The effects of prolonged exposure to elevated temperatures and elevated CO2 levels on the growth, yield and dry matter partitioning of field-sown meadow fescue

Selostus: Kohotetun lämpötilan ja kohotetun CO2-pitoisuuden vaikutukset peltoon kylvetyn nurminadan kasvuun, satoon ja kuiva-aineen jakautumiseen

Uncertainties in the prediction of spatial variability of soil CO2 emissions and related properties

The soil CO2 emission has high spatial variability because it depends strongly on soil properties. The purpose of this study was to (i) characterize the spatial variability of soil respiration and related properties, (ii) evaluate the accuracy of results of the ordinary kriging method and sequential Gaussian simulation, and (iii) evaluate the uncertainty in predicting the spatial variability of soil CO2 emission and other properties using sequential Gaussian simulations. The study was conducted in a sugarcane area, using a regular sampling grid with 141 points, where soil CO2 emission, soil temperature, air-filled pore space, soil organic matter and soil bulk density were evaluated. All variables showed spatial dependence structure. The soil CO2 emission was positively correlated with organic matter (r = 0.25, p < 0.05) and air-filled pore space (r = 0.27, p < 0.01) and negatively with soil bulk density (r = -0.41, p < 0.01). However, when the estimated spatial values were considered, the air-filled pore space was the variable mainly responsible for the spatial characteristics of soil respiration, with a correlation of 0.26 (p < 0.01). For all variables, individual simulations represented the cumulative distribution functions and variograms better than ordinary kriging and E-type estimates. The greatest uncertainties in predicting soil CO2 emission were associated with areas with the highest estimated values, which produced estimates from 0.18 to 1.85 t CO2 ha-1, according to the different scenarios considered. The knowledge of the uncertainties generated by the different scenarios can be used in inventories of greenhouse gases, to provide conservative estimates of the potential emission of these gases.

The application of agricultural land rating and crop models to CO2 and climate change issues in Northern regions : the Mackenzie Basin case study

Selostus: Viljelyvyöhykkeiden ja kasvumallien soveltaminen ilmastonmuutoksen tutkimisessa: Mackenzien jokialue, Kanada

Monitoramento contínuo do potencial redox e de variáveis complementares em ambiente hipersazonal no Pantanal Norte

A análise conjunta do potencial redox com outras variáveis pode ser útil para o entendimento da dinâmica dos solos hidromórficos, ao longo de todo o ciclo hidrológico a que o Pantanal está submetido. Neste trabalho, foram estudados o potencial redox e algumas variáveis do solo (CO2, O2, temperatura, umidade e potencial matricial) pelo monitoramento contínuo e ininterrupto. Para isso, foram realizadas determinações nas profundidades de 10 e 30 cm num Planossolo Háplico alítico gleissólico, na fitofisionomia Cerrado sensu stricto. O trabalho foi realizado de fevereiro de 2010 a julho de 2011 na RPPN (Reserva Particular do Patrimônio Natural/Sistema Nacional de Unidades de Conservação - SNUC), Estância Ecológica SESC (Serviço Social do Comércio) Pantanal, município de Barão de Melgaço, nordeste do Pantanal de Mato Grosso. Os valores do potencial redox variaram de 636 mV (enchente) a -341 mV (cheia), caracterizando ambiente anaeróbico na estação da cheia e ambiente oxidado nas demais estações do ciclo hidrológico, o que indica que o potencial redox é ferramenta versátil para compreender as reações de oxirredução nos solos hidromórficos do Pantanal mato-grossense, pois os valores diminuíram quando o teor de umidade era elevado. Além disto, o estudo evidenciou também que o monitoramento contínuo de variáveis complementares pode ser importante por permitir análise mais aprofundada das condições de hipersazonalidade, em que esses solos estão submetidos. Neste contexto, o potencial matricial e a umidade foram as variáveis de maior importância para explicar a variação do conjunto de dados obtidos ao longo do ciclo hidrológico, o que indica que esses parâmetros físicos são determinantes nos processos biológicos desse solo tropical com hipersazonalidade hídrica.

An overview of how rubisco and carbohydrate metabolism may be regulated at elevated atmospheric [CO2] and temperature

Selostus: Hiilihydraatti- ja proteiiniaineenvaihdunnan säätely kohonneen hiilidioksidipitoisuuden ja lämpötilan vallitessa

Arrangement of experiments for simulating the effects of elevated temperatures and elevated CO2 levels on field-sown crops in Finland

Selostus: Koejärjestelyt kohonneen lämpötilan ja CO2-tason vaikutusten simuloimiseksi peltokasveilla Suomessa

Efeito do preparo do solo e resíduo da colheita de cana-de-açúcar sobre a emissão de CO2

O solo é um dos principais compartimentos de carbono no ecossistema terrestre, capaz de armazenar quantidades expressivas desse elemento e, portanto, a compreensão dos fatores que contribuem para as perdas de CO2 em solos agrícolas é fundamental para determinar estratégias de redução das emissões desse gás e ajudar a mitigar o efeito estufa. O objetivo deste estudo foi investigar o efeito do preparo do solo e da deposição de resíduos da cultura da cana-de-açúcar na emissão de CO2, temperatura e umidade do solo, durante a reforma do canavial, ao longo de um período de 15 dias. Os manejos avaliados foram: sem preparo do solo e mantendo os resíduos da colheita sobre a superfície do solo (SPCR); sem preparo do solo e sem resíduo (SPSR) e com preparo do solo e sem resíduo (CPSR). A menor média de emissão de CO2 do solo (FCO2) foi observada no manejo SPCR (2,16 µmol m-2 s-1), quando comparado aos manejos SPSR (2,90 µmol m-2 s-1) e CPSR (3,22 µmol m-2 s-1), indicando que as maiores umidades e menores variações da temperatura do solo, observadas em SPCR, foram os fatores responsáveis por tal diminuição. Durante o período de estudo, a menor média diária da FCO2 foi registrada em SPCR (1,28 µmol m-2 s-1) e a maior em CPSR (6,08 µmol m-2 s-1), após a ocorrência de chuvas. A menor perda de C-CO2 do solo foi observada no manejo SPCR (367 kg ha-1 de C-CO2), diferindo significativamente (p<0,05) dos manejos: SPSR (502 kg ha-1 de C-CO2) e CPSR (535 kg ha-1 de C-CO2). A umidade do solo foi a variável que apresentou valores mais diferenciados entre os manejos, sendo positivamente correlacionada (r = 0,55; p<0,05) com as variações temporais da emissão de CO2 nos manejos SPCR e CPSR. Em adição, a temperatura do solo diferiu (p<0,05) somente no manejo SPCR (24 ºC), quando comparada aos manejos SPSR (26 ºC) e CPSR (26,5 ºC), sugerindo que, para as condições deste estudo, o resíduo da cana-de-açúcar retido sobre a superfície propiciou uma temperatura do solo, em média, 2 ºC mais amena.

Sensitivity of temperate grassland species to elevated atmospheric CO2 and the interaction with temperature and water stress

Selostus: Kohonneen hiilidioksidipitoisuuden, lämpötilan ja kuivuuden vaikutus nurmikasveihin

Deep hypothermia and rewarming alters glutamate levels and glycogen content in cultured astrocytes.

BACKGROUND: Deep hypothermia has been associated with an increased incidence of postoperative neurologic dysfunction after cardiac surgery in children. Recent studies suggest an excitotoxic mechanism involving overstimulation of glutamate receptors. Extracellular glutamate uptake occurs primarily by astrocytes. Astrocytes also store glycogen, which may be used to sustain the energy-consuming glutamate uptake. Extracellular glutamate and glycogen content were studied during temperature changes mimicking cardiopulmonary bypass in vivo. METHODS: Primary cultures of cerebral cortical astrocytes were used in a specially designed incubator allowing continuous changes of temperature and ambient gas concentrations. The sequence of events was as follows: normothermia, rapid cooling (2.8 degrees C/min) followed by 60 min of deep hypothermia (15 degrees C), followed by rewarming (3.0 degrees C/min) and subsequent 5 h of mild hyperthermia (38.5 degrees C). Two different conditions of oxygenation were studied: (1) normoxia (25% O2, 70% N2, 5% CO2); or (2) hyperoxia (95% O2, 5% CO2). The extracellular glutamate concentrations and intracellular glycogen levels were measured at nine time points. RESULTS: One hundred sixty-two cultures were studied in four independent experiments. The extracellular concentration of glutamate in the normoxic group increased significantly from 35+/-10 nM/mg protein at baseline up to 100+/-15 nM/mg protein at the end of 5 h of mild hyperthermia (P < 0.05). In contrast, extracellular glutamate levels did not vary from control in the hyperoxic group. Glycogen levels decreased significantly from 260+/-85 nM/mg protein at baseline to < 25+/-5 nM/mg protein at the end of 5 h in the normoxic group (P < 0.05) but returned to control levels after rewarming in the hyperoxic group. No morphologic changes were observed in either group. CONCLUSION: The extracellular concentration of glutamate increases, whereas the intracellular glycogen content decreases when astrocytes are exposed to a sequence of deep hypothermia and rewarming. This effect of hypothermia is prevented when astrocytes are exposed to hyperoxic conditions.

Intérêt du monitorage du CO2 expiré pour évaluer la PaCO2 lors d'insuffisance respiratoire aiguë hypercapnique traitée par ventilation non invasive.

Introduction: L'efficacité d'une séance de VNI est habituellement évaluée selon la réponse clinique, l'amélioration de l'acidose respiratoire et de l'hypercapnie. Le but de cette étude était d'évaluer l'intérêt de la mesure du CO2 en fin d'expiration (PETCO2) pour estimer la PaCO2 et son évolution dans le temps. Patients et Méthodes: Des patients de réanimation souffrant d'une insuffisance respiratoire aiguë hypercapnique (PaCO2 >45 mmHg) ont été inclus dans cette étude prospective. La PETCO2était mesurée à l'aide d'un capteur nasobuccal (SmartLine®, Oridion) au cours d'une séance de VNI de 60 minutes. Une gazométrie artérielle et la valeur de PETCO2 étaient enregistrées au début de la séance puis chaque 15 minutes. Des manoeuvres d'expiration complète passives et actives étaient effectuées à 30 et 60 minutes. Le gradient de CO2 (PaCO2- PETCO2) a été calculé pour l'ensemble des mesures, spécifiquement pour chaque manoeuvre d'expiration complète, ainsi qu'individuellement pour chaque patient. Ces grandeurs sont exprimées en moyenne et écart-type pour évaluer le biais et la dispersion observés entre PaCO2 et PETCO2. La différence entre chaque valeurs consécutives de gradient de CO2 (delta gradient de CO2) a été calculées par patient. Cette mesure quantifie la variation au cours du temps du gradient de CO2 pour un patient donné. Résultats: 11 patients ont été inclus (7 BPCO, 1 restrictif et 1 syndrome d'apnée du sommeil). Sur l'ensemble des mesures, le gradient de CO2 était de 14.7 + 10.6 mmHg, lors des manoeuvres d'expiration complètes active il était de 8.1 + 13.0 mmHg, et de 8.8 + 11.9 mmHg lors des expirations passives. Conclusion: Chez les patients présentant une insuffisance respiratoire aiguë hypercanique traitée par VNI, la mesure de la PETCO2 par capteur nasobuccal ne permet de prédire ni la valeur de PaCO2, ni son évolution dans le temps. Les manoeuvres d'expiration complète n'apportent aucune plus value.

CO2 wedged hepatic venography in the evaluation of portal hypertension.

BACKGROUND/AIMS/METHODS During hepatic vein catheterisation, in addition to measurement of hepatic venous pressure gradient (HVPG), iodine wedged retrograde portography can be easily obtained. However, it rarely allows correct visualisation of the portal vein. Recently, CO2 has been suggested to allow better angiographic demonstration of the portal vein than iodine. In this study we investigated the efficacy of CO2 compared with iodinated contrast medium for portal vein imaging and its role in the evaluation of portal hypertension in a series of 100 patients undergoing hepatic vein catheterisation, 71 of whom had liver cirrhosis. RESULTS In the overall series, CO2 venography was markedly superior to iodine, allowing correct visualisation of the different segments of the portal venous system. In addition, CO2, but not iodine, visualised portal-systemic collaterals in 34 patients. In cirrhosis, non-visualisation of the portal vein on CO2 venography occurred in 11 cases; four had portal vein thrombosis and five had communications between different hepatic veins. Among non-cirrhotics, lack of portal vein visualisation had a 90% sensitivity, 88% specificity, 94% negative predictive value, and 83% positive predictive value in the diagnosis of pre-sinusoidal portal hypertension. CONCLUSIONS Visualisation of the venous portal system by CO2 venography is markedly superior to iodine. The use of CO2 wedged portography is a useful and safe complementary procedure during hepatic vein catheterisation which may help to detect portal thrombosis. Also, lack of demonstration of the portal vein in non-cirrhotic patients strongly suggests the presence of pre-sinusoidal portal hypertension.

[Voyage en Italie : 1824-1830]. , [Détails de peintures décoratives] : [un motif de char tiré par des lionnes] : [dessin] / [Henri Labrouste]

Référence bibliographique : Weigert, 436