Academic literature on the topic 'Diffuse light fertilization'

The nutrient and nutraceutical quality of greenhouse wild rocket is strongly influenced by the light environment and nitrogen fertilization. We investigated the effects of two cover materials, a diffuse light film (Film1) and a traditional clear film (Film2), and three nitrogen regimes, no N supply (N0) and sub-optimal (N1) and optimal (N2) doses, also in combination with a biostimulant (Stimolo Mo), on the mineral composition, antioxidant properties and chlorophyll and carotenoid content of rocket plants grown in the autumn–spring cycle. The leaf concentration of most of the minerals was higher under Film1 compared to Film2. In general, K, Ca, Mg and Na were higher, and S was lower in the presence of N supply, and the addition of the biostimulant promoted the mineral uptake. Under Film1, the hydrophilic antioxidant activity (HAA) was higher in some harvests, and the ABTS antioxidant activity (ABTS AA) in the first one, while always lower afterward, than under Film2. Nitrogen fertilization did not affect the antioxidant activity, while it reduced the content of total phenols and ascorbic acid. The biostimulant application increased ABTS AA at the optimal N dose and reduced total phenols in unfertilized plants. Both the diffuse light and the N supply inhibited the synthesis of ascorbic acid, while N fertilization and the biostimulant promoted the synthesis of chlorophylls. The experimental treatments exerted variable effects over time and significant interactions with the harvest period were found for many of the investigated parameters.

Abstract. The Amazon experiences fires every year, and the resulting biomass burning aerosols, together with cloud particles, influence the penetration of sunlight through the atmosphere, increasing the ratio of diffuse to direct photosynthetically active radiation (PAR) reaching the vegetation canopy and thereby potentially increasing ecosystem productivity. In this study, we use the NASA Goddard Earth Observing System (GEOS) model with coupled aerosol, cloud, radiation, and ecosystem modules to investigate the impact of Amazon biomass burning aerosols on ecosystem productivity, as well as the role of the Amazon's clouds in tempering this impact. The study focuses on a 7-year period (2010–2016) during which the Amazon experienced a variety of dynamic environments (e.g., La Niña, normal years, and El Niño). The direct radiative impact of biomass burning aerosols on ecosystem productivity – called here the aerosol diffuse radiation fertilization effect – is found to increase Amazonian gross primary production (GPP) by 2.6 % via a 3.8 % increase in diffuse PAR (DFPAR) despite a 5.4 % decrease in direct PAR (DRPAR) on multiyear average during burning seasons. On a monthly basis, this increase in GPP can be as large as 9.9 % (occurring in August 2010). Consequently, the net primary production (NPP) in the Amazon is increased by 1.5 %, or ∼92 Tg C yr−1 – equivalent to ∼37 % of the average carbon lost due to Amazon fires over the 7 years considered. Clouds, however, strongly regulate the effectiveness of the aerosol diffuse radiation fertilization effect. The efficiency of this fertilization effect is the highest in cloud-free conditions and linearly decreases with increasing cloud amount until the cloud fraction reaches ∼0.8, at which point the aerosol-influenced light changes from being a stimulator to an inhibitor of plant growth. Nevertheless, interannual changes in the overall strength of the aerosol diffuse radiation fertilization effect are primarily controlled by the large interannual changes in biomass burning aerosols rather than by changes in cloudiness during the studied period.

The quantity and quality of wall rocket (Diplotaxis tenuifolia L.) production are strongly influenced by the cultivation system, in particular the protected environment conditions and nitrogen fertilization. In the present research, we tested two greenhouse cover films (Film1: diffuse light; Film2: clear), to verify the effects on yield and nitrate content (a detrimental factor of quality) of rocket leaves, fertilized with optimal (N2) or sub-optimal nitrogen dose (N1), or unfertilized (N0). In addition, we combined the N fertilization with a biostimulant application, declared by the manufacturer as able to reduce nitrate content. Film1 provided a 36% yield increase over Film2 and allowed an increasing production until the V harvest, opposite to what was recorded under Film2, where the yield increased only until the III harvest. Additionally, biostimulant application boosted the yield (+40%), as well as nitrogen fertilization. Both factors had the best performance under Film1, where N1 yield was even equal to N2-Film2. The nitrate content showed a seasonal trend (lower values in spring harvests) and it was boosted by nitrogen (1096, 3696, and 4963 mg/kg fresh weight, for N0, N1, and N2, respectively) and biostimulant application (3924 vs. 2580 mg/kg fresh weight). Therefore, the use of diffuse-light film seems useful to obtain higher yield with a halved N dose as well as in combination with biostimulant application, but the latter did not confirm the capacity to contain nitrate, at least for this crop and in this cultivation system.

Light and nitrogen are the main factors commanding horticulture production. Therefore, this study aims at evaluating the effects of two different greenhouse cover films (clear-Film A and diffuse light-Film B) on yield and nutritive value of a ready-to-eat salad lamb’s lettuce (Valerianella locusta L.), grown under several nitrogen regimes (no nitrogen [N0], sub-optimal [N25] and optimal N fertilization [N50] corresponding to 0, 25 and 50 kg ha-1 , respectively). The combination N50 and Film B boosted SPAD index by 10.3% and yield by 91.9% compared to N0 × Film A. Concerning antioxidant activity and bioactive compounds, only total ascorbic acid was positively affected by Film B (9.4%), while there was no effect of this cover film on carotenoids and chlorophyllous pigments, which increased along the increment of nitrogen rates. Nitrate content in leaves was influenced by both factors and it showed increasing values, when nitrogen doses increased, reaching the highest value under N50-Film B conditions (3312.3 mg kg-1 fw). Our study showed that in the Mediterranean area, the use of greenhouse diffuse light film improved lamb’s lettuce yield, but on the other hand incurred significant increase in nitrate level, nonetheless remaining constantly under the legal threshold imposed by the commission regulation (EU). Secondary metabolites, such as total phenols and carotenoids, showed similar values under both films, instead the diffuse light film improved total ascorbic acid content.

Aerosols affect the gross primary productivity (GPP) of plants by absorbing and scattering solar radiation. However, it is still an open question whether and to what extent the effects of aerosol on the diffuse fraction (Df) can enhance GPP globally. We quantified the aerosol diffuse fertilization effect (DFE) and incorporated it into a light use efficiency (LUE) model, EC-LUE. The new model is driven by aerosol optical depth (AOD) data and is referred to as AOD-LUE. The eddy correlation variance (EC) of the FLUXNET2015 dataset was used to calibrate and validate the model. The results showed that the newly developed AOD-LUE model improved the performance in simulating GPP across all ecosystem types (R2 from 0.6 to 0.68), with the highest performance for mixed forest (average R2 from 0.71 to 0.77) and evergreen broadleaf forest (average R2 from 0.34 to 0.45). The maximum LUE of diffuse photosynthetic active radiation (PAR) (3.61 g C m−2 MJ−1) was larger than that of direct PAR (1.68 g C m−2 MJ−1) through parameter optimization, indicating that the aerosol DFE seriously affects the estimation of GPP, and the separation of diffuse PAR and direct PAR in the GPP model is necessary. In addition, we used AOD-LUE to quantify the impact of aerosol on GPP. Specifically, aerosols impaired GPP in closed shrub (CSH) by 6.45% but enhanced the GPP of grassland (GRA) and deciduous broadleaf forest (DBF) by 3.19% and 2.63%, respectively. Our study stresses the importance of understanding aerosol-radiation interactions and incorporating aerosol effects into regional and global GPP models.

Abstract. China suffers from frequent haze pollution episodes that alter the surface solar radiation and influence regional carbon uptake by the land biosphere. Here, we apply combined vegetation and radiation modeling and multiple observational datasets to assess the radiative effects of aerosol pollution in China on the regional land carbon uptake for the 2009–2011 period. First, we assess the inherent sensitivity of China's land biosphere to aerosol pollution by defining and calculating two thresholds of aerosol optical depth (AOD) at 550 nm, (i) AODt1, resulting in the maximum net primary productivity (NPP), and (ii) AODt2, such that if local AOD < AODt2, the aerosol diffuse fertilization effect (DFE) always promotes local NPP compared with aerosol-free conditions. Then, we apply the thresholds, satellite data, and interactive vegetation modeling to estimate current impacts of aerosol pollution on land ecosystems. In the northeast, observed AOD is 55 % lower than AODt1, indicating a strong aerosol DFE on local NPP. In the southeastern coastal regions, observed AOD is close to AODt1, suggesting that regional NPP is promoted by the current level of aerosol loading, but that further increases in AOD in this region will weaken the fertilization effects. The North China Plain experiences limited enhancement of NPP by aerosols because observed AOD is 77 % higher than AODt1 but 14 % lower than AODt2. Aerosols always inhibit regional NPP in the southwest because of the persistent high cloud coverage that already substantially reduces the total light availability there. Under clear-sky conditions, simulated NPP shows widespread increases of 20–60 % (35.0 ± 0.9 % on average) by aerosols. Under all-sky conditions, aerosol pollution has spatially contrasting opposite sign effects on NPP from −3 % to +6 % (1.6 ± 0.5 % on average), depending on the local AOD relative to the regional thresholds. Stringent aerosol pollution reductions motivated by public health concerns, especially in the North China Plain and the southwest, will help protect land ecosystem functioning in China and mitigate long-term global warming.

Multiple drivers perturb the terrestrial carbon cycle, which ultimately reshapes the fertilization of carbon dioxide (CO2) and reorientates the climate. One such driver is atmospheric aerosols, which cascade the ecosystem’s productivity in a large proportionality. Investigating this relation is non-conventional and limited across the globe. With the abundance of heterogenetic terrestrial ecosystems, India’s primary productivity has a large proportion of the global carbon balance. Under climate change stress, India’s unique spatial and climatological features perturb atmospheric aerosols from natural sources to anthropogenic sources. In light of that, this study utilizes the Carnegie–Ames Stanford Approach (CASA) model to elucidate the consequence by examining the potential effect of aerosol load on the ecosystem productivity (Net Primary Production; NPP) for various agroclimatic zones of India from 2001–2020. CASA reveals a negative decadal amplitude with an overall increase in the NPP trend. In contrast, aerosol loadings from MODIS highlight the increasing trend, with definite seasonal intensities. Employing the CASA model and earth observations, the study highlights the increase in NPP in forest-based ecosystems due to relatively lower aerosols and higher diffuse radiation. Critically, strong dampening of NPP was observed in the agroecological and sparse vegetation zones inferring that the aerosol loadings affect the primary productivity by affecting the photosynthesis of canopy architecture. Spatial sensitivity zones across different ecological regions result in a non-homogenous response because of different phenological and canopy architecture that is mediated by the radiation intensities. Based on the analysis, the study infers that AOD positively influences the canopy-scale photosynthesis by diffuse radiation, which promotes NPP but is less likely for the crop canopy ecosystems. Barring the limitations, enhancement of NPP in the forest ecosystems offset the demand for carbon sink in the agroecosystems. Findings from this study reveal that a more precise provenance of aerosol effects on carbon fluxes is required to understand the uncertainties in the terrestrial carbon cycle.

AbstractDiffuse radiation can improve the efficiency of terrestrial carbon uptake. Both light absorption and canopy light use efficiency (LUE) are affected by the fraction of diffuse radiation (DF). However, the relative contribution of these two factors to the diffuse fertilization effect (DFE) in the short term is not well understood. To investigate the mechanism of DFE in cropland, we collected gross primary productivity, fraction of absorbed photosynthetically active radiation (FAPAR), and other meteorological parameters from June to August in three crop sites. Our results indicated that the short‐term DFE in soybean and maize was primarily driven by the improvement of LUE rather than light absorption. The LUE increased significantly with DF, while the FAPAR changed a little with DF. The increased DF is typically associated with reduced photosynthetically active radiation (PAR). Our results showed that the potential gain in light absorption and canopy LUE from DF could not fully offset the reduced PAR in soybean and maize. The findings in this study contribute to our understanding of the mechanisms underlying the DFE.

Anthropogenic emissions affect vegetation photosynthesis and carbon flux through meteorological variations induced by aerosols and clouds. However, the insufficient consideration of meteorological conditions limits the understanding of relevant mechanisms, and further inhibits the projection of future terrestrial carbon balance. Based on multiple sets of model simulations, we characterized changes in gross primary production (GPP) due to three typical individual pollutants emissions (black carbon, organic carbon, and sulfate), quantified the relative contributions of co-varied environmental factors, and explored the regulatory roles of background meteorological conditions across China. Our results showed that the heterogeneous GPP enhancement induced by emissions was dominated by cloud cover (CC) change. During its short-term effect, air temperature (Tair), vapor pressure deficit (VPD), and radiation (both quality and quantity) played a collectively non-negligible role in GPP variation, among which the universal diffuse radiation fertilization effect was generally far less than the benefits of brighter, cooler, and wetter environmental conditions. However, the sensitivity of GPP to an individual environmental variable was also altered by background meteorological gradients, whose changing pattern differed substantially among factors, indicating that the meteorological-regulated vegetation optimal photosynthetic range was a trade-off among heat, water, and light instead of being controlled by the univariable. This study implies that a deeper understanding of concurrent environmental variables is an effective way to reduce uncertainties in assessing the terrestrial carbon cycle perturbation exerted by human-induced emissions, especially under future scenarios with ongoing climate change.

Il est reconnu que les aérosols atmosphériques d’origine anthropique ont eu un impact significatif sur le système climatique au cours des dernières décennies via leurs interactions avec le rayonnement et les nuages. Outre ces processus physiques bien connus mais mal compris, des études récentes ont fait état de fortes influences des aérosols sur le cycle du carbone, en particulier sur sa composante terrestre. Les changements du cycle du carbone vont alors modifier le climat par le biais de la rétroaction climat-carbone. On ne sait toujours pas bien dans quelle mesure les aérosols anthropiques perturbent le cycle du carbone terrestre. Cette thèse vise à quantifier et à attribuer les impacts des aérosols anthropiques sur le cycle terrestre en utilisant une approche de modélisation. Au chapitre 2, un ensemble de simulations « hors ligne » utilisant le modèle de surfaces continentales ORCHIDEE forcé par les champs climatiques de différents modèles climatiques de la génération CMIP5 ont été réalisées pour étudier les impacts des aérosols anthropiques sur le cycle du carbone terrestre au travers de leurs impacts sur le climat. Les résultats indiquent une augmentation du puits de carbone terrestre de 11,6 à 41,8 PgC cumulé entre 1850 et 2005 en raison des aérosols anthropiques. L'augmentation de la production nette du biome (net biome production, NBP) se situe principalement dans les tropiques et les latitudes moyennes de l’hémisphère nord. Le refroidissement induit par les aérosols est le principal facteur à l'origine de cette évolution de la NBP. Aux hautes latitudes, le refroidissement induit par les aérosols a provoqué une diminution plus forte de la production primaire brute (gross primary production, GPP) que de la respiration totale de l'écosystème (total ecosystem respiration, TER), ce qui a entraîné une baisse de la NBP. Aux latitudes moyennes, la diminution de la TER due au refroidissement est plus forte que celle de la GPP, ce qui entraîne une augmentation nette de la NBP. Aux basses latitudes, la NBP a également augmenté en raison de l'augmentation de la GPP due au refroidissement, mais la diminution des précipitations régionales en réponse aux émissions d'aérosols anthropiques peut annuler l'effet de la température. Comme les modèles de climat sont actuellement en désaccord sur la manière dont les émissions d'aérosols affectent les précipitations tropicales, la modification des précipitations en réponse aux aérosols devient la principale source d'incertitude dans les changements de flux de C causés par les aérosols. Les résultats suggèrent qu'une meilleure compréhension et simulation de la manière dont les aérosols anthropiques affectent les précipitations dans les modèles de climat est nécessaire pour une attribution plus précise des effets des aérosols sur le cycle du carbone terrestre. Le chapitre 3 présente le développement et l'évaluation d'une nouvelle version du modèle ORCHIDEE appelé ORCHIDEE_DF. Par rapport à la version standard d’ORCHIDEE, ORCHIDEE_DF comprend un nouveau module de partitionnement de la lumière pour séparer le rayonnement solaire descendant en ses composantes directe et diffuse, ainsi qu'un nouveau module de transfert radiatif pour simuler la transmission du rayonnement diffus et direct dans la canopée, et différentier l'absorption de la lumière parles feuilles éclairées et ombragées. Le nouveau modèle ORCHIDEE_DF a été évalué à l'aide d'observations de flux par la méthode « eddy covariance » provenant de 159 sites de mesures sur le globe
Anthropogenic atmospheric aerosols have been recognized to have significantly affected the climate system through their interactions with radiation and cloud during the last decades. Besides these well-known butpoorly-understood physical processes in the atmosphere, recent studies reported strong influences of aerosols on the carbon cycle, especially its terrestrial component. The changes in carbon cycle will further alter the climate through the climate-carbon feedback. It remains uncertain how much anthropogenic aerosols perturb the land carbon cycle. This thesis aims to quantify and attribute the impacts of anthropogenic aerosols on the terrestrial cycle using a modeling approach. In Chapter 2, a set of offline simulations using the ORCHIDEE land surface model driven by climate fields from different CMIP5 generation climate models were performed to investigate the impacts of anthropogenic aerosols on the land C cycle through their impacts on climate. The results indicate an increased cumulative land C sink of 11.6-41.8 PgC during 1850-2005 due to anthropogenic aerosols. The increase in net biome production (NBP) is mainly found in the tropics and northern mid latitudes. Aerosol-induced cooling is the main factor driving this NBP changes. At high latitudes, aerosol-induced cooling caused a stronger decrease in gross primary production (GPP) than in total ecosystem respiration (TER), leading to lower NBP. At mid latitudes, cooling‐induced decrease in TER is stronger than for GPP, resulting in a net NBP increase. At low latitudes, NBP was also enhanced due to the cooling‐induced GPP increase, but regional precipitation decline in response to anthropogenic aerosol emissions may negate the effect of temperature. As climate models currently disagree on how aerosol emissions affect tropical precipitation, the precipitation change in response to aerosols becomes the main source of uncertainty in aerosol-caused C flux changes. The results suggest that better understanding and simulation of how anthropogenic aerosols affect precipitation in climate models is required for a more accurate attribution of aerosol effects on the terrestrial carbon cycle