Nitrogen dynamics in flooded soil systems: an overview on concepts and performance of models.

Extensive modelling studies on nitrogen (N) dynamics in flooded soil systems have been published. Consequently, many N dynamics models are available for users to select from. With the current research trend, inclined towards multidisciplinary research, and with substantial progress in understanding of N dynamics in flooded soil systems, the objective of this paper is to provide an overview of the modelling concepts and performance of 14 models developed to simulate N dynamics in flooded soil systems. This overview provides breadth of knowledge on the models, and, therefore, is valuable as a first step in the selection of an appropriate model for a specific application. © 2017 The Authors. Journal of The Science of Food and Agriculture published by John Wiley & Sons Ltd on behalf of Society of Chemical Industry.

Spatially explicit estimates of N2 O emissions from croplands suggest climate mitigation opportunities from improved fertilizer management.

With increasing nitrogen (N) application to croplands required to support growing food demand, mitigating N2 O emissions from agricultural soils is a global challenge. National greenhouse gas emissions accounting typically estimates N2 O emissions at the country scale by aggregating all crops, under the assumption that N2 O emissions are linearly related to N application. However, field studies and meta-analyses indicate a nonlinear relationship, in which N2 O emissions are relatively greater at higher N application rates. Here, we apply a super-linear emissions response model to crop-specific, spatially explicit synthetic N fertilizer and manure N inputs to provide subnational accounting of global N2 O emissions from croplands. We estimate 0.66 Tg of N2 O-N direct global emissions circa 2000, with 50% of emissions concentrated in 13% of harvested area. Compared to estimates from the IPCC Tier 1 linear model, our updated N2 O emissions range from 20% to 40% lower throughout sub-Saharan Africa and Eastern Europe, to >120% greater in some Western European countries. At low N application rates, the weak nonlinear response of N2 O emissions suggests that relatively large increases in N fertilizer application would generate relatively small increases in N2 O emissions. As aggregated fertilizer data generate underestimation bias in nonlinear models, high-resolution N application data are critical to support accurate N2 O emissions estimates.

Genome Characteristics of a Novel Type I Methanotroph (Sn10-6) Isolated from a Flooded Indian Rice Field.

Flooded rice fields are important sources of atmospheric methane. Aerobic methanotrophs living in the vicinity of rice roots oxidize methane and act as environmental filters. Here, we present genome characteristics of a gammaproteobacterial methanotroph, isolate Sn10-6, which was isolated from a rice rhizosphere of a flooded field in India. Sn10-6 has been identified as a member of a putative novel genus and species within the family Methylococcaceae (Type I methanotrophs). The draft genome of Sn10-6 showed pathways for the following: methane oxidation, formaldehyde assimilation (RuMP), nitrogen fixation, conversion of nitrite to nitrous oxide, and other interesting genes including the ones responsible for survival in the rhizosphere environment. The majority of genes found in this genome were most similar to Methylovulum miyakonese which is a forest isolate. This draft genome provided insight into the physiology, ecology, and phylogeny of this gammaproteobacterial methanotroph.

Eddy covariance assessment of alternate wetting and drying floodwater management on rice methane emissions.

Reducing methane emissions and water use is critical for combating climate change and declining aquifers on food production. Reductions in irrigation water use and methane emissions are known benefits of practicing alternate wetting and drying (AWD) over continuous flooding (CF) water management in lowland rice (Oryza sativa L.) production systems. In a two-year (2020 and 2021) study, methane emissions from large farm-scale (∼50 ha) rice fields managed under CF and AWD in soils dominated by Sharkey clay (Sharkey clay, clay over loamy, montmorillonitic non-acid, thermic Vertic halauepet) were monitored using the eddy covariance method (EC). In the EC system, an open-path laser gas analyzer was used to monitor air methane gas density in the constant flux layer of the atmosphere over the rice-crop canopies. Total water pumped into the field for floodwater management was higher in CF compared to AWD by 24 and 14% in 2020 and 2021, respectively. Considerable variations between seasons in the amount of methane emitted from the CF and AWD treatments were observed: CF emitted 29 and 75 kg ha-1 and AWD emitted 14 and 34 kg ha-1 methane in 2020 and 2021, respectively. Notwithstanding, the extent of reduction in methane emissions due to AWD over CF was similar for each crop season (52% in 2020 and 55% in 2021). Rice grain yield harvested differed by only ±2% between AWD and CF. This investigation of large-scale system-level evaluation, using the EC method, confirmed that by practicing AWD floodwater management in rice, water pumped from aquifers could be reduced by about a quarter and methane emissions from rice fields could be cut down by about half without affecting grain yields, thereby promoting sustainable water management and greenhouse gas emission reduction during rice production in the Lower Mississippi Delta.

Nitrogen fertilizer application in the rice-growing season can stimulate methane emissions during the subsequent flooded fallow period.

Winter-flooded rice paddy field (FR), characterized by water conserved in the field during the fallow period, is a typical cropping system in southwest China, leading to considerable methane (CH4) emissions. The effect of nitrogen (N) fertilization on CH4 emissions during rice-growing seasons is well studied in FR, further studies covering N fertilizer applied in the rice-growing seasons affects CH4 emissions during the subsequent fallow period is needed. Therefore, a field experiment was conducted in an FR of Sichuan province, China, with conventional N fertilized (CN) and N unfertilized (NN) treatments. The cumulative CH4 emission from CN treatment during the rice-growing season and the subsequent fallow period was 389 ± 29.4 and 158 ± 31.2 kg C ha-1, which were increased by 29.5% and 395% in comparison with the NN treatment, indicting N applied during the rice growing-season significantly facilitated CH4 emission during the subsequent fallow period. During the rice-growing season, higher CH4 emission from CN treatment could be attributed to elevated soil dissolved organic carbon (DOC) content that might have provided sufficient substrates for CH4 production. During the fallow period, as compared to NN treatment, higher CH4 emissions from CN treatment could be explained by greater linear regression slopes between CH4 fluxes, soil temperature and DOC to dissolved inorganic N (DIN) (DOC/DIN) ratio. Moreover, the structural equation model (SEM) described that the soil temperature exhibited the most significant effects on CH4 emissions for both treatments during the rice-growing season and subsequent fallow period. These findings are a major step forward to showing that N fertilizer applied in the rice-growing season could also affect CH4 emission during the subsequent fallow period, accompanying other soil parameters controlling CH4 emission.

Evaluating the GHG mitigation-potential of alternate wetting and drying in rice through life cycle assessment.

Alternate wetting and drying (AWD), has gained increasing attention as a promising strategy for mitigating greenhouse gas emissions (GHG) in flooded rice systems. AWD involves periodic drainage of rice paddies in order to inhibit methane (CH4) emissions. To date, studies evaluating this practice have been limited in their scope and resolution. Our study evaluates the mitigation potential of AWD from a life cycle perspective using high-resolution CH4 modeling to more accurately estimate the mitigation potential of this practice. We simulated California rice production under continuous flooding and under five AWD schedules ranging in the severity and frequency of dry-downs. Production models were coupled with the Peatland Ecosystem Photosynthesis Respiration and Methane Transport (PEPRMT) model to simulate CH4 fluxes at daily intervals. We then evaluated the GHG mitigation potential of AWD using life cycle assessment models. Frequent or severe dry-downs reduced simulated grain yields, which negated some of the benefits of AWD when assessed on a yield-scaled basis. We also found AWD-induced mitigation of CH4 emissions modeled with PEPRMT to be roughly half the magnitude reported from up-scaling of chamber measurements, highlighting the importance of high resolution field data to better characterize GHGs in rice systems. Reduced yields and conservative CH4 mitigation in our model lessened the overall mitigation potential of AWD. When the entire rice life cycle was considered, mitigation of overall global warming potential (GWP) was further reduced by the presence of additional GHG sources, which comprised roughly half of life cycle GWP. Our simulations resulted in ≤12% reductions in GWP kg-1 across all AWD scenarios and saw an increase in GWP when yields were severely reduced. Our results highlight the importance of constraining uncertainties in CH4 emissions and considering a life cycle perspective expressed on a yield-scaled basis in characterizing the mitigation potential of AWD.

High resolution depth distribution of Bacteria, Archaea, methanotrophs, and methanogens in the bulk and rhizosphere soils of a flooded rice paddy.

The communities and abundances of methanotrophs and methanogens, along with the oxygen, methane, and total organic carbon (TOC) concentrations, were investigated along a depth gradient in a flooded rice paddy. Broad patterns in vertical profiles of oxygen, methane, TOC, and microbial abundances were similar in the bulk and rhizosphere soils, though methane and TOC concentrations and 16S rRNA gene copies were clearly higher in the rhizosphere soil than in the bulk soil. Oxygen concentrations decreased sharply to below detection limits at 8 mm depth. Pyrosequencing of 16S rRNA genes showed that bacterial and archaeal communities varied according to the oxic, oxic-anoxic, and anoxic zones, indicating that oxygen is a determining factor for the distribution of bacterial and archaeal communities. Aerobic methanotrophs were maximally observed near the oxic-anoxic interface, while methane, TOC, and methanogens were highest in the rhizosphere soil at 30-200 mm depth, suggesting that methane is produced mainly from organic carbon derived from rice plants and is metabolized aerobically. The relative abundances of type I methanotrophs such as Methylococcus, Methylomonas, and Methylocaldum decreased more drastically than those of type II methanotrophs (such as Methylocystis and Methylosinus) with increasing depth. Methanosaeta and Methanoregula were predominant methanogens at all depths, and the relative abundances of Methanosaeta, Methanoregula, and Methanosphaerula, and GOM_Arc_I increased with increasing depth. Based on contrasts between absolute abundances of methanogens and methanotrophs at depths sampled across rhizosphere and bulk soils (especially millimeter-scale slices at the surface), we have identified populations of methanogens (Methanosaeta, Methanoregula, Methanocella, Methanobacterium, and Methanosphaerula), and methanotrophs (Methylosarcina, Methylococcus, Methylosinus, and unclassified Methylocystaceae) that are likely physiologically active in situ.

How different soil moisture levels affect the microbial activity / Como diferentes níveis de umidade do solo afetam a atividade microbiana de um solo de terras baixas usado para cultivo do arroz?

ABSTRACT: The lowland soils are characterized by high susceptibility to water saturation. This anaerobic condition is usually reported in paddy fields and alters the decomposition process of soil organic compounds. The aim of this study was to evaluate the soil microbial and enzymatic activity of a lowland soil at different soil moisture contents. A poorly drained Albaqualf cultivated with irrigated rice was used to evaluate microbial and enzymatic activity in treatments with different levels of soil moisture, being: i) 60% of field capacity (FC) (60%FC); ii) 100% of FC (100%FC); iii) flooded soil with a 2 cm water layer above soil surface, and iv) soil kept at 60%FC with late flood after 29 days the incubation. The greater soil microbial activity was observed in the 100%FC treatment, being 41% greater than 60%FC treatment and only 2% higher than flooded treatment. The enzymatic activity data by fluorescein diacetate (FDA) hydrolysis corroborated the higher CO2 release in treatments with higher soil moisture content. Differently from the results reported, the main methodologies to evaluate microbial activity still recommend maintenance of the soil with a moisture content close to 60% of the FC. However, in lowland soil with history of frequent paddy fields, the maintenance of moisture close to 60% of the FC can limit the microbial activity. The soil respiration technique can be used to evaluate the microbial activity in flooded soil conditions. However, further studies should be conducted to understand the effect of the cultivation history on the microbial community of these environments.

RESUMO: Os solos de várzea são caracterizados pela alta suscetibilidade à saturação por água. Esta condição anaeróbica é geralmente encontrada em solos arrozeiros e altera o processo de decomposição dos compostos orgânicos do solo. O objetivo deste estudo foi avaliar a atividade microbiana e enzimática de um solo de várzea sob diferentes teores de umidade no solo. Um Planossolo historicamente cultivado com arroz irrigado foi utilizado para avaliar a atividade microbiana e enzimática em tratamentos com diferentes níveis de umidade do solo, sendo: i) 60% de capacidade de campo (CC) (60%CC); ii) 100% da CC (100%CC); iii) solo inundado com uma camada de água de 2 cm acima da superfície do solo; e iv) solo mantido a 60%CC com inundação após 29 dias da incubação. A maior atividade microbiana do solo foi observada no tratamento 100%CC, sendo 41% maior que o tratamento 60%CC e 2% maior que tratamento inundado. Os dados da atividade enzimática pela hidrólise do diacetato de fluoresceína (FDA) corroboraram a maior liberação de CO2 nos tratamentos com maior umidade do solo. Diferentemente dos resultados encontrados, as principais metodologias para avaliação da atividade microbiana ainda recomendam manter o solo com umidade próxima a 60% da CC. No entanto, em solos de várzea com históricos de cultivos de arroz, a manutenção de umidade próxima a 60% da CC pode limitar a atividade microbiana. A técnica de respiração do solo pode ser usada para avaliar a atividade microbiana em condições de solo inundado. No entanto, mais estudos devem ser realizados para entender o efeito do histórico de cultivo na comunidade microbiana nesses ambientes.

Methane emission from a flooded rice field under pre-germinated system / Emissão de metano em área de arroz irrigado sob sistema pré-germinado

ABSTRACT: Local greenhouse gas flow measurement studies have been encouraged at a global level as a subsidy for national and state inventories. This study aimed to evaluate the seasonal methane emission during the 2008/2009 harvest, from an irrigated rice plantation, under pre-germinated system, in the municipality of Tremembé, State of São Paulo, using the static chamber technique and gas chromatography. The study showed high seasonal emission of methane (CH4) for the studied area, probably due to the long flooding period. It was estimated the CH4 emission factor (6.51 kg CH4 ha-1 dia-1), the partial global warming potential (pGWP, 27.2 Mg CO2eq growing season-1 ha-1) and the yield-scaled pGWP (YpGWP, 3.9 kg CO2eq kg-1 grain).

RESUMO: Estudos locais de mensuração de fluxos de gases de efeito estufa em sistemas agrícolas têm sido incentivados a nível global como base para subsidiar estimativas nacionais e estaduais de emissão. Este estudo objetivou quantificar a emissão sazonal de metano (CH4) em cultivo de arroz irrigado, sob sistema pré-germinado, no município de Tremembé, Estado de São Paulo, na safra de 2008/2009, utilizando o método de câmara estática e cromatografia gasosa. O estudo mostrou elevada emissão sazonal de CH4 para a área estudada, em função, provavelmente do longo período de inundação. Foi estimado o fator de emissão de CH4 (6,51 kg CH4 ha-1 dia-1), o potencial de aquecimento global parcial (PAGp, 27,2 Mg CO2eq estação de crescimento-1 ha-1) e o PAGp escalonado pelo rendimento (R) de grãos (PAGpR, 3,9 kg CO2eq kg-1 grão).

Impact of elevated CO2 and temperature on soil C and N dynamics in relation to CH4 and N2O emissions from tropical flooded rice (Oryza sativa L.).

A field experiment was carried out to investigate the impact of elevated carbon dioxide (CO2) (CEC, 550 µmol mol(-1)) and elevated CO2+elevated air temperature (CECT, 550 µmol mol(-1) and 2°C more than control chamber (CC)) on soil labile carbon (C) and nitrogen (N) pools, microbial populations and enzymatic activities in relation to emissions of methane (CH4) and nitrous oxide (N2O) in a flooded alluvial soil planted with rice cv. Naveen in open top chambers (OTCs). The labile soil C pools, namely microbial biomass C, readily mineralizable C, water soluble carbohydrate C and potassium permanganate oxidizable C were increased by 27, 23, 38 and 37% respectively under CEC than CC (ambient CO2, 394 µmol mol(-1)). The total organic carbon (TOC) in root exudates was 28.9% higher under CEC than CC. The labile N fractions were also increased significantly (29%) in CEC than CC. Methanogens and denitrifier populations in rhizosphere were higher under CEC and CECT. As a result, CH4 and N2O-N emissions were enhanced by 26 and 24.6% respectively, under CEC in comparison to open field (UC, ambient CO2, 394 µmol mol(-1)) on seasonal basis. The global warming potential (GWP) was increased by 25% under CEC than CC. However, emissions per unit of grain yield under elevated CO2 and temperature were similar to those observed at ambient CO2. The stimulatory effect on CH4 and N2O emissions under CEC was linked with the increased amount of soil labile C, C rich root exudates, lowered Eh, higher Fe(+2) concentration and increased activities of methanogens and extracellular enzymes.

Diurnal variation of methane emission from a paddy field in Brazilian Southeast / Variação diurna da emissão de metano em arroz irrigado no Sudeste do Brasil

ABSTRACT: This study aimed to investigate the diurnal variation of methane (CH4) emission in a flooded-irrigated rice field at different stages of the plant development under tropical climate in three growing seasons, in order to determine the most appropriate time for gas sampling in the Brazilian Southeast region. It aimed also to verify correlations between CH4 flux and air, water and soil temperatures, and solar radiation. The CH4 emissions were measured every 3-hour interval on specific days in different development stages of the flooded rice in the Experiment Station of the Agência Paulista de Tecnologia dos Agronegócios (APTA), Pólo Regional Vale do Paraíba, at Pindamonhangaba, State of São Paulo (22°55' S, 45°30' W), Brazil. Different CH4 emission rates were observed among the plant growth stages and also among the growing seasons. The CH4 emission showed high correlation with the soil temperature at 2cm depth. At this depth, the CH4 emission activation energy in response to soil temperature was higher in the stage R2. Emission peaks were observed at afternoon, while lower fluxes were recorded at the early morning. The most appropriate local time for gas sampling was estimated at 12:11:15a.m.±01:14:16 and 09:05:49p.m.±01:29:04.

RESUMO: Este estudo teve como objetivo investigar a variação diurna de emissões de metano (CH4) em uma lavoura de arroz irrigado por inundação em diferentes estágios de desenvolvimento de plantas de arroz irrigado, sob clima tropical, em três estações de crescimento, para determinar o período de tempo mais apropriado à amostragem de gás na região Sudeste do Brasil. O trabalho objetivou também verificar correlações entre o fluxo de CH4 e as temperaturas do ar, da água e do solo e a radiação solar. As emissões diurnas de CH4 foram medidas a cada intervalo de três (3) horas em dias específicos em diferentes estágios de desenvolvimento da planta de arroz inundado na Estação Experimental da Agência Paulista de Tecnologia dos Agronegócios (APTA), Pólo Regional Vale do Paraíba, em Pindamonhangaba, Estado de São Paulo (22°55' S, 45°30' W), Brasil. Diferentes taxas de emissão foram observadas entre os estágios de desenvolvimento da planta avaliados e também entre as estações de cultivo. A emissão de CH4 mostrou alta correlação com a temperatura do solo a 2cm de profundidade. Nesta profundidade, a energia de ativação da emissão de CH4 em resposta à temperatura do solo foi maior no estágio R2. Os picos de emissão foram observados no período da tarde, enquanto que menores fluxos foram registrados no início da manhã. O horário mais apropriado para amostragem de gás foi estimado em 12:11:15a.m.±01:14:16 and 09:05:49p.m.±01:29:04.

Adubação nitrogenada sobre rendimento industrial e composição dos grãos de arroz irrigado / Nitrogen fertilization on industrial yield and composition of flood-irrigated rice grains

O efeito de doses em cobertura de adubação nitrogenada foi avaliado sobre o rendimento do beneficiamento, a incidência de grãos gessados e barriga branca, os teores de proteína e de amilose nos grãos polidos da variedade de arroz irrigado IRGA 422CL. Utilizando a ureia como fonte de nitrogênio (N), os tratamentos constituíram-se de doses crescentes distribuídas em cobertura na primeira aplicação (0, 40, 63, 80 e 120kg ha-1 de N), na parcela principal (10x5m), e na segunda aplicação (0, 25, 50 e 75kg ha-1 de N), na subparcela (2,5x5m). Assim, foram obtidos 20 tratamentos com variação de 0 a 195kg ha-1 de N aplicado durante o cultivo. As doses em cobertura de adubação nitrogenada influenciaram quadrática e positivamente o rendimento de grãos inteiros (R²=0,75) e negativamente a percentagem de grãos quebrados (R²=-0,89), não apresentando efeitos significativos na percentagem de casca + farelo. As doses de nitrogênio influenciaram de forma linear positiva sobre o teor de proteína (R²=0,81) e linear negativa sobre o teor de amilose (R²=-0,66), nos grãos polidos da variedade de arroz irrigado IRGA 422CL.

The effect of nitrogen (N) fertilization levels was assessed by the industrial yield, the incidence of chalky and white belly grains as well as protein and amylose content of IRGA 422CL cultivar polished grains. The experiment was consisted with N levels applied in coverage using urea as a N source. The first application (0, 40, 63, 80 and 120kg ha-1 of N) was carried out on a main plot (10x5m) and the second application (0, 25, 50 and 75kg ha-1 of N) on a subplot (2,5x5m). Therefore, 20 treatments were obtained varying from 0 to 195kg ha-1 of N applied during cultivation. The nitrogen levels presented a positive quadratic influence on the yield of whole grains (R²=0.75) and a negative influence on the percentage of broken grains (R²=-0.89), not demonstrating significant effects on the percentage of rice hulls + bran. The nitrogen levels influenced protein content in a positive linear way (R²=0.81) and amylose content in a negative linear way (R²=-0.66), in IRGA 422CL cultivar flood-irrigated polished grains.

Propriedades enzimáticas da enzima ALS de Cyperus difformis e mecanismo de resistência da espécie ao herbicida pyrazosulfuron-ethyl / Enzymatic properties of Cyperus difformis ALS enzyme and mechanism resistance of the species to pyrazosulfuron-ethyl herbicide

Cyperus difformis L. é uma planta daninha ocorrente em lavouras de arroz irrigado, que tem apresentado dificuldade de controle devido à resistência a herbicidas inibidores da enzima ALS. Os objetivos deste trabalho foram investigar características cinéticas da enzima ALS de biótipos de C. difformis e determinar as bases bioquímicas da resistência da espécie ao herbicida pyrazosulfuron-ethyl. Para isso, foram conduzidos experimentos em laboratório do BIOAGRO/UFV. O método utilizado baseou-se na metologia utilizada por CAREY et al. (1997) e adaptada por VARGAS et al. (1999), com algumas modificações. Foram avaliadas a concentração de substrato (piruvato) que fornece velocidade inicial igual à metade da velocidade máxima de reação (K M) e velocidade máxima de reação (Vmáx), bem como a atividade da enzima ALS na presença do inibidor (pyrazosulfuron-ethyl). Diante dos resultados, pode-se observar que a resistência de C. difformis a pyrazosulfuron-ethyl é decorrente da insensibilidade da enzima ALS ao herbicida, não acarretando, porém, prejuízo aos parâmetros cinéticos K M e Vmáx da enzima ALS.

Cyperus difformis L. is a weed that occurs in flooded rice, which has presented difficulty in controlling due to the resistance to ALS inhibiting herbicides. The objectives of this research were to investigate kinetic characteristics of ALS enzyme from C. difformis biotypes and to determine the biochemical bases of resistance from the species to pyrazosulfuron-ethyl herbicide. For that, experiments were conducted at the BIOAGRO/UFV laboratory. The method used was based on the methodology used by CAREY et al. (1997) and adapted by VARGAS et al. (1999), with some modifications. It was evaluated substratum concentration (pyruvate) that provides initial velocity equal to half the speed reaction (K M) and maximum velocity of reaction (Vmáx), as well the activity of the ALS enzyme in the presence of the inhibitor (pyrazosulfuron-ethyl). According to the results, it is possible to observe that C. difformis resistance to pyrazosulfuron-ethyl is due to the insensibility of the ALS enzyme to the herbicide, however without penalty to K M and Vmáx kinetic parameters of the ALS enzyme.

Doses e épocas de aplicação de nitrogênio na suscetibilidade do arroz à temperatura baixa na fase reprodutiva / Nitrogen doses and timing on rice susceptibility to low temperature in reproductive stage

A aplicação de nitrogênio (N) deve afetar a sensibilidade das plantas de arroz quando submetidas ao frio na fase reprodutiva. Assim, foram instalados dois experimentos em casa de vegetação, no Instituto Nacional de Investigação Agropecuária (INIA), INIA Treinta y Tres, Uruguai, na safra agrícola 2007/08. O primeiro experimento teve o objetivo de determinar o efeito da época e o segundo, o efeito de dose de aplicação de N sobre a suscetibilidade de plantas de arroz irrigado à temperatura baixa na fase reprodutiva. Realizou-se um experimento bifatorial em delineamento inteiramente casualizado (fator A: épocas ou doses de aplicação de N e fator B: aplicação ou não de frio nos dois experimentos), com quatro repetições. No experimento 1, os tratamentos do fator A foram a aplicação de N (30kg ha-1) nos estádios V4, V5, V6, V7, V8, R0, R1+4 dias e a testemunha sem N em cobertura. Nesse experimento, os tratamentos que receberam N de V4 a V8 também receberam mais 30kg ha-1 no estádio R0, e os tratamentos que receberam N nos estádios R0 e R1+4 dias também receberam 30kg ha-1 no estádio V4. No experimento 2, o fator A foram níveis de N de 0, 23, 46 e 69kg ha-1 de N no estádio V4 mais uma aplicação de 23kg ha-1 no estádio R0 e as mesmas doses em R0 com 23kg ha-1 no estádio V4, mais uma testemunha sem aplicação de N nos dois estádios. No tratamento com frio, as plantas foram submetidas a 12,5°C durante sete horas em quatro noites quando o colar da folha bandeira ficou com a mesma altura que o colar da folha anterior. Foram avaliados os seguintes parâmetros: a percentagem de esterilidade de espiguetas, o índice SPAD, realizado aos três, 10 e 16 dias após o tratamento do frio no estádio R2-R3, a produtividade de grãos por vaso, o número de panículas por balde e a massa de mil grãos. A esterilidade de espiguetas não foi influenciada pela época, pela dose de aplicação de N ou pelo tratamento de frio, mas encontrou-se efeito temporário do frio no índice...

Nitrogen doses and timing of topdressing application affects the sensibility of rice plants to low temperature in reproductive stage. For these reasons it were installed two experiments with the objective of determining the effect of nitrogen topdressing application doses and timing on the susceptibility of rice plants to low temperature in the reproductive phase. The experiments were sowed in 2007/08 growing season in a greenhouse at Instituto Nacional de Investigação Agropecuária (INIA), INIA Treinta y Tres, Uruguay, with INIA Olimar cultivar. In both experiments, a factorial experiment was carried out in a completely randomized design, with four replications (factor A: stages or rates of N application and factor B: temperature treatment, with or without cold). In the experiment 1 the treatments of factor A were N application of 30 kg ha-1 in V4, V5, V6, V7, V8, R0, R1+4 days and an untreated check without N in topdressing. In experiment 2, the factor A was doses of N: 0, 23, 46 and 69kg ha-1 in V4 stage and the same levels of N in R0 stage plus a check without N in topdressing. The plants were treated with 12.5 C during seven hours for four nights when the collar of the flag leaf was at the same height of the previous leaf. The following aspects were evaluated: grain yield; spikelet sterility; SPAD index at three, ten and sixteen days of low temperature treatment; number of panicles per plot and weight of 1000 grains. Spikelet sterility was not affected by the application of N in different stages or doses, by cold treatment or their interaction, but the cold treatment affected temporally the SPAD index with delaying panicle emerge. It is not necessary to modify the N applications for this variety in Uruguay.