ ^--nitrogen, and that low root temperatures, in conjunction with other environmental limitations, may be responsible for the lack of induction of NR in D. integrifolia and Salix arctica under field conditions.     

The fate of spring applied fertilizer N during the autumn-winter period: comparison between winter-fallow and green manure cropped soil

A field experiment was carried out at a pilot plot that was cropped with oilseed rape, and then left partly fallow and partly cropped with a green manure (mustard) during the autumn after harvest of the oilseed rape. The rape residues were incorporated in the soil. Methods used to quantify the N fluxes from harvest until sowing of the next crop were (1) ¹⁵N balance method, (2) total mineral N analysis and (3) NO emission measurements. Losses of spring applied fertilizer N were negligible in cropped plots and minimal in fallow plots during the following autumn-winter period. Most of the plant-N residues was retained by the organic N pool of the upper 30-cm soil layer. The green manure contributed slightly to soil available N at sowing of the next crop. However, the incorporation of plant material resulted in a nitrate flux that was at risk of leaching on the fallow plots, and on the green manure plots after incorporation of the green manure. This nitrate was largely derived from soil organic N, not from unused fertilizer applied in spring or from immobilized fertilizer. The NO emissions from the green manure plots were significantly higher than emissions from the fallow plots. The plants had a stimulating effect on the NO emission. A relationship between the NO emission and the soil nitrate concentration could not be established. No emissions were measured after green manure incorporation due to the low temperatures at the pilot plot. However, a greenhouse experiment showed an increased emission after incorporation. The NO emissions seemed to be related with the soil ammonium concentration.     

Biological nitrogen fixation in four Gliricidia sepium genotypes

A field experiment was conducted at the Coconut Research Institute in Sri Lanka to examine the biological nitrogen fixation potential of three Gliricidia sepium provenances (OFI 14/84, 17/84, 12/86) and a local landrace (designated LL), using the ¹⁵N isotope dilution method. There was marked variation in dry matter, total N, nodulation and ¹⁵N enrichment among the Gliricidia genotypes (=0.001), and the dry matter yield of Cassia siamea (syn. Senna siamea), the non-N₂ fixing reference plant was higher than for G. sepium. In all cases, highest biomass and total N were aboveground, with roots on average accounting for < 20 % of total dry matter or the total N in plants. Atom % ¹⁵N excess was highest in C. siamea, and lowest in OFI 14/84. Although atom % ¹⁵N excess was lower in Gliricidia leaves than in the other organs (all of which had similar ¹⁵N enrichments), values of % N derived from atmospheric N₂ fixation (% Ndfa) calculated for any individual organ or for the whole plant were similar. This was because the relative distribution of ¹⁵N in the different parts of the fixing plant followed the same trend as in the reference plant. There were significant differences (p=0.01) in N₂ fixation between the Gliricidia genotypes. The values ranged from 17.8 g N tree^-1 (equivalent to 86 kg N ha^-1 at 5000 trees ha^-1) in OFI 12/86 to 61.7g N tree^-1 (equivalent to 309 kg N ha^-1) in OFI 14/84. Although most of this variability was due to differences in both % Ndfa and total N in plant, amount of N fixed was more correlated with total N in plant (r=0.935) than with % Ndfa (r=0.707). On average, % Ndfa in all three G. sepium provenances and LL was about 55 % or 34.6 g N tree^-1 (equivalent to some 166 kg N ha^-1) in the 9 months within which N₂ fixation was measured. This represents a substantial contribution of N into the soil-plant system.     

Carbon distribution and nitrogen partitioning in a soil-plant system with barley (Hordeum vulgare L.), ryegrass (Lolium perenne) and rape (Brassica napus L.) grown in a14CO2-atmosphere

To examine the influence of plant-microorganism interactions on soil-N transformations (e.g. net mineralization, net immobilization) a pot experiment was conducted in a¹⁴C-labelled atmosphere by using different (two annuals, one perennial) plants species. It was assumed that variation in below-ground, microorganism-available C would influence N transformations in soil. Plant species were fertilized (low rate) with¹⁵N-labelled nitrogen and grown, during days 13 and 62 after germination, in a growth chamber with a¹⁴C-labelled atmosphere. Nitrification was inhibited by using nitrapyrin (N-Serve). During the chamber period, shoots were harvested, and associated roots and soil were collected on two sampling occasionm, e.g. after 4 and 7 weeks in the growth chamber.The distribution of net (%) assimilated¹⁴C was significantly affected by both plant and time factors, and there was a significant plant × time interaction. There were significant differences between plants in all plant-soil compartments examined as well as in the degree of the plant × time interaction.Differences in the¹⁴C distribution between plants were due to both interspecific and developmental variation. In general, when comparing¹⁵N and¹⁴C quantities between species, many of the differences found between plants can be explained by the differences determined in the weight of shoot or root parts. Despite the fact that amounts of C released were greater in ryegrass than in the other plant-treatments no unequivocal evidence was found to show that the effects of plant-microorganism interactions on soil-N mineralization were greater under ryegrass. Possible mechanisms accounting for the partitioning of N found among plant biomass, soil biomass and soil residues are discussed.